Articles | Volume 12, issue 7
https://doi.org/10.5194/cp-12-1435-2016
© Author(s) 2016. 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-12-1435-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
05 Jul 2016
Research article |
| 05 Jul 2016
Constant wind regimes during the Last Glacial Maximum and early Holocene: evidence from Little Llangothlin Lagoon, New England Tablelands, eastern Australia
James Shulmeister
CORRESPONDING AUTHOR
School of Geography, Planning and Environmental Management, University of
Queensland, St. Lucia 4072, Queensland, Australia
Justine Kemp
Australian Rivers Institute, Griffith University, Nathan 4111, Queensland,
Australia
Kathryn E. Fitzsimmons
Department of Human Evolution, Max Planck Institute for Evolutionary
Anthropology, Deutscher Platz 6, 04103 Leipzig, Germany
Allen Gontz
School for the Environment, University of Massachusetts Boston, Boston, MA
02125, USA
current address: Department of Geological Sciences, San Diego State
University, San Diego, CA 92182, USA
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Cited
18 citations as recorded by crossref.
- Large mammal species richness and late Quaternary precipitation change in south‐western Australia J. Faith et al. 10.1002/jqs.2888
- An investigation of human responses to climatic fluctuations at Allen’s Cave, South Australia, from ca 40,000 to 5,000 BP, by a technological analysis of stone artefacts S. Munt et al. 10.1080/03122417.2018.1458446
- Legacy archaeology: Aboriginal subsistence response to Holocene environmental changes using faunal evidence from archaeological sites on the Lower Murray, South Australia H. Allen et al. 10.1177/09596836221145384
- Last Glacial Maximum and Last Glacial–Interglacial Transition pollen record from northern NSW, Australia: evidence for a humid late Last Glacial Maximum and dry deglaciation in parts of eastern Australia D. Ellerton et al. 10.1002/jqs.2960
- 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
- 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
- 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
- Hydroclimate of the Last Glacial Maximum and deglaciation in southern Australia's arid margin interpreted from speleothem records (23–15 ka) P. Treble et al. 10.5194/cp-13-667-2017
- Palaeohydrology of lowland rivers in the Murray-Darling Basin, Australia P. Hesse et al. 10.1016/j.quascirev.2018.09.035
- Evidence for a change in wind regime during the Last Glacial Maximum from the Sydney region B. Thom & T. Oliver 10.1080/08120099.2019.1522668
- Reconstructing palaeoenvironments on desert margins: New perspectives from Eurasian loess and Australian dry lake shorelines K. Fitzsimmons 10.1016/j.quascirev.2017.05.018
- Butzer ‘Down Under’: Debates on anthropogenic erosion in early Colonial Australia D. Cook 10.1016/j.geomorph.2018.12.011
- Optical dating of sediments affected by post-depositional mixing: Modelling, synthesizing and implications J. Peng et al. 10.1016/j.catena.2023.107383
- Cloggs Cave pollen sequences, GunaiKurnai Country, East Gippsland (SE Australia): 25,000 years of cultural plant use and changing environments E. Grono et al. 10.3389/fearc.2024.1488477
- Late‐Quaternary miliolite (biogenic carbonate) deposits and their implications for sea‐level fluctuations and climatic variability A. Durga Prasad et al. 10.1002/esp.5067
- Continuity and discontinuity at the burial site of Roonka, Murray Gorge, South Australia J. Littleton et al. 10.1177/09596836241254491
- Minimum founding populations for the first peopling of Sahul C. Bradshaw et al. 10.1038/s41559-019-0902-6
- Northward expansion of the westerlies over glacial southeastern Australia: evidence from semi-arid lunette dunes, temperate basalt plains, and wind modelling K. Fitzsimmons & S. Gromov 10.3389/feart.2022.921264
18 citations as recorded by crossref.
- Large mammal species richness and late Quaternary precipitation change in south‐western Australia J. Faith et al. 10.1002/jqs.2888
- An investigation of human responses to climatic fluctuations at Allen’s Cave, South Australia, from ca 40,000 to 5,000 BP, by a technological analysis of stone artefacts S. Munt et al. 10.1080/03122417.2018.1458446
- Legacy archaeology: Aboriginal subsistence response to Holocene environmental changes using faunal evidence from archaeological sites on the Lower Murray, South Australia H. Allen et al. 10.1177/09596836221145384
- Last Glacial Maximum and Last Glacial–Interglacial Transition pollen record from northern NSW, Australia: evidence for a humid late Last Glacial Maximum and dry deglaciation in parts of eastern Australia D. Ellerton et al. 10.1002/jqs.2960
- 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
- 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
- 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
- Hydroclimate of the Last Glacial Maximum and deglaciation in southern Australia's arid margin interpreted from speleothem records (23–15 ka) P. Treble et al. 10.5194/cp-13-667-2017
- Palaeohydrology of lowland rivers in the Murray-Darling Basin, Australia P. Hesse et al. 10.1016/j.quascirev.2018.09.035
- Evidence for a change in wind regime during the Last Glacial Maximum from the Sydney region B. Thom & T. Oliver 10.1080/08120099.2019.1522668
- Reconstructing palaeoenvironments on desert margins: New perspectives from Eurasian loess and Australian dry lake shorelines K. Fitzsimmons 10.1016/j.quascirev.2017.05.018
- Butzer ‘Down Under’: Debates on anthropogenic erosion in early Colonial Australia D. Cook 10.1016/j.geomorph.2018.12.011
- Optical dating of sediments affected by post-depositional mixing: Modelling, synthesizing and implications J. Peng et al. 10.1016/j.catena.2023.107383
- Cloggs Cave pollen sequences, GunaiKurnai Country, East Gippsland (SE Australia): 25,000 years of cultural plant use and changing environments E. Grono et al. 10.3389/fearc.2024.1488477
- Late‐Quaternary miliolite (biogenic carbonate) deposits and their implications for sea‐level fluctuations and climatic variability A. Durga Prasad et al. 10.1002/esp.5067
- Continuity and discontinuity at the burial site of Roonka, Murray Gorge, South Australia J. Littleton et al. 10.1177/09596836241254491
- Minimum founding populations for the first peopling of Sahul C. Bradshaw et al. 10.1038/s41559-019-0902-6
- Northward expansion of the westerlies over glacial southeastern Australia: evidence from semi-arid lunette dunes, temperate basalt plains, and wind modelling K. Fitzsimmons & S. Gromov 10.3389/feart.2022.921264
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Discussed (final revised paper)
Latest update: 14 Dec 2024
Short summary
This paper highlights that small dunes (lunettes) formed on the eastern side of a lake in the Australian sub-tropics at the height of the last ice age (about 21,000 years ago) and in the early part of the current interglacial (9–6,000 years ago). This means that it was fairly wet at these times and also that there were strong westerly winds to form the dunes. Today strong westerly winds occur in winter, and we infer that the same was also true at those times, suggesting no change in circulation.
This paper highlights that small dunes (lunettes) formed on the eastern side of a lake in the...
