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

Bibliographic Details
Published in:Paleoceanography
Main Authors: Cortese, Giuseppe, Dunbar, Gavin, Carter, L, Scott, G, Bostock, Helen, Bowen, M, Crundwell, M, Hayward, B, Howard, William, Martinez, J Ignacio, Moy, Andrew D, Neil, Helen, Sabaa, A, Sturm , A
Format: Article in Journal/Newspaper
Language:unknown
Published: American Geophysical Union
Subjects:
Keywords: calibration
cooling
depositional environment
interglacial
marine isotope stage
marine sediment
paleoceanography
planktonic foraminifera
sea surface temperature
sediment core
warming
western boundary current
wind stress
Australia
Campbell Pla Foraminifera
Interglacial climate
Marine Isotope Stage 5
South Pacific Ocean
Pacific
Planktonic foraminifera
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
Description
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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