Page 14 - Bulletin 2 1998
P. 14

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               sea-level of the Middle Pliocene. Nearby, at another quarry, fragmentary fossils, probably of

               very  late  Pliocene  or  early  Pleistocene  age,  include  the  one-toed  horse  (zebra?),  which  is
               known  to  have  entered  Africa  from  Eurasia  2  million  years  ago.  At  Elandsfontein,  near

               Hopefield,  some  of  the  earlier  remains  are  Early  Pleistocene  or  earlier  in  age  (1,7  mya  –
               800,000 years ago) and include the short-necked giraffe, a sabre-toothed cat, giant bushpig

               and warthog-like pigs and a giant baboon, which became extinct about 1 mya. At Baard’s
               Quarry, near Langebaanweg, and at Skurwerug, near Saldanha, isolated fossils from the Early

               or Middle Pleistocene, include a skull of a giant pig such as mentioned previously.




               The earliest evidence of human activity, in the form of hand axes and other tools used by

               Early  Stone  Age  (ESA)  people,  is  found  in  deposits  of  probably  one  million  years  old.

               Possible examples are from the Cape of Good Hope Nature Reserve and from the gravels in
               Tokai and Constantia vineyards.




               Middle Pleistocene Epoch (800,000 – 125,000 years ago)




               But, in order to continue our story, we must move to the farm Elandsfontein near Hopefield,

               where the wind exposed accumulations of fossilized bones and Stone Age artefacts, most of

               which were laid down from 500 – 200,000 years ago and later, during the Upper Pleistocene
               and Holocene. The fossils appear to have accumulated from a limited variety of habitats in

               the  vicinity  of  inland  springs  or  pans  and  the  variety  of  species  found  is,  therefore,  also
               limited. In spite of this, the site is also a globally important source of information on our past.




               Little detail is known of the vegetation, although pollens from a fossil hyaena scat (coprolite)

               included a species of tree now only found some 500 km to the north. The presence in some

               assemblages, where we know we are dealing with material deposited at  the same time, of
               mammalian species such as kudu and black rhinoceros indicate that there was probably more

               bush  than  at  present,  while  the  grazers,  such  as  white  rhinoceros,  wildebeest,  hartebeest,

               springbok, reed buck and zebras, indicate grassland. All the Elandsfontein species are African
               types, and most are directly ancestral to modern ones. Few extinctions have taken place.
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