Palaeoecology of giraffe tracks in Late Pleistocene aeolianites on the Cape south coast

Charles Helm, Hayley Cawthra, Richard Cowling, Jan De Vynck, Curtis Marean, Richard McCrea, Renee Rust

Research output: Contribution to journalArticlepeer-review

28 Scopus citations


Until now there have been no reliable historical or skeletal fossil records for the giraffe (Giraffa camelopardalis) south of the Orange River or northern Namaqualand. The recent discovery of fossil giraffe tracks in coastal aeolianites east of Still Bay, South Africa, significantly increases the geographical range for this species, and has implications for Late Pleistocene climate and vegetation in the southern Cape. Giraffe populations have specialised needs, and require a savanna ecosystem. Marine geophysical and geological evidence suggests that the broad, currently submerged floodplains of the Gouritz and Breede Rivers likely supported a productive savanna of Vachellia karroo during Pleistocene glacial conditions, which would have provided a suitable habitat for this species. We show evidence for the hypothesis that the opening of the submerged shelf during glacial periods acted as a pathway for mammals to migrate along the southern coastal plain.

Original languageEnglish (US)
Article number2017-0266
JournalSouth African Journal of Science
Issue number1-2
StatePublished - Jan 1 2018


  • Fossil tracks
  • Savanna
  • South Africa
  • Still Bay

ASJC Scopus subject areas

  • General Biochemistry, Genetics and Molecular Biology
  • General Agricultural and Biological Sciences
  • General Earth and Planetary Sciences


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