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    Volume 51 Issue 7
    Jul.  2026
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    Article Navigation >  Earth Science  > 2026  >  51(7): 2869-2893
    Hou Haihai, Zhao Ming'en, Shao Longyi, Liang Guodong, He Qian, Hu Bo, Fan Lele, 2026. Distribution of Global Paleowildfire Events and Controlling Factors from Late Triassic to Early Jurassic Based on Geological Big Data. Earth Science, 51(7): 2869-2893. doi: 10.3799/dqkx.2026.194
    Citation: Hou Haihai, Zhao Ming'en, Shao Longyi, Liang Guodong, He Qian, Hu Bo, Fan Lele, 2026. Distribution of Global Paleowildfire Events and Controlling Factors from Late Triassic to Early Jurassic Based on Geological Big Data. Earth Science, 51(7): 2869-2893. doi: 10.3799/dqkx.2026.194
    shu

    Distribution of Global Paleowildfire Events and Controlling Factors from Late Triassic to Early Jurassic Based on Geological Big Data

    doi: 10.3799/dqkx.2026.194
    • 1.

      School of Mining, Liaoning Technical University, Fuxin 123000, China

    • 2.

      College of Geoscience and Surveying Engineering, China University of Mining and Technology, Beijing 100083, China

    • Received Date: 2026-01-26
    • Publish Date: 2026-07-25
      Abstract
    • Terrestrial wildfires are among the important driving forces in the evolution of global ecosystems. Studying paleowildfire events and their control mechanisms during key periods in geological history helps reveal the intrinsic connections between climatic and environmental evolution and wildfire activity. A total of 268 paleowildfire records reported worldwide, including records of charcoal, inertinite, and pyrogenic polycyclic aromatic hydrocarbons, were analyzed for the interval from Late Triassic to Early Jurassic (237-174.7 Ma). The study reveals that the spatial distribution of paleowildfires from the Carnian of the Late Triassic to the Norian-Rhaetian boundary was concentrated in tropical and warm-temperate zones at low to mid-latitudes in the Northern Hemisphere, with only a small number of Carnian paleowildfires distributed in the warm-temperate zone of the Southern Hemisphere. From the Rhaetian to the Rhaetian-Hettangian boundary (the Triassic-Jurassic/T-J boundary), paleowildfires were uniformly distributed across multiple climatic belts at mid-latitudes in the Northern Hemisphere. Wildfires in the Early Jurassic were concentrated in the warm-temperate and northern tropical zones at mid-latitudes in the Northern Hemisphere. Global paleowildfire activity from the Late Triassic to the Early Jurassic was controlled by combined effects of pCO2 (10-6; atmospheric CO2 concentration) and pO2 (vol%; atmospheric O2 volume fraction), vegetation change, and major geological events. The volcanic activity of the Wrangellia Large Igneous Province (LIP) in the Early Late Triassic promoted a rapid rise in pCO2. This rise, together with flourishing vegetation and high pO2, collectively drove the high frequency of wildfires during the Carnian. After pCO2 peaked in the Early Norian, it continued to decline, and this decline, together with the decrease in pO2, suppressed wildfire activity during the Norian. Subsequently, volcanic activity associated with the Angayucham LIP and the Central Atlantic Magmatic Province (CAMP) sequentially promoted the long-term recovery in pCO2 across Triassic-Jurassic (T-J) boundary. During this period, the structure of vegetation communities remained relatively stable, which contributed to an increase in wildfire frequency at the Norian-Rhaetian boundary, during the Rhaetian, at the Rhaetian-Hettangian boundary, and during the Hettangian. Negative carbon-isotope excursions recorded in multiple representative T-J boundary sections worldwide are interpreted as responses to the high-frequency wildfire events at the Rhaetian-Hettangian boundary, which were mainly driven by CAMP volcanism. With the continued decline in pO2 and climatic cooling during the Sinemurian, wildfire frequency dropped sharply. In the middle and late stages of the Early Jurassic, pCO2 generally remained at a low level. Only the recovery of pO2 during the Toarcian resulted in a slightly higher number of wildfires than in the Pliensbachian, while wildfire frequency remained almost unchanged.

       

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