Southwest Pacific modulation of abrupt climate change during the Antarctic Cold Reversal - Younger Dryas

L. Carter, B. Manighetti, G.M. Ganssen

Research output: Contribution to JournalArticleAcademicpeer-review

Abstract

The giant piston core, MD97-2121 (2314-m water depth), collected north of the Subtropical Front, New Zealand, provides a well-dated, stable isotopic record of subtropical and sub-Antarctic influences on the surface and deep ocean over the last deglaciation, especially during the Antarctic Cold Reversal (ACR; ~ 14.1-12.4 ka) and Younger Dryas (YD; 13.0-11.5 ka). After the Last Glacial Maximum, benthic foraminiferal δ
Original languageEnglish
Pages (from-to)284-298
JournalPalaeogeography, Palaeoclimatology, Palaeoecology
Volume260
Issue number1-2
DOIs
Publication statusPublished - 2008

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