Paleoenvironmental and Human Behavioral Implications of the Boegoeberg 1 Late Pleistocene Hyena Den, Northern Cape Province, South Africa

1999 ◽  
Vol 52 (3) ◽  
pp. 393-403 ◽  
Author(s):  
Richard G. Klein ◽  
Kathryn Cruz-Uribe ◽  
David Halkett ◽  
Tim Hart ◽  
John E. Parkington

Boegoeberg 1 (BOG1) is located on the Atlantic coast of South Africa, 850 km north of Cape Town. The site is a shallow rock shelter in the side of a sand-choked gully that was emptied by diamond miners. Abundant coprolites, chewed bones, and partially digested bones implicate hyenas as the bone accumulators. The location of the site, quantity of bones, and composition of the fauna imply it was a brown hyena nursery den. The abundance of Cape fur seal bones shows that the hyenas had ready access to the coast. Radiocarbon dates place the site before 37,000 14C yr ago, while the large average size of the black-backed jackals and the presence of extralimital ungulates imply cool, moist conditions, probably during the early part of the last glaciation (isotope stage 4 or stage 3 before 37,000 14C yr ago) or perhaps during one of the cooler phases (isotope substages 5d or 5b) within the last interglaciation. Comparisons of the BOG1 seal bones to those from regional Middle Stone Age (MSA) and Later Stone Age (LSA) archeological sites suggest (1) that hyena and human seal accumulations can be distinguished by a tendency for vertebrae to be much more common in a hyena accumulation and (2) that hyena and LSA accumulations can be distinguished by a tendency for hyena-accumulated seals to represent a much wider range of individual seal ages. Differences in the way hyenas and people dismember, transport, and consume seal carcasses probably explain the contrast in skeletal part representation, while differences in season of occupation explain the contrast in seal age representation. Like modern brown hyenas, the BOG1 hyenas probably occupied the coast year-round, while the LSA people focused their coastal visits on the August–October interval when nine-to-eleven-month-old seals were abundant. The MSA sample from Klasies River Mouth Cave 1 resembles BOG1 in seal age composition, suggesting that unlike LSA people, MSA people obtained seals more or less throughout the year.

1978 ◽  
Vol 9 (2) ◽  
pp. 219-230 ◽  
Author(s):  
G. P. Rightmire

Substantial numbers of human skeletons have been recovered from caves and shelters of the southern Cape Province, South Africa, and these constitute a valuable source of information about evolutionary change and population movement during Upper Pleistocene and Holocene times. A few fragments from Klasies River Mouth and Die Kelders are firmly associated with Middle Stone Age cultural assemblages, but most of the material is probably linked with the Later Stone Age Albany and Wilton industries. Unfortunately the largest collections of relatively well-preserved remains have come from earlier excavations (Matjes River Shelter, Oakhurst), and the stratigraphic provenance of these burials is frequently in doubt. Other skeletal samples are small, and paleodemographic approaches are diffcult to apply. However, Bushman- or Hottentot-like individuals can certainly be identified, and this is important to the questions of Bushman antiquity or origins. Other problems concerning early Cape populations can also be examined, and this work on the human skeletons should complement ongoing cave sediment and other geological studies, faunal and plant analyses, and archaeological investigations of associated cultural remains.


Radiocarbon ◽  
1986 ◽  
Vol 28 (3) ◽  
pp. 1133-1172 ◽  
Author(s):  
J C Vogel ◽  
Annemarie Fuls ◽  
Ebbie Visser

This list contains 14C dates pertaining to the Stone Age in southern Africa and covers the region from Zambia in the north to Natal and the northern Cape Province in South Africa. The southern and southwestern Cape Province are not included. Descriptions are based on information supplied by the submitters.


1984 ◽  
Vol 39 (139) ◽  
pp. 77
Author(s):  
Peter B. Beaumont ◽  
R. Singer ◽  
J. Wymer

2016 ◽  
Vol Volume 112 (Number 11/12) ◽  
Author(s):  
Hugo G. Nami ◽  
Paloma de la Peña ◽  
Carlos A. Vásquez ◽  
James Feathers ◽  
Paloma de la Peña ◽  
...  

Abstract Palaeomagnetic data from Klasies River main site Cave 1 (Eastern Cape Province, South Africa) are reported. Natural remanent magnetisation directions obtained from 77 oriented samples were determined by progressive alternating field demagnetisation methodology. Three palaeomagnetic samplings from the Witness Baulk from the Middle Stone Age (MSA) Late Pleistocene White Sand member and the Holocene Later Stone Age (LSA) middens in Cave 1 were dated and analysed to obtain the palaeomagnetic directions recorded in the sediments. Here we provide new optically stimulated luminescence (OSL) dates for the White Sand Member, and new accelerator mass spectrometry (AMS) radiocarbon dates for the LSA midden of areas not previously dated. The palaeomagnetic analysis took into account rock magnetism and directional analysis. The former reveals that the main magnetic carrier was magnetite; the latter shows that characteristic remanent magnetisation of normal and anomalous directions was observed in the lower portion of the White Sand Member and LSA midden. Normal directions correspond to the palaeosecular variation record for South Africa during the Late Pleistocene. On the other hand, the anomalous directions recorded in the LSA midden might represent the likely Sterno-Etrussia geomagnetic field excursion which occurred during the Late Holocene and is observed in other places on the planet. Finally, the directional data obtained are a potential tool for discussing the age of deposits corresponding to those periods.


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