Repeated Wildfires in the Middle Jurassic Xishanyao Formation(Aalenian and Bajocian Ages) in Northwestern China  

作　　者：HOU Haihai SHAO Longyi LIANG Guodong TANG Yue ZHANG Huajie ZHANG Jiaqiang 

机构地区：[1]College of Mining,Liaoning Technical University,Fuxin,Liaoning 123000,China [2]College of Geoscience and Surveying Engineering,China University of Mining and Technology,Beijing 100083,China [3]Oil&Gas Resource Survey Center,China Geological Survey,Ministry of Land and Resource,Beijing 100029,China

出　　处：《Acta Geologica Sinica(English Edition)》2022年第5期1752-1763,共12页地质学报（英文版）

基　　金：supported by the National Natural Science Foundation of China (41572090;42102223);China Postdoctoral Science Foundation (2021M693844;2022T150284);the China Geological Survey Project (DD20160204-3);the discipline innovation team of Liaoning Technical University (LNTU20TD-05;LNTU20TD-14)。

摘　　要：The coal-bearing strata in the southern Junggar Basin in northwestern China have recently attracted the attention of coal geologists. Its abundance of coal resources is of great interest as there is a potential of unlocking details about the palaeoclimatic information. Coal deposits have the capacity to record wildfire events, even those with inefficient combustions. To characterize wildfire events and palaeoclimatic history of the Middle Jurassic Xishanyao Formation(Aalenian and Bajocian ages), 22 coal samples from borehole cores and coal mines in the southern Junggar Basin were collected and their macerals were analyzed. The results indicated that fusinite and semi-fusinite were the dominant components of inertinite with proportions of 35.27% and 54.67%, respectively. The presence of inertinite is an indicator that wildfires occurred at the time of peat land development, and the widespread occurrence suggests large scale wildfires during the Middle Jurassic. This study proposes a new parameter for the evaluation of wildfire features by combining burning frequency and burning temperature. The comprehensive evaluation index(CEI) was influenced by the lacustrine basin level and ancient plant types from a sequence framework. During the Middle Jurassic, most wildfires were surface fires with low level and ground fire with high level. High oxygen levels were estimated in the lower, middle, and upper members of the Xishanyao Formation with corresponding to 26.78%, 24.55%, and 23.55%, respectively. The high oxygen levels would be the primary cause of repeated wildfires in the Middle Jurassic. These results are helpful for understanding palaeoclimatic changes in the Middle Jurassic.

关 键 词：WILDFIRE charcoal Middle Jurassic comprehensive evaluation index northwestern China 

分 类 号：P534.52[天文地球—古生物学与地层学]