首页 | 本学科首页   官方微博 | 高级检索  
   检索      

山西兴县中奥陶统马家沟组五5亚段遗迹化石组合及其古环境意义
引用本文:刘梦瑶,史云鹤,董国栋,王彦卿,张鑫,苏中堂,张立军.山西兴县中奥陶统马家沟组五5亚段遗迹化石组合及其古环境意义[J].古生物学报,2019,58(4):487-501.
作者姓名:刘梦瑶  史云鹤  董国栋  王彦卿  张鑫  苏中堂  张立军
作者单位:河南理工大学资源环境学院,河南省生物遗迹与成矿过程重点实验室,中原经济区煤层(页岩)气河南省协同创新中心,焦作454003;中国石油天然气股份有限公司长庆油田分公司,西安710016;成都理工大学沉积地质研究院,成都6100591
基金项目:国家自然科学基金项目(41602112),中国石油天然气股份有限公司长庆油田分公司委托开发项目(20171205),河南省高等学校重点科研项目(17A170001),中国博士后科学基金(2016M592288)资助。
摘    要:鄂尔多斯盆地东缘关家崖剖面奥陶系马家沟组五5亚段地层中保存大量无脊椎动物遗迹化石,可识别出居住迹、牧食迹、觅食迹三大类,共7个遗迹属、14个遗迹种,分别是Arenicolites isp.,Cylindricumisp.,Helminthopsis abeli,Helminthopsis isp.1,Helminthopsis isp.2,Lorenziniaisp.,Planolites isp.,Planolites beverleyensis,Planolites montanus,Teichichnus rectus,Thalassinoides isp.1,Thalassinoides isp.2,Thalassinoides isp.3,Thalassinoides isp.4。根据遗迹化石特征及其沉积环境,可划分3个遗迹组合:1、Helminthopsis-Planolites组合,该组合以觅食迹为主,部分为居住迹,出现在潮间带和潮下带;2、Thalassinoides-Teichichnus组合,该组合遗迹化石种类较单一,主要为觅食迹,分布于潮间带和潮上带;3、Thalassinoides-Helminthopsis组合,该组合出现在潮间带。基于遗迹化石组合的分布特点,提出山西兴县奥陶系马家沟组五5亚段的沉积环境模式。

关 键 词:遗迹组合  古环境  马家沟组  奥陶系  鄂尔多斯盆地

CHARACTERISTICS OF PALEOENVIRONMENTAL EVOLUTION AND ICHNOCOENOSIS IN THE 55 SUBMEMBER OF THE MIDDLE ORDOVICIAN MAJIAGOU FORMATION, XINGXIAN, SHANXI
LIU Meng-yao ,SHI Yun-he ,DONG Guo-dong ,WANG Yan-qing ,ZHANG Xin ,SU Zhong-tang ,ZHANG Li-jun.CHARACTERISTICS OF PALEOENVIRONMENTAL EVOLUTION AND ICHNOCOENOSIS IN THE 55 SUBMEMBER OF THE MIDDLE ORDOVICIAN MAJIAGOU FORMATION, XINGXIAN, SHANXI[J].Acta Palaeontologica Sinica,2019,58(4):487-501.
Authors:LIU Meng-yao  SHI Yun-he  DONG Guo-dong  WANG Yan-qing  ZHANG Xin  SU Zhong-tang  ZHANG Li-jun
Abstract:A large number of invertebrate fossils are preserved in the stratum of the 55 Submember of Ordovician Majiagou Formation in the Guanjiaya section, eastern margin of Ordos Basin, identified types of domichnia, fodinichnia and grazing traces, 8 ichnogenera and 15 ichnospecies, Arenicolites isp., Cylindricum isp., Helminthopsis abeli, Helminthopsis isp. 1, Helminthopsis isp. 2, Lorenzinia isp. , Planolites isp., Planolites beverleyensis, Planolites montanus, Teichichnus rectus, Thalassinoides isp.1, Thalassinoides isp.2, Thalassinoides isp.3, Thalassinoides isp.4. Three trace fossil assemblages under different sedimentary environments have been recognized as follows: 1) Helminthopsis-Planolites trace fossil assemblages mainly consists of fodinichnia and domichnia from intertidal and subtidal zone; 2) Thalassinoides-Teichichnus trace fossil assemblages, its trace fossils are relatively simple mainly consists of fodinichnia from intertidal and supratidal zone; 3) Thalassinoides-Helminthopsis trace fossil assemblages from intertidal zone. Based on the distribution characteristics of the trace fossil assemblages, the sedimentary environment model of the submember 55 of Middle Ordovician Majiagou Formation in the eastern margin of Ordos Basin was proposed.
Keywords:
本文献已被 维普 万方数据 等数据库收录!
点击此处可从《古生物学报》浏览原始摘要信息
点击此处可从《古生物学报》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号