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...
Published in: | Journal of Quaternary Science |
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Format: | Article in Journal/Newspaper |
Language: | English |
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John Wiley & Sons
2006
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Online Access: | https://espace.library.uq.edu.au/view/UQ:81907 |
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ftunivqespace:oai:espace.library.uq.edu.au:UQ:81907 2023-05-15T16:39:17+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, C. S. M. Haberle, S. Fink, D. Kershaw, A. P. Barbetti, M. Barrows, T. T. Black, M. Cohen, T. J. Correge, T. Hesse, P. P. Hua, Q. Johnstone, R. Morgan, V. Moss, P. Nanson, G. van Ommen,T. Rule, S. Williams, N. J. Zhao,J.-X. D'Costa, D. Feng, Y. -X. Gagan, M. Mooney, S. Xia, Q. 2006-01-01 https://espace.library.uq.edu.au/view/UQ:81907 eng eng John Wiley & Sons doi:10.1002/jqs.1073 issn:0267-8179 issn:1099-1417 orcid:0000-0003-1546-9242 orcid:0000-0002-2413-6178 orcid:0000-0002-2944-9632 orcid:0000-0002-8279-323X Paleontology Bipolar Seesaw High-precision Radiocarbon Dating Last Glacial-interglacial Transition (lgit) Lateglacial Interstadial Thermohaline Circulation Younger Dryas Stadial Sea surface Temperatures Southwest Pacific-ocean Abrupt Climate-change Franz-josef glacier Younger Dryas New Zealand Southern-hemisphere North atlantic Late Pleistocene Simpson Desert Geosciences Multidisciplinary 260114 Geomorphology 260304 Inorganic Geochemistry not elsewhere classified 780102 Physical sciences 040308 Palaeontology (incl.Palynology) 040606 Quaternary Environments 060206 Palaeoecology Journal Article 2006 ftunivqespace https://doi.org/10.1002/jqs.1073 2020-12-14T23:23:05Z 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. Copyright (c) 2006 John Wiley & Sons, Ltd. Article in Journal/Newspaper ice core North Atlantic The University of Queensland: UQ eSpace New Zealand Pacific Journal of Quaternary Science 21 7 751 761 |
institution |
Open Polar |
collection |
The University of Queensland: UQ eSpace |
op_collection_id |
ftunivqespace |
language |
English |
topic |
Paleontology Bipolar Seesaw High-precision Radiocarbon Dating Last Glacial-interglacial Transition (lgit) Lateglacial Interstadial Thermohaline Circulation Younger Dryas Stadial Sea surface Temperatures Southwest Pacific-ocean Abrupt Climate-change Franz-josef glacier Younger Dryas New Zealand Southern-hemisphere North atlantic Late Pleistocene Simpson Desert Geosciences Multidisciplinary 260114 Geomorphology 260304 Inorganic Geochemistry not elsewhere classified 780102 Physical sciences 040308 Palaeontology (incl.Palynology) 040606 Quaternary Environments 060206 Palaeoecology |
spellingShingle |
Paleontology Bipolar Seesaw High-precision Radiocarbon Dating Last Glacial-interglacial Transition (lgit) Lateglacial Interstadial Thermohaline Circulation Younger Dryas Stadial Sea surface Temperatures Southwest Pacific-ocean Abrupt Climate-change Franz-josef glacier Younger Dryas New Zealand Southern-hemisphere North atlantic Late Pleistocene Simpson Desert Geosciences Multidisciplinary 260114 Geomorphology 260304 Inorganic Geochemistry not elsewhere classified 780102 Physical sciences 040308 Palaeontology (incl.Palynology) 040606 Quaternary Environments 060206 Palaeoecology Turney, C. S. M. Haberle, S. Fink, D. Kershaw, A. P. Barbetti, M. Barrows, T. T. Black, M. Cohen, T. J. Correge, T. Hesse, P. P. Hua, Q. Johnstone, R. Morgan, V. Moss, P. Nanson, G. 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 |
Paleontology Bipolar Seesaw High-precision Radiocarbon Dating Last Glacial-interglacial Transition (lgit) Lateglacial Interstadial Thermohaline Circulation Younger Dryas Stadial Sea surface Temperatures Southwest Pacific-ocean Abrupt Climate-change Franz-josef glacier Younger Dryas New Zealand Southern-hemisphere North atlantic Late Pleistocene Simpson Desert Geosciences Multidisciplinary 260114 Geomorphology 260304 Inorganic Geochemistry not elsewhere classified 780102 Physical sciences 040308 Palaeontology (incl.Palynology) 040606 Quaternary Environments 060206 Palaeoecology |
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. Copyright (c) 2006 John Wiley & Sons, Ltd. |
format |
Article in Journal/Newspaper |
author |
Turney, C. S. M. Haberle, S. Fink, D. Kershaw, A. P. Barbetti, M. Barrows, T. T. Black, M. Cohen, T. J. Correge, T. Hesse, P. P. Hua, Q. Johnstone, R. Morgan, V. Moss, P. Nanson, G. 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, C. S. M. Haberle, S. Fink, D. Kershaw, A. P. Barbetti, M. Barrows, T. T. Black, M. Cohen, T. J. Correge, T. Hesse, P. P. Hua, Q. Johnstone, R. Morgan, V. Moss, P. Nanson, G. 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, C. S. M. |
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 |
John Wiley & Sons |
publishDate |
2006 |
url |
https://espace.library.uq.edu.au/view/UQ:81907 |
geographic |
New Zealand Pacific |
geographic_facet |
New Zealand Pacific |
genre |
ice core North Atlantic |
genre_facet |
ice core North Atlantic |
op_relation |
doi:10.1002/jqs.1073 issn:0267-8179 issn:1099-1417 orcid:0000-0003-1546-9242 orcid:0000-0002-2413-6178 orcid:0000-0002-2944-9632 orcid:0000-0002-8279-323X |
op_doi |
https://doi.org/10.1002/jqs.1073 |
container_title |
Journal of Quaternary Science |
container_volume |
21 |
container_issue |
7 |
container_start_page |
751 |
op_container_end_page |
761 |
_version_ |
1766029616368058368 |