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Reconstructing grassland fire history using sedimentary charcoal: Considering count, size and shape
Berangere A Leys1, Julie L Commerford1, Kendra K McLauchlan1
1Department of Geography, Kansas State University, Manhattan, Kansas, United States of America.
Plos One
|April 28, 2017
Summary
Reconstructing grassland fire history is improved by analyzing charcoal particle size and shape. A smaller mesh size and width-to-length ratio help identify fire regimes and fuel types in these ecosystems.
Area of Science:
- Earth System Science
- Paleoecology
- Fire Ecology
Background:
- Grassland fires constitute 80% of annual fire activity, yet reconstructing past fire regimes is challenging due to difficulties in interpreting charcoal signals.
- Accurate quantification of past grassland fire regimes requires assessing charcoal count and shape.
Purpose of the Study:
- To improve reconstructions of grassland fire regimes by evaluating charcoal count and shape as proxies.
- To test the relevance of charcoal count by examining factors influencing it, including fire regime components, vegetation, and climate.
- To assess the utility of charcoal width-to-length (W:L) ratio as a proxy for fuel types in grassland environments.
Main Methods:
- Quantified charcoal particle count in 51 sediment samples from Great Plains ponds.
- Examined 13 factors influencing charcoal count, such as fire frequency, area burned, fire season, vegetation, and climate variables.
- Quantified the W:L ratio of charcoal particles and compared it with vegetation cover and pollen assemblages.
Main Results:
- Grassland fire charcoal particles are smaller than forest fire particles; a 60μm mesh is recommended over 120μm for grasslands.
- A W:L ratio of ≤0.5 indicates specific fuel types when grassland vegetation exceeds 40%.
- The area burned within 1060m of depositional sites significantly correlated with charcoal count and area.
Conclusions:
- Charcoal analysis, with adjusted mesh sizes and W:L ratio interpretation, provides a reliable method for reconstructing grassland fire regimes.
- Changes in charcoal count and area over time reflect alterations in the area burned.
- Long-term charcoal records can characterize grassland fire regimes, incorporating human and climatic influences.

