Fig. 3: Evolutionary assembly across bedrocks and elevational belts based on ClaSSE models. | Nature Communications

Fig. 3: Evolutionary assembly across bedrocks and elevational belts based on ClaSSE models.

From: Tempo and drivers of plant diversification in the European mountain system

Fig. 3: Evolutionary assembly across bedrocks and elevational belts based on ClaSSE models.The alternative text for this image may have been generated using AI.

a, c The differences between siliceous and calcareous habitats in constant-state speciation and migration rates, respectively. b, d The differences between high and mid-elevation habitats in constant-state speciation and migration rates, respectively. The dots represent mean parameter estimates and the bars indicate 95% credibility intervals, based on 5000 MCMC samples from the ClaSSE model posterior. Black dots and bars represent the shared parameter estimates from the multi-clade model, where each of the 6 phylogenies is regarded as an independent realization of the same diversification process. e The proportions of species inhabiting siliceous, calcareous or both types of habitats (light, dark and middle gray, respectively), and f the proportion of species inhabiting high elevation, mid-elevation or both types of habitats (light, dark and middle gray, respectively). Source data are provided as a Source Data file.

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