Issue 3,2002 Table of Contents

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  • 1  HELCIONELLOID MOLLUSK FROM THE LOWER CAMBRIAN HEILINPU FORMATION, CHENGJIANG, YUNNAN
    Loren E.BABCOCK
    2002(3):303-307. DOI: 1 CSTR:
    [Abstract](522) [HTML](0) [PDF 0.00 Byte](7)
    Abstract:
    A small cap shaped fossil from the Shiyantou and Yuanshan Members of the Heilinpu Formation (Lower Cambrian) of eastern Yunnan, China, is here referred to the new species Helcionella yunnanensis. The holotype of the species represents the first record of a helcionelloid mollusk from strata yielding the Chengjiang Biota in the upper part of the Heilinpu Member. Its stratigraphic range, based on two occurrences, is through the upper part of the Meishucunian Stage and into the Qiongzhusian Stage. Rarity of the species in the Yuanshan Member of the Heilinpu Formation may be related to fluctuating environmental condition associated with the inferred tidally influenced, coastal marine depositional environment in which the Chengjiang Biota was preserved.
    2  DISCOVERY OF DICHOTOMOUSLY FORKED GIGANTOPTERID FRONDS FROM CHINA, WITH SPECIAL COMPARISON BETWEEN ASIAN AND AMERICAN GIGANTOPTERIDS
    YAO Zhao Qi LIU Lu Jun
    2002(3):308-321. DOI: 1 CSTR:
    [Abstract](325) [HTML](0) [PDF 0.00 Byte](7)
    Abstract:
    The main difference between the Asian and the American gigantopterids lies in the frond: the fronds of the American gigantopterids are dichotomously bifurcated or simple, while the Asian plants are hitherto only known bearing pinnate or simple fronds that do not fork. The discovery of dichotomously bifurcated fronds of Gigantonoclea from the late Early Permian Tongtseyan Formation in Fujian Province is thus a matter of vital importance, for it brings a much closer relationship between the Asian and the American gigantopterids, although there are still many substantial differences between them. Meanwhile, the resemblance and the differences between the Asian and the American species of Cathaysiopteris are discussed in some length.
    3  COMPARISON IN LEAF ARCHITECTURE BETWEEN CHINESE AND AMERICAN SPECIES OF GIGANTOPTERIDIUM
    Abstract
    2002(3):322-333. DOI: 1 CSTR:
    [Abstract](294) [HTML](0) [PDF 0.00 Byte](5)
    Abstract:
    Among the enigmatic plant group gigantopterids, three genera, Gigantonoclea, Zeilleropteris and Cathaysiopteris, are shared by the American and the Asian Permian floras, but the first recorded American gigantopterid Gigantopteridium has not been described formally in the Gigantopteris flora of China up to now. In the present article a Chinese species of Gigantopteridium is described in detail, and a new emendation is made. Furthermore, some relevant problems about the Chinese species of Gigantopteridium are discussed at some length. The system of Koidzumi (1936) adopted in the classification of the American gigantopterids is an artificial grouping, held together only by characters of venation (Mamay et al ., 1988). According to this system the Chinese and the American specimens here concerned should be ascribed to the genus Gigantopteridium . Thus, the common genera in the Gigantopteris flora of North America and East Asia have increased from three to four. The similarity and difference between the American and the Chinese species of Gigantopteridium are compared in the leaf architecture, although no reproductive organs and anatomical data of Gigantopteridium have been provided for the time being.
    4  CALCISPONGES AND HYDROZOANS FROM PERMIAN REEFS IN WESTERN GUANGXI
    FAN Jia Song ) WANG Yu Mao ) and WU Ya Sheng ) ) Institute of Geology Geophysics the Chinese Academy of Sciences Beijing ) The second geological team Guangxi Bureau of Geology Mineral Resources Nanning
    2002(3):334-348. DOI: 1 CSTR:
    [Abstract](299) [HTML](0) [PDF 0.00 Byte](7)
    Abstract:
    广西西部田林,凌云、凤山地区二叠纪生物礁的造礁生物-海绵、水螅化石保存完美。文中描述串管海绵7属:Stylothalamia,Lichuanospongia,Tebagathalamia,Imbricatocoelia,Intrasporeocoelia,Rhabdactinia,Lingyunocoelis;纤维海绵3属:Peronidella,Intratubospongia,Cavusonella;水螅1属Radiotrabeculopora以及海托盘类Calathium,其中Lingyunocoelia spherica为新属新种,Lichuanospongia guangxiensis为新种,其它均为中国南方二叠纪生物礁内常见分子。Senowbari-Daryan(1990)提出以Discosiphonella来代替Cystauletes,Ascosymplegma,Lichunospongia3属,但Lichuanospongia的房室形状和中央腔缺失横板(泡沫板)显著不同于Discosiphonella,因此文中仍把Lichuanospongia视作独立属,Lingyuncoelia gen.nov。与Sollasia,Girtyocoelia相似,但房室外壁缺乏任何种类的穿孔,因此明显不同于后两属,作者仍把Radiotrabeculopora视为螅纲内的一属,而没有归于纤维海绵目,因为它最明显的特征是发育分布较规则的放射状支柱(不能视为骨纤构造),且那些纵向分布的出水管实际上应视为支柱之间的沟道。
    5  TRIASSIC CONODONTS FROM ZHUGANPO AND "WAYAO" FORMATIONS OF GUANLING, SOUTHWEST CHINA
    陈立德 王成源
    2002(3):349-360. DOI: 1 CSTR:
    [Abstract](329) [HTML](0) [PDF 0.00 Byte](5)
    Abstract:
    贵州关岭地区三叠系“瓦窑组”以N.polygnathiformis繁盛为特征,关岭新铺巴毛林至小洼一带“瓦窑组”一段与杨守仁等(1995)Neogondolella polygnathiformis带的下部相当,相当于卡尼阶。“瓦窑组”中N.polyg-nathiformis(Budurov et Stefanov)的幼年期个体丰富,为研究这一晚三叠的重要属种的个体发育提供条件,在该区竹杆坡组上部发现的Celsigondolella baiyunensis sp.nov.和Neogondolella parafoliata sp.nov。为研究Celsigon dolella与Neogondolella这间的演化关系提供新材料。
    6  SOME LATE WENLOCK-EARLY LUDLOW (SILURIAN) GRAPTOLITES FROM NORTHWEST CHINA
    NI Yu Nan ) SONG Li Sheng ) ) Nanjing Institute of Geology Palaeontology the Chinese Academy of Sciences Nanjing ) Xi''''an Institute of Geology Mineral Resources Xi''''an
    2002(3):361-371. DOI: 1 CSTR:
    [Abstract](286) [HTML](0) [PDF 0.00 Byte](6)
    Abstract:
    记述西北地区志留纪温洛克世晚期-罗德洛世早期笔石5属,11种,进一步肯定罗德洛世早期nilssoni带的地层在陕西紫阳,甘肃迭部和内蒙古额济纳旗的存在,首次确认陕西紫阳和内蒙古额济纳旗发育温洛克世侯默中晚期含笔石地层,大致为parvus带或稍高。
    7  DISCOVERY OF THE CARBONIFEROUS-PERMIAN FORAMINIFERAL MIXED FAUNA FROM THE BOTTOM OF CHIHSIA FORMATION IN SOUTHEASTERN HUNAN
    ZHANG Zu Hui
    2002(3):372-375. DOI: 1 CSTR:
    [Abstract](248) [HTML](0) [PDF 0.00 Byte](5)
    Abstract:
    首次报道湖南省邵东保和堂柳东地区栖霞组底部与史塔夫(Staffella)Ting类群共生的丰富的小有孔虫动物群,包括19属、62种,其中新种2个,该动物群具有非常典型的石炭-二叠纪有孔虫群的混生特点,称Bradyina-Geinitzina组合,它标志着“隆林阶”在湖南地区的首次发现。
    8  FOSSIL OPHIUROIDS FROM TONGZIYAN FORMATION(Middle PERMIAN) IN LONGYAN, FUJIAN
    LIAO Zhuo Ting WANG Xiao Juan
    2002(3):396-402. DOI: 1 CSTR:
    [Abstract](240) [HTML](0) [PDF 0.00 Byte](5)
    Abstract:
    依据福建龙岩坑柄煤矿童子岩组保存完好的化石材料,建立中二叠世(阳新统)蛇尾纲一新种--Aganaster?fujianensis sp.nov。,并根据蛇尾纲与腕足类,双壳类等共生化石组合的埋葬特征,认为古代蛇尾纲具有与现生蛇尾纲相似的集群而居的生活习性。
    9  AN ASSEMBLAGE OF THE NEOPROTEROZOIC STROMATOLITES FROM THE XUZHOU-HUAINAN REGION
    QIAN Mai Ping ) YUAN Xun Lai ) XU Xue Si ) HU Jie and LI Jian Hua ) ) Department of Earth Science Nanjing University Nanjing ) Nanjing Institute of Geology Mineral Resources Nanjing ) Na
    2002(3):403-418. DOI: 1 CSTR:
    [Abstract](364) [HTML](0) [PDF 0.00 Byte](5)
    Abstract:
    徐淮地区新元古代海相碳酸盐岩地层分布广泛,其中由微生物生命活动形成的叠层石十分发育,构成了各种形态及规模的礁体,文内拟就该区地层序列中叠层石组合及其演变过程,讨论其环境的变迁及区域地层对比,根据徐淮地区叠层石组合的层位分布特点,可划分为3个亚组合,自上而下分别为:亚组合I,星散分布于贾园组,赵圩组及九里桥组,以Baicalia,Jurusania,Inzeria,Crassphloem,Grmnosolen及Stratifera为特征,形成小型点礁和生物丘,亚组合Ⅱ。广泛分布于倪园组,九顶山组,张渠组,魏集组,史家组,望山组及四顶山组,包括Conophyton,Jacutophyton,Acaciella,Baicalia,Jurusania,Linella,Tungussia,Anabaria,Minjaria,Katavia,Gymnosolen,Colonnella及Stratifera等多种类型,建造起巨大而复杂的堡礁,堤礁,斑礁,环礁及生物丘/层,亚组合Ⅲ,仅见于金山寨组,以Boxonia,Xiehiella及Anabaria为主,构成中型的点礁及生物丘,这套叠层石组合面貌,造礁规模及多样化程度说明,它们显然形成于新元古代大冰期之前的叠层石繁盛期,其层位大致可与我国华北及东北青白口系上部,俄罗斯上里菲系及澳大利亚苦泉组的叠层石组合对比。
    10  ON A NEW GENUS, ZHUZHAIIA, OF TRIMERELLOID BRACHIOPODS FROM SANQUSHAN FORMATION (MIDDLE ASHGILL OF LATE ORDOVICIAN), YUSHAN AREA, JIANGXI PROVINCE, SOUTHEAST CHINA
    XU Gui Rong
    2002(3):419-427. DOI: 1 CSTR:
    [Abstract](387) [HTML](0) [PDF 0.00 Byte](5)
    Abstract:
    论文描述的三分贝类化石标本发现于江西省玉山县祝宅和马鞍山地区的三衢山组中,新种Zhuzhaiia transitense gen.et sp.nov,的特征是贝体大,两壳近等大,光滑;假铰合面大;腹内肌痕台悬空,无中板;背内肌痕台也悬空,腕腔中部有内向隆起,文中讨论该种的分类位置,根据假铰合面和肌痕台的特征,在总体上可以归入三分贝类,但发育了三分贝科没有的一些特征,如两壳近等大,肌痕台完全悬空,有简单的铰齿和铰窝,所以作者另立新科Zhuzhaiidae fam.nov.,Costitrimerella Rong et Li,1993属的一些特征,如其背壳内肌痕台前部悬空,无中板支持,似乎显示从三分贝科到新科的过渡性质,而新科在许多特征上也显示了从三分贝类到五房贝类的一些过渡性质。
    11  A NEW SPECIES OF THE TRILOBITE ABADIELLA FROM THE LOWER CAMBRIAN OF THE EASTERN OFFICER BASIN, SOUTH AUSTRALIA
    J.B.JAGO J.N.DUNSTER
    2002(3):428-433. DOI: 1 CSTR:
    [Abstract](398) [HTML](0) [PDF 0.00 Byte](8)
    Abstract:
    The first well preserved Cambrian trilobites are described from the Ouldburra Formation, eastern Officer Basin, South Australia. A new trilobite species, Abadiella officerensis, of Atdabanian age, is described. Abadiella and Parabadiella are considered to be synonyms.
    12  SO-CALLED MIDDLE TRIASSIC "CLARAIA" (BIVALVIA) FROM GUANGXI, SOUTH CHINA
    CHEN Jin Hua ) Toshifumi KOMATSU ) ) Nanjing Institute of Geology Paleontology the Chinese Academy of Sciences Nanjing China ) Department of Science Kumamoto University Kurokami Kumamoto Japan
    2002(3):434-447. DOI: 1 CSTR:
    [Abstract](200) [HTML](0) [PDF 0.00 Byte](6)
    Abstract:
    描述报道广西中三叠世地层中一类形态相似于克氏蛤(Claraia)的双壳纲化石,经研究,发现海扇科的关键特征丝梳,认为不属于克氏蛤,而可能是Periclaraia属的一个新种,并初步探讨化石层的生态环境,认为可能是相对隔离的盆地中央区,新种是由海扇类进入隔离环境后经特化形成的,新种与克氏蛤的表面相似性是生活习性的相似性导致的形态趋同现象。
    13  PRESERVATION AND MORPHOLOGIC INTERPRETATION OF LATE SINIAN GAOJIASHANIA FROM SOUTHERN SHAANXI
    CHENZheandSUNWei Guo
    2002(3):448-454. DOI: 1 CSTR:
    [Abstract](252) [HTML](0) [PDF 0.00 Byte](5)
    Abstract:
    OneofthemostabundantfossilsofGaojiashanBiota,GaojiashaniaYangetal.,1986,wasoriginallydescribedbyLinandZhang(1986)fromtheGaojiashanMember,DengyingFormaitonintheGaojiashansection,NingqiangCounty,southernShaanxi.Theyareburiedinsitu,occurringinthesiltstoneandlimestone.Gaojiashaniaisastraightorcurvedtubelikefossilcomposedofaseriesofridgesandrings.MostofGaojiashaniaarethreedimensionallypreservedandsomespecimensarepreservedasmembraneslyingonthesurface.Thedifferentappearanceandcharacterareassumedtoberesultedfromthediageneticprocessandmineralization.Earlydiageneticpyriteplayedanimportantroleinthepreservationofthefossils.Thesoftbodiesofthefossilscanbepreserved,thissuggeststhatthepyritemineralizationoccurredveryearlyinthediagenetichistoryofafossilandpriortoappreciabledecayofsoftbodiesofthefossils.Exceptionalpreservationisduetorapidmineralizationpriortodecay.Gaojiashaniawasfirstdescribedaswormandreferredtoannelids.Thespecimensareoftenthreedimensionallypreservedandcomposedofaseriesofseparateringslinedonthesubstrate.Thesefeatureshavenotbeenknownfromanykindofwormsandtracefossils.TheGaojiashaniaappearsmetamericandtheringsasthehardpartsofthebodyseemtohavebeenbiomineralized,perhapshadnorelationshipwiththeannelids.
    14  DIATOM ASSEMBLAGES IN SEDIMENT AND DYNAMIC PROCESS OF LAKE TROPHIC EVOLUTION FROM LONGGAN LAKE, EAST CHINA
    羊向东 沈吉 夏威岚 朱育新
    2002(3):455-460. DOI: 1 CSTR:
    [Abstract](305) [HTML](0) [PDF 0.00 Byte](5)
    Abstract:
    通过龙感湖浅孔沉积物硅藻分析,结合210Pb代代测定和鞘拱对应分析(DCA)方法,恢复近两个世纪以来龙感湖硅植物群演替历史和营养动态演化过程,结果表明,20世纪初期(1906AD),硅藻种群中小型底禁的Fragilaria类型,Amphora libyca,Pinularia sp.等迅速减少或消失,而浮游种Aulancoseira granulata 增多,与Eunotia类型共同组成优势属种,反映龙感湖开始由贫营养状态向中营养状态转变,为水体富营养化开始发生时间;20世纪70年代初期以来,硅藻又逐渐由营附生为主的Cocconeis placentula,Epithemia sp.,Gomphonema,.sp。等占主导地位,反映了营养程度的又一次提高,并呈现加重趋势,硅藻组合变化反映的湖泊营养级的增加与流域人类活动影响有关,早期的湖泊富营养化响应于流域土壤侵蚀速率的增加,而70年代以来湖泊营养程度的加重则与龙感湖流域农业化肥的使用和湿地植被的破坏导致湿地拦截功能的减弱或消失有关。
    15  ON THE MOST PRIMITIVE AMIID FISH FROM UPPER TRIASSIC OF XINGYI, GUIZHOU
    LIU Guan Bang ) Yin Gong Zheng ) and Wang Xue Hua ) . Department of Earth Sciences Nanjing University Nanjing . Geological Survey of Guizhou Guiyang . State Key Laboratory of Paleobiology Stratigr
    2002(3):461-463. DOI: 1 CSTR:
    [Abstract](274) [HTML](0) [PDF 0.00 Byte](5)
    Abstract:
    A primitive amiid fish, Guizhouamia bellula gen. et sp. nov., is described in this paper, which is found from the marine Upper Triassic rocks of Xingyi, Guizhou. This fish is of great palaeontological interest because it belongs to a form of amiid which is so primitive in the nature of vertebral column, the unusual small size and the simply bifurcated rays that serve well to represent the genuine ancestor of the common Cretaceous Cenozoic amiid genera such as Cyclurus, Amia , etc., which have very wide distribution in North America and Western Europe. The new discovery shows that the history of the amiid fishes could be further traced back from about 150 million years ago to about 220 million years ago.
    16  ADVANCE IN STUDY OF THE TAXONOMY OF CNIDARIA AND THE ORIGINS AND RELATIONSHIPS OF PALAEOZOIC CORALS
    LIAO Wei Hua
    2002(3):464-468. DOI: 1 CSTR:
    [Abstract](358) [HTML](0) [PDF 0.00 Byte](11)
    Abstract:
    国际最新研究表明,刺丝胞动物门包括水螅,钵水母和珊瑚3个纲,古生代的床板珊瑚和皱纹珊瑚以及中,新生代的石珊瑚是珊瑚纲中最主要的3个月,分别出现于早奥陶世,中奥陶世和中三叠世,它们在地层的划分,对比和古地理环境的解释方面都起着非常重要的作用,寒武纪发现的所谓“珊瑚”化石,大部分不是珊瑚,而应归属于藻类,海绵和苔藓虫,只有其中的一部分可能是珊瑚或刺丝胞,但它们并不属于真正的皱纹珊瑚或床板珊瑚,皱纹珊瑚不是起源于寒武纪的这些所谓的“珊瑚化石”,而可能是起源于一种具有骨骼的单体海葵,奥陶纪和二叠纪都曾先后出现类似于石珊瑚的化石,但它们并不是中三叠世石珊瑚直接的祖先,石珊瑚也不是起源于皱纹珊瑚而可能是起源于一种或多种带骨骼的海葵,古生代的珊瑚化石是研究生物灭绝,复苏事件最理想的生物门类之一,奥陶纪末的O/S和晚泥盆地的F/F这两次灭绝事件使许多珊瑚分类单元惨遭浩劫,而二叠纪末的P/T灭绝事件则使全部古生代的皱纹珊瑚和床板珊瑚消亡。

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