赤潮铜绿微囊藻rDNA基因间隔区的序列分析以及与淡水微囊藻的比较   总被引：3，自引：0，他引：3  

陈月琴  庄丽  屈良鹄  郑天凌  王大志  王艳丽 《海洋科学》1999,23(1):48-50

采用ＰＣＲ及序列测定 厦门西港海域采集的赤潮铜绿微囊藻１６Ｓ和２３Ｓ ｒＤＮＡ基因间隔区Ｉｎｔｅｒｇｅｎｉｃ Ｓｐａｃｅｒ Ｒｅｇｉｏｎ（ＩＳＲ）区进行了序列测定和分析,并通过与两种淡水微囊藻的比较,找出了其特征性核苷酸作为专一性分子探针设计的靶序列,为该藻种以及微囊藻属的快速鉴定及系统学研究提供了分子基础。  相似文献   

伊舒地堑构造演化的沉积充填响应   总被引：18，自引：1，他引：17       下载免费PDF全文

任建业  陆永潮 《地质科学》1999,34(2):196-203

伊舒地堑是一典型的转换伸展型盆地,它以构造上和沉积上的不对称结构,沉降中心的明显迁移和快速沉降充填为主要特征。本文应用盆地充填记录、盆地构造格架和盆地沉降史分析论证了伊舒地堑构造演化过程中不同级别的幕式裂陷作用,确定了幕式裂陷作用的沉积响应。此外,文章还总结了3种类型的沉积体系域构成样式和沉积特征。  相似文献   

山旺组与馆陶组馆上段层序地层格架对比   总被引：1，自引：0，他引：1  

邢焕清  姜在兴  王亚青 《煤田地质与勘探》2005,33(4):6-9

运用经典层序地层学理论,对中新世沉积的山旺盆地山旺组和渤海湾盆地济阳坳陷馆陶组馆上段的层序地层格架进行了对比分析。从野外露头、岩心、古生物、地球物理以及其他资料分析的结果显示,这两个盆地中新世层序地层格架具有较好的相似性。两盆地中控制层序地层格架发育的构造运动特征、沉积物供给、海平面升降和古气候等要素,都具有明显的可对比性。山旺盆地所处的地区是渤海湾盆地的主要物源区之一。这种在沉积体系上的天然联系,可能是山旺组和馆上段发育类似的层序地层格架的一个重要原因。   相似文献   

A 32-million year cycle detected in sea-level fluctuations over the last 545 Myr     

《地学前缘(英文版)》2020,11(6):2061-2065

Spectral analyses of past relative sea-level oscillations as represented by the ages of 57 Phanerozoic (the last 545 Myr) stratigraphic sequence boundaries from the Canadian Arctic show a strong spectral peak at 32 Myr (>99.9% confidence). These findings concur with previous reports of significant cycles with periods of around 30 Myr in various records of fluctuations of sea level, and in potentially related episodes of tectonism, volcanism, climate, and biotic extinctions. Sequence boundaries commonly coincide with stage boundaries based on biostratigraphy, and are correlated with episodes of extinction and times of flood-basalt volcanism. The connection between tectonics and sea-level variations may come from changes in rates of ocean-floor spreading and subduction, intraplate stresses from plate-reorganizations, and pulsations of hotspot volcanism. These coordinated periodic fluctuations in tectonics, sea level and climate may be modulated by cyclical activity in the Earth’s mantle, although some pacing by astronomical cycles is suspected.  相似文献   

泥蚶(Tegillarca granosa) cDNA 文库的构建及铁结合蛋白基因(Ferritin)序列分析     

贺静静  李晔  李太武  苏秀榕  王孟前  李松伟  周军  马斌  李强芳 《海洋与湖沼》2009,40(3):289-295

取正常泥蚶肌肉组织获得总RNA,纯化mRNA后,利用含SfiⅠ酶切位点的CDSⅢ引物逆转录合成cDNA第一链,通过LD—PCR合成cDNA双链,经胶回收除去短片段,与pDNR—LIB载体进行连接,电转化到大肠杆菌DH10B中,构建形成原始文库,进行滴度测试和重组率鉴定。结果表明原始文库的滴度为3．17×10^5cfu／ml,重组率为86．3％,插入片段多在500--2500bp间。随机挑选458个克隆测序,经分析获得94种已知基因及87种未知基因。其中包括铁结合蛋白（Ferritin）的全长cDNA序列。该基因序列全长895bp,5’-端非编码区为163bp,3’-非编码区为213bp,开放阅读框为519bp,编码172个氨基酸。推测其蛋白分子量和等电点分别为20kDa和4．89。氨基酸序列与皱纹盘鲍、太平洋牡蛎、血红扇头蜱、文昌鱼、中华蟾蜍、非洲爪蟾、小家鼠以及人等的同源性有62％-82％。比对结果表明,铁结合蛋白基因在动物进化中高度保守。  相似文献   

Sequence stratigraphy of an argillaceous,deepwater basin-plain succession: Vischkuil Formation (Permian), Karoo Basin,South Africa     

Willem C. van der Merwe  Stephen S. FlintDavid M. Hodgson 《Marine and Petroleum Geology》2010

The 380 m thick fine-grained Vischkuil Formation comprises laterally extensive hemipelagic mudstones, separated by packages of graded sandstone and siltstone turbidites, and volcanic ash beds, and is an argillaceous precursor to a 1 km thick sand-prone basin floor fan to shelf succession. The Vischkuil Formation provides an insight into the process by which regional sand supply is initiated and for testing sequence stratigraphic principles in a basin plain setting. Regionally mapped 1–2 m thick hemipelagic mudstone units are interpreted as condensed drapes that represent the starved basin plain equivalents of transgressive systems tracts and maximum flooding surface on the coeval shelf (now removed during later uplift). The section above each mudstone drape comprises siltstone turbidites interpreted as highstand systems tract deposits and a surface of regional extent, marked by an abrupt grain size shift to fine sandstone. These surfaces are interpreted as sequence boundaries, related to abrupt increases in flow volume and delivery of sand grade material to the basin-plain. The interpreted lowstand systems tract comprises sandstone-dominated turbidites and is overlain by another hemipelagic mudstone drape. The upper Vischkuil Formation is marked by three 20–45 m thick debrites, with intraformational sandstone clasts up to 20 cm in diameter that can be mapped over 3000 km². In each case, debrite emplacement resulted in widespread deformation of the immediately underlying 3–10 m of silty turbidites. A sequence boundary is interpreted at the base of each deformation/debrite package. Six depositional sequences are recognised and the interfered energy shift across each successive sequence boundary and LSTs include a larger volume of sandstone increases up section. The lower two sequences thin to the NW and show NW-directed palaeocurrents. The four overlying sequences show a polarity switch in palaeocurrent directions and thinning, to the E and SE. Sequence 6 is overlain sharply by the 300 m thick sandstone dominated Fan A of the Laingsburg Formation. The LST debrites may indicate gradual development of major routing conduits that subsequently fed Fan A. The polarity shift from westward flowing turbidity currents to an eastward prograding deepwater to shelf system represents establishment of a long term feeder system from the west. Sand supply to the Karoo basin floor was established in an incremental, stepwise manner. Given the early post-glacial setting in an icehouse climate, glacio-eustatic sea-level changes are considered to have been the main control on sequence development.  相似文献   

Timing and mechanism of reservoir forming in the Upper Triassic Halahatang Formation,Yuqi block,Tarim Basin,northwestern China     

Lixiong Kuang  Hao Zheng  Mingyan Wang  Taizhu Huang  Chensheng Liu 《Marine and Petroleum Geology》2010

The Yuqi block is an important area for oil and gas exploration in the northern Akekule uplift, Tarim Basin, northwestern China. The Upper Triassic Halahatang Formation (T₃h) within the Yuqi block can be subdivided into a lowstand system tract (LST), a transgressive system tract (TST), and a highstand system tract (HST), based on a study of initial and maximum flood surfaces. Oil in the lowstand system tract of the Halahatang Formation is characterized by medium to lightweight (0.8075 g/cm³–0.9258 g/cm³), low sulfur content (0.41%–1.4%), and high paraffin content (9.65%–10.25%). The distribution of oil and gas is principally controlled by low-amplitude anticlines and faults. Based on studies of fluorescence thin sections and homogenization temperatures of fluid inclusions, reservoirs in the T₃h were formed in at least two stages of hydrocarbon charge and accumulation. During the first stage (Jurassic–Cretaceous) both the structural traps and hydrocarbon reservoirs were initiated; during the second stage (Cenozoic) the structural traps were finally formed and the reservoirs were structurally modified. The reservoir-forming mechanism involved external hydrocarbon sources (i.e. younger reservoirs with oil and gas sourced from old rocks), two directions (vertical and lateral) of expulsion, and multi-stage accumulation. This model provides a theoretical fundament for future oil and gas exploration in the Tarim Basin and other similar basins in northwestern China.  相似文献   

Allocycles in the upper part of the limestone coal group (pendleian,E1) of the glasgow-stirling region viewed in the light of sequence stratigraphy     

W. A. Read  I. H. Forsyth 《Geological Journal》1991,26(1):85-89

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The Millstone Grit (namurian) of the southern pennines viewed in the light of eustatically controlled sequence stratigraphy     

W. A. Read 《Geological Journal》1991,26(2):157-165

The overall lithological succession in the Millstone Grit of the southern Pennines was most probably controlled by glacial-eustatic sea-level oscillations and may be interpreted in terms of the systems tracts of sequence stratigraphy. Bands containing thick-shelled goniatites represent ‘condensed sections’ formed at times of maximum flooding. Turbidite-fronted deltas, marking major basin-filling episodes, resemble ‘lowstand systems tracts’. However all sand influxes did not necessarily occur during lowstands. Millstone Grit sheet deltas and elongate deltas resemble lobate and birdfoot deltas in Recent ‘highstand systems tracts’. The prograding fluviodeltaic complexes at the tops of some major turbidite-fronted deltas were braid deltas. So was the sheet-like channel complex of the Rough Rock at the top of the Millstone Grit, but this was probably part of a ‘highstand systems tract’.  相似文献