Annals of the South African Museum, Volume 69The Museum,., 1976 - Natural history |
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Page 209
Secondly , Ostrom ( 1964 ) indicates that because of their vertical orientation the
origin of the adductor fibres would encroach on to the facial region , restricting
their size and power . This statement is true except in cases where the orbit is ...
Secondly , Ostrom ( 1964 ) indicates that because of their vertical orientation the
origin of the adductor fibres would encroach on to the facial region , restricting
their size and power . This statement is true except in cases where the orbit is ...
Page 257
The fossa thus indicates the presence of a laterally placed muscle whose area of
origin may well have included the lateral surface of the squamosal . If so , the
impression of the squamosal left on the matrix suggests that the posterior root of
the ...
The fossa thus indicates the presence of a laterally placed muscle whose area of
origin may well have included the lateral surface of the squamosal . If so , the
impression of the squamosal left on the matrix suggests that the posterior root of
the ...
Page 259
primitive dinocephalians in that there is no specialized origin of the external
adductor from the dorsal surface of the temporal roof in Venjukovia . Unless a
reversal ( i.e. secondary elimination of this area of origin ) is postulated , animals
which ...
primitive dinocephalians in that there is no specialized origin of the external
adductor from the dorsal surface of the temporal roof in Venjukovia . Unless a
reversal ( i.e. secondary elimination of this area of origin ) is postulated , animals
which ...
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Common terms and phrases
abbreviations adductor Anchisaurus anterior appear assemblage attachment aurantiacus authors Barnard base bearing bone border Cape Cape Town capensis capitals cent cervical coast collected consists coxal plates deposits described distal dorsal East environment extends Family fauna fibres figures Formation forms fossils genus given Haughton headings Huene illustrations indicate insertion Island Late Pleistocene lateral length lies lower margin material medial Member molluscs muscle musculature Note occur origin ovig Pleistocene portion position posterior present probably quadrate Quartzose Sand ramus range recorded referred region represented River Saldanha Sand sea level sediments segments separates shell short shows similar skull Smith South African Museum species specimens spines St Paul suggests surface Table Table Bay temperature third Typhlosaurus upper ventral vertebrae
Bibliographic information
| Title | Annals of the South African Museum, Volume 69 Annals of the South African Museum, South African Museum |
| Contributor | South African Museum |
| Publisher | The Museum,., 1976 |
| Original from | the University of California |
| Digitized | 21 Apr 2010 |
| Export Citation | BiBTeX EndNote RefMan |