11 000 years of fire history and climate in the mountain hemlock rain forests of southwestern British Columbia based on sedimentary charcoal

By D. Hallett, D. Lepofsky, R. Mathewes, Ken Lertzman. 2003

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Did climatic seasonality control late Quaternary artiodactyl densities in western North America (2008, background): “…Whitlock and Bartlein, 1993; Anderson and Smith, 1994; Long et al., 1998; Millspaugh et al., 2000; Mohr et al., 2000; Doerner and Carrara, 2001; Barron et al., 2003; Brunelle and Anderson, 2003; Hallett et al., 2003; Gavin et al., 2003; Strong and Hills, 2003; West, 2004; Minckley et al., 2007).”
Documenting ancient plant management in the northwest of North America 1 (2008, background): “The recent description of the Fraser Valley Fire Period (Hallett et al. 2003) and its cultural correlate, the Marpole Phase (Lepofsky et al.”
An 1800-year record of the spatial and temporal distribution of fire from the west coast of Vancouver Island, Canada (2003, methodology): “A similar study that compared soil-charcoal and lake sediment records from subalpine forest in southeast British Columbia found a strong correlation between large charcoal peaks and fires within 300 m of the lake (Hallett et al. 2003).”