Changes in the vertical structure of the North Atlantic Ocean between glacial and modern times

The distribution of planktic foraminiferal δ 18O over the North Atlantic Ocean has been interpreted by Duplessy et al. (1991, 1992) in terms of the distribution of surface water salinity during the last glacial maximum (LGM) and the Younger Dryas (YD). We present here the implications of this surfac...

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Veröffentlicht in:	Quaternary science reviews 1992, Vol.11 (4), p.401-413
Hauptverfasser:	Labeyrie, Laurent D., Duplessy, Jean-Claude, Duprat, Josette, Juillet-Leclerc, Anne, Moyes, Jean, Michel, Elizabeth, Kallel, Nejib, Shackleton, Nicholas J.
Format:	Artikel
Sprache:	eng
Schlagworte:	Continental interfaces, environment Earth sciences Earth, ocean, space Exact sciences and technology Geochronology Isotope geochemistry. Geochronology Marine and continental quaternary Ocean, Atmosphere Sciences of the Universe Surficial geology
Online-Zugang:	Volltext
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