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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last deglaciation
Younger Dryas
Last Glacial Maximum
water depth
climate change
pistons
ocean
oceans
water
cold

Cite this

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title = "Southwest Pacific modulation of abrupt climate change during the Antarctic Cold Reversal - Younger Dryas",
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",
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Southwest Pacific modulation of abrupt climate change during the Antarctic Cold Reversal - Younger Dryas. / Carter, L.; Manighetti, B.; Ganssen, G.M.

In: Palaeogeography, Palaeoclimatology, Palaeoecology, Vol. 260, No. 1-2, 2008, p. 284-298.

Research output: Contribution to JournalArticleAcademicpeer-review

TY - JOUR

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AU - Manighetti, B.

AU - Ganssen, G.M.

PY - 2008

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N2 - 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

AB - 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

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DO - 10.1016/j.palaeo.2007.08.013

M3 - Article

VL - 260

SP - 284

EP - 298

JO - Palaeogeography, Palaeoclimatology, Palaeoecology

JF - Palaeogeography, Palaeoclimatology, Palaeoecology

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