Annals of the South African Museum |
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Page 232
It is also consequently more flexible in achieving the best possible clustering of
variables , particularly where moderate or high correlations are shown to exist
between factors . This means , in effect , that the higher the correlation between
the ...
It is also consequently more flexible in achieving the best possible clustering of
variables , particularly where moderate or high correlations are shown to exist
between factors . This means , in effect , that the higher the correlation between
the ...
Page 331
1979 ) has correlated the Eemian ( Last ) Interglacial with oxygen - isotope stage
5e by means of analysis of pollen and marine fossils . ... 1972 ) . There is ,
however , good general correlation between the different ice - cores ( Johnsen et
al .
1979 ) has correlated the Eemian ( Last ) Interglacial with oxygen - isotope stage
5e by means of analysis of pollen and marine fossils . ... 1972 ) . There is ,
however , good general correlation between the different ice - cores ( Johnsen et
al .
Page 337
Although it is not possible to be precise about the correlation , it is clear that
fluctuations were occurring in the south which were very similar to those in ...
Palaeoenvironmental unit 3 can be correlated with the upper pleniglacial , 180
stage 2.
Although it is not possible to be precise about the correlation , it is clear that
fluctuations were occurring in the south which were very similar to those in ...
Palaeoenvironmental unit 3 can be correlated with the upper pleniglacial , 180
stage 2.
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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