African Archaeological Review

, Volume 32, Issue 4, pp 813–838 | Cite as

Macrobotanical Remains from Wonderwerk Cave (Excavation 1), Oldowan to Late Pleistocene (2 Ma to 14 ka bp), South Africa

Original Article

Abstract

Wonderwerk Cave in the Northern Cape Province of South Africa has a record of occupation spanning some 2 million years, comprising flora, fauna and cultural artifacts and, therefore, potentially, has the most complete macrobotanical record associated with hominin/human activities. The flora is described here for the lower levels: the Oldowan Stratum 12 (ca. 2 Ma) to the Late Pleistocene Stratum 5 (ca. 14 ka). The older material includes calcified roots, leaf litter of small dicotyledonous twigs and seeds, grass and sedge culms. From Stratum 5, there are about 134 pieces of charcoal that have been identified to eight woody species. Assuming the firewood was of local origin, the climate during the latest Pleistocene would have been slightly more mesic than today’s arid to semi-arid climate.

Keywords

Macrobotanical remains Sedges Grasses Seeds Charcoal Fire-sticks 

Résumé

La grotte de Wonderwerk, située dans la province du Cap-Nord, en Afrique du Sud, a une occupation qui s’étend sur près de 2 millions d’années, attestée par la flore, la faune et des artefacts culturels. Les données botaniques associées à des activités d’homininés et/ou d’humains forment l’ensemble jusqua le plus complet découvert à ce jour. La flore décrite ici provient des couches inférieures, du niveau 12 (env. 2 Mio. au niveau 5 (env. 14 k). Le matériel le plus ancien comprend des détritus de feuilles, des brindilles et des graines de petites dicotylédones, des racines calcifiées, des tiges d’herbes et de laîches. Dans le niveau 5, les 134 fragments de charbon de bois appartiennent à huit espèces ligneuses. En assumant que le bois de feu est d’origine locale, le climat de la fin du Pléistocène serait légèrement plus mésoïque que le climat aride à semi-aride d’aujourd’hui.

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© Springer Science+Business Media New York 2015

Authors and Affiliations

  1. 1.Evolutionary Studies Institute and School of GeosciencesUniversity of the WitwatersrandJohannesburgSouth Africa

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