Temporal evolution of mechanisms controlling ocean carbon uptake during the last glacial cycle-Reference-Cited by-同舟云学术

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Temporal evolution of mechanisms controlling ocean carbon uptake during the last glacial cycle

Published:2017-08 Issue: Volume:472 Page:206-215
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Kohfeld Karen E.^ORCID,Chase Zanna

Funder

National Sciences and Engineering Research Council of Canada

Canada Research Chairs

Australian Research Council

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference63 articles.

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

2. Multiple timescales for neutralization of fossil fuel CO2;Archer;Geophys. Res. Lett.,1997

3. Insolation values for the climate of the last 10 million years;Berger;Quat. Sci. Rev.,1991

4. The Southern Ocean surface between Marine Isotope Stages 6 and 5d: shape and timing of climate changes;Bianchi;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2002

5. Strong and deep Atlantic meridional overturning circulation during the last glacial cycle;Böhm;Nature,2014

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