Annals of the South African Museum |
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Page 316
It is possible that the restioid or ' grassy ' element is that which is today called
Dense Restioid - Proteoid Shrubland ( Moffett & Deacon 1977 ) and confined to
higher altitudes , especially where conditions are relatively dry . At the time of
level ...
It is possible that the restioid or ' grassy ' element is that which is today called
Dense Restioid - Proteoid Shrubland ( Moffett & Deacon 1977 ) and confined to
higher altitudes , especially where conditions are relatively dry . At the time of
level ...
Page 318
... of unit BRL , the climate apparently continued to be moderately dry , as is
suggested by the relatively high proportion of sparse possibly semi - arid scrub
on the hillsides and even a relative increase in semi - arid scrub on the valley
floor .
... of unit BRL , the climate apparently continued to be moderately dry , as is
suggested by the relatively high proportion of sparse possibly semi - arid scrub
on the hillsides and even a relative increase in semi - arid scrub on the valley
floor .
Page 327
Evidence for changes in sea - level has long been studied , but the relatively
recent advances in the interpretation of deep - sea cores have had a profound
effect upon palaeoclimatic studies . These cores have the advantage of providing
...
Evidence for changes in sea - level has long been studied , but the relatively
recent advances in the interpretation of deep - sea cores have had a profound
effect upon palaeoclimatic studies . These cores have the advantage of providing
...
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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