Antarctic records of precession-paced insolation-driven warming during early Pleistocene Marine Isotope Stage 31

Precisely dated Antarctic continental margin and Southern Ocean geological records show that the early Pleistocene interglacial Marine Isotope Stage 31 (MIS-31) was characterized by warmer than present surface waters with reduced sea-ice and enhanced high latitude marine carbonate production. Microp...

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Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Scherer, R, Bohaty, S, Dunbar, Robert B, Esper, O, Flores, J, Gersonde, R, Harnwood, D, Roberts, Andrew, Taviani, M
Format: Article in Journal/Newspaper
Language:unknown
Published: American Geophysical Union
Subjects:
Keywords: Atmospheric temperature
Glacial geology
Global warming
Oceanography
Sea ice
Thermal stratification
Pleistocene marine isotope
Sea surface temperature
Water mass stratification
Geochronology
continental margin
ice sheet
interglacial
marine iso
Antarctic
Southern Ocean
Cape Roberts
Antarc*
Ice Sheet
Online Access:http://hdl.handle.net/1885/18971
https://doi.org/10.1029/2007GL032254
https://openresearch-repository.anu.edu.au/bitstream/1885/18971/5/Antarctic_Roberts.pdf.jpg
https://openresearch-repository.anu.edu.au/bitstream/1885/18971/7/01_Scherer_Antarctic_records_of_2008.pdf.jpg

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