Abstract
The significance of the Chinese Loess Plateau (CLP) in maintaining biodiversity for northern China has rarely been shown, as previous phylogeographic studies are mostly woody species and they have revealed that Quaternary refugia are mainly located in mountain regions. We selected a drought-enduring endemic herb, Speranskia tuberculata (Euphorbiaceae), to determine its glacial refugia and postglacial demographic history. To this end, we sampled 423 individuals from 38 populations covering its entire geographic distribution. Three chloroplast DNA (cpDNA) fragments, two low-copy nuclear genes, and six nuclear microsatellites (nSSRs) were used and supplemented with ecological niche modeling (ENM) to infer the phylogeographic history of this species. Populations with private haplotypes and high haplotype diversity of cpDNA are mainly located in the CLP or scattered around northeastern China and the coastal region. Spatial expansion, detected using a neutrality test and mismatch distribution, may have resulted in a widely distributed ancestral cpDNA haplotype, especially outside of the CLP. For nuclear DNA, private haplotypes are also distributed mainly in the CLP. In nSSRs, STRUCTURE clustering identified two genetic clusters, which are distributed in the west (western cluster) and east (eastern cluster), respectively. Many populations belonged, with little to no admixture, to the western cluster while (hardly) pure populations of the eastern cluster were barely found. Genetic differentiation is significantly correlated with geographic distance, although genetic diversity is uniformly distributed. ENM suggests that the distribution of S. tuberculata has recently expanded northwards from the southern CLP, whereas it has experienced habitat loss in the south. Thus, S. tuberculata populations probably survived the last glacial maximum (LGM) in the southern CLP and experienced post-glacial expansion. Wind-dispersed pollen could bring the majority of genotypes to the front during spatial expansion, resulting in uniformly distributed genetic diversity. Based on evidence from molecular data and vegetation and climate changes since the LGM, we conclude that drought-enduring species, especially herbaceous species, are likely to have persisted in the CLP during the LGM and to have experienced expansion to other regions in northern China.
Highlights
The Chinese Loess Plateau (CLP), which spans from 34 – 40◦N and 101 – 113◦E in northern China, contains heterogeneous topography and climate (Zhang et al, 2002) and is at the intersection of multiple floristic regions (Wang, 1999; Wu et al, 2010)
Paleovegetation reconstruction for northern China indicates that steppe and even desert vegetation covered this area during the last glacial maximum (LGM, ca. 26,000 – 18,000 years ago), while the present coniferous and deciduous forests experienced southward retreat to below 30◦N (Harrison et al, 2001; Ni et al, 2010)
34 variable sites including 15 indels were detected in 423 S. tuberculata individuals, and 26 haplotypes were identified with a total of 2,600 bp using three chloroplast fragments (Supplementary Table 3)
Summary
The Chinese Loess Plateau (CLP), which spans from 34 – 40◦N and 101 – 113◦E in northern China, contains heterogeneous topography and climate (Zhang et al, 2002) and is at the intersection of multiple floristic regions (Wang, 1999; Wu et al, 2010). Phylogeographic studies, challenged this hypothesis by discovering multiple LGM refugia, which have allowed species to persist across northern China (Chen et al, 2008; Tian et al, 2009; Zeng et al, 2011). Multiple localized refugia patterns were discovered in a tree, Quercus liaotungensis (Zeng et al, 2011) and a shrub, Ostryopsis davidiana (Tian et al, 2009), as different plastid haplotypes were geographically restricted. Other studies on widely distributed East Asian species have shown that northern China is likely a contact zone between southern subtropical and northern cold temperate populations (Guo et al, 2014; Bai et al, 2016)
Sign-in/Register to view highlights & summary Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
