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Holocene Driftwood Incursion to Southwestern Victoria Island, Canadian Arctic Archipelago, and Its Significance to Paleoceanography and Archaeology

Published online by Cambridge University Press:  20 January 2017

Arthur S. Dyke  and
James M. Savelle
Arthur S. Dyke
Affiliation:
Terrain Sciences Division, Geological Survey of Canada, 601 Booth Street, Ottawa, Ontario, Canada, K1A 0E8
James M. Savelle
Affiliation:
Department of Anthropology, McGill University, 855 Sherbrooke Street West, Montreal, Quebec, Canada, H3A 2T7
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Abstract

Holocene driftwood is found on postglacial raised beaches of Wollaston Peninsula, Victoria Island. The highest driftwood appears on the 12- to 13-m beach, which formed about 4000 yr B.P., and is common on beaches 12–6 m in elevation. The earliest Paleoeskimo dwelling features also occur on the 12- to 13-m beach. Wood increases on the 5- to 6-m beach, which formed about 2000 yr B.P., and is abundant below that level. Thus, zonation of wood suggests the following hypotheses: (1) that the coastal Mackenzie Current, the source of modern driftwood, did not operate before 4000 yr B.P. and lacked its present vigor or persistence until 2000 yr B.P.; and (2) that the apparent sudden influx of driftwood at 4000 yr B.P. may have provided a fuel resource and (or) may have been related to conditions that enabled first peopling. Radiocarbon ages indicate that (1) the first wood arrived about 4700 yr B.P.; (2) little wood arrived from 4700–2000 yr B.P.; and (3) influx of wood was episodic after 2000 yr B.P. Much of the wood that arrived after 1100 yr B.P. was redistributed by people and scattered on higher beaches. Explanation of the evident correlation between highest wood and highest dwelling features must await archaeological studies.

Keywords

driftwoodArtic Ocean circulationarchaeologyPaleoeskimoThuleclimate changesea-level change
Type
Research Article
Information
Quaternary Research , Volume 54 , Issue 1 , July 2000 , pp. 113 - 120
Copyright
University of Washington

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References

Blake, W. Jr. (1972). Climatic implications of radiocarbon-dated driftwood in the Queen Elizabeth Islands, Arctic Canada. Vasari, Y., Hyvärinen, H., Hicks, S. Climatic Changes in Arctic Areas during the Last 10,000 Years 77–104., Google Scholar
Dyke, A.S. Geological Survey of Canada, Open File(1996). 3296 Google Scholar
Dyke, A.S., England, J., Reimnitz, E., Jetté, H. (1997). Changes in driftwood delivery to the Canadian Arctic Archipelago: The hypothesis of postglacial oscillations of the Transpolar Drift. Arctic,50, 1–16., Google Scholar
Dyke, A.S., Morris, T.F. (1990). Postglacial History of the Bowhead Whale and of Driftwood Penetration: Implications for Paleoclimate, Central Canadian Arctic. Geological Survey of Canada, Paper,89-24, 17 Google Scholar
Dyke, A.S., Savelle, J.M. (2000). Major end moraines of Younger Dryas age on Wollaston Peninsula, Victoria Island, Canadian Arctic: Implications for paleoclimate and for formation of hummocky moraine. Canadian Journal of Earth Sciences,37, 601–619., Google Scholar
Eggertsson, O. (1994). Mackenzie River driftwood—A dendrochronological study. Arctic,47, 128–186., Google Scholar
Häggblom, A. (1982). Driftwood in Svalbard as an indicator of sea ice conditions. Geografiska Annaler,64A, 81–94., Google Scholar
Hopkins, D.M., Smith, P.A., Matthews, J.V. Jr. (1981). Dated wood from Alaska and the Yukon: Implications for forest refugia in Beringia. Quaternary Research,15, 217–249., CrossRefGoogle Scholar
Jenness, D. (1922). The Life of the Copper Eskimos. Report of the Canadian Arctic Expedition 1913–1918,Vol, XII, (A), King's Printer, Ottawa.Google Scholar
Jenness, S.E. (1991). Arctic Odyssey: The Diary of Diamond Jenness, Ethnologist with the Canadian Arctic Expedition in Northern Alaska and Canada, 1913–1916. Canadian Museum of Civilization, Hull.Google Scholar
Maxwell, M.S. (1985). Prehistory of the Eastern Arctic. Academic Press, New York.Google Scholar
McGhee, R. (1996). Ancient People of the Arctic. Univ. of British Columbia Press, Vancouver.Google Scholar
Pelletier, B.R. (1984). Geological Survey of Canada, Miscellaneous Report,38, Google Scholar
Rigor, I. (1992). Arctic Ocean buoy program. ARCOS Newsletter,44, 1–3., Google Scholar
Ritchie, J.C. (1984). Past and Present Vegetation of the Far Northwest of Canada. Univ. of Toronto Press, Toronto.Google Scholar
Ritchie, J.C., Hare, F.K. (1971). Late Quaternary vegetation and climate near the Arctic treeline of northwestern North America. Quaternary Research,1, 331–342., Google Scholar
Sharpe, D.R. (1992). Geological Survey of Canada, Memoir,434, 84 Google Scholar
Stewart, T.G., England, J. (1983). Holocene sea-ice variations and paleoenvironmental change, northernmost Ellesmere Island, N.W.T., Canada. Arctic and Alpine Research,15, 1–17., Google Scholar
Tremblay, L-B., Mysak, L.A., Dyke, A.S. (1997). Evidence from driftwood records for century-to-millennial scale variations of the high latitude atmospheric circulation during the Holocene. Geophysical Research Letters,24, 2027–2030., Google Scholar