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本研究自胶州湾分离了两种底栖硅藻,形态学初步鉴定为长菱形藻和新月细柱藻。对其18S rDNA和rbcL基因进行了测序并用邻接法构建了系统树。结果表明,两藻在18S rD-NA和rbcL基因序列上均存在较大的差异,基于DNA序列的分类结果与形态学分类结果一致。在依据形态指标难以确定藻类分类地位的情况下,18S rDNA和rbcL基因序列是有用的鉴定工具。  相似文献   
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Geotechnical and Geological Engineering - Grout curtains are commonly constructed under dams to reduce the seepage through the rock foundation. In the design of grout curtains, empirical methods...  相似文献   
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The genus Cylindrotheca consists of a small group of marine diatoms with a few species described. Eleven isolates of diatoms identified as Cylindrotheca closterium morphologically were obtained from Jiaozhou Bay with their nuclear-encoded small-subunit ribosomal RNA (SSU rDNA) and chloroplast-encoded rbcL gene sequences determined in this study. Interestingly, very high sequence divergences of SSU rDNA and rbcL gene were found among these isolates, and numerous nucleotide variation of rbcL gene caused relatively few variation of deduced amino acid sequence. Phylogenetic analyses based on SSU rDNA and rbcL gene, respectively, grouped the isolates into 6 clades. Phylogenetic tree of SSU rDNA placed all the Cylindrotheca isolates together, separating them into two lineages clearly. LineageⅠ was composed of the eleven C. closterium isolates obtained in this study together with another C. closterium isolate, but some clades were not well supported. LineageⅠwas contained two C. closterium isolates and one C. fusiformis isolate. Phylogenetic analysis of rbcL gene also separated the Cylindrotheca isolates into two well-defined lineages. The eleven C. closterium isolates formed a lineage and all clades were supported strongly. Statistical comparisons of SSU rDNA indicated that the average distance within lineageⅠwas significantly higher than that of other microalgae species (P 〈0.01). These results suggested the existence of cryptic species within C. closterium.  相似文献   
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新疆哈密红石铜矿控矿构造研究   总被引:1,自引:0,他引:1       下载免费PDF全文
红石铜矿是一个新近发现并勘查的超大中低温火山热液型铜矿床。文章通过对矿区构造特征、控矿构造形式的研究,阐述了红石铜矿的控矿构造主要表现为:矿区的EW-NWW向、SN向断裂是控岩(火山岩)控矿构造;断裂构造类型、活动方式控制着矿脉(体)形态、矿石组构;成矿期后构造叠加改造强烈,NE-NEE向断裂构造是破矿断裂;构造应力场方向为成矿前期近SN向挤压,主成矿期为NNE向,成矿期后变为近SN向。  相似文献   
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