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(Article of periodic en Anglais - 1995)

Document title

Deposition of organic matter in the Norwegian-Greenland Sea during the past 2.7 million years

Authors(s) and Affiliation(s)

WAGNER T. ; HÖLEMANN J.A. ;

Abstract

Variations in the amount and composition of sedimentary organic matter in glacial and interglacial deposits of the last 2.7 myr correlate with late Cenozoic climatic and oceanographic changes in the Norwegian-Greenland Sea (NGS). These variations are predominantly caused by the changing supply of terrestrial and reworked organic matter (OM). To introduce the general total organic carbon (TOC) patterns observed in NGS deposits, the AA. discuss how Quaternary glacial to interglacial climatic cycles have affected changes in the deposition of OM in the area of investigation

Source

Article of periodic

published at : Quaternary research / ISSN 0033-5894 / CODEN QRESAV

Editor : Elsevier, San Diego, CA - ETATS-UNIS (1970)

Millesime : 1995, vol. 44, no3 [pp. 355-366]

Bibliographic references : 73 ref.

Collation : Illustration ;

Language

Anglais

INIST-CNRS, Cote INIST : 15739

Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 1996.
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