Annals of the South African Museum, Volume 84 |
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Page 22
Since the primary phosphatic rock might also have been formed in a similar environment , it is possible that sea - level was at an elevation of about 30 m for much of the middle to late Miocene . However , this interpretation is not ...
Since the primary phosphatic rock might also have been formed in a similar environment , it is possible that sea - level was at an elevation of about 30 m for much of the middle to late Miocene . However , this interpretation is not ...
Page 29
The fossiliferous deposits of the QSM and PPM range between elevations of 30 m and 40 m , which is a possible indication of the magnitude of the sea - level rise which took place during their deposition . However , the actual rise might ...
The fossiliferous deposits of the QSM and PPM range between elevations of 30 m and 40 m , which is a possible indication of the magnitude of the sea - level rise which took place during their deposition . However , the actual rise might ...
Page 44
In the case of some levels it is possible that the assemblages include specimens derived from pre - existing deposits . This applies particularly in the case of the fluviatile deposits ( beds 3aS and 3aN ) which are , in addition ...
In the case of some levels it is possible that the assemblages include specimens derived from pre - existing deposits . This applies particularly in the case of the fluviatile deposits ( beds 3aS and 3aN ) which are , in addition ...
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Common terms and phrases
abbreviations acrae age profiles alcelaphines Anyskop basal breadth Bed 3aN Bergh bicuspidata bone Brink Broom & Robinson buccal cusp Cape Town cerata cervical enamel prominence cervical margin Coryphella Cragievarus kitchingi crest crown height deciduous dentary denticles dentition deposits Diademodon dicynodonts distal marginal ridge dorsal early Pliocene evidence facet fauna femur Flabellina fossa fossils Gastropoda genus Giraffa Giraffa sp giraffids Grine groove Hendey holotype hypocone iliofemoralis incisal indicated Langebaanweg Langebaanweg area late Miocene late Tertiary lateral lingual cusp mandibular Marcus maxilla maxillary MD diameter Mesembriportax mesial mesial marginal ridge mesiodistal metacone Miocene moderately molars muscle occlusal Pleistocene Pliocene posterior present protoconid QSM and PPM Quarry reconstructed from cast recorded relatively represented rhinophores river Robertia Scale in cm scapula sea-level separated shorelines Sivatherium Sivatherium hendeyi slightly South Africa South African Museum south-western Cape species specimen Tankard taxa teeth terrestrial THERAPSIDA tooth transgression unworn Varswater Formation ventral vertebrae
Bibliographic information
| Title | Annals of the South African Museum, Volume 84 Annals of the South African Museum, South African Museum Volume 84 of Annals of the South African Museum: Annale Van Die Suid-Afrikaanse Museum, South African Museum |
| Author | South African Museum |
| Publisher | The Museum, 1981 |
| Original from | the University of California |
| Digitized | 15 May 2007 |
| ISBN | 0868130095, 9780868130095 |
| Export Citation | BiBTeX EndNote RefMan |