Table 2 Results of the multimodel inference at the grid cell scale for co1.

From: Evolutionary history and past climate change shape the distribution of genetic diversity in terrestrial mammals

Independent variables

AICc

R2

R2 adj

ΔAICc

wAICc

Moran’s I

P value (Moran’s I)

Phylogenetic diversity +temperature trend

−322.95

0.377

0.36

0

0.695

−0.038

0.38

Phylogenetic diversity

−320.88

0.341

0.332

2.07

0.246

−0.008

0.44

Species richness + temperature trend

−317.97

0.335

0.317

4.97

0.057

0.002

0.389

  1. All possible combinations of variables identified as significant from the hierarchical partitioning approach (see Supplementary Table 5) were evaluated using linear models. Models that contained highly collinear variables (Pearson’s |r| > 0.7) were excluded. The ranking of the models is based on the corrected Akaike’s information criterion (AICc). We retained only models with ΔAICc ≤ 5 compared to the best model (ΔAIC = 0). Residual spatial autocorrelation was computed for each retained explanatory model across spatial scales using Moran’s I and 10,000 simulations (P value). Note that all explanatory variables for co1 at the zoogeographic scale were insignificant.
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