Figure 3: Regional plots of subsampled biodiversity versus palaeolatitudinal centroid and subsampling curves for non-marine genera.
From: Climate constrains the evolutionary history and biodiversity of crocodylians
(a) Triassic–early Late Cretaceous (K6) subsampled biodiversity versus palaeolatitudinal centroid. (b) Late Triassic (Tr4) log10-transformed subsampling curves. (c) Late Cretaceous (K7 and K8) subsampled biodiversity versus palaeolatitudinal centroid. (d) Paleogene subsampled biodiversity versus palaeolatitudinal centroid. (e) Neogene subsampled biodiversity versus palaeolatitudinal centroid. (f) Early Neogene (Ng1) log10-transformed subsampling curves. (g) Middle Neogene (Ng2) log10-transformed subsampling curves. Dashed arrows denote notable changes in biodiversity between consecutive time intervals within a single continental region. K, Cretaceous; Ng, Neogene; Tr, Triassic.
