Issue 1,2008 Table of Contents

  • Display Type:
  • Text List
  • Abstract List
  • 1  CHARACTERISTICS OF PRE-LATE CARBONIFEROUS FLORA OF CHINA:A NOTE ON PRO-CATHAYSIAN FLORA
    WU Xiu-yuan ) WANG Jun ) ZHANG Yi )) Nanjing Institute of Geology Palaeontology the Chinese Academy of Sciences Nanjing ) State Key Laboretory of Palaeobiology Stratigraphy Nanjing
    2008(1):1-20. DOI: 1 CSTR:
    [Abstract](326) [HTML](0) [PDF 0.00 Byte](16)
    Abstract:
    "前华夏植物群"一词由李星学等提出,原义指以西北地区下石炭统(臭牛沟组、靖远组为主)及华南相当地层中的植物总称。作者分析了当前古植物地理区划的有关理论,结合中国的具体情况,提出"前华夏植物群"的涵义不但可以代替欧美植物群中拟鳞木植物群(Lepidodendropsis flora),而且还可能包括自早志留世植物登陆以来至早石炭世,在中国大陆(或称华夏复合大陆)生长的、独立的植物群。文中以晚泥盆世—早石炭世的植物群中独特的科、属、种等地方性土著分子为例,以当前古植物地理区的有关理论为依据,认为"前华夏植物群区"可以从以往的"欧美植物群"或"拟鳞木植物群"区中单独划分出来成为独立的植物地理区。
    2  RECONSTRUCTION OF PINNA OF PECDPTERIS LATIVENOSA HALLE BASED ON STATISTIC ANALYSIS
    ZHANG Yi ) WANG Jun ) LIU Lu-jun )) Nanjing Institute of Geology Palaeontology the Chinese Academy of Sciences Nanjing ) State Key Laboratory of Palaeobiology Stratigraphy Nanjing
    2008(1):21-38. DOI: 1 CSTR:
    [Abstract](252) [HTML](0) [PDF 0.00 Byte](12)
    Abstract:
    Pecopteris lativenosa Halle is one of the pecopterid species with marked intraspecific variation of leaf morphology. Based on observation of numerous specimens collected from the Early Permian Taiyuan Formation in Wuda, Inner Mongolia, and with an application of statistic analysis, the major features of Pecopteris lativenosa Halle are tested and verified. Five types of pinnules, six types of ultimate pinnae and two types of penultimate pinnae are differentiated, and their spatial locations on a tripinnate leaf are evaluated. As a result, a reconstruction of a tripinnate leaf is realized. It is applicable to interpret previously described specimens of this species. Qualitative and quantitative methodology in morphological reconstruction of fossil plant is briefly reviewed.
    3  THE ASSEMBLAGE SEOUENCES AND BIOGEOGRAPHIC PROVINCES OF THE EIFELIAN RUGOSE CORALS IN NEAR-SHORE FACIES FROM SOUTH CHINA
    LIAO Wei-hua ) MA Xue-ping )) Nanjing Institute of Geology Palaeontology the Chinese Academy of Sciences Nanjing ) Department of Geology Peking University Beijing
    2008(1):39-46. DOI: 1 CSTR:
    [Abstract](270) [HTML](0) [PDF 0.00 Byte](12)
    Abstract:
    The Eifelian Stage has been divided from bottom to top into four conodont zones: partitus, costatus, australis and kocklianus by SDS. However, we have rarely found the above-mentioned standard zonation conodonts in the near-shore deposits from South China though we have found some important Devonian organism groups such as conodonts, ammonoids, tentaculites and others in the pelagic deposits of South China. Up to now, we have only found some long-term conodonts such as Eognathodus bipennatus bipennatus, Eognathodus bipennatus montensis and Icriodus corniger corniger in the Eifelian shallow water environments from South China.Devonian near-shore deposits are widespread in South China and rich in benthic brachiopods and corals. Based on a revised taxonomy and biostratigraphic range of rugose coral assemblages in South China, a coral biostratigraphy has been established, which indicates a subdivision of Eifelian into two discrete coral assemblages.Their correlation with the standard conodont zonation allows age determination of coral-bearing sequences. Lower-Middle Eifelian and Upper Eifelian rugose coral assemblage sequences in South China are shown as follows (in descending order): Upper Eifelian(2) Columnaria spinosa-Dendrostella praerhenana Assemblage (australis and kocklianus zones)Lower-Middle Eifelian(1) Utaratuia sinensis-Sociophyllum minor Assemblage (partitus and costatus zones).The Upper Eifelian coral assemblage is quite different from the Lower-Middle ones. Favositids, heliolitids and some rugose coral genera were extinct at the Mid-Eifelian bioevent. Some older elements of corals which lasted from Silurian and Lower Devonian survived in the Lower-Middle Eifelian. While the Upper Eifelian contained some advanced taxa of Rugosa.Biogeographic provincialism increased in late Lochkovian and Pragian time and reached a maximum during the early Emsian fauna. Lower Emsian rugose corals of South China are relatively endemic. However, after this time they became gradually cosmopolitan. The Eifelian rugose corals of South China are close to those of West Canada, Russia, West Europe and Australia. They all belong to the same Old World Realm.
    4  THE BUILDINC PROCESS AND INFLUENTIAL FACTORS OF THE STROMATOLITE REEFS IN THE NEOPROTEROZOIC JIULIQIAO FORMATION IN HUAINAN REGION,ANHUI
    JIA Zhi-hai HONG Tian-qiu WANG WeiSchool of Resources Environmental Engineering Hefei University of Technology
    2008(1):47-57. DOI: 1 CSTR:
    [Abstract](285) [HTML](0) [PDF 0.00 Byte](6)
    Abstract:
    淮南地区新元古代九里桥组中段灰岩中发育有形态多变的叠层石礁体,具有与显生宙生物礁相似的相分异特征,基底、礁核、盖层、礁前、礁后、礁翼等不同微相可以明确区分,定殖期、拓殖期、泛殖期和衰亡期等不同造礁阶段的叠层石柱体变化特征明显。该组叠层石礁体自下而上分别为分散分布的小型丘状礁体、连绵分布的大型丘状礁体和分散分布的小型丘状礁体或透镜状礁体,该变化趋势指示了九里桥组沉积时期海平面先升高后降低的变化趋势,结合该组沉积期沉积环境变化特征可将该组叠层石礁体划分为风暴环境型礁体、海进环境型礁体和海退环境型礁体三种类型。对九里桥组沉积学、古生物学等研究表明,该组沉积时期造叠层石生物与其它生物之间存在较强的生存竞争关系,但更能适应风暴沉积环境,叠层石在该组沉积晚期的消失很可能与以海平面变化为特征的沉积构造环境变化有关。
    5  MIDDLE TRIASSIC SPORE-POLLEN ASSEMBLAGE FROM NORTHERN QILIAN,QINGHAI AND ITS SIGNIFICANCE IN SEDIMENTOLOGY
    JI Liu-xiang ) LUO Wei ) ZHU Huai-cheng ) OUYANG Shu ))Regional Geological Survey of Qinhai Province Xining )Shiyan Architectural Design Institute Hubei Shiyan )State Key Laboratory of Palaeobiology Stratigraphy Nanjing )Nanjing Institute of Geology Palaeontology the Chinese Academy of Sciences Nanjing
    2008(1):58-72. DOI: 1 CSTR:
    [Abstract](261) [HTML](0) [PDF 0.00 Byte](6)
    Abstract:
    青海省祁连县俄博乡大擦汗沟、土圈沟、柯柯里等三叠系剖面的粉砂岩、砂质页岩、泥质页岩中首次发现较丰富的孢粉和疑源类化石,计57属98种。孢粉中的蕨类植物孢子占总组合的44.6%,裸子植物花粉占33.9%;疑源类有8属13种,占21.5%,称Verrucosisporites-Triadispora-Trematosp haeridium孢粉组合。该组合面貌与国内外中三叠世不同相区的孢粉组合特征基本相似并可对比。北祁连山南坡本组合及上下其它组合中海相疑源类的存在,表明该区在三叠纪受到海水影响,海水完全退出是在三叠纪之后。文章还初步探讨其沉积相意义。
    6  PRELIMINARY RESEARCHES FOR MIXOSAURID FOSSILS FROM MIDDLE TRIASSIC GUANLING FORMATION IN PANXIAN OF GUIZHOU
    LIU Guan-bang ) YIN Gong-zheng )) Department of Earth Sciences Nanjing University Nanjing ) Regional Geological Survey of Guizhou Guiyang
    2008(1):73-90. DOI: 1 CSTR:
    [Abstract](392) [HTML](0) [PDF 0.00 Byte](5)
    Abstract:
    In the summers of 2001 and 2002 we went to the Xingyi district of southwestern Guizhou to explore the Triassic marine vertebrates and got in Xingyi an information occurred in neighboring Panxian the saurian and fish fossils. Because of the inconvenience of the traffic we did not go to Panxian to do field exploring, and therefore we did not se at that time the saurian and fish specimens of that county. Soon after we collected in Nanjing a few ichthyosaur fossils of small size, which were said to come from the Yangjuan village of Panxian, only then did we realize that the saurian fossils in Panxian were the Middle Triassic mixosaurid, hence different from the Late Triassic Keichousaurus from Xingyi. In the July of 2004 we went to the Yangjuan village of Panxian in an attempt to confirm the locality and horizon of the mixosaurid fossils that we collected in Nanjing; besides, in Panxian we saw some mixosaurid and fish fossils just discovered from the dark carbonaceous and mud limestone of the Middle Triassic Guanling Formation. During this trip we also found out that the mixosaurid fossils of Guanling Formation in Yangjuan village of Panxian, Guizhou Province, were found during the opening years of the present century by a group of peasants with rich experience in digging the keichousaur and fish fossils, which were from Dingxiao of Xingyi. Through fossil dealers the mixosaurid fossils from the Yangjuan village had been partially delivered to the hands of some palaeontologists. During our studying of the mixosaurid fossils from Yangjuan village of Panxian we saw one after another that Jiang et al. published from 2003 to 2006 4 articles on the the mixosaurid fossils found in late Early Anisian conodont-zone of Nicoraella germanicus in Yangjuan village of Panxian, Guizhou Province. According to our understanding, around Yangjuan village there are many localities that have yiedled the mixosaurid fossils, we have not explored and studied in detail these fossil one by one, therefore we do not know for certain that they all came from the same fossil bed, or different fossil beds, we conjecture that it is very possible that they all come occurred from a group of beds from the late Early Anisian to the Ladinian in age. Recently we collected again in Nanjing two mixosaurid fossils from another locality, Xindian of Puan County, about 15 km east of Yangjuan village. In the last few years we have seen in Nanjing of Jiangsu and in Guizhou more than thirty mixosaurid specimens dug out in Yangjuan area of Panxian, most of them are complete skeletons and some very beautifully preserved. According to our examination of these mixosaurid fossils we inspected in Nanjing, collected from Yangjuan area of Panxian, they represent three species of Mixosaurus, one of them is new. These mixosaur fossils from Panxian are of very important palaeontological interest because they may fill up some deficience in the finding and studying of Mixosaurus for more than a century ever since it was named by Baur in 1887 and may deepen our understanding of their morphology and taxonomy.
    7  CONODONT SUCCESSION AROUND THE PERMIAN-TRIASSIC BOUNDARY AT THE HUANGZHISHAN SECTIoN,ZHEJIANG AND ITS STRATIGRAPHIC CORRELATION
    Charles M. Henderson
    2008(1):91-114. DOI: 1 CSTR:
    [Abstract](295) [HTML](0) [PDF 0.00 Byte](5)
    Abstract:
    Conodonts from the Permian-Triassic boundary beds at the Huangzhishan Section, Zhejiang are systematically studied for the first time, with a total of 16 species assigned to 2 genera. On the basis of the ranges of identified species, five conodont zones are recognized in ascending order as follows: the Clarkina changxingensis changxingensis Zone, the C. parasubcarinata Zone, the C. changxingensis yini-C. meishanensis zhangi Zone, the C. meishanensis meishanensis Zone, and the Hindeodus parvus Zone. The successive occurrences of Hindeodus changxingensis in Bed 15, Hindeodus eurypyge in the lower part of Bed 18 and Hindeodus parvus in the middle part of Bed 18 serve as proxies for defining the Permian-Triassic boundary at the base of Bed 18-3 in the Huangzhishan Section. Correlations with the stratotype Meishan Section, Zhejiang and sections in Iran are also discussed in terms of conodonts.
    8  RESTUDY OF GUANGWEJCARIS LUO,FU ET HU,2007 FROM THE LOWER CAMBRIAN CANGLANGPU FORMATION IN KUNMING AREA
    YANG Jie ) HOU Xian-guang ) DONG Wei )) Yunnan Key Laboratory for Palaeobiology Yunnan University Kunming ) State Key Laboratory of Palaeobiology Stratigraphy Nanjing ) Yunnan Institute for Protection Research of Fossils Kunming
    2008(1):115-122. DOI: 1 CSTR:
    [Abstract](291) [HTML](0) [PDF 0.00 Byte](7)
    Abstract:
    昆明地区下寒武统沧浪铺组乌龙箐段所产的节肢动物Guangweicaris Luo,Fu et Hu,2007,为研究寒武纪生命大爆发之后节肢动物辐射特征提供了重要资料。罗惠麟等(2007)在报道该节肢动物时,因标本不完整,对其头部和尾部特征均作了错误鉴别和描述。笔者根据完整且保存有软体附肢的标本,对Guangweicaris Luo,Fu et Hu,2007作了重新研究和复原,据此讨论了该节肢动物的分类归属问题。
    9  POLLEN ANALYSIS OF HYAENA COPROLITES FROM THE TUOZI CAVE AT TANGSHAN,NANJING
    HAO Rui-hui ) XIAO Jia-yi ) FANG Ying-san ) LIU Lin-jing ) TONG Xiu-fang )) Department of Geographical Science Nanjing Normal University Nanjing ) Nanjing Museum Nanjing
    2008(1):123-128. DOI: 1 CSTR:
    [Abstract](237) [HTML](0) [PDF 0.00 Byte](5)
    Abstract:
    Pollen analysis of hyaena coprolites presents relatively high pollen concentration from the Tuozi Cave at Tangshan, Nanjing. Although some coprolites were sterile, it is postulated that after hyaenas devouring plant-consuming prey, pollen were well preserved in the coprolites, and then deposited in the cave, formed hyaena coprolite fossils. Pollen spectra with higher frequencies of Pinus, Tsuga, Quercus, Carpinus, Artemisia, Cyperaceae, Polygonum and Polypodiaceae suggests that the vegetation was grassland or forest-grassland and the climate was humid or semi-humid in earlyPleistocene. This conclusion is consistent with the environmental interpretation derived from the associated fossil fauna found in the Tuozi Cave. This therefore demonstrates that the hyaena coprolites deposit is useful in studying the cave deposits, and reconstructing past vegetation and climate conditions.

    Current Issue


    Volume , No.

    Table of Contents

    Archive

    Volume

    Issue

    Most Read

    Most Cited

    Most Downloaded



    WeChat

    Mobile website