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Large perturbations in CO2 flux and subsequent chemosynthesis are induced in agricultural soil by the addition of elemental sulfur.


ABSTRACT: The microbial contribution to soil organic matter has been shown to be much larger than previously thought and thus it plays a major role in carbon cycling. Among soil microorganisms, chemoautotrophs can fix CO2 without sunlight and can glean energy through the oxidation of reduced elements such as sulfur. Here we show that the addition of sulfur to soil results in an initial surge in production of CO2 through microbial respiration, followed by an order of magnitude increase in the capture of carbon from the atmosphere as elemental sulfur is oxidised to sulfate. Thiobacillus spp., take advantage of specific conditions to become the dominant chemoautotrophic group that consumes CO2. We discern the direct incorporation of atmospheric carbon into soil carbohydrate, protein and aliphatic compounds and differentiate these from existing biomass. These results suggest that chemoautotrophs can play a large role in carbon cycling and that this carbon is heavily influenced by land management practises.

SUBMITTER: Kelleher BP 

PROVIDER: S-EPMC5498539 | biostudies-literature | 2017 Jul

REPOSITORIES: biostudies-literature

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Large perturbations in CO<sub>2</sub> flux and subsequent chemosynthesis are induced in agricultural soil by the addition of elemental sulfur.

Kelleher Brian P BP   Flanagan Paul V PV   Hart Kris M KM   Simpson Andre J AJ   Oppenheimer Seth F SF   Murphy Brian T BT   O'Reilly Shane S SS   Jordan Sean F SF   Grey Anthony A   Ibrahim Aliyu A   Allen Christopher C R CCR  

Scientific reports 20170705 1


The microbial contribution to soil organic matter has been shown to be much larger than previously thought and thus it plays a major role in carbon cycling. Among soil microorganisms, chemoautotrophs can fix CO<sub>2</sub> without sunlight and can glean energy through the oxidation of reduced elements such as sulfur. Here we show that the addition of sulfur to soil results in an initial surge in production of CO<sub>2</sub> through microbial respiration, followed by an order of magnitude increas  ...[more]

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