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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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Cambios en el carbón orgánico del suelo en la cuenca superior del río Heihe, China Phyton
Qin,YY; Qi,F; Holden,NM; Cao,JJ.
The Heihe River Basin is a globally significant carbon pool, but its soil organic carbon dynamics is poorly understood. Soil samples taken between 2500 m and 4100 m revealed that the majority (>75%) of soil organic carbon was from 0-40 cm. It showed a negative relationship with pH and soil bulk density, and a positive relationship with altitude and soil water content, respectively. From 2005 to 2011, soil carbon content in the upper catchment decreased from 93 g/kg to 53 g/kg. These results suggest that policies should aim to reduce carbon loss by transferring it from the top- to the sub-soil.
Tipo: Info:eu-repo/semantics/article Palavras-chave: Soil properties; Soil carbon content; Soil carbon storage; Qilian Mountains.
Ano: 2016 URL: http://www.scielo.org.ar/scielo.php?script=sci_arttext&pid=S1851-56572016000100020
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