Deep-water mass source and dynamic associated with rapid climatic variations during the last glacial stage in the North Atlantic: A multiproxy investigation of the detrital fraction of deep-sea sediments-Reference-Cited by-同舟云学术

Deep-water mass source and dynamic associated with rapid climatic variations during the last glacial stage in the North Atlantic: A multiproxy investigation of the detrital fraction of deep-sea sediments

Published:2006-02 Issue:2 Volume:7 Page:n/a-n/a
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Ballini M.¹,Kissel C.¹,Colin C.²,Richter T.³

Affiliation:

1. Laboratoire des Sciences du Climat et de l'Environnement; Unité Mixte CEA/CNRS; Avenue de la Terrasse,; F-91198; Gif-sur-Yvette Cedex; France

2. Laboratoire Interactions et Dynamique des Environnements de Surface; Université de Paris XI; F-91405; Orsay Cedex; France

3. Royal Netherlands Institute for Sea Research; 1790 AB; Den Burg; Netherlands

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference59 articles.

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3. Mineralogy of the clay-sized fractions of some North Atlantic-Arctic ocean bottom sediments;Berry;Geol. Soc. Am. Bull.,1966

4. Mineralogy and sedimentation of the recent deep-sea clay in the Atlantic Ocean and adjacent seas and oceans;Biscaye;Geol. Soc. Am. Bull.,1965

5. Correlation between climate records from North Atlantic sediments and Greenland ice;Bond;Nature,1993

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