You are hereNitrogen
Nitrogen
Disentangling plant and soil microbial controls on carbon and nitrogen loss in grassland mesocosms
Summary
It is well known that plant–soil interactions play an important role in determining the impact of global change phenomena on biodiversity and ecosystem functioning. Little is known, however, about the individual and relative importance for carbon (C) and nitrogen (N) cycling of non-random changes in plant and soil communities that result from global change phenomena, such as fertilization and agricultural intensification.
Enzyme activity and microbial community structure in the rhizosphere of two maize lines differing in N use efficiency
Link http://download-v2.springer.com.proxy.lib.iastate.edu/static/pdf/625/art...
Pathan et al. Plant Soil (2015) 387:413–424
Abstract
Soil microbial organic nitrogen uptake is regulated by carbon availability by Farrell et al. SBB
Plants and microorganisms intensely compete for nitrogen (N) at many stages of the terrestrial N cycle. In particular, the dissolved organic N (DON) pool, and competition for low molecular weight dissolved organic N (LMWDON) compounds such as amino acids and peptides (and LMW dissolved organic matter; LMWDOM as a whole) has received significant recent research interest. However, as LMWDON compounds contain both N and carbon (C), a question that remains is whether soil microorganisms are primarily taking up LMWDON mainly for the C or the N contained therein.
Bradford et al. 2014. Ecosystem multifunctionality and soil community complexity. PNAS 111:14478-14483
Bradford et al. 2014. Discontinuity in the responses of ecosystem processes and multifunctionality to altered soil community composition. PNAS 111:14478-14483
http://www.pnas.org/content/111/40/14478.abstract
Significance
Nitrogen input quality changes the biochemical composition of soil organic matter stabilized in the fine fraction: a long-term s
The chemical composition of soil organic matter (SOM) is a key determinant of its biological stability. Our objective in this study was to evaluate the effects of various sources of supplemental N on the chemical composition of SOM in the fine (<5 μm) mineral fraction. Treatments were fallow, maize/soybean in rotation, and continuous maize receiving no fertilizer (maize0N), synthetic fertilizer N (maize + N), or composted manure (maize + manure).
Fellbaum et al. 2014 Fungal nutrient allocation is regulated by C source strength of host plant. New Phytologist
Fellbaum et al. 2014 Fungal nutrient allocation in common mycorrhizal networks is regulated by the carbon source strength of individual host plants. New Phytologist pre-print
http://onlinelibrary.wiley.com/doi/10.1111/nph.12827/abstract
Summary
Common mycorrhizal networks (CMNs) of arbuscular mycorrhizal (AM) fungi in the soil simultaneously provide multiple host plants with nutrients, but the mechanisms by which the nutrient transport to individual host plants within one CMN is controlled are unknown.
New Phytologist Virtual Issue: Scaling root processes
Some of the papers are already posted but the whole issue might be of interests to many of us.
Microbial drivers of global change at the aggregate scale: linking genomic function to carbon metabolism and warming
Co-PI: Adina Howe, Folker Meyer, Galya Orr
Xu et al. 2013. Global analysis of soil microbial biomass C, N, P
Xu et al. 2013. A global analysis of soil microbial biomass carbon, nitrogen and phosphorus in terrestrial ecosystems. Global Ecology and Biogeography 22:737-749.
Main conclusions