01488nas a2200229 4500008004100000245013200041210006900173260003300242300001000275520071400285653001900999653002101018653002101039653002101060653001601081653002701097100001601124700002501140700001301165700001301178856006701191 2011 eng d00aTesting the Paleo-Maritime Hypothesis for Glacial Lake Iroquois: Implications for Changing Views of Past Culture and Technology0 aTesting the PaleoMaritime Hypothesis for Glacial Lake Iroquois I aNew York, New YorkbSpringer a27-433 a

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

10aEarly Holocene10alate Pleistocene10amaritime culture10apaleo-shorelines10aPaleoindian10astone tool assemblages1 aSchultz, M.1 aWinchell-Sweeney, S.1 aRush, L.1 aFord, B. uhttp://link.springer.com/chapter/10.1007%2F978-1-4419-8210-0_200829nas a2200169 4500008004100000245005300041210005200094300001200146490000700158520029400165653002100459653002700480653001800507100002000525700002100545856009300566 2010 eng d00a33Ms391: A Paleoindian Site in Southeastern Ohio0 a33Ms391 A Paleoindian Site in Southeastern Ohio a120-1220 v273 a

A 2006 CRM study explored Paleoindian Site 33Ms391, located in Meigs
County, southeastern Ohio, in the unglaciated Appalachian Plateaus province
(GAI 2006a, 2006b). The site lies on a late-Pleistocene dune field that mantles
a T3 terrace above the Ohio River.

10alate Pleistocene10aPaleoindian settlement10asouthern Ohio1 aLothrop, J., C.1 aCremeens, D., L. uhttps://www.nysm.nysed.gov/staff-publications/33ms391-paleoindian-site-southeastern-ohio00994nas a2200205 4500008004100000245010700041210006900148300001200217490000700229520033600236653001500572653002100587653001200608100002000620700001600640700001600656700001900672700001500691856008200706 2007 eng d00aRadiocarbon Dates from the Pleistocene Fossil Deposits of Samwell Cave, Shasta County, California, USA0 aRadiocarbon Dates from the Pleistocene Fossil Deposits of Samwel a117-1210 v493 a

Dates obtained from the collagen of 5 mammals from the fossil deposits of Samwel Cave, Shasta County, California,
USA, show emplacement during the last glacial maximum. These dates support the assignment of the fauna to the late
Pleistocene. The Samwel Cave deposits currently do not appear to be stratified.

10aCalifornia10alate Pleistocene10amammals1 aFeranec, R., S.1 aHadly, E.A.1 aBlois, J.L.1 aBarnosky, A.D.1 aPaytan, A. uhttps://journals.uair.arizona.edu/index.php/radiocarbon/article/view/2904/pdf02052nas a2200205 4500008004100000245012900041210006900170300001200239490000800251520137700259653002301636653002101659653001301680653001301693653001701706653002301723100001901746700001901765856006201784 2006 eng d00aPaleoecology of a late Pleistocene Wetland and Associated Mastodon Remains in the Hudson Valley, Southeastern New York State0 aPaleoecology of a late Pleistocene Wetland and Associated Mastod a291-3040 v3993 a

Late Quaternary history and paleoecology of a small oxbow wetland on glaciated terrain were investigated using sediment lithology (cores, bulk samples, backhoedug trenches), ground-penetrating radar, vascular plant and moss macrofossil stratigraphies, and accelerator mass spectrometric radiocarbon dating. A nearly complete mastodon skeleton was recovered from late Pleistocene detrital peat and peaty marl near the top of the sediment sequence. Sedimentation in the basin began with silt and clay over dense cobble outwash transported southward from the nearby Hyde Park Moraine. Overbank sediment deposition occurred between ∼13,000 and 12,220 yr B.P. during a period of tundra vegetation, which ended with a sharp rise in spruce needle abundance and a shift to autochthonous marl and finally peat deposition. Fossils of aquatic and wetland plants began to accumulate before the tundra-spruce transition and increased after it. Rich fen wetland began to infill the pond with peat, while the upland supported open white spruce and later white spruce–balsam fir–tamarack forest. The mastodon, 11,480 ± 40 radiocarbon years old, was contemporaneous with spruce–balsam fir–tamarack forest and rich fen wetland. Many mastodon bones were articulated or nearly so, indicating that the animal died in the basin and that postmortem bone dispersal was slight.

10acalcareous wetland10alate Pleistocene10amastodon10aNew York10apaleoecology10aplant macrofossils1 aMiller, N., G.1 aNester, P., L. uhttp://specialpapers.gsapubs.org/content/399/291.abstract02289nas a2200181 4500008004100000245010500041210006900146300000900215490000800224520150500232653001301737653002101750653002301771100002101794700001801815700001401833856026001847 1993 eng d00aLate Pleistocene and Holocene Vertebrates from Joralemon's (Fish Club) Cave, Albany County, New York0 aLate Pleistocene and Holocene Vertebrates from Joralemons Fish C a9-150 v1053 a

At least 35 species of fish, amphibians, reptiles, birds, and mammals were recovered from excavations conducted in 1988 and 1990 at Joralemon's Cave, Town of Coeymans. Albany County, New York. Formerly known as Fish Club Cave, this site was excavated initially in 1962-1964 by R.E. Funk and R.A. Johnson, who reported bones of whitetailed deer (96% of all bones) and five other species associated with lithic artifacts of Woodland and Late Archaic age. Our more recent excavations yielded bones of one
species that no longer occurs in New York State (Neotoma magister, Allegheny woodrat) and three other species that either are absent or extremely rare within 70-20 km of the site (Crotalus horridus, timber rattlesnake; Synaptomys cooperi, southern bog lemming; Ursus americanus, black bear). Our larger, faunal assemblage, obtained front a much smaller volume of excavated sediment, reflects: 1) the use of finemesh (1/16-in) screens: 2), faunal and cultural differences between the front and back of the cave; and 3) a search image oriented as much to bones as artifacts. While Joralemon's Care clearly is an archaeological site, it is also partly paleontological in origin (i.e., it contains bones deposited by non-human means). We believe that the vertebrate faunas
from most "archaeological" sites in caves and rockshelters include a significant paleontological component that should be regarded as such when interpreting faunal assemblages in terms of human subsistence.

10aHolocene10alate Pleistocene10avertebrate fossils1 aSteadman, D., W.1 aCraig, L., J.1 aEngel, T. uhttps://www.google.com/url?sa=t&rct=j&q=&esrc=s&source=web&cd=4&ved=0ahUKEwjWoLbMvbvJAhWC7yYKHTwKBMEQFggsMAM&url=http%3A%2F%2Fnysarchaeology.org%2Fdownload%2Fnysaa%2Fbulletin%2Fnumber_105.pdf&usg=AFQjCNFwOZNNDMqj2r_2Bn5NDGi2Xeuqqw&sig2=7fBB8EA76CbCKmv9aEo