Geologic history explains freshwater fish species richness across the conterminous USA
On this page:
Freshwater fishes comprise over 20% of extant vertebrate biodiversity despite occupying <1% of the Earth’s surface area, while species richness across river basins differs by several orders of magnitude. Explanations for these patterns often invoke spatial variation in origination times, diversification rates, and local species capacities, as well as how these macroevolutionary processes are shaped by landscape change over geologic timescales. However, most large-scale fish biodiversity studies have focused on species pools aggregated across entire river basins, even though species richness and geologic history can vary substantially among sites within basins. In this study, we analyzed freshwater fish species richness from a spatially representative survey of streams and rivers across the conterminous United States, which provided 5,321 observations from 3,609 unique sites and sampled 466 native species. We hypothesized that species richness would exhibit predictable patterns based on regional geologic history and would be positively associated with species origination times. To test these hypotheses, we used spatial linear models to relate species richness to proxies of geologic history (tectonic activity, glaciation, sea level fluctuations, river capture frequency), species capacity, and an independent phylogenetic origination time dataset. Results often, but not always, supported our initial hypotheses. Within tectonically stable regions east of the Rocky Mountains, richness was highest in unglaciated lowlands as predicted, but was lower than expected in unglaciated highlands and higher than expected in glaciated regions. Richness was lowest in tectonically active western regions, which largely contained assemblages dominated by species with young evolutionary origins. This study demonstrates that large-scale and deep-time processes can leave a persistent mark on species richness, which could conceivably extend to other aspects of community assembly. Moreover, the geologic history proxies developed in this study should support more accurate assessments of aquatic biodiversity and biological condition in the United States and beyond.