Reconstruction of glaciation over the past 6 Myr from ice-borne deposits in the Norwegian Sea

In a recent study, the history of high-northern-latitude glaciation over the past six Myr was deduced from records of ice-borne deposits in deep-sea sediments of the Norwegian Sea.

Saved in:
Bibliographic Details
Published inNature (London) Vol. 349; no. 6310; pp. 600 - 603
Main Authors Jansen, E, Sjøholm, J
Format Journal Article
LanguageEnglish
Published London Nature Publishing Group 14.02.1991
Subjects
Amplification
Deep sea
Deep sea sediments
Geology
Glaciation
Glaciers
Glaciology
Ice
Ice sheets
Marine
Northern Hemisphere
Oxygen
Oxygen isotopes
Prehistoric era
Sea level
Sediment deposits
Sediments
Variation
Norwegian Sea
Northern Hemisphere
Arctic region
ANE, Norwegian Sea
Online AccessGet full text

Cover

More Information
Summary:In a recent study, the history of high-northern-latitude glaciation over the past six Myr was deduced from records of ice-borne deposits in deep-sea sediments of the Norwegian Sea.
Bibliography:ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ObjectType-Article-2
ObjectType-Feature-1
ISSN:0028-0836
1476-4687
DOI:10.1038/349600a0