02375nas a2200217 4500008004100000022001400041245015700055210006900212300001400281490000700295520161600302100001701918700001601935700001601951700001601967700001601983700001301999700001802012700002002030856010702050 2025 eng d a2205-887700aTrilobite biostratigraphy of the upper Skullrockian Stage (Lower Ordovician; lower Tremadocian) on the northern Laurentian margin, western United States0 aTrilobite biostratigraphy of the upper Skullrockian Stage Lower  a397–4320 v573 aOngoing field collecting has permitted the development of a high resolution trilobite biostratigraphy of the upper part of the Skullrockian Stage (lower Tremadocian; Lower Ordovician) in shallow water facies along the (Ordovician) northern Laurentian margin. This follows previous work documenting new schemes for the Tulean and Blackhillsian stages (upper Tremadocian and Floian) and Stairsian Stage (mid-Tremadocian). Relevant sections are in the Red Canyon Member of the House Formation in the Ibex area, Millard County, western Utah, and in the Garden City Formation, Bear River Range, Franklin County, southeast Idaho. The interval under study was previously assigned to the genus-based “Bellefontia-Xenostegium Zone.” This is replaced with seven formally proposed species level zones, all of which are new in concept. Each zone is characterised by a set of species mostly exclusive to it, and turnover between zones is extensive, with only a limited number of species occurring in more than one zone. Turnover rates are high, as in the most fossiliferous section (Lava Dam North in the southern House Range, western Utah) the seven zones occur through less than 75 m of section. The new zones in ascending order are the Praepatokephalus housensis Zone, Skullrockicurus plummeri Zone, Parabellefontia concinna Zone, Politicurus edwardsi Zone, Bellefontia ibexensis Zone, Politicurus politus Zone, and Rossicurus lepidus Zone. Atop the R. lepidus Zone is the Paraplethopeltis genacurva Zone, the lowest zone of the overlying Stairsian Stage. Three of the name-bearing species of the new z​o​n​e​1 aAdrian, J.D.1 aWestrop, J.1 aLanding, E.1 aKarim, T.S.1 aLosso, S.R.1 aNg, R.Y.1 aBradley, A.B.1 aPerez-Peris, F. uhttps://www.nysm.nysed.gov/staff-publications/trilobite-biostratigraphy-upper-skullrockian-stage-lower03212nas a2200217 4500008004100000245017200041210006900213300000900282490000800291520232300299653001702622653001302639653003202652653002402684653001302708653001302721100002202734700001802756700002102774856019902795 2024 eng d00aTwo new species of lichenicolous Arthonia (Arthoniaceae) from southeastern North America highlight the need for comparative studies of lichen parasites and their hosts0 aTwo new species of lichenicolous Arthonia Arthoniaceae from sout a1-210 v1273 a

Arthonia frostiicola and A. galligena are described as new to science based on collections from mountainous regions of southeastern North America. Arthonia frostiicola infects the saxicolous lichen Dirinaria frostii, producing emarginate black apothecia which erupt from within the host thallus. It is characterized by a dark hypothecium and 1-septate, obovoid ascospores which turn brownish and verruculose in age. It is known from five collections made in the southern Appalachian Mountains and Ozark Mountains in southeastern North America. Arthonia galligena produces galls in the thallus and apothecia of the corticolous lichens Lecanora masana and L. rugosella, and is apparently endemic to the high elevations of the southern Appalachian Mountains. It is characterized by a variably pigmented, pale to red-brown hypothecium and 2-septate, macrocephalic ascospores which turn brownish and verruculose in age. Keys to the species of Arthonia on Caliciales and Lecanoraceae are provided.

10abiodiversity10aendemism10ahost-parasite relationships10alichenicolous fungi10aNew taxa10ataxonomy1 aHollinger, J., P.1 aScott, P., A.1 aLendemer, J., C. uhttps://bioone.org/journals/the-bryologist/volume-127/issue-1/0007-2745-127.1.001/Two-new-species-of-lichenicolous-Arthonia-Arthoniaceae-from-southeastern-North/10.1639/0007-2745-127.1.001.short01873nas a2200157 4500008004100000022001400041245007100055210006900126300001400195490000800209520137700217100001901594700001901613700001601632856006701648 2024 eng d a0305-871900aA tectonic solution for the Early Cambrian palaeogeographic enigma0 atectonic solution for the Early Cambrian palaeogeographic enigma a167 - 1770 v5423 a
The Early Cambrian paleogeographic enigma arises when tectonic reconstructions are made using palaeoclimatic versus palaeomagnetic data that result in possibly contradictory tropical, mid-latitude, and south polar locations for major continents. For example, northwest Africa and Cadomia may have lain in a tropical zone (0° to +/−30° latitude) based on the presence of archaeocyath reefs, minor evaporites, and carbonate platforms at ca. 520 Ma +/− 5 Ma or, alternatively, northwest Africa and Cadomia may have lain in a south polar zone (90° to 60° south latitude) based on palaeomagnetic constraints. Greater Avalonia may have evolved independently from northwest Africa if a dropstone constraint implying polar latitudes at ca. 530 Ma and a palaeomagnetic constraint implying ca. 50° latitude at ca. 505 Ma are accommodated. We show here how counter-clockwise rotation of Gondwana during the Cambrian about an interior axis may solve the enigma. Gondwanan apparent polar wander becomes consistent with tropical conditions inferred for northwest Africa when adjusted to accommodate constraints placing the south pole near Peru for ca. 540–520 Ma. Concurrent counter-clockwise rotation of Baltica and Gondwana during the Middle Cambrian may have facilitated separation of Greater Avalonia from Baltica across dextral shear zones.
1 aKeppie, D., F.1 aKeppie, J., D.1 aLanding, E. uhttps://www.lyellcollection.org/doi/abs/10.1144/SP542-2022-35501477nas a2200157 4500008004100000022001400041245017000055210007100225260001600296520082100312100001601133700001801149700001601167700002101183856011501204 2024 eng d a0040-026200aTypification of the Lace Lichen,Ramalina menziesii Taylor—and its synonyms—reiterates the need for complete typification of names for well‐known or iconic taxa0 aTypification of the Lace LichenRamalina menziesii Taylor—and its cSep-04-20253 a

A lectotype is designated for the name of the iconic and well-known macrolichen Ramalina menziesii Taylor from among a suite of largely overlooked syntypes deposited in the Thomas Taylor Herbarium at the Farlow Herbarium, Harvard University. Lectotypes are also selected for the synonyms of R. menziesii: Chlorodictyon foliosum, Ramalina reticulata (≡ Lichen reticulatus Noehd., nom. illeg.) and R. retiformis. The place of publication of L. reticulatus Noehd. is discussed in detail. The case highlights the surprising degree to which the application of names for taxa that have been extensively studied and are widely known outside a narrow specialist field, can remain unresolved.

1 aLaGreca, S.1 aTocci, G., E.1 aBriscoe, L.1 aLendemer, J., C. uhttps://onlinelibrary.wiley.com/doi/10.1002/tax.13164https://onlinelibrary.wiley.com/doi/pdf/10.1002/tax.1316401978nas a2200145 4500008004100000022001400041245018200055210006900237490000800306520140600314100001601720700001601736700001901752856006101771 2024 eng d a0305-871900aTerminal Ediacaran-Late Ordovician evolution of the NE Laurentia palaeocontinent: rift–drift-onset of Taconic orogeny, sea-level change, and ‘Hawke Bay’ onlap (not offlap)0 aTerminal EdiacaranLate Ordovician evolution of the NE Laurentia 0 v5423 a
Rodinia breakup with late Ediacaran rifting defined a NE Laurentia triple junction (New York Promontory-Ottawa-Bonnechere aulacogen (OBA)-Quebec Reentrant). Rifting persisted to c. 510 Ma. The oldest passive margin shelf units (Forestdale, Moosalamoo) underlie a sandstone (Cheshire) commonly regarded as the oldest passive unit. Late Dyeran–Middle Cambrian rifting led to the oldest OBa sedimentation and formed the Franklin Basin (NW Vermont). Cambrian-Darriwillian shelf-slope facies are linked eustatically-not Taconic orogeny onset. Onlap and shelf carbonates are coeval with black slope mud; lowstand shelf unconformities with green, oxic slope mud. Early-middle Dyeran eustatic change defined slope units: 1) Browns Pond dysoxic/anoxic (d/a) interval with debrite cap (Holcombville Member, new); 2) Middle Granville oxic interval (new); and 3) lower Hatch Hill d/a interval. Our analysis leads to two controversial conclusions: (i) existence of the Dashwoods and other micro-continental blocks due to hyper-extension is not supported by cover sequences linking Laurentia to proposed Dashwoods areas (i.e., Green Mountains) and an arc origin of the type Dashwoods, and (ii) ‘Hawke Bay Event(s),’ widely interpreted as Cambrian global regressive event(s), is a local HST facies with shelf sand by-pass onto the Hatch Hill slope in its NE Laurentia type region.
1 aLanding, E.1 aWebster, M.1 aBowser, S., S. uhttps://www.lyellcollection.org/doi/10.1144/SP542-2023-400526nas a2200109 4500008004100000245003700041210003700078300001200115490000800127100002100135856026000156 2024 eng d00aTorrey Monograph Award Recipient0 aTorrey Monograph Award Recipient a229-2300 v1511 aLendemer, J., C. uhttps://bioone.org/journals/the-journal-of-the-torrey-botanical-society/volume-151/issue-4/1095-5674-151.4.229/Torrey-Monograph-Award-Recipient/10.3159/1095-5674-151.4.229.full?casa_token=p-9sgSojuH8AAAAA:vNeWFT7CxQO_BXXN42gEXhR20ShyFolRq_GSOmUi9Y2KGZ7Xh202109nas a2200217 4500008004100000022001400041245006600055210006600121260001600187300001600203490000900219520148200228100001201710700001801722700001801740700001201758700001401770700001601784700001601800856007501816 2024 eng d a0016-764900aTesting the salinity of Cambrian to Silurian epicratonic seas0 aTesting the salinity of Cambrian to Silurian epicratonic seas cJul-02-2025 ajgs2023-2170 v20243 a

Ancient epicratonic formations, which represent the bulk of pre-Jurassic sedimentary rocks, have been widely interpreted as marine deposits, but recently developed bulk-shale elemental proxies for paleo-watermass salinity (i.e., B/Ga, Sr/Ba, and S/TOC) have shown this inference to be frequently incorrect. Here, we use these proxies to test the salinity conditions of 22 representative shale and marl formations of early Cambrian to early Silurian age from five cratons (Laurentia, Avalonia, Baltica, Iran and South China) in the context of formation-specific paleogeographic and paleoclimatic reconstructions. Our dataset shows that around half of these formations were probably deposited under brackish or mixed brackish-marine conditions rather than fully marine conditions (as previously inferred), and that one of them represents a freshwater facies (previously interpreted as marine mainly on the basis of Cruziana traces). In most cases, the development of reduced-salinity conditions can be related to the coastal and/or humid climate belt setting in which the formation of interest was deposited. Our dataset also reveals systematically low Sr/Ba values (i.e., relative to modern brackish and marine facies), suggesting that seawater Sr concentrations were lower during the Early Paleozoic than in the modern. Our findings suggest that re-evaluation of the salinity characteristics of many ancient epicratonic shale and marl formations is necessary.

1 aLiu, Z.1 aAlgeo, T., J.1 aArefifard, S.1 aWei, W.1 aBrett, C.1 aLanding, E.1 aLev, S., M. uhttps://geoscienceworld.org/jgs/article-lookup?doi=10.1144/jgs2023-21700415nas a2200109 4500008004100000245011900041210006900160300001400229490000800243100001400251856004000265 2023 eng d00aTerrorism in American Memory: Memorials, Museums, and Architecture in the Post-9/11 Era by Marita Sturken (review)0 aTerrorism in American Memory Memorials Museums and Architecture  a453 - 4550 v1041 aNoble, A. uhttps://muse.jhu.edu/article/91828601926nas a2200193 4500008004100000245010500041210006900146260001600215300001400231490000600245520124400251653003501495653003201530653002201562653002301584653003701607100001701644856007101661 2022 eng d00aTracing Maize History in Northern Iroquoia Through Radiocarbon Date Summed Probability Distributions0 aTracing Maize History in Northern Iroquoia Through Radiocarbon D cAug-16-2022 a594 - 6070 v83 a

The evolution of maize as an organism, its spread as an agricultural crop, and the evolution of Native American maize-based agricultural systems are topics of research throughout the Western Hemisphere. Maize was adopted in Northern Iroquoia, comprising portions of present-day New York, Ontario, and Québec by 300 BC. By the fourteenth-century AD, maize accounted for >50 to >70% of ancestral Iroquoian diets. Was this major commitment to maize agriculture a gradual incremental evolution, or was there a rapid increase in commitment to maize-based agriculture around AD 1000 as traditional archaeological narratives suggest? Summed probability distributions of direct radiocarbon dates on maize macrobotanical remains and cooking residues containing maize phytoliths combined with maize macrobotanical maize densities at sites and previously published stable isotope values on human bone collagen used with Bayesian dietary mixing models and cooking residues show an initial increase in maize use at AD 1200–1250 and a subsequent increase at AD 1400–1450. These results indicate maize history in Northern Iroquoia followed an exponential growth curve, consistent with Rindos’ (1984) model of agricultural evolution.

10aBayesian dietary mixing models10amaize agriculture evolution10anorthern Iroquoia10aradiocarbon dating10asummed probability distributions1 aHart, J., P. ufhttps://www.degruyter.com/document/doi/10.1515/opar-2022-0256/xml02359nas a2200145 4500008004100000022001400041245019700055210007100252260001600323520176300339100001602102700002002118700001402138856006102152 2022 eng d a0008-407700aTrans-Avalonian green–black boundary (early Middle Cambrian): transform fault-driven epeirogeny and onset of 26 m.y. of shallow marine anoxia in Avalonia (Rhode Island–Belgium) and Baltica0 aTransAvalonian green–black boundary early Middle Cambrian transf cJun-08-20243 a

The Avalonia microcontinent has diagnostic terminal Ediacaran–Ordovician lithostratigraphy, depositional sequence architecture, and igneous activity that extends for 2000+ km and reflects epeirogeny related to the Avalonian transform fault. Avalonia records an abrupt early Middle Cambrian (late Wuliuan) change from green, purple, or light grey to overlying black, dark grey, and brown facies in platform and off-platform areas (Meguma, North Wales). This change within one trilobite zone marks onset of ca. 26 m.y. of shallow-marine anoxia/strong dysoxia lasting into the Ordovician with Hatch Hill OMZ onlap onto the shelf. A Bakken model (new, based on the middle Paleozoic Bakken Formation) is applied to shallow-shelf–shoreline organic-rich mud deposition. Erosion of greenish Avalonian depositional sequence (Ads) 7 was followed by Ads 8 tilting, volcanism, debris flows, and bentonite deposition on a cryptic unconformity in SE Newfoundland. The early Middle Cambrian age of the Ads 7–8 boundary is obscured by referring the lower Manuels River Formation and Cristallinium cambriense Zone to the younger Drumian Stage. Ads 8 has thin ashes in coterminous British and American Avalonia where erosion and subaerial exposure with caliche development preceded onlap of upper Middle or Upper Cambrian Ads 9 black muds and sands. The green–black change emphasizes Avalonian unity; it precludes multiple Avalonian “micro-terranes” or assigning parts of Avalonia to West Gondwana or “Ganderia” (the Little River, Brookville, and Bras d’Or “terranes” are part of the Avalonian marginal platform). Coeval green–black transitions and similar later Cambrian faunas show comparable paleoenvironments in Avalonia and Baltica. 

1 aLanding, E.1 aWestrop, S., R.1 aGeyer, G. uhttps://cdnsciencepub.com/doi/pdf/10.1139/cjes-2022-006502612nas a2200301 4500008004100000022001400041245025200055210006900307260001200376300001300388490000700401520158200408653001301990653001302003653003002016653001802046653001002064653001102074653002002085653001902105653002602124653001402150653001802164653002502182100001602207700001602223856007102239 2021 eng d a1042-094000aTrace fossils, depositional context, and paleogeography of the upper Tal Group (upper lower Cambrian), Lesser Himalaya, India: a Gondwanan succession with no affinities to the Avalonia microcontinent – discussion of paper by Singh et al. (2019)0 aTrace fossils depositional context and paleogeography of the upp c11/2020 a143-156 0 v283 a

Terminal Ediacaran–late early Cambrian deposition, faunas and passive margin evolution of the north Indian margin are recorded in the Nigali Dhar syncline succession. Restudy of the upper Tal Group (upper lower Cambrian Koti Dhaman Formation, KDF) ichnofauna from the Khud-Drabil section reduces it to 18 confidently named forms. The lower KDF (Lower Quartzite Member) Cruziana-Rusophycus assemblage is in subtidal (not intertidal) sandsheet facies. The overlying black Shale Member (SM) records trans-East Gondwanan deepening, not intertidal facies, in the Palaeolenus Zone. The SM, with low diversity Planolites-Palaeophycus assemblage, is overlain by subtidal (not intertidal) sandsheet facies of the middle KDF (Arkosic Sandstone Member, ASM) with shallow burrowers and furrowers (Gordia marina assemblage, new; Cruziana ichnofacies). KDF faunas with Cruziana and Rusophycus are similar to coeval, shallow marine associations elsewhere in Gondwana and NW Laurentia. Interpretation of a second KDF section 20 km from Khud-Drabil has confused an understanding of Lesser Himalaya geologic evolution as it claims Ordovician Cruziana species in the ASM and an angular SM–ASM unconformity caused by the Cambrian–Ordovician boundary Kurgiakh orogeny. However, upper lower Cambrian microfaunas occur in and above the ASM, while the angular SM–ASM unconformity is consistent with submarine sliding. KDF-type ichnofaunas do not show a tropical location of Avalonia, which has the distinctive lithofacies and biotas of a high-latitude continent unrelated to Gondwana.

10aAvalonia10aCambrian10adepositional environments10aEast Gondwana10aIndia10aIsrael10aLesser Himalaya10apaleogeography10asequence stratigraphy10aTal Group10atrace fossils10aupper Lower Cambrian1 aLanding, E.1 aGeyer, Gerd uhttps://www.tandfonline.com/doi/full/10.1080/10420940.2020.184345700556nas a2200133 4500008004100000245009500041210006900136260002100205490000900226100001400235700002300249700002100272856012900293 2020 eng d00aTribes mount organized responses to COVID-19, in contrast to state and federal governments0 aTribes mount organized responses to COVID19 in contrast to state bThe Conversation0 v20201 aHardy, L.1 aSaul, Gwendolyn, W1 aThompson, K., F. uhttps://theconversation.com/tribes-mount-organized-responses-to-covid-19-in-contrast-to-state-and-federal-governments-15062700390nas a2200109 4500008004100000245009300041210006900134300001400203490000800217100001500225856004000240 2020 eng d00aTeach NY: Exploring Haudenosaunee Influence on America's Suffrage Movement with Students0 aTeach NY Exploring Haudenosaunee Influence on Americas Suffrage  a377 - 3820 v1011 aWeller, K. uhttps://muse.jhu.edu/article/77554201907nas a2200205 4500008004100000022001400041245012600055210006900181300001600250490000700266520125400273653001301527653001601540653001501556653001501571653001901586100001901605700002201624856005501646 2019 eng d a1866-955700aTesting the effectiveness of osteometrics in the identification of North American gallinaceous bird post-cranial elements0 aTesting the effectiveness of osteometrics in the identification  a2623–26360 v113 a

Galliformes, or game birds, are an order of birds commonly utilized by people and are regularly found in zooarchaeological assemblages. Morphological and size similarities make many galliforms difficult to distinguish from each other, thereby prohibiting specific identification of these taxa. Non-identified bones lead to a decrease in information available about archeological sites, particularly for bird species which provide a wealth of information about the economy and environment of historic and prehistoric sites. In this paper, we test the effectiveness of osteometrics in nine North American gallinaceous species to assess their utility for identifying post-cranial skeletal elements to genus or species. Statistical analysis of measurements successfully separated several Phasianidae subfamilies and identified the largest (turkey) and smallest (quail) species. Measurements driving variation between taxa were primarily long bone length and epiphyseal breadth. Few elements showed statistically significant differences within Tetraoninae and Phasianinae clades. We suggest that zooarchaeologists adopt long bone metrics as a standard, complementary technique to traditional morphological identifications for unknown galliforms.

10aAvifauna10aGalliformes10aOsteometry10aPhasianids10aZooarchaeology1 aWatson, J., E.1 aHeins-Ledogar, S. uhttp://link.springer.com/10.1007/s12520-018-0697-403228nas a2200301 4500008004100000022001400041245011700055210006900172260001600241300001100257490000600268520226200274653002402536653001902560653003002579653002202609653001102631653002502642653002302667653002002690653002402710653002002734653002902754100002702783700002502810700002102835856007002856 2018 eng d a2150-892500aTesting the predictive capabilities of ecological niche models: a case study examining Red‐bellied Woodpeckers0 aTesting the predictive capabilities of ecological niche models a cDec-12-2018 ae024960 v93 a

As humans continue to alter natural habitats indirectly and directly, species’ geographic ranges may change as they track shifting climate regimes or changing landscapes. Ecological niche models (ENMs) are frequently used to show modern ranges and forecast future range changes. These models, however, assume that a species will exhibit niche conservatism, though this is rarely tested. Here, we examine a woodpecker species with a well‐documented recent range expansion to assess the effectiveness of predictive models by comparing the pre‐ and post‐expansion climate/habitat niche using ENMs and multivariate principal components analysis. Occurrence data for the Red‐bellied Woodpecker (Melanerpes carolinus) were obtained from the pre‐expansion (1910–1939; n = 299) and post‐expansion (1980–2009; n = 868) time periods. Ecological niche models were constructed using GIS layers describing climate data and crop cover for the pre‐ and post‐expansion time periods. We then used the pre‐expansion ENM to forecast the distribution of Red‐bellied Woodpeckers into the post‐expansion time period, and vice versa, and calculated the niche overlap of the projected distributions and the actual distributions in those time periods to determine whether pre‐ and post‐expansion niches were similar. Predictive ENMs did not closely match the actual distributions in the pre‐ and post‐expansion time periods, respectively, and the pre‐expansion and post‐expansion niches were significantly different from each other (Schoener's D = 0.745, P < 0.001). Multivariate analyses revealed that the present‐day niche encompasses the past niche and that Red‐bellied Woodpeckers today have broader temperature and precipitation tolerances and are found in both more‐ and less‐forested areas than they were in the pre‐expansion era. Our analyses reveal that Red‐bellied Woodpeckers are not exhibiting climate or habitat niche conservatism, explaining why predictive ENMs for this species could not effectively track their range shift. This study emphasizes that predictive models may not be effective for species undergoing niche changes.

10aCarolinian avifauna10aclimate change10aecological niche modeling10aland cover change10aMaxent10aMelanerpes carolinus10aniche conservatism10aniche expansion10apredictive modeling10arange expansion10aRed‐bellied Woodpecker1 aFitzGerald, Alyssa, M.1 aStarkloff, Naima, C.1 aKirchman, J., J. uhttps://esajournals.onlinelibrary.wiley.com/doi/10.1002/ecs2.249601130nas a2200121 4500008004100000245010300041210006900144300000900213490000700222520072500229100001600954856003800970 2018 eng d00aTropical Weathering of the Taconic Orogeny (i.e., “orogen”) as a Driver for Ordovician Cooling0 aTropical Weathering of the Taconic Orogeny ie orogen as a Driver ae4360 v463 a

Swanson-Hysell and Macdonald (2017) follow Kump et al.’s (1999) proposal that decreasing temperatures through the Ordovician (e.g., Trotter et al., 2008) are largely explained by CO2 sequestration with weathering of silicates exposed by Taconic arc-Laurentia collision. They propose higher weatherability of the west-east‒trending Taconic orogen that they shift to a more equatorial, wet-tropical setting. The concerns that may be raised by a reader are whether the following are all responses to this orogeny: (1) the Ordovician temperature record, (2) the strontium and neodymium isotope record interpreted to reflect the Taconic orogeny (Swanson-Hysell and Macdonald, 2017), and (3) the interpreted pCO2.

1 aLanding, E. uhttps://doi.org/10.1130/G39987C.102587nas a2200205 4500008004100000245013300041210006900174300001200243490000700255520190300262653001202165653001702177653001702194653001702211653001402228100001802242700002002260700001802280856008302298 2017 eng d00aTrace Element Analysis Provides Insight into the Diets of Early Late Miocene Ungulates from the Rudabánya II Locality (Hungary)0 aTrace Element Analysis Provides Insight into the Diets of Early  a231-2430 v153 a

The early Late Miocene vertebrate locality of Rudabánya II (R. II) in northeastern Hungary preserves an abundance of forest-adapted ungulate species. To better understand the ecological relationships within this ancient ecosystem, we used analysis of enamel strontium/calcium (Sr/Ca) ratios to infer dietary preferences. The goals of the analysis were to: i) determine whether these ungulate species specialized in specific plants or plant parts; ii) discern whether the Sr/Ca ratios support what was previously suggested about the ecology of these species; and iii) evaluate the factors that may have acted to promote coexistence within this diverse community of predominantly browsing herbivores. Results show significant differences in the diets of the sampled species. The highest Sr/Ca ratios were displayed by the suids Parachleuastochoerus kretzoii [B1] and Propotamochoerus palaeochoerus implying a preference for Sr-rich underground plant parts. Elevated Sr/Ca ratios yielded by the cervid Lucentia aff. pierensis and equid Hippotherium intrans are indicative of intermediate feeding. The bovid Miotragocerus sp. showed higher Sr/Ca ratios than the gomphothere Tetralophodon longirostris, which is incongruent with morphological and stable isotope data, and suggested browsing by both taxa. This finding is likely the result of a difference in digestive physiology (ruminant vs. monogastric) rather than a difference in dietary behaviour. The lowest Sr/Ca ratios were displayed by the traguild Dorcatherium naui and moschid Micromeryx flourensianussuggesting a preference for Sr-poor fruits. Resource specialization and partitioning within the local environment likely acted to decrease interspecific competition and promote coexistence within the diverse ungulate community at R. II.

10aHungary10aLate Miocene10apaleoecology10aSr/Ca ratios10aUngulates1 aEastham, L.C.1 aFeranec, R., S.1 aBegun, D., R. uhttp://revistes.ub.edu/index.php/GEOACTA/article/view/GeologicaActa2017.15.3.602970nas a2200313 4500008004100000022001400041245010700055210006900162300000700231490000700238520208600245653001702331653001302348653001302361653002402374653001202398653001102410653001302421653001702434653001702451653001502468653001302483100002702496700002602523700001802549700002102567700002302588856004502611 2017 eng d a1712-656800aTaxonomy and distribution of the imperilled Newfoundland Gray-cheeked Thrush, Catharus minimus minimus0 aTaxonomy and distribution of the imperilled Newfoundland Grayche a100 v123 a

Gray-cheeked Thrushes breeding on Newfoundland are purported to be a distinct subspecies (Catharus minimus minimus) and have declined precipitously since the 1980s. To assess the validity of Gray-cheeked Thrush subspecies we collected blood samples and morphological measurements from 51 individuals captured at 15 sites in Newfoundland and Labrador (2013–2015). Analysis of mitochondrial (ND2) and nuclear intron (ADAM-TS 6, FIB7) sequences from these and additional samples from Nova Scotia, Newfoundland, Labrador, Quebec, Alaska, and Siberia showed low genetic variation at both nuclear loci, and shallow mitochondrial divergence between subspecies; there were no shared haplotypes between thrushes from Newfoundland / Nova Scotia (n = 41) and those from western Labrador and further west (n = 24). Thrushes from Newfoundland also had shorter wing chords, tails, and culmens and less black in the mandible compared to those from western Labrador and Quebec. Samples from the southeast coast of Labrador (n = 13) included ND2 haplotypes both from Newfoundland and western Labrador plus one putative hybrid that was phenotypically a Gray-cheeked Thrush but that had a Bicknell’s Thrush (C. bicknelli) ND2 haplotype and was heterozygous at a segregating site in FIB7. We detected thrushes during point counts at 7 of 24 sites on Newfoundland, but failed to detect them at 10 historically occupied sites on Newfoundland or in the reported distribution gap between subspecies in Labrador. Sites where thrushes have apparently disappeared had less shrub habitat within 1250 m and more large broadleaf trees within territory-scale areas compared to sites where they persist. Additionally, red squirrels (Tamiasciurus hudsonicus) are an introduced species on Newfoundland and thrush occurrence was > 3x higher at sites where red squirrels were not detected. Our results support previous designations of C. m. minimus from Newfoundland and southeastern Labrador as a subspecies distinct from C. m. aliciae found further west.

10adistribution10aendemism10agenetics10aGray-cheeked Thrush10ahabitat10ahybrid10aLabrador10aNewfoundland10ared squirrel10asubspecies10ataxonomy1 aFitzGerald, Alyssa, M.1 aWhitaker, Darroch, M.1 aRalston, Joel1 aKirchman, J., J.1 aWarkentin, Ian, G. uhttp://www.ace-eco.org/vol12/iss1/art10/03014nas a2200301 4500008004100000022001300041245007300054210006900127260001600196300001200212490000700224520218800231653001102419653001302430653002002443653001302463653001102476653001202487653001702499653001702516100002202533700002102555700001602576700002102592700002302613700001902636856005702655 2017 eng d a0567792000aTerreneuvian Stratigraphy and Faunas from the Anabar Uplift, Siberia0 aTerreneuvian Stratigraphy and Faunas from the Anabar Uplift Sibe cMay-31-2017 a311-4400 v623 a

Assemblages of mineralized skeletal fossils are described from limestone rocks of the lower Cambrian Nemakit-Daldyn, Medvezhya, Kugda-Yuryakh, Manykay, and lower Emyaksin formations exposed on the western and eastern flanks of the Anabar Uplift of the northern Siberian Platform. The skeletal fossil assemblages consist mainly of anabaritids, molluscs, and hyoliths, and also contain other taxa such as Blastulospongia, Chancelloria, Fomitchella, Hyolithellus, Platysolenites, Protohertzina, and Tianzhushanella. The first tianzhushanellids from Siberia, including Tianzhushanella tolli sp. nov., are described. The morphological variation of Protohertzina anabarica and Anabarites trisulcatus from their type locality is documented. Prominent longitudinal keels in the anabaritid Selindeochrea tripartita are demonstrated. Among the earliest molluscs from the Nemakit-Daldyn Formation, Purella and Yunnanopleura are interpreted as shelly parts of the same species. Fibrous microstructure of the outer layer and a wrinkled inner layer of mineralised cuticle in the organophosphatic sclerites of Fomitchella are reported. A siliceous composition of the globular fossil Blastulospongia is reported herein and a possible protistan affinity similar to Platysolenites is discussed. New carbon isotope data facilitate correlation both across the Anabar Uplift and with the Terreneuvian Series of the IUGS chronostratigraphical scheme for the Cambrian System. The base of Cambrian Stage 2 is provisionally placed herein within the Fortunian‒Cambrian Stage 2 transitional interval bracketed by the lowest appearance of Watsonella crosbyi and by a slightly higher horizon at the peak of carbon isotope excursion Iʹ from western flank of the Anabar Uplift. Correlation across the Siberian Platform of the fossiliferous Medvezhya and lower Emyaksin formations showing δ13Ccarb excursion Iʹ with the upper Sukharikha Formation containing excursion 5p and upper Ust’-Yudoma Formation containing excursion I is supported herein.

10aAnabar10aCambrian10aCarbon isotopes10aMollusca10aRussia10aSiberia10astratigraphy10aTerreneuvian1 aKouchinsky, Artem1 aBengtson, Stefan1 aLanding, E.1 aSteiner, Michael1 aVendrasco, Michael1 aZiegler, Karen uhttp://www.app.pan.pl/article/item/app002892016.html03427nas a2200253 4500008004100000022001400041245014400055210006900199300001400268490000700282520262900289653001602918653002202934653001702956653001202973653001702985653001803002653000803020100002203028700001903050700002503069700001903094856006003113 2017 eng d a0008-447600aTexture, Crystal Structure, and Composition of Fluorapatites From Iron Oxide-Apatite (Ioa) Deposits, Eastern Adirondack Mountains, New York0 aTexture Crystal Structure and Composition of Fluorapatites From  a399 - 4170 v553 a

The iron oxide-apatite (IOA) deposits of the eastern Adirondack Mountains consist of intrusive sheets or dikes of magnetite, fluorapatite, augitic pyroxene, quartz, and microcline. Other trace mineral phases include ilmenite with hematite exsolution, V-rich titanite rimming magnetite, zircon, monazite-(Ce), stillwellite-(Ce), lanthanite-(Ce), allanite-(Ce), and thorite. Observations under transmitted light show polygonal and cumulate textures. The ore bodies, each with knife-edge contacts with the host gneisses, are closely associated in time with A-type leucogranites and granitic gneisses (ca. 1070–1050 Ma). Backscattered electron (BSE) images highlight the following types of fluorapatite-monazite-(Ce) relations that formed as a result of metamorphism and fluid-rock interaction: (1) areas of relatively low BSE intensities containing tiny secondary monazite-(Ce) and thorite crystals developed within brighter apatite grains and along crystal margins and fractures; (2) areas of low BSE intensity within larger fluorapatite grains; (3) oriented rods of quartz in fluorapatite; (4) monazite-(Ce) rimming fluorapatite; and (5) multi-domain clusters of fluorapatite in unzoned fluorapatite.

Fluorapatite samples from these IOA deposits were analyzed by electron microprobe and laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) for major and trace elements. All grains contain high concentrations of light and heavy rare earth elements and yttrium, and samples from some deposits are exceptionally enriched in heavy rare earth elements and yttrium. The crystal structures of the fluorapatites from Cheever, Mineville, Palmer Hill, Arnold Hill, and Rutgers mine were analyzed. Rare earth elements (REE) are dominant at the Ca2 site, and in the most REE-rich sample, from Cheever, 5.7% of the Ca2 sites and 3.5% of the Ca1 sites are occupied by REEs. We consider that the most likely geological scenario for the incorporation of the REEs in fluorapatite includes high concentrations of incompatible elements in a dense iron- and phosphorus-rich melt that formed by immiscibility with the silicate melt of the Lyon Mountain granite. The high REE concentration appears to have been accommodated in the fluorapatite structure through a coupled substitution with Si4+. A later, low-temperature stage of fluid infiltration, probably at greenschist facies conditions, re-mobilized the REE and produced secondary minerals within the ore, including low-actinide bearing monazite-(Ce), tremolite, ferro-actinolite, chlorite, rutile, and hematite.

10aAdirondacks10aCheever Mineville10afluorapatite10aGranite10aIOA deposits10aLyon Mountain10aREE1 aLupulescu, M., V.1 aHughes, J., M.1 aChiarenzelli, J., R.1 aBailey, D., G. uhttp://www.canmin.org/lookup/doi/10.3749/canmin.160005701647nas a2200121 4500008004100000245012800041210006900169300001100238490000700249520113800256100002301394856010801417 2016 eng d00a“To our Inn we March’d Away”: Public Contexts for Consuming Alcohol and Tobacco in a Small Chesapeake Town, 1690-17200 aTo our Inn we March d Away Public Contexts for Consuming Alcohol a93-1150 v323 a

Historical archaeology has been interested in public drinking houses since its beginnings. Even with the support of years of archaeological case studies, significant challenges remain in making a connection between the material culture recovered from the archaeological record and the operation of a drinking house. Most scholarship accepts the importance of drinking houses, or ordinaries, in the Chesapeake, in the social, political, and economic development of the region. In many ways the experience and social fabric of early Chesapeake towns are synonymous with the ordinary. A constructive approach to defining the place of ordinaries in the early modern Chesapeake requires considerable interpretive flexibility. Contrasting the historical and archaeological data on the ordinaries in Charles Town (1684-1721), Prince George’s County, Maryland, illustrates the methodological difficulties in triangulating among these sources, but also the capacity for archaeology to tangibly demonstrate how social drinking and smoking structured the broader landscape of public interaction in the early modern Chesapeake region.

1 aLucas, Michael, T. uhttps://www.nysm.nysed.gov/staff-publications/our-inn-we-march-d-away-public-contexts-consuming-alcohol02085nas a2200217 4500008004100000245013600041210006900177300001400246490000700260520131700267653001701584653002201601653001801623653004201641653003101683100001901714700002001733700001801753700001601771856008001787 2014 eng d00aTrilobite Biostratigraphy of the Stairsian Stage (upper Tremadocian) of the Ibexian Series, Lower Ordovician, Western United States0 aTrilobite Biostratigraphy of the Stairsian Stage upper Tremadoci a167–2140 v453 a

New field collections from sections in western Utah and southeastern Idaho permit the development of a high resolution trilobite biostratigraphy for the northern Laurentian Lower Ordovician (upper Tremadocian) Stairsian Stage similar to that proposed previously for the overlying Tulean and Blackhillsian stages. Four zones recognised previously are replaced with 11 formally proposed zones, most of which are new in concept. The new zonal scheme in ascending order includes the 'Paraplethopeltis genacurva' Zone (replaces 'Paraplethopeltis Zone'/'Zone C'), 'Paraplethopeltis helli' Zone (new), 'Hystricurus zanderi' Zone (new), 'Rossaspis leboni' Zone (new), Unnamed Zone 1 (new), 'Bearriverops loganensis' Zone (new; contains much of the diversity previously assigned to 'Tesselacauda Zone'/'Zone E'), 'Bearriverops deltaensis' Zone (new), 'Bearriverops alsacharovi' Zone (new), 'Pseudoclelandia weymouthae' Zone (new), 'Pseudoclelandia cornupsittaca' Zone (new) and 'Pseudohystricurus obesus' Zone (new). The latter two zones were previously lumped as the 'Rossaspis superciliosa Zone'/'Zone F'. Four of the name bearers of the new zones, 'Paraplethopeltis helli' sp. nov., 'Hystricurus zanderi' sp. nov., 'Rossaspis leboni' sp. nov. and 'Pseudoclelandia weymouthae' sp. nov., are formally described.

10apaleontology10aSpecies diversity10aStratigraphic10aTrilobites--Collectors and collecting10aTrilobites--Type specimens1 aAdrain, J., M.1 aWestrop, S., R.1 aKarin, T., S.1 aLanding, E. uhttp://search.informit.com.au/documentSummary;dn=343657705520848;res=IELHSS01394nas a2200133 4500008004100000245010700041210006900148300001000217490000800227520079600235100001901031700002101050856018901071 2013 eng d00aTaxonomy and distribution of Grimmia (Bryophyta) in mountain regions of the Northeastern United States0 aTaxonomy and distribution of Grimmia Bryophyta in mountain regio a28-330 v1163 a

Summarized are results of field studies of small, cushion-forming species of Grimmia in high altitude mountain areas of New York State, Vermont, New Hampshire, and Maine, and of associated research with herbarium specimens from these regions. We here report eight species. Grimmia anodon is added to the flora of the Northeast, and new records and clarifications are presented for G. donniana, G. incurva, G. longirostris, G. milleri, G. sessitana, and G. trichophylla. Collections of these species came from rock types of varying composition (calcareous to acidic), sometimes different vegetation, and varying altitudinal ranges. In spite of these advancements in knowledge, Grimmia of the northeastern United States remains incompletely understood, taxonomically and ecologically.

1 aMiller, N., G.1 aHastings, R., I. uhttps://bioone.org/journals/the-bryologist/volume-116/issue-1/0007-2745-116.1.028/Taxonomy-and-distribution-of-Grimmia-Bryophyta-in-mountain-regions-of/10.1639/0007-2745-116.1.028.full02670nas a2200181 4500008004100000245013400041210006900175300001200244490001200256520206300268653001602331653001302347653002402360653002202384653001502406100001602421856005102437 2012 eng d00aTime-specific Black Mudstones and Global Hyperwarming on the Cambrian-Ordovician Slope and Shelf of the Laurentia Palaeocontinent0 aTimespecific Black Mudstones and Global Hyperwarming on the Camb a256-2720 v367-3683 a

The Early Paleozoic featured nine intervals of strong expansion of an upper slope, dysoxic/anoxic (d/a) water mass with eustatic rise or epeirogenic transgression. Strong expansion of this d/a water mass led to deposition of time-specific, macroscale alternations of dark grey-black mudstone within oxic, green to red mudstone on the middle–lower slope. This d/a facies even onlapped warm- (carbonate) and cool-water (siliciclastic) shelves. As in the Mesozoic, d/a muds were deposited in shallow water, perhaps tens of metres deep, with sea-level rise. These nine d/a macroscale alternations correspond to intervals of “global hyperwarming”—times of very intense greenhouse conditions that resulted from a feedback initiated by higher insolation and heat storage as shallow seas onlap tropical palaeocontinents. Warm epeiric seas heated the ocean, and thermal expansion accelerated eustatic rise. Ever more extensive epeiric seas heightened oceanic and global temperature as heat storage capacity increased. Deep ocean circulation intensity fell below that of a greenhouse interval and lead to d/a deposition low on the slope and on the platforms to provide the signature of global hyperwarming. Global hyperwarming differs from a hothouse interval as it does not require CO2 input from large igneous provinces to produce high temperatures and never shows deep-sea anoxia. Late Ordovician and Late Devonian black mudstones that cover much of Laurentia record epeirogenic transgressions that led to global hyperwarming, and suggest that cold water upwelling or plant terrestrialisation had nothing to do with epeiric sea anoxia. Global hyperwarming reduced oxygen solubility in these seas, and erosion of orogens produced muddy water that limited light penetration and promoted shallow-water anoxia. The global hyperwarming hypothesis means that relative eustatic and epeirogenic sea levels complement the effect of global pCO2 on climate, and sea level must also be regarded as a primary driver of Phanerozoic climate.

10aBlack shale10aCambrian10aGlobal hyperwarming10aOcean oxygenation10aOrdovician1 aLanding, E. uhttp://dx.doi.org/10.1016/j.palaeo.2011.09.00503502nas a2200241 4500008004100000245016300041210006900204300001100273490000800284520274900292653001403041653001203055653001403067653002103081653001303102653001503115653001203130100001603142700001903158700002003177700001503197856004803212 2012 eng d00aTribes Hill-Rochdale Formations in East Laurentia: Proxies for Early Ordovician (Tremadocian) Eustasy on a Tropical Passive Margin (New York and West Vermont)0 aTribes HillRochdale Formations in East Laurentia Proxies for Ear a93-1230 v1493 a

Slow subsidence and tectonic quiescence along the New York Promontory margin of Laurentia mean that the carbonate-dominated Tribes Hill and overlying Rochdale formations serve as proxies for the magnitude and timing of Tremadocian eustatic changes. Both formations are unconformity-bound, deepening–shoaling, depositional sequences that double in thickness from the craton into the parautochthonous, western Appalachian Mountains. A consistent, ‘layer cake’ succession of member-level units of the formations persists through this region. The Tribes Hill Formation (late early Tremadocian, late Skullrockian, late Fauna B–Rossodus manitouensis Chron) unconformably overlies the terminal Cambrian Little Falls Formation as the lowest Ordovician unit on the New York Promontory. It was deposited during the strong early Tremadocian, or Stonehenge, transgression that inundated Laurentia, brought dysoxic/anoxic (d/a) slope water onto the shelf and led to deposition of the Schaghticoke d/a interval (black mudstone and ‘ribbon limestone’) on the Laurentian continental slope. The uniform lithofacies succession of the Tribes Hill includes a lower sand-rich member; a middle, dark grey to black mudstone that records d/a in eastern exposures; and an upper, shoaling-up carbonate highstand facies. A widespread (12000+ km2) thrombolitic interval in the highstand carbonate suggests the New York Promontory was rimmed by thrombolites during deposition of the Tribes Hill. Offlap and erosion of the Tribes Hill was followed by the relatively feeble sea-level rise of the Rochdale transgression (new) in Laurentia, and deposition of the Rochdale Formation. The Rochdale transgression, correlated with the Kierograptus Drowning Interval in Baltica, marks a eustatic rise. The Rochdale Formation represents a short Early Ordovician interval (early late Tremadocian, middle–late Stairsian, Macerodus dianae Chron). It correlates with a depositional sequence that forms the middle Boat Harbour Formation in west Newfoundland and with the Rte 299 d/a interval on the east Laurentian slope. The Rochdale has a lower carbonate with abundant quartz silt (Comstock Member, new) and an upper, thrombolitic (Hawk Member, new) high-stand facies. Tribes Hill and Rochdale faunas are mollusc-rich, generally trilobite-poor, and have low diversity, Laurentian faunal province conodonts. Ulrichodina rutnika Landing n. sp. is rare in Rochdale conodont assemblages. Trilobites are also low in diversity, but locally form coquinas in the middle Tribes Hill. The poorly preserved Rochdale trilobites include the bathyurid Randaynia, at least two hystricurid species and Leiostegium.

10aconodonts10aeustasy10aLaurentia10aLower Ordovician10aNew York10atrilobites10aVermont1 aLanding, E.1 aAdrian, J., M.1 aWestrop, S., R.1 aKroger, B. uhttp://dx.doi.org/10.1017/S001675681100059801600nas a2200145 4500008004100000022001400041245007600055210006900131300001400200490000700214520113700221100001901358700001901377856005801396 2012 eng d a0008-407700aTree macrofossils of Younger Dryas age from Cohoes, New York State, USA0 aTree macrofossils of Younger Dryas age from Cohoes New York Stat a671 - 6800 v493 a

Tree macrofossils dating from the middle to end (about 1000 years, ca. 12 600–11 600 cal years BP) of the Younger Dryas chronozone were found in an organic deposit on the southwest side of the Mohawk River, near its junction with the Hudson River in Cohoes, New York, USA. The fossils included substantial wood fragments, associated plant remains, and pollen, which indicate a forest of white spruce (Picea glauca), balsam fir (Abies balsamea), and tamarack (Larix laricina). The presence of white, rather than black (P. mariana) or red (P. rubens) spruce in the Younger Dryas was probably due to a riparian-type environment, confirmed by its location and American beaver tooth marks on some of the wood fragments. The clusters of wood radiocarbon dates indicate periodic changes in erosion and deposition at the site. One possible but very short decline (temperature reversal?) may be indicated by tree-ring growth, but in general, the ring widths of the trees and their growth responses suggest variable but slowly improving conditions over time, possibly from warming temperatures, before the end of the Younger Dryas.

1 aMiller, N., G.1 aGriggs, C., B. uhttp://www.nrcresearchpress.com/doi/10.1139/e2012-01001899nas a2200301 4500008004100000245009200041210006900133300001200202490000700214520102700221653002201248653001601270653002201286653002601308653002401334100001501358700001501373700001901388700002001407700001801427700001901445700001401464700001701478700001801495700002101513700001701534856004601551 2011 eng d00aTechnology on the Move: Recent and Forthcoming Innovations for Tracking Migratory Birds0 aTechnology on the Move Recent and Forthcoming Innovations for Tr a689-6980 v613 a

Basic questions about the life histories of migratory birds have confounded scientists for generations, yet we are nearing an era of historic discovery as new tracking technologies make it possible to determine the timing and routes of an increasing number of bird migrations. Tracking small flying animals as they travel over continental-scale distances is a difficult logistical and engineering challenge. Although no tracking system works well with all species, improvements to traditional technologies, such as satellite tracking, along with innovations related to global positioning systems, cellular networks, solar geolocation, radar, and information technology are improving our understanding of when and where birds go during their annual cycles and informing numerous scientific disciplines, including evolutionary biology, population ecology, and global change. The recent developments described in this article will help us answer many long-standing questions about animal behavior and life histories.

10acellular tracking10ageolocators10aradar ornithology10asatellite transmitter10atracking technology1 aBridge, E.1 aThorup, K.1 aBowlin, M., S.1 aChilson, P., B.1 aDiehl, R., H.1 aFleron, R., W.1 aHartl, P.1 aKays, R., W.1 aKelly, J., F.1 aRobinson, W., D.1 aWikelski, M. uhttp://dx.doi.org/10.1525/bio.2011.61.9.700530nas a2200157 4500008004100000245011400041210006900155300001200224490000600236653001200242100002500254700002200279700001400301700001600315856004100331 2011 eng d00aTectonic Implications of the Discovery of a Shawinigan Ophiolite (Pyrites Complex) in the Adirondack Lowlands0 aTectonic Implications of the Discovery of a Shawinigan Ophiolite a333-3560 v710ageology1 aChiarenzelli, J., R.1 aLupulescu, M., V.1 aThern, E.1 aCousens, B. uhttp://dx.doi.org/10.1130/GES00608.101662nas a2200229 4500008004100000245006900041210006900110300001100179490000600190520098400196653001001180653001501190653001301205653001301218653002301231653003001254100001701284700001901301700002101320700001401341856007701355 2011 eng d00aTeosinte Inflorescence Phytolith Assemblages Mirror Zea Taxonomy0 aTeosinte Inflorescence Phytolith Assemblages Mirror Zea Taxonomy aE183490 v63 a

Molecular DNA analyses of the New World grass (Poaceae) genus Zea, comprising five species, has resolved taxonomic issues including the most likely teosinte progenitor (Zea mays ssp. parviglumis) of maize (Zea mays ssp. mays). However, archaeologically, little is known about the use of teosinte by humans both prior to and after the domestication of maize. One potential line of evidence to explore these relationships is opaline phytoliths produced in teosinte fruit cases. Here we use multidimensional scaling and multiple discriminant analyses to determine if rondel phytolith assemblages from teosinte fruitcases reflect teosinte taxonomy. Our results indicate that rondel phytolith assemblages from the various taxa, including subspecies, can be statistically discriminated. This indicates that it will be possible to investigate the archaeological histories of teosinte use pending the recovery of appropriate samples.

10amaize10aphytoliths10ataxonomy10ateosinte10aZea mays ssp. mays10aZea mays ssp. parviglumis1 aHart, J., P.1 aMatson, R., G.1 aThompson, R., G.1 aBlake, M. uhttp://journals.plos.org/plosone/article?id=10.1371/journal.pone.001834903605nas a2200301 4500008004100000245010800041210006900149300001400218490000700232520274600239653002002985653001803005653002203023653002003045100001703065700001403082700002003096700001703116700001503133700001503148700001703163700001503180700001603195700001603211700001503227700001703242856004403259 2011 eng d00aTracking Animal Location and Activity with an Automated Radio Telemetry System in a Tropical Rainforest0 aTracking Animal Location and Activity with an Automated Radio Te a1931-19480 v543 a

How do animals use their habitat? Where do they go and what do they do? These basic questions are key not only to understanding a species’ ecology and evolution, but also for addressing many of the environmental challenges we currently face, including problems posed by invasive species, the spread of zoonotic diseases and declines in wildlife populations due to anthropogenic climate and land-use changes. Monitoring the movements and activities of wild animals can be difficult, especially when the species in question are small, cryptic or move over large areas. In this paper, we describe an Automated Radio-Telemetry System (ARTS) that we designed and built on Barro Colorado Island (BCI), Panama to overcome these challenges. We describe the hardware and software we used to implement the ARTS, and discuss the scientific successes we have had using the system, as well as the logistical challenges we faced in maintaining the system in real-world, rainforest conditions. The ARTS uses automated radio-telemetry receivers mounted on 40-m towers topped with arrays of directional antennas to track the activity and location of radio-collared study animals, 24 h a day, 7 days a week. These receiving units are connected by a wireless network to a server housed in the laboratory on BCI, making these data available in real time to researchers via a web-accessible database. As long as study animals are within the range of the towers, the ARTS system collects data more frequently than typical animal-borne global positioning system collars (∼12 locations/h) with lower accuracy (approximately 50 m) but at much reduced cost per tag (∼10X less expensive). The geographic range of ARTS, like all VHF telemetry, is affected by the size of the radio-tag as well as its position in the forest (e.g. tags in the canopy transmit farther than those on the forest floor). We present a model of signal propagation based on landscape conditions, which quantifies these effects and identifies sources of interference, including weather events and human activity. ARTS has been used to track 374 individual animals from 38 species, including 17 mammal species, 12 birds, 7 reptiles or amphibians, as well as two species of plant seeds. These data elucidate the spatio-temporal dynamics of animal activity and movement at the site and have produced numerous peer-reviewed publications, student theses, magazine articles, educational programs and film documentaries. These data are also relevant to long-term population monitoring and conservation plans. Both the successes and the failures of the ARTS system are applicable to broader sensor network applications and are valuable for advancing sensor network research.

10aanimal tracking10aenvironmental10aobserving systems10asensor networks1 aKays, R., W.1 aTilak, S.1 aCrofoot, M., C.1 aFountain, T.1 aObando, D.1 aOrtega, A.1 aKuemmeth, F.1 aMandel, J.1 aSwenson, G.1 aLambert, T.1 aHirsch, B.1 aWikelski, M. uhttp://dx.doi.org/10.1093/comjnl/bxr07202937nas a2200253 4500008004100000245009300041210006900134300001200203490000700215520222300222653001102445653001602456653001602472653002302488653001702511653001402528653002102542653001502563653001602578653001502594100001602609700001902625856003902644 2011 eng d00aTremadocian (Lower Ordovician) Biotas and Sea-level Changes on the Avalon Microcontinent0 aTremadocian Lower Ordovician Biotas and Sealevel Changes on the  a680-6960 v853 a

The Chesley Drive Group, an Upper Cambrian–Lower Ordovician mudstone-dominated unit, is part of the Ediacaran–Ordovician cover sequence on the North American part of the Avalon microcontinent. The upper Chesley Drive Group on McLeod Brook, Cape Breton Island (previously “McLeod Brook Formation”), has two lithofacies-specific Tremadocian biotas. An older low-diversity benthic assemblage (shallow burrowers, Bathysiphon, phosphatic brachiopods, asaphid trilobites) is in lower upper Tremadocian green-gray mudstone. This wave-influenced, slightly dysoxic facies has Bathysiphon–brachiopod shell lags in ripple troughs. The upper fauna (ca. 483 +/− 1 Ma) is in dysoxic-anoxic (d-a), unburrowed, dark gray-black, upper upper (but not uppermost) Tremadocian mudstone with a “mass kill” of the olenid Peltocare rotundifrons (Matthew)—a provincial trilobite in Avalonian North America that likely tolerated low oxygen bottom waters. Scandodus avalonensis Landing n. sp. and Lagenochitina aff. conifundus (Poumot), probable nektic elements and the first upper Tremadocian conodont and chitinozoan reported from Avalon, occur in diagenetic calcareous nodules in the dark gray–black mudstone. An upper Tremadocian transition from lower greenish to upper black mudstone is not exposed on McLeod Brook, but is comparable to a coeval green-black mudstone transition in Avalonian England. The successions suggest that late late Tremadocian (probable Baltic Hunnebergian Age) sea level was higher in Avalon than is suggested from successions on other paleocontinents. The Tremadocian sea-level history of Avalon was a shoaling–deepening–shoaling sequence from d-a black mudstone (lower Tremadocian), to dysoxic green mudstone (lower upper Tremadocian), and back to black mudstone (upper upper Tremadocian).

Scandodus Lindström is emended, with the early species S. avalonensis Landing n. sp. assigned to the emended Family Protopanderodontidae. Triangulodus Van Wamel is considered a junior synonym of Scandodus. Peltocare rotundifrons is emended on the basis of complete specimens.

10aAvalon10aBathysiphon10abrachiopods10aCape Breton Island10achitinozoans10aconodonts10aLower Ordovician10asea-levels10aTremadocian10atrilobites1 aLanding, E.1 aFortey, R., A. uhttp://dx.doi.org/10.1666/10-076.100345nas a2200121 4500008004100000245003000041210002900071300000800100490000600108653001200114100002200126856007500148 2011 eng d00aTourmaline-Group Minerals0 aTourmalineGroup Minerals a8-90 v610ageology1 aLupulescu, M., V. uhttps://www.nysm.nysed.gov/staff-publications/tourmalinegroup-minerals01233nas a2200169 4500008004100000245007200041210006900113260006200182300001000244520061600254653001700870100001800887700002000905700001800925700001700943856010300960 2011 eng d00aTrace Element Analysis of Lithic Artifacts from the Trapps Gap Site0 aTrace Element Analysis of Lithic Artifacts from the Trapps Gap S aAlbany, New YorkbThe University of the State of New York a41-523 a

Traditional models of Late Prehistoric (A.D. 700–1300) interaction in the middle Hudson Valley suggest strong ties with contemporaneous groups in southern New England. Recent research, in the form of trace element analysis of lithic artifacts from the Trapps Gap site in Ulster County, New York, questions this assumption suggesting a more diverse and complex landscape in which groups interacted. This paper will discuss whether all of the samples were procured from the same deposit, how such procurement patterns may have changed over time, and what such data might reveal about regional behavior.

10aanthropology1 aRieth, C., B.1 aJohnson, L., L.1 aRieth, C., B.1 aHart, J., P. uhttps://www.nysm.nysed.gov/staff-publications/trace-element-analysis-lithic-artifacts-trapps-gap-s01488nas a2200229 4500008004100000245013200041210006900173260003300242300001000275520071400285653001900999653002101018653002101039653002101060653001601081653002701097100001601124700002501140700001301165700001301178856006701191 2011 eng d00aTesting the Paleo-Maritime Hypothesis for Glacial Lake Iroquois: Implications for Changing Views of Past Culture and Technology0 aTesting the PaleoMaritime Hypothesis for Glacial Lake Iroquois I aNew York, New YorkbSpringer a27-433 a

Comparison of stone tool assemblages and their associations with paleo-shorelines across North America encourages us to begin thinking in terms of maritime culture dating back as far as 8,000–10,000 years. Locations as diverse as Fort Drum, New York, San Clemente Island, California, and Hill AFB Bombing Range, Utah, all offer sites, collections, and information that can illuminate a possible early type of maritime cultural landscape. Evidence for human adaptation to Late Pleistocene and Early Holocene shoreline environments will emphasize the potential for use and construction of boats with a discussion of the implications for changing archaeological characterization of Paleoindian people.

10aEarly Holocene10alate Pleistocene10amaritime culture10apaleo-shorelines10aPaleoindian10astone tool assemblages1 aSchultz, M.1 aWinchell-Sweeney, S.1 aRush, L.1 aFord, B. uhttp://link.springer.com/chapter/10.1007%2F978-1-4419-8210-0_201668nas a2200193 4500008004100000245013800041210006900179260002100248300001200269520099900281653002001280653002101300653001801321653001301339100001601352700001901368700002101387856006601408 2010 eng d00aTowards Automating Artifact Analysis: A Study Showing Potential Application in Computer Vision and Morphometrics to Artifact Typology0 aTowards Automating Artifact Analysis A Study Showing Potential A aBerlinbSpringer a289-3053 a

First released in 1961, William A. Ritchie’s A Typology and Nomenclature of New York State Projectile Points remains an influential resource for archaeologists working in the northeastern US. Ritchie examined a large and diverse sample of stone projectile points, but not all fit neatly into his typology. In this chapter, we propose that alternative approaches afforded by computer vision and morphometrics can shed light on this and other problems of traditional stone tool typology. With the advent of computer vision, we can now examine the entire morphological continuum of projectile points through statistical shape analysis. Following automated image capture, three analytical methods were evaluated using silhouette, outline, and landmark data. Biased free capture methods to record the form of an individual projectile point, together with using invariant shape descriptors to quantify the data, may result in more objective analysis than was possible in the past.

10acomputer vision10alithics typology10amorphometrics10aNew York1 aLenardi, M.1 aMerwin, D., E.1 aElewa, A., M. T. uhttp://link.springer.com/chapter/10.1007/978-3-540-95853-6_1301068nas a2200181 4500008004100000245005200041210005100093300001100144490000700155520057500162653001700737653001600754653001500770653001600785653001200801100001800813856005500831 2010 eng d00aThree 19th-Century House Sites in Rural Ireland0 aThree 19thCentury House Sites in Rural Ireland a81-1040 v443 a

This report describes archaeological research at three house sites in rural Ireland. The anthropologically-based research began in 1994 with the goal of attempting to understand the material conditions of daily life in the 19th-century Irish countryside. The excavation results presented here were obtained from individual households in counties Roscommon, Sligo and Donegal, at sites dating from the early to mid-19th century. Two of the sites are known to have been abandoned as a result of forced eviction. Particular attention is paid to the ceramics found.

10a19th-century10aArchaeology10adaily life10ahouse sites10aIreland1 aOrser, C., E. uhttp://dx.doi.org/10.1179/174581310X1266238262917501276nas a2200181 4500008004100000245004800041210004700089300001200136490000700148520078200155653001500937653002400952653002700976653001501003653001001018100001801028856004801046 2010 eng d00aTwenty-First Century Historical Archaeology0 aTwentyFirst Century Historical Archaeology a111-1500 v183 a

The practice of historical archaeology has exploded over the past two decades, and especially since 2000. Methodological advances and new theoretical insights mean that archaeological research requires periodic evaluation, and this overview builds on the work of three earlier assessors of the discipline. Here, I concentrate on four areas of research currently being pursued by historical archaeologists: analytical scale, capitalism, social inequality, and heritage and memory. I conclude that historical archaeologists have made major strides in understanding the modern world and that future research promises to offer diverse perspectives that will deepen our appreciation for how the past influences the present.

10aCapitalism10aHeritage and memory10aHistorical archaeology10aInequality10aScale1 aOrser, C., E. uhttp://dx.doi.org/10.1007/s10814-009-9035-902698nas a2200205 4500008004100000245007400041210006900115300001200184490000600196520208700202653001202289100001702301700002502318700002302343700001602366700001802382700001702400700003202417856004302449 2009 eng d00aTerminology of Geological Time: Establishment of a Community Standard0 aTerminology of Geological Time Establishment of a Community Stan a100-1050 v63 a

It has been recommended that geological time be described in a single set of terms and according to metric or SI (“Système International d’Unités”) standards, to ensure “worldwide unification of measurement”. While any effort to improve communication in scientific research and writing is to be encouraged, we are also concerned that fundamental differences between date and duration, in the way that our profession expresses geological time, would be lost in such an oversimplified terminology. In addition, no precise value for ‘year’ in the SI base unit of second has been accepted by the international bodies.Under any circumstances, however, it remains the fact that geological dates – as points in time – are not relevant to the SI. Known dates may define durations, just as known durations may define dates, or dates may simply be punctual references that support historical narratives, but dates are not quantities. Furthermore, dates, as datum points, belong to a specific type of guiding information that is in constant use not only by the disciplines that explore the unwritten past, but in the physical sciences and engineering as well. Accordingly, we recommend a new standardization of the distinction between geohistorical date, in years before present expressed in ‘annus’, symbol ‘a’,with the multiples ‘ka’, ‘Ma’, and ‘Ga’ for thousands, millions and billions of years ago, according to a convention that has been very widely adopted during the last 30 years, and geohistorical duration, expressed in ‘year’, symbol ‘yr’, with multiples ‘kyr’, ‘Myr’ and ‘Gyr’, respectively, as the most appropriate among the various formats in the current literature. Agreement on these two sets of terms throughout the wide community that deals with paleochronology would remove a false impression of improvisation and uncertainty as to appropriate terminology, and would lead to more effective communication in areas where a simplified but needlessly SI-conisistent terminology would be less, not more useful.

10ageology1 aAubry, M.-P.1 aVan Covering, J., A.1 aChristie-Blick, N.1 aLanding, E.1 aPratt, B., R.1 aOwen, D., E.1 aFerrusquía-Villafranca, I. uhttp://hdl.handle.net/10022/AC:P:2142002574nas a2200301 4500008004100000245015900041210006900200300001000269490000700279520158800286653001001874653001701884653001801901653003001919653001001949653001301959653001801972653001301990100001902003700001702022700001902039700003002058700001802088700001902106700001602125700002202141856010902163 2009 eng d00aTaxonomic Boundaries and Geographic Distributions Revealed by an Integrative Systematic Overview of the Mountain Coatis, Nasuella (Carnivora: Procyonidae)0 aTaxonomic Boundaries and Geographic Distributions Revealed by an a65-740 v413 a

The procyonid taxon Nasuella Hollister, 1915, is currently recognized as a monotypic genus comprising the single species N. olivacea (Gray, 1865), the Mountain Coati, found in montane habitats (circa 1300-4250 m) in the Andes of Venezuela, Colombia, and Ecuador. In this study we utilize museum specimens to examine the phylogenetic relationships, taxonomy and geographic distribution of Nasuella populations with an integrative systematic approach. Drawing on morphological comparisons of pelage, cranial, and dental characters, and molecular comparisons of the mitochondrial gene cytochrome b (from recent and historical samples), we confirm that Nasuella is closely related to other coatis (Nasua) and show that there are two deeply divergent lineages represented within the taxonomic bounds of Nasuella. We recognize and diagnose these taxa as two distinctive mountain coati species, corresponding to the Eastern Mountain Coati Nasuella meridensis (Thomas, 1901), endemic to the Venezuelan Andes, and the Western Mountain Coati N. olivacea, distributed in the Andes of Colombia and Ecuador. We use locality and habitat data associated with museum specimens to model the global geographic range of both species. From this we predict areas of undocumented (i.e., currently unvouchered) occurrence, areas of habitat loss associated with land use changes, and the geographic barrier separating the distributions of N. meridensis and N. olivacea. This newfound understanding of taxonomy and distribution should allow for a revised conservation assessment for mountain coatis.

10aAndes10acytochrome b10aecomorphology10ageographic range modeling10aNasua10aNasuella10aPhylogenetics10ataxonomy1 aHelgen, K., M.1 aKays, R., W.1 aHelgen, L., E.1 aTsuchiya-Jerep, M., T. N.1 aPinto, C., M.1 aKoepfli, K.-P.1 aEizirik, E.1 aMaldonado, J., E. uhttps://www.nysm.nysed.gov/staff-publications/taxonomic-boundaries-and-geographic-distributions-revealed00614nas a2200169 4500008004100000245009000041210006900131300001200200490000600212653001200218100002300230700001900253700002300272700001900295700001800314856011200332 2009 eng d00aTaxonomy and Identification of Phoberia species (Lepidoptera: Noctuidae: Catocalinae)0 aTaxonomy and Identification of Phoberia species Lepidoptera Noct a103-1080 v110abiology1 aLafontaine, J., D.1 aDickel, T., S.1 aSchweitzer, D., F.1 aMcCabe, T., L.1 aMetlevski, J. uhttps://www.nysm.nysed.gov/staff-publications/taxonomy-and-identification-phoberia-species-lepidoptera-noct00519nas a2200133 4500008004100000245007300041210006900114260001300183300001000196653003600206100001800242700002000260856010500280 2009 eng d00aTrace Element Analysis of Lithic Artifacts from the Trapp's Gap Site0 aTrace Element Analysis of Lithic Artifacts from the Trapps Gap S aNew York a15-2310aanthropology Cultural Resources1 aRieth, C., B.1 aJohnson, L., L. uhttps://www.nysm.nysed.gov/staff-publications/trace-element-analysis-lithic-artifacts-trapps-gap-s-001704nas a2200241 4500008004100000245014300041210006900184300001200253490000700265520096400272653001101236653002901247653002001276653001101296653001501307653001401322653001301336100001701349700001801366700002101384700001601405856004101421 2008 eng d00aTaking Variation Seriously: Testing the Steatite Mast-Processing Hypothesis with Microbotanical Data from the Hunter's Home Site, New York0 aTaking Variation Seriously Testing the Steatite MastProcessing H a729-7410 v763 a

In a series of recent publications, Truncer (2004a, 2004b, 2006) presents a hypothesis that during what he interprets as the peak period of use (cal. 2500--1500 B.C.) in eastern North America, steatite (soapstone) vessels were specialized cooking tools used to process mast. A key component of Truncer’s hypothesis building is his interpretation of an analysis of fatty acids extracted from charred residue adhering to four steatite sherds, which he interpreted to be consistent with mast. This is the only component of his hypothesis building that directly links steatite vessel use to mast processing. Here we convey the results of a reassessment of Truncer’s analytical results and the results of our own analysis of phytoliths and fatty acids extracted from charred residue adhering to three sherds from the Hunter’s Home site. Our results undermine this key component of Truncer’s hypothesis building and therefore the hypothesis itself.

10aacorns10acooking residue analysis10acooking vessels10alipids10aphytoliths10asoapstone10aSteatite1 aHart, J., P.1 aReber, E., A.1 aThompson, R., G.1 aLusteck, R. uhttp://www.jstor.org/stable/2547052500337nas a2200121 4500008004100000245002800041210002800069300001000097490000600107653001200113100001900125856007100144 2008 eng d00aTo Preserve and Protect0 aTo Preserve and Protect a12-160 v410ahistory1 aHoude, Frisbee uhttps://www.nysm.nysed.gov/staff-publications/preserve-and-protect00786nas a2200133 4500008004100000245005000041210004900091300001200140490000700152520041100159653001200570100002200582856004800604 2008 eng d00aTourmaline-Group Minerals from New York State0 aTourmalineGroup Minerals from New York State a202-2080 v833 a

Tourmaline is a chemically complex group of silicates. Essentially, it is an aluminum boron silicate with extensive substitutions at the different crystallographic sites that confer varied physical properties to the mineral. Mineral collectors very much appreciate the size and beauty of tourmaline crystals, and thus the species of the group have become among the most hunted of the mineral world

10ageology1 aLupulescu, M., V. uhttp://dx.doi.org/10.3200/RMIN.83.3.202-20800459nas a2200121 4500008004100000245007600041210006900117300000800186490000600194653001200200100002000212856010500232 2008 eng d00aTickling the Ivories: The NYSM Piano Collection Symbolizes a Bygone Era0 aTickling the Ivories The NYSM Piano Collection Symbolizes a Bygo a8-90 v410ahistory1 aScherer, J., L. uhttps://www.nysm.nysed.gov/staff-publications/tickling-ivories-nysm-piano-collection-symbolizes-bygo00362nas a2200121 4500008004100000245003800041210003600079300001000115490000600125653001200131100001800143856007900161 2008 eng d00aA Tradition of Published Research0 aTradition of Published Research a17-190 v410ahistory1 aSkiba, J., B. uhttps://www.nysm.nysed.gov/staff-publications/tradition-published-research00628nas a2200193 4500008004100000245012000041210006900161300001200230490000800242653001200250100001700262700002300279700002100302700001800323700001900341700001800360700000500378856005100383 2007 eng d00aTiming and Local Perturbations to the Carbon Pool in the Lower Mississippian Madison Limestone, Montana and Wyoming0 aTiming and Local Perturbations to the Carbon Pool in the Lower M a231-2530 v25610ageology1 aKatz, D., A.1 aBuoniconti, M., R.1 aMontanez, I., P.1 aSwart, P., K.1 aEberli, G., P.1 aSmith, L., B.1 a uhttp://dx.doi.org/10.1016/j.palaeo.2007.02.04800490nas a2200157 4500008004100000245005500041210005300096260003300149300001000182653001200192100001800204700002200222700001800244700001500262856005500277 2007 eng d00aTunnel Channels of the Saginaw Lobe, Michigan, USA0 aTunnel Channels of the Saginaw Lobe Michigan USA bGeological Survey of Finland a69-7810ageology1 aKehew, A., E.1 aKozlowski, A., L.1 aJohansson, P.1 aSarala, P. uhttp://arkisto.gtk.fi/sp/sp46/sp46_pages_69_77.pdf00543nas a2200145 4500008004100000245013600041210006900177300001200246490000800258653002500266100001600291700001800307700001600325856005600341 2007 eng d00aTerminal Cambrian and Lowest Ordovician Succession of Mexican West Gondwana: Biotas and Sequence Stratigraphy of the Tinu Formation0 aTerminal Cambrian and Lowest Ordovician Succession of Mexican We a909-9360 v14410ageology paleontology1 aLanding, E.1 aWestrop, S.R.1 aKeppe, J.D. uhttp://dx.doi.org/10.1016/10.1017/S001675680700358500468nas a2200133 4500008004100000245006200041210006100103300001000164490000700174653001700181100001800198700001600216856010200232 2007 eng d00aTeaching Our Teachers: A Case Study in Public Archaeology0 aTeaching Our Teachers A Case Study in Public Archaeology a15-270 v7310aanthropology1 aRieth, C., B.1 aPrimeau, K. uhttps://www.nysm.nysed.gov/staff-publications/teaching-our-teachers-case-study-public-archaeology00470nas a2200145 4500008004100000245009100041210006900132300001000201490000700211653001700218100001800235700001700253700001400270856004000284 2007 eng d00aA Trace Element Analysis of Ceramics from the Pethick Site, Schoharie County, New York0 aTrace Element Analysis of Ceramics from the Pethick Site Schohar a59-800 v2810aanthropology1 aRieth, C., B.1 aRafferty, S.1 aSaputo, D uhttp://dx.doi.org/10.2190/NA/28.1.c06112nas a2200205 4500008004100000245016300041210006900204300001400273490000700287520538900294653002605683653002605709653003605735653002705771100001505798700001705813700001605830700001805846856004205864 2006 eng d00aTectonic-Hydrothermal Brecciation Associated with Calcite Precipitation and Permeability Detruction in Mississippian Carbonate Reservoirs, Wyoming and Montana0 aTectonicHydrothermal Brecciation Associated with Calcite Precipi a1803-18420 v903 a

The Mississippian Madison Formation contains abundant fracture zones and breccias that are hydrothermal in origin based on their morphology, distribution, and geochemical signature. The hydrothermal activity is related to crustal shortening during the Laramide orogeny. Brecciation is accompanied by dedolomitization, late-stage calcite precipitation, and porosity occlusion, especially in outcrop dolomites. The tectonic-hydrothermal late-stage calcite reduces permeability in outcrops and, potentially, high-quality subsurface reservoir rocks of the subsurface Madison Formation, Bighorn Basin. The reduction of permeability and porosity is increased along the margins of the Bighorn Basin but not predictable at outcrop scale. The destruction of porosity and permeability by hydrothermal activity in the Madison Formation is unique in comparison to studies that document enhanced porosity and permeability and invoke hydrothermal dolomitization models.

Hydrothermal breccias from the Owl Creek thrust sheet are classified into four categories based on fracture density, calcite volume, and clast orientation. Shattered breccias dominate the leading edge of the tip of the Owl Creek thrust sheet in the eastern Owl Creek Mountains, where tectonic deformation is greatest, whereas fracture, mosaic, and chaotic breccias occur throughout the Bighorn Basin. The breccias are healed by calcite cements with delta18O values ranging between minus26.5 and minus15.1permil Peedee belemnite (PDB), indicating that the cements were derived from isotopically depleted fluids with elevated temperatures. In the chaotic and mosaic breccia types, large rotated and angular clasts of the host rock float in the matrix of coarse and nonzoned late-stage calcite. This appearance, combined with similar delta18O values across even large calcite veins, indicates that the calcite precipitated rapidly after brecciation. Values for delta13C (sim5–12permil PDB) from the frontal part of the Owl Creek thrust sheet indicate equilibrium between methane and CO2-bearing fluids at about 180degC. Fluid inclusions from the eastern basin margin show that these cements are in equilibrium with fluids having minimum temperatures between 120 and 140degC and formed from relatively low-salinity fluids, less than 5 wt.% NaCl. Strontium isotope ratios of these hydrothermal fluids are more radiogenic than proposed values for Mississippian seawater, suggesting that the fluids mixed with felsic-rich basement before migrating vertically into the Madison Formation.

We envisage that the tectonic-hydrothermal late-stage calcite-cemented breccias and fractures originated from undersaturated meteoric groundwaters that migrated into the burial environment while dissolving and incorporating Ca2+ and Equation 1 and radiogenic Sr from the dissolution of the surrounding carbonates and the felsic basement, respectively. In the burial environment, these fluids were heated and mixed with hypersaline brines from deeply buried parts of the basement. Expulsion of these fluids along basement-rooted thrust faults into the overlying strata, including the Madison Formation, occurred most likely during shortening episodes of the Laramide orogeny by earthquake-induced rupturing of the host rock. The fluids were injected forcefully and in an explosive manner into the Madison Formation, causing brecciation and fracturing of the host rock, whereas the subsequent and sudden decrease in the partial pressure of CO2 caused the rapid precipitation of calcite cements.

The explosive nature of hydrothermal fluid migration ultimately produces heterogeneities in reservoir-quality carbonates. In general, flow units in the Madison Formation are related to sequence boundaries, which create vertical subdivisions in the porous dolomite. The late-stage calcite cement surrounds hydrothermal breccia clasts and invades the dolomite, reducing porosity and permeability of the reservoir-quality rock. As a consequence, horizontal flow barriers and compartments are established that are locally unpredictable in their location and extent and regionally predictable along the margins of the Bighorn Basin.

10aHydrothermal breccias10ahydrothermal dolomite10aMississippian Madison Formation10aOwl Creek thrust sheet1 aKatz, D.A.1 aEberli, G.P.1 aSwart, P.K.1 aSmith, L., B. uhttp://dx.doi.org/10.1306/0320060507200326nas a2200121 4500008004100000245002500041210002500066300000800091490000700099653001700106100001700123856006400140 2005 eng d00aTales from the Field0 aTales from the Field a6-70 v1510aanthropology1 aDale, B., R. uhttps://www.nysm.nysed.gov/staff-publications/tales-field-000334nas a2200121 4500008004100000245002800041210002400069300001000093490000700103653001200110100002000122856007000142 2005 eng d00aThe Tompkins Collection0 aTompkins Collection a29-320 v5410ahistory1 aScherer, J., L. uhttps://www.nysm.nysed.gov/staff-publications/tompkins-collection02403nas a2200205 4500008004100000245012100041210006900162300001200231490000700243520172900250653001401979653002601993653002502019100001802044700002102062700001802083700002102101700002002122856005502142 2004 eng d00aTreehopper Trees: Phylogeny of Membracidae (Hemiptera: Cicadomorpha: Membracoidea) Based on Molecules and Morphology0 aTreehopper Trees Phylogeny of Membracidae Hemiptera Cicadomorpha a441-4540 v293 a

Recent independent phylogenetic analyses of membracid relationships based on molecular and morphological data have identified monophyletic lineages within the family. However, the results of these studies have not fully resolved treehopper phylogeny, and relationships among some higher membracid lineages remain in doubt. Portions of three datasets (958 aligned nucleotides from elongation factor-1α, 2363 aligned nucleotides from 28S ribosomal DNA, and eighty-three morphological features of adults and nymphs) introduced in recent studies were reanalysed separately and in combination with two new molecular datasets (321 aligned nucleotides from wingless and 1829 aligned nucleotides from 18S ribosomal DNA). The results of the combined data analyses, contrary to previous analyses of morphological data alone, grouped membracids into two well-supported lineages, one comprising Stegaspidinae and Centrotinae, the other comprising Membracinae, Darninae and Smiliinae. The analyses recovered Centrotinae, Membracinae and Darninae as monophyletic groups, but Stegaspidinae was paraphyletic with respect to Centrotinae, and Smiliinae was polyphyletic with Micrutalini placed as a sister group to the clade comprising Membracinae, Darninae and Smiliinae. These results are consistent with the following hypotheses, proposed previously based on an analysis of morphological data: (1) the posterior pronotal process was derived and lost multiple times during the evolution of Membracidae; (2) Membracidae originated in the New World and reached the Old World subsequently via dispersal; (3) maternal care evolved independently multiple times and may or may not have been preceded by the acquisition of ant mutualism.

10amembracid10aPhylogenetic analyses10atreehopper phylogeny1 aCryan, J., R.1 aWiegmann, B., M.1 aDeitz, L., L.1 aDietrich, C., H.1 aWhiting, M., F. uhttp://dx.doi.org/10.1111/j.0307-6970.2004.00260.x00335nas a2200121 4500008004100000245002900041210002500070300000800095490000700103653001200110100002000122856007100142 2004 eng d00aThe Thompkins Collection0 aThompkins Collection a4-60 v1510ahistory1 aScherer, J., L. uhttps://www.nysm.nysed.gov/staff-publications/thompkins-collection02072nas a2200205 4500008004100000245011900041210006900160300001000229490000700239520138700246653001901633653002101652653001301673653002301686653001401709653001601723100002301739700001901762856008501781 2004 eng d00aThe Taxonomy, Larva, and Ecology of Agrotis buchholzi (Noctuidae), with a New Sibling Species from North Carolina0 aTaxonomy Larva and Ecology of Agrotis buchholzi Noctuidae with a a65-740 v583 a

Agrotis huchholz.i is one of four Lepidoptera species believed to be endemic to the New Jersey Pine Barrens. It occurs primarily in recently burned or exceptionally xelic or sterile areas where its sole larval food plant, Pyxidanthera barbulata (Diapensiaceae), occurs in openings in the shrub layer. Adults can be quite common locally. There are two broods approximately two months apart with the first sarting about late May. Hibernation is as prepupal larvae in the sand. The la,va is similar to that of other species of Agrotis. Adults are very active and feed but their natural food sourees are not known. A sibling species, Agrotis carolina, new species, is closely associated with P. barbu/ata in southeastern North Carolina. Its range resembles that of another endemic, Hemipachnobia subporphyrea. The combined ranges of these two Agrotis are very similar to those of an unnamed Cyclophora (Geometridae) and Spartiniphaga carterae Schweitzer (Noduidae) and their habitats commonly overlap in both states. Fire is a crucial factor in forming and maintaining habitat for all of these species. A buchho/zi may become imperiled hecause of a decline of wildfires. A carolina, but not A. buchholzi , is thriving in habitats maintained by prescribed bums.

10aAgmtis obliqua10aAgrotis stigmosa10abivoltin10alarval hibernation10amonophagy10aSand plains1 aSchweitzer, D., F.1 aMcCabe, T., L. uhttp://images.peabody.yale.edu/lepsoc/jls/2000s/2004/2004-58(2)65-Schweitzer.pdf00324nas a2200121 4500008004100000245002500041210002500066300000800091490000700099653001200106100002200118856006200140 2004 eng d00aTales from the Field0 aTales from the Field a6-70 v1410abiology1 aSiegfried, C., A. uhttps://www.nysm.nysed.gov/staff-publications/tales-field00571nas a2200133 4500008004100000245009300041210006900134260006200203300001000265653001700275100001900292700001900311856010700330 2003 eng d00aTrace Elements and Stable Isotope Analysis of Human Remains from the Lutheran Church Lot0 aTrace Elements and Stable Isotope Analysis of Human Remains from aAlbany, New YorkbThe University of the State of New York a63-6810aanthropology1 aFisher, C., L.1 aFisher, C., L. uhttps://www.nysm.nysed.gov/staff-publications/trace-elements-and-stable-isotope-analysis-human-remains00465nam a2200121 4500008004100000245005800041210005700099260006200156653001700218100001700235700001700252856007400269 2003 eng d00aThree Sixteenth-Century Mohawk Iroquois Village Sites0 aThree SixteenthCentury Mohawk Iroquois Village Sites aAlbany, New YorkbThe University of the State of New York10aanthropology1 aFunk, R., E.1 aKuhn, R., D. uhttp://exhibitions.nysm.nysed.gov/publications/bulletin/503-14603.pdf00383nas a2200121 4500008004100000245004900041210004800090300000800138490000700146653001700153100001300170856007800183 2003 eng d00aTales from the Field: The Battle of New York0 aTales from the Field The Battle of New York a6-70 v1410aanthropology1 aGore, A. uhttps://www.nysm.nysed.gov/staff-publications/tales-field-battle-new-york02567nas a2200217 4500008004100000245013600041210006900177300001400246490000700260520188500267653002602152653001402178653001802192653001702210653001902227100001602246700001602262700002002278700001302298856003802311 2003 eng d00aTectonic Setting of Outer Trench Slope Volcanism: Pillow Basalt and Limestone in the Ordovician Taconian Orogen of Eastern New York0 aTectonic Setting of Outer Trench Slope Volcanism Pillow Basalt a a1773-17870 v403 a

The only pillow basalt in synorogenic sedimentary rocks at the exterior margin of the Taconic orogen in eastern North America is at Stark's Knob in eastern New York. Earlier reported as extrusive into allochthonous Ordovician slope and rise facies, this small lens (ca. 125+ m long, 39 m thick) is a fault-bounded block in Upper Ordovician melange under the Taconian frontal thrust. Its N-MORB (normal mid-ocean ridge basalt) basalt geochemistry and spinel composition are characteristic of oceanic ridge settings at a water depth of 2 km or more. Abundant limestone lenses on pillows and lava shelves within pillows yielded a middle Late Ordovician gastropod. The limestones are reconciled with this extrusion depth and with limited early Paleozoic pelagic carbonate production by lime mud transport from the Laurentian platform or abiotic carbonate precipitation with sea-water heating during basalt extrusion. A genetic relationship between the parautochthonous Stark's Knob basalts and the allochthonous Jonestown volcanics in slope and rise facies of the Hamburg klippe, eastern Pennsylvania, is likely. Both are Ordovician MORB basalts that reflect volcanism on the subducting outer trench slope prior to the Taconic arc – Laurentia collision. Taconic orogenesis may have led to basalt production on the subducting plate by (1) the setting up of orogen-parallel, predominantly strike-slip motion on the subducting slab with MORB basalt generated at offsets in a setting analogous to the Gulf of California or (2) development of faults in a flexure-induced extensional regime. By either process, mafic volcanism appears to be a rare but tectonically significant process on outer trench slopes as continental margins or oceanic plates enter subduction zones.

10aEastern North America10aNew York.10apillow basalt10aStark's Knob10aTaconic orogen1 aLanding, E.1 aPe-Piper, G1 aKidd, W., S. F.1 aAzmy, K. uhttp://dx.doi.org/10.1139/e03-07600667nas a2200181 4500008004100000245016900041210006900210300001200279490000800291653001200299100002000311700001900331700001800350700002500368700002200393700001800415856005200433 2003 eng d00aA Tale of Shales: The Relative Roles of Production, Decomposition, and Dilution in the Accumulation of Organic-rich Strata, Middle-Upper Devonian, Appalachian Basin0 aTale of Shales The Relative Roles of Production Decomposition an a229-2730 v19510ageology1 aSageman, B., B.1 aMurphy, A., E.1 aWerne, J., P.1 aVer Straeten, C., A.1 aHollander, D., J.1 aLyons, T., W. uhttp://dx.doi.org/10.1016/S0009-2541(02)00397-200324nas a2200121 4500008004100000245002500041210002500066300000800091490000700099653001200106100002000118856006400138 2003 eng d00aTales from the Field0 aTales from the Field a4-50 v1410abiology1 aSheviak, C., J. uhttps://www.nysm.nysed.gov/staff-publications/tales-field-100377nas a2200121 4500008004100000245004400041210003800085300001000123490000800133653001700141100001600158856008100174 2003 eng d00aA Tribute to Robert E. Funk (1932-2003)0 aTribute to Robert E Funk 19322003 a64-680 v11910aanthropology1 aWellman, B. uhttps://www.nysm.nysed.gov/staff-publications/tribute-robert-e-funk-1932200300474nas a2200157 4500008004100000245001400041210001400055260004800069653001800117653001200135653001200147100002000159700002000179700004700199856007000246 2002 eng d00aTipularia0 aTipularia aNew York, New YorkbOxford University Press10aNorth America10aorchids10aspecies1 aCatling, P., M.1 aSheviak, C., J.1 aFlora of North America Editorial Committee uhttp://www.efloras.org/florataxon.aspx?flora_id=1&taxon_id=13304401262nas a2200181 4500008004100000245008700041210006900128260004900197300001200246520067000258653001300928653001200941653001300953653001900966100001800985700001801003856005901021 2002 eng d00aTrace Element Analysis and Its Role in Analyzing Ceramics in the Eastern Woodlands0 aTrace Element Analysis and Its Role in Analyzing Ceramics in the aWashington, D. C.bAmerican Chemical Society a199-2133 a

Clemson Island and Owasco ceramics are used to document interaction in Pennsylvania during the Early Late Prehistoric Period (A.D. 700-1300). Clemson Island ceramics are regarded as the by-products of local manufacture while Owasco ceramics are considered to be foreign wares. X-ray fluorescence is used to determine the provenance of manufacture and assess whether compositional profiles reflect the reciprocal exchange of ceramic vessels. The results of this project suggest no clear distinction between ceramic types and clay deposits. Instead, similarities in attributes may reflect the utilization of similar resources.

10aCeramics10aPottery10asourcing10atrace elements1 aRieth, C., B.1 aJakes, K., A. uhttp://pubs.acs.org/doi/abs/10.1021/bk-2002-0831.ch01300496nas a2200145 4500008004100000245004400041210004400085260005300129300001500182653001700197100002000214700002000234700001500254856008100269 2001 eng d00aTextiles from the Wickliffe Mounds Site0 aTextiles from the Wickliffe Mounds Site aTuscaloosa, AlabamabUniversity of Alabama Press aChapter 1410aanthropology1 aKutruff, J., T.1 aDrooker, P., B.1 aWesler, K. uhttps://www.nysm.nysed.gov/staff-publications/textiles-wickliffe-mounds-site00458nas a2200121 4500008004100000245007900041210006900120300000600189490000700195653001200202100001900214856010300233 2001 eng d00aTales from the field: North to Tundra and ice-Kalaallit Nunaat (Greenland)0 aTales from the field North to Tundra and iceKalaallit Nunaat Gre a70 v1110abiology1 aMiller, N., G. uhttps://www.nysm.nysed.gov/staff-publications/tales-field-north-tundra-and-icekalaallit-nunaat-gre00526nas a2200145 4500008004100000245007300041210006900114300001200183490000700195653001200202100001800214700001800232700001900250856011100269 2001 eng d00aThermal Maturity Patterns in New York State Using CAI and %R (sub o)0 aThermal Maturity Patterns in New York State Using CAI and R sub  a356-3760 v2310ageology1 aWeary, D., J.1 aRyder, R., T.1 aNyahay, R., E. uhttps://www.nysm.nysed.gov/staff-publications/thermal-maturity-patterns-new-york-state-using-cai-and-r-sub00538nas a2200133 4500008004100000245007300041210006900114260002100183653002500204100002000229700001800249700002500267856011200292 1999 eng d00aA Trip to Secret Caverns and Fossil Collecting, Schoharie County, NY0 aTrip to Secret Caverns and Fossil Collecting Schoharie County NY aAlbany, New York10ageology paleontology1 aCadwell, D., H.1 aKelly, W., M.1 aVanAller Hernick, L. uhttps://www.nysm.nysed.gov/staff-publications/trip-secret-caverns-and-fossil-collecting-schoharie-county-ny02165nas a2200217 4500008004100000245008800041210006900129300001200198490000700210520153500217653001601752653001401768653001001782653001401792653001401806653001801820653001801838100001701856700002201873856005201895 1998 eng d00aTributary Water Quality Feedback from the Spread of Zebra Mussels: Oswego River, NY0 aTributary Water Quality Feedback from the Spread of Zebra Mussel a453-4630 v243 a

Dramatic changes in the water quality of the Oswego River system, including Oswego Harbor, since the early 1990s brought about by zebra mussel (Dreissena polymorpha) infestation are documented. The analysis is based on summertime (June to September) water quality monitoring of the Oswego Harbor (1981 and 1993), the mouth of the Oswego River (1983 to 1993), and three upstream sites in the Oswego River system (1990, 1991, and 1994), and two benthic surveys conducted along a 70 km reach of the system to the mouth of the Oswego River in 1994. It is estimated that water in the Oswego River was filtered more than twice over this length by the mussels in 1994 (at median flow) before it reached Oswego Harbor. The zebra mussel infestation converted the Oswego River and the harbor from a turbid (low clarity), phytoplankton-rich, nutrient-depleted system, to a system with distinctly greater clarity, reduced phytoplankton concentrations, enriched in soluble reactive phosphorus. Most of this impact was attributable to dense zebra mussel populations (e.g., ∼ 30,000 indiv/m2) in a 5 km river section, located > 60 km upstream of Oswego Harbor. These changes in tributary water quality represent a form of feedback associated with the spread of the zebra mussel from the Laurentain Great Lakes. Increased attached algae growth in the Great Lakes proximate to the inflow of infested tributaries is a reasonable expectation in response to the more available form of the phosphorous load.

10achlorophyll10anutrients10ariver10atributary10aturbidity10awater quality10aZebra mussels1 aEffler, S.W.1 aSiegfried, C., A. uhttp://dx.doi.org/10.1016/S0380-1330(98)70835-402447nas a2200205 4500008004100000245009300041210006900134300001200203490000800215520181900223653001102042653001902053653001202072653002302084653001002107100002102117700002002138700001902158856006402177 1998 eng d00aTsivat Basin Conduit System persists through two surges, Bering Piedmont Glacier, Alaska0 aTsivat Basin Conduit System persists through two surges Bering P a877-8870 v1103 a

The 1993–1995 surge of Bering Glacier, Alaska, occurred in two distinct phases. Phase 1 of the surge began on the eastern sector in July, 1993 and ended in July, 1994 after a powerful outburst of subglacial meltwater into Tsivat Lake basin on the north side of Weeping Peat Island. Within days, jökulhlaup discharge built a 1.5 km2 delta of ice blocks (25–30 m) buried in outwash. By late October 1994, discharge temporarily shifted to a vent on Weeping Peat Island, where a second smaller outburst dissected the island and built two new sandar. During phase 2, which began in spring 1995 and ended within five months, continuous discharge issued from several vents along the ice front on Weeping Peat Island before returning to the Tsivat Basin.

Surge-related changes include a five- to six-fold increase in meltwater turbidity; the redirection of supercooled water in two ice-contact lakes; and an increase in the rate of glaciolacustrine sedimentation. U.S. Geological Survey aerial photos by Austin Post show large ice blocks in braided channels indicating excessive subglacial discharge in a similar position adjacent to Weeping Peat Island during the 1966–1967 surge. During the subsequent three decades of retreat, the location of ice-marginal, subglacial discharge vents remained aligned on a linear trend that describes the position of a persistent subglacial conduit system. The presence of a major conduit system, possibly stabilized by subglacial bedrock topography, is suggested by (1) high-level subglacial meltwater venting along the northern side of Weeping Peat Island during the 1966–1967 surge, (2) persistent low-level discharge between surges, and (3) the recurrence of localizing meltwater outbursts associated with both phases of the 1993–1995 surge.

10aAlaska10aBering Glacier10aglacier10ameltwater turbidit10asurge1 aFleisher, P., J.1 aCadwell, D., H.1 aMuller, E., H. uhttp://bulletin.geoscienceworld.org/content/110/7/877.short00694nas a2200193 4500008004100000245007400041210006900115260005400184300001100238653001200249100001900261700002100280700001800301700001900319700002000338700001800358700001600376856010800392 1995 eng d00aTracking the Mosses and Vascular Plants of New York State (1836-1994)0 aTracking the Mosses and Vascular Plants of New York State 183619 aWashington, D.C.bU.S. Department of the Interior a209-2110abiology1 aMiller, N., G.1 aMitchell, R., S.1 aLaRoe, E., T.1 aFarris, G., S.1 aPuckett, C., E.1 aDoran, D., P.1 aMac, M., J. uhttps://www.nysm.nysed.gov/staff-publications/tracking-mosses-and-vascular-plants-new-york-state-18361900541nas a2200145 4500008004100000245009500041210006900136300001000205490000700215653001200222100002200234700001300256700001800269856010800287 1994 eng d00aTectonic Subdivisions of the Mid-Proterozoic Adirondack Highlands in Northeastern New York0 aTectonic Subdivisions of the MidProterozoic Adirondack Highlands a82-930 v1610ageology1 aFakundiny, R., H.1 aYang, J.1 aGrant, N., K. uhttps://www.nysm.nysed.gov/staff-publications/tectonic-subdivisions-midproterozoic-adirondack-highlands00458nas a2200121 4500008004100000245007000041210006600111300001000177490000700187653001700194100001300211856011200224 1994 eng d00aTaverns, Forts, and Castles: Rediscovering Kin Hendrick's Village0 aTaverns Forts and Castles Rediscovering Kin Hendricks Village a62-940 v5210aanthropology1 aLord, P. uhttps://www.nysm.nysed.gov/staff-publications/taverns-forts-and-castles-rediscovering-kin-hendricks-village00506nas a2200121 4500008004100000245012000041210006900161300001200230490000600242653001200248100001900260856010500279 1994 eng d00aTechnology of Application of Microbials in Aquatic Environments: Use of BTI Against Blackflies in Mountainous Areas0 aTechnology of Application of Microbials in Aquatic Environments  a479-4800 v110abiology1 aMolloy, D., P. uhttps://www.nysm.nysed.gov/staff-publications/technology-application-microbials-aquatic-environments01829nas a2200145 4500008004100000245005100041210005100092300001000143490000600153520137800159653001201537100002001549700002001569856009401589 1993 eng d00aTaxonomic Notes on Some North American Orchids0 aTaxonomic Notes on Some North American Orchids a77-810 v83 a

Five taxa are discussed. (1) The new name Sacoila lanceolata var. lanceolata f. albidaviridis Catling and Sheviak is provided for the whitish-green-flowered plants, recently referred to var. luteoalbus (Rchb.f.) Luer, that occur in Florida. (2) The hydrid of Spiranthes lacera (Raf.) Raf. var. lacera and S. romanzoffiana Cham., now known from 4 localities ranging from New Brunswick west to Wisconsin, is described as Spiranthes x simpsonii Catling and Sheviak. Like its parents it has a sparsely pubescent rachis. The lip is oblong as in S. lacera var. lacera (Raf.) Raf., but the basal calli are relatively small, and the lateral sepals are basally connate and usually terminally connivent as in S. romanzoffiana Cham. The pollen in groups of 1 to 8, including the normal tetrads, is a distinctive feature of this hybrid. (3) Patterns of variation within the genus Cephalanthera and the occurrence of saprophytes in Europe and China suggest against recognizing the single North American representative within genus Eburyophyton. (4) The two species of Datylorhiza naturalized in eastern North America are D. majalis (Rchb.f.) P. F. Summerhayes ssp. praetermissa (Druce) D. M. Moore and Soo from Newfoundland, and D. cf. fuchsii (Druce) Soo from northern Ontario. (5) The new combination Platanthera zothecina (Higgins and Welsh) Catling and Sheviak is provided.

10abiology1 aCatling, P., M.1 aSheviak, C., J. uhttps://www.nysm.nysed.gov/staff-publications/taxonomic-notes-some-north-american-orchids00466nas a2200121 4500008004100000245007900041210006900120300000900189490000600198653001700204100001700221856010600238 1992 eng d00aThe Tivoli Bays as a Middle-Scale Setting for Cultural-Ecological Research0 aTivoli Bays as a MiddleScale Setting for CulturalEcological Rese a1-240 v910aanthropology1 aFunk, R., E. uhttps://www.nysm.nysed.gov/staff-publications/tivoli-bays-middlescale-setting-culturalecological-rese00641nas a2200121 4500008004100000245022700041210006900268260002200337653001200359100001800371700001800389856011200407 1991 eng d00aTitanium-zirconium-rare-earth placer resources potential of surficial sediments on the Atlantic continental shelf offshore of New York, Rhode Island, and southern Massachusetts: NYS Geological Survey Open-File Report 8m0260 aTitaniumzirconiumrareearth placer resources potential of surfici aWashington, D. C.10ageology1 aGrosz, A., E.1 aKelly, W., M. uhttps://www.nysm.nysed.gov/staff-publications/titaniumzirconiumrareearth-placer-resources-potential-surfici01384nas a2200169 4500008004100000245016400041210006900205300001400274490000700288520074400295653002501039100002101064700001901085700001801104700001901122856007301141 1990 eng d00aTerrestrial fossils within the marine Presumpscot Formation: implications for late Wisconsinan paleoenvironments and isostatic rebound along the coast of Maine0 aTerrestrial fossils within the marine Presumpscot Formation impl a1241-12460 v273 a

Investigation of terrestrially derived organic remains within the late-glacial-marine Presumpscot Formation near Portland, Maine, adds one new shrub species, six moss species, and representatives of six families of insects to the fossil biota of the deposit. White spruce (Picea glauca) dominates the plant macrofossil assemblage; the dominant pollen type is also spruce. The total biotic assemblage probably represents remnants of a forest-floor litter layer, eroded along a stream and subsequently deposited offshore. Three accelerator mass spectrometer (AMS) dates on spruce needles and cones suggest rapid burial, with marine regression from the area by ca. 11 500 BP.

10abiology paleontology1 aAnderson, R., S.1 aMiller, N., G.1 aDavis, R., B.1 aNelson, R., E. uhttp://www.nrcresearchpress.com/doi/abs/10.1139/e90-132#.VoleLlK1Xgk00651nas a2200145 4500008004100000245011700041210006900158260010200227300001200329653001200341100001800353700002200371700001400393856009800407 1990 eng d00aTransition and Change: Episodes in the Coming of Age of an Early American Community, Albany, New York, 1780-17930 aTransition and Change Episodes in the Coming of Age of an Early  aAlbany, New YorkbNew York State Commission on the Bicentennial of the United States Constitution a109-13810ahistory1 aBielinski, S.1 aSchechter, S., L.1 aTripp, W. uhttps://www.nysm.nysed.gov/staff-publications/transition-and-change-episodes-coming-age-early00572nam a2200133 4500008004100000245007900041210006900120260006200189653002500251100001600276700002100292700001400313856011100327 1988 eng d00aTrace Fossils, Small Shelly Fossils, and the Precambrian-Cambrian Boundary0 aTrace Fossils Small Shelly Fossils and the PrecambrianCambrian B aAlbany, New YorkbThe University of the State of New York10ageology paleontology1 aLanding, E.1 aNarbonne, G., M.1 aMyrow, P. uhttps://www.nysm.nysed.gov/staff-publications/trace-fossils-small-shelly-fossils-and-precambriancambrian-b00652nas a2200157 4500008004100000245010300041210006900144260006800213300000800281653002500289100001600314700001600330700002100346700001400367856011300381 1988 eng d00aTrace Fossils, Small Shelly Fossils, and the PrecambrianCambrian Boundary--A Pre-meeting Viewpoint0 aTrace Fossils Small Shelly Fossils and the PrecambrianCambrian B aAlbany, North CarolinabThe University of the State of New York a1-310ageology paleontology1 aLanding, E.1 aLanding, E.1 aNarbonne, G., M.1 aMyrow, P. uhttps://www.nysm.nysed.gov/staff-publications/trace-fossils-small-shelly-fossils-and-precambriancambrian-b-002729nas a2200145 4500008004100000245011400041210006900155300001200224490000700236520225300243653001702496100001602513700001402529856004002543 1987 eng d00aTrace Fossils and Regional Significance of a Middle Devonian (Givetian) Disconformity in Southwestern Ontario0 aTrace Fossils and Regional Significance of a Middle Devonian Giv a205-2300 v613 a
The Hungry Hollow Formation on the southeastern margin of the Michigan Basin is interpreted as a composite stratigraphic unit representing the lateral equivalents of two depositional cycles in the northern Appalachian Basin. The basal beds (? = Pompey and upper Levanna transgressive hemicycle of the upper Skaneateles Formation in New York) are separated by disconformity surfaces both from the underlying Arkona Shale and from the upper part of the Hungry Hollow (=upper part of Centerfield Limestone Member). These basal beds were deposited on eroded, overcompacted claystones of the Arkona Shale, contain a diverse suite of remanie sediments, and fill deep, delicately sculpted furrows of Cruziana transversa n. ichnosp., C. reticulata n. ichnosp., and Rusophycus bilobatum (Vanuxem, 1842). This lower disconformity may be recognizable regionally over the Northern Midcontinent. Overlying beds feature the lowest local occurrence of an offshore-aspect conodont fauna of the lower Polygnathus varcus Subzone. The underlying Arkona Shale yields Icriodus-dominated (nearer-shore aspect) faunas apparently representing Polygnathus xylus ensensis Zone assemblages. The upper part of the Hungry Hollow Formation and overlying lower part of the Widder Formation represent an offlap-onlap cycle within the lower Polygnathus varcus Subzone that is comparable to that of the upper part of the Centerfield Limestone. Cruziana and Rusophycus from the Hungry Hollow were not originally produced as "undertracks" but were formed at the sediment--water interface on erosion-resistant, overconsolidated muds. The producer of Cruziana reticulata n. ichnosp. appeared in the benthic community of the field area before the excavator of C. transversa n. ichnosp. and of Rusophycus bilobatum (possibly the trilobite Dipleura). The degree of limb swing required to produce the reticulate scratch patterns in C. reticulata n. ichnosp. suggests the evolution of specialized coxa-sternite and inter-podomere hinges that were not previously considered to be present in trilobites. Comparable reticulate scratch patterns occur as early as the earliest Cambrian and are apparently related to excavation on disconformity-related mud firmgrounds.
10apaleontology1 aLanding, E.1 aBrett, C. uhttp://www.jstor.org/stable/130531800493nas a2200133 4500008004100000245010100041210006900142300001200211490000800223653002500231100002100256700002200277856006000299 1987 eng d00aTwo New Species of Parrots (Aves: Psittacidae) from Archeological Sites in the Marquesas Islands0 aTwo New Species of Parrots Aves Psittacidae from Archeological S a518-5280 v10010aanthropology biology1 aSteadman, D., W.1 aZarriello, M., C. uhttps://www.biodiversitylibrary.org/part/44710#/summary00561nas a2200145 4500008004100000245005800041210005700099260007100156300001000227653001200237100002200249700002000271700002100291856010300312 1986 eng d00aTrans-Adirondack Mountains Structural Discontinuities0 aTransAdirondack Mountains Structural Discontinuities aSalt Lake City, UtahbInternational Basement Tectonics Association a64-7510ageology1 aFakundiny, R., H.1 aAldrich, M., J.1 aLaughlin, A., W. uhttps://www.nysm.nysed.gov/staff-publications/transadirondack-mountains-structural-discontinuities02420nas a2200157 4500008004100000245012200041210006900163300001400232490000700246520185600253653002502109100001602134700001902150700002002169856007302189 1986 eng d00aTempo of Earliest Ordovician Graptolite Faunal Succession: Conodont-based Correlations from the Tremadocian of Quebec0 aTempo of Earliest Ordovician Graptolite Faunal Succession Conodo a1928-19490 v233 a

Successive Tremadocian planktic dendroid graptolite assemblages from continental slope sequences in Quebec can be correlated with North American platform biozonations on the basis of conodonts. Anisograptid-bearing (Assemblage 2), middle Tremadocian "Matane faunas" are associated with Early Ordovician Rossodus manitouensis Zone (new designation) conodonts. Younger middle Tremadocian faunas with adelograptids (Assemblage 3) are no younger than the Rossodus manitouensis Zone. Key dendroid evolutionary–immigration events take place within the lower conodont Fauna B interval. Rooted dendroids near Cap des Rosiers, Quebec, and in eastern New York State occur with lower Fauna B conodonts and the trilobites Pareuloma and Borthaspidella. However, the earliest Tremadocian (and earliest Ordovician) dendroid immigration event, represented by the local lowest occurrence of faunas with Dictyonema flabelliforme s.l. at localities in western Newfoundland, eastern New York State, Norway, and eastern China, also lies within the lower Fauna B interval. Finally, the lowest occurrence of key Assemblage 2 dendroid taxa falls within the lower Fauna B interval at the latter localities.The Rossodus manitouensis Zone is proposed as a new designation for a biostratigraphic unit that is appropriate for North American marginal and open shelf sequences. This zone is approximately equivalent to the "Loxodus bransoni Interval" of other authors and is characterized by Fauna C conodonts. Newly described taxa include Rossodus? highgatensis n. sp., Scolopodus? praecornuformis n. sp., and Variabiloconus n. gen.

10ageology paleontology1 aLanding, E.1 aBarnes, C., R.1 aStevens, R., K. uhttp://www.nrcresearchpress.com/doi/abs/10.1139/e86-180#.Vo5q61K1Xgk02162nas a2200133 4500008004100000245008200041210006900123300001000192490000700202520170800209653001201917100002101929856007801950 1986 eng d00aTwo New Species of Rails (Aves: Rallidae) from Mangaia, Southern Cook Islands0 aTwo New Species of Rails Aves Rallidae from Mangaia Southern Coo a38-540 v403 a

Two species of rails, Porzana rua n. sp. and Gallirallus ripleyi n. sp., are described from bones of late Holocene age found in caves on Mangaia, southern Cook Islands. Their relatively small pectoral elements show that both of these species were flightless. Porzana rua resembles most closely the living P. atra of Henderson Island and the recently extinct P. monasa of Kosrae Island, Carolines. Gallirallus ripleyi is most similar to the recently extinct G. wakensis of Wake Island. Some combination of predation and habitat alteration by humans and introduced mammals (rats, dogs, and pigs) is probably responsible for the extinction of P. rua and G. ripleyi within the past 1000 years. Fossils of a third species of rail from the Mangaian caves are referred to the living species Porzana tabuensis, although these specimens may represent an undescribed subspecies. Porzana tabuensis might survive on Mangaia and elsewhere in the southern Cook Islands, although entire specimens have never been collected. An X ray of the only two specimens (skins) of Porzana monasa (Kittlitz) shows that this species from Kosrae (Kusai) Island, Carolines, was flightless or nearly so. It is likely that all islands in the Pacific were inhabited by one or more species of flightless rail before the arrival of humans. In both Porzana and Gallirallus, at least one early wave of colonization produced flightless species throughout Oceania, followed by a less thorough and much more recent (probably late Holocene) wave of colonization by the volant P. tabuensis and G. philippensis.

10abiology1 aSteadman, D., W. uhttp://scholarspace.manoa.hawaii.edu/bitstream/10125/1002/1/v40-27-43.pdf00441nas a2200133 4500008004100000245003600041210003600077260003300113300001400146653002500160100001900185700002100204856008200225 1984 eng d00aTertiary and Quaternary fossils0 aTertiary and Quaternary fossils bHattori Botanical Laboratory a1194-123710abiology paleontology1 aMiller, N., G.1 aSchuster, R., M. uhttps://www.nysm.nysed.gov/staff-publications/tertiary-and-quaternary-fossils00598nas a2200133 4500008004100000245012500041210006900166260006100235300000900296653001700305100001900322700001800341856010500359 1983 eng d00aTrading in Metaphors: The Magic of Beads, Another Perspective Upon Indian-European Contact in Northeastern North America0 aTrading in Metaphors The Magic of Beads Another Perspective Upon aRochester, New YorkbRochester Museum and Science Center a5-2810aanthropology1 aHamell, G., R.1 aHayes, C., F. uhttps://www.nysm.nysed.gov/staff-publications/trading-metaphors-magic-beads-another-perspective-upon02268nas a2200157 4500008004100000245015300041210006900194300001200263490000700275520169100282653001201973100001901985700001802004700001802022856007002040 1983 eng d00aTesting of the Air Resources Laboratories Trajectory Model on Cases of Pollen Wet Deposition After Long-distance Transport from Known Source Regions0 aTesting of the Air Resources Laboratories Trajectory Model on Ca a213-2200 v173 a
A version of the Air Resources Laboratories Atmospheric Transport and Dispersion Model was tested to determine how well it could identify probable pathways and source regions of airborne pollens from non-local sources which were deposited in precipitation at Albany, New York. The model calculates either forward or backward trajectories from any selected location starting every 6-h during a chosen time period. Each trajectory is calculated using transport winds averaged over a selected vertical layer and is based on past upper air observations stored in the computer.
At Albany, New York, airborne pollens were sampled during both wet and dry weather. Samples were examined under a microscope and pollen grains identified and counted. In this study, only obviously fresh pollens of non-local origin are considered. These were obtained primarily in the winter and early spring months before local pollens of the same or similar species were released and include species whose ranges do not reach the north-eastern states. These cases document atmospheric transport from distant source regions and subsequent wet deposition.
Probable source regions were determined from ranges and flowering dates of the taxa collected. Backward trajectories from Albany were computed for nine precipitation events. In all cases, the trajectories passed through or very near previously identified source regions located to the south or south-west. Travel times ranged from 10 to over 50 h but were mostly from 18 to 42 h. Results demonstrate the utility of the model and the feasibility of locating source regions of materials transported over long distances.
10abiology1 aRaynor, G., S.1 aHayes, J., V.1 aLewis, D., M. uhttp://www.sciencedirect.com/science/article/pii/000469818390035500464nas a2200121 4500008004100000245008400041210006900125300001000194490000600204653001200210100002000222856010000242 1983 eng d00aA Three-stage Model for the Tectonic History of the Adirondack Region, New York0 aThreestage Model for the Tectonic History of the Adirondack Regi a61-720 v510ageology1 aWhitney, P., R. uhttps://www.nysm.nysed.gov/staff-publications/threestage-model-tectonic-history-adirondack-regi00545nas a2200121 4500008004100000245014900041210006900190300001200259490000700271653001200278100002200290856011100312 1982 eng d00aTrophic Relations of Crangon franciscorum Stimpson and Palaemon macrodactylus Rathbum: Predation on the Opossum Shrimp, Neomysis mercedis Holmes0 aTrophic Relations of Crangon franciscorum Stimpson and Palaemon  a129-1390 v8910abiology1 aSiegfried, C., A. uhttps://www.nysm.nysed.gov/staff-publications/trophic-relations-crangon-franciscorum-stimpson-and-palaemon01272nas a2200157 4500008004100000245013600041210006900177300001200246490000800258520074500266653001201011100001701023700001901040700001501059856004001074 1981 eng d00aTetrahymena rotunda sp. n. (Hymenostomatida: Tetrahymenidae), A Ciliate Parasite of the Hemolymph of Simulium (Diptera: Simuliidae)0 aTetrahymena rotunda sp n Hymenostomatida Tetrahymenidae A Ciliat a134-1410 v1003 a
This report is the first confirmed record of ciliatosis in North American black flies. A new species, Tetrahymena rotunda n. sp. is diagnosed as a parasite of Simulium spp. This species is characterized by its globose shape, large size and total kinety number, and relatively small buccal cavity. In a five-year period (1976-1980) in upper New York State, the infection rate in Simulium spp. parasitized by this tetrahymenid was low, usually <2%. Ciliates were found in Simulium tuberosum larvae and in the larval, pupal, and adult stages of Simulium venustum. Hosts typically harbored ~10 ciliates, a number far less than generally reported for ciliate-infected dipterans.
10abiology1 aLynn, D., H.1 aMolloy, D., P.1 aLeBrun, R. uhttp://www.jstor.org/stable/322579600856nas a2200145 4500008004100000245008000041210006900121300001200190490000700202520041000209653001700619100001700636700001700653856004000670 1978 eng d00aTotiglobus, an Unusual New Edrioasteroid from the Middle Cambrian of Nevada0 aTotiglobus an Unusual New Edrioasteroid from the Middle Cambrian a243-2660 v523 a
A new and unusual edrioasteroid, Totiglobus nimius n. gen., n. sp., from the Middle Cambrian Chisholm Shale, eastern Nevada, is the earliest representative of the order Edrioasterida. Totiglobus has a fully plated aboral surface which suggests this is a primitive trait within the class. It has a large basal discoidal structure which was probably used for attachment.
10apaleontology1 aBell, B., M.1 aSprinkle, J. uhttp://www.jstor.org/stable/130370101026nas a2200133 4500008004100000245007800041210006900119300001000188490000700198520061100205653001200816100002200828856004200850 1978 eng d00aTerrestrial Mites of New York-VI. Further Notes on Tarsonemidae (Acarina)0 aTerrestrial Mites of New YorkVI Further Notes on Tarsonemidae Ac a66-860 v863 a
Twenty-one species of Tarsonemus known from New York are keyed. Five new species are described and illustrated: Tarsonemus acerbilis and T. edwardi found associated with eriophyid mites in galls, and T. blakemorei, T. socius and T. vulgaris taken from bird nests and stored grain. Five tarsonemid mites previously reported from nest habitat are newly recorded from stored grain; these are: T. ascitus Delfinado, T. confusus Ewing, T. granarius Lindquist, T. imitatus Delfinado and T. waitei Banks.
10abiology1 aDelfinado, M., D. uhttp://www.jstor.org/stable/25009100 01432nas a2200145 4500008004100000245010600041210006900147300001100216490000700227520095900234653001201193100002201205700001801227856004101245 1978 eng d00aTerrestrial Mites of New York-VII. Key to the Species of Scutacaridae and Descriptions of New Species0 aTerrestrial Mites of New YorkVII Key to the Species of Scutacari a87-1010 v863 a
  1. Thirty-five species and three subspecies of Scutacaridae are listed from New York. An identification key to the species is given. In addition, three new species and 1 new subspecies are described and figured; these are: Imparipes cupes, Scutacarus (S.) meansi, S. (S.) unicus indefinitus, and S. (Variatipes) subaffinis. The specimens were collected from bird nests, dog food, and from a cupedid beetle. Scutacarus (S.) subellipticus Delfinado & Baker, 1976 (Dec.) is a synonym of S. (S.) curtus Delfinado, Baker & Abbatiello, 1976 (June). The following are transferred from Imparipes Berlese to Archidispus Karafiat: insulanus (Delfinado, Baker & Abbatiello), longitarsus (Delfinado, Baker & Abbatiello), similis (Delfinado, Baker & Abbatiello) and tarsalis (Delfinado, Baker & Abbatiello).
10abiology1 aDelfinado, M., D.1 aBaker, E., W. uhttp://www.jstor.org/stable/2500910100521nas a2200145 4500008004100000245007000041210006600111300001000177490000700187653001200194100001800206700002200224700002300246856010600269 1976 eng d00aTerrestrial Mites of New York II. Mites in Birds' Nests (Acarina)0 aTerrestrial Mites of New York II Mites in Birds Nests Acarina a48-660 v8410abiology1 aBaker, E., W.1 aDelfinado, M., D.1 aAbbatiello, M., J. uhttps://www.nysm.nysed.gov/staff-publications/terrestrial-mites-new-york-ii-mites-birds-nests-acarina00516nas a2200133 4500008004100000245008100041210006900122300001200191490000700203653001200210100002200222700002600244856011200270 1976 eng d00aTerrestrial Mites of New York (Acarina). IV. Cheyletidae and Cheyletiellidae0 aTerrestrial Mites of New York Acarina IV Cheyletidae and Cheylet a189-1960 v8410abiology1 aDelfinado, M., D.1 aKhaing-Fields, A., A. uhttps://www.nysm.nysed.gov/staff-publications/terrestrial-mites-new-york-acarina-iv-cheyletidae-and-cheylet00408nas a2200121 4500008004100000245005100041210004900092300001200141490000700153653001200160100002200172856009200194 1976 eng d00aTerrestrial Mites of New York. V- Tarsonemidae0 aTerrestrial Mites of New York V Tarsonemidae a255-2740 v8410abiology1 aDelfinado, M., D. uhttps://www.nysm.nysed.gov/staff-publications/terrestrial-mites-new-york-v-tarsonemidae00531nas a2200145 4500008004100000245007300041210006900114300001200183490000700195653001200202100002200214700001800236700002300254856010800277 1976 eng d00aTerrestrial Mites of New York-III. The Family Scutacaridae (Acarina)0 aTerrestrial Mites of New YorkIII The Family Scutacaridae Acarina a106-1450 v8410abiology1 aDelfinado, M., D.1 aBaker, E., W.1 aAbbatiello, M., J. uhttps://www.nysm.nysed.gov/staff-publications/terrestrial-mites-new-yorkiii-family-scutacaridae-acarina00493nas a2200145 4500008004100000245005900041210005900100300001200159490000700171653001200178100001900190700001800209700001800227856010200245 1976 eng d00aTemporal Variability in Airborne Pollen Concentrations0 aTemporal Variability in Airborne Pollen Concentrations a386-3960 v3610abiology1 aRaynor, G., S.1 aHayes, J., V.1 aOgden, E., C. uhttps://www.nysm.nysed.gov/staff-publications/temporal-variability-airborne-pollen-concentrations00955nas a2200145 4500008004100000245011100041210006900152300001200221490000700233520047600240653001200716100002200728700001800750856004100768 1974 eng d00aTerrestrial Mites of New York (Acarina: Prostigmata), I: Tarsocheylidae, Paratydeidae, and Pseudocheylidae0 aTerrestrial Mites of New York Acarina Prostigmata I Tarsocheylid a202-2110 v823 a
The mites here described were collected from Long Island, Lake Champlain region, and the Mohawk Valley area, New York, in June-October of 1973. The new species described are: Tarsocheylidae, Hoplocheylus similis, H. americanus; Paratydeidae, Scolotydaeus simplex; Pseudocheylidae, Anoplocheylus transiens. Twenty-six figures are presented. The genus Neotydeus Baker is synonymized with Scolotydaeus Berlese.
10abiology1 aDelfinado, M., D.1 aBaker, E., W. uhttp://www.jstor.org/stable/2500892900461nas a2200133 4500008004100000245006100041210006100102300001000163490000700173653001700180100001700197700001300214856010000227 1972 eng d00aTwo Stratified Alluvial Sites in the Upper Hudson Valley0 aTwo Stratified Alluvial Sites in the Upper Hudson Valley a27-610 v4210aanthropology1 aFunk, R., E.1 aLord, P. uhttps://www.nysm.nysed.gov/staff-publications/two-stratified-alluvial-sites-upper-hudson-valley00447nam a2200109 4500008004100000245008900041210006900130260006200199653001700261100002000278856003900298 1971 eng d00aA Typology and Nomenclature for New York Projectile Points (Second, revised edition)0 aTypology and Nomenclature for New York Projectile Points Second  aAlbany, New YorkbThe University of the State of New York10aanthropology1 aRitchie, W., A. uhttp://purl.nysed.gov/nysl/108805300433nas a2200133 4500008004100000245006500041210006500106300001200171490000700183653001200190100001700202700002300219856005700242 1966 eng d00aTesting Blackfly Larvicides in the Laboratory and in Streams0 aTesting Blackfly Larvicides in the Laboratory and in Streams a405-4210 v3410abiology1 aJamnback, H.1 aFrempong-Boadu, J. uhttp://www.ncbi.nlm.nih.gov/pmc/articles/PMC2475988/00549nas a2200157 4500008004100000245005200041210005200093260005100145300001200196653002500208100001800233700001800251700001500269700001300284856009400297 1965 eng d00aTrapping Methods for Modern Pollen Rain Studies0 aTrapping Methods for Modern Pollen Rain Studies aSan Francisco, CaliforniabW. H. Freeman & Co. a613-62610abiology paleontology1 aLewis, D., M.1 aOgden, E., C.1 aKummel, B.1 aRaup, D. uhttps://www.nysm.nysed.gov/staff-publications/trapping-methods-modern-pollen-rain-studies00353nas a2200121 4500008004100000245005000041210004600091300001200137490000700149653001700156100001900173856003900192 1962 eng d00a"This Island, the World on the Turtle's Back"0 aThis Island the World on the Turtles Back a283-3000 v7510aanthropology1 aFenton, W., N. uhttp://www.jstor.org/stable/53836500415nam a2200109 4500008004100000245006300041210006100104260006400165653001700229100002000246856003900266 1961 eng d00aA Typology and Nomenclature for New York Projectile Points0 aTypology and Nomenclature for New York Projectile Points aAlbany, New JerseybThe University of the State of New York10aanthropology1 aRitchie, W., A. uhttp://purl.nysed.gov/nysl/108805300423nas a2200109 4500008004100000245005900041210005800100260002100158653001200179100001800191856010400209 1960 eng d00aTagging and Sampling Ragweed Pollen, progress Report 10 aTagging and Sampling Ragweed Pollen progress Report 1 aAlbany, New York10abiology1 aOgden, E., C. uhttps://www.nysm.nysed.gov/staff-publications/tagging-and-sampling-ragweed-pollen-progress-report-100327nas a2200121 4500008004100000245002400041210002400065300001000089490000700099653001200106100002000118856006700138 1958 eng d00aTurtles of New York0 aTurtles of New York a22-270 v1210abiology1 aReilley, E., M. uhttps://www.nysm.nysed.gov/staff-publications/turtles-new-york00377nam a2200109 4500008004100000245004100041210004100082260006200123653001700185100002000202856004500222 1957 eng d00aTraces of Early Man in the Northeast0 aTraces of Early Man in the Northeast aAlbany, New YorkbThe University of the State of New York10aanthropology1 aRitchie, W., A. uhttp://purl.org/net/nysl/nysdocs/108801200496nas a2200121 4500008004100000245016000041210006900201300001200270490000800282653002500290100001900315856004000334 1956 eng d00aToward the Gradual Civilization of the Indian Natives: The Missionary and Linguistic Work of Asher Wright (1803-1875) among the Senecas of Western New York0 aToward the Gradual Civilization of the Indian Natives The Missio a567-5810 v10010aanthropology history1 aFenton, W., N. uhttp://www.jstor.org/stable/314379000337nas a2200121 4500008004100000245003900041210003900080300001200119490000600131653001700137100002000154856004100174 1951 eng d00aTheir Mouths are Stopped with Dust0 aTheir Mouths are Stopped with Dust a136-1440 v410aanthropology1 aRitchie, W., A. uhttp://www.jstor.org/stable/4166298800453nas a2200133 4500008004100000245007800041210006900119300001200188490000700200653001200207100002000219700002000239856006000259 1946 eng d00aThermal Aerosol Fogs to Control Clothes Moths in a Wool Storage Warehouse0 aThermal Aerosol Fogs to Control Clothes Moths in a Wool Storage  a241-2450 v3910abiology1 aCollins, D., L.1 aGlasgow, R., D. uhttp://jee.oxfordjournals.org/content/39/2/241.abstract00447nas a2200121 4500008004100000245009600041210006900137490000700206653001200213100002000225700002000245856006000265 1946 eng d00aThe Thermal Aerosol Fog Generator for Large Scale Application of DDT and Other Insecticides0 aThermal Aerosol Fog Generator for Large Scale Application of DDT0 v3910abiology1 aGlasgow, R., D.1 aCollins, D., L. uhttp://jee.oxfordjournals.org/content/39/2/227.abstract00379nas a2200121 4500008004100000245006500041210006500106300001200171490000700183653001200190100001500202856004000217 1945 eng d00aTemperature and Growth Studies of the Northern Cliff Swallow0 aTemperature and Growth Studies of the Northern Cliff Swallow a207-2160 v6210abiology1 aStoner, D. uhttp://www.jstor.org/stable/407969800433nam a2200109 4500008004100000245007100041210006900112260006200181653001200243100002300255856004500278 1944 eng d00aTitaniferous Magnetite Deposits of the Lake Sanford Area, New York0 aTitaniferous Magnetite Deposits of the Lake Sanford Area New Yor aAlbany, New YorkbThe University of the State of New York10ageology1 aStephenson, R., C. uhttp://purl.org/net/nysl/nysdocs/279141000501nam a2200109 4500008004100000245007100041210006800112260006500180653001700245100001800262856011100280 1939 eng d00aType invertebrate fossils of North America (Devonian): Eurypterida0 aType invertebrate fossils of North America Devonian Eurypterida aPhiladelphia, PennsylvaniabWagner Free Institute of Science10apaleontology1 aRuedemann, R. uhttps://www.nysm.nysed.gov/staff-publications/type-invertebrate-fossils-north-america-devonian-eurypterida00461nam a2200109 4500008004100000245006000041210005900101260006200160653001200222100001500234856010200249 1939 eng d00aTemperature, Growth and Other Studies on Eastern Phoebe0 aTemperature Growth and Other Studies on Eastern Phoebe aAlbany, New YorkbThe University of the State of New York10abiology1 aStoner, D. uhttps://www.nysm.nysed.gov/staff-publications/temperature-growth-and-other-studies-eastern-phoebe00335nas a2200121 4500008004100000245003600041210003600077300001200113490000700125653001200132100001500144856005400159 1937 eng d00aThree Returns of a Bank Swallow0 aThree Returns of a Bank Swallow a469-4700 v8610abiology1 aStoner, D. uhttp://science.sciencemag.org/content/86/2238/46900429nam a2200109 4500008004100000245005000041210004900091260006200140653001200202100001500214856009000229 1936 eng d00aTen Years' Returns from Banded Black Swallows0 aTen Years Returns from Banded Black Swallows aAlbany, New YorkbThe University of the State of New York10abiology1 aStoner, D. uhttps://www.nysm.nysed.gov/staff-publications/ten-years-returns-banded-black-swallows00359nas a2200121 4500008004100000245005500041210005500096300001200151490000700163653001200170100001500182856004000197 1935 eng d00aTemperature and Growth Studies on the Barn Swallow0 aTemperature and Growth Studies on the Barn Swallow a400-4070 v5210abiology1 aStoner, D. uhttp://www.jstor.org/stable/407751200418nas a2200121 4500008004100000245005600041210005600097300001200153490000700165653001200172100001800184856009400202 1931 eng d00aTree Planting for the 1932 Washington Commemoration0 aTree Planting for the 1932 Washington Commemoration a172-1730 v1710abiology1 aHouse, H., D. uhttps://www.nysm.nysed.gov/staff-publications/tree-planting-1932-washington-commemoration00424nas a2200121 4500008004100000245006100041210005600102300001200158490000700170653001200177100001800189856009500207 1931 eng d00aThe Tangential Master-Streams of the Adirondack Drainage0 aTangential MasterStreams of the Adirondack Drainage a431-4400 v2210ageology1 aRuedemann, R. uhttps://www.nysm.nysed.gov/staff-publications/tangential-masterstreams-adirondack-drainage00429nas a2200133 4500008004100000245003000041210002600071260006200097300001000159653001700169100001900186700001800205856007200223 1929 eng d00aThe Thatcher Wampum Belts0 aThatcher Wampum Belts aAlbany, New YorkbThe University of the State of New York a53-5810aanthropology1 aClarke, N., T.1 aAdams, C., C. uhttps://www.nysm.nysed.gov/staff-publications/thatcher-wampum-belts00414nas a2200121 4500008004100000245005400041210005200095300001200147490000700159653001200166100001900178856009500197 1929 eng d00aThree New Species of Spiders (Family Linyphiidae)0 aThree New Species of Spiders Family Linyphiidae a101-1050 v4110abiology1 aCrosby, R., J. uhttps://www.nysm.nysed.gov/staff-publications/three-new-species-spiders-family-linyphiidae00353nas a2200121 4500008004100000245003300041210003300074300001000107490000600117653001200123100001700135856007900152 1924 eng d00aTwo New Javanese Gall Midges0 aTwo New Javanese Gall Midges a89-920 v210abiology1 aFelt, E., P. uhttps://www.nysm.nysed.gov/staff-publications/two-new-javanese-gall-midges00373nas a2200121 4500008004100000245005200041210004300093300000800136490000700144653002500151100001900176856005600195 1921 eng d00aThe Temple Hill (Orange County, N. Y.) Mastodon0 aTemple Hill Orange County N Y Mastodon a1700 v5410abiology paleontology1 aBishop, S., C. uhttp://science.sciencemag.org/content/54/1391/170.100371nas a2200121 4500008004100000245003800041210003800079300001200117490000700129653001200136100001700148856008400165 1921 eng d00aThree New Subtropical Gall Midges0 aThree New Subtropical Gall Midges a141-1430 v2210abiology1 aFelt, E., P. uhttps://www.nysm.nysed.gov/staff-publications/three-new-subtropical-gall-midges00349nas a2200121 4500008004100000245003100041210003100072300001200103490000600115653001200121100001700133856007700150 1918 eng d00aTwo Injurious Leaf Maggots0 aTwo Injurious Leaf Maggots a425-4260 v210abiology1 aFelt, E., P. uhttps://www.nysm.nysed.gov/staff-publications/two-injurious-leaf-maggots00320nas a2200121 4500008004100000245002100041210002100062300001200083490000700095653001200102100001700114856006700131 1917 eng d00aTwo New Sawflies0 aTwo New Sawflies a191-1920 v4910abiology1 aFelt, E., P. uhttps://www.nysm.nysed.gov/staff-publications/two-new-sawflies00365nas a2200121 4500008004100000245003800041210003800079300001000117490000600127653001200133100001700145856008100162 1913 eng d00aTable of Hickory Leaf Gall Midges0 aTable of Hickory Leaf Gall Midges a98-990 v810abiology1 aFelt, E., P. uhttps://www.nysm.nysed.gov/staff-publications/table-hickory-leaf-gall-midges00335nas a2200121 4500008004100000245002600041210002600067300001200093490000700105653001200112100001700124856007200141 1913 eng d00aThree New Gall Midges0 aThree New Gall Midges a304-3080 v4510abiology1 aFelt, E., P. uhttps://www.nysm.nysed.gov/staff-publications/three-new-gall-midges00344nas a2200121 4500008004100000245002900041210002900070300001200099490000700111653001200118100001700130856007500147 1913 eng d00aTwo Canadian Gall Midges0 aTwo Canadian Gall Midges a417-4180 v4010abiology1 aFelt, E., P. uhttps://www.nysm.nysed.gov/staff-publications/two-canadian-gall-midges00354nas a2200121 4500008004100000245003500041210003100076300001200107490000700119653001200126100001700138856007700155 1911 eng d00a Three New Gall Midges (Dipt.)0 aThree New Gall Midges Dipt a190-1930 v1910abiology1 aFelt, E., P. uhttps://www.nysm.nysed.gov/staff-publications/three-new-gall-midges-dipt00329nas a2200121 4500008004100000245002400041210002400065300001200089490000700101653001200108100001700120856007000137 1911 eng d00aTwo New Gall Midges0 aTwo New Gall Midges a194-1960 v4310abiology1 aFelt, E., P. uhttps://www.nysm.nysed.gov/staff-publications/two-new-gall-midges00347nas a2200121 4500008004100000245003200041210002900073300001200102490000700114653001200121100001700133856007500150 1911 eng d00aTwo New Gall Midges (Dipt.)0 aTwo New Gall Midges Dipt a109-1110 v2210abiology1 aFelt, E., P. uhttps://www.nysm.nysed.gov/staff-publications/two-new-gall-midges-dipt00307nas a2200121 4500008004100000245001800041210001800059300000800077490000700085653001200092100001700104856006400121 1910 eng d00aTree Spraying0 aTree Spraying a7890 v7510abiology1 aFelt, E., P. uhttps://www.nysm.nysed.gov/staff-publications/tree-spraying00301nas a2200121 4500008004100000245001600041210001600057300000800073490000700081653001200088100001700100856006200117 1910 eng d00aTulip Scale0 aTulip Scale a8400 v7510abiology1 aFelt, E., P. uhttps://www.nysm.nysed.gov/staff-publications/tulip-scale00333nas a2200121 4500008004100000245002600041210002600067300001000093490000700103653001200110100001700122856007200139 1910 eng d00aTwo New Cecidomyiidae0 aTwo New Cecidomyiidae a10-120 v2110abiology1 aFelt, E., P. uhttps://www.nysm.nysed.gov/staff-publications/two-new-cecidomyiidae00313nas a2200121 4500008004100000245002000041210002000061300000800081490000700089653001200096100001700108856006600125 1909 eng d00aTortoise Beetle0 aTortoise Beetle a7550 v7410abiology1 aFelt, E., P. uhttps://www.nysm.nysed.gov/staff-publications/tortoise-beetle00313nas a2200109 4500008004100000245002500041210002500066300001200091653001200103100001700115856007100132 1907 eng d00aThree Imported Pests0 aThree Imported Pests a144-14910abiology1 aFelt, E., P. uhttps://www.nysm.nysed.gov/staff-publications/three-imported-pests00299nas a2200121 4500008004100000245001600041210001600057300000600073490000700079653001200086100001700098856006200115 1907 eng d00aTree Brands0 aTree Brands a80 v7210abiology1 aFelt, E., P. uhttps://www.nysm.nysed.gov/staff-publications/tree-brands00343nas a2200121 4500008004100000245003000041210003000071300000800101490000700109653001200116100001700128856007600145 1907 eng d00aTwo Common Orchard Scales0 aTwo Common Orchard Scales a5520 v7210abiology1 aFelt, E., P. uhttps://www.nysm.nysed.gov/staff-publications/two-common-orchard-scales00333nas a2200121 4500008004100000245002700041210002700068300000800095490000600103653001200109100001700121856007300138 1907 eng d00aTwo Destructive Borers0 aTwo Destructive Borers a3000 v410abiology1 aFelt, E., P. uhttps://www.nysm.nysed.gov/staff-publications/two-destructive-borers00316nas a2200121 4500008004100000245002100041210002100062300000800083490000700091653001200098100001700110856006700127 1906 eng d00aTulip Tree Scale0 aTulip Tree Scale a7540 v7110abiology1 aFelt, E., P. uhttps://www.nysm.nysed.gov/staff-publications/tulip-tree-scale00313nas a2200121 4500008004100000245002100041210002100062300000800083490000700091653001200098100001700110856006400127 1905 eng d00aTo Corn Planters0 aTo Corn Planters a4920 v7010abiology1 aFelt, E., P. uhttps://www.nysm.nysed.gov/staff-publications/corn-planters00328nas a2200121 4500008004100000245002500041210002500066300000800091490000700099653001200106100001700118856007100135 1905 eng d00aTrapping Squash Bugs0 aTrapping Squash Bugs a7470 v7010abiology1 aFelt, E., P. uhttps://www.nysm.nysed.gov/staff-publications/trapping-squash-bugs00318nas a2200121 4500008004100000245002100041210002100062300000800083490000700091653001200098100001700110856006900127 1903 eng d00aTulip Tree Scale0 aTulip Tree Scale a7120 v6810abiology1 aFelt, E., P. uhttps://www.nysm.nysed.gov/staff-publications/tulip-tree-scale-000310nas a2200121 4500008004100000245001900041210001900060300000800079490000700087653001200094100001700106856006500123 1903 eng d00aTwo Tree Pests0 aTwo Tree Pests a8520 v6810abiology1 aFelt, E., P. uhttps://www.nysm.nysed.gov/staff-publications/two-tree-pests00316nas a2200121 4500008004100000245002100041210002100062300000800083490000700091653001200098100001700110856006700127 1902 eng d00aTent Caterpillar0 aTent Caterpillar a4140 v6710abiology1 aFelt, E., P. uhttps://www.nysm.nysed.gov/staff-publications/tent-caterpillar00304nas a2200121 4500008004100000245001700041210001700058300000800075490000700083653001200090100001700102856006300119 1902 eng d00aTussock Moth0 aTussock Moth a3510 v6710abiology1 aFelt, E., P. uhttps://www.nysm.nysed.gov/staff-publications/tussock-moth00319nas a2200121 4500008004100000245002200041210002200063300000800085490000700093653001200100100001700112856006800129 1901 eng d00aTent Caterpillars0 aTent Caterpillars a3860 v6610abiology1 aFelt, E., P. uhttps://www.nysm.nysed.gov/staff-publications/tent-caterpillars00331nas a2200121 4500008004100000245002800041210002500069300000800094490000700102653001200109100001700121856007100138 1901 eng d00aTrap-lanterns - Warning0 aTraplanterns Warning a4060 v6610abiology1 aFelt, E., P. uhttps://www.nysm.nysed.gov/staff-publications/traplanterns-warning00547nas a2200145 4500008004100000245005700041210005700098260006200155300001000217653001700227100001800244700002000262700001900282856010000301 1901 eng d00aTrenton conglomerate of Rysedorph Hill and Its Fauna0 aTrenton conglomerate of Rysedorph Hill and Its Fauna aAlbany, New YorkbThe University of the State of New York a3-11410apaleontology1 aRuedemann, R.1 aMerrill, J., H.1 aClarke, J., M. uhttps://www.nysm.nysed.gov/staff-publications/trenton-conglomerate-rysedorph-hill-and-its-fauna00370nas a2200121 4500008004100000245003900041210003900080300000800119490000700127653001200134100001700146856008500163 1900 eng d00aTent Caterpillars and Canker Wbrms0 aTent Caterpillars and Canker Wbrms a6050 v6510abiology1 aFelt, E., P. uhttps://www.nysm.nysed.gov/staff-publications/tent-caterpillars-and-canker-wbrms00318nas a2200121 4500008004100000245002100041210002100062300000800083490000700091653001200098100001700110856006900127 1900 eng d00aTulip Tree Scale0 aTulip Tree Scale a7220 v6510abiology1 aFelt, E., P. uhttps://www.nysm.nysed.gov/staff-publications/tulip-tree-scale-100321nas a2200121 4500008004100000245002200041210002200063300000800085490000700093653001200100100001700112856007000129 1899 eng d00aTent Caterpillars0 aTent Caterpillars a4700 v6410abiology1 aFelt, E., P. uhttps://www.nysm.nysed.gov/staff-publications/tent-caterpillars-000301nas a2200121 4500008004100000245001600041210001600057300000800073490000700081653001200088100001700100856006200117 1899 eng d00aTurnip Pest0 aTurnip Pest a6460 v6410abiology1 aFelt, E., P. uhttps://www.nysm.nysed.gov/staff-publications/turnip-pest00325nas a2200121 4500008004100000245002500041210002500066300000800091490000700099653001200106100001700118856006800135 1898 eng d00aTo Destroy Ant Hills0 aTo Destroy Ant Hills a4460 v6310abiology1 aFelt, E., P. uhttps://www.nysm.nysed.gov/staff-publications/destroy-ant-hills00313nas a2200121 4500008004100000245002000041210002000061300000800081490000700089653001200096100001700108856006600125 1898 eng d00aTwo Bad Insects0 aTwo Bad Insects a2060 v6310abiology1 aFelt, E., P. uhttps://www.nysm.nysed.gov/staff-publications/two-bad-insects00321nas a2200121 4500008004100000245002100041210002100062300000800083490000700091653001200098100002000110856006900130 1897 eng d00aTent Caterpillar0 aTent Caterpillar a3900 v6210abiology1 aLintner, J., A. uhttps://www.nysm.nysed.gov/staff-publications/tent-caterpillar-000309nas a2200121 4500008004100000245001700041210001700058300000800075490000700083653001200090100002000102856006500122 1897 eng d00aTussock Moth0 aTussock Moth a6860 v6210abiology1 aLintner, J., A. uhttps://www.nysm.nysed.gov/staff-publications/tussock-moth-000304nas a2200121 4500008004100000245001600041210001600057300000800073490000700081653001200088100002000100856006200120 1897 eng d00aTwo Insects0 aTwo Insects a1060 v6210abiology1 aLintner, J., A. uhttps://www.nysm.nysed.gov/staff-publications/two-insects00321nas a2200121 4500008004100000245002100041210002100062300000800083490000700091653001200098100002000110856006900130 1896 eng d00aTent Caterpillar0 aTent Caterpillar a5710 v6110abiology1 aLintner, J., A. uhttps://www.nysm.nysed.gov/staff-publications/tent-caterpillar-100403nas a2200121 4500008004100000245004800041210004800089300001200137490000600149653001200155100002000167856009400187 1896 eng d00aThousand Legged Worms Infesting Greenhouses0 aThousand Legged Worms Infesting Greenhouses a251-2520 v410abiology1 aLintner, J., A. uhttps://www.nysm.nysed.gov/staff-publications/thousand-legged-worms-infesting-greenhouses00346nas a2200121 4500008004100000245003400041210003400075300000700109490000600116653001200122100002000134856007000154 1895 eng d00aTo Kill Red Ants in the House0 aTo Kill Red Ants in the House a120 v410abiology1 aLintner, J., A. uhttps://www.nysm.nysed.gov/staff-publications/kill-red-ants-house00340nas a2200121 4500008004100000245002800041210002800069300000800097490000700105653001200112100002000124856007400144 1893 eng d00aThree Lined Leaf Beetle0 aThree Lined Leaf Beetle a5240 v5810abiology1 aLintner, J., A. uhttps://www.nysm.nysed.gov/staff-publications/three-lined-leaf-beetle00333nas a2200121 4500008004100000245002300041210002300064300001200087490000700099653001700106100001900123856006900142 1892 eng d00aTerataspis grandis0 aTerataspis grandis a111-1140 v4410apaleontology1 aClarke, J., M. uhttps://www.nysm.nysed.gov/staff-publications/terataspis-grandis00321nas a2200121 4500008004100000245002100041210002100062300000800083490000700091653001200098100002000110856006900130 1892 eng d00aTent Caterpillar0 aTent Caterpillar a7670 v5710abiology1 aLintner, J., A. uhttps://www.nysm.nysed.gov/staff-publications/tent-caterpillar-200340nas a2200121 4500008004100000245002900041210002900070300000800099490000700107653001200114100002000126856007200146 1892 eng d00aThrips Attack on Cabbage0 aThrips Attack on Cabbage a8090 v5710abiology1 aLintner, J., A. uhttps://www.nysm.nysed.gov/staff-publications/thrips-attack-cabbage00349nas a2200121 4500008004100000245003100041210003100072300000800103490000700111653001200118100002000130856007700150 1892 eng d00aTischeria Apple Leaf Miner0 aTischeria Apple Leaf Miner a8090 v5710abiology1 aLintner, J., A. uhttps://www.nysm.nysed.gov/staff-publications/tischeria-apple-leaf-miner00334nas a2200121 4500008004100000245002600041210002600067300000800093490000700101653001200108100002000120856007200140 1888 eng d00aThousand Legged Worms0 aThousand Legged Worms a7250 v5310abiology1 aLintner, J., A. uhttps://www.nysm.nysed.gov/staff-publications/thousand-legged-worms00321nas a2200121 4500008004100000245002300041210002300064300000800087490000600095653001200101100002000113856006600133 1888 eng d00aTo Kill Plant Lice0 aTo Kill Plant Lice a1580 v910abiology1 aLintner, J., A. uhttps://www.nysm.nysed.gov/staff-publications/kill-plant-lice00355nas a2200121 4500008004100000245003400041210003400075300000800109490000700117653001200124100002000136856007700156 1887 eng d00aThrips in Strawberry Blossoms0 aThrips in Strawberry Blossoms a4590 v5210abiology1 aLintner, J., A. uhttps://www.nysm.nysed.gov/staff-publications/thrips-strawberry-blossoms00337nas a2200121 4500008004100000245002700041210002700068300000800095490000700103653001200110100002000122856007300142 1887 eng d00aTwo Marked Tree Hopper0 aTwo Marked Tree Hopper a7830 v5210abiology1 aLintner, J., A. uhttps://www.nysm.nysed.gov/staff-publications/two-marked-tree-hopper00454nas a2200121 4500008004100000245006900041210006700110300000800177490000700185653001200192100002000204856010800224 1883 eng d00aThousand Legged Worms in a Nursery - Julus caerulieocinctus Wood0 aThousand Legged Worms in a Nursery Julus caerulieocinctus Wood a4210 v4810abiology1 aLintner, J., A. uhttps://www.nysm.nysed.gov/staff-publications/thousand-legged-worms-nursery-julus-caerulieocinctus-wood00338nas a2200121 4500008004100000245002900041210002900070300001000099490000600109653001200115100001700127856007200144 1881 eng d00aTwo New Species of Fungi0 aTwo New Species of Fungi a49-510 v810abiology1 aPeck, C., H. uhttps://www.nysm.nysed.gov/staff-publications/two-new-species-fungi00382nas a2200121 4500008004100000245004200041210004200083300001200125490000600137653001200143100002000155856008500175 1880 eng d00aTallow to Preserve Insect Collections0 aTallow to Preserve Insect Collections a145-1460 v310abiology1 aLintner, J., A. uhttps://www.nysm.nysed.gov/staff-publications/tallow-preserve-insect-collections00316nas a2200121 4500008004100000245002000041210002000061300000800081490000700089653001200096100002000108856006600128 1879 eng d00aTwo Carpet Bugs0 aTwo Carpet Bugs a5030 v4410abiology1 aLintner, J., A. uhttps://www.nysm.nysed.gov/staff-publications/two-carpet-bugs00351nas a2200121 4500008004100000245003400041210003400075300000800109490000700117653001200124100002000136856007300156 1879 eng d00aTwo Pests of the Clover Plant0 aTwo Pests of the Clover Plant a6310 v4410abiology1 aLintner, J., A. uhttps://www.nysm.nysed.gov/staff-publications/two-pests-clover-plant00331nas a2200121 4500008004100000245002500041210002500066300000800091490000700099653001200106100002000118856007100138 1879 eng d00aTwo Spotted Lady Bug0 aTwo Spotted Lady Bug a4070 v4410abiology1 aLintner, J., A. uhttps://www.nysm.nysed.gov/staff-publications/two-spotted-lady-bug00325nas a2200121 4500008004100000245002300041210002300064300000800087490000700095653001200102100002000114856006900134 1878 eng d00aTurnip Flea Beetle0 aTurnip Flea Beetle a5830 v4310abiology1 aLintner, J., A. uhttps://www.nysm.nysed.gov/staff-publications/turnip-flea-beetle00304nas a2200121 4500008004100000245001600041210001600057300000800073490000700081653001200088100002000100856006200120 1878 eng d00aTwo Beetles0 aTwo Beetles a3440 v4310abiology1 aLintner, J., A. uhttps://www.nysm.nysed.gov/staff-publications/two-beetles00307nas a2200121 4500008004100000245001700041210001700058300000800075490000700083653001200090100002000102856006300122 1877 eng d00aTree Hoppers0 aTree Hoppers a4630 v4210abiology1 aLintner, J., A. uhttps://www.nysm.nysed.gov/staff-publications/tree-hoppers00305nas a2200121 4500008004100000245001800041210001800059300000700077490000600084653001200090100001700102856006400119 1876 eng d00aTwo New Fungi0 aTwo New Fungi a770 v610abiology1 aPeck, C., H. uhttps://www.nysm.nysed.gov/staff-publications/two-new-fungi00342nas a2200121 4500008004100000245002800041210002800069300000800097490000700105653001200112100002000124856007600144 1874 eng d00aThree Lined Leaf Beetle0 aThree Lined Leaf Beetle a4710 v3910abiology1 aLintner, J., A. uhttps://www.nysm.nysed.gov/staff-publications/three-lined-leaf-beetle-000312nas a2200121 4500008004100000245002000041210001800061300000800079490000700087653001200094100002000106856006400126 1874 eng d00aA Timothy Eater0 aTimothy Eater a4710 v3910abiology1 aLintner, J., A. uhttps://www.nysm.nysed.gov/staff-publications/timothy-eater00470nas a2200121 4500008004100000245008800041210006900129300001200198490000700210653001200217100001400229856010500243 1871 eng d00aThirteenth Report on Noxious, Beneficial and Other Insects of the State of New York0 aThirteenth Report on Noxious Beneficial and Other Insects of the a495-5660 v2910abiology1 aFitch, A. uhttps://www.nysm.nysed.gov/staff-publications/thirteenth-report-noxious-beneficial-and-other-insects00467nas a2200121 4500008004100000245008500041210006900126300001200195490000700207653001200214100001400226856010500240 1868 eng d00aTwelfth Report on Noxious, Beneficial and Other Insects of the State of New York0 aTwelfth Report on Noxious Beneficial and Other Insects of the St a889-9320 v2710abiology1 aFitch, A. uhttps://www.nysm.nysed.gov/staff-publications/twelfth-report-noxious-beneficial-and-other-insects-st00465nas a2200121 4500008004100000245008300041210006900124300001200193490000700205653001200212100001400224856010500238 1865 eng d00aTenth Report on Noxious, Beneficial and Other Insects of the State of New York0 aTenth Report on Noxious Beneficial and Other Insects of the Stat a433-4610 v2410abiology1 aFitch, A. uhttps://www.nysm.nysed.gov/staff-publications/tenth-report-noxious-beneficial-and-other-insects-stat00414nas a2200121 4500008004100000245006300041210005600104300000700160490000700167653001200174100001400186856009200200 1859 eng d00aThe Thousand-Legged Worm. Answer to the Above by Dr. Fitch0 aThousandLegged Worm Answer to the Above by Dr Fitch a270 v1410abiology1 aFitch, A. uhttps://www.nysm.nysed.gov/staff-publications/thousandlegged-worm-answer-above-dr-fitch00407nas a2200121 4500008004100000245005500041210005500096300001000151490000700161653001700168100001300185856008700198 1859 eng d00aTrilobites of the Shales of the Hudson River Group0 aTrilobites of the Shales of the Hudson River Group a59-620 v1210apaleontology1 aHall, J. uhttps://www.nysm.nysed.gov/staff-publications/trilobites-shales-hudson-river-group00465nas a2200121 4500008004100000245008300041210006900124300001200193490000700205653001200212100001400224856010500238 1857 eng d00aThird Report on Noxious, Beneficial and Other Insects of the State of New York0 aThird Report on Noxious Beneficial and Other Insects of the Stat a315-4900 v1610abiology1 aFitch, A. uhttps://www.nysm.nysed.gov/staff-publications/third-report-noxious-beneficial-and-other-insects-stat00465nas a2200121 4500008004100000245008000041210006900121300001200190490000600202653002500208100001300233856009700246 1850 eng d00aOn the Trails and Tracks in the Sandstones of the Clinton Group of New York0 aTrails and Tracks in the Sandstones of the Clinton Group of New  a256-2600 v210ageology paleontology1 aHall, J. uhttps://www.nysm.nysed.gov/staff-publications/trails-and-tracks-sandstones-clinton-group-new00456nas a2200121 4500008004100000245008500041210006900126300001000195490000600205653001700211100001900228856008700247 1849 eng d00aTo the Honorable the Board of Regents of the University of the State of New-York0 aTo the Honorable the Board of Regents of the University of the S a84-910 v210aanthropology1 aMorgan, L., H. uhttps://www.nysm.nysed.gov/staff-publications/honorable-board-regents-university-s00304nas a2200121 4500008004100000245001800041210001800059300001000077490000600087653001200093100001300105856006400118 1844 eng d00aTrenton Falls0 aTrenton Falls a33-360 v410ageology1 aHall, J. uhttps://www.nysm.nysed.gov/staff-publications/trenton-falls00459nas a2200121 4500008004100000245008300041210006900124300001200193490000600205653001200211100001300223856010100236 1839 eng d00aThird Annual Report of the Fourth Geological District of the State of New York0 aThird Annual Report of the Fourth Geological District of the Sta a287-3390 v310ageology1 aHall, J. uhttps://www.nysm.nysed.gov/staff-publications/third-annual-report-fourth-geological-district-sta