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The Role of Paleofire in Boreal and Other Cool-Coniferous Forests

  • Chapter
Fire in Ecosystems of Boreal Eurasia

Part of the book series: Forestry Sciences ((FOSC,volume 48))

Abstract

Two qualities distinguish the paleo record of fire in boreal regions. First is its highly fragmentary nature in light of the importance of boreal forests for carbon storage and emissions to the atmosphere. One might expect boreal forests to be a focus of research on impacts of temperature change and biospheric feedbacks due to C release. Fire can have effects on the C balance of individual stands that persist for decades in boreal regions (Van Cleve and Viereck 1981). Combustion-produced elemental (graphitic) C can have several important environmental impacts, influencing climate (Shaw 1982; Rosen et al. 1984; Ch’ylek et al. 1984; Penner et al. 1991), air quality (Sandberg et al. 1979), human health (Laflamme and Hites 1978), and the concentrations of greenhouse gases in the atmosphere (Seiler and Crutzen 1980; Crutzen and Andreae 1990; Crutzen and Goldammer 1993). Stratigraphic records of several important combustion products (e.g. charcoal, fly ash, reduced organic tracers) exist from some regions, but there is a conspicous lack of synthesis needed to establish baseline (i.e. pre-industrial) biomass burning emissions (Malingreau et al. 1993). Such records are particularly scarce in boreal regions (Clark and Robinson 1993).

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Clark, J.S., Richard, P.J.H. (1996). The Role of Paleofire in Boreal and Other Cool-Coniferous Forests. In: Goldammer, J.G., Furyaev, V.V. (eds) Fire in Ecosystems of Boreal Eurasia. Forestry Sciences, vol 48. Springer, Dordrecht. https://doi.org/10.1007/978-94-015-8737-2_5

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