The reconstruction of burned area and fire severity using charcoal from boreal lake sediments

Although lacustrine sedimentary charcoal has long been used to infer paleofires, their quantitative reconstructions require improvements of the calibration of their links with fire regimes (i.e. occurrence, area, and severity) and the taphonomic processes that affect charcoal particles between the p...

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Bibliographic Details
Published in:	Holocene (Sevenoaks) Vol. 30; no. 10; pp. 1400 - 1409
Main Authors:	Hennebelle, Andy, Aleman, Julie C, Ali, Adam A, Bergeron, Yves, Carcaillet, Christopher, Grondin, Pierre, Landry, Josianne, Blarquez, Olivier
Format:	Journal Article
Language:	English
Published:	London, England SAGE Publications 01-10-2020 Sage Publications Ltd London: Sage
Subjects:	Biodiversity and Ecology Boreal forests Calibration Charcoal Deposition Environmental Sciences Fires Lake deposits Lake sediments Lakes Landsat Landsat satellites Remote sensing Satellite imagery Sediment Sediments Surface area Taphonomy Transport severity taphonomy forest dNBR fire charcoal trap calibration lake
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Summary:	Although lacustrine sedimentary charcoal has long been used to infer paleofires, their quantitative reconstructions require improvements of the calibration of their links with fire regimes (i.e. occurrence, area, and severity) and the taphonomic processes that affect charcoal particles between the production and the deposition in lake sediments. Charcoal particles >150 µm were monitored yearly from 2011 to 2016 using traps submerged in seven head lakes situated in flat-to-rolling boreal forest landscapes in eastern Canada. The burned area was measured, and the above-ground fire severity was assessed using the differentiated normalized burn ratio (dNBR) index, derived from LANDSAT images, and measurements taken within zones radiating 3, 15, and 30 km from the lakes. In order to evaluate potential lag effects in the charcoal record, fire metrics were assessed for the year of recorded charcoal recording (lag 0) and up to 5 years before charcoal deposition (lag 5). A total of 92 variables were generated and sorted using a Random Forest-based methodology. The most explanatory variables for annual charcoal particle presence, expressed as the median surface area, were selected. Results show that, temporally, sedimentary charcoal accurately recorded fire events without a temporal lag; spatially, fires were recorded up to 30 km from the lakes. Selected variables highlighted the importance of burned area and fire severity in explaining lacustrine charcoal. The charcoal influx was thus driven by fire area and severity during the production process. The dispersion process of particles resulted mostly of wind transportation within the regional (<30 km) source area. Overall, charcoal median surface area represents a reliable proxy for reconstructing past burned areas and fire severities.
ISSN:	0959-6836 1477-0911
DOI:	10.1177/0959683620932979