Dynamic intermediate ocean circulation in the North Atlantic during Heinrich Stadial 1: A radiocarbon and neodymium isotope perspective-Reference-Cited by-同舟云学术

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Dynamic intermediate ocean circulation in the North Atlantic during Heinrich Stadial 1: A radiocarbon and neodymium isotope perspective

Published:2014-11 Issue:11 Volume:29 Page:1072-1093
ISSN:0883-8305
Container-title:Paleoceanography
language:en
Short-container-title:Paleoceanography

Author:

Wilson David J.¹,Crocket Kirsty C.¹²,van de Flierdt Tina¹,Robinson Laura F.³⁴,Adkins Jess F.⁵

Affiliation:

1. Department of Earth Science and Engineering; Imperial College London; London UK

2. Scottish Association for Marine Science; Scottish Marine Institute; Oban UK

3. School of Earth Sciences; University of Bristol; Bristol UK

4. Department of Marine Chemistry and Geochemistry; Woods Hole Oceanographic Institution; Woods Hole Massachusetts USA

5. Caltech Division of Geology and Planetary Sciences, MS 131-24; Pasadena California USA

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

Reference110 articles.

1. Age Screening of Deep-Sea Corals and the Record of Deep North Atlantic Circulation Change at 15.4KA

2. Deep-sea coral evidence for rapid change in ventilation of the deep North Atlantic 15,400 years ago;Adkins;Science,1998

3. Growth rates of the deep-sea scleractinia Desmophyllum cristagalli and Enallopsammia rostrata;Adkins;Earth Planet. Sci. Lett.,2004

4. Reconstructing the Nd oceanic cycle using a coupled dynamical-biogeochemical model;Arsouze;Biogeosciences,2009

5. Extreme deepening of the Atlantic overturning circulation during deglaciation;Barker;Nat. Geosci.,2010

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