四川广安谢家槽剖面早三叠世地层中的时错相沉积及其古生态意义——一个传统地层剖面的重新解读EARLY TRIASSIC ANACHRONISTIC SEDIMENTS AT THE XIEJIACAO SECTION OF GUANGAN,SICHUAN PROVINCE AND THEIR PALEOECOLOGICAL SIGNIFICANCES : A RESTUDY OF A CLASSICAL SECTION
周志澄,罗辉,祝幼华,蔡华伟,许波,陈金华,赵媛瑗
摘要(Abstract):
四川广安谢家槽剖面下三叠统夜郎组和嘉陵江组中含有扁平砾石灰岩、蠕虫状灰岩、叠层石、层纹状灰岩、薄层泥晶灰岩、条带状灰岩和水平分布的遗迹化石等类型丰富的时错相沉积,由下至上时错相沉积呈现出逐渐减弱的总趋势。早三叠世晚期,时错相沉积从正常海洋环境沉积中退出,只是出现在高压力环境的沉积物中。时错相沉积的这种时空分布和发育程度的变化,反映二叠纪末生物大灭绝事件后,早三叠世海洋生态系复苏的历程。
关键词(KeyWords): 时错相沉积;早三叠世;生物复苏;夜郎组;嘉陵江组;四川广安谢家槽
基金项目(Foundation): 中国科学院资源环境领域知识创新工程重要方向性项目(KZCX2-YW-154);; 国家自然科学基金(No.40772004,41072008);; 中国科学院“外国专家特聘研究员”计划项目(No.2009Z2-7)~~
作者(Author): 周志澄,罗辉,祝幼华,蔡华伟,许波,陈金华,赵媛瑗
DOI: 10.19839/j.cnki.dcxzz.2013.01.012
参考文献(References):
- ①杨昊.2010.四川、贵州三叠纪有孔虫的生物地层学研究[硕士学位论文].北京:中国科学院研究生院.43-45
- 方宗杰.2004.从华南二叠—三叠纪礁生态系的演变探讨与灭绝—残存—复苏相关的几个问题.见:戎嘉余,方宗杰主编.生物大灭绝与复苏——来自华南古生代和三叠纪的证据。合肥:中国科技大学出版社.476-521
- 郭成贤,夏克东,段太忠.1988.湖北大冶沙田下三叠统大冶群岩石学特征及沉积环境.见:冯增昭,王英华,李尚武主编.下扬子地区下三叠统青龙群岩相古地理研究.昆明:云南科技出版社.175-185
- 姜月华,岳文浙,业治铮等.1992.蠕虫状灰岩特征和成因新探.矿物岩石,12(1):1-7
- 李子舜,詹立培,戴进业,金若谷,朱秀芳,张景华,黄恒铨,徐道一,严正,李华梅等.1989.川北陕南二叠-三叠纪生物地层学研究.北京:地质出版社.1-435
- 刘怀波,罗顺社.1988.湖北蒲圻三叠系大冶群沉积环境.见:冯增昭,王英华,李尚武主编.下扬子地区下三叠统青龙群岩相古地理研究.昆明:云南科技出版社.186-197
- 刘建波,江崎洋一,杨守仁,王海峰,足立奈津子.2007.贵州罗甸二叠纪末生物大灭绝事件后沉积的微生物岩的时代和沉积学特征.古地理学报,9(5):473-486
- 钱迈平.1995.中下扬子区海相三叠纪叠层石及其环境演变.古生物学报,31(6):731-741
- 四川省区域地层表编写组.1978.西南地区区域地层表,四川分册,北京:地质出版社.28-72
- 四川地质矿产局.1982.四川省区域地质志.北京:地质出版社.23:206-237,567-585
- 王生海,范嘉松,Rigby J K.1996.贵州紫云二叠纪生物礁的基本特征及发育规律.沉积学报,14:66-74
- 王一刚,文应初,洪海涛,夏茂龙,范毅,文龙,孔令霞,武川红.2009.四川北部晚二叠世—早三叠世碳酸盐斜坡相带沉积特征.古地理学报.11(2):143-156
- 吴歧.1998.福建晚二叠世长兴期—早三叠世溪口期古生态群落及古环境分析.见:中国地质科学新探索.北京:石油工业出版社.65-77
- 吴应林,朱洪发,朱忠发,颜仰基,秦建华,牟传龙,王尊周,罗崇迅,田传荣,谭钦银,杜泽英.1994.中国南方三叠纪岩相古地理与成矿作用.北京:地质出版社.1-143
- 杨遵仪,殷鸿福,吴顺宝,杨逢清,丁梅华,徐桂荣.1987.华南二叠-三叠系界线地层及动物群.北京:地质出版社.1-379
- 赵小明,牛志军,童金南,姚华舟.2010.早三叠世生物复苏期的特殊沉积——“错时相”沉积.沉积学报,28(2):314-323
- 周志澄,罗辉,祝幼华,许波,蔡华伟,陈金华.2012.四川广安谢家槽下三叠统碳酸盐微相及沉积环境.古生物学报,51(1):114-126
- Camoin G F&Montaggioni L F.1994.High energy coralgal-strom-atolite frameworks from Holocene reefs(Tahiti,French Polyne-sia).Sedimentology,41:655-676
- Ezaki Y,Liu Jain-bo&Adachi N.2003.Earliest Triassic microbi-alite micro-to megastructures in the Huaying Area of SichuanProvince,South China:implications for the nature of oceanicconditions after the end-Permian Extinction.Palaios,18(4):388-402
- Kershaw S,Zhang Ting-shan&Lan Guang-zhi.1999.A?microbi-alite crust at the Permian-Triassic boundary in South China,andits Palaeoenvironmental significance.Palaeogeography,Palaeo-climatology,Palaeoecology,146:1-18
- Kershaw S,Guo Li,Swift A&Fan Jia-song.2002.?Microbialitesin the Permian-Triassic boundary interval in Central China:structure,age and distribution.Facies,47:83-90
- Lehrman D J.1999.Early Triassic calcimicrobial mounds and bio-stromes of the Nanpanjiang Basin.South China.Geology,27(4):359-362
- Lehrman D J,Wei Jia-yong&Enos P.1998.Controls on faciesarchtecture of a large Triassic carbonate platform:the GreatBank of Guizhou,Nanpanjiang Basin.South China.Journal ofSedimentary Research,68:311-326
- Lehrman D J,Wan Yang,Wei Jia-yong,Yu You-yi&Xiao Jia-fei.2001.Lower Triassic peritidal cyclic limestones:an example ofanachronistic carbonate facies from the Great Bank of Guizhou.Nanpanjiang Basin.Guizhou Province.South China.Palaeo-geography,Palaeoclimatology,Palaeoecology,173:103-123
- Lehrman D J,Payne J L,Felix S V,Dillett P M,Wang Hong-mei,Yu You-yi&Wei Jia-yong.2003.Permian-Triassic boundarysections from shallow-marine carbonate platforms of the Nan-panjiang Basin,South China:implications for oceanic conditionsassociated with the end-Permian extinction and its aftermath.Palaios,18(2):138-152
- Pruss S B,Corsetti F A&Bottjer D J.2005.The unusual sedimen-tary rock record of the Early Triassic a case study from thesouthwestern United States.Palaeogeography,Palaeoclimatol-ogy,Palaeoecology,222:33-52
- Reid R P,Visscher P T,Decho A W,Stolz J F,Bebout B M,Du-plaz C,Macintyre I G,Paerl H W,Pinckney J I,Prufert B L,Stepper T F&DesMarais D J.2000.The role of microbes inaccretion,lamination and early lithification of modern marinestromatolites.Natrure,406:989-992
- Sepkoski J J Jr.1982.Flat-pebble conglomerates,storm deposits,and the Cambrian bottom fauna.In:Einsele G&Seilacher Aeds.Cyclic and event stratification.Berlin:Springer-Verlag.371-385
- Sepkoski J J Jr,Bambach R K&Drose M L.1991.Secular changesin Phanerozoic event bedding and the biological overprint.In:Einsele G,Ricken W&Seilacher A eds.Cycles and Events inStratigraphy.Heideberg:Springer-Verlag.298-312
- Stanley S M&Yang X.1994.A double mass extinction at the endof the Paleozoic Era.Science,266(5189):1340-1344
- Wignal P B,Hallam A,Lai Xu-long&Yang Feng-qing.1995.Palaeoenvironmemtal across the Permian-Triassic boundary atShangsi(N.Sichuan,China).Historical Biology,10:175-189
- Wignall P B&Twitchett R J.1999,Unusual intraclastic limestonein Lower Triassic carbonates and their bearing on the aftermathof the end-Permian mass extinction.Sedimentology,46:303-316