2020
DOI: 10.1080/24701394.2020.1779239
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Genetic diversity and structure of the Chinese lake gudgeon ( Sarcocheilichthys sinensis )

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Cited by 3 publications
(2 citation statements)
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“…The geographic distributions of Lineage B display a few haplotypes across two or three drainages, while other haplotypes are confined to a single drainage (Figure 3B). Our timing of the crown age of the Lineage B at ~0.40 Ma (node 2 in Figure 2) indicates that the phylogeographic pattern in Lineage B could be explained by recent historical connections among the lower Yangtze River, Qiantang River, Jiaojiang River, and Ou River (Chen et al, 2017;Ding et al, 2020;Yang et al, 2022). The recent historical connections between the Yangtze and Qiantang rivers are supported by the coalescence of the two rivers during the Last Glacial Maximum (Figure 1).…”
Section: Major Drivers Of the Lineage Diversificationmentioning
confidence: 83%
“…The geographic distributions of Lineage B display a few haplotypes across two or three drainages, while other haplotypes are confined to a single drainage (Figure 3B). Our timing of the crown age of the Lineage B at ~0.40 Ma (node 2 in Figure 2) indicates that the phylogeographic pattern in Lineage B could be explained by recent historical connections among the lower Yangtze River, Qiantang River, Jiaojiang River, and Ou River (Chen et al, 2017;Ding et al, 2020;Yang et al, 2022). The recent historical connections between the Yangtze and Qiantang rivers are supported by the coalescence of the two rivers during the Last Glacial Maximum (Figure 1).…”
Section: Major Drivers Of the Lineage Diversificationmentioning
confidence: 83%
“…ENMs confirmed the existence of several refugias in southwest China, southern China, and Southeast Asia (Figure 9A). Several population demographic studies across East Asia uncovered that some organisms with similar distribution have not been influenced by past climate change events associated with glacial cycles (e.g., Nanorana yunnanensis : Zhang et al., 2010; Quasipaa boulengeri : Yan et al., 2013; Sarcocheilichthys sinensis : Ding et al., 2020; Odorrana graminea : Chen et al., 2020). In the Middle Holocene (0.007–0.0025 Mya), a warm climate led to population expansion (Figure 8.…”
Section: Discussionmentioning
confidence: 99%