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

Please use this identifier to cite or link to this item: http://hdl.handle.net/1959.14/6570

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Title
Integration of ice-core, marine and terrestrial records for the Australian Last Glacial Maximum and Termination : a contribution from the OZ INTIMATE group
Related
Journal of quaternary science, Vol. 21, Issue 7, p. 751-761
DOI
10.1002/jqs.1073
Publisher
John Wiley and Sons
Date
2006
Author/Creator
Turney, C. S. M
Author/Creator
Haberle, S
Author/Creator
Hua, Q
Author/Creator
Johnston, R
Author/Creator
Morgan, V
Author/Creator
Moss, P
Author/Creator
Nanson, G
Author/Creator
van Ommen, T
Author/Creator
Rule, S
Author/Creator
Williams, N. J
Author/Creator
Zhao, J.-X
Author/Creator
D'Costa, D
Author/Creator
Fink, D
Author/Creator
Feng, Y.-X
Author/Creator
Gagan, M
Author/Creator
Mooney, S
Author/Creator
Xia, Q
Author/Creator
Kershaw, A. P
Author/Creator
Barbetti, M
Author/Creator
Barrows, T. T
Author/Creator
Black, M
Author/Creator
Cohen, T. J
Author/Creator
Correge, T
Author/Creator
Hesse, P. P
Description
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 conflicting evidence for the degree of hemispheric teleconnection and an unresolved debate as to the principle forcing mechanism(s). The available hypotheses are difficult to test robustly, however, because the few detailed palaeoclimatic records in the Southern Hemisphere are widely dispersed and lack duplication. Here we present climatic and environmental reconstructions from across Australia, a key region of the Southern Hemisphere because of the range of environments it covers and the potentially important role regional atmospheric and oceanic controls play in global climate change. We identify a general scheme of events for the end of the last glacial period and early Holocene but a detailed reconstruction proved problematic. Significant progress in climate quantification and geochronological control is now urgently required to robustly investigate change through this period.
Description
11 page(s)
Subject Keyword
bipolar seesaw
Subject Keyword
high-precision radiocarbon dating
Subject Keyword
last glacial-interglacial transition (LGIT)
Subject Keyword
Lateglacial Interstadial
Subject Keyword
thermohaline circulation
Subject Keyword
Younger Dryas Stadial
Resource Type
journal article
Organisation
Macquarie University. Dept. of Physical Geography

Identifier
http://hdl.handle.net/1959.14/6570
Identifier
ISSN:1099-1417
Identifier
mq-rm-2006003385
Language
eng
Reviewed
Reviewed
Save/E-mail Citation
Citation Format
E-mail Address
Subject
"Journal of quaternary science"
 
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