Diversification dynamics in the Neotropics through time, clades and biogeographic regions
Data files
Nov 28, 2022 version files 678.06 KB
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Dataset1.txt
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Dataset2.txt
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README_file.rtf
Abstract
The origins and evolution of the outstanding Neotropical biodiversity are a matter of intense debate. A comprehensive understanding is hindered by the lack of deep-time comparative data across wide phylogenetic and ecological contexts. Here, we quantify the prevailing diversification trajectories and drivers of Neotropical diversification in a sample of 150 phylogenies (12,512 species) of seed plants and tetrapods and assess their variation across Neotropical regions and taxa. Analyses indicate that Neotropical diversity has mostly expanded through time (70% of the clades), while scenarios of saturated and declining diversity account for 21% and 9% of Neotropical diversity, respectively. Five biogeographic areas are identified as distinctive units of long-term Neotropical evolution, including Pan-Amazonia, the Dry Diagonal, and Bahama-Antilles. Diversification dynamics do not differ across these areas, suggesting no geographic structure in long-term Neotropical diversification. In contrast, diversification dynamics differ across taxa: plant diversity mostly expanded through time (88%), while a substantial fraction (43%) of tetrapod diversity accumulated at a slower pace or declined toward the present. These opposite evolutionary patterns may reflect different capacities for plants and tetrapods to cope with past climate changes
Methods
Dataset 1. Chronogram dataset. To compile this dataset, Neotropical clades were extracted from large-scale time-calibrated phylogenies of frogs and toads (Hutter et al. 2017), salamanders (Pyron et al. 2013; Pyron, 2014), lizards and snakes (Pyron & Burbrink 2014), birds (Jetz et al. 2012) (including only species for which genetic data was available), mammals (Bininda-Emonds et al. 2007; Kuhn et al. 2011), and plants (Zanne et al. 2014). To identify independent Neotropical radiations, species in these large-scale phylogenies were coded as distributed in the Neotropics – delimited by the World Wide Fund for Nature WWF – or elsewhere using the R package speciesgeocodeR 1.0-4 (Töpel et al., 2017), and their geographical ranges extracted from the Global Biodiversity Information Facility “GBIF” (https://www.gbif.org/), the PanTHERIA database (https://omictools.com/pantheria-tool), BirdLife (http://www.birdlife.org) and eBird (http://ebird.org/content/ebird), all accessed in 2018, in a procedure similar to (Meseguer et al., 2020). Next, we pruned the trees to extract the most inclusive clades that contained at least 80% Neotropical species, as previously defined. This procedure ensures that the diversification signal pertains to the Neotropics. In addition, phylogenies of particular lineages not represented in the global trees (or with improved taxon sampling) were obtained from published studies or reconstructed de novo in this study (for caviomorph rodents, including 199 species; see SI). In the case of plants and mammals, most phylogenies were obtained from individual studies, given the low taxon sampling of the plant and mammal large-scale trees. However, whenever possible, we extracted phylogenies from a single dated tree rather than performing a meta-analysis of individual trees from different sources (Hoorn et al. 2010; Jansson et al. 2013), such that divergence times would be comparable. The resulting independent Neotropical radiations could represent clades of different taxonomic ranks. We did not perform any specific selection on tree size, crown age, or sampling fraction, but tested the effect of these factors on our results. Note that some of the phylogenies used in this study (10 trees) cannot be provided here, because they were obtained from third parties. These input phylogenies have to be obtained individually from the original sources
Dataset 2. Diversification results for each clade show the strength of support for constant, time-, temperature- and Andean uplift-dependent models by computing Akaike information criterion (AICc), ∆AICc, and Akaike weights (AICω). For each model category, we fitted three models in which speciation (B) and/or extinction (D) remain constant (cst), or vary continuously with time, with temperature changes, or with the elevation of the Andes. Abbreviations: NP = number of parameters; logL = log likelihood.
Usage notes
Both Datasets 1 and 2 could be opened with a simple text editor.
The 150 phylogenetic trees (Datasets 1), and the corresponding diversification results for each of these trees (Dataset 2), are presented concatenated to minimise the number of files uploaded.