Bartish Igor V, Kadereit Joachim W, Comes Hans Peter
Department of Phanerogamic Botany, Swedish Museum of Natural History, PO Box 50007, S-10405 Stockholm, Sweden.
Mol Ecol. 2006 Nov;15(13):4065-83. doi: 10.1111/j.1365-294X.2006.03079.x.
Fossil pollen records indicate that Hippophaë rhamnoides (Sea Buckthorn) was widespread on late- and early postglacial raw soils throughout much of central and northern Europe, but that Early Holocene reforestation restricted populations to northern coastal habitats, or along mountain streams in the Alps, Pyrenees, and Carpathians. We used sequence variation at the nuclear chalcone synthase intron (Chsi), in conjunction with chloroplast DNA-restriction fragment length polymorphism data, to investigate the intraspecific phylogeny, phylogeographic structure, and expansion demographic history of this dioecious and wind-pollinated shrub at its range-wide scale in Europe and Asia Minor. Four major Chsi phylogroups of unresolved relationships were identified with estimated divergences approximately 172,000 years ago. Large-scale phylogeographic structures of nuclear and cytoplasmic markers were congruent in identifying (i) southeastern Europe as the most likely source of colonization into central Europe and Scandinavia, and (ii) the area just north of the Alps as a contact zone between populations from the Alps and the east/central European-Scandinavian lineage. Coalescence-based analyses (i.e. nested clade analysis and mismatch distributions) of Chsi variation were able to detect at least four major episodes of population growth, all within about the last 40,000 years. In particular, these analyses identified a nearly synchronized timing of population expansions in various parts of the species' range in central-eastern Europe/Asia Minor, most likely correlating with the Younger Dryas Stadial ( approximately 13,000-11,600 years ago). It remains to be established whether the phylogeographic history of H. rhamnoides, and particularly its rapid response to the rapid environmental changes of the Younger Dryas cold snap, is unique to the species, or whether it is shared with other cold-tolerant shrub (or grassland) species known from late-glacial raw soils in Europe.
化石花粉记录表明,沙棘在欧洲中部和北部的大部分地区晚冰期和冰后期早期的原始土壤中广泛分布,但全新世早期的重新造林将其种群限制在北部沿海栖息地,或阿尔卑斯山、比利牛斯山和喀尔巴阡山脉的山间溪流沿岸。我们利用核查尔酮合酶内含子(Chsi)的序列变异,结合叶绿体DNA限制性片段长度多态性数据,在欧洲和小亚细亚的全分布范围内,研究了这种雌雄异株且靠风授粉的灌木的种内系统发育、系统地理结构和扩张种群历史。识别出了四个主要的Chsi系统群,它们之间的关系尚未明确,估计分歧时间约在172,000年前。核标记和细胞质标记的大规模系统地理结构在确定(i)东南欧是最有可能向中欧和斯堪的纳维亚半岛殖民的来源地,以及(ii)阿尔卑斯山以北地区是阿尔卑斯山种群与东欧/中欧 - 斯堪的纳维亚谱系种群之间的接触带方面是一致的。基于合并的Chsi变异分析(即嵌套支系分析和错配分布)能够检测到至少四次主要的种群增长事件,均发生在约过去40,000年内。特别是,这些分析确定了中东欧/小亚细亚该物种分布范围内不同地区种群扩张的时间几乎同步,很可能与新仙女木期(约13,000 - 11,600年前)相关。沙棘的系统地理历史,尤其是其对新仙女木期寒冷骤变的快速环境变化的快速响应,是该物种独有的,还是与欧洲晚冰期原始土壤中已知的其他耐寒灌木(或草原)物种共有,仍有待确定。