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

山东济阳坳陷古近系沙河街组深水湖沉积中的遗迹化石
引用本文:胡斌,姜在兴,齐永安,张国成.山东济阳坳陷古近系沙河街组深水湖沉积中的遗迹化石[J].古生物学报,2006,45(1):83-94.
作者姓名:胡斌  姜在兴  齐永安  张国成
作者单位:1. 河南理工大学,河南,焦作,454003
2. 中国地质大学,北京,100083
基金项目:国家自然科学基金(No.40372013),国家十五攻关项目(2001BA605A09),河南省自然科学基金(0311053000)资助课题
摘    要:山东济阳坳陷古近系沙河街组深水湖沉积地层主要由深灰色、褐灰色泥岩、油泥岩、泥灰岩和石灰岩以及岩盐组成,浊流沉积发育。已发现深水型遗迹化石有12个遗迹属14个遗迹种,包括3个新遗迹属6个新遗迹种。根据这些遗迹化石的组成与分布特征及其围岩的沉积特征,可以划分出2种不同沉积环境下的遗迹化石群落,即(1)Mermoides-Neonereites遗迹群落,主要由觅食迹(Fodinichnia)和牧食迹(Pascichnia)组成,常见分子有Mermoides chezhenensis,Mermoides latiusculus,Neonereites uniserialis,Hel minthoidichnitescf.tenuis,Hel-minthopsis abeli,Pilichnus lacustris,Multilagueichnus lingpanensis,Cochlichnus anguineus,Gordiaichnosp.,Palaeophycus tubularis和Planolites beverleyensis等,它们被解释形成于半深水湖或较深水湖沉积环境;(2)Semi-rotundichnus遗迹群落,以半圆形、小碟形牧食迹为其特征,典型组成分子有Semirotundichnus dongyingensis,Pa-tellarisichnus boxingensis和Neonereites uniserialis等,它们均产生于深水湖沉积环境。

关 键 词:遗迹化石  遗迹群落  深湖沉积  古近系  济阳坳陷  山东
收稿时间:2005-07-01
修稿时间:2005年7月1日

TRACE FOSSILS OF DEEPER LACUSTRINE DEPOSITS IN THE PALEOGENE SHAHEJIE FORMATION OF JIYANG DEPRESSION,SHANDONG PROVINCE, EASTERN CHINA
HU Bin,JIANG Zai-Xing,QI Yong-An,ZHANG Guo-Cheng.TRACE FOSSILS OF DEEPER LACUSTRINE DEPOSITS IN THE PALEOGENE SHAHEJIE FORMATION OF JIYANG DEPRESSION,SHANDONG PROVINCE, EASTERN CHINA[J].Acta Palaeontologica Sinica,2006,45(1):83-94.
Authors:HU Bin  JIANG Zai-Xing  QI Yong-An  ZHANG Guo-Cheng
Institution:1 Henan Polytechnic University, Jiaozuo 454003, Henan; 2 China University of Geosciences, Beijing 100083
Abstract:The Paleogene Shahejie Formation of Jiyang Depression , Shandong Province,Eastern China, contains dark and brown grey mudstone, oil-bearing mudstone, marl, limestone and rock salt, in which 12 ichnogenus(including 3 new ichnogenus) and 14 ichnospecies(including 6 new ichnospecies) were discovered in the deeper water lacustrine deposits. According to the composition and distribution characteristics of these trace fossils and their country rock features, two types of ichnocoenosis under different sedimentary environments have been recognized as follows: 1)Mermoides-Neonereites ichnocoenosis,which mainly consists of Fodinichnia and Pascichnia including such common trace fossils as Mermoides chezhenensis ,Mermoides latiusculus ,Neonereites uniserialis,Helminthoidichnites cf.tenuis,Helminthopsis abeli,Multilagueichnus lingpanensis,Pilichnus lacustris,Cochlichnus anguineus,Gordia ichnosp. and Planolites beverleyensis,generates in mid-deep lacustrine sedimentary environment;and(2)Semirotundichnus ichnocoenosis,which is characterized by the semi-round and small dishing Pascichnia containing such representative trace fossils as Semirotundichnus dongyingensis, Patellarisichnus boxingensis and Neonereites uniserialis,forms in deep lacustrine sedimentary environment.
Keywords:Trace fossils  Ichnocoenosis  Deep lacustrine deposits  Paleogene  Jiyang Depression  Shandong  
本文献已被 CNKI 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