Skip to main content
. 2014 Sep 9;9(9):e106499. doi: 10.1371/journal.pone.0106499

Table 2. Results of best fit generalized least squares models relating β diversity and latitudinal turnover gradient (LTG) strength to mean annual precipitation from paleosols (Retallack, 2007), δ18O (‰) from benthic forams (mm/year; Zachos et al. 2001; 2008), length of North American Land Mammal Age subdivision, number of taxa sampled, sampling area (km2), and number of fossil localities.

Dependent Variable Parameters of BestFit Model Variance explainedby model (%) t value p
Beta Diversity Mean annual precipitation (quadratic) 66.51 −3.25 0.005
Length of NALMA subdivision 2.43 0.027
Number of taxa 5.30 <0.001
Beta Diversity Residuals Mean annual precipitation (quadratic) 26.48 −3.50 0.002
Beta Diversity Re-sampled Mean annual precipitation (quadratic) 66.04 −2.39 0.029
Length of NALMA subdivision 2.51 0.023
Number of taxa 5.47 <0.001
Latitudinal Turnover Gradient Strength (LTGs) Mean annual precipitation (quadratic) 46.76 −5.65 <0.001
Area −4.62 <0.001
Number of taxa −4.36 <0.001
Area : Number of taxa 4.85 <0.001
LTG Residuals Mean annual precipitation (linear) 37.48 −3.79 0.001
LTG Re-sampled Number of taxa 28.59 −2.55 0.020