RT Journal Article SR Electronic T1 Evolution of the latitudinal diversity gradient in the hyperdiverse ant genus Pheidole JF bioRxiv FD Cold Spring Harbor Laboratory SP 295386 DO 10.1101/295386 A1 Evan P. Economo A1 Jen-Pan Huang A1 Georg Fischer A1 Eli M. Sarnat A1 Nitish Narula A1 Milan Janda A1 Benoit Guénard A1 John T. Longino A1 L. Lacey Knowles YR 2018 UL http://biorxiv.org/content/early/2018/04/27/295386.abstract AB Aim The latitudinal diversity gradient is the dominant pattern of life on Earth, but a consensus understanding of its origins has remained elusive. The analysis of recently diverged, hyper-rich invertebrate groups provides an opportunity to investigate latitudinal patterns with the statistical power of large trees while minimizing potentially confounding variation in ecology and history. Here, we synthesize global phylogenetic and macroecological data on a hyperdiverse (>1100 species) ant radiation, Pheidole, and evaluate the roles of three general explanations for the latitudinal gradient: variation in diversification rate, tropical conservatism, and ecological regulation.Location Global.Time Period The past 35 million years.Major taxa studied The hyperdiverse ant genus Pheidole Westwood.Methods We assembled geographic data for 1499 species and morphospecies, and inferred a dated phylogeny of Pheidole of 449 species, including 150 species newly sequenced for this study. We tested correlations between diversification rate and latitude with BAMM, HiSSE, GeoSSE, and FiSSE, and examined patterns of diversification as Pheidole spread around the globe.Results We found that Pheidole diversification occurred in series of bursts when new continents were colonized, followed by a slowdown in each region. There was no evidence of systematic variation of net diversification rates with latitude across any of the methods. Additionally, we found latitudinal affinity is moderately conserved with a Neotropical ancestor and phylogenetic inertia alone is sufficient to produce the gradient pattern.Main Conclusions Overall our results are consistent with tropical conservatism explaining the diversity gradient, while providing no evidence that diversification rate varies systematically with latitude. There is evidence of ecological regulation on continental scales through the pattern of diversification after colonization. These results shed light on the mechanisms underlying the diversity gradient, while contributing toward a much-needed invertebrate perspective on global biodiversity dynamics.