Benthic foraminifera indicate Glacial North Pacific Intermediate Water and reduced primary productivity over Bowers Ridge, Bering Sea, since the Mid-Brunhes Transition

The Mid-Brunhes Transition (MBT) saw an increase in the amplitude of glacial cycles expressed in ice core and deep ocean records from about 400 ka, but its influence on high-latitude climates is not fully understood. The Arctic Ocean is thought to have warmed and exhibited reduced sea ice, but littl...

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Bibliographic Details
Published in:Journal of Micropalaeontology
Main Authors: Kender, Sev, Aturamu, Adeyinka, Zalasiewicz, Jan, Kaminski, Michael A., Williams, Mark
Format: Text
Language:English
Published: 2019
Subjects:
Online Access:https://doi.org/10.5194/jm-38-177-2019
https://jm.copernicus.org/articles/38/177/2019/