A regulatory role for phenol oxidase during decomposition in peatlands.
By C. Freeman, N. Ostle, N. Fenner, Hojeong Kang. 2004
460 citations recorded by the source corpus.
Subfields: Ecology, Environmental Chemistry
View Paper: https://www.semanticscholar.org/paper/a41649ac79306c3ae7463a8fcee7699f772eead4
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In Ecology
In Environmental Chemistry
Citations in the corpus
- Phenol oxidase, peroxidase and organic matter dynamics of soil (2010, background): “Thus phenol oxidase and peroxidase activities are especially critical to understanding potential responses to global climate change (Freeman et al., 1996, 2001, 2004).”
- Fungal laccases - occurrence and properties. (2006, background): “The burst of laccase activity can lead to the depletion of phenolic compounds that inhibit organic matter degradation by oxidative and hydrolytic enzymes (Freeman et al., 2004) and it can be assumed that the oxygen-regulated laccase activity plays an important role in carbon cycling in this environm”
- Algal regulation of extracellular enzyme activity in stream microbial communities associated with inert substrata and detritus (2007, background): “Freeman et al. (2004) observed that POA activity in peatlands can be O2 limited and that POA rates can be substantially increased when O2 is provided.”
- Microbial contributions to climate change through carbon cycle feedbacks (2008, background): “…effect of elevated temperature and atmospheric CO2 on microbial decomposition of peat was found to be greater than when these factors operated alone (Fenner et al., 2007a, b), creating an even stronger positive feedback on carbon loss from soil as DOC and respiration (Freeman et al., 2004b).”
- Soil enzyme activity: a brief history and biochemistry as a basis for appropriate interpretations and meta-analysis (2017, unknown): “…of soil enzymology is the attempt to mimic in situ conditions, particularly in terms of in situ pH or temperatures (as just a few of the examples Freeman et al. 2004; Drouillon and Merckx 2005; German et al. 2011; Peacock et al. 2015), by using incubation solutions that are unbuffered or…”
- Climate change feedbacks to microbial decomposition in boreal soils (2011, background): “Overall, these results suggest that decomposition of permafrost C is limited by low microbial activity, but high potential enzyme activity and an abundance of available C could result in rapid losses of soil C following permafrost thaw (Freeman et al. 2001, 2004).”