单条胶黏藻Dumontia simplex Cotton的生长状态研究与分子分析     

王永宇  王昊林  李佳俊  王宏伟 《海洋与湖沼》2018,49(4):829-838

对分布在黄、渤海沿岸的单条胶黏藻Dumontia simplex Cotton的形态结构、生物量、成熟个体比例与成熟个体生物量/总生物量(R/T指数)的变化、温度性质以及rbcL、COI基因序列进行了详细研究。结果表明:(1)10个采集地点的单条胶黏藻藻体直立、扁平或螺旋状,质地胶质黏滑,颜色为红色或紫红色。在大连黑石礁与付家庄采集到的藻体长度和宽度明显高于其他采集地点;(2)藻体由皮层与髓部组成,皮层由4—8层细胞组成,髓部有疏松的根丝细胞。囊果散生,包埋于皮层内,刚发育的囊果较小,色淡,随着藻体生长囊果变大,颜色加深。四分孢子囊侧生在内皮层上,成熟的四分孢子囊呈十字形分裂;(3)4月生物量最大,平均生物量为4.384g/m2。12月至次年6月成熟个体比例逐渐增大,6月达到100%,且均为四分孢子体;(4)单条胶黏藻生长周期为12月至次年6月,属于一年生海藻,温度性质属于亚寒带性;(5)rbcL与COI基因序列分析表明,十个采集地点的样本间无碱基差异,与产自美国单条胶黏藻聚在一起,形成一个独立的分支,均确定为单条胶黏藻。  相似文献   

Petrogenesis of post – orogenic Lower Permian andesites in southern Europe: insights into the collapse of the Variscan range     

《Geodinamica Acta》2013,26(5-6):273-290

In the post-Variscan Early Permian deposits of southwestern Europe, andesites belong to successions characterized by the constant occurrence of a basal rhyolite ignimbrite, followed by andesites, and by abundant dacite-rhyodacite products, interbedded with lacustrine sediments. The subalkaline andesite to K-andesite volcanism developed within intramontane basins following the collapse of the Variscan orogen. The compositional features, including trace element ratios and initial Sr (and Nd) of post-Variscan intermediate products allow excluding continental or island arc settings. The andesite composition of Lower Permian lavas was reproduced starting from two potential primary magmas: picrobasaltic and enriched MORB compositions. In particular, the picrobasalt was modified, by adding incremental amounts of a felsic granulite, from the lower continental crust. Mixing and fractional crystallization (MFC) were modelled by the MELTS software in a closed system under isobaric, isenthalpic conditions (P = 0.3 GPa). The computed residual liquid evolves to match closely the composition of Lower Permian andesite lavas after ~34 % crystallization by adding ~27 % of contaminant to the parental magma.  相似文献   

Source rocks and provenances of the Ladoga Group siliciclastic metasediments (Svecofennian Foldbelt, Baltic Shield): Results of geochemical and Sm-Nd isotopic study     

L. N. Kotova  A. B. Kotov  V. A. Glebovitskii  V. N. Podkovyrov  V. M. Savatenkov 《Stratigraphy and Geological Correlation》2009,17(1):1-19

Siliciclastic metasediments of the Ladoga Group that is the Kalevian stratotype in Karelia correlative with the Kalevian siliciclastic succession in Finland are studied in terms of geochemistry and Sm-Nd isotopic systematics. The results obtained show that rocks in the Ladoga Group lower part are enriched, as compared to rocks of the upper part, in TiO₂, Fe₂O₃, MgO, Cr, Co, Ni, and Sc, being comparatively depleted in Al₂O₃ and Th that is a result of compositional changes in provenances. The Sm-Nd isotopic data evidence that siliciclastic sediments of the Ladoga Group have accumulated during the erosion of rocks, which originated at the time of the Archean and Early Proterozoic crust-forming processes. Siliciclastic material with the Archean and Early Proterozoic T_Nd(DM) values, which are characteristic of metasediments in the group lower part, was derived respectively from granite gneisses of the Archean basement in the Karelian megablock of the Baltic Shield and from volcanic rocks of the Sortavala Group. Volcanic rocks of island-arc terranes of the Svecofennian foldbelt represented main source of siliciclastic material that accumulated in upper part of the succession.  相似文献   

二端员自然混合过程的Sr,Nd同位素体系与端员贡献的定量分离     

孟宪伟  杜德文  龙江平 《海洋科学进展》1999,(3)

二端员物质的混合过程在自然界普遍发生。放射性成因的 Ｓｒ, Ｎｄ 同位素体系因其具有源区示踪和长周期时标特性,在混合物组成端员定量分离和混合机制研究中具有特殊意义。本文较详细地介绍了二端员混合过程形成的混合体中元素组成、 Ｓｒ, Ｎｄ 同位素组成之间的相互关系。在此基础上,介绍了二端员混合过程的 Ｓｒ, Ｎｄ 同位素鉴别准则和混合体中混合比 ｆ 的确定方法。  相似文献   

Nd isotopic compositions of the Tethyan Himalayan Sequence in southeastern Tibet   总被引：3，自引：0，他引：3  

JinGen Dai  An Yin  WenCan Liu  ChengShan Wang 《中国科学D辑(英文版)》2008,51(9):1306-1316

The Himalayan orogen consists of three major lithologic units that are separated by two major north-dipping faults: the Lesser Himalayan Sequence (LHS) below the Main Central Thrust (MCT), the Greater Himalayan Crystalline Complex (GHC) above the MCT, and the Tethyan Himalayan Sequence (THS) juxtaposed by the South Tibet Detachment fault (STD) over the GHC. Due to widespread meta-morphism and intense deformation, differentiating the above three lithologic units is often difficult. This problem has been overcome by the use of Sm-Nd isotopic analysis. The previous studies suggested that the LHS can be clearly distinguished from the GHC and THS by their Nd isotope compositions. However, the lack of detailed and systematic Sm-Nd isotopic studies of the THS across the Himalaya in general has made differentiation of this unit from the nearby GHC impossible, as the two appear to share overlapping Nd compositions and model ages. To address this problem, we systematically sam-pled and analyzed Nd isotopes of the THS in southeastern Tibet directly north of Bhutan. Our study identifies two distinctive fields in a εNd -TDM plot. The first is defined by the εNd(210 Ma) values of -3.45 to -7.34 and TDM values of 1.15 to 1.29 Ga from a Late Triassic turbidite sequence, which are broadly similar to those obtained from the Lhasa block. The second field is derived from the Early Cretaceous meta-sedimentary rocks with εNd(130 Ma) values from -15.24 to -16.61 and TDM values from 1.63 to 2.00 Ga; these values are similar to those obtained from the Greater Himalayan Crystalline Complex in Bhutan directly south of our sampling traverse, which has εNd(130 Ma) values of -10.89 to -16.32 and Nd model ages (TDM) of 1.73 to 2.20 Ga. From the above observations, we suggest that the Late Triassic strata of the southeast Tibetan THS were derived from the Lhasa block in the north, while the Early Cretaceous strata of the THS were derived from a source similar to the High Himalayan Crystalline Complex or Indian craton in the south. Our interpretation is consistent with the existing palaeocurrent data and provenance analysis of the Late Triassic strata in southeastern Tibet, which indicate the sediments derived from a northern source. Thus, we suggest that the Lhasa terrane and the Indian craton were close to one another in the Late Triassic and were separated by a rift valley across which a large submarine fan was transported southward and deposited on the future northern margin of the Indian continent.  相似文献   

星洲银罗非鱼线粒体细胞色素b基因的序列分析   总被引：1，自引：1，他引：0  

刘楚吾  李路  林晓坤  刘丽 《广东海洋大学学报》2008,28(4)

克隆并测定了星洲银罗非鱼(Oreochromis sp.)细胞色素b基因(cyt b)的全序列,得到全长1 141bp的序列用于分析,用MEGA4.0分析软件与GenBank中的线粒体DNA序列进行序列比较,显示星洲银罗非鱼与其他鱼类的cyt b基因的同源性较高,同源度介于83%~93%间;根据星洲银罗非鱼与莫桑比克罗非鱼、尼罗罗非鱼等12种鱼类的cyt b基因序列构建的系统进化树,初步确定尼罗罗非鱼、莫桑比克罗非鱼为星洲银罗非鱼的父母本。  相似文献   

二纺蛛总科（蜘蛛目：新蛛下目）蜘蛛化石研究进展     

郭向博  任东 《地质论评》2022,68(3):2022062030-2022062030

二纺蛛总科包括5个现生科、5个化石科以及一些科级位置未定的化石物种,是蜘蛛目中较为古老的一个类群。目前已知最早的二纺蛛总科化石记录可以追溯到早侏罗世,但分子系统发育研究推测其起源时间为二叠纪。二纺蛛总科蜘蛛在中生代最为繁盛,化石物种相对较多,是蜘蛛化石类群的重要组成部分。而现生二纺蛛总科蜘蛛十分稀少,且主要分布在热带和亚热带地区。近年来的系统发育研究认为二纺蛛总科可能是复杂生殖器类的姐妹群,是蜘蛛演化研究的关键类群。因此,本文对二纺蛛总科分类系统的研究历史进行了回顾,总结了二纺蛛总科化石类群在不同地质历史时期的组成和分布,统计了二纺蛛总科蜘蛛化石的名录。目前,二纺蛛总科蜘蛛化石分类研究基础薄弱,部分化石类群的系统位置存疑,二纺蛛总科内部系统发育关系尚不清晰。在将来的研究中,需要利用多种技术手段获取化石材料的形态学信息,打好分类学基础;结合化石类群和现生类群进行系统发育分析;进而联系古地理、古生态、生物学行为等研究,全方位分析二纺蛛总科的自然演化历史。  相似文献   

The relationship of mantle-derived fluids to gold metallogenesis in the Jiaodong Peninsula: Evidence from D–O–C–S isotope systematics     

Jingwen Mao  Yitian Wang  Houmin Li  Franco Pirajno  Changqing Zhang  Ruiting Wang 《Ore Geology Reviews》2008,33(3-4):361-381

The largest gold district in China is the Jiaodong Peninsula, where three types of gold deposits are recognized: quartz vein, fracture-altered and breccia types. The first two developed along a group of NE-trending faults and are hosted by granitic intrusions, dated at 160 to 150 Ma (biotite granite) and 130 to 126 Ma (granodiorite), and by metamorphic rocks of the Precambrian crystalline basement. The breccia-type gold system is mainly located around the northern margin of the Jiaolai Cretaceous basin, where mineralisation is controlled by both detachment fractures and NE-trending faults. This study is based on stable isotope determinations from ten gold deposits, including Linglong, Jiaojia, Sanshandao, Cangshang, Wang'ershan, Dayigezhuang, Denggezhuang, Pengjiakuang, Fayunkuang and Dazhuangzi, as well as the Linglong Jurassic biotite granite, Guojialing Cretaceous granodiorite and Archean gneiss. The stable isotope systematics reflect the style of the three types of gold deposits, but also show that they belong to the same metallogenic system, in which the hydrothermal fluids were derived from a mantle fluid reservoir and mixed with crustal fluids. The ore-forming age is later than both the Jurassic biotite granite and Cretaceous granodiotite, but overlaps with the 121 to 114 Ma ages of lamprophyre and diabase dykes. The hydrothermal fluids that were responsible for both gold mineralisation and the retrograde alteration of the diabase and lamprophyre dykes are similar, and represent a CO₂ and potassium-rich system. This fluid system is interpreted to be the consequence of Cretaceous lithospheric thinning, asthenospheric upwelling and mantle degassing in Eastern China.  相似文献   

Selenium and Sulfur Systematics of Mafic Dykes in Western Fujian Province, Southern China   总被引：2，自引：1，他引：1  

FAN Haifeng  WEN Hanjie  ZHANG Guishan  HU Ruizhong 《《地质学报》英文版》2008,82(4):884-895

Fifteen samples from three study areas （the Bancun diabase dykes, the Bali hornblende gabbro dykes, the Linzifen gabbro-diabase dykes） were collected and analyzed for selenium （Se）, sulfur （S）, copper （Cu）, major and trace elements. In general, Se, S and Cu do positively correlate to each other. The concentration of S and Se and the S/Se ratio are higher than the corresponding value of primitive mantle （PM）, and the Cu/S ratio falls in a narrow range （0.04-0.29）, which is consistent with that of primitive mantle （0.05-0.20）. The Bancun diabase dykes and the Bali hornblende gabbro dykes were located in an intraplate environment during the Late Mesozoic. Oceanic subduction was closely related to magmatic activities. The magmatic activities play an important role in the transportation mechanism of Se and S. Because those two groups were closer to fault zones, which may affect the distribution of S and Se and other elements. In the two groups, no crustal contamination was observed, indicating that all analyzed elements may come from enriched mantle metasomtism associated with slab subduction. However, the Linzifen gabbro-diabase dykes were located in an intraplate rift environment, and its invading age is older than the other two groups, the primitive magma comes from mantle, and there is an anomalous relation between S, Se and Al2O3, （La/Sm）N, and all these factors could result in higher S and Se concentration.  相似文献   

三种胡子鲶形态特征的统计分析及其分类意义     

庆宁  林岳光  刘学东  赵迪 《热带海洋学报》1992,(3)

本文对胡子鲶Clarias fuscus、两栖胡子鲶Clarias batrachus及革胡子鲶Clarias lazera共125尾样品的10项形态测量性状及5项可数性状进行比较研究,并应用主分量分析和判别分析探讨种(或群体)间的分类关系。多变量统计分析结果:三种胡子鲶种间具有明显的间断,正判率均为100％;而胡子鲶的两个群体间的正判率为93.5％,并且没有明显的间断。研究结果与生化分析结果基本一致,表明中国存在两栖胡子鲶,三种胡子鲶是三个独立的种,区分三者的最有效特征为鳃耙数。我们认为,主分量分析和判别分析对鉴别外形非常相似的种类(如胡子鲶和两栖胡子鲶)有实用价值。  相似文献