Architecture of N orth A tlantic contourite drifts modified by transient circulation of the I celandic mantle plume-Reference-Cited by-同舟云学术

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Architecture of N orth A tlantic contourite drifts modified by transient circulation of the I celandic mantle plume

Published:2015-10 Issue:10 Volume:16 Page:3414-3435
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Parnell‐Turner Ross¹²,White Nicholas J.¹,McCave I. Nick¹,Henstock Timothy J.³,Murton Bramley³,Jones Stephen M.⁴

Affiliation:

1. Department of Earth SciencesUniversity of CambridgeCambridge UK

2. Now at Woods Hole Oceanographic InstitutionWoods Hole Massachusetts USA

3. National Oceanography Centre, University of Southampton, Waterfront Campus, European WaySouthampton UK

4. School of Geography, Earth and Environmental SciencesUniversity of BirminghamBirmingham UK

Funder

Natural Environment Research Council

The University of Cambridge Girdler Fund

BP Exploration

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2015GC005947

Reference74 articles.

1. Arthur M. A. S. P.Srivastava M.Kaminski R.Jarrard andJ.Osler(1989) Seismic stratigraphy and history of deep circulation and sediment drift development in Baffin Bay and the Labrador Sea inProceedings of Ocean Drilling Program Science Results vol. 105 edited by S. P. Srivastava et al. pp.957–988 Ocean Drill. Program College Station Tex.

2. Final closure of Panama and the onset of northern hemisphere glaciation

3. Atmospheric CO 2 decline during the Pliocene intensification of Northern Hemisphere glaciations

4. Hydrography and sedimentation under the deep western boundary current on Björn and Gardar Drifts, Iceland Basin

5. Deep Circulation of the North Atlantic over the Last 200,000 Years: Geochemical Evidence

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