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 conflicting evidence for the degree of hemisp...
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ftunivwollongong:oai:ro.uow.edu.au:scipapers-2150 2023-05-15T16:39:13+02:00 Integration of ice-core, marine and terrestrial records for the Australian Last glacial Maximum and Termination: a contribution from the OZ INTIMATE group Turney, Christian Haberle, S Fink, David Kershaw, A Peter Barbetti, M Barrows, T T Black, M Cohen, Timothy J Correge, T Hesse, P P Hua, Q Johnston, R Morgan, V Moss, P Nanson, Gerald C Van Ommen, T Rule, S Williams, N J Zhao, J -X D'Costa, D Feng, Y -X Gagan, M Mooney, S Xia, Q 2006-01-01T08:00:00Z https://ro.uow.edu.au/scipapers/1084 unknown Research Online https://ro.uow.edu.au/scipapers/1084 Faculty of Science - Papers (Archive) group oz contribution maximum glacial last australian records terrestrial marine intimate termination core integration ice GeoQUEST Life Sciences Physical Sciences and Mathematics Social and Behavioral Sciences article 2006 ftunivwollongong 2020-02-25T11:26:37Z 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.Weidentify 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. Article in Journal/Newspaper ice core University of Wollongong, Australia: Research Online |
institution |
Open Polar |
collection |
University of Wollongong, Australia: Research Online |
op_collection_id |
ftunivwollongong |
language |
unknown |
topic |
group oz contribution maximum glacial last australian records terrestrial marine intimate termination core integration ice GeoQUEST Life Sciences Physical Sciences and Mathematics Social and Behavioral Sciences |
spellingShingle |
group oz contribution maximum glacial last australian records terrestrial marine intimate termination core integration ice GeoQUEST Life Sciences Physical Sciences and Mathematics Social and Behavioral Sciences Turney, Christian Haberle, S Fink, David Kershaw, A Peter Barbetti, M Barrows, T T Black, M Cohen, Timothy J Correge, T Hesse, P P Hua, Q Johnston, R Morgan, V Moss, P Nanson, Gerald C Van Ommen, T Rule, S Williams, N J Zhao, J -X D'Costa, D Feng, Y -X Gagan, M Mooney, S Xia, Q Integration of ice-core, marine and terrestrial records for the Australian Last glacial Maximum and Termination: a contribution from the OZ INTIMATE group |
topic_facet |
group oz contribution maximum glacial last australian records terrestrial marine intimate termination core integration ice GeoQUEST Life Sciences Physical Sciences and Mathematics Social and Behavioral Sciences |
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.Weidentify 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. |
format |
Article in Journal/Newspaper |
author |
Turney, Christian Haberle, S Fink, David Kershaw, A Peter Barbetti, M Barrows, T T Black, M Cohen, Timothy J Correge, T Hesse, P P Hua, Q Johnston, R Morgan, V Moss, P Nanson, Gerald C Van Ommen, T Rule, S Williams, N J Zhao, J -X D'Costa, D Feng, Y -X Gagan, M Mooney, S Xia, Q |
author_facet |
Turney, Christian Haberle, S Fink, David Kershaw, A Peter Barbetti, M Barrows, T T Black, M Cohen, Timothy J Correge, T Hesse, P P Hua, Q Johnston, R Morgan, V Moss, P Nanson, Gerald C Van Ommen, T Rule, S Williams, N J Zhao, J -X D'Costa, D Feng, Y -X Gagan, M Mooney, S Xia, Q |
author_sort |
Turney, Christian |
title |
Integration of ice-core, marine and terrestrial records for the Australian Last glacial Maximum and Termination: a contribution from the OZ INTIMATE group |
title_short |
Integration of ice-core, marine and terrestrial records for the Australian Last glacial Maximum and Termination: a contribution from the OZ INTIMATE group |
title_full |
Integration of ice-core, marine and terrestrial records for the Australian Last glacial Maximum and Termination: a contribution from the OZ INTIMATE group |
title_fullStr |
Integration of ice-core, marine and terrestrial records for the Australian Last glacial Maximum and Termination: a contribution from the OZ INTIMATE group |
title_full_unstemmed |
Integration of ice-core, marine and terrestrial records for the Australian Last glacial Maximum and Termination: a contribution from the OZ INTIMATE group |
title_sort |
integration of ice-core, marine and terrestrial records for the australian last glacial maximum and termination: a contribution from the oz intimate group |
publisher |
Research Online |
publishDate |
2006 |
url |
https://ro.uow.edu.au/scipapers/1084 |
genre |
ice core |
genre_facet |
ice core |
op_source |
Faculty of Science - Papers (Archive) |
op_relation |
https://ro.uow.edu.au/scipapers/1084 |
_version_ |
1766029542265192448 |