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...
Published in: | Geophysical Research Letters |
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Main Authors: | , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
2008
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Subjects: | |
Online Access: | https://eprints.soton.ac.uk/54786/ http://www.agu.org/pubs/crossref/2008/2007GL032254.shtml |