TY - JOUR
T1 - Southwest Pacific modulation of abrupt climate change during the Antarctic Cold Reversal - Younger Dryas
AU - Carter, L.
AU - Manighetti, B.
AU - Ganssen, G.M.
PY - 2008
Y1 - 2008
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
U2 - 10.1016/j.palaeo.2007.08.013
DO - 10.1016/j.palaeo.2007.08.013
M3 - Article
SN - 0031-0182
VL - 260
SP - 284
EP - 298
JO - Palaeogeography, Palaeoclimatology, Palaeoecology
JF - Palaeogeography, Palaeoclimatology, Palaeoecology
IS - 1-2
ER -