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Page 142
This all points to a deep ( > 500 m ) outer continental shelf / upper slope
environment . TABLE 9 Suggested palaeoenvironments and summary of
population characters for ostracod assemblages 4-7 in the Campanian -
Maastrichtian of ...
This all points to a deep ( > 500 m ) outer continental shelf / upper slope
environment . TABLE 9 Suggested palaeoenvironments and summary of
population characters for ostracod assemblages 4-7 in the Campanian -
Maastrichtian of ...
Page 145
Similarly , the change from inner - mid shelf to outer shelf ( 4a to 5b ) during the
period Santonian III to Campanian II ( approximately 3 m.y. ) can be traced in BH
- 9 ( Fig . 70B ) . ostracod assemblages 7 6 5b - MAASTRICHTIAN 5a 4b
1000033 ...
Similarly , the change from inner - mid shelf to outer shelf ( 4a to 5b ) during the
period Santonian III to Campanian II ( approximately 3 m.y. ) can be traced in BH
- 9 ( Fig . 70B ) . ostracod assemblages 7 6 5b - MAASTRICHTIAN 5a 4b
1000033 ...
Page 159
Considering the geographical position of sample 818 ( in the vicinity of the Upper
Cretaceous shelf break where the shelf is about 135 km wide ) , this suggests an
outer shelf / upper slope setting in shallow water ( ? -100 m ) . Such an unusual ...
Considering the geographical position of sample 818 ( in the vicinity of the Upper
Cretaceous shelf break where the shelf is about 135 km wide ) , this suggests an
outer shelf / upper slope setting in shallow water ( ? -100 m ) . Such an unusual ...
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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