内蒙古准格尔旗晚石炭世一早二叠世早期腕足类物种多样性与沉积环境     

Zeng Yong 《古地理学报》2007,(5)

以定性与定量相结合的研究方法,对内蒙古准格尔旗晚石炭世—早二叠世早期的腕足类物种多样性、沉积环境进行了综合研究,指出本区海进序列的腕足类物种多样性远高于海退序列;规模较大、具有一定水深的海进序列是腕足类辐射、分异、物种多样性升高的重要环境体系;本区腕足类辐射起步于晚石炭世早期之初,物种多样性出现了3次峰值(晚石炭世早期之中期、晚石炭世早期之晚期、晚石炭世晚期之中期),其中晚石炭世早期之晚期是本区腕足类物种多样性的顶峰期。  相似文献   

HYPOGLOSSUM FUJIANENSIS SP. NOV. (DELESSERIACEAE,RHODOPHYTA) FROM FUJIAN COAST, CHINA     

郑怡 《中国海洋湖沼学报》1998,(4)

lNwnDUCnoNTheDelesseriaceangenusHopdeumKtitzingincludesabout25speciesoccurringintropicalandtemPerateseasthroughouttheworld-ThereareanuInberofmorphologicalandtaxonodricstudiesonHopghsuminconteInPOngliteratUre(WOInrsleyandShep-ley,l982;Mikdri,l985;WynnandKraf,l985;WynneandBallantin,1986;Yoshi-daandMibo,l986;Miknd,l987;Wynneetal-,'l989).Uptodate,onlyonespecies,H-attenuatam,hasbeendescrihedfrOInChineseseas(Tsengetal.,1983).DuringataXodricstUdyoftheChineseIhadesum,specimenscollectedb…  相似文献   

Hypoglossum fujianensis sp. nov. (Delesseriaceae, Rhodophyta) from Fujian Coast, China     

Zheng Yi 《中国海洋湖沼学报》1998,16(4):369-372

Hypoglossum fujianensis sp. nov. is an epiphytic alga in the intertidal zone. Plants are light red, 0.9–2 cm high. Margin of branches gives rise to uniseriate hair-like rhizoids, formed outward from the fusion of the second-and third-order cells. Blades are single layered (except the midrib) and uncorticated. Tetrasporangial sori are formed on the middle part of blades. The globular tetrasporangia are developed from lateral pericentral cells. Project 39391800 supported by the NSFC.  相似文献   

Preliminary study on pisionids (Annelida: Polychaeta Pisionidae) from Hainan Island coastal waters, South China Sea     

Wu Bao-ling  Ding Zhi-hu  Huang Feng-peng 《中国海洋湖沼学报》1998,16(2):149-160

Of the four species ofPisione Grube (1856) collected from the coastal waters of Hainan Island, the South China Sea, and described in this paper,Pisione hainanensis n. sp. is new to science;Pisione oerstedii Grube, 1857;Pisione complexa Alikunhi, 1947, and Pisione levisetosa Zhao, Westheide & Wu, 1991 are reported for the first time from this area. Project 38970187 supported by NSFC.  相似文献   

云南金线鲃属鱼类二新种(鲤形目:鲤科)     

李维贤  武德方  陈爱玲 《广东海洋大学学报》1998,(4)

描记采于云南省玉溪地区的金线属二新种,以形态特征和采集地县名分别命名为长鳍金线SinocyclocheiluslongifinusLi,sp．nov和华宁金线SincyclocheilushuaningensisLi,sp．nov。前者头的后部不隆起,体表裸露,胸鳍长,后伸达腹鳍起点等特征区别云南省的其他金线;后者外形与大头金线相近,但侧线鳞较少（59～60）,前躯裸露或被稀疏细鳞,口须较长等可区别,两者遗传距离为1．7％,也已达到种级差异。模式标本保存于云南省路南县黑龙潭水库和云南大学生物系。  相似文献   

Geology, Mineralogy, and Formation Environment of the Disseminated Gold-Silver Telluride Bulawan Deposit, Negros Occidental, Philippines     

Victor B. MAGLAMBAYAN  †  Daizo ISHIYAMA  Toshio MIZUTA  Akira IMAI  Yohei ISHIKAWA 《Resource Geology》1998,48(2):87-104

Abstract: The Bulawan deposit is located in the porphyry copper belt of southwest Negros island, Philippines. Propylitic, K–feldspar, sericitic, and carbonate alteration types can be distinguished in the deposit. Propylite alteration occurs mainly in Cretaceous-Eocene andesitic lavas and agglomerates while K–feldspar, sericite and carbonate alteration types occur mostly in the Middle Miocene dacite porphyry breccia pipes and stocks which were intruded into the andesites. K-feldspar zones occur in the inner parts of the sericitized zone. Sericite alteration overprinted the propylitized and K-feldspar alteration zones, at lower temperature than epidote and chlorite in the propylitized zone. Carbonate alteration is associated with the mineralization in the center of the breccia pipes and along faults. Mineralization consists of gold-silver telluride ores that are hosted by the carbonate– and sericite-altered dacite porphyry breccia pipes. The Bulawan ores occur mainly as disseminations, but unlike many epithermal gold deposits, lack classical epithermal colloform and crustiform quartz veins. The ore minerals are sphalerite, galena, chalcopyrite, pyrite and tetrahedite-tennantite with minor amounts of electrum, calaverite, petzite, sylvanite, hessite, tellurobismuthite, coloradoite, altaite, and rucklidgeite. Electrum and telluride minerals are associated mostly with calcite and dolomite-ankerite minerals. Fluid inclusions in quartz and calcite in clasts of propylitized andesite in the breccia pipes homogenize from about 300° to 400°C while fluid inclusions in quartz, calcite and sphalerite within the dacite porphyry breccia pipes homogenize between 300° to 310°C. The ores were formed around 300°C from hydrothermal solutions with salinity of about 6. 6 wt % NaCl equivalent. The presence of sylvanite and calaverite as intergrowths with each other, and the Ag content of calaverite are consistent with the above temperature estimate. Based on paragenesis, the Bulawan deposit formed in a pyrite-stable environment, with pH between 3. 4 and 5. 5, f_O2 between 10^-32 to 10^-30 atm, f_S2 between 10^-9.8 to 10^-7.8 atm, f_Te2 between 10^-8.9 to 10^-6.5 atm, and total sulfur content about 10^-2.8 molal. The dominant reduced sulfur species in the ore solutions may have been H₂S_(aq), and the likely aqueous tellurium species were H₂Te_(aq) and H₂TeO_3(aq). The ore minerals in the Bulawan deposit were probably formed by mixing of slightly saline and low salinity fluids.  相似文献   

Precipitation water storage capacity in a temperate mixed oak–beech canopy     

Frédéric André  Mathieu Jonard  Quentin Ponette 《水文研究》2008,22(20):4130-4141

The storage capacity of a temperate mixed oak–beech stand was investigated as a function of stand density and species composition. Measurements were performed in selected zones delimited by three neighbouring trees. Three independent approaches were compared: (i) a spraying laboratory experiment to estimate the water storage on foliage before and after dripping; (ii) a mechanistic model describing rainfall partitioning within the forest canopy and providing estimates of foliage storage capacities; and (iii) linear regression analyses to evaluate the canopy (foliage + branches) storage capacity using the relationship between throughfall and rainfall. Good agreement was generally observed between the laboratory experiment and the mechanistic model estimates, while estimations from the regression method tended to exceed those from the other approaches. Storage capacity estimates ranged from 0·22 mm to 0·80 mm for pure oak zones, from 0·24 mm to 1·12 mm for mixed zones and from 0·53 mm to 1·17 mm for pure beech zones. The increase of storage capacity with increasing proportion of beech in the canopy resulted from higher beech LAI compared with oak. Similarly, for mixed and pure beech canopies, storage capacity was higher for high density zones than for low density zones as a result of the increase in LAI with increasing local basal area; in contrast, for pure oak, the storage capacity was not related to basal area because of the lower shade‐tolerance of this species compared with beech. Copyright © 2008 John Wiley & Sons, Ltd.  相似文献   

Probabilistic aspects of micropaleontologic assemblage zones     

Isamu Hattori 《Mathematical Geology》1985,17(2):167-175

A micropaleontologic assemblage zone is defined by occurrence of some characteristic species among many coeval species. When number of assemblage-defining species and total number of species observed are designated as Aand N,respectively, the ratio, A/N,is strongly dependent on duration of the assemblage. Theoretical consideration on the basis of a micropaleontologic cohort model shows that, when origination rate and extinction rate of species are obtained, the most reasonable ratio (A/N) and duration of the assemblage can be determined. The probabilistic model described in this paper provides a theoretical relation between the ratio and the duration. Inaccuracy in correlating micropaleontologic data to certain assemblage zones established can not be avoided because of many natural sorting and artificial biases. Ambiguity arising when data with a small number of characteristic species are correlated with a certain assemblage is numerically estimated.  相似文献   

Two New Species of the GenusTinocladia Kylin(Chordariales, Phaeophyta) from Yellow Sea Coasts of China     

丁兰平  陆保仁  黄冰心  曾呈奎 《中国海洋湖沼学报》2004,22(1)

  相似文献   

基于角质颚长度的头足类种类判别   总被引：6，自引：1，他引：5  

刘必林  陈新军  方舟  金岳 《海洋与湖沼》2015,46(6):1365-1372

本文根据2013 年8 月于舟山市沈家门东河菜场采集的5 种近海常见经济头足类(剑尖枪乌 贼、杜氏枪乌贼、金乌贼、曼氏无针乌贼和短蛸), 利用逐步判别和主成分分析法对其上、下角质颚 的各5 种长度指标(喙长、头盖长、脊突长、侧壁长、翼长)进行分析。结果显示, 这5 种头足类角质 颚长度差异显著(ANOVA: P<0.001), 其中以金乌贼的角质颚尺寸最大, 短蛸的角质颚尺寸最小。判 别分析显示, 角质颚长度适合用来划分头足类的种类, 综合判别成功率为96.2%, 其中以上颚侧壁 长、上颚头盖长和下颚脊突长对判定的贡献率最高。然而, 与之相比, 标准化后的角质颚长度则更适 合用来划分头足类的种类, 综合判别成功率达到100%, 其中以标准化下颚喙长和标准化下颚翼长对 判定的贡献率最高。主成分分析显示, 角质颚长度及标准化后角质颚长度对枪乌贼类和乌贼类的判 定成功率均达到100%.本文建立了一种基于角质颚长度判别分析法的头足类种类判定的新方法, 丰 富了头足类种类鉴定的技术手段, 为我国学者在相关领域的研究提供了基础。  相似文献