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Page 33
No specimens of this species occur in association with Inoceramus prisms in the
Campanianlower Maastrichtian strata , nor ... Paracypris occurs throughout the
Santonian II to Maastrichtian III but is rare above the shallow - water facies of the
...
No specimens of this species occur in association with Inoceramus prisms in the
Campanianlower Maastrichtian strata , nor ... Paracypris occurs throughout the
Santonian II to Maastrichtian III but is rare above the shallow - water facies of the
...
Page 240
C. sclateri occurs in areas which experience severe frost and with an annual
rainfall of 700 mm ( Lynch 1975 : 137 ) . Amblysomus hottentotus burrows
extensively in soft but not necessarily sandy soil , generally in open ground with
plenty of ...
C. sclateri occurs in areas which experience severe frost and with an annual
rainfall of 700 mm ( Lynch 1975 : 137 ) . Amblysomus hottentotus burrows
extensively in soft but not necessarily sandy soil , generally in open ground with
plenty of ...
Page 346
( wildebeest ) occurs in rather higher proportions in the upper and lower levels ,
but Hippotragus leucophaeus ( blue antelope ) and Damaliscus sp . ( hartebeest
) occur only in the middle levels . Possibly Hippotragus leucophaeus indicates
that ...
( wildebeest ) occurs in rather higher proportions in the upper and lower levels ,
but Hippotragus leucophaeus ( blue antelope ) and Damaliscus sp . ( hartebeest
) occur only in the middle levels . Possibly Hippotragus leucophaeus indicates
that ...
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Contents
THE CAMPANIAN AND MAASTRICHTIAN OSTRACODA OF SOUTH | 2 |
Systematic descriptions | 12 |
Discussion | 131 |
Copyright | |
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Common terms and phrases
Agulhas Bank analysis appear assemblage BH-9 borehole Boomplaas Byneskranskop Camp Campanian Campanian-Maastrichtian Cape Cave cent climate considerable correlation cytheracean dense depth detailed DIEGO Dingle distribution element environmental environments evidence fact Factor fauna Figure flavescens genera genus glacial grass highly hillsides Igoda important increase indicate individual internal interpretation irroratus late lateral length less levels LIBRARY loading locality lower Maastrichtian material mean Mfolozi River micromammalian moderate Needs Nibela noted occurs ostracod ostracod assemblages Otomys palaeoecology parameters pattern period Pleistocene population possible preference present probably proportions range recorded relatively Remarks represented Richards Bay ridge samples Santonian scrub sequence shelf similar slope South south-east Africa species specimens stage suggested Table unit upper valley valves variation varius vegetation Zululand