Anthropogenic nitrogen (N) deposition affects many natural processes, including forest litter decomposition. Saprotrophic fungi are the only organisms capable of completely decomposing lignocellulosic (woody) litter in temperate ecosystems, and therefore the responses of fungi to N deposition are critical in understanding the effects of global change on the forest carbon cycle. Plant litter decomposition under elevated N has been intensively studied, with varying results. The complexity of forest floor biota and variability in litter quality have obscured N-elevation effects on decomposers. Field experiments often utilize standardized substrates and N-levels, but few studies have controlled the decay organisms. Decomposition of beech (Fagus...
International audienceLeaf litter chemistry and ectomycorrhizal (ECM) fungi are key drivers of the b...
Atmospheric nitrogen (N) deposition has increased dramatically since preindustrial times and continu...
Decomposition of soil organic matter connects the global carbon (C) cycle with the turnover of nitro...
Anthropogenic nitrogen (N) deposition affects many natural processes, including forest litter decomp...
Translocation of nitrogen (N) through mycelial cords of wood decay fungi is thought to be the mechan...
Leaf and fine root litter decomposition is central to biogeochemical cycles in northern forest. I st...
Boreal forests are characterized by spatially heterogeneous soils with low N availability. The decom...
<div><p>Boreal forests are characterized by spatially heterogeneous soils with low N availability. T...
Forest litter decomposition is a major component of the global carbon (C) budget, and is greatly aff...
Increased nitrogen (N) deposition caused by human activities has altered ecosystem functioning and b...
Microbial respiration in dead wood contributes substantially to the long-lived forest carbon (C) poo...
High levels of atmospheric nitrogen (N) deposition may result in greater terrestrial carbon (C) stor...
There is evidence that anthropogenic nitrogen (N) deposition enhances carbon (C) sequestration in bo...
International audienceLeaf litter chemistry and ectomycorrhizal (ECM) fungi are key drivers of the b...
Atmospheric nitrogen (N) deposition has increased dramatically since preindustrial times and continu...
Decomposition of soil organic matter connects the global carbon (C) cycle with the turnover of nitro...
Anthropogenic nitrogen (N) deposition affects many natural processes, including forest litter decomp...
Translocation of nitrogen (N) through mycelial cords of wood decay fungi is thought to be the mechan...
Leaf and fine root litter decomposition is central to biogeochemical cycles in northern forest. I st...
Boreal forests are characterized by spatially heterogeneous soils with low N availability. The decom...
<div><p>Boreal forests are characterized by spatially heterogeneous soils with low N availability. T...
Forest litter decomposition is a major component of the global carbon (C) budget, and is greatly aff...
Increased nitrogen (N) deposition caused by human activities has altered ecosystem functioning and b...
Microbial respiration in dead wood contributes substantially to the long-lived forest carbon (C) poo...
High levels of atmospheric nitrogen (N) deposition may result in greater terrestrial carbon (C) stor...
There is evidence that anthropogenic nitrogen (N) deposition enhances carbon (C) sequestration in bo...
International audienceLeaf litter chemistry and ectomycorrhizal (ECM) fungi are key drivers of the b...
Atmospheric nitrogen (N) deposition has increased dramatically since preindustrial times and continu...
Decomposition of soil organic matter connects the global carbon (C) cycle with the turnover of nitro...