Comparative phylogeography of Meriones meridianus, Dipus sagitta, and Allactaga sibirica: Potential indicators of the impact of the Qinghai-Tibetan Plateau uplift

Impacts of Quaternary glaciation, geological history and geography on animal species history in continental East Asia: A phylogeographic review

Continental East Asia has a mild Pleistocene climate and a complex recent geological history. Phylogeographic studies of animals over the last 30 years have produced several distinctive patterns. Glaciation refugia are numerous and are not restricted to any particular regions. Most of them are localized and species-specific, although several large refugia, for example the mountains of SW China, are shared by multiple species and have refugia-within-refugia. Furthermore, postglaciation range expansion events vary greatly in time, scale and direction. Large-scale south-to-north post-LGM expansions are few and mostly occurred in the northern regions. Additionally, several unique geographic features, including the three-step terrain of China and the northern arid belt, have significant impacts on many species histories. Overall, the impacts of Pleistocene glaciations, particularly the LGM, on species history vary drastically from nondetectable to significant. The impacts are the least for species from the southwestern region and are most dominant for species from the north. Geological events play a more significant role in shaping species history than Pleistocene climatic changes. Phylogeographic patterns among animals species are highly consistent with those of plants. Future phylogeographic endeavour in East Asia should be hypothesis-driven and seek processes that underlie common patterns. The wide use of genomic data allow accurate estimates of historical population processes and exploration of older history beyond the Pleistocene.

Genetic Variation and Phylogeography of Lumbriculus variegatus (Annelida: Clitellata: Lumbriculidae) Based on Mitochondrial Genes

Lumbriculus variegatus is a typical cold-water worm and is mainly distributed in the Tibetan Plateau and Northeast in China. The current study aimed to explore the genetic diversity and phylogeography of L. variegatus sampled from different geographical regions based on concatenated (COI + 16S rRNA, 879 bp) genes. Among 63 L. variegatus specimens, 29 haplotypes were identified with high haplotype diversity (h = 0.923) and nucleotide diversity (π = 0.062). The Bayesian phylogenetic analysis and Median-joining haplotype network revealed two lineages, or species, of L. variegatus. Taxa belonging to lineage I was mainly distributed in the Tibetan Plateau of China, North America, and Sweden, while lineage II composed taxa from Northeast China, southern China, and Sweden. The analysis of molecular variance indicated that the genetic difference was mainly due to differences between lineages. Neutrality tests showed that the overall L. variegatus have a stable population since the time of origin. Divergence time analysis suggested that L. variegatus originated from the Triassic period of Mesozoic in 235 MYA (95%HPD: 199–252 MYA), and the divergence between different lineages of L. variegatus began from the next 170 million years.

Population Genetic Structure of Chlorops oryzae (Diptera, Chloropidae) in China

Frequent outbreaks have made Chlorops oryzae one of the major pests of rice in some regions. In order to understand the ecological adaptation of C. oryzae at the molecular level, and provide a scientific basis for formulating management strategies, we used two molecular markers, COI and ITS1 sequences, to systematically analyze the genetic structure of 31 populations. The higher haplotype diversity and lower nucleotide diversity indicated that the C. oryzae populations experienced rapid expansion after a “Bottleneck effect”. The results of the mismatch distribution, neutrality test (Fu’s Fs < 0, p < 0.001), and haplotype network analysis suggested that the population has recently undergone an expansion. Although genetic differentiation among C. oryzae populations was found to have existed at low/medium levels (Fst: 0.183 for COI, 0.065 for ITS1), the frequent gene flow presented as well (Nm: 2.23 for COI, 3.60 for ITS1) was supposed to be responsible for frequent local outbreaks.

Geological and climatic influences on population differentiation of the Phrynocephalus vlangalii species complex (Sauria: Agamidae) in the northern Qinghai-Tibet Plateau

Extremely heterogeneous topography and complex paleoclimate history of the Qinghai-Tibet Plateau (QTP) have a key role in promoting genetic divergence and lineage/species formation. Here, we sequenced one nuclear and three mitochondrial markers of 532 individuals from the entire range of the Phrynocephalus vlangalii species complex including two species, P. putjatai and P. vlangalii, endemic to the northern QTP. We integrated multilocus phylogeny, demographic analysis and geographic barrier detection to evaluate the population structure and dynamics. We found a new mitochondrial clade (PV-I) in the Gonghe County population of P. vlangalii, partial mitochondrial DNA replacement within P. vlangalii and complete mitochondrial DNA replacement between P. putjatai and P. vlangalii. Neutrality test, mismatch distribution analysis and Extended Bayesian Skyline Plot (EBSP) analysis all supported a significant expansion of the Qaidam Basin population of P. vlangalii (PV-II-2) from 0.091 to 0.026 Ma after Penultimate Glaciation. The uplift of the Arjin and Anyemanqen Mountains during the Kunhuang Movement (∼1.2 Ma) split populations of P. vlangalii in Akesai, Qaidam Basin and source of the Yellow River. The uplift of the Elashan Mountains during the second phase of the Qingzang Movement (∼2.5 Ma) contributed to the divergence of the Gonghe County population of P. vlangalii from other conspecific populations. The third phase of the Qingzang Movement (∼1.7 Ma) contributed to the divergence of the Xinghai population of P. vlangalii from P. putjatai and to the divergence of the northern populations of P. putjatai from the southern conspecific populations. Our data support the idea that the geological and climatic changes following the orogeny of the QTP may have promoted population differentiation and shaped the current population patterns of the P. vlangalii species complex in the northeastern QTP.