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Organic geochemistry evidence for wildfire and elevated pO2 at the Frasnian–Famennian boundary

Liu, Zeyang; Tian, Hui; Selby, David; Hu, Jianfang; Over, D. Jeffrey

Organic geochemistry evidence for wildfire and elevated pO2 at the Frasnian–Famennian boundary Thumbnail


Authors

Zeyang Liu

Hui Tian

Jianfang Hu

D. Jeffrey Over



Abstract

The Devonian experienced radiations of plants and animals, as well as a major mass extinction event during the Frasnian–Famennian (Fsingle bondF) interval. Proposed triggers have been linked to volcanism, extraterrestrial impact, sea-level fluctuations, and climate cooling, etc. However, the nature of the wildfires and its role in the biotic evolution have been rarely investigated for the Fsingle bondF interval. Here, we report organic geochemistry proxies (e.g., polycyclic aromatic hydrocarbons, PAHs) in three sections from New York (USA) to further investigate the wildfire activity and its potential link with the environmental and biotic perturbations around the Fsingle bondF interval. The studied intervals are dominated by three-ring PAHs which display an increasing abundance stratigraphically towards the Fsingle bondF boundary (FFB). An increase of 6-ring over 3-ring PAHs across the FFB is also observed for the studied sections, indicating elevated burning temperature. Additionally, slightly increased plant wax abundance and average chain length values and relatively constant Pr/Ph ratios are observed. Collectively, these results propose an increased burning frequency over the Fsingle bondF interval caused by elevated pO2 level, rather than a change in aridity. Terrestrial input only slightly increased across the FFB, and there is limited evidence for ocean anoxia. This correlates with the hypothesis that pCO2 drawdown and climate cooling could have been a driving mechanism of the Fsingle bondF biocrisis.

Citation

Liu, Z., Tian, H., Selby, D., Hu, J., & Over, D. J. (2022). Organic geochemistry evidence for wildfire and elevated pO2 at the Frasnian–Famennian boundary. Global and Planetary Change, 216, Article 103904. https://doi.org/10.1016/j.gloplacha.2022.103904

Journal Article Type Article
Acceptance Date Jul 28, 2022
Online Publication Date Jul 31, 2022
Publication Date 2022-09
Deposit Date Aug 18, 2022
Publicly Available Date Aug 1, 2023
Journal Global and Planetary Change
Print ISSN 0921-8181
Electronic ISSN 1872-6364
Publisher Elsevier
Peer Reviewed Peer Reviewed
Volume 216
Article Number 103904
DOI https://doi.org/10.1016/j.gloplacha.2022.103904
Public URL https://durham-repository.worktribe.com/output/1194146

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