T122 Archaeological Geology and the Pleistocene-Holocene Transition
Wednesday, 7 November 2001
8:00 AM - 12:00 PM
PROGLACIAL LAKE-MARGINAL WETLANDS AND THE PALEOINDIAN TRADITION IN SOUTHERN MANITOBA, CANADA
Paper number: T122-6
Program: Technical Sessions
Time: 8:00 AM – 12:00 PM
Authors
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Garry L. RunningUniv of Wisconsin-Eau Claire, Eau Claire, WI
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James T. TellerUniv of Manitoba, Winnipeg, MB
Abstract
Paleoindian sites in the Canadian Prairies are often found in association with the margins of large proglacial lakes. However, since these lakes were nearly abiotic due to cold water temperatures and high turbidity, the significance of the archaeological site distributions remains unclear. On-going geoarchaeological research in southern Manitoba is addressing this research question through regional- and local-scale paleoenvironmental reconstructions of proglacial lake-marginal locales. Behind the active beaches of glacial Lakes Agassiz and Hind, we note that paleolagoons and fens/ peatlands on recently-drained lake surfaces were numerous throughout the Pleistocene-Holocene transition. Preliminary macrobotanical (and other paleoecological) data indicate that these small wetlands were sufficiently isolated from the oligotrophic conditions of the larger, meltwater-fed, lakes to support a stable assemblage of economic and medicinal plants by approximately 10.5 ka BP. Because the proglacial lake shorelines would also have constrained animal migration routes, we therefore hypothesize that the adjacent wetlands were highly efficient locales for plant gathering and large mammal entrapment.