Arid
DOI10.1016/j.revpalbo.2019.02.006
Speleothem evidence for C-3 dominated vegetation during the Late Miocene (Messinian) of South Africa
Hopley, Philip J.1,2; Reade, Hazel3; Parrish, Randall4,5; De Kock, Michiel6; Adams, Justin W.7,8
通讯作者Hopley, Philip J.
来源期刊REVIEW OF PALAEOBOTANY AND PALYNOLOGY
ISSN0034-6667
EISSN1879-0615
出版年2019
卷号264页码:75-89
英文摘要During the Late Miocene, Africa experienced a number of ecological transitions including the spread of C-4 grass-lands, the expansion of the Sahara Desert, the Messinian Salinity Crisis and a number of mammalian migrations and expansions, including the origin of the hominin Glade. A detailed understanding of the relationship between environmental change and hominin evolution is hampered by the paucity of data available from terrestrial localities, especially in southern Africa. Here, we present a stable isotope and trace element record from a speleothem from the South African cave site of Hoogland. Uranium-lead dating and magnetostratigraphy places the speleothem within the Messinian Age (7.25-5.33 Ma) of the Late Miocene, making it the oldest known cave deposit from the region near the UNESCO Fossil Hominids of South Africa World Heritage Site (locally known as the Cradle of Humankind). Low carbon isotope values indicate a predominantly C-3 vegetation in the vicinity of the cave throughout the period of speleothem growth. It is not possible to determine if this represents a C-3 grassland or a C-3 woodland, but it is clear that an equivalent C-3-rich environment has yet to be found during the Messinian of east Africa. We conclude that the C-4 grass expansion occurred millions of years later in South Africa than it did in eastern Africa, and that this vegetation shift should be considered when comparing African vegetation change with the late Miocene hominin fossil record. (C) 2019 Elsevier B.V. All rights reserved.
英文关键词Messinian Speleothem U-Pb age Stable isotopes C-3 vegetation South Africa
类型Article
语种英语
国家England ; South Africa ; Australia
开放获取类型Green Accepted
收录类别SCI-E ; SSCI
WOS记录号WOS:000466452800007
WOS关键词NORTH-WEST PROVINCE ; STABLE-ISOTOPE ; MAGNETOBIOSTRATIGRAPHIC CHRONOLOGY ; AUSTRALOPITHECUS-SEDIBA ; GAUTENG PROVINCE ; ATMOSPHERIC CO2 ; PLIOCENE ; CLIMATE ; HOMINID ; EVOLUTION
WOS类目Plant Sciences ; Paleontology
WOS研究方向Plant Sciences ; Paleontology
来源机构University of London
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/218471
作者单位1.Birkbeck Univ London, Dept Earth & Planetary Sci, London, England;
2.UCL, Dept Earth Sci, London, England;
3.UCL, Inst Archaeol, London, England;
4.Univ Portsmouth, Sch Earth & Environm Sci, Portsmouth, Hants, England;
5.British Geol Survey, NERC Isotope Geosci Labs, Keyworth, Notts, England;
6.Univ Johannesburg, Dept Geol, Johannesburg, South Africa;
7.Monash Univ, Dept Anat & Dev Biol, Ctr Human Anat Educ, Melbourne, Vic, Australia;
8.Univ Johannesburg, Ctr Anthropol Res, Johannesburg, South Africa
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Hopley, Philip J.,Reade, Hazel,Parrish, Randall,et al. Speleothem evidence for C-3 dominated vegetation during the Late Miocene (Messinian) of South Africa[J]. University of London,2019,264:75-89.
APA Hopley, Philip J.,Reade, Hazel,Parrish, Randall,De Kock, Michiel,&Adams, Justin W..(2019).Speleothem evidence for C-3 dominated vegetation during the Late Miocene (Messinian) of South Africa.REVIEW OF PALAEOBOTANY AND PALYNOLOGY,264,75-89.
MLA Hopley, Philip J.,et al."Speleothem evidence for C-3 dominated vegetation during the Late Miocene (Messinian) of South Africa".REVIEW OF PALAEOBOTANY AND PALYNOLOGY 264(2019):75-89.
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