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An endemic rat species complex is evidence of moderate environmental changes in the terrestrial biodiversity centre of China through the late Quaternary
Author(s) -
Deyan Ge,
Liang Lu,
Jilong Cheng,
Lin Xia,
Ying Chang,
Zhixin Wen,
Xue Lv,
Yuanbao Du,
Qiyong Liu,
Qisen Yang
Publication year - 2017
Publication title -
scientific reports
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.24
H-Index - 213
ISSN - 2045-2322
DOI - 10.1038/srep46127
Subject(s) - biodiversity , ecology , quaternary , biology , holarctic , range (aeronautics) , clade , endemism , population , geography , phylogenetics , paleontology , genus , biochemistry , materials science , demography , sociology , gene , composite material
The underlying mechanisms that allow the Hengduan Mountains (HDM), the terrestrial biodiversity centre of China, to harbour high levels of species diversity remain poorly understood. Here, we sought to explore the biogeographic history of the endemic rat, Niviventer andersoni species complex (NASC), and to understand the long-term persistence of high species diversity in this region. In contrast to previous studies that have proposed regional refuges in eastern or southern of the HDM and emphasized the influence of climatic oscillations on local vertebrates, we found that HDM as a whole acted as refuge for the NASC and that the historical range shifts of NASC mainly occurred in the marginal regions. Demographic analyses revealed slight recent population decline in Yunnan and south-eastern Tibet, whereas of the populations in Sichuan and of the entire NASC were stable. This pattern differs greatly from classic paradigms of temperate or alpine and holarctic species. Interestingly, the mean elevation, area and climate of potential habitats of clade a ( N. excelsior ), an alpine inhabitant, showed larger variations than did those of clade b ( N. andersoni ), a middle-high altitude inhabitant. These species represent the evolutionary history of montane small mammals in regions that were less affected by the Quaternary climatic changes.

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