Issue 1,2004 Table of Contents

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  • 1  LATE MESOPROTEROZOIC MICROFOSSIL ASSEMBLAGE ON NORTHERN SLOPE OF EASTERN QINLING MOUNTAINS,CHINA:A NEW WINDOW ON EARLY EUKARYOTES
    YIN Lei Ming ) YUAN Xun Lai ) BIAN Li Zeng ) and HU Jie ) ) Nanjing Institute of Geology Palaeontology the Chinese Academy of Sciences Nanjing ) Department of Earth Sciences Nanjing University Nanjing
    2004(1):1-13. DOI: 1 CSTR:
    [Abstract](359) [HTML](0) [PDF 0.00 Byte](8)
    Abstract:
    山西南部永济地区位于东秦岭北坡,在该地区出露良好未变质的中一新元古代地层。在水幽剖面的中元古界汝阳群北大尖组中保存类型多样的微体化石,包括具刺疑源类(Shuiyousphaeridium(Du)Yan,emend.Yin,1997;Tappania Yin,1997),球形、舟形疑源类和多种带状、管状藻类化石。其大的膜壳,突起附属物,脱囊开口,以及同平面不规则分枝丝体等都显示了真核原生物的形态特征。线形和螺旋形微细管体和网状结构物首次见于部分带状丝体和膜状碎片,推测这些管状物是底栖藻类为适应干旱缺水环境而发育的输导或加固支撑的结构物。当前,以具刺疑源类Tappania为特征的相似微体化石组合相继在印度、澳大利亚南部中元古代地层中发现,揭示了约10亿年前真核生物的阶段性发展和海洋原生物生态系统状况。
    2  CONODONTS ACROSS THE LOWER-MIDDLE ORDOVICIAN BOUNDARY IN THE HUANGHUACHANG SECTION OF YICHANG,HUBEI
    LI Zhi-Hong ) WANG Zhi Hao ) WANG Xiao Feng ) CHEN Xiao Hong ) WANG Chuan Shang ) and QI Yu Ping ) ) Yichang Institute of Geology Resources CGS Yichang Hubei ) Nanjing Institute of Geology Paleontology the Chinese Academy of Sciences Nanjing
    2004(1):14-31. DOI: 1 CSTR:
    [Abstract](392) [HTML](0) [PDF 0.00 Byte](6)
    Abstract:
    This paper describes in detail the conodont zonation and some important conodont species across the Lower Middle Ordovician boundary at the Huanghuachang section of Yichang. The first appearance datum (FAD) and the content of the Oepikodus evae , Baltoniodus triangularis zones etc. are revised. North American Midcontinent provincial conodonts Tripodus laevis and Protoprioniodus aranda referred to warm water fauna have been found for the first time in the lower part of the Dawan Formation at Huanghuachang section. The FAD of Tripodus laevis was found at a level, which is 0.3m above the base of Baltoniodus triangularis Zone. The first occurrence of Tripodus laevis was proposed as the base of the Middle Ordovician (see Chen Xu et al ., 2000). So its first occurrence very close to the base of the Baltoniodus triangularis Zone is very important. The evolutionary lineage of Baltoniodus crassulus B. gladiatus (= Acodus ? gladiatus Serpagli, 1974) B. triangularis can be recognized at the Huanghuachang section. So the first occurrence of B. triangularis is a better marker for the base of Middle Ordovician. The correlation of the conodont sequences across the Lower Middle Ordovician boundary among Yichang of Hubei, Newfoundland of Canada, Nevada of USA, Europe as well as Argentina is discussed here. The Huanghuachang section of Yichang, Hubei, can be proposed as a global stratotype for the base of the Middle Ordovician Series.
    3  NEW MATERIAL OF PALAEOLENUS (TRILOBITE, CAMBRIAN) FROM THE EASTERN YANGTZE GORGE AREA, WESTERN HUBEI
    LIN Tian Rui
    2004(1):32-42. DOI: 1 CSTR:
    [Abstract](360) [HTML](0) [PDF 0.00 Byte](11)
    Abstract:
    对采自峡东地区宜昌、秭归等地的Palaeolenus Mansuy,1912的新材料的形态、保存状态、挤压变形以及个体发育等方面的研究,提出Megapalaeolenus Chang,1966的模式种Palaeolenus deprati Mansuy。1912是Palaeolenus Mansuy的模式种Palaeolenus douvillei Mansuy,1912的晚出异名,属名Mega palaeolenus Chang和种名Palaeolenus deprati Mansuy均应予以废弃。文中还对原归于Palaeolenus和Megapalaeolenus的种作较大的归并和修订。
    4  NEW MATERIAL OF THE TRILOBITE GENUS HEXACOPYGE FROM THE ORDOVICIAN OF THE UPPER YANGTZE REGION
    ZHOU Zhi Qiang
    2004(1):43-52. DOI: 1 CSTR:
    [Abstract](286) [HTML](0) [PDF 0.00 Byte](5)
    Abstract:
    Since Yuan and Zhou (1998) erected the remopleuridid genus Hexacopyge , with Remopleurides nasutus Lu, 1957 as the type species, more forms of the genus have been reported from South China (Zhou et al. , 2000; Peng et al ., 2001; Zhou et al., 2001). The hypostome of Hexacopyge as described by Peng et al . (2001, pl. 2, figs. 4, 9, 10) has a tripartite but with no median boss, showing an additional important diagnostic character. New material from the Middle Upper Ordovician of the Upper Yangtze Region indicates that the morphology of species of Hexacopyge changed rapidly through the Middle and Late Odovician, and may have great potential in correlating the regional stratigraphy. Five species of which two are new are described in this paper. They are H. cf. nasuta (Lu, 1957) from the Xiaotan Formation (late Arenig) of Cheng kou, Chongqing; H. turbiniformis sp. nov. from the lower part of the Pagoda Formation (late Llanvirn early Caradoc) of Yichongqiao, Cili and Maocaopu, Taoyuan, Hunan; H. yichangensis sp. nov. from the Puxihe member (middle Caradoc) of the Pagoda Formation (Zhou et al., 1999) of Huanghuachang and Puxiheqiao, Yichang, Hubei; H. cf. yichangensis from the middle part of the Pagoda Formation (middle Caradoc) of Yichongqiao and Maocaopu; and H. sp. from the middle part of the Pagoda Formation (middle Caradoc) of Maocaopu (Text fig. 1).
    5  ONTOGENY OF CAMBRIAN TRILOBITE CHEIRUROIDES PRIMIGENIUS
    ZHU Xue Jian PENG Shan Chi
    2004(1):53-62. DOI: 1 CSTR:
    [Abstract](244) [HTML](0) [PDF 0.00 Byte](13)
    Abstract:
    描述采自皖南东至庞汪剖面黄柏岭组黄绿色页岩中的处于不同发育阶段的Cheiruroides primigenius标本的形态特征和各器官在个体发育过程中的变化趋势。在个体发育过程中,该种最显著的变化是头鞍沟形态的改变和面线后支的逐渐后伸。
    6  NEW POLYMERID TRILOBITES AND THE FIRST RECORD OF ERIXANIUM FROM UPPER CAMBRIAN IN WESTERN HUNAN, CHINA
    DUAN Ye
    2004(1):63-71. DOI: 1 CSTR:
    [Abstract](264) [HTML](0) [PDF 0.00 Byte](6)
    Abstract:
    文中描记3个多节类三叶虫新种:Hardyoides damaensissp.nov.,Meringaspis damaensis sp.nov.,and Rhyssometopus(Rostrifinis)nitidus.sp.nov.,均产自湘西凤凰花桥组中部。同时描记首次在江南斜坡带中发现的Erixanium一属的保留命名种Erixanium cf.E.sentum.Erixanium是全球性分布的多节类三叶虫,其发现对湘西地区生物地层的精确划分和全球对比具有重要意义。
    7  NOTES ON THE PALAEOECOLOGY OF LATE PALAEOZOIC NOEGGERATHIALES
    WANG Jun WU Xiu Yuan
    2004(1):72-85. DOI: 1 CSTR:
    [Abstract](225) [HTML](0) [PDF 0.00 Byte](7)
    Abstract:
    A comprehensive analysis on the palaeoecology of Noeggerathiales indicates that the ecological condition of this group of plants from Cathaysian and Euramerican floras may be similar. It is very possible that Noeggerathiales from both Cathaysian and Euramerican floras could live in wet lower land or arid upland. Palaeoecological sample statistics on certain lower land Cathaysian floras containing noeggerathialean plants indicates that generally in a community, the quantity of genera and species (diversification) of noeggerathialean plants is relatively very limited. However, the number of a particular species (abundance) is usually very high, sometimes even taking the predominant position in the community. As far as the structure of the community is concerned, the community usually has well defined forest layers. Noeggerathiales together with some shenophyllaleans, ferns and seed ferns comprise the understory of a forest. The middle and upper layers may be composed of Lepidodendron, Cordaites, Calamites and some tree ferns or seed ferns.
    8  DISCOVERY OF LATE LLANDOVERIAN BRACHIOPOD XINANOSPIRIFER FROM HAINAN ISLAND AREA, CHINA WITH COMMENTS ON THE NANHAO FORMATION
    ZENG Qing Luan LI Zhi Hong XIE Cai Fu FU Tai An and ZHANG Miao
    2004(1):86-93. DOI: 1 CSTR:
    [Abstract](416) [HTML](0) [PDF 0.00 Byte](12)
    Abstract:
    The Nanhao Formation of the lectostratotype section (usually assigned to the Yanguanian of Early Carboniferous age) contains brachiopods Xinanospirifer flabellum Rong, Xu et Yang, X. cf. sanduensis (Jiang), Plectatrypa ? sp., Cyrtiidae gen. et sp. indet., and trilobite Latiproetus cf. latilimbatus (Grabau) in Maogan Region, Baoting County, Southwest of Hainan Province, China. Among them, Xinanospirifer is a typical element of the Salopinella Xinanospirifer Assemblage Zone of Late Telychian of Late Llandoverian in Yangtze Region, China, its horizon is general equivalent to the upper parts of the graptolite griestoniensis Biozone to graptolite spiralis grandis Biozone (Rong Jia yu and M. G. Bassett, 1996); trilobite Latiproetus ( Astroproetus ) latilimbatus (Grabau) is also a significant element of the Coronocephalus Assemblage Zone of the Upper Member of Xiushan Formation of the Telychian Stage in Yangtze Region, China (Wu Hong ji and P. D. Lane, 1996). The present indisputable fact indicates that the Nanhao Formation of the lectostratotype section belongs to the Late Telychian of Llandoverian, rather than the Yanguanian of Early Carboniferous. The Nanhao Formation must be abandoned.
    9  FACIES CHARACTERISTICS AND TIERING DISTRIBUTIONS OF CHONDRITES
    GONG Yi Ming
    2004(1):93-102. DOI: 1 CSTR:
    [Abstract](349) [HTML](0) [PDF 0.00 Byte](7)
    Abstract:
    Basic characteristics and prevailing genetic models of Chondrites have been introduced and commented. Unusual features of Chondrites from the Lower Middle Ordovician transition have been reported in the west central Utah, USA. They include that tiny Chondrites were cut by other trace fossils associated with them and formed in softground,and that Chondrites were the earliest or shal lowest tiering in the complex ichnofabrics. In existing ichnofacies model trace making courses with ulti stages and ulti tiering are not stressed. Existing ichno tiering models are based mainly on the Mesozoic Cenozoic data. The reported data show that tiering distributions of Chondrites are different in Palaeozoic and Mesozoic Cenozoic. It seems that Palaeozoic tiny Chondrites can be formed in shallowest and middle tierings.
    10  THE POSSIBLE GENETIC EVOLUTIONARY MECHANISM OF THE ORIGIN OF CAMBRIAN "GREAT APPENDAGE" LINEAGE ARTHROPOD
    WANG Xiu Qiang CHEN Jun Yuan
    2004(1):103-107. DOI: 1 CSTR:
    [Abstract](409) [HTML](0) [PDF 0.00 Byte](5)
    Abstract:
    在节肢动物早期演化阶段,前附肢的演化是提高动物感觉和捕食能力的重要事件。化石和发育生物学实验结果表明节肢动物前附肢(即口前附肢)的原型为短棒形触角,在此基础上分别演化为长鞭形触角和腿肢形大附肢;大附肢与螯肢形态相似,为同源构造,因此寒武纪大附肢类群可能是现生螯肢类的干支类群。文中结合发育生物学研究进展分析节肢动物演化早期大附肢产生可能的分子进化机制。认为腿肢形大附肢的发生可能与Hox基因或其它未知发育调控因子参与触角或者附肢原型的发育有关,从而改变原有前附肢发育中Dll基因、dac基因和hth基因间特异的相互作用,导致前附肢获得腿肢特异性发育程序。
    11  RESTUDY OF CRATOSTRACUS SONGHUAJIANGENSIS FROM THE UPPER CRETACEOUS QINGSHANKOU FORMATION OF HEILONGJIANG PROVINCE, CHINA
    LI Gang ) HUANG Qing Hua ) CHEN Chun Rui ) and JIN Xue Xin ) ) Nanjing Institute of Geology Palaeontology the Chinese Academy of Science Nanjing ) Research Institute of Exploration Development of Daqing Oilfield Co. Ltd. Daqing Heilongjiang Province
    2004(1):108-111. DOI: 1 CSTR:
    [Abstract](264) [HTML](0) [PDF 0.00 Byte](5)
    Abstract:
    Through the SEM restudy of the holotype of Cratostracus songhuajiangensis (N. Chen,1976), a circle of serration structure in the lower margin of the growth lines of carapace valve has been detected, which was overlooked in the original descriptions of all species of the genus Cratostracus Huang in the past. This structure has been considered as base of classification of genus or subgenus (Shen et al ., 2002). Thus in the future the further study of the type species Cratostracus merus Huang is needed.
    12  TWO APTIAN BIVALVE GENERA OF HETERODONTA FROM THE QIHULIN FORMATION IN EASTERN HEILONGJIANG PROVINCE
    JIANG Bao Yu CAI Hua Wei
    2004(1):112-117. DOI: 1 CSTR:
    [Abstract](399) [HTML](0) [PDF 0.00 Byte](5)
    Abstract:
    Several bivalve genera or species, ranging from the late Early Cretaceous to early Late Cretaceous, have been found in the Qihulin Formation of the Longzhaogou Group. Among them, the age of Vectianella Casey and Pseudaphrodina Casey is confined to Aptian as known so far, which has great significance to date the Qihulin Formation and Longzhaogou Group. In this paper, the two genera as well as their type species are described systematically, and the age of the Qihulin Formation is also briefly discussed and dated as mainly Aptian.
    13  A NEW SPECIES OF APHRAXONIA FROM THE UPPER MIDDLE DEVONIAN OF THE SOUTH TIANSHAN AREA, XINJIAGN, CHINA
    ZHANG Yu Bo SUN Yuan Lin ) LIU Jian Bo ) and HAN Bao Fu ) ) School of Earth Space Sciences Peking University Beijing China ) The Key Laboratory of Orogenic Belts Crustal Evolution Peking University Beijing China
    2004(1):118-123. DOI: 1 CSTR:
    [Abstract](253) [HTML](0) [PDF 0.00 Byte](5)
    Abstract:
    描述泡沫轴珊瑚属一新种——Aphraxonia wuqiaensis sp.nov,标本产于沿新疆南天山地区乌恰县托帕-吐乐尕特山口公路边的中泥盆统托格买提组。泡沫珊瑚属过去仅在土耳其Anatolia地区和我国湖南株州地区发现,目前在新疆中泥盆统的发现,不仅丰富了该属的化石种资料,同时也表明在中晚泥盆世南天山地区可能与土耳其Anatolia地区和华南地区存在密切的生物地理区联系。通过与该属已知2个种特征和产出时代的对比,看出从中泥盆世Givetian期到晚泥盆世,可能存在从A.zhuzhouensis→A.wuqiaensis sp.nov→A.taurensis的演化谱系和由华南→新疆南天山→土耳其的迁移路线。其演化趋势体现为:1)一级隔壁数目逐渐减少;2)隔壁由中部加厚→边缘加厚;3)主、对隔壁分离,对隔壁伸过中心形成轴端微膨胀板状中轴→轴端膨胀明显的板状中轴→主、对隔壁在中心交汇形成轴端膨胀中轴;4)一级隔壁不达中轴→与中轴相交。
    14  THE DISCOVERY OF BURIED METASEQUOIA WOOD IN LICHUAN, HUBEI, CHINA, AND ITS SIGNIFICANCE
    YANG Jian Ming ) YANG Xin Yu ) and LIANG HUI ) ) Faculty of Life Science Hubei University Wuhan ) Medical College Wuhan University Wuhan
    2004(1):124-131. DOI: 1 CSTR:
    [Abstract](282) [HTML](0) [PDF 0.00 Byte](5)
    Abstract:
    湖北省利川市水杉坝近年发现的阴沉木,有不同时期沉积的茎干、树蔸和树桩,直径最大可达2.32m。根据对6个材料样品的初步比较解剖及扫描电镜图像分析,证明阴沉木为水杉(Metasequoia glyptostroboides Hu et Cheng,1948)。这一发现为树轮年代学的研究及水杉年表的建立提供了材料,为进一步了解水杉的历史演化及华中地区环境变迁创造了条件。
    15  SOME TRACE FOSSILS AFTER THE FRASNIAN-FAMENNIAN EXTINCT IN DUSHAN AREA, SOUTHERN GUIZHOU PROVINCE, CHINA
    WANG Yue
    2004(1):132-141. DOI: 1 CSTR:
    [Abstract](398) [HTML](0) [PDF 0.00 Byte](5)
    Abstract:
    黔南独山地区晚泥盆世弗拉期-法门期(F/F)生物灭绝事件发生后,遗迹化石的出现早于其它化石。描述产于独山地区晚泥盆世法门期早期的遗迹化石,并分析其生态习性,它们在地层中的产出呈现出习性构造逐渐复杂、潜穴管逐渐“粗化”、由层面线性向二维空间到三维空间的发展,反映造迹生物有机体的逐渐变大和完善、生活和活动空间的不断扩大、觅食效率的不断提高以及对环境适应方式的多样性增大的演化历程。
    16  A NEW SPECIES OF ASTEROZOA FROM THE MIDDLE DEVONIAN OF XIANGZHOU, GUANGXI
    HAN Nai Ren ZHANG Jia Zhi
    2004(1):142-146. DOI: 1 CSTR:
    [Abstract](310) [HTML](0) [PDF 0.00 Byte](6)
    Abstract:
    A new species of Asterozoa, i.e., Devonaster guangxiensis sp. nov., is described from the Middle Devonian Tungkangling Formation in Xiangzhou, Guangxi. It is characterized by a very large central disk with long and straight arms, a developed inframarginal and a fat but a little sharpened mouth angle plate. By these features, it differs from the known species Devonaster eucharis (Hall) of America.
    17  THE TERTIARY SEAWAY AND NEW RESERVOIR PROBE IN DONGPU DEPRESSION AS WELL AS ITS SURROUNDED BASINS
    WU Xian Tao
    2004(1):147-154. DOI: 1 CSTR:
    [Abstract](264) [HTML](0) [PDF 0.00 Byte](5)
    Abstract:
    文中列举了海相生物实体化石、海相痕迹化石、海相生物碎屑、以及海相自生矿物等实据后,认为在辽河至长江问的“第二沉降带”这一南北向区间,在孔店组-沙河街组沉积期,存在一条类似于北美的白垩纪海路(Cretaceous seaway)那样的海水通道,通道内海水水体浅,且停留时间短,只在高位期出现。此时海域,宽120~340km,可从下辽河延伸到江汉盆地。就储层沉积环境而言,此时古构造台地区,可形成点礁或碳酸盐岩滩坝。到低位期,海水即离开“第二沉降带”,转而成为星罗棋布的湖泊和下切河流,并随之出现与湖泊相关特别是与下切谷相关的储层。
    18  Digital Technique and its Application in Processing Images of Fossil Speciments - A Brief Introduction
    郝增明
    2004(1):155-157. DOI: 1 CSTR:
    [Abstract](223) [HTML](0) [PDF 0.00 Byte](4)
    Abstract:
    文章简要介绍了利用数码技术处理古生物标本图像的意义,对将古生物标本(或纸质照片)转化为数字化图像的主要设备及其使用特点进行了分析,并介绍了古生物数字图像的主要处理技术和加工软件。
    19  9th International Symposium on Fossil Cnidaria and Porifera Held in Graz(Austria)
    廖卫华 王向东
    2004(1):158-158. DOI: 1 CSTR:
    [Abstract](209) [HTML](0) [PDF 0.00 Byte](5)
    Abstract:
    第9届国际刺丝胞与多孔类化石学术讨论会(9^th International Symposium on Fossil Cnidaria and Porifera)于2003年8月3日-7日在奥地利格拉茨举行。参加会议的除东道主奥地利的代表之外,还有来自澳大利亚、俄罗斯、日本、西班牙、韩国、加拿大、美国、波兰、德国、瑞典、意大利、英国、比利时、法国、阿联酋、乌克兰、捷克、爱沙尼亚、荷兰、瑞士、塔吉
    20  Biodiversity and the Evolution of Palaeoecosystems - A brief Introduction to the 73rd Annual Conference of Palaeontological Society of Germany
    王永栋
    2004(1):159-159. DOI: 1 CSTR:
    [Abstract](233) [HTML](0) [PDF 0.00 Byte](4)
    Abstract:
    德国古生物学会第73届年会于2003年9月29日-10月3日在德国中部的美茵茨大学举行。来自德国各大学、研究所、博物馆、联邦州地质与环境、国土资源部门,以及英国、法国、瑞士、瑞典、荷兰、奥地利等国家的280余位古生物学家、地层学家和地质学家聚集一堂,共同就生物多样性和古 生物演化为主题进行广泛的学术交流和研讨。
    21  Chinese Bioliography of Palaeobotany (Megafossils)
    吴向午
    2004(1):160-160. DOI: 1 CSTR:
    [Abstract](189) [HTML](0) [PDF 0.00 Byte](5)
    Abstract:
    《中国古植物学(大化石)文献目录(1865—2000)》一书近期将由中国科技大学出版社出版。该书是一部集体劳动的成果。由周志炎、吴向午、吴秀元、赵修祜、邓龙华、冷琴、张小弘等悉心编写完成,在编写过程中得到我国绝大多数古植物学专家、学者的积极支持和帮助,约有50多位同行(包括国际友人)热情提供他们的论著目录或查实和澄清有关疑难问题。

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