Intermediate ocean circulation and cryosphere dynamics in the northeast Atlantic during Heinrich Stadials: benthic foraminiferal assemblage response-Reference-Cited by-同舟云学术

Intermediate ocean circulation and cryosphere dynamics in the northeast Atlantic during Heinrich Stadials: benthic foraminiferal assemblage response

Published:2022-06-14 Issue:7 Volume:37 Page:1207-1221
ISSN:0267-8179
Container-title:Journal of Quaternary Science
language:en
Short-container-title:J Quaternary Science

Author:

Depuydt Pauline¹^ORCID,Mojtahid Meryem¹,Barras Christine¹,Bouhdayad Fatima Zohra¹²,Toucanne Samuel³

Affiliation:

1. Univ Angers, Nantes Université, Le Mans Université, CNRS, UMR 6112, Laboratoire de Planétologie et Géosciences F‐49000 Angers France

2. Presently at: Institute of Geology and Mineralogy, Faculty of Mathematics and Natural Sciences University of Cologne Cologne Germany

3. Univ Brest, CNRS, Ifremer, Geo‐Ocean F‐29280 Plouzane France

Publisher

Wiley

Subject

Paleontology,Earth and Planetary Sciences (miscellaneous),Arts and Humanities (miscellaneous)

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.3444

Reference163 articles.

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2. Scaling percentages and distributional patterns of benthic Foraminifera with flux rates of organic carbon;Altenbach AV;Journal of Foraminiferal Research,1999

3. Iceberg discharges of the last glacial period driven by oceanic circulation changes

4. Identification of Heinrich Layers in core KS 01 North‐Eastern Atlantic (46 °N, 17 °W), implications for their origin. Marine Geology, Ice Rafting and Paleocengraphy of the Northeast Atlantic Ocean;Auffret GA;Selected papers presented at the 7th European Union of Geosciences,1996

5. Terrigenous fluxes at the Celtic margin during the last glacial cycle

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