Articles | Volume 38, issue 2
https://doi.org/10.5194/jm-38-177-2019
https://doi.org/10.5194/jm-38-177-2019
Research article
 | 
03 Dec 2019
Research article |  | 03 Dec 2019

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

Sev Kender, Adeyinka Aturamu, Jan Zalasiewicz, Michael A. Kaminski, and Mark Williams

Viewed

Total article views: 2,460 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,936 458 66 2,460 473 45 56
  • HTML: 1,936
  • PDF: 458
  • XML: 66
  • Total: 2,460
  • Supplement: 473
  • BibTeX: 45
  • EndNote: 56
Views and downloads (calculated since 03 Dec 2019)
Cumulative views and downloads (calculated since 03 Dec 2019)

Viewed (geographical distribution)

Total article views: 2,193 (including HTML, PDF, and XML) Thereof 2,120 with geography defined and 73 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 23 Nov 2024
Download
Short summary
The Mid-Brunhes Transition saw an enigmatic shift towards increased glacial temperature variations about 400 kyr ago. High-latitude Southern Ocean stratification may have been a causal factor, but little is known of the changes to the high-latitude Bering Sea. We generated benthic foraminiferal assemblage data and are the first to document a glacial decrease in episodic primary productivity since the Mid-Brunhes Transition, signifying possible reductions in sea ice summer stratification.