China Geological Survey Chinese Academy of Geological SciencesHost
科学出版社Publish
Advanced Search
Previous Article Next Article
2018 Vol. 45, No. 5
Article Contents
Article navigation > Geology in China > 2018 > 45(5): 1039-1048
Next Article Previous Article

HU Zhidan, XIE Tao, YIN Fuguang. 2018. Carbon and oxygen isotopic studies of the horizon of Kueichousaurus Fauna[J]. Geology in China, 45(5): 1039-1048. doi: 10.12029/gc20180511
Citation: HU Zhidan, XIE Tao, YIN Fuguang. 2018. Carbon and oxygen isotopic studies of the horizon of Kueichousaurus Fauna[J]. Geology in China, 45(5): 1039-1048. doi: 10.12029/gc20180511
shu

Carbon and oxygen isotopic studies of the horizon of Kueichousaurus Fauna

  • 1.

    College of Earth Sciences, Chengdu University of Technology, Chengdu 610059, Sichuan, China

  • 2.

    Chengdu Center of China Geological Survey, Chengdu 610081, Sichuan, China

    • Fund Project: Supported by China Geological Survey Project (No. 12120114068101, 12120114030601, DD20160020), National Natural Science Foundation of China (No. 41502013)
More Information
  • Author Bio: HU Zhidan, male, born in 1992, master candidate, engages in regional geological research; E-mail:605166787@qq.com
  • Corresponding author: XIE Tao, male, born in 1982, senior engineer, engages in the investigation of regional geology and mineral resources; E-mail:xt1982cd@163.com 
Received Date:  30 August 2016
Revised Date:  04 May 2018
Publish Date:  25 October 2018
    Abstract

  • Kueichousaurus fauna is the typical representative of the biological radiation in the latest Triassic marine ecosystem, In order to study the palaeoenvironment of the Kueichousaurus fauna, the authors measured the fine sections in Dingxiao and its adjacent areas of Xingyi, Guizhou Province, and tested the whole rock carbon and oxygen isotope compositions by using the carbonate rock. According to the analytical results, the δ13C values in Nimaigu section range from -6.3 ‰ to 2.6 ‰, and δ18O values are between -5.7‰ and -1.2‰; the δ13C values in Xiemi section range from-4.5‰ to 2.5‰, and δ18O values are in the range of -5.7‰——1.2‰; the δ13C values of Bawei section range from 0.5 ‰ to 2 ‰, and δ18O values are between -6.4‰ and 0.1‰; the δ13C values in Dingxiao section range from-4.3‰-2.1‰, and δ18O values are between-7.3‰ and 2.5‰. According to the correlation analysis of carbon and oxygen isotope data, the isotopic values of Nimaigu, Xiemi and Dingxiao sections were less affected by diagenesis. There are obvious negative δ13C anomalies in the lower part of the horizon of Kueichousaurus fauna in Nimaigu, Xiemi and Dingxiao, closely related to the rapid death of marine organisms in low-water-level periods and the volcanism. Due to the influence of late diagenesis on the Dingxiao section, the seawater paleotemperature in Xingyi area was recovered by using δ18O data of Nimaigu, Xiemi and Dingxiao sections. It is shown that the temperature was between 19 and 27℃, with an average about 23℃, which indicates a warm climate during that period.

    • FullText(HTML)
  • 加载中
    • References
  • Chen Xiaohong, Wei Kai, Zhang Baomin, Cheng Long. 2013. Carbon isotope chemo-stratigraphy and ocean oxidation event in the Lower Triassic Yongningzhen Formation of Guanling, Guizhou Province[J]. Geology in China, 40(5):1466-1473(in Chinese with English abstract).

    Google Scholar

    Craig H. 1965. The measurement of oxygen isotope palaeotemperatures[C]//Tongiorgi E(ed.). Stable isotopes in oceanographic studies and palaeotemperatures. Pisa: Consiglio Nazionale delle Ricerche Laboratorio di Geologia Nucleare, 161-182.

    Google Scholar

    Dong Zhizhong, Wang Wei. 2006. The Cambrian-Triassic Conodont Faunas in Yunnan, China——Correlative Biostratigraphy and the Study of Palaeobiogeographic Province of Conodont[M]. Kunming:Yunnan Science and Technology Press, 1-347(in Chinese).

    Google Scholar

    Feng Zengzhao, Bao Zhidong, Li Shangwu. 1994. Lithofacies Paleogeography of Early and Middle Triassic of Yunnan-Guizhou-Guanxi Region[M]. Dongying:University of Petroleum Press, 1-180(in Chinese).

    Google Scholar

    Himmler T, Birgel D, Bayon G, Pape T, Ge L, Bohrmann G, Peckmann G. 2015. Formation of seep carbonates along the Makran convergent margin, northern Arabian Sea and a molecular and isotopic approach to constrain the carbon isotopic composition of parent methane[J]. Chemical Geology, 415(4):102-117.

    Google Scholar

    Horacek M, Brandner R, Abart R. 2007. Carbon isotope record of the P/T boundary and the Lower Triassic in the Southern Alps:Evidence for rapid changes in storage of organic carbon[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 252(1):347-354.

    Google Scholar

    Jia Peng, Li Wei, LuYuanzheng, Fan Ru, Li Xin, Feng Yuan, ChenYuhang, Li Ming, Zeng Yiyang, Liu Xin. 2017. The carbon and oxygen isotopic compositions and their evolution of the Xixiangchi Group carbonate rocks in Sichuan Basin and their geological implications[J]. Journal of Radioanalytical & Nuclear Chemistry, 311:755-768.

    Google Scholar

    Kaufman A J, Knoll A H, 1995. Neoproterozoic variations in the Cisotopic composition of seawater:Stratigraphic and biogeochemical implications[J]. Precambrian Research, 73(1-4):27-49. doi: 10.1016/0301-9268(94)00070-8

    CrossRef Google Scholar

    Kong Rui, Gao Xiaowei. 2006. Statistics[M]. Beijing:China Land Press, 1-273.

    Google Scholar

    Korte C, Kozur H W, Veizer J. 2005. δ13C and δ18O values of Triassic brachiopods and carbonate rocks as proxies for coeval seawater and palaeotemperature[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 226(3):287-306.

    Google Scholar

    Li Jinling, RIieppel Olivier. 2004. A new nothosaur form Middle Triassic of Guizhou, China[J]. Vertebrata Palasiatica, 42(1):1-5(in Chinese with English abstract).

    Google Scholar

    Li Rongxi, Wei Jiayong, Xiao Jiafei, Wang Xingli, Lehrmann D J. 2007. Response of carbon and oxygen isotopic geochemistry to transgressive systems tract:an example from Triassic Stratigraphy in Southwestern Guizhou Province[J]. Journal of Earth Sciences and Environment, 29(1):1-5(in Chinese with English abstract).

    Google Scholar

    Li Zhiguang, Sun Zuoyu, Jiang Dayong, Ji Cheng. 2016. LA-ICPMS Zircon U-Pb age of the fossil layer of Triassic Xingyi Fauna from Xingyi, Guizhou, and its significance[J]. Geological Review, 62(3):779-790(in Chinese with English abstract).

    Google Scholar

    Luo Beiwei, Wei Guoqi, Yang Wei, Dong Caiyuan. 2013. Reconstruction of the late Sinian paleo-ocean environment in Sichuan basin and its geological significance[J]. Geology in China, 40(4):1099-1111(in Chinese with English abstract).

    Google Scholar

    Luo Shunshe, Wang Kaiming. 2010. Carbon and oxygen isotope composition of carbonatic rock from the Mesoproterozoic Gaoyuzhuang Formation in the Kuancheng area, Hebei Province[J]. Aata Geologica Sinica, 84(4):492-499.

    Google Scholar

    Ma Letian, Ji Cheng, Sun Zuoyu, Yang Pengfei, Zou Xiaodong. 2013. Biodiversity and stratigraphic distribution of the Triassic Xingyi marine reptile fauna, Guizhou Province[J]. Journal of Stratigraphy, 37(2):178-185 (in Chinese with English abstract).

    Google Scholar

    Marshall J D. 1992. Climatic and oceanographic isotopic signals from carbonate rock record and their preservation[J]. Geological Magazine, 129:143-160. doi: 10.1017/S0016756800008244

    CrossRef Google Scholar

    Mei Mingxiang, Ma Yongsheng, Deng Jun, Meng Qingfen, Yi Dinghong, Li Donghai. 2003. Sequence-stratigraphic frame work of the Early to Middle Triassic and evolution of Sedimentaryfacies and paleogeography in the Nanpanjiang Basin and its adjacent areas:discussion on evolutionary process from the Dianqiangui Basin to the Nanpanjiang[J]. Geological Journal of China Universities, 9(3):427-439 (in Chinese with English abstract).

    Google Scholar

    Meyer K M, Yu M, Lehrmann D, Schootbrugge B, Payne J L. 2013. Constraintson on Early Triassic carbon cycle dynamics from paired organic and inorganic carbon isotope records[J]. Earth and Planetary Science Letters, 361(1):429-435.

    Google Scholar

    Moustafa M S H, Pope M C, Grossman E L, Mriheel I Y. 2016. Carbon and oxygen isotope variations of the Middlee Late Triassic Al Aziziyah Formation, northwest Libya[J]. Journal of African Earth Sciences, 118:149-162. doi: 10.1016/j.jafrearsci.2016.02.011

    CrossRef Google Scholar

    Muttoni G, Mazza M, Mosher D, Katz M E, Kent D V, Balini M. 2014.. A Middle-Late Triassic (Ladinian-Rhaetian) carbon and oxygen isotope record from the Tethyan Ocean[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 399(4):246-259.

    Google Scholar

    Qing H R, Veizer J. 1994. Oxygen and carbon isotopic composition of Ordovician brachiopods:implications for coeval seawater[J]. Geochimica et Cosmochimica Acta, 58(20):4429-4442. doi: 10.1016/0016-7037(94)90345-X

    CrossRef Google Scholar

    Scholle P A, Arthur, M A. 1980. Carbon isotope fluctuations in Cretaceous pelagic limestone:potential stratigraphic and petroleum exploration tool[J]. American Association of Petroleum Geologists Bulletin, 64(1):67-87.

    Google Scholar

    Shao Longyi. 1994. The relation of the oxygen and carbon isotopic in the carbonate rocks to the Paleotemperature etc.[J]. Journal of China University of Mining & Technology, 23(1):39-45 (in Chinese with English abstract).

    Google Scholar

    Song Huyue, Tong Jinnan, Tian Li, Song Haijun, Qiu Haiou, Zhu yuanyuan, Thomas Algeo. 2014. Paleo-redox conditions across the Permian-Triassic boundary in shallow carbonate platform of the Nanpanjiang Basin, South China[J]. Science China:Earth Sciences, 57:1030-1038 (in Chinese). doi: 10.1007/s11430-014-4843-2

    CrossRef Google Scholar

    Song H Y, Tong J N, Algeo T J, Horacekc M, Qiu H O, Song H J, Tian L, Chen Z Q. 2013. Large vertical δ13CDIC gradients in Early Triassic seas of the South China craton:implications for oceanographic changes related to Siberian Traps volcanism[J]. Global and Planetary Change, 105:7-20. doi: 10.1016/j.gloplacha.2012.10.023

    CrossRef Google Scholar

    Suess E. 1980. Particulate organic carbon flux in the ocean-surface productivity and oxygen utilization[J]. Nature, 288:260-263. doi: 10.1038/288260a0

    CrossRef Google Scholar

    Tang Dongjie, Shi xiaoying, Liu Juan, Wang Xinqiang, Pei Yunpeng. 2009. Authigenic carbonate precipitation and pyrites from sandveinsin the Chuanlinggou Formation of the North China Platform-Evidence for anaerobic oxidation of methane in the Mesoproterozoic[J]. Journal of Palaeogeography, 11(4):361-374(in Chinese with English abstract).

    Google Scholar

    Veizer J, Ala D, Azmy K, Bruckschen P, Buhl D, Bruhn F, Carden G, Diener A, Ebneth S, Godderis Y, Jasper T, Korte C, Pawellek F, Podlaha O G, Strauss H. 1999. 87Sr/86Sr, δ13C and δ18O evolution of Phanerozoic seawater[J]. Chemical Geology, 161(1):59-88.

    Google Scholar

    Wang Chengyuan, Kang Peiquan, Wang Zhihao. 1998. Conodontbased age of the Kueichousaurus hui Yang[J]. Acta Micropalaeontologica Sinica, 15(2):196-198(in Chinese with English abstract).

    Google Scholar

    Wang Chuanshang, Li Zhihong, Peng Zhongqin, Wang Baozhong, Zhang Guotao. 2014. The carbon isotope variation and its responses to sea level changes during the late Early Devonian period in Guizhou and Guangxi[J]. Geology in China, 41(6):2039-2047(in Chinese with English abstract).

    Google Scholar

    Wang Liting. 1996. A discussion on horizon and age of Kueichousaurus hui occurrence[J]. Guizhou Geology, 13(3):209-212(in Chinese with English abstract).

    Google Scholar

    Yang Ruidong. 1996. Palaeoecology and fossil communities in Southern and Central Guizhou during Triassic Time[J]. Lithology Palaeogeography, 16(6):42-47(in Chinese with English abstract).

    Google Scholar

    Zeng Xiongwei, Chen Xiaohong, Cheng Long, Wang Jianpo. 2013. Redefinition of the Zhuganpo Formation in the southest Yangtze platform[J]. Journal of Stratigraphy, 37(4):479-484(in Chinese with English abstract).

    Google Scholar

    Zhang Xiulian. 1985. Relationship between carbon and oxygen stable isotopic in carbonate rocks and paleosalinity and paletemperature of seawater[J]. Acta Geologica Sinica, 3(4):17-30(in Chinese with English abstract).

    Google Scholar

    Zou X D, Balini M, Jiang D Y. 2015. Ammonoids from the Zhuganpo Member of the Falang Formation at Nimaigu and their relevance for dating the Xingyi Fossil-Lagerstaette (Late Ladinian, Guizhou, China)[J]. Rivista Italiana Di Paleontologia E Stratigrafia, 121(2):135-161.

    Google Scholar

    Zou Xiaodong, Guo Wen, Jiang Dayong, Sun Zuoyu. 2015.Preliminary analysis of environment of fossils reservoir of Xingyi Fauna in Guizhou Province[J]. Acta Scientiarum Naturalium Universitatis Pekinensis, 51(3):472-484.

    Google Scholar

    Zuo Jingxun, Tong Jinnan, Qiu Haiou, Zhao Laishi. 2006. Oxygen and carbon isotopic compositions of Middle Triassic carbonates from Lower Yangtze[J]. Science in China (Series D), 36(2):109-122(in Chinese).

    Google Scholar

    陈孝红, 危凯, 张保民, 程龙. 2013.贵州关岭下三叠统永宁镇组碳同位素化学地层与海洋氧化事件[J].中国地质, 40(5):1466-1473. doi: 10.3969/j.issn.1000-3657.2013.05.011

    CrossRef Google Scholar

    董致中, 王伟. 2006.云南牙形类动物群——相关生物地层及生物地理区研究[M].昆明:云南科技出版社, 1-347.

    Google Scholar

    冯增昭, 鲍志东, 李尚武. 1994.滇黔桂地区早中三叠世岩相古地理[M].东营:石油大学出版社, 1-180.

    Google Scholar

    孔锐, 高孝伟, 2006.统计学[M].北京:中国大地出版社, 1-273.

    Google Scholar

    李锦玲, 奥利维尔. 2004.贵州兴义中三叠世Nothosaurus——新种[J].古脊椎动物学报, 42(1):1-5. doi: 10.3969/j.issn.1000-3118.2004.01.001

    CrossRef Google Scholar

    李荣西, 魏家庸, 肖家飞, 王兴理, Lehrmann D J. 2007.海进体系域碳氧同位素地球化学响应——以黔西南地区三叠系为例[J].地球科学与环境学报, 29(1):1-5. doi: 10.3969/j.issn.1672-6561.2007.01.001

    CrossRef Google Scholar

    李志广, 孙作玉, 江大勇, 季承. 2016.贵州兴义三叠纪兴义动物群化石层锆石LA-ICP-MSU-Pb年龄及其意义[J].地质论平, 62(3):779-790.

    Google Scholar

    罗贝维, 魏国齐, 杨威, 董才源. 2013.四川盆地晚震旦世古海洋环境恢复及地质意义[J].中国地质, 40(4):1099-1111. doi: 10.3969/j.issn.1000-3657.2013.04.009

    CrossRef Google Scholar

    罗顺社, 汪凯明. 2010.河北宽城地区中元古代高于庄组碳酸盐岩碳氧同位素特征[J].地质学报, 84(4):492-499. doi: 10.3969/j.issn.1006-7493.2010.04.009

    CrossRef Google Scholar

    马乐天, 季承, 孙作玉, 杨鹏飞, 邹晓东. 2013.贵州兴义三叠纪海生爬行动物群的地层分布及其生物多样性[J].地层学杂志, 37(2):178-185.

    Google Scholar

    梅冥相, 马永生, 邓军, 孟庆芬, 易定红, 李东海. 2003.南盘江盆地及邻区早中三叠世层序地层格架及其古地理演化——兼论从"滇黔桂盆地"到"南盘江盆地"的演变过程[J].高校地质学报, 9(3):427-439. doi: 10.3969/j.issn.1006-7493.2003.03.013

    CrossRef Google Scholar

    邵龙义. 1994.碳酸盐岩氧、碳同位素与古温度等的关系[J].中国矿业大学学报, 23(1):39-45.

    Google Scholar

    宋虎跃, 童金南, 田力, 宋海军, 邱海鸥, 朱园园. 2014.南盘江地区二叠纪-三叠纪之交浅水台地古氧相研究[J].中国科学:地球科学, 44(6):1273-1282.

    Google Scholar

    汤冬杰, 史晓颖, 刘娟, 王新强, 裴云鹏. 2009.华北地台串岭沟组砂脉中自生碳酸盐沉淀和自生黄铁矿——中元古代甲烷厌氧氧化的沉积证据[J].古地理学报, 11(4):361-374.

    Google Scholar

    王成源, 康沛泉, 王志浩. 1998.以牙形刺确定胡氏贵州龙(Kueichousaurus hui Yang)层的时代[J].微体古生物学报, 15(2):196-198.

    Google Scholar

    王传尚, 李志宏, 彭中勤, 王保忠, 张国涛. 2014.黔桂地区早泥盆世晚期碳稳定同位素变化及其对海平面变化的响应[J].中国地质, 41(6):2039-2047. doi: 10.3969/j.issn.1000-3657.2014.06.018

    CrossRef Google Scholar

    王立亭. 1996.胡氏贵州龙(Kueichousaurus hui)的产出层位及时代讨论[J].贵州地质, 13(3):209-212.

    Google Scholar

    杨瑞东. 1996.黔中、黔南三叠纪古生态、古群落研究[J].岩相古地理, 16(6):42-47.

    Google Scholar

    曾雄伟, 陈孝红, 程龙, 王建坡. 2013.扬子地台西南缘竹竿坡组的厘定[J].地层学杂志, 37(4):479-484.

    Google Scholar

    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.

    Google Scholar

    邹晓东, 郭文, 江大勇, 孙作玉. 2015.贵州省兴义地区中三叠世兴义动物群化石储集层古环境初步分析[J].北京大学学报(自然科学版), 51(3):472-484.

    Google Scholar

    左景勋, 童金南, 邱海鸥, 赵来时. 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), 36(2):109-122.

    Google Scholar

    • Relative Articles
  • Cited by
  • Supplements
    • Proportional views
  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Figures(4)

Tables(1)

Export Citation
PDF
XML

Article Metrics

Article views(2901) PDF downloads(1160) Cited by(0)

Access History

Other Articles By Authors

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    版权所有：中国地质调查局发展研究中心 copyright @2020