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
|Collections||ANU Research Publications|
|01_Russon_The_mid-Pleistocene_transition_2011.pdf||3.69 MB||Adobe PDF||Request a copy|
Items in Open Research are protected by copyright, with all rights reserved, unless otherwise indicated.