Boschman, L. M. | bioRxiv Science

bioRxiv2021

South American freshwater fish diversity shaped by Andean uplift since the Late Cretaceous

South America is home to the highest freshwater fish biodiversity on Earth1,2. The hotspot of species richness is located in the western Amazon Basin, and richness decreases downstream along the Amazon River towards the mouth at the Atlantic coast (Fig. 1b, c)3,4, which contradicts the positive relationship between stream size and biodiversity that is commonly observed in river systems across the world5,6. We investigate the role of river rerouting events caused by Andean mountain building and repeated episodes of flooding in western Amazonia in shaping the modern-day richness pattern of freshwater fishes in South America. To this end, we combine a reconstruction of river networks following Andean surface uplift since 80 million years ago with a mechanistic biological model simulating dispersal, allopatric speciation and extinction over the dynamic landscape of rivers and lakes. We show that the numerous small river rerouting events in western Amazonia resulting from mountain building produced highly dynamic riverine habitats that caused high diversification rates, shaping the exceptional present-day richness of this region. The history of marine incursions and lakes, including the Miocene Pebas megawetland system in western Amazonia, played a secondary role. This study is a major step towards the understanding of the processes involved in the interactions between the solid Earth, landscapes, and life of extraordinary biodiverse South America. O_FIG O_LINKSMALLFIG WIDTH=200 HEIGHT=90 SRC="FIGDIR/small/444133v1_fig1.gif" ALT="Figure 1"> View larger version (35K): org.highwire.dtl.DTLVardef@c4643forg.highwire.dtl.DTLVardef@1916aa5org.highwire.dtl.DTLVardef@1f0900forg.highwire.dtl.DTLVardef@81ea9b_HPS_FORMAT_FIGEXP M_FIG O_FLOATNOFig. 1.C_FLOATNO a, Major rivers and drainage basins of South America. HydroRIVERS data from the HydroSHEDS database17; rivers shown that drain a surface area of >4000 km2. b, Freshwater fish species richness per sub-basin (level 5 HydroBASINS17), reproduced from data from Cassemiro, et al. 4. c and d, Richness versus distance to outlet per sub-basins (as shown in panel b), illustrating the positive relationship (richness decreases towards the mouth of the river) for the Amazon (c), and, for comparison, a negative relationship for the Parana-Paraguay river basin (d). C_FIG

evolutionary biology↗

bioRxiv2021

Mountain radiations are not only rapid and recent: ancient diversification of South American frog and lizard families related to Paleogene Andean orogeny and Cenozoic climate variations

Mountainous areas host a disproportionately large fraction of Earths biodiversity, suggesting a causal relationship between mountain building and biological diversification. Mountain clade radiations are generally associated with changes in environment, climate, and the increase in heterogeneity therein during mountain building. However, examining the causal relationship between mountain building and diversification is a complex challenge, because isolating the effects of surface uplift from other abiotic (climate) or biotic variables is not straightforward. In this study, we investigate the relative contributions of abiotic climate-driven (temperature) and geology-driven (elevation) drivers on evolutionary rates of ancient groups of organisms in the South American Andes. We present regional curves of Andean elevation based on a recent compilation of paleo-elevational data back to the Late Cretaceous, and analyse the diversification history of six Andean frog and lizard families that originated equally far back in time. For two clades (Aromobatidae and Leptodactylidae), we find that they diversified most rapidly during the early phase of mountain building (Late Cretaceous - Paleogene), when the first high-elevation habitats emerged in South America. The diversification of one clade (Centrolenidae) is correlated with Cenozoic temperature variations, with higher speciation rates during warm periods. The last three clades (Dendrobatidae, Hemiphractidae and Liolaemidae) are best explained by environment-independent diversification, although for Liolaemidae, an almost equally strong positive correlation was found between speciation and Andean elevation since the late Eocene. Our findings imply that throughout the long-lived history of surface uplift in the Andes, mountain building drove the diversification of different clades at different times, while not directly affecting other clades. Our study illustrates the importance of paleogeographic reconstructions that capture the complexity and heterogeneity of mountain building in our understanding of the effects that a changing environment plays in shaping biodiversity patterns observed today. HighlightsO_LIWe provide novel regional paleoelevation curves for the Andes back to the Late Cretaceous C_LIO_LIThe diversification history of six Andean-centered clades is studied C_LIO_LIWe find clade-specific responses to environmental changes C_LIO_LIThe impact of Andean uplift could reach further back in time than previously thought C_LI

evolutionary biology↗