ArticlePloS one2015
Vicariance and Its Impact on the Molecular Ecology of a Chinese Ranid Frog Species-Complex (Odorrana schmackeri, Ranidae).
Article in PloS one, 2015. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 9 papers.
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Who cites it
9 citing papers in PubMed.
- A New Species ofAnimals : an open access journal from MDPI · 2025Article
- Phylogeography and Species Distribution Modeling of Guizhou Odorous Frog (Ecology and evolution · 2025Article
- A new odorous frog species ofZooKeys · 2024Article
- Genomic insights into local adaptation in the Asiatic toadEvolutionary applications · 2023Article
- The phylogeographical pattern of the Amur minnowEcology and evolution · 2022Article
- Mitochondrial DNA phylogeography of the Guizhou odorous frog: limited population genetic structure and evidence for recent population size expansion.Mitochondrial DNA. Part B, Resources · 2021Article
- A new species ofZooKeys · 2021Article
- Phylogeography and demographic history ofEcology and evolution · 2020Article
- A new species of the odorous frog genusPeerJ · 2018Article
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6 authors.
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Abstract
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.
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