2011/03/01 by Hervé Bocherens, Oliver Sandrock, Ottmar Kullmer +1 · 3 citations
Social Sciences · Earth and Planetary Sciences · Arts and Humanities · #Pleistocene-Era Hominins and Archaeology #Evolution and Paleontology Studies #Forensic Anthropology and Bioarchaeology Studies
paper · pdf · doi:10.4102/sajs.v107i3/4.331
openalex publication_date 2011/03/01 · openalex created_date 2016/06/24 · openalex updated_date 2026/07/22
Carbon-13 and oxygen-18 abundances were measured in large mammal skeletal remains (tooth enamel, dentine and bone) from the Chiwondo Beds in Malawi, which were dated by biostratigraphic correlation to ca. 2.5 million years ago. The biologic isotopic patterns, in particular the difference in carbon-13 abundances between grazers and browsers and the difference in oxygen-18 abundances between semi-aquatic and terrestrial herbivores, were preserved in enamel, but not in dentine and bone. The isotopic results obtained from the skeletal remains from the Chiwondo Beds indicate a dominance of savannah habitats with some trees and shrubs. This environment was more arid than the contemporaneous Ndolanya Beds in Tanzania. The present study confirms that robust australopithecines were able to live in relatively arid environments and were not confined to more mesic environments elsewhere in southern Africa.