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Publicação
Late pleistocene and holocene fauna from waterfall bluff rRck shelter, mpondoland, South Africa
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Autores
Fisher, Erich Christopher
Orientador(es)
Resumo(s)
Archaeological deposits from Waterfall Bluff Rock Shelter (Eastern Cape) span from Marine Isotope Stage 3 (similar to 39-29 ka) to the mid-Holocene (similar to 8 ka), showing persistent human occupations. The site's consistent proximity to the shoreline and stable coastline over millennia makes it key for exploring human settlement patterns. This study reports on preliminary results of identifiable fauna from Marine Isotope Stage 3 to the Early Holocene layers at Waterfall Bluff. The identified species may suggest a mosaic environment, although caution is warranted given the small sample size. Furthermore, leopard seal remains were recovered in layers dating to the Last Glacial Maximum. This is the first direct evidence of a leopard seal recovered from Pleistocene and Holocene archaeo-faunal assemblages along the South African coast.
Significance:
Last Glacial Maximum (LGM) sites are rare in southern Africa. Waterfall Bluff in the Eastern Cape shows that human occupation persisted there from Marine Isotope Stage 3 to the mid-Holocene. A leopard seal tooth was identified in the LGM layers, making it the first evidence of this species recovered off South Africa's coast.
Descrição
Palavras-chave
Palaeoenvironment Archaeozoology Pleistocene–Holocene transition Marine Isotope Stage 3 Last Glacial Maximum
Contexto Educativo
Citação
Editora
Academy of Science of South Africa