Glacial water mass geometry and the distribution of δ13C of ΣCO2in the western Atlantic Ocean

Author:

Curry W. B.1,Oppo D. W.1

Affiliation:

1. Department of Geology and Geophysics; Woods Hole Oceanographic Institution; Woods Hole Massachusetts USA

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

Reference41 articles.

1. The salinity, temperature, and δ18O of the glacial deep ocean;Adkins;Science,2002

2. Core top evaluation of benthic foraminiferal isotopic ratios for paleoceanographical interpretations;Belanger;Palaeogeogr. Palaeoclimatol. Palaeoecol.,1981

3. Late Pliocene to Holocene (2.6-0 Ma) western equatorial Atlantic deep-water circulation: Inferences from stable isotopes;Bickert;Proc. Ocean Drill. Program Sci. Results,1997

4. Geophys. Monogr. Ser.;Boyle,1984

5. Deep circulation in the North Atlantic over the last 200,000 years, geochemical evidence;Boyle;Science,1982

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