1. Millennial-scale instability of the Antarctic Ice Sheet during the last glaciation
- Author
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P. Graham Mortyn, Christopher D. Charles, Thomas P. Guilderson, Ulysses S Ninnemann, David A. Hodell, Sharon L. Kanfoush, and Marine Biogeology
- Subjects
geography ,Multidisciplinary ,geography.geographical_feature_category ,North Atlantic Deep Water ,Ocean current ,Antarctic ice sheet ,Ice shelf ,Oceanography ,Glacial period ,Stadial ,SDG 14 - Life Below Water ,Ice sheet ,Geology ,Ice rafting - Abstract
Records of ice-rafted detritus (IRD) concentration in deep-sea cores from the southeast Atlantic Ocean reveal millennial-scale pulses of IRD delivery between 20,000 and 74,000 years ago. Prominent IRD layers correlate across the Polar Frontal Zone, suggesting episodes of Antarctic Ice Sheet instability. Carbon isotopes (δ 13 C) of benthic foraminifers, a proxy of deepwater circulation, reveal that South Atlantic IRD events coincided with strong increases in North Atlantic Deep Water (NADW) production and inferred warming (interstadials) in the high-latitude North Atlantic. Sea level rise or increased NADW production associated with strong interstadials may have resulted in destabilization of grounded ice shelves and possible surging in the Weddell Sea region of West Antarctica.
- Published
- 2000
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