Vicariance and Its Impact on the Molecular Ecology of a Chinese Ranid Frog Species-Complex (Odorrana schmackeri, Ranidae)

• Published in: PloS one 2015-09, Vol.10 (9), p.e0138757-e0138757
• Main Authors: Li, Yongmin, Wu, Xiaoyou, Zhang, Huabin, Yan, Peng, Xue, Hui, Wu, Xiaobing
• Format: Article
• Language: English
• Subjects: Amphibians; Analysis; Animals; Bayes Theorem; Biodiversity; Canyons; China; Climate change; Conservation; Cryptic species; Demographics; Demography; Divergence; DNA, Mitochondrial - chemistry; DNA, Mitochondrial - genetics; East Asian monsoon; Ecology; Evolution; Evolution, Molecular; Exploitation; Frogs; Gene sequencing; Genetic diversity; Genetic structure; Genetic Variation; Geography; Geology; Haplotypes; Laboratories; Last Glacial Maximum; Life sciences; Mitochondria; Molecular Sequence Data; Monsoons; Mountains; ND2 gene; Paleogeology; Phylogeny; Phylogeography; Pleistocene; Pliocene; Population genetics; Population growth; Population studies; Ranidae; Ranidae - classification; Ranidae - genetics; Refugia; Sequence Analysis, DNA; Species; Species Specificity; Studies; Summer monsoon; Time Factors; Uplift
• ISSN: 1932-6203; 1932-6203
• DOI: 10.1371/journal.pone.0138757

Paleogeological events and Pleistocene climatic fluctuations have had profound influences on the genetic patterns and phylogeographic structure of species in southern China. In this study, we investigated the population genetic structure and Phylogeography of the Odorrana schmackeri species complex, mountain stream-dwelling odorous frogs, endemic to southern China. We obtained mitochondrial sequences (1,151bp) of the complete ND2 gene and two flanking tRNAs of 511 individuals from 25 sites for phylogeographic analyses. Phylogenetic reconstruction revealed seven divergent evolutionary lineages, with mean pairwise (K2P) sequence distances from 7.8% to 21.1%, except for a closer ND2 distance (3.4%). The complex geological history of southern China drove matrilineal divergence in the O. schmackeri species complex into highly structured geographical units. The first divergence between lineage A+B and other lineages (C-G) had likely been influenced by the uplift of coastal mountains of Southeast China during the Mio-Pliocene period. The subsequent divergences between the lineages C-G may have followed the formation of the Three Gorges and the intensification of the East Asian summer monsoon during the late Pliocene and early Pleistocene. Demographic analyses indicated that major lineages A and C have been experienced recent population expansion (c. 0.045-0.245 Ma) from multiple refugia prior to the Last Glacial Maximum (LGM). Molecular analysis suggest that these seven lineages may represent seven different species, three described species and four cryptic species and should at least be separated into seven management units corresponding to these seven geographic lineages for conservation.