Arid
DOI10.1016/j.chemgeo.2020.119764
Continental records of organic carbon isotopic composition (delta C-13(org)), weathering, paleoclimate and wildfire linked to the End-Permian Mass Extinction
Lu, Jing; Zhang, Peixin; Yang, Minfang; Shao, Longyi; Hilton, Jason
通讯作者Lu, J
来源期刊CHEMICAL GEOLOGY
ISSN0009-2541
EISSN1872-6836
出版年2020
卷号558
英文摘要The late Permian was the acme of Pangea assembly, with collision and subduction of global plates accompanied by major changes in atmospheric composition, paleoclimates and paleoenvironments of the Earth's surface system. These events are extensively recorded in marine successions from the Tethys, but much less are known from continental successions that typically lack high-resolution stratigraphic control. In order to reveal these fluctuations in terrestrial strata and their relationship with the End-Permian Mass Extinction (EPME), we investigate continental delta C-13(org), mercury and nickel concentrations, wildfire, and climate change proxies from the late Permian Changhsingian stage to Early Triassic Induan stage in the Yuzhou coalfield in the North China Plate (NCP). Results show two negative organic carbon isotope excursions (CIE) within the Changhsingian aged Sunjiagou Formation, the first (CIE-I, 2.2 parts per thousand) during mid-Changhsingian and a second, larger, excursion (CIE-II, 2.7 parts per thousand) near the end of the Changhsingian that coincides with the peaks in the Chemical Index of Alteration (CIA) value and extinction of plant species. We infer CIE-II to be the global negative excursion of delta C-13(org) associated with the EPME. Arid climates prevailed in the study area from the Changhsingian to the early Induan inferred from the low kaolinite contents and weak continental weathering, except for two short-duration episodes with higher humidity that correspond with CIE-I and CIE-II. Extremely high fusinite content ((x) over bar = 63.1%) and its increasing abundance through the Changhsingian indicates that frequent wildfires may have been a direct cause for both the destruction of terrestrial vegetation ecosystems and the rapid decline of terrestrial biodiversity at the EPME. We consider that terrestrial ecosystems may have played an important role in the extinction of marine communities at the EPME. This represents the first time the EMPE has been demonstrated in the NCP based on combined evidence from negative carbon isotope excursion, concurrent weathering trends, Ni/Al ratio and biotic extinctions, representing an important step in accurately identifying and correlating the EPME in continental settings from the NCP.
英文关键词Terrestrial strata Organic carbon isotope composition Weathering Palaeoclimate Wildfire End-Permian Mass Extinction North China Plate
类型Article
语种英语
开放获取类型hybrid, Green Submitted
收录类别SCI-E
WOS记录号WOS:000599667400004
WOS关键词TRIASSIC BOUNDARY ; NORTH CHINA ; CRISIS ; ANOXIA ; PRODUCTIVITY ; CLIMATE ; OCEAN ; PROVINCES ; TECTONICS ; EVOLUTION
WOS类目Geochemistry & Geophysics
WOS研究方向Geochemistry & Geophysics
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/327905
作者单位[Lu, Jing; Zhang, Peixin; Shao, Longyi] China Univ Min & Technol, Coll Geosci & Surveying Engn, State Key Lab Coal Resources & Safe Min, Beijing 100083, Peoples R China; [Yang, Minfang] PetroChina, Petr Explorat & Dev Res Inst, Beijing 100083, Peoples R China; [Hilton, Jason] Univ Birmingham, Sch Geog Earth & Environm Sci, Birmingham B15 2TT, W Midlands, England
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Lu, Jing,Zhang, Peixin,Yang, Minfang,et al. Continental records of organic carbon isotopic composition (delta C-13(org)), weathering, paleoclimate and wildfire linked to the End-Permian Mass Extinction[J],2020,558.
APA Lu, Jing,Zhang, Peixin,Yang, Minfang,Shao, Longyi,&Hilton, Jason.(2020).Continental records of organic carbon isotopic composition (delta C-13(org)), weathering, paleoclimate and wildfire linked to the End-Permian Mass Extinction.CHEMICAL GEOLOGY,558.
MLA Lu, Jing,et al."Continental records of organic carbon isotopic composition (delta C-13(org)), weathering, paleoclimate and wildfire linked to the End-Permian Mass Extinction".CHEMICAL GEOLOGY 558(2020).
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