Arid
DOI10.1016/j.quascirev.2019.106112
Pluvial periods in Southern Arabia over the last 1.1 million-years
Nicholson, Samuel L.1; Pike, Alistair W. G.2; Hosfield, Rob1; Roberts, Nick3; Sahy, Diana3; Woodhead, Jon4; Cheng, Hai5,6; Edwards, R. Lawrence5; Affolter, Stephane7,8,11; Leuenberger, Markus7; Burns, Stephen J.9; Matter, Albert10; Fleitmann, Dominik1,11
通讯作者Nicholson, Samuel L. ; Fleitmann, Dominik
来源期刊QUATERNARY SCIENCE REVIEWS
ISSN0277-3791
EISSN1873-457X
出版年2020
卷号229
英文摘要Past climates and environments experienced by the Saharo-Arabian desert belt are of prime importance for palaeoclimatic and palaeoanthropological research. On orbital timescales transformations of the desert into a grassland landscape in response to higher precipitation provided windows of opportunity for hominin dispersal from Africa into Eurasia. On long timescales, palaeoenvironmental reconstructions for the region are predominantly derived from marine sediments and available terrestrial records from the Arabian Peninsula are limited to 450 ka before present (BP). Here, we present a new stalagmite-based palaeoclimate record from Mukalla Cave in Yemen which extends back to similar to 1.1 million years BP or Marine Isotope Stage (MIS) 31, as determined by Uranium-lead dating. Stalagmite Y99 grew only during peak interglacial periods and warm substages back to similar to 1.1 Ma. Stalagmite calcite oxygen isotope (delta O-18) values show that every past interglacial humid period was wetter than the Holocene, a period in which large lakes formed in the now arid areas of southern Arabia. Carbon isotope (delta C-13) values indicate habitable grassland environments developed during these pluvial periods. A total of 21 pluvial periods with precipitation of more than 300 mm yr(-1) occurred since similar to 1.1 Ma and thus numerous opportunities for hominin dispersals occurred throughout the Pleistocene. New determinations of hydrogen (delta D-Fl) and oxygen (delta O-18(Fl)) isotopes in stalagmite fluid inclusion water demonstrates that enhanced precipitation in Southern Arabia was brought by the African and Indian Summer Monsoons. When combined with sub-annual calcite analysis of delta O-18 and delta C-13, these data reveal a distinct wet (summer) and dry (winter) seasonality. (C) 2019 Elsevier Ltd. All rights reserved.
英文关键词Human dispersal Middle east Pleistocene Speleothems Arabia Oxygen-isotopes Carbon -isotopes Water-isotopes Uranium-series dating Monsoon
类型Article
语种英语
国家England ; Australia ; USA ; Peoples R China ; Switzerland
开放获取类型Green Accepted
收录类别SCI-E ; SSCI
WOS记录号WOS:000514018700008
WOS关键词REASSESSING LACUSTRINE ENVIRONMENTS ; EASTERN MEDITERRANEAN REGION ; SPELEOTHEM FLUID INCLUSIONS ; HOLOCENE CLIMATIC RECORDS ; PLEISTOCENE CLIMATE ; MODERN HUMANS ; SAUDI-ARABIA ; HOMO-SAPIENS ; NEGEV DESERT ; DELTA-D
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/2XILL650/315386
作者单位1.Univ Reading, Dept Archaeol, Reading, Berks, England;
2.Univ Southampton, Dept Archaeol, Southampton, Hants, England;
3.British Geol Survey, Geochronol & Tracers Facil, Nottingham, England;
4.Univ Melbourne, Sch Earth Sci, Melbourne, Vic, Australia;
5.Univ Minnesota, Dept Earth Sci, Minneapolis, MN USA;
6.Xi An Jiao Tong Univ, Inst Global Environm Change, Xian, Peoples R China;
7.Univ Bern, Phys Inst, Bern, Switzerland;
8.Int Fdn High Altitude Res Stn Jungfraujoch & Gorn, Bern, Switzerland;
9.Univ Massachusetts, Dept Geosci, Amherst, MA 01003 USA;
10.Univ Bern, Inst Geol Sci, Bern, Switzerland;
11.Univ Basel, Dept Environm Sci, Quaternary Environm Geol, Basel, Switzerland
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GB/T 7714
Nicholson, Samuel L.,Pike, Alistair W. G.,Hosfield, Rob,et al. Pluvial periods in Southern Arabia over the last 1.1 million-years[J],2020,229.
APA Nicholson, Samuel L..,Pike, Alistair W. G..,Hosfield, Rob.,Roberts, Nick.,Sahy, Diana.,...&Fleitmann, Dominik.(2020).Pluvial periods in Southern Arabia over the last 1.1 million-years.QUATERNARY SCIENCE REVIEWS,229.
MLA Nicholson, Samuel L.,et al."Pluvial periods in Southern Arabia over the last 1.1 million-years".QUATERNARY SCIENCE REVIEWS 229(2020).
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