Paleo-oil reservoir pyrolysis and gas release in the Yangtze Block imply an alternative mechanism for the Late Permian Crisis

被引:10
作者
Yang, Chengyu [1 ]
Li, Meijun [1 ,2 ]
Ni, Zhiyong [1 ]
Wang, Tieguan [1 ]
Qiu, Nansheng [1 ]
Fang, Ronghui [3 ,4 ]
Wen, Long [5 ]
机构
[1] China Univ Petr, Coll Geosci, State Key Lab Petr Resources & Prospecting, Beijing, Peoples R China
[2] Yangtze Univ, Coll Resources & Environm, Minist Educ, Key Lab Explorat Technol Oil & Gas Resources, Wuhan 430100, Hubei, Peoples R China
[3] China Geol Survey, Oil & Gas Survey, Beijing 100083, Peoples R China
[4] China Geol Survey, Key Lab Unconvent Petr Geol, Beijing 100083, Peoples R China
[5] PetroChina, Southwest Oil & Gas Field Co, Explorat & Dev Res Inst, Chengdu 610041, Sichuan, Peoples R China
关键词
Oil reservoir pyrolysis; Hydrothermal fluid; Emeishan Large Igneous Province; Gas release; Mass extinction; LARGE IGNEOUS PROVINCES; THERMOCHEMICAL SULFATE REDUCTION; HYDROTHERMAL DOLOMITE RESERVOIR; PLUME-LITHOSPHERE INTERACTION; SINIAN DENGYING FORMATION; CENTRAL SICHUAN BASIN; SOLID BITUMEN; SOURCE-ROCK; ORGANIC PETROLOGY; MASS EXTINCTION;
D O I
10.1016/j.gsf.2021.101324
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The causes of the global mass extinction that occurred around the Permian-Triassic boundary have been widely studied through the geological record and in various locations. The results show that volcanic activity was a key factor in initiating the crisis during the Late Permian. Compared to other thermal events triggered by volcanic activity, pyrolysis of petroleum in Pre-Permian reservoirs has rarely been suggested as a significant source of the greenhouse gases that caused the mass extinction. In this study, geochemical analysis is carried out of a huge paleo-oil reservoir in the Yangtze Block (YB), South China. The detection of mineral inclusions and pyrobitumens is evidence of rapid pyrolysis of accumulated oil in the Ediacaran reservoir. New evidence from hydrothermal minerals and the presence of domain mesophase in the pyrobitumen suggest that the pyrolysis process occurred abruptly and that greenhouse gases were rapidly released through venting pipes. The dating of such a complex geological event in this old and deeply buried reservoir is inevitably difficult and potentially unreliable. However, cross-validation of the multiple evidence sources, including hydrothermal minerals and domain mesophase, indicates that the rapid oil pyrolysis must have been driven by a major thermal event. Reconstruction of burial and thermal histories suggests that the thermal event was most likely to have been triggered by the Emeishan Large Igneous Province (ELIP), which was in a period of significant volcanic activity during the Late Permian. Massive volumes of gases, including methane, carbon dioxide, and possibly hydrogen sulfide, were released, causing a significant increase in greenhouse gases that may have contributed to global warming and the resulting mass extinction during the Late Permian Crisis (LPC). (c) 2021 China University of Geosciences (Beijing) and Peking University. Production and hosting by Elsevier B.V. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/ licenses/by-nc-nd/4.0/).
引用
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页数:14
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