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We studied the phylogeography of Swertia tetraptera Maxim, which is an annual herbaceous plant endemic to the Qinghai-Tibetan Plateau (QTP), by sequencing one intergenic chloroplast spacer, trnL-trnF (773 bp). The sampling design included 35 populations and 399 individuals, and spanned the entire distribution of the species. Forty-four haplotypes were characterized, and one of them was widely distributed in all of the populations. The level of differentiation among the populations studied was relatively low (GST = 0.128). Estimates of NST -GST for populations of S. tetraptera indicated that no phylogeographical structure exists, which was supported by the distribution of haplotypes. The neutrality test, mismatch distribution and a ‘star-like’ genealogy all suggested that this species experienced population expansion. According to the number of rare haplotype and geological evidence, this study suggested that two potential refugia existed during the last glaciation: the first refugium was identified in a restricted semi-continuous area around the eastern margin of the plateau; the second refugium was located in the central of QTP. In fact, the findings of our study are somewhat similar as the third phylogeographical structure occurring in the QTP, that is, alpine plants have refugia not only in the edge area but also in the Plateau platform. However, the location of plateau edge and plateau platform refugia is very different among them due to the difference of species-specific characteristic such as distributional range and life history traits.
Using the characteristic of accumulated woody debris, data on vegetation, and data on previous climate fluctuations, we reconstructed the history of Scots pine (Pinus sylvestris L.) encroachment and retreat in a raised bog. The available patchy information on plant cover allowed us to pinpoint events in the development of pine seedlings and the first cases of trees dying off on the time scale. The results obtained show that the process of natural bog afforestation and deforestation was very dynamic and lasted only 22 years. These short-term changes in the tree populations were clearly linked to short-term climate fluctuations. The annual precipitation and mean temperature of winter months were the most important variables and the main factors directly influencing the young woodland. We assumed that the woody remnants represent the last stage of the contemporary phase of high germination and dying-off (GDO) of pine trees. The spatial distribution of woody debris and its characteristics indicate the naturalness of vegetation during this temporary ‘woodland phase’. The study show that the investigation of woody debris can be used to further improve our understanding of bog vegetation dynamics, especially with regard to the influence of periodical climate fluctuations on transitions between open and forested peatland.
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