Variations in microbial isotopic fractionation during soil organic matter decomposition (Q58991422)

1

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N. Nunan

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C. Chenu

4

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A. Mariotti

https://scigraph.springernature.com/pub.10.1007/s10533-010-9432-7

5

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publication date

3 April 2010

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published in

Biogeochemistry

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volume

106

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issue

1

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page(s)

5-21

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exact match

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cites work

Chapter 6 Combining Biomarker with Stable Isotope Analyses for Assessing the Transformation and Turnover of Soil Organic Matter

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Impacts of Carbon and Flooding on Soil Microbial Communities: Phospholipid Fatty Acid Profiles and Substrate Utilization Patterns

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13C and 15N natural abundance of the soil microbial biomass

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15N enrichment as an integrator of the effects of C and N on microbial metabolism and ecosystem function

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CARBON ISOTOPE RATIOS IN BELOWGROUND CARBON CYCLE PROCESSES

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Stability of organic carbon in deep soil layers controlled by fresh carbon supply

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Shifts in the structure of soil microbial communities in limed forests as revealed by phospholipid fatty acid analysis

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Carbon isotope fractionation during dark respiration and photorespiration in C3 plants

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Correlations between the 13C Content of Primary and Secondary Plant Products in Different Cell Compartments and That in Decomposing Basidiomycetes.

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Soil microbial community structure: Effects of substrate loading rates

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The 15N natural abundance (δ15N) of ecosystem samples reflects measures of water availability

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Insights into nitrogen and carbon dynamics of ectomycorrhizal and saprotrophic fungi from isotopic evidence

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Natural (13)C abundance reveals trophic status of fungi and host-origin of carbon in mycorrhizal fungi in mixed forests

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A climate-driven switch in plant nitrogen acquisition within tropical forest communities

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Hydrogen and carbon isotope fractionation during aerobic biodegradation of benzene

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Changes in properties of soil-derived dissolved organic matter induced by biodegradation

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Tracing 2,4-D metabolism in Cupriavidus necator JMP134 with 13C-labelling technique and fatty acid profiling

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Dynamics of soil microbial populations involved in 2,4-D biodegradation revealed by FAME-based Stable Isotope Probing

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Atmospheric nitrogen is a reliable standard for natural 15N abundance measurements

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How relevant is recalcitrance for the stabilization of organic matter in soils?

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Fate of microbial biomass-derived amino acids in soil and their contribution to soil organic matter

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Characterization of multiple-substrate utilization by anthracene-degrading Mycobacterium frederiksbergense LB501T.

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