Issue 4,2001 Table of Contents

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  • 1  ULTRASTRUCTURES IN THE SPIROTHECA OF LATE PERMIAN GALLOWAYINELLA AND ITS AGE
    ZHOU Jian Ping ZHANG Lin Xin
    2001(4). DOI: 1 CSTR:
    [Abstract](234) [HTML](0) [PDF 0.00 Byte](6)
    Abstract:
    电子显微镜研究显示 ,Gallowayinella旋壁的透明层与Fusulinella型 (四层式旋壁 )的透明层在晶粒形状、大小和排列方式方面有较大的差异 ,而与Palaeofusulina旋壁的超微构造特征一致。Gallowayinella属的分类位置应归于古纺锤亚科 (PalaeofusulininaeM .-Maclay ,196 3) ,时限为晚二叠世吴家坪期早期至长兴期早期。G .meitienensis一种不能作为我国长兴阶下部的一个带化石
    2  STUDY ON THE FUSULINIDA FAUNA IN THE TAIYUAN FORMATION FROM THE EAST AREA OF JINING COALFIELD, SHANDONG PROVINCE
    JIANG Han Chao ) WANG Ming Zhen ) ZHANG Xi Qi ) LI Zeng Xue ) ) Institute of Geology Geophysics Chinese Academy of Sciences Beijing ) Department of Geoscience Shandong University of Science Technolog
    2001(4). DOI: 1 CSTR:
    [Abstract](317) [HTML](0) [PDF 0.00 Byte](11)
    Abstract:
    通过对山东济宁煤田东区太原组类动物群的系统研究 ,共鉴定出类化石 15属 10 8种。根据类化石在地层中的分布和垂向的变化规律 ,自上而下建立一个带三个亚带 :Pseudoschwagerina带 ,3)Boultoniawillsi Schwagerinacervicalis亚带 ,2 )Pseudofusulinasphaeroidea Schwagerinaneolata亚带 ,1)Rugosofusulinacom plicata Quasifusulinalongissima亚带。通过与邻区及华北部分地区对比 ,本区太原组类动物群的地质时代为早二叠世早期 ,本区石炭 二叠系应置于太原组第十一层灰岩之底
    3  A NEW SMALL PLANT FROM THE XICHONG FORMATION OF YUNNAN, AND DISCUSSION ON THE FLORAL ASSEMBLAGE OF LATE MIDDLE DEVONIAN IN SOUTH CHINA
    Abstract
    2001(4):424-432. DOI: 1 CSTR:
    [Abstract](356) [HTML](0) [PDF 0.00 Byte](12)
    Abstract:
    研究我国云南中泥盆世晚期西冲组的一种细小植物Psilophyton striatum sp.nov.,它具有二歧分叉光滑轴和生殖枝,生殖枝由三次等二歧分叉枝系和族生孢子囊组成,枝系末端对生两对直立孢子囊,根据对已有材料的分析,宜将华南中泥盆世晚期植物组合改名为Lepidodendropsis arborescense-Minarodendron cathaysiense Eocladoxylon minutum(LME)组合,它以石松类植物为主,共生有“真蕨植物”和三枝蕨类,分为小形树状植物和地面植物两个生态系统,同时,与世界上同期植物群进行了对比。
    4  FOSSIL RECORDS OF MAGNOLIACEAE
    Abstract
    2001(4):433-442. DOI: 1 CSTR:
    [Abstract](555) [HTML](0) [PDF 0.00 Byte](11)
    Abstract:
    Based on the fossil records, it is found that no credible megafossil record of Magnoliaceae exists in Jurassic deposits and all Jurassic microfossil reports remain equivocal and require further study up to now. Many species of Magnoliaceae were widely distributed in the Northern Hemisphere, such as Asia, Europe and North America while there was no fossil record in Africa and Oceania since Cretaceous. Among the magnoliaceous fossils, the earliest one is Archimagnolia rostrato stylosa Tao et Zhang reported from the Lower Cretaceous Dalazi Formation of Yanji district, Northeast China. According to the fossil records and the distribution pattern of extant Magnoliaceae, the results can be drawn as follows: 1) This family originated no later than Early Cretaceous (Aptian to Albian). 2) It seems that this family probably originated in East Asia, and then spread southward to tropical Asia and northward to Europe. The North American Magnoliaceae may have been derived from the Eurasian landmass before the complete separation between North America and Europe, and the South American Magnoliaceae might come from North America. 3) The fact that Magnolia occurred earlier than Liriodendron supports the result drawn from morphological and molecular analysis that Magnolia is more primitive than Liriodendron.
    5  ON THE APPLICATION OF THE EQUILIBRIUM THEORY OF ISLAND BIOGEOGRAPHY TO THE PERMIAN CATHAYSIAN FLORA OF CHINA
    WANG Jun ) SHEN Guang Long ) ZHANG Hong ) WU Xiu Yuan ) ) Nanjing Institute of Geology Palaeontology Chinese Academy of Sciences Nanjing ) Department of Geology Northwest University Xi''''an ) Xi''''an
    2001(4):443-449. DOI: 1 CSTR:
    [Abstract](343) [HTML](0) [PDF 0.00 Byte](5)
    Abstract:
    岛屿生物地理平衡理论已被初步证明能够运用于古生物地理学研究,但由于地质古生物学资源的局限性,目前运用这一理论对地史生物群进行相关研究主要表现在对相关问题进行检验。文章总结了对我国二叠纪华夏植物群进行岛屿生物地理平衡理论偿试性研究的各项成果,指出开展此项研究所需的地质古生物学基础和目前存在的一些缺陷,此外,还展望了岛屿生物地理平衡理论运用于地质古生物学的前景。
    6  AN EARLIEST CRETACEOUS PALYNOLOGICAL ASSEMBLAGE FROM THE TUNTIANYIN FORMATION IN ANTU, JILIN PROVINCE
    LI Wen-Ben
    2001(4):450-456. DOI: 1 CSTR:
    [Abstract](255) [HTML](0) [PDF 0.00 Byte](7)
    Abstract:
    吉林省安县明月镇屯田营组上部的孢粉化石组合以含大量松柏类各种两气囊花粉,伴以少量Schizaeoisportes,Fixisporites,Cicatricosisporites等属孢子为特征,组合面貌与辽西义县组下部尖山沟层的组合一致,时代属早白垩世贝利亚斯期,整个屯田营组只相当于义县组的下部,缺乏与义县组上部相当的地层。
    7  GECUNPOLLIS GEN.NOV.FROM CRETACEOUS GECUN FORMATION OF JURONG AREA IN JIANGSU, AND ITS DISTRIBUTION
    ZHOU Shan-Fu
    2001(4):457-462. DOI: 1 CSTR:
    [Abstract](326) [HTML](0) [PDF 0.00 Byte](11)
    Abstract:
    建立并描述新属葛村粉(Gecunpollis gen.nov)及其3新种和1比较种,新属以球形,远极具大口,口上益有薄膜为特征,产于苏南句容地句11井葛村组下部上段至中上部,其可能属于一种已灭的裸子植物花粉,分布时代为晚Barremian晚期至Aptian期,葛村组以往被归属为Aptian期至Albian期,句11井下部出现棒纹粉带表明,完整的葛村组应为晚Barremian期至Albian期。
    8  PERMIAN CONODONT PROVINCIALISM, EVOLUTION AND THEIR CONTROLLING FACTORS
    MEI Shi Long
    2001(4):471-485. DOI: 1 CSTR:
    [Abstract](403) [HTML](0) [PDF 0.00 Byte](11)
    Abstract:
    阐述二叠纪6个时期牙形石的分布及其古地理分区的划分和演变,探讨牙形石古地区分区的主控因素及其与古气候演变的关系,应用上述古地理分区模式恢复科迪勒拉山脉有关地体牙形石群落的古地理。
    9  HELMET-LIKE FOSSILS FROM THE BASAL CAMBRIAN PHOSPHORIC STRATA OF CHINA
    Qian Yi Li Guo-Xiang
    2001(4):486-496. DOI: 1 CSTR:
    [Abstract](355) [HTML](0) [PDF 0.00 Byte](11)
    Abstract:
    This paper mainly deals with several kinds of peculiar metazoan fossil remains, which were collected from the basal Cambrian phosphoric rock series of both Yangtze and Tarim platforms, China. They were artificially taken as helmet like fossils by their appearance, since they are usually low cone like with apex curved downward, and are somewhat similar to ancient helmets. Three genera and 4 species are described, including 1 new genus and 1 new species; and their distributions, preservation and affinities are briefly discussed. Based on their features, the authors deduce that they should represent outer hardparts of various metazoans.
    10  DISCOVERY OF TIANZHUSHANIA IN DOUSHANTUO PHOSPHORITES IN WENG''''AN, GUIZHOU PROVINCE
    YIN Chong Yu GAO Lin Zhi XING Yu Sheng
    2001(4):497-504. DOI: 1 CSTR:
    [Abstract](440) [HTML](0) [PDF 0.00 Byte](11)
    Abstract:
    The large acanthomorphic acritarch Tianzhushania spinosa (Yin L et Li) Yin C(1988) and a new species Tianzhushania tuberifera sp. nov. are first described from the Doushantuo phosphorites in Weng'an, Guizhou Province. The former is usually preserved as globoids and their morphological character and inner structure are quite similar to those typical Tianzhushania spinosa (silicified) found in chert of the Sinian Doushantuo Formation in eastern Yangtze Gorges, Hubei Province. The distinct new species, preserved as globoids too, shows a dense inner wall with distinctly uniform tubers and stretching out one or more tube like processes. The phosphatized Tianzhushania found in Weng'an further confirms that the fossiliferous horizons in Guizhou and eastern Yangtze Gorge are coeval, which provides a new datum for studying those phosphatized spheroidal fossils.
    11  DISTRIBUTION PATTERNS OF NANNOFOSSIL GEPHYROCAPSA OCEANICA IN SURFICIAL SEDIMENTS OF JIAOZHOU BAY, SOUTHERN SHANDONG PENINSULA,CHINA
    ZHONG Shi Lan ) WANG Ya Ping ) GAO Shu ) CAO Qi Yuan ) ZHU You Hua ) ) Nanjing Institute of Geology Palaeontology Chinese Academy of Sciences Nanjing ) Institute of Oceanology Chinese Academy o
    2001(4):505-513. DOI: 1 CSTR:
    [Abstract](312) [HTML](0) [PDF 0.00 Byte](11)
    Abstract:
    Surficial sediment samples were collected from the Jiaozhou Bay and adjoining seawaters to study the spatial distribution patterns of calcareous nannofossils within the embayment. The result shows that Gephyrocapsa oceanica monopolized the nannofossil assemblage, whilst some subordinate taxa Braarudosphaera bigelowii, Syracosphaera histrica, S. lamina and Acantholithus sp. etc. scarcely occur in some samples. Three zones for the distribution of Gephyrocapsa oceanica are recognized, according to variations in its abundance value: They are the onshore common zone, shallow water rich zone and deep water accumulation zone, from the coastline to deep waters. Geomorphologically, these zones successively correspond to silty clay tidal flat, sub tidal erosional channels and submarine erosional highlands. The same nannofossil assemblage with an analogous distribution pattern is also observed on the adjacent continental shelf. It is well known that Emiliania huxleyi is one of the most common species in the ocean and Florisphaera profunda is a marker of deep water environments. However, these two species were not found in the study area, which may be explained by ecological controls related to water fertility and quality, and to water depth.
    12  TWO MISTAKES IN THE STUDY OF THE FORMATION AGE OF THE OPHIOLITE BELTS, CHINA
    WANG Yu Jing
    2001(4):529-532. DOI: 1 CSTR:
    [Abstract](392) [HTML](0) [PDF 0.00 Byte](5)
    Abstract:
    There are two mistakes in researching the formation age of the ophiolite belts, China. The first mistake took place before 1970's when many geologists determined the formation age of the Ophiolite belts mainly based on the macrofossils of the limestone block in the melanges. Because the age shown by these macrofossils is generally earlier than the formation age of the Ophiolite belts, it can not represent the true time of plate collisions. The second one took place after the 1970's when numerous geological workers determined the formation age of the Ophiolite belts commonly based on the radiolites and radiolarian faunas. But, in the Ophiolite belts sometimes there are two sets of radiolites. The first radiolite belongs to allochthonous removal with the characters of deep water and without any relation with the oceanic crust; the second radiolite represents relics of true oceanic crust overlying the pillow basalt. In all published geological references, most geologists did not describe the positions of the radiolites in the ophiolite belts, therefore, the conclusions drawn by them for the formation age of the ophiolite belts are always doubtful.
    13  AMINO ACID VERTICAL DISTRIBUTIONS IN QUATERNARY SEDIMENTS FROM CHANGBAISHAN BOG AND TAIHU LAKE,CHINA, AND THEIR PALEOECOLOGICAL IMPLICATIONS
    WANG Jin Quan
    2001(4):533-542. DOI: 1 CSTR:
    [Abstract](306) [HTML](0) [PDF 0.00 Byte](5)
    Abstract:
    近几十年来,随着稳定性碳同位素和^14C测年等新技术,新方法的应用,使第四纪研究迅速地由定性向定量发展,然而,氨基酸应用于第四纪古生态和古气候的研究在国内仍少有人知,在国际期刊上也不多见。近年来,作者开展了长白山孤山屯和太湖全新世沉积物的氨基酸和有机碳同位素分布与古生态,古气候意义的分析研究,结果表明,化石氨基酸同样可为第四纪的生态环境和古气候的研究提供信息,并为全球性对比提供证据。
    14  A NEW SPECIFIC EPITHET NILSONIA STOCKMANSII NOM. NOV. PROPOSED FOR NILSONIA UNDULATA SENSU STOCKMANS ET MATHIEU,1939
    LIU Lu Jun YAO Zhao Qi
    2001(4):543-545. DOI: 1 CSTR:
    [Abstract](293) [HTML](0) [PDF 0.00 Byte](5)
    Abstract:
    Nilssonia undulata Stockmans et Mathieu,1939是Nilssonia undulata Harris,1932的晚出异物同名,为此,作者为Nilssonia undulata sensu Stockmans et Mathieu建立了一个新名称。据《植物命名国际规范》,属名的原始拼缀Nilsonia应优先于后来拼缀Nilssonia,因之,新名称拼缀为Nilsonia stockmansii nom.nov.。

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