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...

Full description

Bibliographic Details
Published in:Journal of Micropalaeontology
Main Authors: S. Kender, A. Aturamu, J. Zalasiewicz, M. A. Kaminski, M. Williams
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2019
Subjects:
Online Access:https://doi.org/10.5194/jm-38-177-2019
https://doaj.org/article/8c1288e21ef64f2fb56635ba1c125494