Subarctic Front migration at the Reykjanes Ridge during the mid- to late Holocene: evidence from planktic foraminifera-Reference-Cited by-同舟云学术

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Subarctic Front migration at the Reykjanes Ridge during the mid- to late Holocene: evidence from planktic foraminifera

Published:2017-05-29 Issue:1 Volume:47 Page:175-188
ISSN:0300-9483
Container-title:Boreas
language:en
Short-container-title:Boreas

Author:

Perner Kerstin¹²^ORCID,Moros Matthias¹,Jansen Eystein²,Kuijpers Antoon³,Troelstra Simon R.⁴,Prins MAARTIN A.⁴

Affiliation:

1. Department of Marine Geology; Leibniz Institute for Baltic Sea Research; Rostock Germany

2. Department of Earth Science and Bjerknes Centre for Climate Research; University of Bergen; Allégaten 41 Bergen 5055 Norway

3. Geological Survey of Denmark and Greenland; Øster Voldgade 10 Copenhagen DK-1350 Denmark

4. Faculty of Earth and Life Sciences; Vrije Universiteit; de Boelelaan 1085 Amsterdam 1081HV The Netherlands

Funder

Deutsche Forschungsgemeinschaft

European Research Council

Publisher

Wiley

Subject

Geology,Archaeology,Ecology, Evolution, Behavior and Systematics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/bor.12263/fullpdf

Reference116 articles.

1. Nonuniform response of the major surface currents in the Nordic Seas to insolation forcing: implications for the Holocene climate variability;Andersen;Paleoceanography,2004a

2. A highly unstable Holocene climate in the subpolar north Atlantic: evidence from diatoms;Andersen;Quaternary Science Reviews,2004b

3. Holocene trends in the foraminifer record from the Norwegian Sea and the North Atlantic Ocean;Andersson;Climate of the Past,2010

4. Mid- to late-Holocene oceanographic variability on the Southeast Greenland shelf;Andresen;The Holocene,2013

5. Multi-proxy records showing significant Holocene environmental variability: the inner N. Iceland shelf (Hunafloi);Andrews;Quaternary Science Reviews,2003

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