Abstract

The Tehuacán-Cuicatlán Valley, located at the southeast of the state of Puebla and the northeast of the state of Oaxaca in Central Mexico, south of the Trans-Mexican Volcanic Belt (TMVB), is of particular interest for understanding the evolutionary dynamics of arid and semi-arid environments, being one of the main reservoirs of biological diversity for the arid zones of North America, including the highest diversity of Agavaceae worldwide and high levels of endemism. Studying in detail the phylogeography, environmental history and population genetics of representative species will hopefully shed light on the evolutionary and ecological dynamics that generated the tremendous biodiversity and endemism of this important region in Mexico. We sequenced three non-coding regions of chloroplast genome of Agave kerchovei, a representative species of the Tehuacán Valley, generating 2,188 bp from 128 individuals sampled from eight populations throughout the species range. We used this data set to (i) characterize the levels of genetic diversity and genetic structure in A. kerchovei; (ii) predict the distribution of A. kerchovei for the present day, and to reconstruct the past geographical history of the species by constructing ecological niche models (ENM); and (iii) compare the levels of diversity in this species with those estimated for the widely distributed Agave lechuguilla. Agave kerchovei has high levels of total chloroplast genetic variation (Hd = 0.718), especially considering that it is a species with a very restricted distribution. However, intrapopulation diversity is low (zero in some populations), and genetic structure is high (FST = 0.928, GST = 0.824), which can be expected for endemic species with isolated populations. Our data suggest that Pleistocene glacial cycles have played an important role in the distribution of A. kerchovei, where the climatic variability of the region – likely associated with its topographic complexity – had a significant effect on the levels of genetic diversity and population dynamics, while the potential distribution of the species seems to be stable since the middle Holocene (6 kya). We conclude that in A. kerchovei there is a core group of populations in the Tehuacán Valley, and peripheric populations that appear to be evolving independently and thus the species is fundamentally an endemic species from the Tehuacán Valley while the populations outside the Valley appear to be in the process of incipient speciation.

Highlights

  • The Pleistocene glacial periods have been major factors influencing the geographical distribution, demographic dynamics and patterns of genetic diversity of many species (Haffer and Prance, 2001; Hewitt, 2004; Stewart et al, 2010; Ramírez-Barahona and Eguiarte, 2013; Castellanos-Morales et al, 2016)

  • As occurs in many rare or endemic species with few and usually small populations, some of its populations are completely depleted of genetic variation and genetic structure is high, which may be a consequence of demographic phenomena such as inbreeding, genetic bottlenecks or drift (Hamrick and Godt, 1990; Nybom and Bartish, 2000; Gibson et al, 2008)

  • Pleistocene glacial cycles had an important role in the distribution of A. kerchovei, and climatic variability appears to have had a significant effect on the levels of genetic diversity and differentiation among populations

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Summary

Introduction

The Pleistocene glacial periods have been major factors influencing the geographical distribution, demographic dynamics and patterns of genetic diversity of many species (Haffer and Prance, 2001; Hewitt, 2004; Stewart et al, 2010; Ramírez-Barahona and Eguiarte, 2013; Castellanos-Morales et al, 2016). The Tehuacán Valley is located at the southeast of the state of Puebla and the northeast of the state of Oaxaca in Central Mexico, south of the Trans-Mexican Volcanic Belt (TMVB), representing the southernmost semiarid area in Mexico (Rzedowski and Huerta, 1978; Hafner and Riddle, 2011; El-Ghani et al, 2017) (Figure 1A). It has a distinctive biotic megadiversity and it is one of the main reservoirs of biological diversity for the arid zones of North America. According to Valiente-Banuet et al (2009) the late Pleistocene climate changes (10,000 to 1,000 kya) were very important for the current geomorphic and biotic composition of the Tehuacán Valley, suggesting that local plant communities were recently assembled

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