Journal
JOURNAL OF BIOGEOGRAPHY
Volume 41, Issue 11, Pages 2162-2172Publisher
WILEY
DOI: 10.1111/jbi.12358
Keywords
Biogeography; divergence time; glacial refugia; long-distance dispersal; migration corridors; mitochondrial DNA; phylogeography; Thermophis baileyi; Tibetan Plateau uplift; Yarlung River
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Funding
- German Research Council [MI 271/21]
- 'Network for University Co-operation Tibet-Norway'
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AimOur aims were to investigate the geographical distribution, population history and demographics of the hot-spring snake Thermophis baileyi, and to examine how the Pleistocene glacial stages and geomorphological configurations resulting from the uplift of the Tibetan-Himalayan orogen shaped the genetic diversity and evolutionary history of the species. LocationTibetan Plateau. MethodsWe surveyed potential habitat sites throughout Tibet. Sequence data were obtained for three mitochondrial markers (ND2, ND4 and cytb; 2185bp) in 181 individuals from 18 populations across the species' distribution range. We conducted population-genetic (samova; baps), phylogenetic (maximum likelihood; Bayesian), demographic (Tajima's D; Fu's F-S; mismatch distribution) and ecological analyses (logistic regression for presence/absence data) to examine the recent distribution, evolutionary history and diversification of the species. ResultsThe geographical range of T.baileyi is a restricted area between the Transhimalaya and the Himalaya, along the central part of the Yarlung Tsangpo suture zone. The divergence times of sequences matched the Guxiang glaciation (300-130ka) and the last glacial period (70-10ka). We observed two genetically distinct lineages north of the Yarlung Tsangpo river. These lineages are known from previous work and are largely congruent with a division across the drainage divide of the Nyainqentanglha rift. Haplotype grouping based on cluster analysis indicated the existence of riverine migration corridors between populations. Main conclusionsThe evolutionary history of T.baileyi is consistent with a model of range expansion from different refugia during interglacial and post-glacial times. All lines of evidence suggest that Pleistocene glacial oscillations, triggered by tectonic activity during plateau uplift, have had the strongest influence on intraspecific differentiation. Physical barriers, such as high-elevation mountains and the drainage system, however, also appear to have affected the population structure and distribution of this snake. Population clustering suggests that there has been long-distance dispersal along riverine corridors.
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