Dynamics of North Atlantic Deep Water masses during the Holocene

High resolution flow speed reconstructions of two core sites located on Gardar Drift in the northeast Atlantic Basin and Orphan Knoll in the northwest Atlantic Basin reveal a long-term decrease in flow speed of Northeast Atlantic Deep Water (NEADW) after 6,500 years. Benthic foraminiferal oxygen iso...

Szczegółowa specyfikacja

Opis bibliograficzny
Główni autorzy: Hoogakker, B, Chapman, MR, McCave, I, Hillaire-Marcel, C, Ellison, C, Hall, I, Telford, R
Format: Journal article
Język:English
Wydane: 2011