Origin of abyssal NW atlantic water masses since the last glacial maximum

Deglacial ocean circulation changes were recorded with εNd in high resolution at the abyssal Corner Rise - Distinct contribution of Northern Component Water is detectable at the abyssal northwest

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Bibliographic Details
Main Authors: Pöppelmeier, Frerk (Author) , Blaser, Patrick (Author) , Lippold, Jörg (Author)
Format: Article (Journal)
Language:English
Published: 31 May 2018
In: Paleoceanography and paleoclimatology
Year: 2018, Volume: 33, Issue: 5, Pages: 530-543
ISSN:2572-4525
DOI:10.1029/2017PA003290
Online Access:Verlag, lizenzpflichtig, Volltext: https://doi.org/10.1029/2017PA003290
Verlag, lizenzpflichtig, Volltext: https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2017PA003290
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Author Notes:F. Pöppelmeier, M. Gutjahr, P. Blaser, L.D. Keigwin, and J. Lippold
Description
Summary:Deglacial ocean circulation changes were recorded with εNd in high resolution at the abyssal Corner Rise - Distinct contribution of Northern Component Water is detectable at the abyssal northwest
Item Description:First published: 07 May 2018
Gesehen am 23.04.2020
Physical Description:Online Resource
ISSN:2572-4525
DOI:10.1029/2017PA003290