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Long-Term Fire Regime Estimated from Soil Charcoal in Coastal Temperate Rainforests Ecology and Society
Lertzman, Ken; Simon Fraser University; lertzman@sfu.ca; Gavin, Daniel; Department of Plant Biology, University of Illinois, Urbana, IL 61801, USA; dgavin@life.uiuc.edu; Hallett, Douglas; Center for Environmental Sciences & Quaternary Sciences Program, Northern Arizon; Douglas.Hallett@NAU.EDU; Brubaker, Linda; College of Forest Resources, University of Washington, Seattle, WA 98195, USA; lbru@u.washington.edu; Lepofsky, Dana; Simon Fraser University; dlepofsk@sfu.ca; Mathewes, Rolf; Department of Biological Sciences, Simon Fraser University; mathewes@sfu.ca.
Coastal temperate rainforests from southeast Alaska through to southern Oregon are ecologically distinct from forests of neighboring regions, which have a drier, or more continental, climate and disturbance regimes dominated by fires. The long-term role of fire remains one of the key outstanding sources of uncertainty in the historical dynamics of the wetter and less seasonal forests that dominate the northerly two thirds of the rainforest region in British Columbia and Alaska. Here, we describe the long-term fire regime in two forests on the south coast of British Columbia by means of 244 AMS radiocarbon dates of charcoal buried in forest soils. In both forests, some sites have experienced no fire over the last 6000 years and many other sites have...
Tipo: Peer-Reviewed Reports Palavras-chave: Clayoquot Sound; Fraser Valley; Coastal temperate rainforests; Fire intervals; Long-term fire regime; Soil carbon storage; Soil charcoal; Sub-alpine forest; Time-since-fire.
Ano: 2002
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Extreme temporal interpolation of sparse data is not a sufficient basis to substantiate a claim to have uncovered Pleistocene forest microrefugia ArchiMer
Huntley, Brian.
Tipo: Text Palavras-chave: Fagus sylvatica (beech); Heinrich Events 1 and 2; Landes de Gascogne; Last glacial maximum; Last glacial stage; Late Pleniglacial; Soil charcoal.
Ano: 2014 URL: https://archimer.ifremer.fr/doc/00289/40065/39263.pdf
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Relationship between soil oxidizable carbon and physical, chemical and mineralogical properties of umbric ferralsols Rev. Bras. Ciênc. Solo
Marques,Flávio Adriano; Calegari,Márcia Regina; Vidal-Torrado,Pablo; Buurman,Peter.
The occurrence of Umbric Ferralsols with thick umbric epipedons (> 100 cm thickness) in humid Tropical and Subtropical areas is a paradox since the processes of organic matter decomposition in these environments are very efficient. Nevertheless, this soil type has been reported in areas in the Southeast and South of Brazil, and at some places in the Northeast. Aspects of the genesis and paleoenvironmental significance of these Ferralsols still need a better understanding. The processes that made the umbric horizons so thick and dark and contributed to the preservation of organic carbon (OC) at considerable depths in these soils are of special interest. In this study, eight Ferralsols with a thick umbric horizon (UF) under different vegetation types...
Tipo: Info:eu-repo/semantics/article Palavras-chave: Ferralsols; Tropical soils; Soil total carbon; Soil organic carbon; Pyrogenic carbon; Soil charcoal; Umbric epipedon.
Ano: 2011 URL: http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0100-06832011000100003
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