气候变化领域集成服务门户(CCPortal): Wildfires and deforestation during the Permian–Triassic transition in the southern Junggar Basin, Northwest China

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DOI	10.1016/j.earscirev.2021.103670
	Wildfires and deforestation during the Permian–Triassic transition in the southern Junggar Basin, Northwest China
	Cai Y.-F.; Zhang H.; Cao C.-Q.; Zheng Q.-F.; Jin C.-F.; Shen S.-Z.
发表日期	2021
ISSN	0012-8354
卷号	218
英文摘要	Despite a continuous increase in fossil charcoal records from Late Palaeozoic deposits, which are used as direct evidence for palaeo-wildfires, detailed studies on the charcoal particles are still rare. To investigate the relationship between wildfire activities and the evolution of the terrestrial ecosystem at the end of the Permian, we report on the charcoal recovered from the classic non-marine Permian–Triassic Dalongkou section in Jimsar, Xinjiang Uygur Autonomous Region, Northwest China. Allochthonous and parautochthonous charcoals, identified by both macroscopic and microscopic morphological techniques, were collected from several stratigraphic horizons. These charcoals were classified into 11 categories (which do not represent the taxonomic group) according to their anatomical characteristics and gross morphology. The reflectance values of the charcoals indicate that surface fires were dominant throughout the sequence, with fire regime changing in a distinct interval. The distribution and abundance of all categories and the reflectance of the charcoals suggest that the intensity of wildfires increased in the upper part of the Guodikeng Formation. This trend coincides with the Hg/TOC peaks and a conspicuous excursion in the organic carbon isotope (δ13Corg) values, which may indicate volcanic activities and the disturbance of the carbon cycle that occurred during the Permian–Triassic transition. It is reasonable to infer that the end-Permian mass extinction (EPME) is located at the intensive wildfire interval. The reduction in spore pollen and the decrease in charcoal reflectance hint at a vegetational impoverishment that occurred after this interval. We proposed that increased wildfires, promoted by dry climate conditions and volcanism, aggravated the collapse of the forest ecosystem during the latest Permian. © 2021 Elsevier B.V.
英文关键词	Charcoal; Dalongkou section; Permian–Triassic; Reflectance; Terrestrial; δ13Corg
语种	英语
scopus关键词	carbon cycle; carbon isotope; charcoal; deforestation; organic carbon; Permian-Triassic boundary; surface reflectance; terrestrial ecosystem; volcanism; wildfire; China; Junggar Basin; Xinjiang Uygur
来源期刊	EARTH-SCIENCE REVIEWS
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/209283
作者单位	State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology and Center for Excellence in Life and Paleoenvironment, Chinese Academy of Sciences, 39 East Beijing Road, Nanjing, 210008, China; College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing, 100049, China; State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, 163 Xianlin Avenue, Nanjing, Jiangsu 210023, China
推荐引用方式 GB/T 7714	Cai Y.-F.,Zhang H.,Cao C.-Q.,等. Wildfires and deforestation during the Permian–Triassic transition in the southern Junggar Basin, Northwest China[J],2021,218.
APA	Cai Y.-F.,Zhang H.,Cao C.-Q.,Zheng Q.-F.,Jin C.-F.,&Shen S.-Z..(2021).Wildfires and deforestation during the Permian–Triassic transition in the southern Junggar Basin, Northwest China.EARTH-SCIENCE REVIEWS,218.
MLA	Cai Y.-F.,et al."Wildfires and deforestation during the Permian–Triassic transition in the southern Junggar Basin, Northwest China".EARTH-SCIENCE REVIEWS 218(2021).