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Page 108
Age , distribution , palaeoecology If these specimens are conspecific with H ?.
arcus then they probably extend the known range of this species from late
Campanian / early Maastrichtian ( Igoda and Needs Camp ) to Maastrichtian II (
Zululand ) ...
Age , distribution , palaeoecology If these specimens are conspecific with H ?.
arcus then they probably extend the known range of this species from late
Campanian / early Maastrichtian ( Igoda and Needs Camp ) to Maastrichtian II (
Zululand ) ...
Page 165
Hermanites kennedyi Zone - range Campanian II to middle Campanian IV .
Definition : period which begins with first appearance of Hermanites kennedyi
and ends with the first appearance of Dutoitella dutoiti . Remarks : can be divided
into ...
Hermanites kennedyi Zone - range Campanian II to middle Campanian IV .
Definition : period which begins with first appearance of Hermanites kennedyi
and ends with the first appearance of Dutoitella dutoiti . Remarks : can be divided
into ...
Page 166
In addition , in the lower part ( Campanian V ) it includes the uppermost range of
Hermanites kennedyi as well as the typical Campanian V species Curfsina
monziensis . The early Maastrichtian I part sees the appearance of
Pterygocythere ...
In addition , in the lower part ( Campanian V ) it includes the uppermost range of
Hermanites kennedyi as well as the typical Campanian V species Curfsina
monziensis . The early Maastrichtian I part sees the appearance of
Pterygocythere ...
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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