Botanical remains from a coprolite from the Pleistocene hominin site of Malapa, Sterkfontein Valley, South Africa

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dc.contributor.author Bamford, M.K.
dc.contributor.author Neumann, F.H.
dc.contributor.author Pereira, L.M.
dc.contributor.author Scott, L.
dc.contributor.author Dirks, P.H.G.M.
dc.contributor.author Berger, L.R.
dc.date.accessioned 2014-02-18T07:41:41Z
dc.date.available 2014-02-18T07:41:41Z
dc.date.issued 2010-12
dc.identifier.issn 0078-8554
dc.identifier.uri http://hdl.handle.net10539/13822
dc.description.abstract A coprolite probably from a carnivore described in this paper was recovered from the decalcified sediments of Facies D, close to the cranium of a hominid child, Australopithecus sediba, at Malapa, and is dated at 1.95–1.78 Ma based on a combination of faunal, U-Pb and palaeomagnetic dating techniques. Maceration of the coprolite yielded wood fragments and pollen of Podocarpus sp. as well as phytolith morphotypes that occur in leaves of Podocarpus and many other woody taxa. The Malapa site today is in the Grassland Biome, close to the transition to the Savanna Biome. Podocarpus/Afrocarpus occurs about 30km distance in the Northern Afromontane Forest Biome and is restricted to small patches in the mountain kloofs or small canyons (altitude: 1500–1900 m). The occurrence of this vegetation at Malapa in the past implies that the cooler, moister forest vegetation was more widespread. en_ZA
dc.language.iso en en_ZA
dc.publisher Bernard Price Institute for Palaeontological Research, University of the Witwatersrand en_ZA
dc.subject Podocarpus en_ZA
dc.subject pollen en_ZA
dc.subject wood en_ZA
dc.subject phytoliths en_ZA
dc.title Botanical remains from a coprolite from the Pleistocene hominin site of Malapa, Sterkfontein Valley, South Africa en_ZA
dc.type Article en_ZA


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