A modern view on brine formation in relation to low δ18O signals

Deep water formation may be triggered by the density effect of brines that are released during sea-ice formation. But are sea-ice related brines also a likely mechanism to transport low δ18O signals into deep and bottom waters? Glacial foraminiferal δ18O records in the Nordic seas, covering the peri...

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Bibliographic Details
Main Author: Bauch, Dorothea
Format: Conference Object
Language:unknown
Published: PAGES, International Project Office; University of Bern, Oeschger Centre 2013
Subjects:
Arctic
Arctic Ocean
Barents Sea
Dokken
Meland
Rasmussen
Thomsen
Foraminifera*
Kara-Laptev
laptev
Nordic Seas
Sea ice
Online Access:https://oceanrep.geomar.de/id/eprint/22201/

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