Rapid changes in the oceanic fronts in the Norwegian Sea during the last deglaciation: implications for the Younger Dryas cooling event

Author:

Klitgaard-Kristensen D,Rasmussen T.L,Sejrup H.P,Haflidason H,van Weering Tj.C.E

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology,Oceanography

Reference31 articles.

1. The 14C age of the Icelandic Vedde ash: implications for the Younger Dryas marine reservoir correction;Austin;Radiocarbon,1995

2. The North Atlantic atmosphere–sea surface 14C gradient during the Younger Dryas climatic event;Bard;Earth Planet. Sci. Lett.,1994

3. Bé, A.W.H., Tolderlund, D.S., 1971. Distribution and ecology of living planktic foraminifera in surface waters of the Atlantic and Indian Oceans. In: Funnell, B.M., Riedel, W.R. (Eds.), The Micropaleontology of the Oceans. Cambridge University Press, Cambridge, pp. 105–149.

4. Younger Dryas episode: ice collapse and super-fjord heat pump. In: Troelstra, S.R., van Hinte, J.E., Ganssen, G.M. (Eds.), The Younger Dryas;Berger;R. Dutch Acad. Sci. Proc., Nat. Sci.,1995

5. New radiocarbon dates for the Vedde ash and the Saksurnavatn Ash from Western Norway;Birks;Quat. Res.,1996

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