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Recent burning of boreal forests exceeds fire regime limits of the past 10,000 years

2013· article· en· 431 citations· W2002507842 on OpenAlex· 10.1073/pnas.1305069110

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About CanadaIts subject is Canada, wherever its authors sit.

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Opus teacher head0.021
GPT teacher head0.253
Teacher spread
0.232 · how far apart the two teachers sit on this one work
Validation status
score_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Abstract

Wildfire activity in boreal forests is anticipated to increase dramatically, with far-reaching ecological and socioeconomic consequences. Paleorecords are indispensible for elucidating boreal fire regime dynamics under changing climate, because fire return intervals and successional cycles in these ecosystems occur over decadal to centennial timescales. We present charcoal records from 14 lakes in the Yukon Flats of interior Alaska, one of the most flammable ecoregions of the boreal forest biome, to infer causes and consequences of fire regime change over the past 10,000 y. Strong correspondence between charcoal-inferred and observational fire records shows the fidelity of sedimentary charcoal records as archives of past fire regimes. Fire frequency and area burned increased ∼6,000-3,000 y ago, probably as a result of elevated landscape flammability associated with increased Picea mariana in the regional vegetation. During the Medieval Climate Anomaly (MCA; ∼1,000-500 cal B.P.), the period most similar to recent decades, warm and dry climatic conditions resulted in peak biomass burning, but severe fires favored less-flammable deciduous vegetation, such that fire frequency remained relatively stationary. These results suggest that boreal forests can sustain high-severity fire regimes for centuries under warm and dry conditions, with vegetation feedbacks modulating climate-fire linkages. The apparent limit to MCA burning has been surpassed by the regional fire regime of recent decades, which is characterized by exceptionally high fire frequency and biomass burning. This extreme combination suggests a transition to a unique regime of unprecedented fire activity. However, vegetation dynamics similar to feedbacks that occurred during the MCA may stabilize the fire regime, despite additional warming.

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The record

Venue
Proceedings of the National Academy of Sciences
Topic
Fire effects on ecosystems
Field
Environmental Science
Canadian institutions
Funders
University of Illinois at Urbana-ChampaignNational Science Foundation
Keywords
Fire regimeTaigaBorealVegetation (pathology)Environmental scienceFire ecologyBiomeFlammabilityClimate changeBoreal ecosystemCharcoalEcologyClimatologyPhysical geographyDisturbance (geology)EcosystemGeographyGeologyForestry
Has abstract in OpenAlex
yes