Evolution of Atlantic-Pacific δ13C gradients over the last 2.5 m.y.-Reference-Cited by-同舟云学术

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Evolution of Atlantic-Pacific δ13C gradients over the last 2.5 m.y.

Published:1990-03 Issue:3-4 Volume:97 Page:353-368
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Raymo M.E.,Ruddiman W.F.,Shackleton N.J.,Oppo D.W.

Publisher

Elsevier BV

Subject

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

Reference52 articles.

1. The Norwegian Sea as a Mediterranean basin;Worthington;Deep Sea Res.,1970

2. The role of vertical chemical fractionation in controlling late Quaternary atmospheric carbon dioxide;Boyle;J. Geophys. Res.,1988

3. On the late Pleistocene ocean geochemistry and circulation;Keir;Paleoceanogr.,1988

4. The cause of the glacial to interglacial atmospheric CO2 change: A polar alkalinity hypothesis;Broecker;Global Biogeochem. Cycles,1989

5. Quaternary deep-water circulation changes in the distribution of δ13C of deep water σCO2 between the last glaciation and the Holocene;Curry;Paleoceanogr.,1988

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