Reconstruction of late Quaternary sea-level change in southwestern British Columbia from sediments in isolation basins |
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Authors: | IAN HUTCHINSON THOMAS S. JAMES JOHN J. CLAGUE J. VAUGHN BARRIE KIM W. CONWAY |
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Affiliation: | (e-mail: ), Department of Geography, Simon Fraser University, Burnaby, B.C., Canada V5A 1S6;Geological Survey of Canada, Sidney, B.C., Canada V8L 4B2;Department of Earth Sciences, Simon Fraser University, Burnaby, B.C., Canada V5A 1S6. |
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Abstract: | Bracketing ages on marine—freshwater transitions in isolation basins extending from sea level to 100 m elevation on Lasqueti Island, and data from shallow marine cores and outcrops on eastern Vancouver Island, constrain late Pleistocene and Holocene sea-level change in the central Strait of Georgia. Relative sea level fell from 150 m elevation to about —15 m from 14000 cal. yr BP to 11 500 cal. yr BP. Basins at higher elevations exhibit abrupt changes in diatom assemblages at the marine-freshwater transition. At lower elevations an intervening brackish phase suggests slower rates of uplift. Relative sea level rose to about +1 m about 9000 cal. yr BP to 8500 cal. yr BP, and then slowly fell to the modern datum. The mean rate of glacio-isostatic rebound in the first millennium after deglaciation was about 0.11 in a -1, similar to the peak rate at the centres of the former Laurentide and Fennoscandian ice complexes. The latter feature smooth, exponential-style declines in sea level up to the present day, whereas in the study area the uplift rate dropped to less than one-tenth of its initial value in only about 2500 years. Slower, more deeply seated isostatic recovery generated residual uplift rates of <0.01 m a-1 in the early Holocene after the late-Pleistocene wasting of the Cordilleran ice sheet. |
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