scholarly journals Evolution of the latitudinal diversity gradient in the hyperdiverse ant genus Pheidole

2018 ◽  
Author(s):  
Evan P. Economo ◽  
Jen-Pan Huang ◽  
Georg Fischer ◽  
Eli M. Sarnat ◽  
Nitish Narula ◽  
...  

ABSTRACTAimThe 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.LocationGlobal.Time PeriodThe past 35 million years.Major taxa studiedThe hyperdiverse ant genus Pheidole Westwood.MethodsWe 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.ResultsWe 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 ConclusionsOverall 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.

2016 ◽  
Author(s):  
Michael G. Branstetter ◽  
John T. Longino ◽  
Joaquín Reyes-López ◽  
Ted R. Schultz ◽  
Seán G. Brady

Aim.The standard latitudinal diversity gradient (LDG), in which species richness decreases from equator to pole, is a pervasive pattern observed in most groups of organisms. Despite its commonness, an increasing number of non-conforming lineages have been identified, presenting a challenge for general explanations of the standard LDG. Although problematic, documenting and studying these contrarian groups can help us to better understand LDGs generally. To that end we identify the ant tribe Stenammini, a diverse lineage with over 400 species, as a contrarian clade, and we attempt to explain the group's atypical diversity pattern using a historical approach. We evaluate the following alternative hypotheses: time-for-speciation/center-of-origin (TFS/COO), niche conservatism, and differences in diversification rate.Location.Global.Methods.We examine the shape of the LDG in Stenammini by plotting latitudinal midpoints for all extant species. We then infer a robust phylogeny using a phylogenomic approach that employs ultraconserved element loci and we use the phylogeny to estimate divergence dates, biogeographic history, and ancestral habitats. We also test for diversification rate heterogeneity across the tree and among lineages within the tribe.Results.Stenammini has a skewed inverse latitudinal diversity gradient with an extratropical richness peak in the northern temperate zone. Our phylogenomic approach resulted in a robust phylogeny revealing five major clades and several instances of non-monophyly among genera (Goniomma,Aphaenogaster). The tribe and most major lineages originated in the temperate zone and inhabited temperate niches. Crown Stenammini dates to 52 Ma (Eocene Climatic Optimum) and most major lineages appeared soon after during a period of global cooling. Despite its temperate origin, the group invaded the tropics at least six times, but failed to diversify greatly there. Across the tree diversification increased from 17.2-1.9 Ma following the Mid-Miocene Climatic Optimum, and among lineages there was a rate increase in HolarcticAphaenogaster+Messorjust prior to 17.2 Ma.Main Conclusions.Our results suggest that time, niche conservatism, and increased diversification have all contributed to the inverse latitudinal gradient in Stenammini. Among these processes, niche conservatism may be less important given that the tribe has dispersed to the tropics multiple times.


2012 ◽  
pp. n/a-n/a
Author(s):  
Harald SCHNEIDER ◽  
Li-Juan HE ◽  
Jeannine MARQUARDT ◽  
Li WANG ◽  
Jochen HEINRICHS ◽  
...  

2019 ◽  
Vol 34 (3) ◽  
pp. 211-223 ◽  
Author(s):  
Mikael Pontarp ◽  
Lynsey Bunnefeld ◽  
Juliano Sarmento Cabral ◽  
Rampal S. Etienne ◽  
Susanne A. Fritz ◽  
...  

2018 ◽  
Vol 121 (4) ◽  
pp. 480 ◽  
Author(s):  
Aline Anjos de Menezes ◽  
Marcela Eugenia da Silva Cáceres ◽  
Cid José Passos Bastos ◽  
Robert Lücking

2015 ◽  
Vol 24 (9) ◽  
pp. 1059-1071 ◽  
Author(s):  
Jonathan Rolland ◽  
Fabien L. Condamine ◽  
Champak R. Beeravolu ◽  
Frédéric Jiguet ◽  
Hélène Morlon

2018 ◽  
Vol 21 (8) ◽  
pp. 1229-1236 ◽  
Author(s):  
Kevin Frank ◽  
Frank-Thorsten Krell ◽  
Eleanor M. Slade ◽  
Elizabeth H. Raine ◽  
Li Yuen Chiew ◽  
...  

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