Eastern Mediterranean surface water temperatures and δ18O composition during deposition of sapropels in the late Quaternary-Reference-Cited by-同舟云学术

Eastern Mediterranean surface water temperatures and δ18O composition during deposition of sapropels in the late Quaternary

Published:2003-02-11 Issue:1 Volume:18 Page:n/a-n/a
ISSN:0883-8305
Container-title:Paleoceanography
language:en
Short-container-title:Paleoceanography

Author:

Emeis K.-C.¹,Schulz H.¹,Struck U.²,Rossignol-Strick M.³,Erlenkeuser H.⁴,Howell M. W.⁵,Kroon D.⁶,Mackensen A.⁷,Ishizuka S.⁸,Oba T.⁹,Sakamoto T.¹⁰,Koizumi I.¹⁰

Affiliation:

1. Baltic Sea Research Institute; Warnemuende Germany

2. Institute of Paleontology and Historical Geology; University of Munich; Munich Germany

3. Laboratoire de Paléobiologie et Palynologie; Université Pierre et Marie Curie; Paris France

4. Leibniz-Laboratory for Radiometric Dating and Stable Isotope Research; Kiel University; Kiel Germany

5. Department of Geological Sciences; University of South Carolina; Columbia South Carolina USA

6. Faculty of Earth Sciences; Vrije Universiteit Amsterdam; Amsterdam Netherlands

7. Alfred-Wegener-Institut für Polar- und Meeresforschung; Bremerhaven Germany

8. The Education Bureau of Aomori Prefecture; Seihoku Educational Office; Goshogawara Japan

9. Graduate School of Environmental Earth Science; Hokkaido University; Sapporo Japan

10. Department of Earth and Planetary Sciences, Graduate School of Science; Hokkaido University; Sapporo Japan

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

Reference103 articles.

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3. Interhemispheric synchrony of the last deglaciation inferred from alkenone palaeothermometry;Bard;Nature,1997

4. Long-term variations of caloric insolation resulting from the earth's orbital elements;Berger;Quat. Res.,1978

5. Mediterranean sapropel formation, dynamic and climatic viewpoints;Béthoux;Oceanol. Acta,1993

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