In:
Geophysical Research Letters, American Geophysical Union (AGU), Vol. 44, No. 22 ( 2017-11-28)
Abstract:
At the onset of the Last Interglacial, δ 18 O of Globorotalia inflata remains close to glacial values for ~7 kyr High δ 18 O at the onset of the Last Interglacial can be explained by the existence of a colder and/or saltier South Atlantic thermocline A colder thermocline may have resulted from the North Atlantic heat piracy, following the resumption of deepwater convection from ~129 ka
Type of Medium:
Online Resource
ISSN:
0094-8276
,
1944-8007
DOI:
10.1002/2017GL074457
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2017
detail.hit.zdb_id:
2021599-X
detail.hit.zdb_id:
7403-2
SSG:
16,13
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