Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/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
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ISSN | 0034-6667 |
EISSN | 1879-0615 |
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 |
推荐引用方式 GB/T 7714 | 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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