Middle Eocene to early Oligocene paleoceanography of the Antarctic Ocean (Maud Rise, ODP Leg 113, Site 689): change from a low to a high productivity ocean-Reference-Cited by-同舟云学术

Middle Eocene to early Oligocene paleoceanography of the Antarctic Ocean (Maud Rise, ODP Leg 113, Site 689): change from a low to a high productivity ocean

Published:1995-02 Issue:2-4 Volume:113 Page:311-334
ISSN:0031-0182
Container-title:Palaeogeography, Palaeoclimatology, Palaeoecology
language:en
Short-container-title:Palaeogeography, Palaeoclimatology, Palaeoecology

Author:

Diester-Haass L.

Publisher

Elsevier BV

Subject

Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

Reference63 articles.

1. Biosiliceous particle flux in the Southern Ocean;Abelmann;Mar. Chem.,1991

2. Evolution of biosiliceous sedimentation patterns Eocene through Quaternary: paleoceanographic response to polar cooling;Baldauf,1990

3. Leg 113;Barker,1988

4. Paleogene and early Neogene oceanography of the southern Indian Ocean: Leg 119 foraminifer stable isotope results;Barrera,1991

5. Leg 113;Barron,1991

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