Issue 2,2007 Table of Contents

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  • 1  EARLY AND MIDDLE ORDOVICIAN GRAPTOLITES FROM THE MEITAN FORMATION IN ZUNYI, GUIZHOU, CHINA
    ZHANG Yuan-dong LIU Xiao ZHAN Ren-bin
    2007(2):145-166. DOI: 1 CSTR:
    [Abstract](262) [HTML](0) [PDF 0.00 Byte](9)
    Abstract:
    对贵州遵义高桥大角寺剖面的奥陶系湄潭组下段和中段笔石的研究结果表明,湄潭组下段从下而上可以识别出Didymograptellus eobifidus带、Corymbograptellus deflexus带和Azygograptus suecicus带;中段含有一层笔石,缺少特征属种,根据其总体面貌,可能相当于Expansograptus hirundo带。文章描述其中11属16种:Pseudophyllograptus angustifolius(Hall),Phyllograptus claviger(Monsen),P.annaHall,Didymograptelluseobifidus(Chen and Xia),D.protoindentus(Monsen),Acrograptus kurcki(T rnquist),Corymbograptus vacil-lans(Tullberg,1880),C.deflexus(Elles and Wood),Expansograptus extensus(Hall),E.nitidus(Hall),Xi-phograptus lofuensis(Lee),X.cf.lofuensis(Lee),Azygograptus suecicusMoberg,Dictyonemasp.,Den-drograptussp.,Inocaulis plumulosusHall。这一笔石动物群分异度较低,大多数为上扬子区的常见属种,代表当时黔中古陆北缘近岸海洋环境中的笔石动物群面貌。
    2  MOULTING VARIABILITY IN THE MIDDLE DEVONIAN TRILOBITE DUCTINA FROM NANDAN,GUANGXI, CHINA
    HAN Nai-ren CHEN Gui-ying
    2007(2):167-182. DOI: 1 CSTR:
    [Abstract](255) [HTML](0) [PDF 0.00 Byte](7)
    Abstract:
    Ductina vietnamila Maximova产于广西南丹罗富中泥盆统下部塘丁组上部,三叶虫化石多为原地埋葬,其中有一些为蜕壳标本。蜕壳构造的特征是:头胸分开,头前移并沿轴向错开、翻转180°;胸节基本按序排列,有时后两三个胸节前倾;胸与尾多分离,沿轴向微错开,有时尾向后翻转180°。
    3  A LYCOPSID PLANT FROM THE UPPER DEVONIAN OF CHANGYANG, HUBEI PROVINCE, CHINA
    XUE Jin-zhuang HAO Shou-gang
    2007(2):183-194. DOI: 1 CSTR:
    [Abstract](277) [HTML](0) [PDF 0.00 Byte](8)
    Abstract:
    A lycopsid plant with preserved morphology and anatomy is described from the Huangjiadeng Formation (Frasnian) of Hubei Province. Its stems are slender. The leaf bases are spindle in shape, and arranged in helices. Leaves are persistent and spiny. This plant bears distal cones. Sporophyll is spoon-like and lanceolate in form,with spines along its margins. Sporangia are circular or elliptical in surface view. In anatomy, the stem has a solid strand of exarch primary xylem. Protoxylem tracheids, composed of annular or helical elements, appear as minute ridges on the stele periphery. Metaxylem tracheids are composed of scalariform elements, showing no connecting "Williamson's striations" between the bars. The shared characteristics of the present plant and Longostachys (Zhu,Hu and Feng) Cai and Chen, from the upper Middle Devonian (Givetian) of Hunan Province, lie in linear and spiny leaves, spindle-shaped and helically arranged leaf bases, spoon-like or lanceolate sporophylls; further more, the dimensions of leaves, leaf bases and sporophyll are also quite alike. However, they show differences in some anatomical characteristics; the present plant bears no secondary xylem, no pith, and no connecting materials between thickened bars of metaxylem tracheids. The preserved characteristics, however, are incomplete for establishing a new species.We temporarily assign our specimens to cf. Longostachys sp.
    4  PLANT MEGAFOSSILS FROM THE PERMIAN CHANGHSINGIAN MARINE DEPOSITS OF FUSUI, GUANGXI, CHINA
    LIU Lu-jun YAO Zhao-qi
    2007(2):195-212. DOI: 1 CSTR:
    [Abstract](314) [HTML](0) [PDF 0.00 Byte](7)
    Abstract:
    SummaryA taphoflora from the marine Changhsiangian deposits in the area of Dongluo Town, Fusui County, Guangxi Zhuang Autonomous Region is described for the first time. The flora is composed of 14 genera and 23 species, including four new species. The characteristics of the flora as well as its taphonomic and ecological significance are also briefly discussed.Gymnosperms occupied 61% of the total content in this upland flora, while the gymnosperms in the coal-forming lowland flora of the neighbouring area only made up 33% of the floral content. Thus it can be seen that the upland flora from Fusui, Guangxi reveals a transitional character of the land floras from the Palaeozoic to the Mesozoic.In addition, the specific composition of the described flora is quite different from that of the coeval upland flora from North China. Consequently, the Changhsingian upland floras from North and South China are not attributed to the same phytogeographic province as usually considered.
    5  THE ASSEMBLAGE SEQUENCES AND CHARACTERISTICS OF THE DEVONIAN GIVETIAN AND FRASNIAN RUGOSE CORALS IN NEAR-SHORE FACIES FROM SOUTH CHINA
    LIAO Wei-hua MA Xue-ping
    2007(2):213-224. DOI: 1 CSTR:
    [Abstract](340) [HTML](0) [PDF 0.00 Byte](16)
    Abstract:
    SummaryDevonian near-shore deposits are widespread in South China and rich in benthic corals. The Middle Devonian (Givetian) and Upper Devonian (Frasnian) rugose corals in South China flourished in a near-shore shallow water environment. Significant works on Devonian biostratigraphy and corals have been done in the sixties and the seventies of the previous century by Wang and Yu(1962), Wang et al.(1964, 1965, 1974, 1979), Nanjing Institute of Geology and Palaeontology, CAS (1974), Liao (1977), Liao et al. (1978, 1979), Hou (1978), Yang et al. (1979), Yu et al. (1979).
    6  ONTOGENY AND MALFORMATION OF TAMDASPIS JINGXIENSIS SP. NOV.(TRILOBITA, CAMBRIAN) FROM JINGXI, GUANGXI, CHINA
    ZHU Xue-jian PENG Shan-chi DU Sheng-xian HU You-shan
    2007(2):225-231. DOI: 1 CSTR:
    [Abstract](448) [HTML](0) [PDF 0.00 Byte](9)
    Abstract:
    SummaryTamdaspis jingxiensis sp. nov. is described from the Sandou Formation, Guole section, Jingxi County, southwestern Guangxi, China. The material includes a number of complete exoskeletons that added thoracic characters to the genus. Based on articulated materials of T. jingxiensis sp. nov., Liushuicephalus Luo, 1983 is regarded as a junior synonym of Tamdaspis. The material of T. jingxiensis includes two malformed exoskeletons, and the malformation seems to be caused by predation.
    7  MEDUSIFORM FOSSILS FROM THE MIDDLE MIDDLE CAMBRIAN JIALAO FORMATION OF JIANHE COUNTY, GUIZHOU, CHINA
    YANG Xing-lian ZHU Mao-yan ZHAO Yuan-long MAO Yong-qin WANG Yu-xuan
    2007(2):232-237. DOI: 1 CSTR:
    [Abstract](339) [HTML](0) [PDF 0.00 Byte](8)
    Abstract:
    Medusiform eldoniids, which are a group of pelagic animals with coiled alimentary canal and tentacles, are confined to the Cambrian, especially in lower to middle Cambrian of Poland, Spain, Siberia, North America and South China, etc. Eldoniids are one of important components of the three Burgess Shale-type hiotas, including the Chengjiang Biota, Kaili Biota and Burgess Shale Biota. Here we describe a medusiform fossil from the middle Cambrian Jialao Formation at Balang village, Gedong Town, Jianhe County, Guizhou Province. Although the fossil has the similar features as eldoniids with bifurcated lobes, the poor preservation of a single specimen makes it premature to assign it to a genus or species. The undefined genus and species is discoid in shape with 32-36 rough radial lobes. The fossil horizon is about 1 fossil zone above that of Pararotadiscus guizhouensis from the Kaili Biota. Based on the study of trilobites, the geological age is middle middle Cambrian. It is the highest horizon of eldoniids in China. In the past, the exceptional preservation of soft-bodied fossils was often discovered in the mudstone, and was infrequent in the carbonate. Thus this occurrence in the Jialao Formation is an important evidence of soft-bodied fossils in the carbonate. The medusiform fossil reported here provides new information of the Cambrian life.
    8  A NEW GENUS OF EARLY TRIASSIC PERLEIDID FISH FROM CHANGXING, ZHEJIANG, CHINA
    ZHAO Li-jun LU Li-wu
    2007(2):238-243. DOI: 1 CSTR:
    [Abstract](347) [HTML](0) [PDF 0.00 Byte](13)
    Abstract:
    SummaryThe fossil fish described in this paper is found from Early Triassic Yinkeng Formation in the P-T GSSP section (D), Changxing County of Zhejiang Province, South China.
    9  EARLY CRETACEOUS CONCHOSTRACANS FROM THE BAYINGEBI FORMATION OF INNER MONGOLIA, CHINA
    FU Guo-bin LI Gang REN Yu-guang REN Zhong-yue DING Liang-tang
    2007(2):244-248. DOI: 1 CSTR:
    [Abstract](321) [HTML](0) [PDF 0.00 Byte](7)
    Abstract:
    The Early Cretaceous fossil conchostracans are collected from the Bayingebi Formation of Huluntaolegai, Bagemaode in the Inggen-Ejin Qi Basin, weastern Inner Mongolia. The conchostracan fauna consists of Diestheria jiayuguanensis Shen and Chen, in Shen et al., 1982, Yumenestheria delicatula Shen and Chen, in Shen et al., 1982. These two species are common in the Chijinpu Formation of the Hexi Corridor, Gansu. This indicates a correlative relationship between these two formations, and both of them are of Jiufotangian age.
    10  TRACE FOSSILS FROM THE UPPER MEMBER OF LOWER SILURIAN TATAAIERTAGE FORMATION, KALPIN AREA,TARIM BASIN, XINJIANG, CHINA
    BAI Zhong-kai HU Bin QI Yong-an ZHANG Guo-cheng
    2007(2):249-256. DOI: 1 CSTR:
    [Abstract](232) [HTML](0) [PDF 0.00 Byte](7)
    Abstract:
    Based on the study of the Silurian sections in the Kalpin area of the northwestern Tarim Basin, eight ichnogenus and eight ichnospecies were recognized in the Lower Silurian Tataaiertage Formation. According to the composition, occurrence and distribution characteristics of these trace fossils and their host rock features, two types of ichnoassemblages under different sedimentary environments have been proposed as follows: 1)Thalassinoides-Macaronichnus ichnoassemblage, including such common trace fossils as Thalassinoides suevicus,Macaronichnus segregatis and Rhizocorallium ganxiensis, indicating a sand flat sedimentary environment with high oxygen content and energy; and 2) Scoyenia-Beaconites ichnoassemblage, containing such trace fossils as Scoyenia gracilis, Beaconites antarcticus, Planolites vulgaris, Palaeophycus wutingensis and Monocraterion cf.tentaculatum, suggesting a mixed sand flat-mud flat sedimentary environment with mid-low energy condition.
    11  OSTRACOD BIOSTRATIGRAPHY OF THE UPPER CRETACEOUS FIRST MEMBER OF THE NENJIANG FORMATION IN THE SONGLIAO BASIN
    ZHANG Zhi-li LIU Zhen-wen ZHANG Min ZHANG Ying
    2007(2):257-266. DOI: 1 CSTR:
    [Abstract](339) [HTML](0) [PDF 0.00 Byte](7)
    Abstract:
    Based on a detailed study of ostracod specimens in 87 samples from the selected Xing-104 well, Xing-1- Ding-3-Jian-323 well and Ta-3 well, a total of seven ostracod fossil zones of the Upper Cretaceous First Member of the Nenjiang Formation in the Songliao Ba- sin were established, including one newly established ostracod fo zone. The detail. The important f tion of rock ssil zone and one revised ostracod fossil seven ostracod fossil zones are described in seven ostracod fossil zones could provide an ramework for the subdivision and correlaunits of oil-bearing beds in the oilfield.
    12  PLICATOUNIO (GUANGXIPLICATOUNIO), A NEW NAME FOR PLICATOUNIO(GUANGXICONCHA) YAO AND YU, 1986 (BIVALVIA: PLICATOUNIONIDAE),PREOCCUPIED BY GUANGXICONCHA ZHANG, 1977 (BIVALVIA: LUNULACARDIIDAE)
    FANG Zong-jie
    2007(2):267-268. DOI: 1 CSTR:
    [Abstract](256) [HTML](0) [PDF 0.00 Byte](6)
    Abstract:
    姚培毅、于菁珊(1986)为广西扶绥下白垩统的褶珠蚌类标本建立了一个新亚属Plicatounio(Guangxiconcha)Yao and Yu,以Plicatounio(Guangxiconcha)fortisYao and Yu,1986(230页,图版1,图4;图版2,图3,6)作为模式种。然而,早在1977年,张仁杰(张仁杰等,1977,492页)就已为广西河池下泥盆统的小月鸟蛤科(Lunulac-ardiidae)标本创建了新属名GuangxiconchaZhang,模式种是Guangxiconcha hechiensisZhang(张仁杰等,1977,492页,图版193,图1—3)。根据“国际动物命名法规”(Rideet al.,1999),本人提出一个新的亚属名广西褶珠蚌Plicatounio(Guan-gx…
    13  Editorial Committee of Acta Palaeontologica Sinica
    2007(2):F0004-F0004. DOI: 1 CSTR:
    [Abstract](235) [HTML](0) [PDF 0.00 Byte](6)
    Abstract:

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