Issue 1,2005 Table of Contents

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  • 1  DISCOVERY OF MUFUSHANELLA FROM THE MIDDLE PERMIAN IN XAINZA AREA OF TIBET
    CHENG Li-Ren~
    2005(1). DOI: 1 CSTR:
    [Abstract](245) [HTML](0) [PDF 0.00 Byte](7)
    Abstract:
    Mufushanella是陈旭教授 1964年创立的,以侧坡内凹、外部壳圈具列孔区别于Nankinella。该属成立与否曾有多人讨论过,争论焦点在于建属时所谓列孔是否与隔壁孔一样,有待进一步证实。采自西藏申扎地区的标本证实了确实是列孔。而且在外部壳圈两列孔之间发育有类似拟旋脊状暗色物质聚集,可能是拟旋脊的“雏形”。并建立新种Mufushanellanankinellaeformissp.nov.
    2  MIDDLE JURASSIC (BATHONIAN-CALLOVIAN) AMMONITES FROM THE AMDO AREA, NORTHERN TIBET
    YIN Jia-Run
    2005(1):1-16. DOI: 1 CSTR:
    [Abstract](248) [HTML](0) [PDF 0.00 Byte](7)
    Abstract:
    New collections of ammonites have been recently carried out in the Amdo area, northern Tibet. The Bathonian ammonites have been referred to Oxycerites oppeli Elmi,Homoeoplanulites cf. homoeomorphus (Buckman),H. cf. acuticosta (Roemer), Choffatia cf. vicenti Mangold, Siemiradzkia cf. matisconensis (Lissajous), Procerites sp., Neuqueniceras cf. yokoyamai Kobayashi and Fukada, and Indosphinctes sp. The Callovian ammonites include Oxycerites cf. subcotarius (Oppel),Macrocephalites? sp., Homoeoplanulites cf. furculus (Neumayr), Indospinctes (Elatmites) cf. reveli Mangold and Reineckeites sp. At generic level Indosphinctes,Indospinctes (Elatmites),Neuqueniceras, Siemiradzkia and Procerites are found in North Tibet for the first time, suggesting an age from middle Bathonian to early Callovian. The Middle Jurassic ammonites in this area exhibit a strong endemicity. Both ORBIS of the Upper Bathonian and KOENIGI zones of the Lower Callovian are significant intervals for faunal dispersal.
    3  NEW RECORD OF DEVONIAN LOCHKOVIAN CONODONTS FROM THE TSAGAANBULAG FORMATION IN THE SHINE JINST AREA, SOUTH MONGOLIA
    Abstract
    2005(1):17-24. DOI: 1 CSTR:
    [Abstract](249) [HTML](0) [PDF 0.00 Byte](6)
    Abstract:
    蒙古南部新金斯特地区萨克黑尔剖面察甘安布拉格组上部发现的牙形刺, 包括Caudicriodusneowos chmidtisp. nov., Caudicriodussp. A, Kimognathussp., “Ozarkodina”planilingua, Pandorinellinaoptima, Ozarkodinaexcavata, 清楚地表明察甘安布拉格组上部应当归到中洛霍考夫阶(泥盆系)而不是像以往那样归到中-上志留统。海相温洛克统和罗德洛统地层在蒙古南部是否存在还需要寻找证据。文章描写了一个新种Caudicriodusneowos chmidtisp. nov.和一个未定种Caudicriodussp. A。
    4  EARLY CRETACEOUS CRUSTACEA (OSTRACODA,CONCHOSTRACA) FROM THE SHINE-KHUDUK FORMATION OF SE MONGOLIA
    YUAN Feng-Tian~
    2005(1):25-35. DOI: 1 CSTR:
    [Abstract](306) [HTML](0) [PDF 0.00 Byte](5)
    Abstract:
    SummaryIn Summer of 2000, an international research group consisted of Japanese, Mongolian, Chinese and American scientists and led by Dr. M.Matsukawa had carried out a field investigation on dinosaur tracks and strata concerned in SE Mongolia, N and NE China for about two months. Here described and illustrated are some crustacean fossils. They include 9 species in 2 genus of ostracodes, and two species of conchostracans (Yanjiestheria gobiensis Chen sp. nov., Neodiestheria mongolensis Chen sp. nov.). These ostracodes could be called the Cypridea-Lycopterocypris assemblage including C. (Cypridea) actuosa, C.(C.) cf. vitimensis, C. (C.) prognata, C. (Pseudocypridina)globra, C.(P.) ellipselloides, C. (Ulwellia) cf. orbiculatodes, Lycopterocypris cf. circulata, L. liaoxiensis, and L.? semirotunda. These forms appeared in several Cretaceous basins of N and NE China, and especially they are very similar to those from the Jiufotang Formation with the famous late Jehol biota in western Liaoning. The Yanjiestheria and Neodiestheria are two common genera of the Lower Cretaceous of China, SW Japan and southern Korean Penusula. Therefore the Shine-Khuduk Formatrion yielding above-mentioned fossil ostracodes and conchostracans of SE Mongolia should be Early Cretaceous in age.
    5  ON THE BOTANICAL RELATION AND THEIR SIGNIFICANCE OF TILIAEPOLLENITES IN CHINA
    SONG Zhi-Chen WANG Wei-Ming and HUANG Fei
    2005(1):36-43. DOI: 1 CSTR:
    [Abstract](262) [HTML](0) [PDF 0.00 Byte](6)
    Abstract:
    文章分析了我国所发现的椴粉属花粉特征,并与现代相关植物花粉进行了对比,发现本属不单与椴树科(Tiliaceae)而且与梧桐科(Sterculiaceae)的某些属种有关系,从而在讨论孢粉植物群的性质及其气候等方面的问题时有了可靠的对比资料,使孢粉学的植物学意义更加可信。
    6  EARLY ORDOVICIAN CHITINOZOANS FROM THE HONGHUAYUAN FORMATION AND LOWER PART OF MEITAN FORMATION IN DATANGKOU OF CHENGKOU, CHONGQING
    CHEN Xiao-Hong ZHANG Miao
    2005(1):44-56. DOI: 1 CSTR:
    [Abstract](252) [HTML](0) [PDF 0.00 Byte](8)
    Abstract:
    Summary The Ordovician sequence is complete and well exposed at Datangkou of Chengkou County, Chongqing City. The investigation has been carried out on chitinozoans, together with the graptolites and conodonts, from the Honghuayuan Formation and the Yingpan Member of the Meitan Formation which represents the late Early Ordovician and early Middle Ordovician in the eastern Dabashan, belonging to the north Yangtze carbonate platform. For this study thirty-five chitinozoan samples were collected so that a stratigraphical control can be expected based on graptolite or conodont zones in this interval. Chitinozoans are lacking in eleven samples while in others are abundant but poorly diversified. A total of seventeen species, three new species (Conochitina datangkouensis sp. nov., C.wengxigouensis sp. nov., Rhabdochitina chenkouense sp. nov.) included, belonging to six genera have been described and figured. Among the key species recorded, the FAD of Lagenochitina esthonica, C. poumoti, C. brevis and ?Eremochitina brevis allow biostratigraphical correlation with graptolite zones of the same section and chitinozoan zones from Quebec, Bohemia, and south-eastern Europe. Yet, we must emphasize the absence of the typical Conochitina symmetrica which is unrecorded in the Honghuayuan Formation.
    7  AN EARLY CAMBRIAN PROBLEMATIC ORGANISM (ANABARITES) AND ITS POSSIBLE AFFINITY
    CHEN Jun-Yuan PENG Qing-Qing
    2005(1):57-65. DOI: 1 CSTR:
    [Abstract](279) [HTML](0) [PDF 0.00 Byte](5)
    Abstract:
    Anabarites is a representative of Early Cambrian tri-radially symmetrical tubecolous organisms with unknown affinity, although it has been speculated as sperpulid worm or as cnidarian with possibly scyphozoan affinity. The present SEM and TEM observation of the phosphate specimens from Lower Cambrian Kuanchuanpu Formation, Ningqiang, southern Shaanxi however reveals a number of diagenetic features of their exoskeleton, which allows to drawn a conclusion of their original mineral composition as aragonite. Ontogenic transition from circular to tri-radial symmetry in Early Meishucunian form and from tri-radial to hexa-radial symmetry in the forms from younger Lower Cambrian strata indicates that a stepwise evolutionary change of circular-radial, tri-radial toward hexa-radial symmetry already evolved in Early Cambrian Anabarites lineage. The hexa-radially symmetrical, extant hexacoralian Anthozoa may have been descending from the circular-radially symmetrical ancestor symmetry through Anabarites-like, tri-radially symmetrical intermediate form. Although the naked crown lineage group of hexacoralians may have evolved in a deep time, the first appearance of aragonitic exoskeleton is far back until Middle Triassic. Anabarites may represent a stem lineage group of hexacoralians and the presence of aragonitic exoskeleton in Anabarites may suggest that the protein molecules in determining the formation of aragonitic exoskeleton of the crown lineage hexacoralian corals may have evolved in Early Cambrian. Life habitat of Anabarites is also speculating and its mass occurrence with micromat-stabilized sea bed suggests that the animal is sessile, with its narrow end attaching to the micromat-stabilized sea bed.
    8  OSTRACODA FROM THE QINGYUANGANG FORMATION IN THE SOUTHERN HAILAER BASIN, Nei MONGOL
    HUANG Qing-Hua~
    2005(1):66-73. DOI: 1 CSTR:
    [Abstract](342) [HTML](0) [PDF 0.00 Byte](6)
    Abstract:
    Abundant Ostracods have been found from the red clastic rocks of the Qingyuangang Formation, the wells of Beier Depression and Wuerxun Depression, southern Hailaer Basin in Inner Mongolia Autonomous Region. Based on the composition and distribution of these Ostracoda species, two Ostracoda assemblages have been classified: Altanicypris obesa-Talicypridea turgida assemblage (lower member) and Chinocypridea augusta-Talicypridea qingyuangangensis assemblage (upper member). These fossils mainly consist of Altanicypris,Talicypridea, Chinocypridea with cristid and Harbinia with reticulation, and are characterized by the strong endemic color, representing the late stage of Late Cretaceous fossil ostracoda fauna in Northeast China. These Ostracoda assemblages may be correlated with that of the Sifangtai Formation of Songliao Basin, indicating their Maastrichtian age, Late Cretaceous.
    9  A SCANNING ELECTRON MICROSCOPICAL OBSERVATION ON A CHEIROLEPIDIACEOUS CONIFER FROM THE LOWER CRETACEOUS OF HUALONG, QINGHAI
    YANG Xiao-Ju
    2005(1):79-86. DOI: 1 CSTR:
    [Abstract](279) [HTML](0) [PDF 0.00 Byte](19)
    Abstract:
    利用扫描电镜对原鉴定为cf. FrenelopsishoheneggeriSchenk的青海化隆早白垩世河口群的标本重新进行了扫描电镜观察和研究,并与我国已知的有关的掌鳞杉科化石以及Frenelopsishoheneggeri的波兰 (模式产地 )标本做了对比研究。结果显示青海标本的表皮构造与Frenelopsishoheneggeri完全不同,而与Pseudofrenelopsispapillosa基本一致。
    10  NEW EXCAVATION OF LIANHUA CAVE IN ZHENJIANG CITY,JIANGSU, EAST CHINA
    房迎三 何未艾 沈冠军 朱玲
    2005(1):87-95. DOI: 1 CSTR:
    [Abstract](241) [HTML](0) [PDF 0.00 Byte](4)
    Abstract:
    2001年对镇江莲花洞进行了第二次考古发掘,从洞内首次获7件石制品和一批哺乳动物化石。5件石核和2件刮削器分别用石英和火成岩制成,初步判断属于旧石器时代中期或稍早,文化面貌似与上世纪末在苏南地区发现的旧石器早、中期文化略有不同。根据对第2、3堆积层间的新生碳酸盐岩并参考动物化石的铀系年代测定,主要含化石的第2层年代应在~100-300ka之间,相当于中更新世晚期到晚更新世早期。由地层堆积、出土石制品和动物化石等埋藏情况分析,莲花洞不是人类的长期居址,很可能只是一处临时停留地。
    11  ICHNOCOENOSIS OF SHORE-SHALLOW LACUSTRINE SHAHEJIE FORMATION (PALEOGENE) IN CHEZHEN SAG, JIYANG DEPRESSION OF BOHAIWAN BASIN, SHANDONG
    SHI Zhen-Sheng~
    2005(1):96-105. DOI: 1 CSTR:
    [Abstract](357) [HTML](0) [PDF 0.00 Byte](5)
    Abstract:
    This ichnocoenosis from the Paleogene Shahejie Formation consists of at least 10 ichnogenera 11 ichnospecies, namely, Beaconites antarcticus, Beaconites capronus, Planolites montanus, Macaronichnus segregatis, Taenidium barretti, Cochlichnus anguineus, Gordia sp., Skolithos sp., Ophiomorpha nodosa, Sagittichnus sp. and Favreina sp. Besides, a type of unknown arthropod crawling trace is also described in this paper. These trace fossils represent Fodinichnia, Pascichnia, Domichnia and Cubichnia of invertebrates such as Vermes, Mollusca, Arthropoda (mainly insects) and others. Most of them were formed in a regularly desiccated shore-shallow lacustrine environment and preserved in full relief and epirelief.Two ichnofossil assemblages are recognized: (1) Beaconites-Taenidium Assemblage, reflecting a shore-shallow lake sedimentary environment under periodically arid climate; and (2) Skolithos-Ophiomorpha Assemblage, representing a relatively high energy shore lake under humid climate.
    12  LATEST BIOSTRATIGRAPHIC ADVANCES OF CAMBRIAN-ORDOVICIAN BOUNDARY IN QINGZHOU AREA, SHANDONG
    WU Gui-Chun~
    2005(1):106-116. DOI: 1 CSTR:
    [Abstract](280) [HTML](0) [PDF 0.00 Byte](4)
    Abstract:
    A new study on conodont biostratigraphy of Cambrian-Ordovician boundary in Yaowangshan Section, Qingzhou area, Shandong Province is first reported in this paper. 9 conodont zones have been recognized in the Chaomidian limestone formation, among which 3 are from the Lower Ordovician and 6 from the Fengshanian Stage of upper Upper Cambrian. The first discovery of the Cambrian-Ordovician Boundary species Iapetognathus fluctivagus in this section is of great significance. It will provide a new rule for Cambrian-Ordovician Boundary study in the Shandong area as well as in the whole North China. Additionally, through the further detailed study, the well-developed Yaowangshan Section will probably become the stratotype section in China, which will deeply affect the establishment of Cambrian stages, a still uncompleted work so far.
    13  AN OUTLINE OF CATHAYSIA FLORA
    QU Li-Jun
    2005(1):117-124. DOI: 1 CSTR:
    [Abstract](253) [HTML](0) [PDF 0.00 Byte](5)
    Abstract:
    作为晚古生代全球四大著名植物群之一的华夏植物群 (CathaysiaFlora),一直是国内外古植物学家研究的焦点。100多年来,有关华夏植物群的研究已取得重要进展。文章在总结前人科研成果的基础上,择要对华夏植物群的分布、组成、起源、演替、绝灭以及与同期其他植物群的比较等作一综述。
    14  INTERPRETATION OF THE PROXIMAL DEVELOPMENT AND BRANCHING DIVISIONS OF SOME EARLY AND MIDDLE ORDOVICIAN GRAPTOLITES BASED ON BSE IMAGES
    ZHANG Yuan-Dong LUO Tian-Tian and MAO Yong-Qiang
    2005(1):125-137. DOI: 1 CSTR:
    [Abstract](239) [HTML](0) [PDF 0.00 Byte](6)
    Abstract:
    背散射电子成像 (BackscatteredElectronImaging,简称BSE),是依托扫描电镜的一种电子成像技术,它的成像原理和特点非常适合用来研究那些表皮尚存的各类笔石标本,是二次电子成像 (SEM)无法替代的。文中简要介绍了这一技术的工作原理,并利用它对我国早奥陶世和中奥陶世部分笔石的始端发育和分枝方式等进行了研究。当前BSE图象显示了许多以往其他途径无法观察到的笔石微细结构,特别是笔石复杂的始端发育特征,结果验证了Psigraptusjacksoni的二分岔式和Rhabdinoporaflabelliformisparabola的四分岔式原始分枝的观点,显示它们都具有最原始的等称笔石式(isograptid type)始端发育型式。此外,BSE图象还显示,底栖固着的树形笔石Airograp tusfurciferus的胞管排列和分枝方式与奥陶纪最早期的漂浮笔石非常相似,表明二者可能存在祖 裔演化关系,或者至少是原始性状上的相似性。
    15  PALYNOFACIES: PRINCIPLES AND METHODS
    LI Jian-Guo~
    2005(1):138-156. DOI: 1 CSTR:
    [Abstract](313) [HTML](0) [PDF 0.00 Byte](5)
    Abstract:
    Summary Palynofacies analyses have been widely applied to determinations of palaeoenvironment and petroleum source potential during the last 20 years. More recently they have also contributed to improving sequence stratigraphic determinations and, to a lesser extent, to detailed biostratigraphic correlations on a regional or local level. However, they are still not used as much as they could be for solving geological problems, especially in China. In this article we review the general principles and methods involved. These include the terminology that is applied to the components of palynological matter, sampling requirements, laboratory techniques, data collection, statistical and numerical methods, and the basis for arriving at reasonable palaeoenvironmental and source potential assessments. Compared to traditional methods of palynological study, which merely focus on palynomorphs, palynofacies analyses place emphasis on the entire composition of acid-resistant organic matter that can be recovered from a rock or unconsolidated sediment. Such an approach commonly enables more precise determinations of depositional environment to be made than is possible using traditional methods of clastic and carbonate sedimentological analyses. Interpretations of organic geochemical and coal petrographic data and the terminology involved are also briefly considered. The types of palynological matter recorded do not necessarily correspond directly to the organic components that can be recognized by other methods of analysis, but this does not prevent similar results from being obtained. Indeed, when palynofacies data are integrated with those derived from other methods, the reliability of the conclusions drawn is usually increased. Hence, they are more likely to stand the test of time.
    16  A NEW SPECIFIC EPITHET PECOPTERIS XIANGYUANENSIS NOM. NOV. FOR SUBSTITUTION OF THE JUNIOR HOMONYM PECOPTERIS LINGULATA LIU, 1987
    刘陆军 曲利军
    2005(1):157-158. DOI: 1 CSTR:
    [Abstract](321) [HTML](0) [PDF 0.00 Byte](14)
    Abstract:
    最近,在与姚兆奇教授一起研究有关栉羊齿类植物的过程中,发现在发表《晋东南地区含煤地层和古生物群》(1987)时,由于付印仓卒,不及仔细参阅相关文献,以致未及时发现书中山西组的一种植物化石舌形栉羊齿PecopterislingulataLiu, 1987(赵修祜等, 1987, 82-83、126页,图版 13

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