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Radiometrically determined sedimentary fluxes in the sub-polar North Atlantic during the last 140,000 years

✍ Scribed by Jerry F McManus; Robert F Anderson; Wallace S Broecker; Martin Q Fleisher; Sean M Higgins


Book ID
117095262
Publisher
Elsevier Science
Year
1998
Tongue
English
Weight
665 KB
Volume
155
Category
Article
ISSN
0012-821X

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**Abstract** Changes in North Atlantic sea surface temperature (SST) are regarded as a key element of the climate during the Quaternary. However, there are relatively few long‐term records providing quantitative SST estimates from this region. Using planktic foraminiferal‐derived SSTs together with