Abstract
Four sediment cores were collected to determine the depositional environments of the King George Basin northeast of Bransfield Strait, Antarctica. The cored section revealed three distinct lithofacies: laminated siliceous ooze derived from an increased paleoproductivity near the receding sea-ice edges, massive muds that resulted from hemipelagic sedimentation in open water, and graded sediments that originated from nearby local seamounts by turbidity currents. Clay mineral data of the cores indicate a decreasing importance of volcanic activity through time. Active volcanism and hydrothermal activity appear to be responsible for the enrichment of smectite near the Penguin and Bridgeman Islands.
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Yoon, H.I., Park, B.K., Chang, S.K. et al. Depositional environment of near-surface sediments, King George Basin, Bransfield Strait, Antarctica. Geo-Marine Letters 14, 1–9 (1994). https://doi.org/10.1007/BF01204465
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DOI: https://doi.org/10.1007/BF01204465