High-resolution SIMS oxygen isotope analysis on conodont apatite from South China and implications for the end-Permian mass extinction
文献类型：期刊论文
| 作者 | Chen, Jun1; Shen, Shu-zhong2; Li, Xian-hua3; Xu, Yi-gang1; Joachimski, Michael M.4; Bowring, Samuel A.5; Erwin, Douglas H.6; Yuan, Dong-xun2; Chen, Bo2; Zhang, Hua2 |
| 刊名 | PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
 |
| 出版日期 | 2016-04-15 |
| 卷号 | 448页码:26-38 |
| 关键词 | SIMS Oxygen isotope Conodont apatite South China Climate warming End-Permian mass extinction |
| DOI | 10.1016/j.palaeo.2015.11.025 |
| 文献子类 | Article |
| 英文摘要 | Understanding the interplay of climatic and biological events in deep time requires resolving the precise timing and pattern of paleotemperature changes and their temporal relationship with carbon cycle variations and biodiversity fluctuations. In situ oxygen isotope analyses of conodont apatite from South China enables us to reconstruct high-resolution seawater temperature records across the Permian-Triassic boundary (PTB) intervals in the upper slope (Meishan), lower slope (Shangsi), and carbonate platform (Daijiagou and Liangfengya) settings. Constrained by the latest high-precision geochronological dates and high-resolution conodont biozones, we can establish the temporal and spatial patterns of seawater temperature changes and assess their potential connections with the carbon cycle disruption and biodiversity decline. We find a rapid warming of similar to 10 degrees C during the latest Permian-earliest Triassic that postdated the onset of the negative shift in delta C-13(carb) by similar to 81 kyr (thousand years), the abrupt decline in delta C-13(carb) by similar to 32 kyr and the onset of mass extinction by similar to 23 kyr, which contradicts previous claims that the extreme temperature rise started immediately before or coincided with the onset of mass extinction. Our new evidence indicates that climate warming was most likely not a direct cause for the main pulse of the end-Permian mass extinction (EPME), but rather a later participant or a catalyst that increased the pace of the biodiversity decline. In addition, a prominent cooling is recorded in the earliest Changhsingian, with the main phase (a drop of similar to 8 degrees C in similar to 0.2 Ma) confined to the lower part of the Clarkina wangi zone and synchronous with the positive limb of the carbon isotope excursion (CIE) around the Wuchiapingian-Changhsingian boundary (WCB) in Meishan and Shangsi. Further long-term and high-resolution studies from other sections are needed to confirm the full contexts and underlying dynamics of the WCB "cooling event". (C) 2015 Elsevier B.V. All rights reserved. |
| WOS关键词 | LARGE IGNEOUS PROVINCES ; PALEOZOIC ICE-AGE ; TRIASSIC BOUNDARY ; BIOGENIC APATITES ; OCEAN ACIDIFICATION ; CHANGHSINGIAN STAGE ; STRATOTYPE SECTION ; SIBERIAN TRAPS ; CARBON-CYCLE ; POINT GSSP |
| WOS研究方向 | Physical Geography ; Geology ; Paleontology |
| 语种 | 英语 |
| WOS记录号 | WOS:000372676700003 |
| 资助机构 | National Natural Science Foundation of China(41290260 ; National Natural Science Foundation of China(41290260 ; National Basic Research Program of China(2011CB808900) ; National Basic Research Program of China(2011CB808900) ; State Key Laboratory of Isotope Geochemistry(SKLIG-QD-12-02) ; State Key Laboratory of Isotope Geochemistry(SKLIG-QD-12-02) ; State Key Laboratory of Palaeobiology and Stratigraphy(123111 ; State Key Laboratory of Palaeobiology and Stratigraphy(123111 ; National Science Foundation(EAR-0807475) ; National Science Foundation(EAR-0807475) ; 41203008) ; 41203008) ; 20131101) ; 20131101) ; National Natural Science Foundation of China(41290260 ; National Natural Science Foundation of China(41290260 ; National Basic Research Program of China(2011CB808900) ; National Basic Research Program of China(2011CB808900) ; State Key Laboratory of Isotope Geochemistry(SKLIG-QD-12-02) ; State Key Laboratory of Isotope Geochemistry(SKLIG-QD-12-02) ; State Key Laboratory of Palaeobiology and Stratigraphy(123111 ; State Key Laboratory of Palaeobiology and Stratigraphy(123111 ; National Science Foundation(EAR-0807475) ; National Science Foundation(EAR-0807475) ; 41203008) ; 41203008) ; 20131101) ; 20131101) |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/62038]  |
| 专题 | 地质与地球物理研究所_岩石圈演化国家重点实验室 |
| 作者单位 | 1.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, 511 Kehua St, Guangzhou 510640, Guangdong, Peoples R China 2.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, Nanjing 210008, Jiangsu, Peoples R China 3.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 4.Univ Erlangen Nurnberg, GeoZentrum Nordbayern, Schlossgarten 5, D-91054 Erlangen, Germany 5.MIT, Dept Earth Atmospher & Planetary Sci, 77 Massachusetts Ave, Cambridge, MA 02139 USA 6.Smithsonian Inst, Natl Museum Nat Hist, Dept Paleobiol, MRC 121, Washington, DC 20013 USA 7.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Key Lab Econ Stratig & Palaeogeog, Nanjing 210008, Jiangsu, Peoples R China 8.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Dept Invertebrate Palaeontol, Nanjing 210008, Jiangsu, Peoples R China |
| 推荐引用方式 GB/T 7714 | Chen, Jun,Shen, Shu-zhong,Li, Xian-hua,et al. High-resolution SIMS oxygen isotope analysis on conodont apatite from South China and implications for the end-Permian mass extinction[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2016,448:26-38. |
| APA | Chen, Jun.,Shen, Shu-zhong.,Li, Xian-hua.,Xu, Yi-gang.,Joachimski, Michael M..,...&Mu, Lin.(2016).High-resolution SIMS oxygen isotope analysis on conodont apatite from South China and implications for the end-Permian mass extinction.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,448,26-38. |
| MLA | Chen, Jun,et al."High-resolution SIMS oxygen isotope analysis on conodont apatite from South China and implications for the end-Permian mass extinction".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 448(2016):26-38. |
入库方式： OAI收割
来源：地质与地球物理研究所
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