Abstract

Effects of Pleistocene climatic oscillations on plant phylogeographic patterns are relatively well studied in forest, savanna and grassland biomes, but such impacts remain less explored on desert regions of the world, especially in South America. Here, we performed a phylogeographical study of Monttea aphylla, an endemic species of the Monte Desert, to understand the evolutionary history of vegetation communities inhabiting the South American Arid Diagonal. We obtained sequences of three chloroplast (trnS–trnfM, trnH–psbA and trnQ–rps16) and one nuclear (ITS) intergenic spacers from 272 individuals of 34 localities throughout the range of the species. Population genetic and Bayesian coalescent analyses were performed to infer genealogical relationships among haplotypes, population genetic structure, and demographic history of the study species. Timing of demographic events was inferred using Bayesian Skyline Plot and the spatio-temporal patterns of lineage diversification was reconstructed using Bayesian relaxed diffusion models. Palaeo-distribution models (PDM) were performed through three different timescales to validate phylogeographical patterns. Twenty-five and 22 haplotypes were identified in the cpDNA and nDNA data, respectively. that clustered into two main genealogical lineages following a latitudinal pattern, the northern and the southern Monte (south of 35° S). The northern Monte showed two lineages of high genetic structure, and more relative stable demography than the southern Monte that retrieved three groups with little phylogenetic structure and a strong signal of demographic expansion that would have started during the Last Interglacial period (ca. 120 Ka). The PDM and diffusion models analyses agreed in the southeast direction of the range expansion. Differential effect of climatic oscillations across the Monte phytogeographic province was observed in Monttea aphylla lineages. In northern Monte, greater genetic structure and more relative stable demography resulted from a more stable climate than in the southern Monte. Pleistocene glaciations drastically decreased the species area in the southern Monte, which expanded in a southeastern direction to the new available areas during the interglacial periods.

Highlights

  • Quaternary climatic oscillations profoundly impacted the abundance and distribution of organisms due to changes in landscape configuration, habitats and resource availability [1]

  • We evaluated model performance with statistics commonly used for judging the performance of species distribution models: the AUC, the true skill statistic (TSS), the proportion of presences and absences correctly categorized (PCC), the proportion of presences correctly

  • For M. aphylla, we observed a differential effect of Pleistocene climatic oscillations across the Monte phytogeographic province

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Summary

Introduction

Quaternary climatic oscillations profoundly impacted the abundance and distribution of organisms due to changes in landscape configuration, habitats and resource availability [1]. Paleoflora reconstructions for the late Quaternary period revealed that these fluctuations, involving cold, dry glacial cycles alternating with warm, moist interglacial periods, affected biotic diversity and evolution drastically at global scale Such impacts are relatively well studied in forest, savanna and grassland biomes, but remain less explored on desert regions of the world [2,3,4,5]. The small number of plant phylogeographic studies in arid lands, suggests that even drought-resistant plants suffered a reduction of suitable habitat due to the increased aridity and lower temperatures during Pleistocene glaciations, both in the northern (e.g. North America: [6,7,8]; Asia: [9, 10]) and southern hemisphere (e.g. Australia: [3]; South America: [11,12,13,14,15]) Some of these studies provided evidence that these climatic oscillations would have promoted allopatric divergence among isolated populations [11, 14] and, in some instances, drove speciation [9, 10]. With few exceptions [19,24], all phylogeographic studies involving this region are restricted to limited areas within the Monte Desert, focusing in organisms which do not inhabit exclusively this phytogeographical area, neither considering the whole extension nor the different environmental areas within the region

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