Arid
DOI10.1016/j.quascirev.2022.107635
Late Quaternary climate change in Australia's arid interior: Evidence from Kati Thanda-Lake Eyre
Cohen, Tim J.; Arnold, Lee J.; Gazquez, Fernando; May, Jan-Hendrik; Marx, Sam K.; Jankowski, Nathan R.; Chivas, Allan R.; Garcia, Adriana; Cadd, Haidee; Parker, Adrian G.; Jansen, John D.; Fu, Xiao; Waldmann, Nicolas; Nanson, Gerald C.; Jones, Brian G.; Gadd, Patricia
通讯作者Cohen, TJ
来源期刊QUATERNARY SCIENCE REVIEWS
ISSN0277-3791
EISSN1873-457X
出版年2022
卷号292
英文摘要Williams Point is an iconic late Quaternary sedimentary sequence exposed at the southern margin of Madigan Gulf at Kati Thanda -Lake Eyre (KT-LE), Australia's largest lake. The-15 m high cliff outcrop includes 6 m of aeolian sediments, capping a-0.5 m beach/shoreline facies containing abundant Coxiella (aquatic gastropod) unconformably overlying 5-6 m of fluvio-lacustrine facies. The base of the outcrop and the playa floor comprises shallow and deeper water laminated lacustrine sediments. We re-examine the stratigraphic sequence using detailed excavations, micromorphological analysis and geochemical characterisation (X-ray fluorescence, X-ray diffraction, palaeoecology, stable isotope analysis of gypsum hydration water and biogenic carbonates, rare earth element analysis) and present a revised chronology using single-grain optically stimulated luminescence (OSL) within a Bayesian framework. Our new chronostratigraphic data generally supports previous interpretations for Williams Point, but crucially refines the timing of several of the key sedimentological units. The deeper-water lacustrine facies on the lake floor, unconformably overlying the Miocene Etadunna Formation, were deposited 206 +/- 13 ka (232-169 ka, 95% credible interval; C.I.). A palaeoplaya, or oxidised shallow lake deposits, formed at 153 +/- 11 ka (175-131 ka, 95% C.I.) and the uppermost shallow water lacustrine facies at the base of the cliff was deposited at 131 +/- 9 ka (150-113 ka, 95% C.I.). An unconformity separates these sediments from the overlying fluvio-lacustrine phase, securely constrained (with eight OSL samples) to 86 +/- 4 ka (95-78 ka, 95% C.I.). The isotopic composition of the palaeolake water (318O and 3D), reconstructed from the hy-dration water of syndepositional gypsum formed in-situ in these fluvio-lacustrine sediments, indicates wetter conditions at 95-78 ka than at ca. 232-131 ka. Based on the provenance analysis these fluvio-lacustrine and lacustrine sediments were sourced from the northern catchments within the Lake Eyre basin but with an additional contribution from the northern Flinders Ranges. An erosional unconformity separates this sedimentary unit from the overlying Coxiella beach facies, which itself dates to 71 +/- 4 ka (79-63 ka; 95% C.I.). This beach facies is interpreted to represent a regressional shoreline or near-shore deposit formed during Marine Isotope Stage [MIS] 4. This is the most reliable palaeolake level indicator inthe sequence and indicates a maximum water depth of 12 m. The overlying Williams Point aeolian unit (WPAU) dates to 49 +/- 4 ka (56 - 41 ka, 95% C.I.), slightly younger than previous estimates. The model ledage for WPAU overlaps with (and is within uncertainty of) the last KT-LE megalake phase, which reached +5 m AHD at 48 +/- 2 ka. However, considering its elevation (-3 to +3 m AHD), the age of this gypsiferous aeolian unit demands that it accreted as KT-LE was entering a playa phase with lengthy periods of exposed lake floor. In turn, this means that the putative Genyornis newtoni (a megafaunal flightless bird) which laid its eggs in the gypsiferous dunes, went extinct during a time of hydrological transformation. These results bring fresh perspectives to a site that has held a heavy sway over previous views of the Quaternary history of Australia's arid zone. (C) 2022 Elsevier Ltd. All rights reserved
英文关键词Lake Eyre Kati Thanda Arid OSL Fluvial Lacustrine Gypsum Playa lake Stable isotopes Emu
类型Article
语种英语
收录类别SCI-E
WOS记录号WOS:000860280100002
WOS关键词PERENNIALLY FROZEN DEPOSITS ; TRACE-ELEMENT ; ISOTOPE FRACTIONATION ; SOUTHERN-HEMISPHERE ; OSL CHARACTERISTICS ; NORTHERN AUSTRALIA ; HUMAN OCCUPATION ; GENYORNIS EGG ; COOPER CREEK ; LUMINESCENCE
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/2XILL650/394106
推荐引用方式
GB/T 7714
Cohen, Tim J.,Arnold, Lee J.,Gazquez, Fernando,et al. Late Quaternary climate change in Australia's arid interior: Evidence from Kati Thanda-Lake Eyre[J],2022,292.
APA Cohen, Tim J..,Arnold, Lee J..,Gazquez, Fernando.,May, Jan-Hendrik.,Marx, Sam K..,...&Gadd, Patricia.(2022).Late Quaternary climate change in Australia's arid interior: Evidence from Kati Thanda-Lake Eyre.QUATERNARY SCIENCE REVIEWS,292.
MLA Cohen, Tim J.,et al."Late Quaternary climate change in Australia's arid interior: Evidence from Kati Thanda-Lake Eyre".QUATERNARY SCIENCE REVIEWS 292(2022).
条目包含的文件
条目无相关文件。
个性服务
推荐该条目
保存到收藏夹
导出为Endnote文件
谷歌学术
谷歌学术中相似的文章
[Cohen, Tim J.]的文章
[Arnold, Lee J.]的文章
[Gazquez, Fernando]的文章
百度学术
百度学术中相似的文章
[Cohen, Tim J.]的文章
[Arnold, Lee J.]的文章
[Gazquez, Fernando]的文章
必应学术
必应学术中相似的文章
[Cohen, Tim J.]的文章
[Arnold, Lee J.]的文章
[Gazquez, Fernando]的文章
相关权益政策
暂无数据
收藏/分享

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。