1994
DOI: 10.1007/bf00418669
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Effect of extracellular-enzyme activities on solubilization rate of soil organic nitrogen

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Cited by 140 publications
(53 citation statements)
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“…The production of extracellular hydrolytic enzymes by microorganisms is a primary mechanism for the decomposition of soil organic matter. These enzymes break down complex organic molecules releasing smaller molecules into the environment which can be assimilated and mineralized (Asmar et al 1994;Madigan et al 2003). The availability of different organic substrates regulates the production of these hydrolytic enzymes (Velasco-Ayuso et al 2011).…”
Section: Introductionmentioning
confidence: 99%
See 1 more Smart Citation
“…The production of extracellular hydrolytic enzymes by microorganisms is a primary mechanism for the decomposition of soil organic matter. These enzymes break down complex organic molecules releasing smaller molecules into the environment which can be assimilated and mineralized (Asmar et al 1994;Madigan et al 2003). The availability of different organic substrates regulates the production of these hydrolytic enzymes (Velasco-Ayuso et al 2011).…”
Section: Introductionmentioning
confidence: 99%
“…The availability of different organic substrates regulates the production of these hydrolytic enzymes (Velasco-Ayuso et al 2011). The activity of extracellular enzymes represents the rate-limiting step in processing soil organic matter and constitutes a direct indicator of microbial production (Asmar et al 1994;Chróst 1992;Conant et al 2011;Velasco-Ayuso et al 2011). Extracellular enzyme activity is commonly used to assess the functional capacity of microbial communities (Allison and Treseder 2008).…”
Section: Introductionmentioning
confidence: 99%
“…To gain access to C, microbes synthesize extracellular enzymes that decompose particulate and mineral associated organic matter (Asmar et al 1994;Burns et al 2002;Sinsabaugh and Moorhead 1994). In this way, extracellular enzymes are considered the proximal drivers of decomposition and are important for the stabilization of soil organic matter (Six et al 2006).…”
Section: Introductionmentioning
confidence: 99%
“…First, priming may occur when microorganisms become nutrient-limited during the degradation of new labile C and co-metabolize pre-existing soil organic matter to meet their nutrient demands, leading to soil C being mineralized and released as 'primed' CO 2 (Blagodatskaya and Kuzyakov 2008). Supporting evidence for this mechanism is provided by laboratory experiments on temperate soils, which measured increased activity of organic nitrogen (N)-degrading enzymes during priming (Asmar et al 1994) and a reduction in priming when N was added with labile C, due to a switch from soil C to added labile C as the preferred substrate ('preferential substrate utilization'; Hagedorn et al 2003;Blagodatskaya et al 2007). …”
Section: Introductionmentioning
confidence: 99%