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BIODIVERSITY AND CLIMATE 193

Table 7. Spearman rank test rho values for environmental variables and the percentage of fauna that are
represented by herptile (amphibian + reptile) species, by region


n
Absolute latitude
Elevation
MAT
MART
CMM
WMM
Radiation
Cumulative T 0
Cumulative T 5
Annual precipitation
P range
Months T 10 P 40
PET
Mean annual NDVI
NDVI ISD


South
America

_ - - - - - - - - - - - - - - -

North
America

144
-0.923
NS
0.902
-0.489
0.820
0.897
NS
0.913
0.918
0.520
0.333
0.799
0.901
0.816
-0.832

Europe

204
-0.861
NS
0.769
NS
0.602
0.792
0.830
0.772
0.807
NS
NS
0.380
0.781
0.588
-0.817

Arabia

_ - - - - - - - - - - - _ - - -

Southern
Africa

21
NS
NS
NS
NS
NS
NS
NS
NS
NS
NS
NS
NS
NS
NS
NS

Australia

40
NS
NS
NS
NS
NS
NS
NS
NS
NS
-0.731
NS
-0.763
NS
NS
NS

(p < 0.0001; NS, not significant, p > 0.0001)

consequences of barriers to dispersal during the

Cenozoic. Similarly, the diversity of most

organic groups follows distinct patterns of diver-

sification through time (Sepkoski 1996), which

means that the overall diversity of any group at

a specific moment will depend on where it is

placed in its diversification history.

These historical factors appear to affect the

taxonomic composition of the fauna (names),

rather than absolute numbers or the relationship

between species diversity and environmental

variables. The correspondence analysis of North

American and European non-avian tetrapod

generic names (Figs 13 and 14, Table 8),

supports this. Axis 1 (Fig. 14) reflects historical

compositional differences between the two

continents, but the remaining variance com-

prises the physiological structure of the diversity

(temperature, axis 2, and water, axis 3; Figs 13

and 14), which dominate when the continents

are considered individually. This is consistent

with studies of Pleistocene beetle assemblages

that provide a sensitive measure of palaeo-

climate throughout the Quaternary (Atkinson et

al 1986). Despite the fact that with each inter-

glacial-glacial fluctuation the composition of the

Fig. 13. The results of a correspondence analysis (CA) of North American and European genera, (a) Axes 1
and 2, which comprise 65.2% of the total variance, (b) Axes 3 and 4.

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