History of sedimentation rates in the sea-ice sedimentation zone during the last 130 ka

被引:0
作者
M. A. Levitan
R. Stein
机构
[1] Russian Academy of Sciences,Vernadskii Institute of Geochemistry and Analytical Chemistry
[2] Alfred Wegener Institute of Polar and Marine Investigations,undefined
[3] Columbusstrasse,undefined
来源
Lithology and Mineral Resources | 2008年 / 43卷
关键词
Continental Margin; Arctic Ocean; Pelagic Zone; Oxygen Isotope Stage; Greenland Basin;
D O I
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中图分类号
学科分类号
摘要
Based on literature and our data, analysis of sedimentation rates during the last glacial/interglacial cycle (during the last 130 ka) is given for the Norwegian-Greenland Basin, the Arctic Ocean, Bering and Okhotsk seas, as well as a number of seas in the Southern Ocean. Sedimentation rates in the studied zone are controlled by the development of continental ice sheets, sea ice covers, and biogenic sedimentation, which, in turn, depends on climate variations.
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页码:65 / 75
页数:10
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