Southwest Pacific Ocean response to a warmer world: Insights from marine isotope stage 5e
Paleoceanographic archives derived from 17 marine sediment cores reconstruct the response of the Southwest Pacific Ocean to the peak interglacial, Marine Isotope Stage (MIS) 5e (ca. 125 ka). Paleo-Sea Surface Temperature (SST) estimates were obtained from
Published in: | Paleoceanography |
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Main Authors: | , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
American Geophysical Union
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Subjects: | |
Online Access: | http://hdl.handle.net/1885/77768 https://doi.org/10.1002/palo.20052 https://openresearch-repository.anu.edu.au/bitstream/1885/77768/5/f5625xPUB6554_2013.pdf.jpg https://openresearch-repository.anu.edu.au/bitstream/1885/77768/7/01_Cortese_Southwest_Pacific_Ocean_2013.pdf.jpg |
Summary: | Paleoceanographic archives derived from 17 marine sediment cores reconstruct the response of the Southwest Pacific Ocean to the peak interglacial, Marine Isotope Stage (MIS) 5e (ca. 125 ka). Paleo-Sea Surface Temperature (SST) estimates were obtained from |
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