安徽巢湖北部地区下三叠统和龙山组微生物岩及其意义
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摘要
巢湖北部地区下三叠统和龙山组(Smithian亚阶中上段)含有特征明显的微生物岩。微生物岩包含微生物席和叠层石两种类型,其中最为丰富的类型是以蓝藻为主。该组微生物岩的普遍发育以及宏体化石组合的分布特征表明,和龙山组微生物岩可能是早三叠世生态环境开始改善、生物开始复苏的标志。微生物岩及微生物群落特征表明,该组很可能沉积于低能浅水环境中。
Microbialites,such as microbial mats and stromatolites,have been found in the Lower Triassic Helongshan Formation(middle-upper Smithian)recently in Chaohu area,Anhui Province,east China.Microbial mats mainly consist of cyanobacteria and simpler green algae. Stromatolites,predominating with cyanobacteria,contain a lot of microorganism types. Microbialites,sedimentary features and special minerals suggest that the Helongshan Formation was deposited in quiet shollow environments,the characteristics of biologic evolution during the early Triassic in Chaohu area and other areas of south China indicate that the development of microbialites in Helongshan Formation might be a signature of the better beginning of environments and biological recovery in the Early Triassic.
Microbialites,such as microbial mats and stromatolites,have been found in the Lower Triassic Helongshan Formation(middle-upper Smithian)recently in Chaohu area,Anhui Province,east China.Microbial mats mainly consist of cyanobacteria and simpler green algae. Stromatolites,predominating with cyanobacteria,contain a lot of microorganism types. Microbialites,sedimentary features and special minerals suggest that the Helongshan Formation was deposited in quiet shollow environments,the characteristics of biologic evolution during the early Triassic in Chaohu area and other areas of south China indicate that the development of microbialites in Helongshan Formation might be a signature of the better beginning of environments and biological recovery in the Early Triassic.
引文
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童金南,赵来时,左景勋.2005b.下三叠统殷坑阶和巢湖阶及其界线研究.地层学杂志,29(增刊):548-564. Tong Jinnan,Zhao Laishi and Zuo Jingxun.2005b.Study on the Lower Triassic Yinkengian and Chaohuan stages and their boundary.Journal of Stratigraphy,29 ( suppl.) :548-564.
童金南,Hansen H J,赵来时,左景勋.2005c.印度阶-奥伦尼克阶界线层型候选剖面--安徽巢湖平顶山西剖面地层序列.地层学杂志,29(2) :205-214. Tong Jinnan,Hansen H J,Zhao Laishi and Zuo Jingxun.2005c.A GSSP candidate of the Induan-Olenekian boundary:Stratigraphic sequence of the west Pingdingshan section in Chaohu,Anhui Province.Journal of Stratigraphy,29 (2) :205-214.
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王永标,童金南,王家生,周修高.2005. 华南二叠纪末大绝灭后的钙质微生物岩及古环境意义.科学通报,50(6) :552-558. Wang Yongbiao,Tong Jinnan,Wang Jiasheng and Zhou Xiugao.2005. Calcimicrobialite after end-Permian mass extinction in South China and its palaeoenvironmental significance.Chinese Science Bulletin ,50 (7) :665-671.
吴亚生,姜红霞,Yang Wan,范嘉松.2007. 二叠纪-三叠纪之交缺氧环境的微生物和微生物岩.中国科学(D辑),37(5) :618-628. Wu Yasheng,Jiang Hongxia,Yang Wan and Fan Jiasong.2007. Mierobialite of anoxic condition from Permian-Triassic transition in Guizhou,China.Science in China( Series D) ,50 (7) :1040-1051.
杨浩,张素新,江海水,王永标.2006. 湖北崇阳二叠纪-三叠纪之交钙质微生物岩的时代及基本特征.地球科学,31(2) :165-170. Yang Hao,Zhang Suxin,Jiang Haishui and Wang Yongbiao.2006. Age and general characteristics of calcimicrobialite near the Permian-Triassic boundary in Chongyang,Hubei Province.Earth Science,31(2) :165-170.
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