Integration of ice-core, marine and terrestrial records for the Australian Last Glacial Maximum and Termination: a contribution from the OZ INTIMATE group

The degree to which Southern Hemisphere climatic changes during the end of the last glacial period and early Holocene (30-8 ka) were influenced or initiated by events occurring in the high latitudes of the Northern Hemisphere is a complex issue. There is

Bibliographic Details
Main Authors: Turney, Christian, Haberle, Simon, Fink, David, Kershaw, Arnold Peter, Barbetti, Mike, Barrows, Timothy, Black, M P, Cohen, Tim J, Correge, T, Hesse, Paul, Hua, Quan, Johnston, R, Morgan, V, Moss, Patrick, Nanson, G., van Ommen, Tas, Rule, S, Williams, Neal, Zhao, Jian-xin, D'Costa, D, Feng, Y-X, Gagan, Michael, Mooney, S, Xia, Q
Format: Article in Journal/Newspaper
Language:unknown
Published: Wiley-VCH Verlag GMBH 2015
Subjects:
Keywords: climate change
Holocene
ice core
Last Glacial Maximum
marine record
Northern Hemisphere
paleoclimate
paleoenvironment
Southern Hemisphere
thermohaline circulation
Australasia
Australia Bipolar seesaw
High-precision radiocarbon dating
Last glacial-interglacial transition (LGIT)
Lateglacial interstadial
Younger dryas stadial
Online Access:http://hdl.handle.net/1885/22128
Description
Summary:The degree to which Southern Hemisphere climatic changes during the end of the last glacial period and early Holocene (30-8 ka) were influenced or initiated by events occurring in the high latitudes of the Northern Hemisphere is a complex issue. There is

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