Circulation changes and nutrient concentrations in the late Quaternary Aegean Sea: A nonsteady state concept for sapropel formation-Reference-Cited by-同舟云学术

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Circulation changes and nutrient concentrations in the late Quaternary Aegean Sea: A nonsteady state concept for sapropel formation

Published:2002-05 Issue:2 Volume:17 Page:14-1-14-11
ISSN:0883-8305
Container-title:Paleoceanography
language:en
Short-container-title:Paleoceanography

Author:

Casford J. S. L.¹,Rohling E. J.¹,Abu-Zied R.¹,Cooke S.¹,Fontanier C.²,Leng M.³,Lykousis V.⁴

Affiliation:

1. Southampton Oceanography Centre; Southampton UK

2. Department of Geology and Oceanography; Bordeaux University; UMR 58-05 Talence France

3. Natural Environment Research Council Isotope Geoscience Laboratory; Keyworth UK

4. National Centre for Marine Research; Athens Greece

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

Reference72 articles.

1. Organic geochemical and palynological evidence for the terrigeneous origin of the organic matter in Aegean Sea sapropel S1;Asku;Mar. Geol.,1999

2. The eastern Mediterranean paleoclimate as a reflection of regional events: Soreq cave, Israel;Bar-Matthews;Earth Planet. Sci. Lett.,1999

3. Temperature and salinity limits for growths and survival of some planktonic foraminifers in laboratory cultures;Bijma;J. Foraminiferal Res.,1990

4. Lunar and semi lunar reproductive cycles in some spinose planktonic foramifers;Bijma;J. Foraminiferal Res.,1990

5. Studies of winter sinking of cold water in the Aegean Sea;Bruce;Rapp. Comm. Int. Mer. Medit.,1965

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