Short communication Reciprocal transfer of carbon and nitrogen by decomposer fungi at the soil -litter interface
By Serita Frey, Johan Six. 2003
289 citations recorded by the source corpus.
Subfields: Insect Science, Plant Science, Soil Science
View Paper: https://www.semanticscholar.org/paper/4dc4a2c0fa0da9ef93f7de1a216179ebfddc6ea8
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Citations in the corpus
- Effects of straw amendment and moisture on microbial communities in Chinese fluvo-aquic soil (2014, background): “…and polyphenols) organic materials by producing a variety of extracellular depolymerizing enzymes (Swift et al. 1979) and their ability to explore soil space for nutrient acquisition and reallocate energy and nutrients at the soil-straw interface through their filaments (Frey et al. 2000, 2003).”
- Nitrogen transfer between decomposing leaves of different N status (2007, background): “Fungi are capable of translocating N relatively long distances and their occurrence and characteristics could dramatically affect the amounts and distances that N is transferred in natural litter layers (Hart and Firestone, 1991; Frey et al., 2003).”
- Dynamics of Microbial Communities during Decomposition of Carbon-13 Labeled Ryegrass Fractions in Soil (2005, background): “…C and nutriamounts of PLFAs because of highly variable extraction ents over larger spatial scales than bacteria (Wessén efficiencies; however, the fact that substrate-derived C and Berg, 1986; Frey et al., 2003; Klein and Paschke, of detritusphere PLFAs increased during the incubation 2004).”
- A microcosm experiment to evaluate the influence of location and quality of plant residues on residue decomposition and genetic structure of soil microbial communities (2007, methodology): “During biodegradation, water soluble C was transferred from the decomposing residues to the detritusphere and bulk soil as observed by Frey et al. (2003).”
- Soil health in agricultural systems (2008, background): “Fungi are often overlooked as ecosystem engineers but they contribute to structural genesis via many mechanisms (Ritz & Young 2004), and fungally mediated translocation of C and N between residue layers and soil horizons can be substantial (Frey et al. 2000, 2003).”
- Bacterial and Fungal Contributions to Carbon Sequestration in Agroecosystems (2006, background): “In addition, reciprocal translocation of C from surface residues to mineral soil via fungal hyphae occurs (Frey et al., 2003).”
- The role of wood decay fungi in the carbon and nitrogen dynamics of the forest floor (2006, background): “Further, in the field nitrogen translocation from soil into surface litter can directly affect the rate of litter decomposition (Frey et al., 2000, 2003).”
- Soil erodibility, microbial biomass, and physical–chemical property changes during long-term natural vegetation restoration: a case study in the Loess Plateau, China (2010, background): “Therefore, microbial diversity is expected to increase as the abandonment time increases ( Frey et al. 2003 ).”
- Soil microbial community composition as affected by restoration practices in California grassland (2006, unknown): “This confirms the important role of fungi as part of the zymogenic microbial biomass at the litter–soil interface (Frey et al., 2003; Potthoff et al., 2005b), and to handle low C/N ratios in plant residues (Paul and Clark, 1996; Paustian and Schnürer, 1987).”