Advanced Search
Volume 32 Issue 2
. 
Turn off MathJax
Article Contents
Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2010  >  32(2): 171-174
Zhang Wentao, Tenger, Qin Jianzhong, Zhang Qingzhen, Xie Xiaomin, Bian Lizeng. RESEARCH OF A DOUBTFUL TUBE FOSSIL FROM THE LOWER CAMBRIAN SOURCE ROCKS IN SONGLIN, ZUNYI, GUIZHOU[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2010, 32(2): 171-174. doi: 10.11781/sysydz201002171
Citation: Zhang Wentao, Tenger, Qin Jianzhong, Zhang Qingzhen, Xie Xiaomin, Bian Lizeng. RESEARCH OF A DOUBTFUL TUBE FOSSIL FROM THE LOWER CAMBRIAN SOURCE ROCKS IN SONGLIN, ZUNYI, GUIZHOU[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2010, 32(2): 171-174. doi: 10.11781/sysydz201002171
shu

RESEARCH OF A DOUBTFUL TUBE FOSSIL FROM THE LOWER CAMBRIAN SOURCE ROCKS IN SONGLIN, ZUNYI, GUIZHOU

doi: 10.11781/sysydz201002171
  • 1.

    Wuxi Research Institute of Petroleum Geology, SINOPEC, Wuxi, Jiangsu 214151, China

  • 2. Nanjing University, Nanjing, Jiangsu 210093, China

  • Received Date: 2009-12-24
  • Rev Recd Date: 2010-02-05
  • Publish Date: 2010-04-28
    Abstract
  • A new type of silicic tube fossil is discovered from the lower part of Niutitang Formation(Lower Cambrian) in Songlin,Guizhou Province.The founded tube fossils are characterized by porous tube wall,and are only 470 nm in diameter.They are regarded as a new species,and might in some cases reflect characters of spongia.The development of source rocks is closely related to ancient biology activities.The doubtful tube fossils may indict many life activities in ancient water,which is helpful to explain why the silicalite has a high TOC.The silicalite is thought to deposit in deep-shelf environment influenced by hot water,which is beneficial for the formation of high quality source rocks.

     

    • FullText(HTML)
  • loading
    • References(14)
  • [1]
    梁狄刚,郭彤楼,陈建平,等.中国南方海相生烃成藏研究的若干新进展(一):南方四套区域性海相烃源岩的分布[J].海相油气地质,2008,13(2):1-16.
    [2]
    陈均远.动物世界的黎明[M].南京:江苏科学技术出版社,2004.
    [3]
    赵元龙,STEINER M,杨瑞东,等.贵州遵义下寒武统牛蹄塘组早期后生生物群的发现及重要意义[J].古生物学报,1999,38 (增刊):132-144.
    [4]
    STEINER M,WALLIS E,ERDTMANN B D,et al.Submarine-hydrothermal exhalative ore layers in black shales from South China and associated fossils-insights into a Lower Cambrian facies and bio-evolution[J].Palaeoecology,2001,169(3-4):165-191.
    [5]
    边立曾.海相烃源岩生烃母质生物构成特征[M]//中国石油化工集团公司油气勘探开发继续教育无锡基地.石油地质样品分析测试技术及应用.北京:石油工业出版社,2006:269-290.
    [6]
    YANG XINGLIAN,ZHAO YUANLONG,WANG YUE,et al.Discovery of sponge body fossils from the Late Meishucunian (Cambrian) at Jinsha,Guizhou,South China[J].Progress in Natural Sciences,2005,15 (8):708-712.
    [7]
    赵元龙,袁金良,朱茂炎,等.贵州寒武纪系列生物群及其研究意义[J].现代地质,1999,13 (2):245-246.
    [8]
    杨兴莲.贵州早寒武世早期地层及古生物学综合研究[D].南京:中国科学院南京地质古生物研究所,2005.
    [9]
    王平丽,赵元龙,杨兴莲,等.贵州下寒武统牛蹄塘生物群中的双孔钱包海绵Crumillospongia biporosa[J].微体古生物学报,2005,22(2):196-201.
    [10]
    赵元龙,杨荣军,杨兴莲,等.贵州松林下寒武统牛蹄塘生物群中的球状海绵化石[J].高校地质学报,2006,12(1):106-110.
    [11]
    杨兴莲,朱茂炎,赵元龙,等.贵州寒武纪海绵动物化石组合特征[J].微体古生物学报,2005,22(3):295-303.
    [12]
    杨兴莲,赵元龙.贵州遵义下寒武统牛蹄塘组生物群中的海绵化石[J].贵州工业大学学报(自然科学版),2000,29 (6):30-36.
    [13]
    WEAVER J C,AIZENBERG J,FANTNER G E,et al.Hierarchical assembly of the siliceous skeletal lattice of the hexactinellid sponge Euplectella aspergillum[J].Journal of structural biology,2007,158(1):93-106.
    [14]
    梁狄刚,郭彤楼,边立曾,等.中国南方海相生烃成藏研究的若干新进展(三):南方四套区域性海相烃源岩的沉积相及发育的控制因素[J].海相油气地质,2009,14(2):1-19.
    • Relative Articles
    • Supplements(0)
    • Cited By
  • 加载中

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索
    Citation
    XML
    PDF-CN

    Article Metrics

    Article views (1351) PDF downloads(1260) Cited by()
    Proportional views
    Related

    Website Copyright © Wuxi Research Institute of Petroleum Geology, SINOPEC 苏ICP备15009037号 苏公网安备32021102000780号

    Address：No. 2060, Lihu Avenue, Wuxi, Jiangsu   (214126) Tel：0510-68787204，68787203 Fax：0510-68787113 Email：sysydz.syky@sinopec.com

    Supported by: Beijing Renhe Information Technology Co. Ltd    

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return