Ocean overturning since the Late Cretaceous: Inferences from a new benthic foraminiferal isotope compilation-Reference-Cited by-同舟云学术

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Ocean overturning since the Late Cretaceous: Inferences from a new benthic foraminiferal isotope compilation

Published:2009-12 Issue:4 Volume:24 Page:
ISSN:0883-8305
Container-title:Paleoceanography
language:en
Short-container-title:Paleoceanography

Author:

Cramer B. S.¹,Toggweiler J. R.²,Wright J. D.³,Katz M. E.⁴,Miller K. G.³

Affiliation:

1. Department of Geological Sciences; University of Oregon; Eugene Oregon USA

2. Geophysical Fluid Dynamics Laboratory; NOAA; Princeton New Jersey USA

3. Department of Earth and Planetary Sciences; Rutgers University; Piscataway New Jersey USA

4. Department of Earth and Environmental Sciences; Rensselaer Polytechnic Institute; Troy New York USA

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

Link

http://www.agu.org/journals/pa/pa0904/2008PA001683/2008PA001683.pdf

Reference103 articles.

1. Extraterrestrial cause for the Cretaceous-Tertiary extinction;Alvarez;Science,1980

2. Origin, signature and palaeoclimatic influence of the Antarctic Circumpolar Current;Barker;Earth Sci. Rev.,2004

3. Evidence for thermohaline-circulation reversals controlled by sea-level change in the Latest Cretaceous;Barrera;Geology,1997

4. Reevaluation of the oxygen isotopic composition of planktonic foraminifera: Experimental results and revised paleotemperature equations;Bemis;Paleoceanography,1998

5. Cenozoic cooling, Antarctic nutrient pump, and the evolution of whales;Berger;Deep Sea Res., Part II,2007

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