Arid
DOI10.1016/j.quascirev.2020.106338
Late Pleistocene lake level history of Lake Mungo, Australia
Barrows, Timothy T.1,2; Fitzsimmons, Kathryn E.3; Mills, Stephanie C.1; Tumney, Jacqui4; Pappin, Daryl5; Stern, Nicola4
通讯作者Barrows, Timothy T.
来源期刊QUATERNARY SCIENCE REVIEWS
ISSN0277-3791
出版年2020
卷号238
英文摘要Lake Mungo is a currently dry lake basin in the semi-arid zone of southeastern Australia. The transverse dune system on the downwind side contains a record of human occupation of international importance. It also contains one of the most continuous records of climate change over the last glacial cycle in the Australia desert. In this paper we provide a framework for the interpretation of lake level history from before the arrival of people (>41 ka) until after the establishment of the pastoral industry in the area. We present 83 optically stimulated luminescence ages from the Lake Mungo lunette. The lake level history is reconstructed from 34 stratigraphic sections along three transects through the lunette. The dating reveals considerable lake level fluctuations through time which occur over a depth range of similar to 10 m in the basin. At its height, probably at multiple times before 20 ka, the lake held more than 1 km(3) of water and at its final level at similar to 19 ka, contained only 0.03 km(3). The inception of Lake Mungo appears to have taken place during the mid-Pleistocene between similar to 256 and 369 ka. During the last glacial cycle, Lake Mungo was almost continuously wetter than present from shortly after 60 ka until similar to 19 ka. The Upper Mungo, Arumpo and Zanci units represent a succession of lake filling and drying events, briefly interspersed by soils. The final Zanci unit does not represent a single high lake phase, but an initial lake filling followed by a series of short-lived lake level events within a brief period of a few thousand years. At the conclusion of this event, the lake remained dry until the present day. Four OSL ages from a linear dune upwind of Lake Mungo indicates regional aeolian activity from similar to 30 ka until present. Widespread erosion that produces the characteristic topography of the lunette began after the arrival of British pastoralists and traditional aboriginal ways of life overlapped briefly with this erosion. The presence of water in Lake Mungo closely corresponds to periods when regional surface temperature was colder than present during the late Pleistocene. Our new data supports a model that decreased evaporation and increased runoff were primarily responsible for increased availability of surface water in the hydrological cycle. (C) 2020 Elsevier Ltd. All rights reserved.
英文关键词Lake Mungo Optically stimulated luminescence Lake levels Australia Arid zone Pleistocene
类型Article
语种英语
国家Australia ; England ; Germany
收录类别SCI-E ; SSCI
WOS记录号WOS:000537559500012
WOS关键词MURRAY-DARLING BASIN ; OLDEST HUMAN REMAINS ; SOUTHERN-HEMISPHERE ; HUMAN OCCUPATION ; WILLANDRA LAKES ; SNOWY MOUNTAINS ; GLACIAL MAXIMUM ; LUMINESCENCE ; AGE ; SINGLE
WOS类目Geography, Physical ; Geosciences, Multidisciplinary
WOS研究方向Physical Geography ; Geology
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/319326
作者单位1.Univ Wollongong, Sch Earth Atmospher & Life Sci, Wollongong, NSW, Australia;
2.Univ Portsmouth, Sch Environm Geog & Geosci, Portsmouth, Hants, England;
3.Max Planck Inst Chem, Res Grp Terr Palaeoclimates, Hahn Meitner Weg 1, D-55128 Mainz, Germany;
4.La Trobe Univ, Dept Archaeol & Hist, Bundoora, Vic 3086, Australia;
5.New South Wales Off Environm & Heritage, Heritage Div, Buronga, Australia
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GB/T 7714
Barrows, Timothy T.,Fitzsimmons, Kathryn E.,Mills, Stephanie C.,et al. Late Pleistocene lake level history of Lake Mungo, Australia[J],2020,238.
APA Barrows, Timothy T.,Fitzsimmons, Kathryn E.,Mills, Stephanie C.,Tumney, Jacqui,Pappin, Daryl,&Stern, Nicola.(2020).Late Pleistocene lake level history of Lake Mungo, Australia.QUATERNARY SCIENCE REVIEWS,238.
MLA Barrows, Timothy T.,et al."Late Pleistocene lake level history of Lake Mungo, Australia".QUATERNARY SCIENCE REVIEWS 238(2020).
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