Carbonate crash and biogenic bloom in the late Miocene: Evidence from ODP Sites 1085, 1086, and 1087 in the Cape Basin, southeast Atlantic Ocean-Reference-Cited by-同舟云学术

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Carbonate crash and biogenic bloom in the late Miocene: Evidence from ODP Sites 1085, 1086, and 1087 in the Cape Basin, southeast Atlantic Ocean

Published:2004-02-04 Issue:1 Volume:19 Page:n/a-n/a
ISSN:0883-8305
Container-title:Paleoceanography
language:en
Short-container-title:Paleoceanography

Author:

Diester-Haass L.¹,Meyers P. A.²,Bickert T.³

Affiliation:

1. Zentrum für Umweltwissenschaften der Universität; Universität des Saarlandes; Saarbrücken; Germany

2. Marine Geology and Geochemistry Program, Department of Geological Sciences; University of Michigan; Ann Arbor; Michigan; USA

3. Fachbereich Geowissenschaften; Universität Bremen; Bremen; Germany

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

Reference101 articles.

1. Sea-level events in the South Pacific linked with the Messinian salinity crisis;Aharon;Geology,1993

2. Anderson , P. A. C. D. Charles W. H. Berger 2001 Walvis paradox confirmed for the early Quaternary at the southern end of the Namibia upwelling system, ODP Site 1085 Ocean Drill, Program College Station, Tex. http://www-odp.tamu.edu/publications/175_SR/chap_21/chap_21.htm.

3. Effect of deep-sea sedimentary calcite preservation on atmospheric CO2 concentration;Archer;Nature,1994

4. Barker , P. F. 1990 Proceedings of the Ocean Drilling Program, Initial Reports 113 Ocean Drill. Program College Station, Tex

5. Barron , J. 1991 Proceedings of the Ocean Drilling Program, Initial Reports 119 Ocean Drill. Program College Station, Tex

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