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Page 89
Holotype SAM - K5747 , LV , sample 818 , Agulhas Bank , Maastrichtian III
Paratypes SAM - K5748 , RV , sample 818 , Agulhas Bank , Maastrichtian III SAM
- K5749 , LV , sample 818 , Agulhas Bank , Maastrichtian III SAM - K5750 , RV ...
Holotype SAM - K5747 , LV , sample 818 , Agulhas Bank , Maastrichtian III
Paratypes SAM - K5748 , RV , sample 818 , Agulhas Bank , Maastrichtian III SAM
- K5749 , LV , sample 818 , Agulhas Bank , Maastrichtian III SAM - K5750 , RV ...
Page 148
Most interesting is the presence of two Agulhas Bank Maastrichtian species in JC
- 1 , Phacorhabdotus ? anomala , and ... Similarly , the genus Australileberis ,
which is common in the Eocene of JC - 1 and the Agulhas Bank , has been ...
Most interesting is the presence of two Agulhas Bank Maastrichtian species in JC
- 1 , Phacorhabdotus ? anomala , and ... Similarly , the genus Australileberis ,
which is common in the Eocene of JC - 1 and the Agulhas Bank , has been ...
Page 156
SOUTHERN AREA : AGULHAS BANK The presence of uppermost Cretaceous
strata on the Agulhas Bank was first established by sea - floor sampling in a
slump - exposed outcrop on the upper continental slope ( Dingle 1971 , 1978 ) .
SOUTHERN AREA : AGULHAS BANK The presence of uppermost Cretaceous
strata on the Agulhas Bank was first established by sea - floor sampling in a
slump - exposed outcrop on the upper continental slope ( Dingle 1971 , 1978 ) .
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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