Articles | Volume 13, issue 6
https://doi.org/10.5194/cp-13-667-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue:
https://doi.org/10.5194/cp-13-667-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
14 Jun 2017
Research article |
| 14 Jun 2017
Hydroclimate of the Last Glacial Maximum and deglaciation in southern Australia's arid margin interpreted from speleothem records (23–15 ka)
Pauline C. Treble
CORRESPONDING AUTHOR
Australian Nuclear Science and Technology Organisation, Lucas Heights 2234 NSW, Australia
Connected Waters Initiative Research Centre, UNSW Australia, Kensington 2052 NSW, Australia
Andy Baker
Connected Waters Initiative Research Centre, UNSW Australia, Kensington 2052 NSW, Australia
Linda K. Ayliffe
Research School of Earth Sciences, Australian National University, Canberra ACT 0200, Australia
Timothy J. Cohen
School of Earth and Environmental Sciences, University of Wollongong, Wollongong NSW 2522, Australia
John C. Hellstrom
School of Earth Sciences, University of Melbourne, Parkville VIC 3052, Australia
Michael K. Gagan
Research School of Earth Sciences, Australian National University, Canberra ACT 0200, Australia
Silvia Frisia
School of Environmental and Life Science, University of Newcastle, Callaghan NSW 2308, Australia
Russell N. Drysdale
School of Geography, University of Melbourne, Parkville VIC 3052, Australia
Alan D. Griffiths
Australian Nuclear Science and Technology Organisation, Lucas Heights 2234 NSW, Australia
Andrea Borsato
School of Environmental and Life Science, University of Newcastle, Callaghan NSW 2308, Australia
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- Last Glacial Maximum cooling induced positive moisture balance and maintained stable human populations in Australia H. Cadd et al. 10.1038/s43247-024-01204-1
- Comment on “Uranium series dating of Great Artesian Basin travertine deposits: Implications for palaeohydrogeology and palaeoclimate” by Priestley et al. (2018) I. Uysal et al. 10.1016/j.palaeo.2019.109420
- Evaluating model outputs using integrated global speleothem records of climate change since the last glacial L. Comas-Bru et al. 10.5194/cp-15-1557-2019
- A continental perspective on the timing of environmental change during the last glacial stage in Australia H. Cadd et al. 10.1017/qua.2021.16
- Elevated Southern Hemisphere moisture availability during glacial periods R. Weij et al. 10.1038/s41586-023-06989-3
- Hydro-climatic variability in the southwestern Indian Ocean between 6000 and 3000 years ago H. Li et al. 10.5194/cp-14-1881-2018
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- Last Glacial Maximum climate and atmospheric circulation over the Australian region from climate models Y. Du et al. 10.5194/cp-20-393-2024
- A 35 ka record of groundwater recharge in south-west Australia using stable water isotopes S. Priestley et al. 10.1016/j.scitotenv.2019.135105
- Insights into the pre-European mammalian fauna of the southern Flinders Ranges, South Australia N. Liddle et al. 10.1071/AM17035
- RADIOCARBON PROTOCOLS AND FIRST INTERCOMPARISON RESULTS FROM THE CHRONOS 14CARBON-CYCLE FACILITY, UNIVERSITY OF NEW SOUTH WALES, SYDNEY, AUSTRALIA C. Turney et al. 10.1017/RDC.2021.23
- A Review of Speleothems as Archives for Paleofire Proxies, With Australian Case Studies M. Campbell et al. 10.1029/2022RG000790
- Late Quaternary Climate Variability and Change from Aotearoa New Zealand Speleothems: Progress in Age Modelling, Oxygen Isotope Master Record Construction and Proxy-Model Comparisons A. Lorrey et al. 10.3390/quat3030024
- The influence of fluid inclusions, organics, and calcite fabric on trace element distributions in stalagmites O. Kost et al. 10.3389/feart.2023.1240888
- An extended last glacial maximum in the Southern Hemisphere: A contribution to the SHeMax project L. Petherick et al. 10.1016/j.earscirev.2022.104090
- The SISAL database: a global resource to document oxygen and carbon isotope records from speleothems K. Atsawawaranunt et al. 10.5194/essd-10-1687-2018
- Relationships between climate change, human environmental impact, and megafaunal extinction inferred from a 4000-year multi-proxy record from a stalagmite from northwestern Madagascar L. Railsback et al. 10.1016/j.quascirev.2020.106244
- Main controls on the stable carbon isotope composition of speleothems J. Fohlmeister et al. 10.1016/j.gca.2020.03.042
- Stalagmite evidence of Last Glacial Maximum to early Holocene climate variability in southwestern Iran M. SOLEIMANI et al. 10.1002/jqs.3478
- A giant raptor (Aves: Accipitridae) from the Pleistocene of southern Australia E. Mather et al. 10.1007/s10336-023-02055-x
- Multi-proxy validation of glacial-interglacial rainfall variations in southwest Sulawesi A. Kimbrough et al. 10.1038/s43247-023-00873-8
- Uranium series dating of Great Artesian Basin travertine deposits: Implications for palaeohydrogeology and palaeoclimate S. Priestley et al. 10.1016/j.palaeo.2017.10.024
- Luminescence dating of Quaternary alluvial successions, Sellicks Creek, South Mount Lofty Ranges, southern Australia R. Bourman et al. 10.1080/08120099.2020.1722967
- A multi-proxy climate record from a northwestern Botswana stalagmite suggesting wetness late in the Little Ice Age (1810–1820 CE) and drying thereafter in response to changing migration of the tropical rain belt or ITCZ L. Railsback et al. 10.1016/j.palaeo.2018.06.029
- Palaeohydrology of lowland rivers in the Murray-Darling Basin, Australia P. Hesse et al. 10.1016/j.quascirev.2018.09.035
- Sedimentary unknowns constrain the current use of frequency analysis of radiocarbon data sets in forming regional models of demographic change I. Ward & P. Larcombe 10.1002/gea.21837
- Millennial-scale variability in south-east Australian hydroclimate between 30,000 and 10,000 years ago G. Falster et al. 10.1016/j.quascirev.2018.05.031
26 citations as recorded by crossref.
- Last Glacial Maximum cooling induced positive moisture balance and maintained stable human populations in Australia H. Cadd et al. 10.1038/s43247-024-01204-1
- Comment on “Uranium series dating of Great Artesian Basin travertine deposits: Implications for palaeohydrogeology and palaeoclimate” by Priestley et al. (2018) I. Uysal et al. 10.1016/j.palaeo.2019.109420
- Evaluating model outputs using integrated global speleothem records of climate change since the last glacial L. Comas-Bru et al. 10.5194/cp-15-1557-2019
- A continental perspective on the timing of environmental change during the last glacial stage in Australia H. Cadd et al. 10.1017/qua.2021.16
- Elevated Southern Hemisphere moisture availability during glacial periods R. Weij et al. 10.1038/s41586-023-06989-3
- Hydro-climatic variability in the southwestern Indian Ocean between 6000 and 3000 years ago H. Li et al. 10.5194/cp-14-1881-2018
- Control of insolation on stalagmite growth, rainfall, and migration of the tropical rain belt in northern Namibia over the last 100 kyr, as suggested by a rare MIS 5b-5c stalagmite from Dante Cave L. Railsback et al. 10.1016/j.palaeo.2019.109348
- Last Glacial Maximum climate and atmospheric circulation over the Australian region from climate models Y. Du et al. 10.5194/cp-20-393-2024
- A 35 ka record of groundwater recharge in south-west Australia using stable water isotopes S. Priestley et al. 10.1016/j.scitotenv.2019.135105
- Insights into the pre-European mammalian fauna of the southern Flinders Ranges, South Australia N. Liddle et al. 10.1071/AM17035
- RADIOCARBON PROTOCOLS AND FIRST INTERCOMPARISON RESULTS FROM THE CHRONOS 14CARBON-CYCLE FACILITY, UNIVERSITY OF NEW SOUTH WALES, SYDNEY, AUSTRALIA C. Turney et al. 10.1017/RDC.2021.23
- A Review of Speleothems as Archives for Paleofire Proxies, With Australian Case Studies M. Campbell et al. 10.1029/2022RG000790
- Late Quaternary Climate Variability and Change from Aotearoa New Zealand Speleothems: Progress in Age Modelling, Oxygen Isotope Master Record Construction and Proxy-Model Comparisons A. Lorrey et al. 10.3390/quat3030024
- The influence of fluid inclusions, organics, and calcite fabric on trace element distributions in stalagmites O. Kost et al. 10.3389/feart.2023.1240888
- An extended last glacial maximum in the Southern Hemisphere: A contribution to the SHeMax project L. Petherick et al. 10.1016/j.earscirev.2022.104090
- The SISAL database: a global resource to document oxygen and carbon isotope records from speleothems K. Atsawawaranunt et al. 10.5194/essd-10-1687-2018
- Relationships between climate change, human environmental impact, and megafaunal extinction inferred from a 4000-year multi-proxy record from a stalagmite from northwestern Madagascar L. Railsback et al. 10.1016/j.quascirev.2020.106244
- Main controls on the stable carbon isotope composition of speleothems J. Fohlmeister et al. 10.1016/j.gca.2020.03.042
- Stalagmite evidence of Last Glacial Maximum to early Holocene climate variability in southwestern Iran M. SOLEIMANI et al. 10.1002/jqs.3478
- A giant raptor (Aves: Accipitridae) from the Pleistocene of southern Australia E. Mather et al. 10.1007/s10336-023-02055-x
- Multi-proxy validation of glacial-interglacial rainfall variations in southwest Sulawesi A. Kimbrough et al. 10.1038/s43247-023-00873-8
- Uranium series dating of Great Artesian Basin travertine deposits: Implications for palaeohydrogeology and palaeoclimate S. Priestley et al. 10.1016/j.palaeo.2017.10.024
- Luminescence dating of Quaternary alluvial successions, Sellicks Creek, South Mount Lofty Ranges, southern Australia R. Bourman et al. 10.1080/08120099.2020.1722967
- A multi-proxy climate record from a northwestern Botswana stalagmite suggesting wetness late in the Little Ice Age (1810–1820 CE) and drying thereafter in response to changing migration of the tropical rain belt or ITCZ L. Railsback et al. 10.1016/j.palaeo.2018.06.029
- Palaeohydrology of lowland rivers in the Murray-Darling Basin, Australia P. Hesse et al. 10.1016/j.quascirev.2018.09.035
- Sedimentary unknowns constrain the current use of frequency analysis of radiocarbon data sets in forming regional models of demographic change I. Ward & P. Larcombe 10.1002/gea.21837
Discussed (final revised paper)
Discussed (preprint)
Latest update: 18 Apr 2024
Short summary
Little is known about the climate of southern Australia during the Last Glacial Maximum and deglaciation owing to sparse records for this region. We present the first high-resolution data, derived from speleothems that grew 23–5 ka. It appears that recharge to the Flinders Ranges was higher than today, particularly during 18.9–15.8 ka, argued to be due to the enhanced availability of tropical moisture. An abrupt shift to aridity is recorded at 15.8 ka, associated with restored westerly airflow.
Little is known about the climate of southern Australia during the Last Glacial Maximum and...
