Microfacies characteristics of the Lower Triassic containing Chaohusaurus fauna in Chaohu area, Anhui Province and its palaeoenvironment
Zhang Yuying1,2, Jiang Dayong1, Fu Wanlu1, Ji Cheng3, Sun Zuoyu1
1 School of Earth and Space Sciences,Peking University,Beijing.100871 2 Liaoning Institute of Geology and Mineral Resources,Shenyang.110031,Liaoning 3 Nanjing Institute of Geology and Palaeontology,CAS, Nanjing.210008,Jiangsu
Abstract The Early Triassic Chaohusaurus fauna was found at No.598-630 layers at the top of the Middle Member-the bottom of the Upper Member of the Nanlinghu Formation in Majiashan section of Chaohu area,Anhui Province. Based on the microfacies characteristics and the carbon and oxygen isotope analysis,the sedimentary environment of the fossil beds where the Chaohusaurus fauna had occurred was studied. 4microfacies types were recognized from the studied layers,which contained the red-grey thick nodular limestone with spicules-bivalves,the gray bioclastic-argillaceous micrite limestone,the gray laminated argillaceous micrite limestone,and the light gray micrite limestone,respectively. It was indicated that the sedimentary environment of the fossil beds was from the foot of the outer ramp-abyssal basin to the outer ramp. The values of the δ13C and δ18O are generally low in the whole of fossil beds. Combined with the above characteristics,it might be inferred that the Chaohusaurus fauna was living in the outer ramp zone with low-energy,less numbers and types of the biocoenose,and high seawater temperature.
Corresponding Authors:
Jiang Dayong,born in 1969,is a professor at School of Earth and Space Sciences,Peking University. Now he is engaged in vertebrate palaeontology and integrated stratigraphy. E-mail: djiang@pku.edu.cn.
About author: Zhang Yuying,born in 1987,is a master at School of Earth and Space Sciences,Peking University. Now she is engaged in carbonate microfacies. E-mail: yycug@163.com.
Cite this article:
Zhang Yuying,Jiang Dayong,Fu Wanlu et al. Microfacies characteristics of the Lower Triassic containing Chaohusaurus fauna in Chaohu area, Anhui Province and its palaeoenvironment[J]. JOPC, 2014, 16(5): 761-768.
Zhang Yuying,Jiang Dayong,Fu Wanlu et al. Microfacies characteristics of the Lower Triassic containing Chaohusaurus fauna in Chaohu area, Anhui Province and its palaeoenvironment[J]. JOPC, 2014, 16(5): 761-768.
曹长群,王伟,金玉玕. 2002. 浙江煤山二叠—三叠系界线附近碳同位素变化[J]. 科学通报,47(4):302-306. 陈烈祖. 1985. 安徽巢县早三叠世鱼龙化石[J]. 中国区域地质,15:139-146. 董兆雄,朱晓惠. 2002. 一种特殊瘤状灰岩的成因研究[J]. 沉积学报,20(1):20-24. 方邺森,任磊夫. 1987. 沉积岩石学教程[M]. 北京:地质出版社,219-220. 郭福生. 1989. 下扬子地区三叠系下统瘤状灰岩成因研究[J]. 东华理工学院学报(自然科学版),12(4):17-22. 李双应. 2005. 安徽巢湖地区下三叠统研究进展及其科学意义[A]. 见:“地质古生物遗迹保护,现代生物、人与自然和谐”学术研讨会论文(摘要)汇编[C]. 罗锐,张利伟. 2013. 巢湖地区楚歌岭剖面下三叠统和龙山组碳同位素变化特征及其意义[J]. 中国煤炭地质,25(1):8-11. 浦万财,李平,苏驰. 2012. 安徽巢北南陵湖组灰岩特征分析及其成因[J]. 中国科技博览,2012(16):90-90. 邵龙义,窦建伟,张鹏飞. 1996. 西南地区晚二叠世氧碳稳定同位素的古地理意义[J]. 地球化学,25(6):575-581. 童金南. 1997. 安徽巢县下三叠统层序地层研究[J]. 地球学报,18(2):215-219. 童金南,殷鸿福. 2005. 国际三叠纪年代地层研究进展[J]. 地层学杂志,29(2):130-136. 童金南,殷鸿福. 2009. 早三叠世生物与环境研究进展[J]. 古生物学报,48(3):497-508. 童金南,Hansen H J,赵来时,等. 2005b. 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[J]. 地层学杂志,29(2):205-214. 童金南,赵来时,左景勋. 2005a. 下三叠统殷坑阶和巢湖阶及其界线研究[J]. 地层学杂志,29(增):548-564. 王伟,沈树忠,朱自力. 1997. 中国西藏色龙二叠—三叠系界线剖面的碳同位素特征及其意义[J]. 科学通报,42(4):406-408. 余素玉. 1989. 化石碳酸盐岩微相[M]. 北京:地质出版社,1-167. 张秀莲. 1985. 碳酸盐岩中氧、碳稳定同位素与古盐度、古水温的关系[J]. 沉积学报,3(4):17-30. 朱洪发,王恕一. 1992. 苏南—皖南三叠纪瘤状灰岩,蠕虫状灰岩的成因[J]. 石油实验地质,14(4):454-460. 左景勋,童金南,邱海鸥,等. 1995. 巢湖平顶山北坡剖面早三叠世碳,氧同位素地层学研究[J]. Journal of Stratigraphy,28(1):35-40. 左景勋,童金南,邱海鸥,等. 2003. 巢湖地区早三叠世碳氧同位素地层对比及其古生态环境意义[J]. 地质地球化学,31(3):26-33. 左景勋,童金南,邱海鸥,等. 2006. 下扬子地区早三叠世碳酸盐岩碳同位素组成的演化特征[J]. 中国科学(D辑):地球科学,36:109. 左景勋,童金南,赵来时,等. 2013. 早三叠世下扬子古海洋地球化学环境的修复过程[J]. 地球科学:中国地质大学学报,38(3):441-453. Burchette T P,Wright V P. 1992. Carbonate ramp depositional systems[J]. Sedimentary Geology,79(1):3-57. Dunham R J. 1962. Classification of carbonate rocks according to deposition texture[J]. AAPG Bulletin,1:108-121. Flügel E. 2004. Microfacies of Carbonate Rocks Analysis,Interpretation and Application[M]. New York:Springer. Folk R L. 1959. Practical petrographic classification of limestones[J]. AAPG Bulletin,43(1):1-38. Jiang D Y, et al. 2009. Correspondence of paleoenvironmental-paleoecological changes with biodiversity sequence of the Middle Triassic Panxian Marine Reptile fauna,Guizhou Province,China[J]. Journal of Vertebrate Paleontology,29(3-Supplement.):123A. Kump L. 1991. Interpreting carbon-isotope excursions:Strangelove oceans[J]. Geology,19(4):299-302. Li S Y,Tong J N,Liu K Y, et al. 2007. The Lower Triassic cyclic deposition in Chaohu,Anhui Province,China[J]. Palaeogeography,Palaeoclimatology,Palaeoecology,252:188-199. Motani Y,You H L. 1998. Taxonomy and limb ontogeny of Chaohusaurus geishanensis(Ichthyosauria),with a note on the allometric equation[J]. Journal of Vertebrate Paleontology,18(3):533-540. Payne J L,Lehrmann D J,Wei J Y, et al. 2004. Large perturbations of the carbon cycle during recovery from the end-Permian extinction[J]. Science,305:506-509. Sun Y D,Michael M J,Paul B W, et al. 2012. Lethally hot temperatures during the Early Triassic greenhouse[J]. Science,338:366-370. Tong J,Yin H. 2002. The Lower Triassic of South China[J]. Journal of Asian Earth Sciences,20(7):803-815. Tong J,Zhao L. 2011. Lower Triassic and Induan-Olenekian Boundary in Chaohu,Anhui Province,South China[J]. Acta Geologica Sinica:English Edition,85(2):399-407. Tong J N,Zakharov Y D. 2004. Lower Triassic ammonoid zonation in Chaohu,Anhui Province,China[J]. Albertiana,31:65-69. Tong J N,Zakharov Y D,Wu S B. 2004. Early Triassic ammonoid succession in Chaohu,Anhui Province[J]. Acta Palaeontologica Sinica,43:192-204. Tong J N,Zhou X G,Erwin D H, et al. 2006. Fossil fishes from the Lower Triassic of Majishan,Chaohu,Anhui Province,China[J]. Journal of Paleontology,80(1):146-161. Young C C,Dong Z M. 1972. Chaohusaurus geishanensis from Anhui Province[J]. Academia Sinica,Institute of Vertebrate Paleontology and Palaeoanthropology,Memoir,9:11-14