Annals of the South African Museum |
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Page 1
... are recorded from the Campanian and Maastrichtian strata of south - east
Africa , where rocks of this age have been sampled in the Natal - Zululand Basin ,
on the Transkei Swell , and in the Outeniqua Basin ( on the Agulhas Bank ) .
... are recorded from the Campanian and Maastrichtian strata of south - east
Africa , where rocks of this age have been sampled in the Natal - Zululand Basin ,
on the Transkei Swell , and in the Outeniqua Basin ( on the Agulhas Bank ) .
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 144
C. Zululand outcrops ( Monzi / Mfolozi / Nibela ) . Having discussed the nature of
the ostracod assemblages and the sedimentary environments that they represent
, it remains to see how these are distributed in time and space in Zululand .
C. Zululand outcrops ( Monzi / Mfolozi / Nibela ) . Having discussed the nature of
the ostracod assemblages and the sedimentary environments that they represent
, it remains to see how these are distributed in time and space in Zululand .
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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