Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/j.gloplacha.2020.103300 |
A possible link between the Carnian Pluvial Event, global carbon-cycle perturbation, and volcanism: New data from the Qinghai-Tibet Plateau | |
Fu, Xiugen; Wang, Jian; Wen, Huaguo; Wang, Zhongwei; Zeng, Shengqiang; Song, Chunyan; Chen, Wenbin; Wan, Youli | |
通讯作者 | Fu, XG |
来源期刊 | GLOBAL AND PLANETARY CHANGE |
ISSN | 0921-8181 |
EISSN | 1872-6364 |
出版年 | 2020 |
卷号 | 194 |
英文摘要 | The Carnian Pluvial Event (CPE) is recorded widely across the Tethys region. Here we present high-resolution carbonate (delta C-13(carb)) and organic (delta C-13(org)) carbon-isotope records and mineral data from the Boli La to lower Bagong formations in the Quemo Co area of the Qiangtang Basin, Qinghai-Tibet Plateau. In this studied section, a calcareous fine-grained sandstone bed that yields a detrital zircon maximum depositional age of 232.5 +/- 3.3 Ma, together with ammonoid species and bivalves, allows identification of the Carnian Stage. An intensification of siliciclastic supply and a large drop in calcite and illite is recorded in the Carnian section, suggesting a palaeoclimatic shift from arid to warm and humid during the CPE. A negative carbon-isotope excursion (CIE) in both delta C-13(org) and delta C-13(carb) is also reported, which could be explained by a global perturbation of the carbon cycle and the release of CO2 enriched in C-12. The magnitude of the negative CIE in the Quemo Co area displays a significant shift towards lighter values compared to other reported carbonate carbon-isotope values across the onset of the CPE. A combination of both volcanic emissions from the synchronous Wrangellia large igneous province and release of methane clathrate hydrate is the most likely explanation for the significant negative excursion in delta C-13. |
英文关键词 | Late Triassic Climatic event Carbon-isotope excursion Qiangtang Basin Eastern Tethys |
类型 | Article |
语种 | 英语 |
收录类别 | SCI-E |
WOS记录号 | WOS:000579858500013 |
WOS关键词 | QIANGTANG BASIN ; CLIMATIC-CHANGE ; ISOTOPE RECORD ; HUMID EPISODE ; BLACK SHALE ; STRATIGRAPHY ; CRISIS ; ZIRCON ; SOUTHERN ; ELEMENTS |
WOS类目 | Geography, Physical ; Geosciences, Multidisciplinary |
WOS研究方向 | Physical Geography ; Geology |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/326908 |
作者单位 | [Fu, Xiugen; Wang, Jian] Southwest Petr Univ, State Key Lab Oil & Gas Reservior Geol & Exploita, Chengdu 610050, Peoples R China; [Fu, Xiugen; Wang, Jian; Wang, Zhongwei] Southwest Petr Univ, Sch Geosci & Technol, Chengdu 610500, Peoples R China; [Wen, Huaguo] Chengdu Univ Technol, Inst Sedimentary Geol, Chengdu 610059, Peoples R China; [Zeng, Shengqiang; Song, Chunyan; Chen, Wenbin; Wan, Youli] China Geol Survey, Chengdu Ctr, Chengdu 610081, Peoples R China |
推荐引用方式 GB/T 7714 | Fu, Xiugen,Wang, Jian,Wen, Huaguo,et al. A possible link between the Carnian Pluvial Event, global carbon-cycle perturbation, and volcanism: New data from the Qinghai-Tibet Plateau[J],2020,194. |
APA | Fu, Xiugen.,Wang, Jian.,Wen, Huaguo.,Wang, Zhongwei.,Zeng, Shengqiang.,...&Wan, Youli.(2020).A possible link between the Carnian Pluvial Event, global carbon-cycle perturbation, and volcanism: New data from the Qinghai-Tibet Plateau.GLOBAL AND PLANETARY CHANGE,194. |
MLA | Fu, Xiugen,et al."A possible link between the Carnian Pluvial Event, global carbon-cycle perturbation, and volcanism: New data from the Qinghai-Tibet Plateau".GLOBAL AND PLANETARY CHANGE 194(2020). |
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