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Understanding the factors that drive variation in species distribution is a central theme of ecological research. Although several studies focused on alpine vegetation, few efforts have been made to identify the environmental factors that are responsible for the variations in species composition and richness of alpine shrublands using numericalmethods. In the present study, we investigated vegetation and associated environmental variables from 45 sample plots in the middle Qilian Mountains of the northwestern China to classify different community types and to elucidate the speciesenvironment relationships. We also estimated the relative contributions of topography and site conditions to spatial distribution patterns of the shrub communities using the variation partitioning. The results showed that four shrub community types were identified and striking differences in floristic composition were found among them. Species composition greatly depended on elevation, slope,shrub cover, soil p H and organic carbon. The important determinants of species richness were soil bulk density and slope. No significant differences in species richness were detected among the community types. Topography and site conditions had almost equal effects on compositional variation. Nonetheless,a large amount of the variation in species composition remained unexplained. 相似文献
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HUO Qiuli ZENG Huasen ZHANG Xiaochang FANG Qinghu WANG Zhenying FU Li 《《地质学报》英文版》2015,89(Z1):151-153
<正>1 Introduction The technology breakthrough in the exploration of shale gas and tight oil has greatly extended the global fossil fuel resources(Jia et al.,2012;Zou et al.,2012;Qiu et al.,2013).Although shale oil has been the global hot topic in the study of unconventional resources,there are varied definitions with respect to shale oil by different researchers. 相似文献
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基于河西走廊疏勒河中下游绿洲天然胡杨林下8个采样点720个土壤样品和6.8524 hm2的7个样方,应用统计学及相邻格子法等研究了胡杨林土壤水盐的空间变化特征及其影响。结果表明:研究区土壤含水量随深度而增加,土壤全盐量变化与之相反,两者在80 cm土层之上变化剧烈,之下变化平缓;土壤水盐含量变异差异明显,均属于中强度变异。各层土壤水盐含量存在着自中游向下游水分减少、盐分增加、表层聚盐加重的显著空间分布规律。研究区胡杨林生长受到土壤水盐胁迫,种群结构残缺;下游胡杨林分偏老,稀疏矮小,已明显衰退。长此下去,下游胡杨林将因快速衰退演替而全部死亡。 相似文献
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