牙形石微量元素对生物绝灭事件的响应: 以二叠-三叠系全球层型剖面第一幕绝灭事件为例

赵来时; 吴元保; 胡兆初; 周炼; 刘勇胜; 史玉芳; 张素新; 童金南; 袁鹏

Volume 34 Issue 5

Sep. 2009

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Article Navigation > Earth Science > 2009 > 34(5): 725-732

ZHAO Lai-shi, WU Yuan-bao, HU Zhao-chu, ZHOU Lian, LIU Yong-sheng, SHI Yu-fang, ZHANG Su-xin, TONG Jin-nan, YUAN Peng, 2009. Trace Element Compositions in Conodont Phosphates Responses to Biotic Extinction Event: A Case Study for Main Act of Global Boundary Stratotype Section and Point of the Permian-Triassic. Earth Science, 34(5): 725-732.

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Trace Element Compositions in Conodont Phosphates Responses to Biotic Extinction Event: A Case Study for Main Act of Global Boundary Stratotype Section and Point of the Permian-Triassic

State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China

Received Date: 2009-02-10
Publish Date: 2009-09-25

Abstract

Abstract

Trace element compositions in Upper Permian conodonts with low color alteration index were measured in situ by laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) from a stratigraphic section of the Meishan in Changxing, Zhejiang Province.The results show that the Ce anomalies and rare earth element (REE) concentrations are characterized by fast fluctuation.These features indicate highly fluctuating environmental conditions including redox and instable ecosystem conditions during the P/T transition.The element compositions couple well with the paleo-oceanic environment and the biotic crisis.The study effective defines and offers new approach for the key issues to the biotic extinction and recovery process, time limit, paleo-ocean chemistry and paleoecology at the end of the Permian.
- condont,
- trace element,
- in situ,
- biotic extinction event,
- LA-ICP-MS

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References

Becker, L., Poreda, R. J., Basu, A. R., et al., 2004. Bedout: A possible end-Permianimpact crater offshore of north-western Australia. Science, 304 (5676): 1469-1476. doi: 10.1126/science.1093925

Becker, L., Poreda, R. J., Hunt, A. G., et al., 2001. Impact event at the Permian-Triassic boundary: Evidence from extraterrestrial noble gases in fullerenes. Science, 291 (5508): 1530-1533. doi: 10.1126/science.1057243

Cao, C. Q., Wang, W., Jin, Y. G., 2002. Carbon isotope ex-cursions across the Permian-Triassic boundary in the Meishan Section, Zhejiang Province, China. Chinese Sci-ence Bulletin, 47 (4): 302-306 (in Chinese).

Clark, D. L., Wang, C., Orth, C. J., et al., 1986. Conodont survival and lowiridium abundances across the Permi-an-Triassic boundary in South China. Science, 233 (4767): 984-986. doi: 10.1126/science.233.4767.984

De Baar, H. J. W., German, C. R., Elderfied, H., et al., 1988. Rear earth element distributions in anoxic waters of the Cariaco Trench. Geochim. Cosmochim. Acta, 52 (5): 1203-1219. doi: 10.1016/0016-7037(88)90275-X

Erwin, D. H., Bowring, S. A., Jin, Y., 2002. End-Permian mass extinctions: A review. In: Koeberl, C., MacLeod, K. G., eds., Catastrophic events and nass extinctions: Impacts and beyond. Geological Society of America Spe-cial Paper356, Boulder, 363-383.

Evelyn, S. K., Danicl, J. L., Dominic, D., et al., 2004. Stable carbon isotope stratigraphy across the Permian-Triassic boundary in shallow marine carbonate platforms, Nan-panjiang basin, South China. Palaeogeography, Palaeo-climatology, Palaeoecology, 204 (3-4): 297-315. doi: 10.1016/S0031-0182(03)00732-6

Fang, Z. J., 2004a. The pattern of the mass extinction and the change of the global ecosystemandits causes during the Permian-Triassic transition. In: Rong, J. Y., Fang, Z. J., eds., Mass extinction and recovery evidence from the Palaeozoic and Triassic of South China. University of Science and Technology of China Press, Hefei, 785-928 (in Chinese).

Fang, Z. J., 2004b. Exploration on the pattern of the extinc-tion of bivalve of South China. In: Rong, J. Y., Fang, Z. J., eds., Mass extinction and recovery evidence from the Palaeozoic and Triassic of South China. China Uni-versity of Science and Technology of China Press, Hefei, 571-646 (in Chinese).

Felitsyn, S., Sturesson, U., Popov, L., et al., 1998. Nd iso-tope composition and rare Earth element distribution in early Paleozoic biogenic apatite from Baltoscandia: A signature of Iapetus ocean water. Geology, 26 (12): 1083-1086. doi: 10.1130/0091-7613(1998)026<1083:NICARE>2.3.CO;2

Gao, S., Liu, X. M., Yuan, H. L., et al., 2002. Determination of forty two major and trace elements in USGS and NIST SRM glasses bylaser ablation-inductively coupled plasma-mass spectrometry. Geostandards Newsletter: The Journal of Geostandards and Geoanalysis, 26 (2): 181-195. doi: 10.1111/j.1751-908X.2002.tb00886.x

Girard, C., Albarède, F., 1996. Trace elements in conodont phosphates from the Frasnian/Famennian boundary. Palaeogeography, Palaeoclimatology, Palaeoecology, 126 (1-2): 195-209. doi: 10.1016/S0031-0182(96)00114-9

Girard, C., Lécuyer, C., 2002. Variations in Ce anomalies ofconodonts through the Frasnian/Famennian boundary of Poland (Kowala-Holy Cross Mountains): Implica-tions for the redox state of seawater and biodiversity. Palaeogeography, Palaeoclimatology, Palaeoecology, 181 (1-3): 299-311. doi: 10.1016/S0031-0182(01)00482-5

Grandjean, P., Cappetta, H., Albare'de, F., 1988. The REE and ε_Nd of 40-70 Ma old fish debris fromthe West Af-rican platform. Geophys. Res. Lett. , 15 (4): 389-392. doi: 10.1029/GL015i004p00389

Grice, K., Cao, C., Love, G. D., et al., 2005. Photic zone eu-xinia during the Permian-Triassic superanoxic event. Science, 307 (5710): 706-709. doi: 10.1126/science.1104323

Gromet, L. P., Haskin, L. A., Korotev, R. L., et al., 1984. The"North American Shale Composite": Its compila-tion, major and trace element characteristics. Geochim. Cosmochim. Acta, 48 (12): 2469-2482. doi: 10.1016/0016-7037(84)90298-9

Huang, X. Y., Jiao, D., Lu, L. Q., et al., 2007. The fluctua-ting enevironment associated with the episodic biotic crisis during the Permo-Triassic transition: Evidence from microbial biomarkers in Changxing, Zhejiang Prov-ince. Science in China (Ser. D), 37 (5): 629-635 (inChinese).

Jin, Y. G., Wang, Y., Wang, W., et al., 2000. Pattern of ma-rine mass extinction near the Permian-Triassic boundary in South China. Science, 289 (5478): 432-443. doi: 10.1126/science.289.5478.432

Kemp, R. A., Trueman, C. N., 2003. Rare earth elements in Solnhofen biogenic apatite: Geochemical clues to the pa-leoenvironment. Sediment. Geol. , 155 (1-2): 109-127. doi: 10.1016/S0037-0738(02)00163-X

Kozur, H. W., 1998. Some aspects of the Permian-Triassic boundary (PTB) and of the possible causes for the biot-ic crisis around this boundary. Palaeogeography, Palaeoclimatology, Palaeoecology, 143 (4): 227-272. doi: 10.1016/S0031-0182(98)00113-8

Lécuyer, C., Grandjean, P., Barrat, J. A., et al., 1998. ¹⁸O and REE contents of phosphatic brachiopods: A com-parison between modern and lower Paleozoic popula-tions. Geochim. Cosmochim. Acta, 62 (14): 2429-2436. doi: 10.1016/S0016-7037(98)00170-7

Lécuyer, C., Reynard, B., Grandjean, P., 2004. Rare earth el-ement evolution of Phanerozoic seawater recordedin bi-ogenic apatites. Chemical Geology, 204 (1-2): 63-102. doi: 10.1016/j.chemgeo.2003.11.003

Luo, G. M., Lai, X. L., Jiang, H. S., et al., 2006. Size varia-tion of the end Permian conodont Neogondolella at Meishan Section, Changxing, Zhejiang and its signifi-cance. Science in China (Ser. D), 49: 337-347. doi: 10.1007/s11430-006-0337-1

Luo, G. M., Lai, X. L., Shi, G. R., et al., 2008. Size variation of conodont elements of the Hindeodus-Isarcicella clade during the Permian-Triassic transition in South China and its implication for mass extinction. Palaeogeogra-phy, Palaeoclimatology, Palaeoecology, 264 (1-2): 176-187. doi: 10.1016/j.palaeo.2008.04.015

Moffett, J. W., 1990. Microbially mediated cerium oxidation in sea water. Nature, 345 (6274): 421-423. doi: 10.1038/345421a0

Pearce, N. J. G., Perkins, W. T., Westgate, J. A., et al., 1997. A compilation of new and published major and trace element data for NIST SRM 610and NIST SRM 612 glass reference materials. Geostandards Newslet-ter: The Journal of Geostandards and Geoanalysis, 21: 115-144. doi: 10.1111/j.1751-908X.1997.tb00538.x

Rampino, M. R., Prokoph, A., Adler, A., 2000. Tempo of the end-Permian event: High-resolution cyclostratigra-phy at the Permian-Triassic boundary. Geology, 28 (7): 643-646. doi: 10.1130/0091-7613(2000)28<643:TOTEEH>2.0.CO;2

Renne, P. R., Black, M. T., Zhang, Z. C., et al., 1995. Syn-chrony and causal relations between Permian-Triassic boundary crisis and Siberian flood volcanism. Science, 269 (5229): 1413-1416. doi: 10.1126/science.269.5229.1413

Reynard, B., Lecuyer, C., Grandjean, P., 1999. Crystal-chemical controls on rare-earth element concentrations in fossil biogenic apatites and implications for paleoen-vironmental reconstructions. Chemical Geology, 155 (3-4): 233-241. doi: 10.1016/S0009-2541(98)00169-7

Trotter, J. A., Eggins, S. M., 2006. Chemical systematics of conodont apatite determined by laser ablation ICPMS. Chemical Geology, 233 (3-4): 196-216. doi: 10.1016/j.chemgeo.2006.03.004

Veeh, H. H., 1982. Concordant ²³⁰Th and ²³¹Pa ages of ma-rine phosphorites. Earth Planet. Sci. Lett. , 57 (2): 278-284. doi: 10.1016/0012-821X(82)90150-9

Wang, Y., Cao, C. Q., 2004. Overviewthe research on mass ex-tinction during Paleozoic-Mesozoic transition of South Chi-na. In: Rong, J. Y., Fang, Z. J., eds., Mass extinction and recovery—Evidence from the Palaeozoic and Triassic of South China. China University of Science and Technology Press, Hefei, 749-772 (in Chinese).

Wignall, P. B., Hallam, A., 1993. Griesbachian (Earliest Tri-assic) palaeoenvironmental changes in the Salt range, Pakistan and Southeast China and their bearing on the Permo-Triassic mass extinction. Palaeogeography, Palaeoclimatology, Palaeoecology, 102 (3-4): 215-237. doi: 10.1016/0031-0182(93)90068-T

Wright, J., Schrader, H., Holser, W. T., 1987. Paleoredox variations in ancient oceans recorded by rare earth ele-ments infossil apatite. Geochimicaet Cosmochimica Ac-ta, 51 (3): 631-644. doi: 10.1016/0016-7037(87)90075-5

Wu, S. B., Li, Q., Wang, W. W., 1988. Characteristics of stratig-raphical andfaunal changes near the Permo-Triassic bound-ary in the Huayingshan area, Sichuan Province. Geoscience, 2 (3): 375-385 (in Chinese with English abstract).

Xie, S. C., Pancost, R. D., Yin, H. F., et al., 2005. Two epi-sodes of microbial change coupled with Permo-Triassic faunal mass extinction. Nature, 434 (7032): 494-497. doi: 10.1038/nature03396

Xu, D. Y., Yan, Z., 1993. Carbon isotope and iridium event markers near the Permian-Triassic boundaryinthe Mei-shan Section, Zhejiang Province, China. Palaeogeogra-phy, Palaeoclimatology, Palaeoecology, 104 (1-4): 171-176. doi: 10.1016/0031-0182(93)90128-6

Yin, H. F., Feng, Q, L., Tong, J. N., et al., 2007. Advances on the research of Permian-Triassic boundary and e-vents. Earth Science—Journal of China University of Geosciences, 32 (Suppl. ): 9-23 (in Chinese with Eng-lish abstract).

Yin, H. F., Lu, L. Q., 2006. A review on the global stratotype section and point of the Permian-Triassic boundary. Earth Science Frontiers, 13 (6): 257-267 (in Chinese with English abstract).

Yin, H. F., Huang, S. J., Zhang, K. X., et al., 1992. The effects of volcanismon the Permo-Triassic mass extinc-tionin South China. In: Sweet, W. C., Yang, Z., Dick-ins, J. M., et al., eds., Permo-Triassic events in the Eastern Tethys. Cambridge University Press, Cam-bridge, 169-174.

Yin, H. F., Tong, J. N., 1998. Multidisciplinary high-resolu-tion correlation of the Permian-Triassic boundary. Palaeogeography, Palaeoclimatology, Palaeoecology, 143 (4): 199-212. doi: 10.1016/S0031-0182(98)00111-4

Yin, H. F., Zhang, K. X., Tong, J. N., et al., 2001. The global stratotype section and point (GSSP) of the Per-mian-Triassic boundary. Episodes, 24 (2): 102-114. doi: 10.18814/epiiugs/2001/v24i2/004

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. 科学通报, 47 (4): 302-306. doi: 10.3321/j.issn:0023-074X.2002.04.014

方宗杰, 2004a. 二叠纪-三叠纪之交生物大灭绝的型式、全球生态系统的巨变及其起因. 见: 戎嘉余, 方宗杰. 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, 785-928.

方宗杰, 2004b. 华南二叠纪双壳类群灭绝型式的探讨. 见: 戎嘉余, 方宗杰. 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, 571-646.

黄咸雨, 焦丹, 鲁立强, 等, 2007. 二叠纪-三叠纪之交环境的不稳定性和生物危机的多阶段性: 浙江长兴微生物分子化石记录. 中国科学(D辑), 37 (5): 629-635.

罗根明, 赖旭龙, 江海水, 等, 2006. 浙江长兴煤山剖面二叠纪末牙形石Neogondolella大小变化及其意义. 中国科学(D辑), 36 (4): 316-325.

吴顺宝, 李庆, 王薇薇, 1988. 四川华莹山二叠纪与三叠纪之交沉积特征与动物群变化. 现代地质, 2 (3): 375-385.

殷鸿福, 冯庆来, 童金南, 等, 2007. 二叠系-三叠系界线及事件研究进展—中国地质大学研究组的报告. 地球科学——中国地质大学学报, 32 (增刊): 9-23.

殷鸿福, 鲁立强, 2006. 二叠系-三叠系界线全球层型剖面——回顾和进展. 地学前缘, 13 (6): 257-267. doi: 10.3321/j.issn:1005-2321.2006.06.029

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Trace Element Compositions in Conodont Phosphates Responses to Biotic Extinction Event: A Case Study for Main Act of Global Boundary Stratotype Section and Point of the Permian-Triassic

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