03023nas a2200301 4500008004100000022001400041245008800055210006900143300001600212490000700228520209900235100001802334700002302352700002102375700001902396700002302415700001702438700002402455700002402479700001902503700001802522700002502540700002302565700001802588700002702606700002002633856006802653 2023 eng d a0730-726800aReview and Development of Best Practices for Toxicity Tests with Dreissenid Mussels0 aReview and Development of Best Practices for Toxicity Tests with a1649 - 16660 v423 a

Since their introduction to North America in the 1980s, research to develop effective control tools for invasive mussels (Dreissena polymorpha and D. rostriformis bugensis) has been ongoing across various research institutions using a range of testing methods. Inconsistencies in experimental methods and reporting present challenges for comparing data, repeating experiments, and applying results. The Invasive Mussel Collaborative established the Toxicity Testing Work Group (TTWG) in 2019 to identify “best practices” and guide development of a standard framework for dreissenid mussel toxicity testing protocols. We reviewed the literature related to laboratory-based dreissenid mussel toxicity tests and determined the degree to which standard guidelines have been used and their applicability to dreissenid mussel testing. We extracted detailed methodology from 99 studies from the peer-reviewed and gray literature and conducted a separate analysis for studies using presettlement and postsettlement mussels. We identified specific components of methods and approaches that could be refined or standardized for dreissenid mussels. These components included species identification, collection methods, size/age class distinction, maintenance practices, testing criteria, sample size, response measures, reporting parameters, exposure methods, and mortality criteria. We consulted experts in the field of aquatic toxicology and dreissenid mussel biology on our proposed. The final recommendations contained in the present review are based on published standard guidelines, methods reported in the published and gray literature, and the expertise of TTWG members and an external panel. In addition, our review identifies research needs for dreissenid mussel testing including improved methods for early–life stage testing, comparative data on life stages and between dreissenid mussel species, inclusion of a reference toxicant, and additional testing of nontarget species (i.e., other aquatic organisms).

1 aWaller, Diane1 aPucherelli, Sherri1 aBarbour, Matthew1 aTank, Samantha1 aMeulemans, Matthew1 aWise, Jeremy1 aDahlberg, Angelique1 aAldridge, David, C.1 aClaudi, Renata1 aCope, Gregory1 aGillis, Patricia, L.1 aKashian, Donna, R.1 aMayer, D., A.1 aStockton‐Fiti, Kelly1 aWong, Wai, Hing uhttps://setac.onlinelibrary.wiley.com/doi/full/10.1002/etc.564801537nas a2200205 4500008004100000245015200041210006900193260005400262520080100316100001801117700001901135700002201154700001801176700002101194700002201215700001701237700001201254700001501266856005001281 2023 eng d00aImplementation plan of the National Cooperative Geologic Mapping Program strategy—Northeast region of the United States: New York and New England0 aImplementation plan of the National Cooperative Geologic Mapping aReston, VirginiabUnited States Geological Survey3 a
1 aWalsh, G., J.1 aThomas, M., A.1 aMarvinney, R., G.1 aMabee, S., B.1 aChormann, F., H.1 aKozlowski, A., L.1 aGale, M., H.1 aKim, J.1 aSavage, B. uhttps://pubs.usgs.gov/publication/ofr2023105901643nas a2200145 4500008004100000022001400041245007800055210006900133300000800202490000800210520113100218100001701349700001901366856011201385 2023 eng d a1046-236800aIntroduction: Exploring African American Contexts in New York Archaeology0 aIntroduction Exploring African American Contexts in New York Arc a1-30 v1373 a

Archaeology, at its best, renders communities that are under-represented in traditional historical narratives discernible. Such communities in New York include those of enslaved, formerly enslaved, and free African American people. The Introduction to this NYSAA Bulletin explores the two research themes pursued by five of the authors who presented papers at the October 1, 2022, NYAC Fall Symposium entitled “Exploring African American Contexts in New York Archaeology.” Weed and Merwin summarize the papers while focusing on the research themes of site types and culturally-defined objects that were pursued by the presenters. Weed and Merwin concluded that the papers in the volume, along with others presented at the October 2022 NYAC meeting, represent a significant contribution to our understanding of African American archaeological sites in New York State, especially those outside of urban centers.

1 aWeed, C., S.1 aMerwin, D., E. uhttps://www.nysm.nysed.gov/staff-publications/introduction-exploring-african-american-contexts-new-york-arc01662nas a2200181 4500008004100000245011900041210006900160260001600229300001000245490000700255520106600262100001801328700001801346700002101364700002001385700002001405856005501425 2022 eng d00aPhylogenomic analysis of the bowfin (Amia calva) reveals unrecognized species diversity in a living fossil lineage0 aPhylogenomic analysis of the bowfin Amia calva reveals unrecogni cJan-12-2022 a165140 v123 a

The Bowfin (Amia calva), as currently recognized, represents the sole living member of the family Amiidae, which dates back to approximately 150 Ma. Prior to 1896, 13 species of extant Bowfins had been described, but these were all placed into a single species with no rationale or analysis given. This situation has persisted until the present day, with little attention given to re-evaluation of those previously described nominal forms. Here, we present a phylogenomic analysis based on over 21,000 single nucleotide polymorphisms (SNPs) from 94 individuals that unambiguously demonstrates the presence of at least two independent evolutionary lineages within extant Amia populations that merit species-level standing, as well as the possibility of two more. These findings not only expand the recognizable species diversity in an iconic, ancient lineage, but also demonstrate the utility of such methods in addressing previously intractable questions of molecular systematics and phylogeography in slowly evolving groups of ancient fishes.

1 aWright, J., J1 aBruce, S., A.1 aSinopoli, D, .A.1 aPalumbo, J., R.1 aStewart, D., J. uhttps://www.nature.com/articles/s41598-022-20875-401502nas a2200121 4500008004100000022001300041245010300054210006900157260001600226520105200242100001901294856006701313 2020 eng d a1040618200aBald eagles and the Thunderbird myth: Birds in pre-contact ceremonialism on Martha's Vineyard, USA0 aBald eagles and the Thunderbird myth Birds in precontact ceremon cJan-03-20203 aCeremonialism is an integral part of human life but difficult to recover from archaeological remains. Among Native groups in Eastern North America, skins and feathers of birds were commonly used as part of ritual feast ceremonies, including those of the Thunderbird, a mythological creature associated with thunder, lightning, and the upper world. Physical evidence for the Thunderbird has been limited to ceramic, lithic, copper, and petroglyphic artifacts, but the recent discovery of a series of Bald eagle (Haliaeetus leucocephalus) wing bones from the Frisby Butler site may present the first faunal evidence for the myth in Native North America. Patterns of skeletal part representation within the assemblage and across the site suggest that the deposit is the remains of a ritual feast and the presence of multiple wings indicates intentional curation of eagles. If so, this is the earliest known Thunderbird association on the island of Martha's Vineyard, showing the spread of extant Algonquin cosmology to this area by at least 2,000 BP.1 aWatson, J., E. uhttps://linkinghub.elsevier.com/retrieve/pii/S104061822030102601766nas a2200133 4500008004100000022001400041245012600055210006900181260001600250300001100266520124300277100001901520856009301539 2020 eng d a0033-822200aAn Updated History of Pre-Contact New England: New AMS Dates for the Hornblower II and Frisby-Butler Archaeological Sites0 aUpdated History of PreContact New England New AMS Dates for the  cMar-04-2020 a1 - 153 a

Faunal assemblages from the pre-Contact period sites Frisby-Butler and Hornblower II on Marthaʼs Vineyard, Massachusetts, USA, remain unstudied since excavation during the 1980s. This project establishes radiocarbon (14C) dates from faunal remains and evaluates occupation and abandonment at each site. 14C measurements were collected from 17 specimens and 13 dates from previous analyses were re-examined. Dates were identified from the archaeological time periods Transitional Archaic (2700–3700 BP), Early Woodland (2000–2700 BP), and Late Woodland (450–1200 BP) at Frisby-Butler. Occupation likely represented seasonal visitations during autumn and winter to hunt based on white-tailed deer (Odocoileus virginianus) demographic profiles. A combined dataset of new and re-calibrated 14C measurements from Hornblower II date to the Late Archaic (3700–6000 BP), Early Woodland, Middle Woodland (1200–2000 BP), and Late Woodland periods. Settlement was focused on gathering warm-weather foods like demersal fish and lakebirds. Together, the sites demonstrate periodic seasonal use of the southwest coast of the island throughout the Late Holocene and fit within an established regional pattern in southern New England.

1 aWatson, J., E. uhttps://www.cambridge.org/core/product/identifier/S0033822220000193/type/journal_article00390nas 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/77554200508nas a2200145 4500008004100000022001400041245006200055210006100117300001000178490000800188100002500196700001800221700002300239856010000262 2020 eng d a1046-236800aNon-Destructive Archaeological Surveys at the Douw 1 Site0 aNonDestructive Archaeological Surveys at the Douw 1 Site a49-600 v1341 aWinchell-Sweeney, S.1 aO'Connell, K.1 aLucas, Michael, T. uhttps://www.nysm.nysed.gov/staff-publications/nondestructive-archaeological-surveys-douw-1-site01833nas a2200145 4500008004100000022001400041245010700055210006900162300001400231490000700245520132500252100001901577700002601596856006501622 2019 eng d a1047-482X00aA reevaluation of bird taxonomic identifications at Contact‐ and historic‐era North American sites0 areevaluation of bird taxonomic identifications at Contact and hi a822 - 8300 v293 a

Domestic chickens (Gallus domesticus) and turkeys (Meleagris gallopavo) are identified more frequently than other bird species in bone assemblages from historic sites in North America. Recent studies on the effectiveness of metric data for identification of galliform bones found high degrees of similarity in size and morphology between wild game birds (e.g., grouse and ptarmigan) and multiple domestic or introduced species (e.g., chicken and pheasant). This finding suggests that wild taxa and less common domesticates may have been misidentified as chicken and as a result are underrepresented in these historic datasets. In this paper, we evaluate the precision of bird taxonomic identifications from five Contact‐ and historic‐era sites in New York State, comparing the initial taxon designations recorded in site reports with our new identifications derived from a combination of comparative morphological and osteometric analyses. After our analysis of the assemblages, game bird diversity at most of the sites expanded, as did the prevalence of other orders (e.g., Anseriformes and Strigiformes). The updated identifications highlight the diversity of birds used in historic contexts and the importance of combining multiple analytical methods to increase accuracy.
 

1 aWatson, J., E.1 aLedogar, Sarah, Heins uhttps://onlinelibrary.wiley.com/doi/full-xml/10.1002/oa.279901907nas 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/s12520-018-0697-400838nas a2200217 4500008004100000245010400041210006900145260001600214300000700230490000700237653001800244653001500262653001800277653001000295653001200305100002300317700002500340700002000365700002200385856021300407 2019 eng d00aFirst Report of Rice Water Weevil, Lissorhoptrus oryzophilus, in Grain Sorghum in the United States0 aFirst Report of Rice Water Weevil Lissorhoptrus oryzophilus in G cJan-01-2019 a360 v3510aBrachycerinae10aColeoptera10aCurculionidae10agrass10aPoaceae1 aWhitehouse, R., J.1 aThrash, Benjamin, C.1 aLorenz, Gus, M.1 aBateman, Nick, R. uhttps://bioone.org/journals/journal-of-agricultural-and-urban-entomology/volume-35/issue-1/1523-5475-35.1.36/First-Report-of-Rice-Water-Weevil-Lissorhoptrus-oryzophilus-in-Grain/10.3954/1523-5475-35.1.36.full01914nas a2200157 4500008004100000022001400041245013600055210006900191300001300260490000700273520134900280100002501629700001601654700002301670856006301693 2018 eng d a0008-407700aPseudocryptic species of the Middle Cambrian trilobite Eodiscus Hartt, in Walcott, 1884, from Avalonian and Laurentian Newfoundland0 aPseudocryptic species of the Middle Cambrian trilobite Eodiscus  a997-10190 v553 a

Two species of the Middle Cambrian trilobite Eodiscus Hartt, in Walcott, 1884, E. punctatus (Salter, 1864) and E. scanicus (Linnarsson, 1883), have been reported from several paleocontinents. However, in their respective type areas of Avalonian Britain and Baltica (Sweden), both species are poorly documented from moulds preserved in siliciclastic mudstone that are variably compacted and distorted. Moreover, variation in such characters as surface sculpture between putative occurrences suggests that widespread use of these names may mask species differentiation within and between paleocontinents. Detailed examination of Eodiscus sclerites that are exquisitely preserved in full relief in limestone from the Manuels River Formation of Avalonian Newfoundland and the Shallow Bay Formation of Laurentian Newfoundland demonstrates the presence of multiple species that are distinct from both E. punctatus and E. scanicus. We interpret them as a group of pseudocryptic species that are comparable to groups that are now identified routinely among modern invertebrates. New species are E. confossus, E. tuberculus, and E. coloholcus. At the current state of knowledge, E. punctatus and E. scanicus are best restricted to their respective types.

1 aWestrop, Stephen, R.1 aLanding, E.1 aDengler, Alyce, A. uhttp://www.nrcresearchpress.com/doi/10.1139/cjes-2018-002700665nas a2200181 4500008004100000020001800041024002000059245013100079210006900210260005600279300001200335100002000347700002000367700001700387700002100404700001700425856004100442 2018 eng d a9781421425566 aLCCN 201703940100aAnalyzing the Tooth Development of Sabertooth Carnivores: Implications Regarding the Ecology and Evolution of Smilodon fatalis0 aAnalyzing the Tooth Development of Sabertooth Carnivores Implica aBaltimore, MarylandbJohns Hopkins University Press a139-1521 aWysocki, M., A.1 aFeranec, R., S.1 aWerdelin, L.1 aMcDonald, H., G.1 aShaw, C., A. uhttps://muse.jhu.edu/chapter/210517802755nas a2200217 4500008004100000022001400041245019900055210006900254260001200323300001400335490000800349520200400357653001402361653002002375653001302395653001402408653001602422100001802438700001602456856006502472 2017 eng d a0016-756800aThe agnostoid arthropod Lotagnostus Whitehouse, 1936 (late Cambrian; Furongian) from Avalonian Cape Breton Island (Nova Scotia, Canada) and its significance for international correlationAbstract0 aagnostoid arthropod Lotagnostus Whitehouse 1936 late Cambrian Fu c07/2016 a1001-10210 v1543 a

New and archival collections from the Chelsey Drive Group of the Avalon terrane of Cape Breton Island, Nova Scotia, Canada, yield late Cambrian trilobites and agnostoid arthropods with full convexity that contrast with compacted, often deformed material from shale and slate typical of Avalonian Britain. Four species of the agnostoid Lotagnostus form a stratigraphic succession in the upper Furongian (Ctenopyge tumidaParabolina lobata zones). Two species, L. ponepunctus (Matthew, 1901) and L. germanus (Matthew, 1901) are previously named; L. salteri and L. matthewi are new. Lotagnostus trisectus (Salter, 1864), the type species of the genus, is restricted to compacted material from its type area in Malvern, England. Lotagnostus americanus (Billings, 1860) has been proposed as a globally appropriate index for the base of ‘Stage 10’ of the Cambrian. All four species from Avalonian Canada are differentiated clearly from L. americanus in its type area in Laurentian North America (i.e., from debris flow blocks in Taconian Quebec). In our view, putative occurrences of L. americanus from other Cambrian continents record very different species. Lotagnostus americanus cannot be recognized worldwide, and other taxa should be sought to define the base of Stage 10, such as the conodont Eoconodontus notchhpeakensis.

10aAgnostida10aBiostratigraphy10aCambrian10aFurongian10aLotagnostus1 aWestrop, S.R.1 aLanding, E. uhttp://www.journals.cambridge.org/abstract_S001675681600057101553nas a2200133 4500008004100000245009700041210006900138260001700207300001400224490000700238520111300245100001801358856004301376 2017 eng d00aA new diminutive genus and species of catfish from Lake Tanganyika (Siluriformes: Clariidae)0 anew diminutive genus and species of catfish from Lake Tanganyika c26 July 2017 a789–8050 v913 a

The examination of material representing one of Lake Tanganyika's six previously recognized endemic catfish lineages, has revealed the presence of an additional genus of clariid, described here as Pseudotanganikallabes new genus. This genus is represented by a single species, Pseudotanganikallabes prognatha sp. nov., which is distinguished from all other clariids by its lack of an infraorbital series, the presence of multiple osseous connections between the swim bladder capsules and elements of the neurocranium, the absence of an ethmoid notch, the presence of a very large, egg-shaped occipital fontanelle and the extension of the lower lip beyond the margin of the upper jaw. A combination of additional external and molecular characters serves to further distinguish this taxon from all currently recognized clariid species. Phylogenetic analysis of mitochondrial (cytb) and nuclear (18S-ITS1-5.8S-ITS2-28S) sequence data supports the creation of a new genus for this species, as it appears to represent an independent, monophyletic lineage within the family Clariidae.

1 aWright, J., J uhttp://doi.wiley.com/10.1111/jfb.1337402564nas a2200133 4500008004100000245017800041210006900219300001200288490000700300520197900307100001602286700001602302856011202318 2016 eng d00aGeological context, biostratigraphy and systematic revision of late early Cambrian olenelloid trilobites from the Parker and Monkton formations, northwestern Vermont, U.S.A.0 aGeological context biostratigraphy and systematic revision of la a193-2400 v493 a

In northwestern Vermont, upper lower Cambrian (Dyeran Stage) dysoxic deposits of the Franklin Basin are separated by 7 km from coeval, shallow-shelf deposits of the Monkton Formation on the Middlebury platform. This report presents a systematic revision of olenelloid trilobites from three localities within the basinal facies of the Parker Formation (including the Parker quarry Lagerstätte) and three localities within the Monkton Formation. The study reveals a previously underestimated diversity of olenelloid species in both formations. Olenellus agellus, O. crassimarginatus, O. transitans and O. aff. transitans are presently known only from the basinal facies; Bolbolenellus hermani, B. cf. brevispinus and several indeterminate olenelloid species are presently known only from the shelf facies; and O. thompsoni, O. aff. fowleri and Mesonacis vermontanus occur in both facies. The revisions demonstrate that (1) the Parker and Monkton formations share several species, thus strengthening previous claims for at least partial age-equivalence of the units; and (2) the regression(s) represented by the Monkton Formation began after the formation of the Franklin Basin but prior to the deposition of the Parker quarry Lagerstätte. Some newly documented elements of the Parker and Monkton formation faunas are possibly conspecific with olenelloids from Nevada, which permits a provisional correlation of the Parker quarry Lagerstätte with the Bolbolenellus euryparia Zone or overlying uppermost Dyeran Nephrolenellus multinodus Zone of the Laurentian Cordilleran margin. The Monkton Formation regression(s) were broadly contemporaneous with one or more of the four late Dyeran shallowing-up events that have been identified in the southwestern United States. This indicates that the regression(s) were a eustastic rather than an epeirogenically controlled phenomenon.

1 aWebster, M.1 aLanding, E. uhttps://www.nysm.nysed.gov/staff-publications/geological-context-biostratigraphy-and-systematic-revision-la01334nas a2200145 4500008004100000245010100041210006900142300001200211490000700223520084200230100001801072700002001090700002301110856005501133 2016 eng d00aNew and Previously Overlooked Records of Several Fish Species from the Marine Waters of New York0 aNew and Previously Overlooked Records of Several Fish Species fr a118-1330 v233 a

The marine fish fauna of New York represents a highly diverse species assemblage, compose of both migratory and resident taxa that utilize a wide variety of habitats. Recently the New York State Museum took position of Dr. Howard Riesman's personal ichthyology collection, which included many specimens from Shinnecock Bay, Long Island. Examinations of these specimens has provided evidence to suggest that an additional 4 species should be added to previously compiled lists of marine species known to occur in the vicinity of New York. The prior lack of recognition of the presence of these species in Shinnecock Bay is apparently attributable to a number of factors, including historical taxonomic confusion, actual range expansion, aquarium releases, and simple lack of historical documentation of rare or transient species.

1 aWright, J., J1 aSchmidt, R., E.1 aWeatherwax, B., R. uhttp://www.bioone.org/doi/abs/10.1656/045.023.011603747nas a2200169 4500008004100000245014900041210006900190260005300259520310900312653001203421100001803433700001803451700001803469700001903487700001903506856005203525 2015 eng d00aExposure-related Effects of Pseudomonas fluorescens (Pf-CL145A) on Juvenile Unionid Mussels: U.S. Geological Survey Open-File Report 2015–10660 aExposurerelated Effects of Pseudomonas fluorescens PfCL145A on J aWashington, D.CbUnited States Geological Survey3 a

The exposure-related effects of a commercially prepared spray-dried powder (SDP) or freeze-dried powder (FDP) formulation of Pseudomonas fluorescens (strain CL145A) on the survival of seven species of newly metamorphosed (<72 hours old) freshwater unionid mussels was evaluated. Forty unionid mussels of each species were randomly distributed to test chambers and each species independently exposed for 24 hours to a static dose of either SDP (four species: Lampsilis cardium, Lampsilis siliquoidea, Lampsilis higginsii, andLigumia recta) or FDP (three species: Obovaria olivaria, Actinonaias ligamentina, andMegalonaias nervosa).

Each test chamber was assigned to one of six treatment groups (n = four chambers per group) by using a randomized block design. The six treatment groups included (1) an untreated control group, (2) groups that received applications with nominal target active ingredient (AI) concentrations of 50, 100, 200, and 300 milligrams per liter (mg/L), and (3) a group that received an application with a nominal target AI concentration of 300 mg/L of heat-deactivated test article (300 HD). After a 24-hour exposure period, water inflow to the test chambers was restored, and the unionid mussels were maintained for an additional 7 days before they were assessed for survival.

Mean survival of four unionid mussels species exposed to SDP varied among species and treatment groups when compared to the untreated control groups. The results indicate that exposure to SDP-formulated P. fluorescens up to the maximum label concentration (100 mg/L AI) and up to three times the maximum label exposure duration (8 hours) is not likely to affect the survival of L. siliquoidea and L. higginsii. Low mean survival in the L. recta control group (25.0 percent) indicates that results for L. recta should be interpreted with caution. Mean survival of the L. cardium was significantly lower in all treated groups (14.4 to 40.6 percent) compared to the control group (68.8 percent). These results indicate that further investigation on the impact of SDP-formulated P. fluorescens on L. recta and L. cardium is warranted.

Mean survival of three unionid mussels species exposed to FDP was not significantly different in the 50-, 100-, and 200-mg/L AI treatment groups and the 300 mg/L heat-deactivated treatment groups when compared to the control groups. Mean survival of O. olivaria and M. nervosa was significantly lower in the 300-mg/L AI treated groups (38.1 and 48.1 percent, respectively) compared to the control groups (71.9 and 88.1 percent, respectively). The results indicate that exposure to FDP-formulated P. fluorescens up to the maximum label concentration (100 mg/L AI) and up to three times the maximum label exposure duration (8 hours) is not likely to affect the survival of O. olivaria, A. ligamentina, and M. nervosa.

10abiology1 aWeber, K., L.1 aLuoma, J., A.1 aMayer, D., A.1 aAloisi, D., B.1 aEckert, N., L. uhttp://pubs.er.usgs.gov/publication/ofr2015106603706nas a2200169 4500008004100000245014900041210006900190260002000259520311100279653001203390100001803402700001803420700001803438700001903456700001903475856004203494 2015 eng d00aExposure-related Effects of Pseudomonas fluorescens (Pf-CL145A) on Juvenile Unionid Mussels: U.S. Geological Survey Open-File Report 2015–10660 aExposurerelated Effects of Pseudomonas fluorescens PfCL145A on J aWashington, D.C3 a

The exposure-related effects of a commercially prepared spray-dried powder (SDP) or freeze-dried powder (FDP) formulation of Pseudomonas fluorescens (strain CL145A) on the survival of seven species of newly metamorphosed (<72 hours old) freshwater unionid mussels was evaluated. Forty unionid mussels of each species were randomly distributed to test chambers and each species independently exposed for 24 hours to a static dose of either SDP (four species: Lampsilis cardium, Lampsilis siliquoidea, Lampsilis higginsii, and Ligumia recta) or FDP (three species: Obovaria olivaria, Actinonaias ligamentina, and Megalonaias nervosa).

Each test chamber was assigned to one of six treatment groups (n = four chambers per group) by using a randomized block design. The six treatment groups included (1) an untreated control group, (2) groups that received applications with nominal target active ingredient (AI) concentrations of 50, 100, 200, and 300 milligrams per liter (mg/L), and (3) a group that received an application with a nominal target AI concentration of 300 mg/L of heat-deactivated test article (300 HD). After a 24-hour exposure period, water inflow to the test chambers was restored, and the unionid mussels were maintained for an additional 7 days before they were assessed for survival.

Mean survival of four unionid mussels species exposed to SDP varied among species and treatment groups when compared to the untreated control groups. The results indicate that exposure to SDP-formulated P. fluorescens up to the maximum label concentration (100 mg/L AI) and up to three times the maximum label exposure duration (8 hours) is not likely to affect the survival of L. siliquoidea and L. higginsii. Low mean survival in the L. recta control group (25.0 percent) indicates that results for L. recta should be interpreted with caution. Mean survival of the L. cardium was significantly lower in all treated groups (14.4 to 40.6 percent) compared to the control group (68.8 percent). These results indicate that further investigation on the impact of SDP-formulated P. fluorescens on L. recta and L. cardium is warranted.

Mean survival of three unionid mussels species exposed to FDP was not significantly different in the 50-, 100-, and 200-mg/L AI treatment groups and the 300 mg/L heat-deactivated treatment groups when compared to the control groups. Mean survival of O. olivaria and M. nervosa was significantly lower in the 300-mg/L AI treated groups (38.1 and 48.1 percent, respectively) compared to the control groups (71.9 and 88.1 percent, respectively). The results indicate that exposure to FDP-formulated P. fluorescens up to the maximum label concentration (100 mg/L AI) and up to three times the maximum label exposure duration (8 hours) is not likely to affect the survival of O. olivaria, A. ligamentina, and M. nervosa.

10abiology1 aWeber, K., L.1 aLuoma, J., A.1 aMayer, D., A.1 aAloisi, D., B.1 aEckert, N., L. uhttp://dx.doi.org/10.3133/ofr2015106602323nas a2200217 4500008004100000022002200041245006100063210006100124260001300185300000900198520169200207653001201899653001601911653001201927653001401939653001301953100001801966700002601984700001702010856007802027 2015 eng d a978-94-007-6727-000aEvolutionary History of Venom Glands in the Siluriformes0 aEvolutionary History of Venom Glands in the Siluriformes bSpringer a1-193 a

The order Siluriformes represents a hyperdiverse group of fishes (>3,000 currently recognized species), which has been known to contain venomous species diversity for over 250 years. In spite of this historical knowledge, scientific examinations of the basic characteristics and evolutionary history of these species’ venom glands, and their products, have been extremely sparse compared to those of terrestrial venomous organisms, or even venomous fishes in general. Here, the current state of knowledge regarding the venom glands of catfishes and their products is examined in a review of morphological, pharmacological, and chemical studies of these structures. Several hypotheses regarding the evolution of siluriform venom glands are able to be drawn from the information contained in these studies as well as the limited work that has attempted to study the evolution of these structures in detail. These include selective scenarios to explain the secondary losses of venom glands in several catfish species and families, compositional variation in siluriform venom chemistry, and the derivation of venom glands from secretory cells of the epidermis. Future work directly addressing multiple issues of venom production and composition in catfishes is necessary before investigations of the evolution of siluriform venoms and delivery structures can reach the levels of detail and sophistication seen in other venomous groups. These studies will benefit greatly from the advent of genomic, transcriptomic, and proteomic methods, which have seen wide use in examinations of venoms produced by other taxa, but have yet to be widely applied to analyses of piscine venoms.

10aCatfish10aCrinotoxins10aDefense10aEpidermal10aProteins1 aWright, J., J1 aGopalakrishnakone, p.1 aMalhotra, A. uhttp://link.springer.com/referenceworkentry/10.1007/978-94-007-6727-0_9-102403nas a2200157 4500008004100000245015300041210006900194300001300263490000700276520180500283100002002088700002002108700001802128700002202146856007702168 2015 eng d00aUsing a Novel Absolute Ontogenetic Age Determination Technique to Calculate the Timing of Tooth Eruption in the Saber-Toothed Cat, Smilodon fatalis.0 aUsing a Novel Absolute Ontogenetic Age Determination Technique t ae01298470 v103 a

Despite the superb fossil record of the saber-toothed cat, Smilodon fatalis, ontogenetic age determination for this and other ancient species remains a challenge. The present study utilizes a new technique, a combination of data from stable oxygen isotope analyses and micro-computed tomography, to establish the eruption rate for the permanent upper canines in Smilodon fatalis. The results imply an eruption rate of 6.0 millimeters per month, which is similar to a previously published average enamel growth rate of the S. fatalis upper canines (5.8 millimeters per month). Utilizing the upper canine growth rate, the upper canine eruption rate, and a previously published tooth replacement sequence, this study calculates absolute ontogenetic age ranges of tooth development and eruption in S. fatalis. The timing of tooth eruption is compared between S. fatalis and several extant conical-toothed felids, such as the African lion (Panthera leo). Results suggest that the permanent dentition of S. fatalis, except for the upper canines, was fully erupted by 14 to 22 months, and that the upper canines finished erupting at about 34 to 41 months. Based on these developmental age calculations, S. fatalis individuals less than 4 to 7 months of age were not typically preserved at Rancho La Brea. On the whole, S. fatalis appears to have had delayed dental development compared to dental development in similar-sized extant felids. This technique for absolute ontogenetic age determination can be replicated in other ancient species, including non-saber-toothed taxa, as long as the timing of growth initiation and growth rate can be determined for a specific feature, such as a tooth, and that growth period overlaps with the development of the other features under investigation.

1 aWysocki, M., A.1 aFeranec, R., S.1 aTseng, Z., J.1 aBjornsson, C., S. uhttp://journals.plos.org/plosone/article?id=10.1371/journal.pone.012984700703nam a2200181 4500008004100000020002200041050001900063245006500082210006100147260005700208653001400265653001500279653001300294100001500307700001800322700001400340856016700354 2014 eng d a978-1-4384-5348-4 a973.7'447-dc2300aAn Irrepressible Conflict: The Empire State in the Civil War0 aIrrepressible Conflict The Empire State in the Civil War aAlbany, New YorkbState University of New York Press10aCivil War10aexhibition10aNew York1 aWeible, R.1 aLemak, J., A.1 aNoble, A. uhttp://books.google.com/books?id=ra9XoAEACAAJ&dq=An+Irrepressible+Conflict:+The+Empire+State+in+the+Civil+War&hl=en&sa=X&ei=MmdOVKXEO47bsATzvYDIDw&ved=0CB0Q6AEwAA01891nas a2200241 4500008004100000245010200041210006900143260004100212300001200253520114200265653001201407653001701419100001701436700002401453700001901477700001601496700001901512700002401531700001701555700001801572700002101590856003801611 2014 eng d00aIs the Fossil Record of Complex Animal Behaviour a Stratigraphical Analogue for the Anthropocene?0 aFossil Record of Complex Animal Behaviour a Stratigraphical Anal aLondonbGeological Society of London a143-1483 a

The base of the Cambrian System is recognized by a characteristic (marine) trace fossil suite assigned to the Treptichnus pedum Biozone, which signals increasing complexity of animal behaviour and demarcates the Cambrian from the (older) Ediacaran System (Proterozoic Eonathem). Ichnotaxa of the T. pedum Biozone are not the earliest trace fossils, and are preceded in the latest Proterozoic by a progressive increase in the diversity of trace-producing organisms and the communities they comprised, the structural and behavioural complexity of the trace fossils, and even the depth of burrowing in sediments. Parallels can be drawn with the increasing complexity of subsurface structures associated with human cities, which also reflect evolution of an increasingly complex community. Before the nineteenth century, these structures were limited and simple, but beginning with the development of London in the mid-nineteenth century as the world's first megacity, subsurface structures have become increasingly complex, reflecting the technology-driven behaviour of twentieth- and twenty-first-century humans.

10ageology10apaleontology1 aWilliams, M.1 aZalasiewicz, J., A.1 aWaters, C., N.1 aLanding, E.1 aWaters, N., N.1 aZalasiewicz, J., A.1 aWilliams, M.1 aEllis, M., A.1 aSnelling, A., M. uhttp://dx.doi.org/10.1144/SP395.800975nas a2200193 4500008004100000245009900041210006900140300001100209490000800220520038100228653002100609653001600630653001100646653002200657653001700679100001900696700001900715856004700734 2011 eng d00aA New Zanclognatha from Eastern North America and a Preliminary Key to the Larvae of the Genus0 aNew Zanclognatha from Eastern North America and a Preliminary Ke a89-1010 v1493 a

The adult of a widespread but previously undescribed species of Zanclognatha Lederer is described from eastern North America. Images of the mature larva and life history datafor Zanclognatha dentata sp. n. are included, along with a preliminary key to the larvae of ten eastern North American Zanclognatha species.

10adetritus feeding10aHerminiinae10alarvae10aspecies radiation10aZanclognatha1 aWagner, D., L.1 aMcCabe, T., L. uhttp://dx.doi.org/10.3897/zookeys.149.234801250nas a2200181 4500008004100000245010500041210006900146300001000215490000700225520068300232653001900915653001100934653002600945653001800971653001700989100001501006856004701021 2011 eng d00aVisions and Reality: Reconsidering the Creation and Development of Lowell's National Park, 1966-19920 aVisions and Reality Reconsidering the Creation and Development o a67-930 v333 a

For more than four decades, historians, historic preservationists, journalists, and public officials have debated the purpose and appropriateness of a national park in Lowell, Massachusetts. This article, written by the first NPS historian in Lowell, builds on existing literature and interprets the founding and early development of Lowell National Historical Park in the context of changing national politics. It locates the concept for the park in the Great Society, documents the contested debate over the park's founding in the 1970s, and argues that the park developed very differently than planned during the radically changed political environment of the 1980s.

10a1980s politics10aLowell10aNational Park Service10aPatrick Mogan10aPaul Tsongas1 aWeible, R. uhttp://dx.doi.org/10.1525/tph.2011.33.2.6700581nas a2200145 4500008004100000245017900041210006900220300001200289490000700301653002500308100002000333700001900353700001600372856004700388 2011 eng d00aThe Cambrian (Sunwaptan, Furongian) Agnostoid Arthropod Lotagnostus Whitehouse, 1936, in Laurentian and Avalonian North America: Systematics and Biostratigraphic Significance0 aCambrian Sunwaptan Furongian Agnostoid Arthropod Lotagnostus Whi a569-5940 v8610ageology paleontology1 aWestrop, S., R.1 aAdrain, J., M.1 aLanding, E. uhttp://dx.doi.org/10.3140/bull.geosci.125601626nas a2200145 4500008004100000245012400041210006900165300001200234490000700246520109400253653001701347100002001364700001601384856008001400 2011 eng d00aLower Cambrian (Branchian) Eodiscoid Trilobites from the Lower Brigus Formation, Avalon Peninsula, Newfoundland, Canada0 aLower Cambrian Branchian Eodiscoid Trilobites from the Lower Bri a209-2620 v423 a

Eodiscoids form a significant component of the Lower Cambrian (Branchian) trilobite fauna of the St. Mary's and lower Jigging Cove members of the Brigus Formation exposed along Conception and Trinity bays, northern Avalon Peninsula, Newfoundland. Two species of Serrodiscus Richter and Richter, four species of Hebediscus Whitehouse, and rare sclerites of Meniscuchus? pik and Calodiscus Howell are documented; type material of M.? helena (Walcott) is reillustrated. Hebediscus attleborensis (Shaler and Foerste) is restricted to the types, and H. williamsi is new. A parsimony analysis indicates that Serrodiscus is paraphyletic but supports monophyly of Acidiscus Rasetti, Bolboparia Rasetti and Stigmadiscus Rasetti. Above a sparsely fossiliferous interval in the lowest part of the Brigus, three eodiscoid faunas can be identified in the upper St. Mary's and lower Jigging Cove members, in ascending order, the Hebediscus planus, H. williamsi and Calodiscus cf. C. lobatus faunas. The lower two faunas correspond to part of the traditional "Callavia Zone" of previous workers.

10apaleontology1 aWestrop, S., R.1 aLanding, E. uhttp://search.informit.com.au/documentSummary;dn=984617395155287;res=IELHSS00382nas a2200133 4500008004100000245003300041210003300074300000700107490000600114653001700120100001800137700001400155856007900169 2010 eng d00aNot Just Another Pretty Face0 aNot Just Another Pretty Face a160 v510aanthropology1 aWalsh, J., P.1 aLenig, W. uhttps://www.nysm.nysed.gov/staff-publications/not-just-another-pretty-face01799nas a2200253 4500008004100000245010800041210006900149300001100218490000600229520099000235653002001225653002601245653002801271653002201299100001701321700001501338700002101353700002401374700001601398700001801414700001901432700001701451856007701468 2010 eng d00aLarge-range Movements of Neotropical Orchid Bees Observed Via Radio Telemetry (Belorussian translation)0 aLargerange Movements of Neotropical Orchid Bees Observed Via Rad ae107380 v53 a

Neotropical orchid bees (Euglossini) are often cited as classic examples of trapline-foragers with potentially extensive foraging ranges. If long-distance movements are habitual, rare plants in widely scattered locations may benefit from euglossine pollination services. Here we report the first successful use of micro radio telemetry to track the movement of an insect pollinator in a complex and forested environment. Our results indicate that individual male orchid bees (Exaerete frontalis) habitually use large rainforest areas (at least 42–115 ha) on a daily basis. Aerial telemetry located individuals up to 5 km away from their core areas, and bees were often stationary, for variable periods, between flights to successive localities. These data suggest a higher degree of site fidelity than what may be expected in a free living male bee, and has implications for our understanding of biological activity patterns and the evolution of forest pollinators.

10aforaging ranges10amicro radio telemetry10aNeotropical orchid bees10atrapline-foragers1 aWikelski, M.1 aMoxley, J.1 aEaton-Mordas, A.1 aLopez-Uribe, M., M.1 aHolland, R.1 aMoskowitz, D.1 aRoubik, D., W.1 aKays, R., W. uhttp://journals.plos.org/plosone/article?id=10.1371/journal.pone.001073800407nas a2200133 4500008004100000245004200041210004100083300000900124490000600133653001600139653001700155100001700172856008400189 2010 eng d00aNew York's Wildflowers in True Colors0 aNew Yorks Wildflowers in True Colors a8-100 v510aphotography10awild flowers1 aWilliams, C. uhttps://www.nysm.nysed.gov/staff-publications/new-yorks-wildflowers-true-colors02769nas a2200205 4500008004100000245010600041210006900147300001400216490000800230520212700238653001702365653003102382653002302413653001702436100001602453700002002469700001802489700001502507856004102522 2009 eng d00aMitochondrial DNA Analysis Indicates Sea Lampreys Are Indigenous to Lake Ontario: Response to Comment0 aMitochondrial DNA Analysis Indicates Sea Lampreys Are Indigenous a1190-11970 v1383 a
Whether sea lampreys Petromyzon marinus are native to Lake Ontario (and Lake Champlain) has been vigorously argued for more than half a century. In earlier decades, this debate was restricted to subjective consideration of historical records of Lake Ontario fishes versus information on the construction of canals hypothesized to have provided a route for colonization in the 19th century and on post-Pleistocene geologic changes to the drainage that might have allowed a much earlier natural invasion. Later, with the development of molecular genetic tools, another, perhaps more objective mode of analysis became available and these studies of two independent genomes indicated that the sea lamprey was indeed indigenous to Lake Ontario (Waldman et al. 2004; Bryan et al. 2005) and Lake Champlain (Bryan et al. 2005; Waldman et al. 2006). But even DNA analyses are equivocal in the sense that highly unlikely, but nonetheless nonfalsifiable alternative scenarios can be proposed to explain what appear to be one-sided results.
Eshenroder provides a service to this controversy by examining in detail, and thus testing, these recent genetic-based publications for their treatment of alternative hypotheses. We, in kind, use this opportunity to reexamine and extend our own analyses. Unlike Eshenroder's comment, our response leads with the genetic argument because if sea lampreys can be reasonably demonstrated to be native to inland New York, then identification of a possible recent dispersal route becomes less important.
10aLake Ontario10aMitochondrial DNA Analysis10aPetromyzon marinus10asea lampreys1 aWaldman, J.1 aDaniels, R., A.1 aHickerson, M.1 aWirgin, I. uhttp://dx.doi.org/10.1577/T08-035R.100939nas a2200169 4500008004100000245006600041210006300107300001200170490000700182520045200189653001200641653001300653653001600666100001500682700002400697856004800721 2009 eng d00aRoad-Cut Mineral Occurrences of St. Lawrence County, New York0 aRoadCut Mineral Occurrences of St Lawrence County New York a254-2620 v843 a

The Oxbow road cut in St. Lawrence County, New York, has produced an enormous quantity of calcite specimens during the past fifty years. These range in size from thumbnail specimens to large-cabinet specimens and in quality from good to outstanding. Of particular interest to collectors has been the presence of penetration twins of simple rhombohedra, the so-called Rossie-habit twins. The locality remains productive to the present day.

10aCalcite10aNew York10arhombohedra1 aWalter, M.1 aChamberlain, S., C. uhttp://dx.doi.org/10.3200/RMIN.84.3.254-26200371nas a2200121 4500008004100000245004200041210003900083300000700122490000600129653001200135100001700147856008500164 2009 eng d00aBerenice Abbott's 'Changing New York'0 aBerenice Abbotts Changing New York a200 v510ahistory1 aWilliams, C. uhttps://www.nysm.nysed.gov/staff-publications/berenice-abbotts-changing-new-york00510nas a2200133 4500008004100000245009400041210006900135300001000204490000800214653001200222100001900234700001900253856010400272 2008 eng d00aLarva of Abablemma (Noctuidae) with Notes on Algivory and Lichenivory in Macrolepidoptera0 aLarva of Abablemma Noctuidae with Notes on Algivory and Licheniv a40-520 v10110abiology1 aWagner, D., L.1 aMcCabe, T., L. uhttps://www.nysm.nysed.gov/staff-publications/larva-abablemma-noctuidae-notes-algivory-and-licheniv00478nas a2200121 4500008004100000245006200041210005900103300001000162490000700172653001200179100001500191856015000206 2008 eng d00aDefining Public History: Is It Possible? Is It Necessary?0 aDefining Public History Is It Possible Is It Necessary a24-250 v4610ahistory1 aWeible, R. uhttps://www.historians.org/publications-and-directories/perspectives-on-history/march-2008/defining-public-history-is-it-possible-is-it-necessary00690nas a2200121 4500008004100000245017400041210006900215260010500284653002300389100001700412700002600429856011300455 2008 eng d00aCultural Resources Reconnaissance Screening Report for PIN 1248.14.121, Route 149, Martindale Road to Washington County Line, Town of Queensbury, Warren County, New York0 aCultural Resources Reconnaissance Screening Report for PIN 12481 aAlbany, New YorkbNew York State Department of Transportation and the Federal Highway Administration10aCultural Resources1 aWilliams, J.1 aNew York State Museum uhttps://www.nysm.nysed.gov/staff-publications/cultural-resources-reconnaissance-screening-report-pin-12481-000566nas a2200109 4500008004100000245017400041210006900215260002100284653002300305100001700328856011100345 2008 eng d00aCultural Resources Reconnaissance Screening Report for PIN 1248.14.121, Route 149, Martindale Road to Washington County Line, Town of Queensbury, Warren County, New York0 aCultural Resources Reconnaissance Screening Report for PIN 12481 aAlbany, New York10aCultural Resources1 aWilliams, J. uhttps://www.nysm.nysed.gov/staff-publications/cultural-resources-reconnaissance-screening-report-pin-1248100602nas a2200193 4500008004100000245009600041210006900137300001200206490000800218653001200226100001700238700001700255700001500272700001500287700001600302700001800318700001800336856005400354 2007 eng d00aGoing Wild: What a Global Small-animal Tracking System Could do for Experimental Biologists0 aGoing Wild What a Global Smallanimal Tracking System Could do fo a181-1860 v21010abiology1 aWikelski, M.1 aKays, R., W.1 aKasdin, J.1 aThorup, K.1 aSmith, J.A.1 aCochran, W.W.1 aSwenson, G.W. uhttp://jeb.biologists.org/content/210/2/181.short00657nas a2200121 4500008004100000245014200041210006900183260010400252653002300356100001700379700002600396856011300422 2007 eng d00aCultural Resources Screening Survey for PIN 1130.60.121, Route 22 over Kinderhook Creek, Town of Stephentown, Rensselaer County, New York0 aCultural Resources Screening Survey for PIN 113060121 Route 22 o aAlbany, New YorkbNew York State Department of Transporation and the Federal Highway Administration10aCultural Resources1 aWilliams, J.1 aNew York State Museum uhttps://www.nysm.nysed.gov/staff-publications/cultural-resources-screening-survey-pin-113060121-route-22-o-000534nas a2200109 4500008004100000245014200041210006900183260002100252653002300273100001700296856011100313 2007 eng d00aCultural Resources Screening Survey for PIN 1130.60.121, Route 22 over Kinderhook Creek, Town of Stephentown, Rensselaer County, New York0 aCultural Resources Screening Survey for PIN 113060121 Route 22 o aAlbany, New York10aCultural Resources1 aWilliams, J. uhttps://www.nysm.nysed.gov/staff-publications/cultural-resources-screening-survey-pin-113060121-route-22-o00422nas a2200121 4500008004100000245006000041210005900101300000800160490000600168653001200174100001700186856009700203 2006 eng d00aSelling the Store: The Johnson Country Store Collection0 aSelling the Store The Johnson Country Store Collection a8-90 v210ahistory1 aWilliams, C. uhttps://www.nysm.nysed.gov/staff-publications/selling-store-johnson-country-store-collection00329nas a2200121 4500008004100000245002700041210002700068300000700095490000600102653001200108100001700120856007000137 2005 eng d00aHistory in Every Place0 aHistory in Every Place a160 v110ahistory1 aWilliams, C. uhttps://www.nysm.nysed.gov/staff-publications/history-every-place04206nas a2200217 4500008004100000245009700041210006900138300001200207490000700219520346800226653002303694653001703717653002903734653001303763100001703776700001903793700001803812700002003830700001503850856012303865 2004 eng d00aReservoir Characterization of the Mississippian Madison Formation, Wind River Basin, Wyoming0 aReservoir Characterization of the Mississippian Madison Formatio a405-4320 v883 a

Significant heterogeneity in petrophysical properties, including variations in porosity and permeability, are well documented from carbonate systems. These variations in physical properties are typically influenced by original facies heterogeneity, the early diagenetic environment, and later stage diagenetic overprint. The heterogeneities in the Mississippian Madison Formation in the Wind River basin of Wyoming are a complex interplay between these three factors whereby differences from the facies arrangement are first reduced by pervasive dolomitization, but late-stage hydrothermal diagenesis introduces additional heterogeneity.

The dolomitized portions of the Madison Formation form highly productive gas reservoirs at Madden Deep field with typical initial production rates in excess of 50 MMCFGD. In the study area, the Madison Formation is composed of four third-order depositional sequences that contain several small-scale, higher frequency cycles. The cycles and sequences display a facies partitioning with mudstone to wackestone units in the transgressive portion and skeletal and oolitic packstone and grainstone in the regressive portions. The grainstone packages are amalgamated tidally influenced skeletal and oolitic shoals that cover the entire study area. The basal three sequences are completely dolomitized, whereas the fourth sequence is limestone. The distribution of petrophysical properties in the system is influenced only in a limited manner by the smaller scale stratigraphic architecture. Porosity and permeability are controlled by the sequence-scale stratigraphic units, where uniform facies belts and pervasive dolomitization result in flow units that are basically tied to third-order depositional sequences with a thickness of 65ndash100 ft (20ndash30 m).

The best reservoir rocks are found in regressive, coarse-grained dolomites of the lower two sequences. Although the amalgamated shoal facies is heterogeneous, dolomitization decompartmentalized these cycles. Fine-grained sediments in the basal transgressive parts of these sequences, along with caliche and chert layers on top of the underlying sequences, are responsible for a decrease of porosity toward the sequence boundaries and potential flow separation. Good reservoir quality is also found in the third sequence, which is composed of dolomitized carbonate mud. However, reservoir-quality predictions in these dolomudstones are complicated by several phases of brecciation. The most influential of these brecciations is hydrothermal in origin and partly shattered the entire unit. The breccia is healed by calcite that isolates individual dolomite clasts. As a result, the permeability decreases in zones of brecciation. The late-stage calcite cementation related to the hydrothermal activity is the most important factor to create reservoir heterogeneity in the uniform third sequence, but it is also influential in the grainstone units of the first two sequences. In these sequences, the calcifying fluids invade the dolomite and partly occlude the interparticle porosity and decrease permeability to create heterogeneity in a rock in which the pervasive dolomitization previously reduced much of the influence of facies heterogeneity.

10acarbonate systems.10apermeability10apetrophysical properties10aporosity1 aWestphal, H.1 aEberli, G., P.1 aSmith, L., B.1 aGrammer, G., M.1 aKislak, J. uhttp://archives.datapages.com/data/bulletns/2004/04apr/0405/0405.HTM?doi=10.1306%2FF48FC4B5-2545-4973-AAEA24831A05723B00530nas a2200169 4500008004100000245005600041210005600097300001000153490000700163653001200170100001300182700001500195700001400210700001800224700001900242856009900261 2003 eng d00aLate Quaternary Climate History of Western New York0 aLate Quaternary Climate History of Western New York a11-170 v3710abiology1 aWebb, T.1 aShuman, B.1 aLeduc, P.1 aNewby, P., E.1 aMiller, N., G. uhttps://www.nysm.nysed.gov/staff-publications/late-quaternary-climate-history-western-new-york00480nam a2200121 4500008004100000245005600041210005300097260006200150653001700212100002000229700001600249856009300265 2003 eng d00aAn Introduction to Invertebrate Fossils of New York0 aIntroduction to Invertebrate Fossils of New York aAlbany, New YorkbThe University of the State of New York10apaleontology1 aWeinman, P., L.1 aLanding, E. uhttps://www.nysm.nysed.gov/staff-publications/introduction-invertebrate-fossils-new-york00377nas 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-1932200300572nas a2200133 4500008004100000245007600041210006900117260006200186653001200248100002000260700002200280700002100302856011500323 2002 eng d00aFulton Chain-of-Lakes Area: West Central Adirondack Mountains, New York0 aFulton ChainofLakes Area West Central Adirondack Mountains New Y aAlbany, New YorkbThe University of the State of New York10ageology1 aWhitney, P., R.1 aFakundiny, R., H.1 aIsachsen, Y., W. uhttps://www.nysm.nysed.gov/staff-publications/fulton-chainoflakes-area-west-central-adirondack-mountains-new-y00490nas a2200121 4500008004100000245010100041210006900142300001200211490000700223653001200230100002000242856010600262 2002 eng d00aGeology, geochemistry, and mineralogy of the Iron Mountain skarn, Adirondack Highlands, New York0 aGeology geochemistry and mineralogy of the Iron Mountain skarn A a245-2600 v2410ageology1 aWhitney, P., R. uhttps://www.nysm.nysed.gov/staff-publications/geology-geochemistry-and-mineralogy-iron-mountain-skarn00503nas a2200121 4500008004100000245011200041210006900153300001200222490000700234653001200241100002000253856010800273 2002 eng d00aSkarns in the Adirondack Highlands, New York: Distribution, geochemistry, origin, and tectonic implications0 aSkarns in the Adirondack Highlands New York Distribution geochem a261-2750 v2410ageology1 aWhitney, P., R. uhttps://www.nysm.nysed.gov/staff-publications/skarns-adirondack-highlands-new-york-distribution-geochem00490nam a2200121 4500008004100000245006800041210006800109260006300177100001500240700001700255700001900272856007700291 2001 eng d00aGeometroid caterpillars of Northeastern and Appalachian Forests0 aGeometroid caterpillars of Northeastern and Appalachian Forests aWashington, D. C.bUnited States Department of Agriculture1 aWagner, D.1 aFerguson, D.1 aMcCabe, T., L. uhttp://babel.hathitrust.org/cgi/pt?id=umn.31951d02067489i;view=1up;seq=300526nas 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-sub01680nas a2200205 4500008004100000245009300041210006900134300001200203490000600215520102300221653002001244653001701264653002901281653001001310653002101320100002101341700002201362700002001384856007001404 2001 eng d00aDistributions of Lake Fishes in the Northeast-IV. Benthic and Small Water-column Species0 aDistributions of Lake Fishes in the NortheastIV Benthic and Smal a455-4820 v83 a

Using data collected at 203 randomly selected lakes in eight states in northeastern USA, we present maps of distributions and native status for 28 fish species: 15 benthic species in five families, 11 small water-column feeders in six families, and two large piscivores. Brown bullhead and white sucker were among the most widespread lake-dwelling fishes, and were collected in 69% and 56% of the sampled lakes. Banded killifish, American eel, and yellow bullhead were collected in 26%, 19% and 17% of sampled lakes respectively. The remaining species were collected in <8% of the sampled lakes. Many of the species that were uncommon in this survey have limited distributions in the Northeast or are more commonly found in streams than in lakes. Seven species discussed in this article are Mississippian and were only collected in Cross Lake, NY. We also present a summary of the extent, geographic distributions, and native status of all 88 fish species collected in the EMAP – Northeast Lakes Project.

10abenthic species10afish species10ageographic distributions10alakes10anortheastern USA1 aWhittier, T., R.1 aHalliwell, D., B.1 aDaniels, R., A. uhttp://dx.doi.org/10.1656/1092-6194(2001)008[0455:DOLFIT]2.0.CO;200543nas a2200157 4500008004100000245005200041210005200093260005100145300000900196653001700205100001600222700002000238700002000258700001600278856009100294 2000 eng d00aArchaeological Textile Research in the Americas0 aArchaeological Textile Research in the Americas aSalt Lake City, UtahbUniversity of Utah Press a1-2410aanthropology1 aWebster, L.1 aDrooker, P., B.1 aDrooker, P., B.1 aWebster, L. uhttps://www.nysm.nysed.gov/staff-publications/archaeological-textile-research-americas00621nas a2200181 4500008004100000245011700041210006900158300001200227490000700239653001300246653001300259653002800272653001800300653001500318100002000333700001600353856007000369 2000 eng d00aLower Cambrian (Branchian) Trilobites and Biostratigraphy of the Hanford Brook Formation, Southern New Brunswick0 aLower Cambrian Branchian Trilobites and Biostratigraphy of the H a858-8780 v7410aAvalonia10aCambrian10aHanford Brook Formation10aNorth America10atrilobites1 aWestrop, S., R.1 aLanding, E. uhttp://dx.doi.org/10.1666/0022-3360(2000)074<0858:LCBTAB>2.0.CO;201570nas a2200217 4500008004100000245007800041210006900119300001200188490000600200520087500206653001701081653005201098653001001150653002201160653001801182653002101200100001901221700002201240700002001262856007001282 2000 eng d00aDistributions of Lake Fish in the Northeast: II. The Minnows (Cyprinidae)0 aDistributions of Lake Fish in the Northeast II The Minnows Cypri a131-1560 v73 a

We discuss the distribution and native status of 24 minnow species (family: Cyprinidae) collected at 203 randomly selected lakes in the northeastern USA (New England, New York, New Jersey) by the Environmental Monitoring and Assessment Program (EMAP). Twenty-four species were collected during the summers of 1991–96. Only golden shiner was frequently collected, occurring in 71% of the sampled lakes. Fallfish, creek chub, and common shiner were also common. The remaining species were taken in <10% of the lakes. Physical (surface area, depth, elevation), chemical (pH, total phosphorus), and watershed disturbance characteristics of the lakes show distinct species-specific patterns. Evidence suggests that native minnow biodiversity has declined over the last 150 years as a result of changing biotic, physical, chemical, and watershed characteristics.

10adistribution10aEnvironmental Monitoring and Assessment Program10alakes10aminnow Cyprinidae10anative status10anortheastern USA1 aWhittier, T.R.1 aHalliwell, D., B.1 aDaniels, R., A. uhttp://dx.doi.org/10.1656/1092-6194(2000)007[0131:DOLFIT]2.0.CO;200402nas a2200133 4500008004100000245004200041210004000083300001200123490000700135653001200142100001700154700001900171856007800190 1999 eng d00aA New Species of Perrotia from Taiwan0 aNew Species of Perrotia from Taiwan a461-4640 v7210abiology1 aWang, Y., Z.1 aHaines, J., H. uhttps://www.nysm.nysed.gov/staff-publications/new-species-perrotia-taiwan01851nas a2200241 4500008004100000245010000041210006900141300001200210490000600222520114600228653001801374653001801392653001301410653001701423653001401440653001801454653001301472653002101485100002101506700002201527700002001549856004001569 1999 eng d00aDistributions of lake fish in the Northeast: I. Centrarchidae, Percidae, Esocidae and Moronidae0 aDistributions of lake fish in the Northeast I Centrarchidae Perc a283-3040 v63 a

Using data collected at 203 randomly selected lakes in eight states in northeastern USA, we present maps of distributions and native status for 22 fish species generally characteristic of warm water lakes, mostly water-column feeders, belonging to four families: Centrarchidae (sunfish and bass), Esocidae (pike and pickerel), Moronidae (white perch), and Percidae (yellow perch, walleye, and darters). Pumpkinseed and yellow perch were the most widespread species in our survey, collected in 74% and 72% of lakes, respectively. Five centrarchid species- large-mouth bass, bluegill, small mouth bass, black crappie, and rock bass-were collected in 55%, 32%, 31%, 22%, and 15% of the sampled lakes, respectively, and were judged as non-native in the majority of those lakes. Chain pickerel, white perch, redbreast sunfish, and tessellate darter were collected in 45%, 19%, 14%, and 10% of lakes. The remaining species were taken in <10% of the sampled lakes. Physical (surface area, depth, elevation), chemical (pH, total phosphorus), and watershed disturbance characteristics of the lakes show distinct species-specific patterns.

10aCentrarchidae10adistributions10aEsocidae10afish species10aMoronidae10anative status10aPercidae10awarm water lakes1 aWhittier, T., R.1 aHalliwell, D., B.1 aDaniels, R., A. uhttp://www.jstor.org/stable/385827100399nas a2200133 4500008004100000245004200041210004000083300001000123490000700133653001200140100001300152700001900165856008100184 1999 eng d00aA New Foliicolous Lachnum from Taiwan0 aNew Foliicolous Lachnum from Taiwan a45-490 v7310abiology1 aWu, M-L.1 aHaines, J., H. uhttps://www.nysm.nysed.gov/staff-publications/new-foliicolous-lachnum-taiwan00401nas a2200133 4500008004100000245003100041210002400072260003900096300001200135653001700147100001600164700001700180856007000197 1998 eng d00aThe Street Site (One 44-2)0 aStreet Site One 442 aBuffalo, New YorkbPersimmon Press a123-14310aanthropology1 aWellman, B.1 aFunk, R., E. uhttps://www.nysm.nysed.gov/staff-publications/street-site-one-44203145nas a2200193 4500008004100000245011400041210006900155300001400224490000700238520249900245653002702744653001302771653002402784653002902808653002202837100002002859700002002879856005202899 1998 eng d00aRare Earth Element Metasomatism in Hydrothermal Systems; the Willsboro-Lewis Wollastonite Ores, New York, USA0 aRare Earth Element Metasomatism in Hydrothermal Systems the Will a2965-29770 v623 a

Wollastonite ores and garnet-pyroxene skarns in the Willsboro-Lewis district, New York, USA were formed in a complex hydrothermal system associated with the emplacement of a large anorthosite pluton. Contact-metamorphic marbles were replaced by wollastonite, garnet, and clinopyroxene during infiltration metasomatism involving large volumes of water of chiefly meteoric origin. Rare earth elements (REE) in these rocks show large departures from the protolith REE distribution, indicative of substantial REE mobility. Three types of chondrite-normalized REE distribution patterns are present. The most common, found in ores and skarns containing andradite-rich garnet, is convex-up in the light REE (LREE) with a maximum at Pr and a positive Eu anomaly. Europium anomalies and Pr/Yb ratios are correlated with XAd in garnet. This pattern (type C) results from uptake of REE from hydrothermal fluids by growing crystals of calcsilicate minerals, principally andradite, with amounts of LREE controlled by the difference in ionic radius between Ca++ and REE3+ in garnet X sites. The Eu anomaly results either from prior interaction of the fluids with plagioclase-rich, Eu-positive anorthositic rocks in and near the ore zone, or by enrichment of divalent Eu on growth surfaces of garnet followed by entrapment, or both.

Relative enrichment in heavy REE (type H) occurs in ores and skarn where calcsilicates, including grossularitic garnet, in contact-metamorphic marble have been concentrated by dissolution of calcite. In most cases a negative Eu anomaly is inherited from the marble protolith. Skarns containing titanite and apatite exhibit high total REE, relative light REE enrichment, and negative Eu anomalies (type L). These appear to be intrusive igneous rocks (ferrodiorites or anorthositic gabbros) that have been converted to skarn by Ca metasomatism. REE, sequestered in titanite, apatite, and garnet, preserve the approximate REE distribution pattern of the igneous protolith.

Post-ore granulite facies metamorphism homogenized zoned mineral grains without causing complete intergranular reequilibration and does not appear to have significantly affected the whole-rock REE distributions. These results demonstrate that extensive REE metasomatism can occur in hydrothermal systems at shallow to intermediate depths and that REE geochemistry may be useful in discerning the origin of skarns and skarn-related ore deposits.

10agarnet-pyroxene skarns10aNew York10arare earth elements10aWillsboro-Lewis district10awollastonite ores1 aWhitney, P., R.1 aOlmsted, J., F. uhttp://dx.doi.org/10.1016/S0016-7037(98)00230-000458nas a2200145 4500008004100000245005100041210005100092300001200143490000700155653001200162100001400174700001900188700001600207856008900223 1998 eng d00aNew Species and Records of Lachnum from Taiwan0 aNew Species and Records of Lachnum from Taiwan a341-3540 v6710abiology1 aWu, M.-L.1 aHaines, J., H.1 aWang, Y.-Z. uhttps://www.nysm.nysed.gov/staff-publications/new-species-and-records-lachnum-taiwan00570nas a2200109 4500008004100000245018000041210006900221260002100290653002300311100001500334856011100349 1996 eng d00aCultural Resources Reconnaissance Survey Report for PIN 1236.14.101, NY 29; Jockey Street, East Galway to Middle Line Road, Town of Galway and Milton Saratoga County, New York0 aCultural Resources Reconnaissance Survey Report for PIN 12361410 aAlbany, New York10aCultural Resources1 aWarren, J. uhttps://www.nysm.nysed.gov/staff-publications/cultural-resources-reconnaissance-survey-report-pin-1236141000470nas a2200145 4500008004100000245003500041210003500076260005200111300001200163653001700175100001600192700001600208700001900224856008100243 1996 eng d00aNew York State Museum Site 3030 aNew York State Museum Site 303 aBethlehem, ConnecticutbArchaeological Services a109-11810aanthropology1 aWellman, B.1 aLindner, C.1 aCurtin, E., V. uhttps://www.nysm.nysed.gov/staff-publications/new-york-state-museum-site-30300636nas a2200145 4500008004100000245017800041210006900219300001200288490000700300653001200307100002000319700002200339700001800361856011100379 1996 eng d00aProterozoic Low-Ti Iron-oxide Deposits in New York and New Jersey; Relation to Fe-oxide (Cu-U-Au-rare earth element) Deposits and Tectonic Implications; Discussion and Reply0 aProterozoic LowTi Ironoxide Deposits in New York and New Jersey  a382-3840 v2410ageology1 aWhitney, P., R.1 aMcLelland, J., M.1 aFoose, M., P. uhttps://www.nysm.nysed.gov/staff-publications/proterozoic-lowti-ironoxide-deposits-new-york-and-new-jersey00563nas a2200145 4500008004100000245010700041210006900148300001000217490000700227653001700234100002000251700002100271700001600292856010900308 1995 eng d00aDeclining Importance of Trilobites in Ordovician Nearshore Paleocommunities; Dilution or Displacement?0 aDeclining Importance of Trilobites in Ordovician Nearshore Paleo a75-790 v1010apaleontology1 aWestrop, S., R.1 aTremblay, J., V.1 aLanding, E. uhttps://www.nysm.nysed.gov/staff-publications/declining-importance-trilobites-ordovician-nearshore-paleo00605nas a2200157 4500008004100000245005800041210005800099260009200157300001000249653001200259100002000271700002000291700001900311700001800330856009900348 1995 eng d00aWollastonite Deposits of the Northeastern Adirondacks0 aWollastonite Deposits of the Northeastern Adirondacks aSchenectady, New Yorkb67th annual meeting of the New York State Geological Association a25-3810ageology1 aWhitney, P., R.1 aOlmsted, J., F.1 aGarver, J., I.1 aSmith, J., A. uhttps://www.nysm.nysed.gov/staff-publications/wollastonite-deposits-northeastern-adirondacks-000537nas a2200157 4500008004100000245005800041210005800099260002600157300001000183653001200193100002000205700002000225700001900245700001800264856009700282 1995 eng d00aWollastonite Deposits of the Northeastern Adirondacks0 aWollastonite Deposits of the Northeastern Adirondacks aSchenectady, New York a25-3810ageology1 aWhitney, P., R.1 aOlmsted, J., F.1 aGarver, J., I.1 aSmith, J., A. uhttps://www.nysm.nysed.gov/staff-publications/wollastonite-deposits-northeastern-adirondacks00484nas a2200121 4500008004100000245009800041210006900139260006200208653001200270100002000282700002000302856004000322 1993 eng d00aBedrock Geology of the Au Sable Forks Quadrangle, Northeastern Adirondack Mountains, New York0 aBedrock Geology of the Au Sable Forks Quadrangle Northeastern Ad aAlbany, New YorkbThe University of the State of New York10ageology1 aWestrop, P., R.1 aOlmsted, J., F. uhttp://purl.nysed.gov/nysl/2966617601893nas a2200193 4500008004100000245011200041210006900153300001400222490000700236520123900243653002901482653002101511653002601532653001501558100002001573700001701593700001601610856007301626 1993 eng d00aLower Ordovician (Ibexian) Trilobites from the Tribes Hill Formation, Central Mohawk Valley, New York State0 aLower Ordovician Ibexian Trilobites from the Tribes Hill Formati a1618-16330 v303 a

The Early Ordovician Tribes Hill Formation of east-central New York State is a sequence of peritidal to subtidal carbonates and minor shales that rests disconformably on Late Cambrian carbonates and is, in turn, succeeded disconformably by Middle Ordovician strata. More than 800 trilobites from 24 collections are assigned to six species: Bellefontia gyracantha (Raymond), Clelandia parabola (Cleland), Hystricurus ellipticus (Cleland), Hystricurus cf. Hystricurus oculilunatus Ross, Symphysurina convexa (Cleland), and Symphysurina cf. Symphysurina woosteri Ulrich. Two distinct biofacies are present: the Bellefontia Biofacies in subtidal shales with thin, storm-generated bioclastic interbeds, and the Gastropod–rostroconch Biofacies in shallow, carbonate bank lithofacies. The trilobites of the Tribes Hill Formation are assigned to a single, informal biostratigraphic unit, the Clelandia parabola Fauna, which is correlative with trilobite Zone B of the Garden City Formation of Utah and with the Bellefontia franklinense Subzone of the McKenzie Hill Formation of Oklahoma.

10aClelandia parabola Fauna10aEarly Ordovician10aTribes Hill Formation10atrilobites1 aWestrop, S., R.1 aKnox, L., A.1 aLanding, E. uhttp://www.nrcresearchpress.com/doi/abs/10.1139/e93-140#.Vl4BO7-1W7000529nas a2200169 4500008004100000245004200041210003700083260003500120300001000155653001200165100002000177700002000197700002100217700001800238700002000256856008300276 1993 eng d00aThe Willsboro-Lewis Wollastonite Ores0 aWillsboroLewis Wollastonite Ores bSociety of Economic Geologists a17-2510ageology1 aWestrop, P., R.1 aOlmsted, J., F.1 aPetersen, E., U.1 aSlack, J., F.1 aOffield, T., W. uhttps://www.nysm.nysed.gov/staff-publications/willsborolewis-wollastonite-ores02575nas a2200133 4500008004100000245009900041210006900140300000800209490000700217520211500224653001202339100002002351856007002371 1992 eng d00aCharnockites and Granites of Western Adirondacks, New York, USA; A Differentiated A-type Suite0 aCharnockites and Granites of Western Adirondacks New York USA A  a1-20 v573 a

Granitic rocks in the west-central Adirondack Highlands of New York State include both relatively homogeneous charnockitic and hornblende granitic gneisses (CG), that occur in thick stratiform bodies and elliptical domes, and heterogeneous leucogneisses (LG), that commonly are interlayered with metasedimentary rocks. Major- and trace-element geochemical analyses were obtained for 115 samples, including both types of granitoids. Data for CG fail to show the presence of more than one distinct group based on composition. Most of the variance within the CG sample population is consistent with magmatic differentiation combined with incomplete separation of early crystals of alkali feldspar, plagioclase, and pyroxenes or amphibole from the residual liquid. Ti, Fe, Mg, Ca, P, Sr, Ba, and Zr decrease with increasing silica, while Rb and K increase. Within CG, the distinction between charnockitic (orthopyroxene-bearing) and granitic gneisses is correlated with bulk chemistry. The charnockites are consistently more mafic than the hornblende granitic gneisses, although forming a continuum with them. The leucogneisses, while generally more felsic than the charnockites and granitic gneisses, are otherwise geochemically similar to them. The data are consistent with the LG suite being an evolved extrusive equivalent of the intrusive CG suite.

Both CG and LG suites are metaluminous to mildly peraluminous and display an A-type geochemical signature, enriched in Fe, K, Ce, Y, Nb, Zr, and Ga and depleted in Ca, Mg, and Sr relative to I- and S-type granites. Rare earth element patterns show moderate LREE enrichment and a negative Eu anomaly throughout the suite. The geochemical data suggest an origin by partial melting of biotite- and plagioclase-rich crustal rocks. Emplacement occurred in an anorogenic or post-collisional tectonic setting, probably at relatively shallow depths. Deformation and granulite-facies metamorphism with some partial melting followed during the Ottawan phase of the Grenville Orogeny, yielding the present migmatitic granitic and charnockitic gneisses.

10ageology1 aWhitney, P., R. uhttp://www.sciencedirect.com/science/article/pii/030192689290092300514nas a2200121 4500008004100000245010500041210006900146260002200215653001200237100001900249700002100268856010300289 1987 eng d00aDetailed studies of Selected, Well-exposed Fracture Zones in the Adirondack Mountains Dome, New York0 aDetailed studies of Selected Wellexposed Fracture Zones in the A aWashington, D. C.10ageology1 aWeiner, R., W.1 aIsachsen, Y., W. uhttps://www.nysm.nysed.gov/staff-publications/detailed-studies-selected-wellexposed-fracture-zones02532nas a2200229 4500008004100000245018900041210006900230300001200299490000700311520173700318653001002055653002402065653002702089653002302116653001002139653001302149653001602162100002002178700001902198700001502217856007002232 1987 eng d00aStudies on the Culicine Mosquito Host Range of Bacillus sphaericus and Bacillus thuringiensis var. israelensis with Notes on the Effects of Temperature and Instar on Bacterial Efficacy0 aStudies on the Culicine Mosquito Host Range of Bacillus sphaeric a291-3020 v493 a
Toxicity tests of three strains of Bacillus sphaericus against late instars of 12 culicine mosquito species indicated a wide range of susceptibility. Culex pipiens and C. salinarius were highly susceptible (LC50s < 104 spores/ml) to strain 1593, and C. pipiens and C. restuans were highly susceptible to strain 2013-4. The potency of strain SSII-1 was approximately one-tenth that of strains 1593 and 2013-4 against C. pipiens. Susceptibility of Aedes species to strain 1593 was highly variable. At temperatures ≥ 20°C, A. fitchii, A. intrudens, A. stimulans, and A. vexans were moderately to highly susceptible (LC50s 6 × 103−4 × 104 spores/ml), A. triseriatus was only slightly susceptible (LC50 > 106 spores/ml), and A. aegypti was refractory. Susceptibility of Aedes mosquitoes to strain SSII-1 was less variable, with LC50s against A. aegypti, A. canadensis, A. stimulans, and A. triseriatus all being between 104 and 106 vegetative cells + spores/ml. All species of mosquitoes tested were, in general, highly susceptible to B. thuringiensis var. israelensis (LC50s 2.3 × 103−2.5 × 104 spores/ml). In B. sphaericus toxicity tests, decreased temperatures resulted in up to a 16-fold increase in LC50 and a substantial reduction in probit line slope. First-instar A. aegypti larvae were more susceptible to B. sphaericus strain SSII-1 than the three later instars, which were approximately equally susceptible; however, no significant difference was observed in the susceptibility of the four instars of A. triseriatus.
10aAedes10aBacillus sphaericus10aBacillus thuringiensis10aBiological control10aCulex10aCuliseta10aisraelensis1 aWraight, S., P.1 aMolloy, D., P.1 aSinger, S. uhttp://www.sciencedirect.com/science/article/pii/002220118790061900528nas a2200133 4500008004100000245005500041210005500096260008300151300001000234653001200244100002000256700002200276856009600298 1985 eng d00aRocks and Problems of the Southeastern Adirondacks0 aRocks and Problems of the Southeastern Adirondacks aSaratoga, New YorkbNew York State Geological Association, 57th annual meeting a47-6710ageology1 aWhitney, P., R.1 aLindemann, R., H. uhttps://www.nysm.nysed.gov/staff-publications/rocks-and-problems-southeastern-adirondacks-000466nas a2200133 4500008004100000245005500041210005500096260002300151300001000174653001200184100002000196700002200216856009400238 1985 eng d00aRocks and Problems of the Southeastern Adirondacks0 aRocks and Problems of the Southeastern Adirondacks aSaratoga, New York a47-6710ageology1 aWhitney, P., R.1 aLindemann, R., H. uhttps://www.nysm.nysed.gov/staff-publications/rocks-and-problems-southeastern-adirondacks00645nas a2200169 4500008004100000245010000041210006900141260003400210300000900244653001200253100001900265700002200284700002100306700001700327700002400344856010700368 1984 eng d00aStratigraphy and Structural Geology of the Adirondack Mountains, New York; Review and Synthesis0 aStratigraphy and Structural Geology of the Adirondack Mountains  bGeological Society of America a1-5510ageology1 aWiener, R., W.1 aMcLelland, J., M.1 aIsachsen, Y., W.1 aHall, L., M.1 aBartholomew, M., J. uhttps://www.nysm.nysed.gov/staff-publications/stratigraphy-and-structural-geology-adirondack-mountains00696nas a2200133 4500008004100000245021300041210006900254260006200323653001200385100001900397700001900416700001900435856010800454 1983 eng d00aBedrock Topography and Glacial Deposits of the Colonie Channel Between Saratoga Lake and Coeymans, New York with a section by R.M. Waller: Ground-Water Potential of the Capital District Buried-Valley Deposits0 aBedrock Topography and Glacial Deposits of the Colonie Channel B aAlbany, New YorkbThe University of the State of New York10ageology1 aWaller, R., M.1 aHanson, E., L.1 aDineen, R., J. uhttps://www.nysm.nysed.gov/staff-publications/bedrock-topography-and-glacial-deposits-colonie-channel-b00464nas 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-regi00330nas a2200121 4500008004100000245003900041210003700080300001000117490000700127653001700134100001600151856004100167 1982 eng d00aA Survey of New York Fluted Points0 aSurvey of New York Fluted Points a39-400 v1010aanthropology1 aWellman, B. uhttp://www.jstor.org/stable/4091419801566nas a2200157 4500008004100000245015700041210006900198300001000267490000800277520095000285653001201235100002001247700001901267700001401286856010801300 1982 eng d00aA Comparison of Laboratory and Field Tests of Bacillus sphaericus Strain 1593 and Bacillus thuringiensis var. israelensis Against Aedes stimulans Larvae0 aComparison of Laboratory and Field Tests of Bacillus sphaericus  a55-610 v1143 a

Bacillus thuringiensis var. israelensis (serotype H-14) and B. sphaericus strain 1593 were tested against Aedes stimulons larvae in the laboratory and in 38-cm-diam, open-ended cylinders embedded in the bottom detritus of a woodland pool. Estimates of LC50 were lower against fourth instars in the field at a mean temperature of 15.9 °C than in the laboratory at 21.1 °C. The greater efficacy in the field was attributed to high daytime water temperatures (mean 20.5 °C) following treatment and exposure of the larvae to substantially greater amounts of toxic material in a larger volume of water than in the laboratory. The regression of probit on log10 concentration was not linear over the entire range of mortality caused by B. sphaericus, increasing the difficulty of estimation of LC values. Bacillus sphaericus was significantly less active than B. thuringiensis.

10abiology1 aWraight, S., P.1 aMolloy, D., P.1 aMcCoy, P. uhttps://www.nysm.nysed.gov/staff-publications/comparison-laboratory-and-field-tests-bacillus-sphaericus00706nas a2200169 4500008004100000245008700041210006900128260009400197300001000291653002500301100002000326700001600346700001900362700001900381700001900400856011700419 1981 eng d00aUpper Cambrian and Lower Ordovician Biostratigraphy, Jasper National Park, Alberta0 aUpper Cambrian and Lower Ordovician Biostratigraphy Jasper Natio aGolden, ColoradobSecond International Symposium on the Cambrian System. Golden, Colorado a45-5310ageology paleontology1 aWestrop, S., R.1 aLanding, E.1 aLudvigsten, R.1 aAitken, J., D.1 aTaylor, M., E. uhttps://www.nysm.nysed.gov/staff-publications/upper-cambrian-and-lower-ordovician-biostratigraphy-jasper-natio-000631nas a2200169 4500008004100000245008700041210006900128260002100197300001000218653002500228100002000253700001600273700001900289700001900308700001900327856011500346 1981 eng d00aUpper Cambrian and Lower Ordovician Biostratigraphy, Jasper National Park, Alberta0 aUpper Cambrian and Lower Ordovician Biostratigraphy Jasper Natio aGolden, Colorado a45-5310ageology paleontology1 aWestrop, S., R.1 aLanding, E.1 aLudvigsten, R.1 aAitken, J., D.1 aTaylor, M., E. uhttps://www.nysm.nysed.gov/staff-publications/upper-cambrian-and-lower-ordovician-biostratigraphy-jasper-natio01554nas a2200217 4500008004100000245016400041210006900205300001000274490000700284520077900291653002001070653003601090653003101126653002301157653001601180100002001196700001901216700001701235700001401252856007001266 1981 eng d00aEffects of Temperature and Instar on the Efficacy of Bacillus thuringiensis var. israelensis and Bacillus sphaericus Strain 1593 Against Aedes stimulans Larvae0 aEffects of Temperature and Instar on the Efficacy of Bacillus th a78-870 v383 a
Laboratory trials of Bacillus thuringiensis var. israelensis (serotype 14) and B. sphaericus strain 1593 against field-collected Aedes stimulans showed that susceptibility declined with increasing instar and decreasing temperature. Test results with B. sphaericus were more erratic than with B. thuringiensis, and the efficacy of the former declined more rapidly with decreasing temperature. B. thuringiensis was significantly more active than B. sphaericus under all treatment conditions. These results indicate that the effective use of this strain of B. sphaericus as a mosquito biological control agent may be limited to warm water situations against more susceptible species.
10aAedes stimulans10aBacillus sphaericus strain 159310aBacillus thuringiensis var10aBiological control10aisraelensis1 aWraight, S., P.1 aMolloy, D., P.1 aJamnback, H.1 aMcCoy, P. uhttp://www.sciencedirect.com/science/article/pii/002220118190037901302nas a2200157 4500008004100000245016700041210006900208300001200277490000800289520066900297653001200966100002000978700001900998700001701017856011001034 1981 eng d00aEfficacy of Bacillus sphaericus Strain 1593 Against the Four Instars of Laboratory Reared and Field Collected Culex pipiens and Laboratory Reared Culex salinarius0 aEfficacy of Bacillus sphaericus Strain 1593 Against the Four Ins a379-3860 v1133 a

Culex pipiens pipiens and C. salinarius were found equally susceptible in laboratory tests to Bacillus sphaericus strain 1593 with LC50 values for the four instars ranging between 20 and 137 ppb (approximately 820 and 5600 spores/ml). Tests against field collected C. p. pipiens larvae revealed a regularly decreasing susceptibility with increasing larval age, the first instars being between 2 and 5 times more susceptible than fourth instars. In contrast, no significant differences in the susceptibility of second, third, and fourth instars were found in tests of laboratory reared larvae.

10abiology1 aWraight, S., P.1 aMolloy, D., P.1 aJamnback, H. uhttp://journals.cambridge.org/action/displayAbstract?fromPage=online&aid=8542389&fileId=S0008347X0001912X01661nas a2200133 4500008004100000245010400041210006900145300001200214490000600226520119300232653001201425100002001437856007001457 1975 eng d00aRelationship of Manganese-iron Oxides and Associated Heavy Metals to Grain Size in Stream Sediments0 aRelationship of Manganeseiron Oxides and Associated Heavy Metals a251-2630 v43 a

The distribution of ammonium citrate-leachable lead, zinc and cadmium among size fractions in stream sediments is strongly influenced by the presence of hydrous Mn-Fe oxides in the form of coatings on sediment grains. Distribution curves showing leachable metals as a function of particle size are given for eight samples from streams in New York State. These show certain features in common; in particular two concentrations of metals, one in the finest fractions, and a second peak in the coarse sand and gravel fraction. The latter can be explained as a result of the increasing prevalence and thickness of oxide coatings with increasing particle size, with the oxides serving as collectors for the heavy metals. The distribution of Zn and Cd in most of the samples closely parallels that of Mn; the distribution of Pb is less regular and appears to be related to Fe in some samples and Mn in others. The concentration of metals in the coarse fractions due to oxide coatings, combined with the common occurrence of oxide deposition in streams of glaciated regions, raises the possibility of using coarse materials for geochemical surveys and environmental heavy-metal studies.

10ageology1 aWestrop, P., R. uhttp://www.sciencedirect.com/science/article/pii/037567427590005900460nas a2200121 4500008004100000245007500041210006900116300000800185490000700193653001200200100002000212856010600232 1975 eng d00aUse of Oxide-coated Stream Gravels in Geochemical Surveys; A Test Case0 aUse of Oxidecoated Stream Gravels in Geochemical Surveys A Test  a2520 v7010ageology1 aWhitney, P., R. uhttps://www.nysm.nysed.gov/staff-publications/use-oxidecoated-stream-gravels-geochemical-surveys-test03233nas a2200145 4500008004100000245007000041210006800111300001000179490000700189520278100196653001202977100002002989700002203009856005603031 1973 eng d00aOrigin of Coronas in Metagabbros of the Adirondack Mts., New York0 aOrigin of Coronas in Metagabbros of the Adirondack Mts New York a81-980 v393 a

Metagabbros from two widely separated areas in the Adirondacks show development of coronas. In the Southern Adirondacks, these are cored by olivine which is enclosed in a shell of orthopyroxene that is partially, or completely, rimmed by symplectites consisting of clinopyroxene and spinel. Compositions of the corona phases have been determined by electron probe and are consistent with a mechanism involving three partial reactions, thus:

(a) Olivine=Orthopyroxene+(Mg, Fe)++.

(b) Plagioclase+(Mg, Fe)+++Ca++=Clinopyroxene+Spinel+Na+.
 
(c) Plagioclase+(Mg, Fe)+++Na+=Spinel+more sodic plagioclase+Ca++.
 
Reaction (a) occurs in the inner shell of the corona adjacent to olivine; reaction (b) in the outer shell; and (c) in the surrounding plagioclase, giving rise to the spinel clouding which is characteristic of the plagioclase in these rocks. Alumina and silica remain relatively immobile. These reactions, when balanced, can be generalized to account for the aluminous nature of the pyroxenes and for changing plagioclase composition. Summed together, the partial reactions are equivalent to:

(d) Olivine + Anorthite = Aluminous orthopyroxene + Aluminous Clinopyroxene + Spinel (Kushiro and Yoder, 1966).

In the Adirondack Highlands, coronas between olivine and plagioclase commonly have an outer shell of garnet replacing the clinopyroxene/spinel shell. The origin of the garnet can also be explained in terms of three partial reactions:

(e) Orthopyroxene+Ca++=Clinopyroxene+(Mg, Fe)++.

(f) Clinopyroxene+Spinel+Plagioclase+(Mg, Fe)++=Garnet+Ca+++Na+.
 
(g) Plagioclase+(Mg, Fe)+++Na+=Spinel + more sodic plagioclase+Ca++.
 

These occur in the inner and outer corona shell and the surrounding plagioclase, respectively, and involve the products of reactions (a)-(d). Alumina and silica are again relatively immobile. Balanced, and generalized to account for aluminous pyroxenes and variable An content of plagioclase, they are equivalent to:

(h) Orthopyroxene+Anorthite+Spinel=Garnet (Green and Ringwood, 1967).

Amphibole coronas about opaque oxides in rocks of both areas are the result of oxide/plagioclase reactions with addition of magnesium from coexisting olivine.

Based on published experimental data, pressure and temperature at the time of corona formation were on the order of 8 kb and 800° C for the garnet bearing coronas, with somewhat lower pressures indicated for the clinopyroxene/spinel coronas.

10ageology1 aWhitney, P., R.1 aMcLelland, J., M. uhttp://link.springer.com/article/10.1007/BF0037424700467nas a2200121 4500008004100000245008200041210006900123300001400192490000700206653001200213100002000225856010000245 1972 eng d00aSpinel Inclusions in Plagioclase of Metagabbros from the Adirondack Highlands0 aSpinel Inclusions in Plagioclase of Metagabbros from the Adirond a1429-14360 v5710ageology1 aWhitney, P., R. uhttps://www.nysm.nysed.gov/staff-publications/spinel-inclusions-plagioclase-metagabbros-adirond00404nam a2200109 4500008004100000245006100041210006100102260006200163653001200225100001900237856003800256 1972 eng d00aEntomology Projects for Elementary and Secondary Schools0 aEntomology Projects for Elementary and Secondary Schools aAlbany, New YorkbThe University of the State of New York10abiology1 aWilcox, J., A. uhttp://purl.nysed.gov/nysl/72640100440nam a2200109 4500008004100000245008900041210006900130260006200199653001200261100001900273856003800292 1972 eng d00aA Review of the North American Chrysomeline Leaf Beetles (Coleoptera: Chrysomelidae)0 aReview of the North American Chrysomeline Leaf Beetles Coleopter aAlbany, New YorkbThe University of the State of New York10abiology1 aWilcox, J., A. uhttp://purl.nysed.gov/nysl/74681500372nam a2200109 4500008004100000245004300041210004100084260006200125653001700187100002000204856003800224 1969 eng d00aA Bibliography of Iroquoian Literature0 aBibliography of Iroquoian Literature aAlbany, New YorkbThe University of the State of New York10aanthropology1 aWeinman, P., L. uhttp://purl.nysed.gov/nysl/19714501052nas a2200181 4500008004100000245013200041210006900173300001200242490000700254520046500261653001200726100001600738700001700754700001800771700001600789700001900805856004600824 1969 eng d00aCalifornia Virus in New York state: Isolation and characterization of California encephalitis virus complex from Aedes cinereus0 aCalifornia Virus in New York state Isolation and characterizatio a123-1310 v183 a

In St. Lawrence County, New York State, in 1964-65, 7, 940 Culicids, Ceratopo-gonids, Simuliids and Tabanids were tested in 769 pools for evidence of virus infection. One of 51 pools of Aedes cinereus Mg. yielded a virus of the California encephalitis complex of a type different from the prototype strain. Antibodies neutralizing California encephalitis virus were found in serum from man, cattle and wild animals in 11 counties of New York.

10abiology1 aWhitney, E.1 aJamnback, H.1 aMeans, R., G.1 aRoz, A., P.1 aRayner, G., A. uhttps://doi.org/10.4269/ajtmh.1969.18.12301111nas a2200133 4500008004100000245008900041210006900130300001400199490000700213520065500220653001200875100002000887856007000907 1969 eng d00aVariations of the K/Rb Ratio in Migmatitic Paragneisses of the Northwest Adirondacks0 aVariations of the KRb Ratio in Migmatitic Paragneisses of the No a1203-12110 v333 a

Data for the migmatitic paragneisses of the Northwest Adirondacks indicate fractionation of potassium and rubidium during metamorphism and migmatization; total rock KRb ratios are controlled to a significant degree by modal composition. Biotite-poor granitic veins and lenses show KRb ratios averaging 431 in contrast to the host gneisses which have an average KRb ratio of 271. Paragneisses from the zone of granulite facies metamorphism show significantly higher (mean 307) KRb ratios than those from the amphibolite facies (231), indicating the possibility of regional depletion in Rb relative to K under intensive metamorphic conditions.

10ageology1 aWhitney, P., R. uhttp://www.sciencedirect.com/science/article/pii/001670376990042802009nas a2200169 4500008004100000245014300041210006900184300001200253490000700265520143700272653001201709100001601721700001701737700001801754700002101772856004601793 1968 eng d00aArthropod-borne-virus Survey in St. Lawrence County, New York. Arbovirus Reactivity in Serum from Amphibians, Reptiles, Birds, and Mammals0 aArthropodbornevirus Survey in St Lawrence County New York Arbovi a645-6500 v173 a

Serological evidence of the presence of groups A, B and Bunyamwera arboviruses in New York State has been reported [Bull Hyg., 1964, v. 39, 75; Am. J. Vet. Res., 1965, v. 26, 914]. In continuation of these studies a further 901 wild animal sera (amphibian, reptilian, avian and mammalian) and 192 human sera were obtained from St. Lawrence County and tested for the presence of haemagglutination inhibiting (HI) and neutralizing (NT) antibodies. Group A reactivity was tested against eastern and western encephalomyelitis viruses, group B reactivity with Powassan and St. Louis encephalitis viruses, while the Bunyamwera group was represented by Cache Valley in NT tests and by Maguari virus in HI tests.

Only a few reactions with group A viruses were found, but there was evidence of considerable activity by group B viruses-particularly Powassan virus. Of 70 sera from woodchucks (Marmota monax), 38 had both NT and HI antibodies against Powassan virus and sera from 9 other mammalian species were also reactive. Despite this high incidence in animal sera, only 2 human sera gave evidence suggesting previous infection with group B arboviruses; one had antibodies to Powassan and the other to St. Louis encephalitis virus. In the Bunyamwera group, 9 of 192 human sera neutralized Cache Valley virus, but no antibodies to this group of viruses were found in any of the 901 animal sera.

10abiology1 aWhitney, E.1 aJamnback, H.1 aMeans, R., G.1 aWatthews, T., H. uhttps://doi.org/10.4269/ajtmh.1968.17.64500967nas a2200145 4500008004100000245006500041210006100106300001200167490000800179520053800187653001200725100001600737700001700753856005100770 1965 eng d00aThe First Isolations of the Powassan Virus in New York State0 aFirst Isolations of the Powassan Virus in New York State a432-4350 v1193 a

Powassan virus was isolated from 2 pools of ticks (1 unidentified, the other Ixodes cookei) removed from 2 Marmota monax live-trapped in northern St. Lawrence County. Powassan virus was also isolated from tissues taken from the same 2 animals. Another strain of POW virus was recovered from the brain of a sick gray fox found in Broome County 200 miles to the south in New York State. The 2 tick strains were compared antigenically with the proto-type POW strain and were found to be antigenically similar.

10abiology1 aWhitney, E.1 aJamnback, H. uhttp://ebm.sagepub.com/content/119/2/432.short00429nam a2200109 4500008004100000245007700041210006900118260006200187653001200249100001900261856003900280 1965 eng d00aA Synopsis of the North American Galerucinae (Coleoptera: Chrysomelidae)0 aSynopsis of the North American Galerucinae Coleoptera Chrysomeli aAlbany, New YorkbThe University of the State of New York10abiology1 aWilcox, J., A. uhttp://purl.nysed.gov/nysl/129309001213nas a2200169 4500008004100000245004500041210004500086300001200131490000600143520073700149653001200886100002200898700001600920700001900936700001500955856007300970 1965 eng d00aArchean Volcanism in the Canadian Shield0 aArchean Volcanism in the Canadian Shield a161-1750 v13 a

Chemical compositions of Archaean volcanic rocks in the Superior province of the Canadian shield have been determined from 261 new analyses from 10 volcanic belts. The analyses are compared with those of the various volcanic associations. This comparison shows that the volcanic rocks of all belts belong to the basalt andesite rhyolite association typical of continental orogenic belts or island are systems. A primitive continent with continental rocks must, therefore, have existed in early Archaean time.The Keewatin lava sequences in the various belts are remnants of a great volcanic sequence that covered the southern half of the Superior province of the Canadian shield.

10ageology1 aWilson, H., D. B.1 aAndrews, P.1 aMoxham, R., L.1 aRamlal, K. uhttp://www.nrcresearchpress.com/doi/abs/10.1139/e65-014#.V0NUl-Q0NNs00341nas a2200121 4500008004100000245002900041210002900070300001000099490000700109653001200116100001900128856007200147 1960 eng d00aSome Beetles of New York0 aSome Beetles of New York a23-270 v1410abiology1 aWilcox, J., A. uhttps://www.nysm.nysed.gov/staff-publications/some-beetles-new-york01937nas a2200145 4500008004100000245008200041210006900123300001200192490000700204520147400211653001201685100001701697700001701714856006001731 1957 eng d00aSampling Methods Used in Estimating Larval Populations of Salt-Marsh Tabanids0 aSampling Methods Used in Estimating Larval Populations of SaltMa a389-3910 v503 a

Two methods of estimating populations of Tabanid larvae in salt-marsh sod were compared on Long Island, New York, in 1954-56. The first was bringing the larvae to the surface of a cleared area at low tide by spraying it twice at an interval of five minutes with a 1: 19 dilution of the New Jersey larvicide. This is a concentrate consisting of 66 per cent. kerosene or similar petroleum distillate, 0.07 per cent. pyrethrins, 0.5 per cent. sodium lauryl sulfate and 33.5 per cent. water [cf. R.A.E., B 23 205]. It was used at 1 U.S. gal. diluted emulsion per sq. yd. About 87 per cent. of the larvae coming to the surface in 60 minutes under its influence did so in the first 40 minutes. Limited tests indicated that O.5 oz. 10 per cent. γ BHC (lindane) in 1 U.S. gal. water [cf. 45 116] was about a; effective as the New Jersey larvicide, and a suspension of a wettable powder of pyrethrum and sulfoxide [1, 2-methylenedioxy-4-(2-(octylsulphinyl)propyl)ben-zene] somewhat more effective. The second method was cutting foot-square samples of sod and drying them in a Berlese funnel, so that larvae driven out in the drying process fell into a jar of marsh water. This water was examined every clay or two days. The samples were 1 1/2 ins. thick, as experiments in which plugs 8 1/2 ins. thick were cut into slices and these were examined separately showed that virtually all the larvae recovered were from the top 1 1/2 ins., even in winter.

10abiology1 aWall, W., J.1 aJamnback, H. uhttp://jee.oxfordjournals.org/content/50/4/389.abstract00445nam a2200109 4500008004100000245008700041210006900128260006200197653001200259100001900271856004500290 1957 eng d00aA Revision of the North American Species of Paria Lec. (Coleoptera: Chrysomelidae)0 aRevision of the North American Species of Paria Lec Coleoptera C aAlbany, New YorkbThe University of the State of New York10abiology1 aWilcox, J., A. uhttp://purl.org/net/nysl/nysdocs/472421800400nas a2200121 4500008004100000245007900041210006900120300001200189490000700201653001200208100001800220856004000238 1942 eng d00aStudies in the Genus Helotium. I A Review of the Species Described by Peck0 aStudies in the Genus Helotium I A Review of the Species Describe a154-1790 v3410abiology1 aWhite, W., L. uhttp://www.jstor.org/stable/375480900314nas a2200121 4500008004100000245001800041210001800059300001200077490000700089653001200096100002000108856006400128 1932 eng d00aWayside Weeds0 aWayside Weeds a225-2270 v1810abiology1 aWhitney, E., G. uhttps://www.nysm.nysed.gov/staff-publications/wayside-weeds00419nas a2200121 4500008004100000245005800041210005600099300001200155490000700167653001200174100001900186856009200205 1915 eng d00aA Critical Discussion of the Crystal Forms of Calcite0 aCritical Discussion of the Crystal Forms of Calcite a289-3520 v5010ageology1 aWhitlock, H.P. uhttps://www.nysm.nysed.gov/staff-publications/critical-discussion-crystal-forms-calcite00376nas a2200133 4500008004100000245002800041210002800069300001200097490000700109653001200116100002100128700001900149856007400168 1912 eng d00aCrystallographic Tables0 aCrystallographic Tables a819-8210 v3510ageology1 aWhitlock, H., P.1 aWherry, E., T. uhttps://www.nysm.nysed.gov/staff-publications/crystallographic-tables00364nam a2200109 4500008004100000245002500041210002500066260006200091653001200153100002100165856006800186 1910 eng d00aCalcites of New York0 aCalcites of New York aAlbany, New YorkbThe University of the State of New York10ageology1 aWhitlock, H., P. uhttps://www.nysm.nysed.gov/staff-publications/calcites-new-york00391nam a2200109 4500008004100000245005000041210005000091260006200141653001200203100002100215856004500236 1905 eng d00aContributions from the Mineralogic Laboratory0 aContributions from the Mineralogic Laboratory aAlbany, New YorkbThe University of the State of New York10ageology1 aWhitlock, H., P. uhttp://purl.org/net/nysl/nysdocs/383491200371nas a2200121 4500008004100000245003800041210003800079300001200117490000700129653001200136100002000148856008100168 1886 eng d00aAnnelida claetopoda of New Jersey0 aAnnelida claetopoda of New Jersey a128-1590 v3910abiology1 aWebster, H., E. uhttps://www.nysm.nysed.gov/staff-publications/annelida-claetopoda-new-jersey00436nas a2200121 4500008004100000245006200041210006200103300001200165490000700177653001700184100002000201856009300221 1884 eng d00aNew Species of Fosslls from the Trenton Group of New York0 aNew Species of Fosslls from the Trenton Group of New York a207-2140 v3510apaleontology1 aWalcott, C., D. uhttps://www.nysm.nysed.gov/staff-publications/new-species-fosslls-trenton-group-new-york00410nas a2200121 4500008004100000245005300041210004800094300001200142490000700154653001700161100001900178856009100197 1884 eng d00aAboriginal Work on Bluff Point, Yates Co. N. Y .0 aAboriginal Work on Bluff Point Yates Co N Y a193-1940 v3510aanthropology1 aWright, S., H. uhttps://www.nysm.nysed.gov/staff-publications/aboriginal-work-bluff-point-yates-co-n-y00358nas a2200121 4500008004100000245003600041210003300077300001200110490000700122653001200129100001900141856007600160 1884 eng d00aGeology of Yaites County, N. Y.0 aGeology of Yaites County N Y a195-2060 v3510ageology1 aWright, B., H. uhttps://www.nysm.nysed.gov/staff-publications/geology-yaites-county-n-y00471nas a2200121 4500008004100000245008400041210006900125300001000194490000700204653001700211100002000228856010100248 1879 eng d00aDiscovery of the Remains of the Natatory and Branchial Appendages of Trilobites0 aDiscovery of the Remains of the Natatory and Branchial Appendage a89-920 v2810apaleontology1 aWalcott, C., D. uhttps://www.nysm.nysed.gov/staff-publications/discovery-remains-natatory-and-branchial-appendage00334nas a2200121 4500008004100000245002600041210002600067300001000093490000700103653001700110100002000127856006500147 1879 eng d00aEggs of the Trilobite0 aEggs of the Trilobite a66-670 v3110apaleontology1 aWalcott, C., D. uhttps://www.nysm.nysed.gov/staff-publications/eggs-trilobite00428nas a2200121 4500008004100000245005900041210005800100300001200158490000700170653001700177100002000194856009200214 1879 eng d00aNew Species of Fossils from the Calcif'erous Formation0 aNew Species of Fossils from the Calciferous Formation a129-1310 v3210apaleontology1 aWalcott, C., D. uhttps://www.nysm.nysed.gov/staff-publications/new-species-fossils-calciferous-formation00446nas a2200121 4500008004100000245006500041210006500106300001000171490000700181653001700188100002000205856009900225 1879 eng d00aNew Species of Fossils from the Chazy and Trenton Limestones0 aNew Species of Fossils from the Chazy and Trenton Limestones a68-710 v3110apaleontology1 aWalcott, C., D. uhttps://www.nysm.nysed.gov/staff-publications/new-species-fossils-chazy-and-trenton-limestones00428nas a2200121 4500008004100000245005900041210005900100300001000159490000700169653001700176100002000193856009300213 1879 eng d00aSome Sections of Trilobites from the Trenton Limestone0 aSome Sections of Trilobites from the Trenton Limestone a61-650 v3110apaleontology1 aWalcott, C., D. uhttps://www.nysm.nysed.gov/staff-publications/some-sections-trilobites-trenton-limestone00371nas a2200121 4500008004100000245003800041210003800079300001200117490000700129653001200136100002000148856008100168 1879 eng d00aAnnelida chaetopoda of New Jersey0 aAnnelida chaetopoda of New Jersey a101-1280 v3210abiology1 aWebster, H., E. uhttps://www.nysm.nysed.gov/staff-publications/annelida-chaetopoda-new-jersey