2014
DOI: 10.1016/j.geoderma.2014.07.001
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Recovery in fungal biomass is related to decrease in soil organic matter turnover time in a boreal fire chronosequence

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Cited by 64 publications
(82 citation statements)
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“…The samples were frozen at Ϫ180°C in liquid nitrogen within a few hours after collection and transported to the laboratory on dry ice for subsequent DNA isolation. The soil microbial biomass was estimated by measuring the ergosterol content from the samples collected from the humus layer (14).…”
Section: Methodsmentioning
confidence: 99%
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“…The samples were frozen at Ϫ180°C in liquid nitrogen within a few hours after collection and transported to the laboratory on dry ice for subsequent DNA isolation. The soil microbial biomass was estimated by measuring the ergosterol content from the samples collected from the humus layer (14).…”
Section: Methodsmentioning
confidence: 99%
“…Soil C and N contents were measured with an elemental analyzer (vario MAX CN elemental analyzer; Elementar Analysensysteme GmbH, Germany) after the soil samples were dried and passed through a 2-mm-pore-size mesh sieve. The soil temperature and water content were also measured at each sampling site, as previously described (14).…”
Section: Methodsmentioning
confidence: 99%
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“…During and after fires, significant changes take place in the forest ecosystems, including the soil. These changes include (i) a significant amount of biomass is combusted, and large amounts of carbon and nitrogen are released to the atmosphere in the form of carbon dioxide and other gases or particles (Harden et al, 2000;Andreae and Merlet, 2001;Kaiser et al, 2012;Konovalov et al, 2014;; (ii) fire alters the microbial community structure in the soil as well as the structure of the vegetation (Dooley and Treseder, 2012;Sun et al, 2015); (iii) fires determine the structure of the vegetation, succession dynamics and the fragmentation of forest cover, tree species composition, and the productivity of boreal forests (Gewehr et al, 2014), and (iv) fire is one of the crucial drivers controlling the dynamics of the carbon stock of boreal forests (Jonsson and Wardle, 2010;Köster et al, 2014).…”
Section: Natural Hazards Extreme Weather and Fire Occurrencementioning
confidence: 99%
“…The total C storage of the soil is 7 kg m -2 ) and it has been formed during the last 7000 years. Frequent forest fires have an influence on soil C recovery and turnover time (Köster et al, 2014) and the last occasion the SMEAR II forest site was burned was in 1962 when the cutting residues were slash burned on site.…”
Section: Measurement Sitementioning
confidence: 99%