Australopithecus sediba at 1.977 Ma and Implications for the Origins of the Genus Homo

Newly exposed cave sediments at the Malapa site include a flowstone layer capping the sedimentary unit containing the Australopithecus sediba fossils. Uranium-lead dating of the flowstone, combined with paleomagnetic and stratigraphic analysis of the flowstone and underlying sediments, provides a ti...

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Veröffentlicht in:Science (American Association for the Advancement of Science) 2011-09, Vol.333 (6048), p.1421-1423
Hauptverfasser: Pickering, Robyn, Dirks, Paul H. G. M., Jinnah, Zubair, de Ruiter, Darryl J., Churchil, Steven E., Herries, Andy I. R., Woodhead, Jon D., Hellstrom, John C., Berger, Lee R.
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container_issue 6048
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container_title Science (American Association for the Advancement of Science)
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creator Pickering, Robyn
Dirks, Paul H. G. M.
Jinnah, Zubair
de Ruiter, Darryl J.
Churchil, Steven E.
Herries, Andy I. R.
Woodhead, Jon D.
Hellstrom, John C.
Berger, Lee R.
description Newly exposed cave sediments at the Malapa site include a flowstone layer capping the sedimentary unit containing the Australopithecus sediba fossils. Uranium-lead dating of the flowstone, combined with paleomagnetic and stratigraphic analysis of the flowstone and underlying sediments, provides a tightly constrained date of 1.977 ± 0.002 million years ago (Ma) for these fossils. This refined dating suggests that Au. sediba from Malapa predates the earliest uncontested evidence for Homo in Africa.
doi_str_mv 10.1126/science.1203697
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subjects Animals
Australopithecus
Biological taxonomies
Caves
Dolomite
Earth sciences
Earth, ocean, space
Evolution
Evolutionary biology
Exact sciences and technology
Flowstone
Fossils
Geologic Sediments
Geological facies
Geology - methods
Hominidae - anatomy & histology
Hominidae - classification
Hominids
Magnetics
Marine and continental quaternary
Paleontology
Prehistoric era
Radiometric Dating
Research universities
Sediments
South Africa
Surficial geology
Time
Uranium
Vertebrate paleontology
title Australopithecus sediba at 1.977 Ma and Implications for the Origins of the Genus Homo
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