Composition and evolution of strontium isotope from the fossiliferous layers of the Luoping biota, Yunnan

XIE Tao; HU Shixue; ZHOU Changyong; ZHANG Qiyue; HUANG Jinyuan; WEN Wen

doi:10.12029/gc20190314

GEOLOGY IN CHINA > 2019 > 46(3): 642-650. > DOI: 10.12029/gc20190314

XIE Tao, HU Shixue, ZHOU Changyong, ZHANG Qiyue, HUANG Jinyuan, WEN Wen. Composition and evolution of strontium isotope from the fossiliferous layers of the Luoping biota, Yunnan[J]. GEOLOGY IN CHINA, 2019, 46(3): 642-650. DOI: 10.12029/gc20190314

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Composition and evolution of strontium isotope from the fossiliferous layers of the Luoping biota, Yunnan

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

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China Geological Survey Program 12120114068101

China Geological Survey Program DD20160020

National Natural Science Foundation of China 41502013

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Author Bio:
XIE Tao, male, born in 1982, senior engineer, engages in regional geological and mineral survey; E-mail: xt1982cd@163.com
Received Date: July 20, 2017
Revised Date: January 17, 2018
Available Online: September 25, 2023

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Abstract

Abstract

The ⁸⁷Sr/⁸⁶Sr curve of seawater is relatively stable in the Anisian period of Middle Triassic according to data available, which is different from the situation of frequent changes in the Early Triassic. The recovery of marine ecosystem from the endPermian mass extinction experienced an accelerating phase during the Anisian period. The Luoping biota is one of the typical representatives of the Triassic biota. The authors studied the composition and evolution of the strontium isotope in 26 carbonate samples from the standard section, i.e., Dawazi section, of the Luoping biota, in order to know the change of strontium isotope from the fossiliferous layers which contain the Luoping biota. The results show three remarkable characteristics:(1) The average value of Sr is more than 2000×10^-6 from the carbonate, which is mainly caused by the aragonite and diagenesis; (2) the low value of Mn and the Mn/Sr ratios less than 0.4 show that the these ⁸⁷Sr/⁸⁶Sr ratios can represent the composition of Sr isotope of the coeval seawater; (3) the ratios of ⁸⁷Sr/⁸⁶Sr of all samples range between 0.707969 and 0.708253, with the average ratio 0.708025. It is notable that the ratios of the ⁸⁷Sr/⁸⁶Sr are larger than the data for the same geological time published from Europe. Nevertheless, they are similar to Sr isotopic values from other areas in southern China. The authors therefore hold that the strontium isotope composition of the fossiliferous layers of the Luoping biota was not directly connected to global geological events, but affected by the regional event, such as the indosinian movement.
- strontium isotope,
- Luoping biota,
- Anisian period,
- marine carbonate rocks,
- Yunnan

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References (66)

References

Benton M J, Twitchett R J. 2003. How to kill (almost) all life:The end-Permian extinction event[J]. Trends in Ecology and Evolution, 18(7):358-365. doi: 10.1016/S0169-5347(03)00093-4

Benton M J, Zhang Qiyue, Hu Shixue, Chen Zhongqiang, Wen Wen, Liu Jun, Huang Jinyuan, Zhou Changyong, Xie Tao, Tong Jinnan, Choo B. 2013. Exceptional vertebrate biotas from the Triassic of China, and the expansion of marine ecosystems after the PermoTriassic mass extinction[J]. Earth-Science Reviews, 125:199-243. doi: 10.1016/j.earscirev.2013.05.014

Boulton S J, Robertson A H F, Ellam R M, Safak Ü, Can Ü N G C. 2007. Strontium Isotopic and Micropalaeontological Dating Used to Help Redefine the tratigraphy of the Neotectonic Hatay Graben, Southern Turkey[J]. Turkish Journal of Earth Sciences, 16:141-179.

Brand U, Veizer J. 1980. Chemical diagenesis of a multicomponent carbonate system-1:Trace elements[J]. Journal of Sedimentary Petrology, 50:1219-1236.

Broecker W S, Peng T H. 1982. Tracers in the Sea[M]. New York:Eldigio Press.

Bruckschen P, Bruhn F, Veizer J, Buhl D. 1995. ⁸⁷Sr/⁸⁶Sr isotopic evolution of Lower Carboniferous seawater:Dinantian of western Europe[J]. Sedimentary Geology, 100:63-81. doi: 10.1016/0037-0738(95)00103-4

Chang Xiaolin, Shi He, Luo Wei, Song Ying, Wan Mingli. 2010. Sr isotopic curve of the Lower-Middle Triassic of East Sichuan and the chronostratigraphic division[J]. Journal of chengdu University of Technology(Science & Technology edition), 37(1):9-14(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cdlgxyxb201001002

Chen Z Q, Benton M J. 2012. The timing and pattern of biotic recovery following the end-Permian mass extinction[J]. Nature Geoscience, 5(6):375-383. doi: 10.1038/ngeo1475

Chen Z Q, Shi G R, Kaiho K. 2002. A New Genus of Rhynchonellid Brachiopod from the Lower Triassic of South China and Implications for Timing the Recovery of Brachiopoda After the End-Permian Mass Extinction[J]. Palaeontology, 45(1):149-164. doi: 10.1111/pala.2002.45.issue-1

Denison R E, Koepnick R B, Burke W H, Hetherington E A, Fletcher A. 1994a. Construction of the Mississippian, Pennsylvanian and Permian seawater ⁸⁷Sr/⁸⁶Sr curve[J]. Chemical geology, 112:145-167. doi: 10.1016/0009-2541(94)90111-2

Denison R E, Koepnick R B, Fletcher A, Howell M W, Callaway W S. 1994b. Criteria for the retention of original seawater in ancient shelf limestones[J]. Chemical Geology, 112:131-143. doi: 10.1016/0009-2541(94)90110-4

Derry L A, Keto L S, Jacobsen S B, Knoll A H, Swett K. 1989. Sr isotopic variations in Upper Proterozoic carbonates from Svalbard and East Greenland[J]. Geochimica et Cosmochimica Acta, 53(9):2331-2339. doi: 10.1016/0016-7037(89)90355-4

Erwin D H. 2006. Extinction:How Life on Earth Nearly Ended 250 Million Years Ago[M]. Princeton:Princeton University Press.

Galfetti T, Bucher H, Brayard A, Hochuli P A, Weissert H, Guodun K, Atudorei V, Guex J. 2007. Late Early Triassic climate change:insights from carbonate carbon isotopes, sedimentary evolution and ammonoid paleobiogeography[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 243(3):394-411. http://d.old.wanfangdata.com.cn/NSTLQK/NSTL_QKJJ023718390/

Hallam A. 1991. Why was there a delayed radiation after the endPalaeozoic extinctions?[J]. Historical Biology, 5(2/4):257-262. doi: 10.1080/10292389109380405

Hu Shixue, Zhang Qiyue, Chen Zhongqiang, Zhou Changyong, Lü Tao, Xie Tao, Wen Wen, Huang Jinyuan, Benton M J. 2011. The Luoping biota:exceptional preservation, and new evidence on the Triassic recovery from end-Permian mass extinction[J]. Proceeding of the Royal Society B, 278:2274-2282. doi: 10.1098/rspb.2010.2235

Hu Zuowei, Huang Sijing, Qing Hairuo, Wang Qingdong, Wang Chunmei, Gao Xiaoyong. 2008. Evolution and global correlation for strontium isotopic composition of marine Triassic from Huaying Mountains, eastern Sichuan, China[J]. Science in China Series D:Earth Sciences, 51(4):540-549. doi: 10.1007/s11430-008-0031-6

Huang Jinyuan, Zhang Kexin, Zhang Qiyue, Lü Tao, Zhou Changyong, Bai Jianke. 2009. Conodonts stratigraphy and sedimentary environment of the Middle Triassic at Daaozi section of Luoping county, Yunnan Province, South China[J]. Acta Micropalaeontologica Sinica, 26(3):211-224(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=wtgswxb200903002

Huang Sijing. 1997. A Study on carbon and strontium isotopes of late paleozoic carbonate rocks in the upper Yangtze platform[J]. Acta Geologica Sinica, 71(1):45-53(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199700067621

Huang Sijing, Huang Keke, Lü Jie, Lan Yefang. 2012. Carbon isotopic composition of Early Triassic marine carbonates, Eastern Sichuan Basin, China[J]. Science China(Earth Sciences), 55(12):2026-2038. doi: 10.1007/s11430-012-4440-1

Huang Sijing, Qing Hairuo, Huang Peipei, Hu Zuowei, Wang Qingdong, Zou Mingliang, Liu Haonian. 2008. Evolution of strontium isotopic composition of seawater from Late Permian to Early Triassic based on study of marine carbonates, Zhongliang Mountain, Chongqing, China[J]. Science in China (Series D):Earth Sciences, 51(4):528-539. doi: 10.1007/s11430-008-0034-3

Huang Sijing, Shi He, Zhang Meng, Wu Wenhui, Shen Licheng. 2002.Global correlation of strontium isotope evolution curve of Devonian in Longmen mountain and dating marine sediments[J]. Progress in Natural Science, 12(9):945-951(in Chinese).

Huang Sijing, Sun Zhilei, Wu Sujuan, Zhang Meng, Pei Changrong, Hu Zuowei. 2006. Strontium isotope composition and control factors of global sea water in Triassic[J]. Journal of Mineralogy and Petrology, 26(1):43-48(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KWYS200601008.htm

Jiang Maosheng, Zhu Jiangquan, Chen Daizhao, Zhang Renhu, Qiao Guangsheng. 2001. Carbon and strontium isotope variations and responses to sea-level fluctuations in the Ordovician of the Tarim Basin[J]. Science in China (Series D):Earth Sciences, 44(9):816-823. doi: 10.1007/BF02907094

Jin Y G, Wang Y, Wang W, Shang Q H, Cao C Q, Erwin D H. 2000.Pattern of marine mass extinction near the Permian-Triassic boundary in South China[J]. Science, 289(5478):432-436. doi: 10.1126/science.289.5478.432

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

Kaufman A J, Knoll A H, Awramik S M. 1992. Biostratigraphic and chemostratigraphic correlation of Neoproterozoic sedimentary successions:Upper Tindir Group, northwestern Canada, as a test case[J]. Geology, 20(2):181-185. doi: 10.1130/0091-7613(1992)020<0181:BACCON>2.3.CO;2

Koepnick R B, Denison R E, Burke W H, Hetherington E A, Dahl D A. 1990. Construction of the Triassic and Jurassic portion of the Phanerozoic curve of seawater ⁸⁷Sr/⁸⁶Sr[J]. Chemical Geology:Isotope Geoscience section, 80(4):327-349. doi: 10.1016/0168-9622(90)90014-4

Korte C, Kozur H W, Bruckschen P, Veizer J. 2003. Strontium isotope evolution of Late Permian and Triassic seawater[J]. Geochimica et Cosmochimica Acta, 67(1):47-62. doi: 10.1016/S0016-7037(02)01035-9

Kozur H W. 2003. Integrated ammonoid, conodont and radiolarian zonation of the Triassic and some remarks to stage/substage subdivision and the numeric age of the Triassic stages[J]. Albertiana, 28:57-74.

Lehrmann D J, Ramezani J, Bowring S A, Martin M W, Montgomery P, Enos P, Payne J L, Orchard M J, Hongmei W, Jiayong W. 2006.Timing of recovery from the end-Permian extinction:geochronologic and biostratigraphic constraints from south China[J]. Geology, 34(12):1053-1056. doi: 10.1130/G22827A.1

Li Rongxi, Wei Jiayong, Xiao Jiafei, Wang Xingli, Lehrmann D J. 2003. Early-Middle Triassic sedimentary facies and LadinianCarnian transgression in southwestern Guizhou Province, South China[J]. Journal of Changpan University (Earth Science Edition), 25(3):1-6(in Chinese with English abstract).

Li Rongxi, Wei Jiayong, Yan Weidong, Guo Qingjun. 2000. Variations of ratio of ⁸⁷Sr/⁸⁶Sr in seawater with time:Implications for sea level changes and global correlation[J]. Advance in Earth Sciences, 15(6):729-733(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXJZ200006018.htm

Mcarthur J M. 1994. Recent trends in strontium isotope stratigraphy[J]. Terra Nova, 6(4):331-358. doi: 10.1111/ter.1994.6.issue-4

Mei Mingxiang. 2010. Stratigraphic impact of the Indo-China Movement and its related evolution of sedimentary-basin pattern of the late Triassic in the middle-upper Yangtze Region[J]. Earth Science Frontiers(4):99-111(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy201004008

Palmer M R, Elderfield H. 1985. Sr isotope composition of sea water over the past 75 Myr[J]. Nature, 314:526-528. doi: 10.1038/314526a0

Payne J L, Kump L R. 2007. Evidence for recurrent Early Triassic massive volcanism from quantitative interpretation of carbon isotope fluctuations[J]. Earth and Planetary Science Letters, 256:264-277. doi: 10.1016/j.epsl.2007.01.034

Payne J L, Lehrmann D J, Wei J, Orchard M J, Schrag D P, Knoll A H. 2004. Large perturbations of the carbon cycle during recovery from the end-Permian extinction[J]. Science, 305:506-509. doi: 10.1126/science.1097023

Posenato R. 2008. Patterns of bivalve biodiversity from Early to Middle Triassic in the Southern Alps (Italy):Regional vs. global events[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 261(1):145-159. https://www.sciencedirect.com/science/article/pii/S0031018208000527

Rhodes M K, Carroll A R, Pietras J T, Beard B L, Johnson C M. 2002.Strontium isotope record of paleohydrology and continental weathering, Eocene Green River Formation, Wyoming[J]. Geology, 30(2):167-170. doi: 10.1130/0091-7613(2002)030<0167:SIROPA>2.0.CO;2

Sawaki Y, Kawai T, Shibuya T, Tahata M, Omori S, Komiya T, Yoshida N, Hirata T, Ohno T, Windley B F. 2010. ⁸⁷Sr/⁸⁶Sr chemostratigraphy of Neoproterozoic Dalradian carbonates below the Port Askaig glaciogenic formation, Scotland[J]. Precambrian Research, 179(1/4):150-164. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=c8ca03192b7b7021d285efd9d97ad0b8

Solé R V, Montoya J M, Erwin D H. 2002. Recovery after mass extinction:evolutionary assembly in large-scale biosphere dynamics[J]. Philosophical Transactions of the Royal Society of London. Series B:Biological Sciences, 357(1421):697-707. doi: 10.1098/rstb.2001.0987

Song Haijun, Wignall P B, Tong Jinnan, Yin Hongfu. 2013. Two pulses of extinction during the Permian-Triassic crisis[J]. Nature Geoscience, 6(1):52-56. https://www.researchgate.net/publication/258807265_Two_pulses_of_extinction_during_the_Permian-Triassic_crisis?ev=auth_pub

Song Haijun, Wignall P B, Tong Jinnan, Song Huyue, Chen Jing, Chu Daoliang, Tian Li, Luo Mao, Zong Keqing, Chen Yanlong, Lai Xulong, Zhang Kexin, Wang Hongmei. 2015. Integrated Sr isotope variations and global environmental changes through the Late Permian to early Late Triassic[J]. Earth and Planetary Science Letters, 424:140-147. doi: 10.1016/j.epsl.2015.05.035

Sun Yuanyuan, Liu Jun, Lü Tao, Xu Xiaosong, Zhang Qiyue, Lou Xiongying, Jiang Xinsheng. 2009. Oxygen and carbon isotopic compositions of Middle Triassic carbonates from the Dawazi Section of Luoping, Yunnan:Implications for paleoenvironment of the Luoping Lagerstätte[J]. Acta Geological Sinica, 83(8):1110-1117(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE200908010.htm

Tong Jinnan, Yin Hongfu. 2009. Advance in the study of early triassic life and environment[J]. Acta Palaeontologica Sinica, 48(3):497-508(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=gswxb200903020

Tong Jinnan, Zhang Suxin, Zuo Jingxun, Xiong Xinqi. 2007a. Events during Early Triassic recovery from the end-Permian extinction[J]. Global and Planetary Change, 55(1):66-80. http://www.sciencedirect.com/science/article/pii/S0921818106001391

Tong Jinnan, Zuo Jingxun, Chen Z Q. 2007b. Early Triassic carbon isotope excursions from South China:Proxies for devastation and restoration of marine ecosystems following the end-Permian mass extinction[J]. Geological Journal, 42:371-389. doi: 10.1002/(ISSN)1099-1034

Veizer J, Ala D, Azmy K, Bruckschen P, Buhl D, Bruhn F, Carden G A F, Diener A, Ebneth S, Godderis Y. 1999. ⁸⁷Sr/⁸⁶Sr, δ¹³C and δ¹⁸O evolution of Phanerozoic seawater[J]. Chemical Geology, 161:59-88. doi: 10.1016/S0009-2541(99)00081-9

Xie Tao, Zhou Changyong, Zhang Qiyue, Hu Shixue, Huang Jinyuan, Wen Wen, Cong Feng. 2013. Zircon U-Pb age for the tuff before the Luoping Biota and its geological implication[J]. Geological Review, 59(1):159-164(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzlp201301017

Yan Zhaobin, Guo Fusheng, Pan Jiayong, Guo Guolin, Zhang Yuejing. 2005. Application of C, O and Sr isotope composition of carbonates in the research of paleoclimate and paleooceanic environment[J]. Contributions to Geology and Mineral Resources Research, 20(1):53-56(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzzklc200501010

Yin Hongfu, Tong Jinnan, Ding Meihua, Zhang Kexin, Lai Xulong. 1994. Late Permian-Middle Triassic sea level changes of Yangtze platform[J]. Earth Science, 19(5):627-632(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199400042369

Zhang Qiyue, Zhou Changyong, Lü Tao, Xie Tao, Lou Xiongying, Liu Wei, Sun Yuanyuan, Huang Jinyuan, Zhao Laishi. 2009. A conodont-based Middle Triassic age assignment for the Luoping Biota of Yunnan, China[J]. Science in China (Series D):Earth Sciences, 52(10):1673-1678. doi: 10.1007/s11430-009-0114-z

常晓琳, 石和, 罗威, 宋莹, 万明礼. 2010.川东地区下-中三叠统的锶同位素曲线及年代地层划分[J].成都理工大学学报(自然科学版), 37(1):9-14 doi: 10.3969/j.issn.1671-9727.2010.01.002

黄金元, 张克信, 张启跃, 吕涛, 周长勇, 白建科. 2009.云南罗平中三叠世大凹子剖面牙形石生物地层及其沉积环境研究[J].微体古生物学报, 26(3):211-224 doi: 10.3969/j.issn.1000-0674.2009.03.002

黄思静. 1997.上扬子地台区晚古生代海相碳酸盐岩的碳、锶同位素研究[J].地质学报, 71(1):45-53 http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199700067621

黄思静, 石和, 张萌, 武文慧, 沈立成. 2002.龙门山泥盆纪锶同位素演化曲线的全球对比及海相地层的定年[J].自然科学进展, 12(9):945-951. doi: 10.3321/j.issn:1002-008X.2002.09.010

黄思静, 孙治雷, 吴素娟, 张萌, 裴昌蓉, 胡作维. 2006.三叠纪全球海水的锶同位素组成及主要控制因素[J].矿物岩石, 26(1):43-48 doi: 10.3969/j.issn.1001-6872.2006.01.009

李荣西, 魏家庸, 肖家飞, 王兴理, Lehrmann D J. 2003.黔西南地区早-中三叠世沉积岩相与Ladinian-Carnian期大海侵[J].长安大学学报(地球科学版), 25(3):1-6. doi: 10.3969/j.issn.1672-6561.2003.03.001

李荣西, 魏家庸, 杨卫东, 郭庆军. 2000.用⁸⁷Sr/⁸⁶Sr研究海平面变化与全球对比问题[J].地球科学进展, 15(6):729-733. doi: 10.3321/j.issn:1001-8166.2000.06.019

梅冥相. 2010.中上扬子印支运动的地层学效应及晚三叠世沉积盆地格局[J].地学前缘, 17(4):99-111. http://d.old.wanfangdata.com.cn/Periodical/dxqy201004008

孙媛媛, 刘俊, 吕涛, 许效松, 张启跃, 楼雄英, 江新胜. 2009.罗平生物群产出层位氧碳稳定同位素的初步研究[J].地质学报, 83(8):1110-1117. doi: 10.3321/j.issn:0001-5717.2009.08.008

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. doi: 10.3969/j.issn.0001-6616.2009.03.020

谢韬, 周长勇, 张启跃, 胡世学, 黄金元, 文芠, 丛峰. 2013.罗平生物群下部凝灰岩锆石年龄及其地质意义[J].地质论评, 59(1):159-164. doi: 10.3969/j.issn.0371-5736.2013.01.017

严兆彬, 郭福生, 潘家永, 郭国林, 张曰静. 2005.碳酸盐岩C, O, Sr同位素组成在古气候、古海洋环境研究中的应用[J].地质找矿论丛, 20(1):53-56. doi: 10.3969/j.issn.1001-1412.2005.01.010

殷鸿福, 童金南, 丁梅华, 张克信, 赖旭龙. 1994.扬子区晚二叠世-中三叠世海平面变化[J].地球科学, 19(5):627-632. doi: 10.3321/j.issn:1000-2383.1994.05.004

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Composition and evolution of strontium isotope from the fossiliferous layers of the Luoping biota, Yunnan