Annals of the South African Museum, Volume 84The Museum, 1981 - Natural history |
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Page 56
... Quarry perissodactyls are palaeoenvironmentally significant since both the rhinoceros and the Hipparion are hyposodont forms , indicating the presence of grasslands , whereas most of the other large herbivores are wood- land browsers ...
... Quarry perissodactyls are palaeoenvironmentally significant since both the rhinoceros and the Hipparion are hyposodont forms , indicating the presence of grasslands , whereas most of the other large herbivores are wood- land browsers ...
Page 83
... Quarry . The group to which it belonged flourished in Eurasia , and perhaps also Africa , during the late Miocene , and ' E ' Quarry may provide a record of its final flowering . There are several instances where descendants of taxa ...
... Quarry . The group to which it belonged flourished in Eurasia , and perhaps also Africa , during the late Miocene , and ' E ' Quarry may provide a record of its final flowering . There are several instances where descendants of taxa ...
Page 93
... Quarry , although the evidence for this is more slender . An undescribed hyaenid from Kanapoi is certainly more advanced than its counterparts in the ' E ' Quarry ' Hyaena group ' ( see Hendey 1978c ) . The presence of the pig ...
... Quarry , although the evidence for this is more slender . An undescribed hyaenid from Kanapoi is certainly more advanced than its counterparts in the ' E ' Quarry ' Hyaena group ' ( see Hendey 1978c ) . The presence of the pig ...
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3aS and 3aN acrae Aeolidiella Ampelisca Amphipoda Anyskop assemblage Baard's Quarry Baba Barnard bed 3aS Bergh bicuspidata bone Brink buccal cusp Cape Province Cape Town capensis Catriona Cenozoic cerata coast columbiana correlated Coryphella Cragievarus kitchingi crown height deciduous demissum dentary denticles deposits Diademodon dicynodonts digestive branch distal dorsal early Pliocene evidence Family fauna femur Flabellina fossa fossils genus Giraffa sp giraffids gland groove Hendey Hipparion holotype indicate Langebaanweg Langebaanweg area late Miocene late Tertiary lateral lingual mammals Marcus & Marcus marginal ridge maxilla Mesembriportax mesial mesiodistal middle Miocene Miocene muscle Namaqualand Nyanzachoerus occlusal pereopod phosphatic Pleistocene Pliocene posterior present QSM and PPM radular recorded region represented rhinophores river Robertia rows sea-level sediments separated shorelines Sivatherium slightly South Africa South African Museum south-western Cape species specimens SUID-AFRIKAANSE MUSEUM surface Tankard taxa teeth terrestrial tooth UNIVERSITY OF CALIFORNIA Varswater Formation ventral vertebrates