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Beyond the South African cave paradigm— Australopithecus africanus from Plio–Pleistocene paleosol deposits at Taung

Bibliographic Data

ID8311685
AuthorsPhilip J Hopley (0000-0001-8138-3813, Department of Earth and Planetary Sciences Birkbeck, University of London London WC1E 7HX UK, corresponding author), Andy I R Herries (0000-0002-2905-2002, Department of Archaeology, Environment and Community Planning, Australian Archaeomagnetism Laboratory, Faculty of Humanities and Social Sciences La Trobe University Melbourne 3086 VIC Australia), Stephanie E Baker (0000-0002-7140-928X, University of the Witwatersrand), Brian F Kuhn (0000-0001-9370-4071, Institute of Human Evolution University of the Witwatersrand South Africa), Colin G Menter (0000-0003-1066-8496, Centre for Anthropological Research University of Johannesburg South Africa)
Year2013
Volume151
Issue2
Pages316-324
Publication date2013-06-01
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueAmerican Journal of Physical Anthropology (JOURNAL)
Journal identifiersISSN: 0002-9483 • E-ISSN: 1096-8644
PublisherWiley (PUBLISHER • GB)
DOI10.1002/ajpa.22272
PMID23633001
OpenAlexW1915358689
LanguageEN
Citations received5
References cited34

Following the discovery of the “Taung Child” ( Australopithecus africanus ) in 1924 in the Buxton‐Norlim Limeworks near Taung, the fossil‐bearing deposits associated with the Dart and Hrdlička pinnacles have been interpreted as the mined remnants of cave sediments that formed within the Plio–Pleistocene Thabaseek Tufa: either as a younger cave‐fill or as contemporaneous carapace caves. When combined with the Plio–Pleistocene dolomitic cave deposits from the “Cradle of Humankind,” a rather restricted view emerges that South African early hominins derived from cave deposits, whereas those of east and central Africa are derived from fluvio‐lacustrine and paleosol deposits. We undertook a sedimentological and paleomagnetic analysis of the pink‐colored deposit (PCS) from which the “Taung Child” is purported to have derived and demonstrate that it is a calcrete, a carbonate‐rich pedogenic sediment, which formed on the paleo‐land surface. The deposit extends 100 s of meters laterally beyond the Dart and Hrdlička Pinnacles where it is interbedded with the Thabaseek Tufa, indicating multiple episodes of calcrete development and tufa growth. The presence of in situ rhizoconcretions and insect trace fossils ( Celliforma sp. and Coprinisphaera sp.) and the distinctive carbonate microfabric confirm that the pink deposit is a pedogenic calcrete, not a calcified cave sediment. Paleomagnetic and stratigraphic evidence indicates that a second, reversed polarity, fossil‐bearing deposit (YRSS) is a younger fissure‐fill formed within a solutional cavity of the normal polarity tufa and pink calcrete (PCS). These observations have implications for the dating, environment, and taphonomy of the site, and increase the likelihood of future fossil discoveries within the Buxton‐Norlim Limeworks. Am J Phys Anthropol 151:316–324, 2013. © 2013 Wiley Periodicals, Inc

Archaeology · Carbonate · Cave · Facies · Geochemistry · Geography · Loess · Paleomagnetism · Paleosol · Pleistocene · Plio-Pleistocene · Speleothem · Structural basin · Taphonomy · Tufa · Archaeology and Rock Art Studies · Evolution and Paleontology Studies · Geology · Paleontology · Pleistocene-Era Hominins and Archaeology

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Unique citing works5
Citations per year0,45
Citation span2015 - 2017 (3)
Citation velocityhistorical
Highly citedNo
Citation typesNeutral: 4

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