Ichnoassemblages and their sedimentary environments in limestoneof the Upper Carboniferous-Lower Permian Taiyuan Formation,southeastern Shanxi Province
Hu Bin1,2, Hu Lei1, Song Huibo1, Yang Lianchao1
1 Institute of Resource and Environment,Henan Polytechnic University,Jiaozuo 454003,Henan 2 Key Laboratory of Biogenic Traces & Sedimentary Minerals of Henan Province,Jiaozuo 454003,Henan
Abstract The abundant ichnofossils were found in the Upper Carboniferous-Lower Permian Taiyuan Formation of Lingchuan area,southeastern Shanxi Province,in which 10 ichnogenus and 14 ichnospecies were distinguished.Common ichnofossils include Zoophycos,Helminthopsis,Planolites,Nereites,Chondrites,Thalassinoides,Rhizocorallium,Ophiomorpha,Palaeophycus and Teichichnus,and the most common ichnofossil is Zoophycos.According to the composition,distribution and occurrence characteristics of ichnofossils,four ichnoassemblages were recognized:(1)Zoophycos-Thalassinoides ichnoassemblage;(2)Planolites-Helminthopsis ichnoassemblage;(3)Zoophycos-Teichichnus ichnoassemblage;(4)Nereites-Chondrites ichnoassemblage.By the analysis of sedimentary characteristics of the host rock of these ichnofossils,it is showed that these ichnoassemblages in the limestone of the Taiyuan Formation mainly distributed respectively in embayment-lagoon(ichnoassemblage 1),the upper shallow sea(ichnoassemblage 2),the middle shallow sea(ichnoassemblage 3)and the lower shallow sea(ichnoassemblage 4).Based on the synthesis analysis of the ichnoassemblages and sedimentary characteristics,this paper puts forward the sedimentary environmental model of ichnoassemblages in the Taiyuan Formation of Lingchuan area.The result will provide the biologic information and basic data for the study of coal and coalbed gas formation palaeoenvironment in the Taiyuan Formation of southeastern Shanxi Province in the future.
About author: Hu Bin,born in 1952,is a professor and Ph.D. supervisor of Henan polytechnic University,and is mainly engaged in teaching and researches of ichnology and sedimentology.E-mail: hub@hpu.edu.cn.
Cite this article:
Hu Bin,Hu Lei,Song Huibo et al. Ichnoassemblages and their sedimentary environments in limestoneof the Upper Carboniferous-Lower Permian Taiyuan Formation,southeastern Shanxi Province[J]. JOPC, 2013, 15(6): 809-818.
Hu Bin,Hu Lei,Song Huibo et al. Ichnoassemblages and their sedimentary environments in limestoneof the Upper Carboniferous-Lower Permian Taiyuan Formation,southeastern Shanxi Province[J]. JOPC, 2013, 15(6): 809-818.
常江林,高强.1993.山西石炭二叠纪古气候初探[J].地层学杂志,17(2):154-160. 陈世悦,刘焕杰.1995.含煤建造露头层序地层分析:以太原西山石炭二叠系剖面为例[J].煤田地质与勘探,23(2):13-17. 陈振宏,宋岩,秦胜飞.2007.沁水盆地南部煤层气藏的地球化学特征[J].天然气地球科学,18(4):561-564. 程保洲,王海生,张玉年.1990.山西省晚古生代含煤地层沉积环境及聚煤规律[J].山西地质,5(4):319-332. 范炳恒,何锡麟.1994.太原东山晚石炭世至早二叠世早期地层研究[J].煤田地质与勘探,22(2):1-5. 范炳恒,竺维彬,何锡麟.1999.山西阳泉地区早二叠世早期腕足动物群[J].古生物学报,38(3):353-364. 龚一鸣.2004.遗迹化石Chondrites的指相意义和阶层分布[J].古生物学报,43(1):123-130. 何锡麟,范炳恒.1990.太原东山本溪、太原组腕足动物组合层序[J].煤炭学报,15(3):41-47. 胡斌,王冠忠,齐永安.1997.痕迹学理论与应用[M].山东徐州:中国矿业大学出版社. 胡斌,周方,宋慧波. 2010.河南焦作地区下二叠统太原组遗迹化石及其沉积环境[J].古地理学报,12(5):577-588. 冀涛,杨德义.2007.沁水盆地煤与煤层气地质条件[J].中国煤田地质,19(5):28-30. 贾建称.2007.沁水盆地晚古生代含煤沉积体系及其控气作用[J].地球科学与环境学报,29(4):374-382. 晋慧娟,李育慈,方国庆.2003.古代深海底质氧控的遗迹化石群落[J].沉积学报,21(1):75-80. 孔宪祯,李润兰,常江林,等.1995.山西晚古生代含煤地层及其生物群[J].中国煤田地质,7(1):18-21. 李五忠,王一兵,崔思华,等.2003.沁水盆地南部煤层气田煤层气成藏条件分析[J].煤田地质与勘探,31(2):23-26. 李增学,余继峰,王明镇,等.2005.沁水盆地煤地质与煤层气聚集单元特征研究[J].山东科技大学学报(自然科学版),24(1):8-13. 刘金华,周修高.1990.山西太原西山晚石炭世太原组介形类研究[J].地球科学:中国地质大学学报,15(3):307-314. 陆小霞,黄文辉,唐修义,等.2012.沁水盆地南部15号煤层顶板灰岩特征对煤层气开采的影响[J].现代地质,26(3):518-526. 秦勇,姜波,王继尧,等.2008.沁水盆地煤层气构造动力条件耦合控藏效应[J].地质学报,82(10):1355-1362. 山西地质矿产局.1989.山西省区域地质志[M].北京:地质出版社,140-173. 邵龙义,肖正辉,何志平,等.2006.晋东南沁水盆地石炭二叠纪含煤岩系古地理及聚煤作用研究[J].古地理学报,8(1):43-52. 邵龙义,肖正辉,汪浩,等.2008.沁水盆地石炭—二叠纪含煤岩系高分辨率层序地层及聚煤模式[J].地质科学,43(4):777-791. 王约.2003.贵州独山泥盆系大河口组遗迹化石Teichichnus及其地质意义[J].贵州地质,20(3):145-149. 王志浩,文国忠.1987.晋东南地区晚石炭世牙形刺.见:晋东南地区晚古生代含煤地层和古生物群[M].江苏南京:南京大学出版社. 夏邦栋,钟立荣,方中.1993.皖南宣城王胡村组Rhizocorallium的发现及环境意义[J].石油与天然气地质,14(1):61-63. 徐振永,王延斌,陈德元,等.2007.沁水盆地晚古生代煤系层序地层及岩相古地理研究[J].煤田地质与勘探,35(4):5-11. 杨式溥.1990.古遗迹学[M].北京:地质出版社. 张志存.1985.山西中、晚石炭世古构造类型[J].中国地质科学院地质力学研究所所刊,(6):127-141. 张志存.1986.山西上石炭统含灰岩的分阶[J].科学通报,31(3):206-208. Hu B,Song H B,Liu S X, et al.2010.Sedimentary facies,ichnofossils and storm deposits in the Lower Permian Taiyuan Formation,Jiaozuo city,Henan Province,Central China[J].Acta Geologica Polonica,60(1):45-52. Ekdale A A,Mason T R.1988.Characteristic trace-fossil associations in oxygen-poor sedimentary environments[J].Geology,16: 720-723. Frey R W.1975.The Realm of Ichnolohy: Its Strengths and Limitations[M].In: Frey R W(ed).The Study of Trace Fossils.New York: Springer-Verlag,19-3-38. Frey R W,Pemberton S G.1984.Trace Fossils Facies Models[M].In: Walker R G(ed).Facies Models(2nd edition).Geol. Assoc. Canada Reprint Ser., 1. Frey R W,Seilacher A.1980.Uniformity in marine invertebrate ichnology[J].Lethaia,13:183-207. Savrda C E,Bottjer D J.1986.Trace-fossil model for reconstruction of paleo-oxygenation in bottom water[J].Geology,14:3-6. Wetzel A.1991.Ecologic interpretation of deep sea trace fossil communities[J].Palaeogeography,Palaeoecology,Palaeoclimatology,85:47-69.
