The mid-Pleistocene transition in the subtropical southwest Pacific

Reconstructions of subtropical southwest Pacific climate variability over the Pleistocene were derived from coupled planktic foraminiferal δ18O-Mg/Ca measurements taken from a southern Coral Sea sediment core. A clear shift from ∼40 kyr to ∼100 kyr m

Bibliographic Details
Published in:Paleoceanography
Main Authors: Russon, T., Elliot, M., Sadekov, A., Cabioch, Guy, Correge, T., De Deckker, Patrick
Format: Article in Journal/Newspaper
Language:unknown
Published: American Geophysical Union
Subjects:
Keywords: air-sea interaction
climate forcing
climate variation
glacial-interglacial cycle
greenhouse gas
hydrological cycle
paleoceanography
paleoclimate
planktonic foraminifera
Pleistocene
reconstruction
sea surface temperature
sediment core
Coral Se
Pacific
Planktonic foraminifera
Online Access:http://hdl.handle.net/1885/68488
https://doi.org/10.1029/2010PA002019
https://openresearch-repository.anu.edu.au/bitstream/1885/68488/5/The_mid-Pleistocene_transition_in_the_subtropical_southwest_Pacific.pdf.jpg
https://openresearch-repository.anu.edu.au/bitstream/1885/68488/7/01_Russon_The_mid-Pleistocene_transition_2011.pdf.jpg
Description
Summary:Reconstructions of subtropical southwest Pacific climate variability over the Pleistocene were derived from coupled planktic foraminiferal δ18O-Mg/Ca measurements taken from a southern Coral Sea sediment core. A clear shift from ∼40 kyr to ∼100 kyr m

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