Logo image
Burning of forest materials under late Paleozoic high atmospheric oxygen levels
Journal article   Peer reviewed

Burning of forest materials under late Paleozoic high atmospheric oxygen levels

R.A. Wildman, L.J. Hickey, M.B. Dickinson, R.A. Berner, J.M. Robinson, M. Dietrich, R.H. Essenhigh and C.B. Wildman
Geology, Vol.32(5), pp.457-460
2004
url
Link to Published Version *Subscription may be requiredView
url
Free to Read *No subscription requiredView

Abstract

Theoretical models suggest that atmospheric oxygen reached concentrations as high as 35% O2 during the past 550 m.y. Previous burning experiments using strips of paper have challenged this idea, concluding that ancient wildfires would have decimated plant life if O2 significantly exceeded its present level of 21 %. New thermochemistry and flame-spread experiments using natural fuels contradict these results and indicate that sustained burning of forest fuels at moisture contents common to living plants does not occur between 21% and 35% O2. Therefore, the fires under atmospheres with high oxygen concentrations would not have prevented the persistence of plant communities. Times of high O2 also agree with observations of concurrent fire-resistant plant morphology, large insects, and high concentrations of fossil charcoal.

Details

UN Sustainable Development Goals (SDGs)

This output has contributed to the advancement of the following goals:

#13 Climate Action
#14 Life Below Water
#15 Life on Land

Source: InCites

Metrics

InCites Highlights

These are selected metrics from InCites Benchmarking & Analytics tool, related to this output

Collaboration types
Domestic collaboration
International collaboration
Citation topics
8 Earth Sciences
8.8 Geochemistry, Geophysics & Geology
8.8.550 Paleoecology and Biogeography
Web Of Science research areas
Geology
ESI research areas
Geosciences
Logo image