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Page 72
Age , distribution , palaeoecology Santonian II to Maastrichtian II ( Umzamba ,
and Richards Bay BH - 9 borehole , and Mfolozi and Nibela outcrops in Zululand
) , late Campanian / early Maastrichtian ( Igoda ) . Dingle ( 1980 ) found this to be
...
Age , distribution , palaeoecology Santonian II to Maastrichtian II ( Umzamba ,
and Richards Bay BH - 9 borehole , and Mfolozi and Nibela outcrops in Zululand
) , late Campanian / early Maastrichtian ( Igoda ) . Dingle ( 1980 ) found this to be
...
Page 131
In this connection , the composite succession from the various outcrops and the
BH - 9 borehole in Zululand is by far the most complete , and provides to a first
approximation an unbroken section through the Campanian - Maastrichtian .
In this connection , the composite succession from the various outcrops and the
BH - 9 borehole in Zululand is by far the most complete , and provides to a first
approximation an unbroken section through the Campanian - Maastrichtian .
Page 132
PALAEOECOLOGY NORTHERN AREA BH - 9 borehole and Zululand outcrops
Figure 2 shows the sampling localities in this area , and Figure 3 shows the
stratigraphic relationships of the various outcrops using Kennedy & Klinger's (
1975 ) ...
PALAEOECOLOGY NORTHERN AREA BH - 9 borehole and Zululand outcrops
Figure 2 shows the sampling localities in this area , and Figure 3 shows the
stratigraphic relationships of the various outcrops using Kennedy & Klinger's (
1975 ) ...
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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