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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Bibliographische Detailangaben
Hauptverfasser: Pöppelmeier, Frerk (VerfasserIn) , Blaser, Patrick (VerfasserIn) , Lippold, Jörg (VerfasserIn)
Dokumenttyp: Article (Journal)
Sprache:Englisch
Veröffentlicht: 31 May 2018
In: Paleoceanography and paleoclimatology
Year: 2018, Jahrgang: 33, Heft: 5, Pages: 530-543
ISSN:2572-4525
DOI:10.1029/2017PA003290
Online-Zugang:Verlag, lizenzpflichtig, Volltext: https://doi.org/10.1029/2017PA003290
Verlag, lizenzpflichtig, Volltext: https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2017PA003290
Volltext
Verfasserangaben:F. Pöppelmeier, M. Gutjahr, P. Blaser, L.D. Keigwin, and J. Lippold

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