Annals of the South African Museum |
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Page 223
The fact that plant life - form is apparently so important it would suggest , in fact ,
that even available general ecological information may allow some acceptable
interpretation of past vegetation changes . It is important , however , to note that ...
The fact that plant life - form is apparently so important it would suggest , in fact ,
that even available general ecological information may allow some acceptable
interpretation of past vegetation changes . It is important , however , to note that ...
Page 299
An interesting fact is that the coefficients of variation vary inversely with mean
depth of mandible ( Fig . 25 ) . Thus , when the depth of mandible is great the
coefficient of variation is low , and vice versa . This suggests that there is some ...
An interesting fact is that the coefficients of variation vary inversely with mean
depth of mandible ( Fig . 25 ) . Thus , when the depth of mandible is great the
coefficient of variation is low , and vice versa . This suggests that there is some ...
Page 322
In fact , this is relative and for the earlier samples , from levels 14 up to 5 , the
index is within the range exhibited by Holocene samples from Byneskranskop 1.
This would then confirm that conditions were comparatively mild during that
period .
In fact , this is relative and for the earlier samples , from levels 14 up to 5 , the
index is within the range exhibited by Holocene samples from Byneskranskop 1.
This would then confirm that conditions were comparatively mild during that
period .
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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