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Centennial-scale evolution of Dansgaard-Oeschger events in the northeast Atlantic Ocean between 39.5 and 56.5 ka B.P

Abstract:

There is much uncertainty surrounding the mechanisms that forced the abrupt climate fluctuations found in many palaeoclimate records during Marine Isotope Stage (MIS)-3. One of the processes thought to be involved in these events is the Atlantic Meridional Overturning Circulation (MOC), which exhibited large changes in its dominant mode throughout the last glacial period. Giant piston core MD95-2006 from the northeast Atlantic Ocean records a suite of palaeoceanographic proxies related to the...

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Publisher copy:
10.1029/2008PA001595

Authors


Journal:
Paleoceanography
Volume:
23
Issue:
3
Pages:
n/a-n/a
Publication date:
2008-09-05
DOI:
ISSN:
0883-8305
URN:
uuid:9de6e900-4323-4cdb-81ee-21f681e8d1c7
Source identifiers:
383760
Local pid:
pubs:383760
Language:
English

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