Enhanced δ13C and δ18O Differences Between the South Atlantic and South Pacific During the Last Glaciation: The Deep Gateway Hypothesis-Reference-Cited by-同舟云学术

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Enhanced δ13C and δ18O Differences Between the South Atlantic and South Pacific During the Last Glaciation: The Deep Gateway Hypothesis

Published:2017-10 Issue:10 Volume:32 Page:1000-1017
ISSN:0883-8305
Container-title:Paleoceanography
language:en
Short-container-title:Paleoceanography

Author:

Sikes Elisabeth L.¹^ORCID,Allen Katherine A.²^ORCID,Lund David C.³^ORCID

Affiliation:

1. Institute of Marine and Coastal Sciences; State University of New Jersey, Rutgers; New Brunswick NJ USA

2. School of Earth and Climate Sciences; University of Maine; Orono ME USA

3. Department of Marine Sciences; University of Connecticut Avery Point; Groton CT USA

Funder

National Sleep Foundation

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2017PA003118/fullpdf

Reference99 articles.

1. The role of deep ocean circulation in setting glacial climates;Adkins;Paleoceanography,2013

2. The salinity, temperature, and 18O of the glacial deep ocean;Adkins;Science,2002

3. Southwest Pacific deep water carbonate chemistry linked to high southern latitude climate and atmospheric CO2 during the Last Glacial Termination;Allen;Quaternary Science Reviews,2015

4. Ross Sea paleo-ice sheet drainage and deglacial history during and since the LGM;Anderson;Quaternary Science Reviews,2014

5. Wind-driven upwelling in the Southern Ocean and the deglacial rise in atmospheric CO2;Anderson;Science,2009

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