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Deconstructing the microbial necromass continuum to inform soil carbon sequestration
Microbial necromass is a large, dynamic and persistent component of soil organic carbon,
the dominant terrestrial carbon pool. Quantification of necromass carbon stocks and its …
the dominant terrestrial carbon pool. Quantification of necromass carbon stocks and its …
Rhizosphere priming effect: a meta-analysis
Rhizosphere priming is crucial for regulating soil carbon and nitrogen biogeochemical
cycles. An appreciable number of studies have been conducted to quantify the rhizosphere …
cycles. An appreciable number of studies have been conducted to quantify the rhizosphere …
Carbon and nitrogen recycling from microbial necromass to cope with C: N stoichiometric imbalance by priming
The impact of increasing amounts of labile C input on priming effects (PE) on soil organic
matter (SOM) mineralization remains unclear, particularly under anoxic conditions and …
matter (SOM) mineralization remains unclear, particularly under anoxic conditions and …
A stoichiometric approach to estimate sources of mineral‐associated soil organic matter
Mineral‐associated soil organic matter (MAOM) is the largest, slowest cycling pool of carbon
(C) in the terrestrial biosphere. MAOM is primarily derived from plant and microbial sources …
(C) in the terrestrial biosphere. MAOM is primarily derived from plant and microbial sources …
Persistent soil carbon enhanced in Mollisols by well-managed grasslands but not annual grain or dairy forage crop** systems
Intensive crop production on grassland-derived Mollisols has liberated massive amounts of
carbon (C) to the atmosphere. Whether minimizing soil disturbance, diversifying crop …
carbon (C) to the atmosphere. Whether minimizing soil disturbance, diversifying crop …
Clarifying the interpretation of carbon use efficiency in soil through methods comparison
Accurate estimates of microbial carbon use efficiency (CUE) are required to predict how
global change will impact microbially-mediated ecosystem functions such as organic matter …
global change will impact microbially-mediated ecosystem functions such as organic matter …
Microorganisms and nutrient stoichiometry as mediators of soil organic matter dynamics
Microbial detritus contributes substantially to the soil organic matter (SOM). Analysis of
global literature indicated that microbial detritus carbon (C) contributed 59 and 64% of total …
global literature indicated that microbial detritus carbon (C) contributed 59 and 64% of total …
[HTML][HTML] The case for digging deeper: soil organic carbon storage, dynamics, and controls in our changing world
Most of our terrestrial carbon (C) storage occurs in soils as organic C derived from living
organisms. Therefore, the fate of soil organic C (SOC) in response to changes in climate …
organisms. Therefore, the fate of soil organic C (SOC) in response to changes in climate …
Soil properties rather than climate and ecosystem type control the vertical variations of soil organic carbon, microbial carbon, and microbial quotient
Small changes in soil organic carbon (SOC) may have great influences on the climate-
carbon (C) cycling feedback. However, there are large uncertainties in predicting the …
carbon (C) cycling feedback. However, there are large uncertainties in predicting the …
Effects of experimental nitrogen deposition on soil organic carbon storage in Southern California drylands
Atmospheric nitrogen (N) deposition is enriching soils with N across biomes. Soil N
enrichment can increase plant productivity and affect microbial activity, thereby increasing …
enrichment can increase plant productivity and affect microbial activity, thereby increasing …