A rice rhizosphere microbial community whose H2 cycling and methanogenesis are reshaped by host overexpression of PLANT PEPTIDES CONTAINING SULFATED TYROSINE (PSY) genes. Two independent transgenic rice genotypes (PSY1 and PSY2) reduced cumulative CH4 emissions by 38 percent and 58 percent over 70 days relative to controls. Genome-resolved metatranscriptomic, metagenomic, metabolomic, and metabolic modeling data from PSY rhizosphere soils show lower ratios of CH4 production versus consumption gene activities (largely hydrogenotrophic), decreased H2-producing gene activity, and increased bacterial H2 oxidation pathways. Assembled genomes of rhizosphere H2-oxidizing bacteria are enriched in gluconeogenic-acid utilization genes, and their activity is likely stimulated by elevated gluconeogenic-acid amino acids in PSY rice root exudates, lowering H2 available for hydrogenotrophic methanogens.
Taxonomy
| Taxon | Ontology ID | Functional Roles | Abundance |
|---|---|---|---|
| rhizosphere H2-oxidizing bacteria — ontology label: Bacteria | NCBITaxon:2 · TaxonMech · TraitMech |
PRIMARY_DEGRADER
CROSS_FEEDER
|
N/A |
|
|||
| hydrogenotrophic methanogens — ontology label: Archaea | NCBITaxon:2157 · TaxonMech · TraitMech |
PRIMARY_PRODUCER
|
N/A |
|
|||
| rhizosphere H2-producing bacteria — ontology label: Bacteria | NCBITaxon:2 · TaxonMech · TraitMech |
CROSS_FEEDER
|
N/A |
|
|||
Ecological Interactions
The graph shows only explicitly linked interaction participants. Community members without an asserted participant link are omitted; membership alone does not imply an interaction.
Proposed H2 Oxidation Competition with Methanogenesis
COMPETITIONHYPOTHESIZED - PSY1 rhizospheres had higher transcription of bacterial H2-consuming hydrogenases, supporting the proposal that bacterial H2 use restricts substrate for hydrogenotrophic methanogens. This is not a measured H2 pool or isolated pairwise competition experiment. Individual genome-scale models predict increased H2 oxidation mainly with higher O2; elevated exudate compounds have little direct effect on oxidation but support biomass. Canonical Bacteria and Archaea IDs denote the named functional guilds, not all members of those domains.
Source Taxon: rhizosphere H2-oxidizing bacteria
Target Taxon: hydrogenotrophic methanogens
Metabolites: dihydrogen (CHEBI:18276 · MediaIngredientMech · CMMMech), methane (CHEBI:16183 · MediaIngredientMech · CMMMech)
Biological Processes:
- methanogenesis (GO:0015948 · PathwayMech)
HYPOTHESIZED - Greater bacterial H2 consumption could reduce substrate available for hydrogenotrophic methanogenesis and contribute to lower methane. Transcript patterns and individual metabolic models support this mechanism indirectly; H2 depletion, pairwise competition and the fraction of methane reduction mediated by this route were not directly isolated.
Evidence
-
PMID:41582156 - PARTIAL (IN_VIVO)"increased activity of bacterial H2 oxidation pathways"
-
PMID:41582156 - PARTIAL (IN_VIVO)"decreased CH4 emissions are due to a lower amount of H2 available for hydrogenotrophic methanogenesis"
PSY Root Exudate Effects and Proposed Bacterial Substrate Preference
The living rice host, not an abiotic source, produces exudates with altered composition. Axenic seedling metabolomics found enriched gluconeogenic compounds, largely amino acids, without a significant total-carbon difference. Adding whole PSY1 or PSY2 exudates to soil caused lower CH4 than Kitaake exudates; water controls produced no detected CH4. HYPOTHESIZED - Genomic substrate preferences and PSY1 transcript associations suggest selective support of H2-consuming bacteria, but a specific amino-acid transfer or uptake-mediated mechanism was not isolated. Seedling exudates are not direct samples of mature soil-grown root flux.
Participating Taxa: rhizosphere H2-oxidizing bacteria
Metabolites: amino acid (CHEBI:33709 · MediaIngredientMech · CMMMech)
Biological Processes:
- gluconeogenesis (GO:0006094 · PathwayMech)
- amino acid catabolic process (GO:0009063 · PathwayMech)
PARTIAL - Altered exudate composition may support biomass and activity of H2-consuming guilds enriched for gluconeogenic-acid use, indirectly contributing to the proposed H2 competition. The model predicts little direct effect of exudate enrichment on H2 oxidation itself; increased oxidation responds mainly to O2. Whole-exudate methane suppression is experimentally supported but does not resolve this specific mediator.
Evidence
-
PMID:41582156 - SUPPORT (IN_VITRO)"Soils treated with Kitaake exudates exhibited consistently higher CH4 emissions than those treated with PSY1 or PSY2 exudates"
-
PMID:41582156 - PARTIAL (OTHER)"their activities are likely stimulated by elevated levels of gluconeogenic acids, primarily amino acids, in PSY root exudates"
Reduced H2-Producing Transcripts and Modeled H2 Supply
PSY1 rhizospheres showed lower expression of H2-producing hydrogenases and nitrogenase markers than Kitaake at specified sampling stages. Individual dFBA models predict less H2 production with enriched PSY1 exudate compounds, even where producer biomass increases. This distinguishes gene-expression measurements and modeled flux from reduced producer abundance or directly measured H2 supply. It is not by itself a -/- competition phenotype.
Participating Taxa: rhizosphere H2-producing bacteria
Metabolites: dihydrogen (CHEBI:18276 · MediaIngredientMech · CMMMech)
HYPOTHESIZED - Lower H2-generating activity could restrict substrate supply for hydrogenotrophic methanogenesis. Gene-expression patterns and predicted H2 flux are consistent with this direction, but do not measure the shared H2 pool or isolate the causal contribution to greenhouse CH4 reduction.
Evidence
-
PMID:41582156 - SUPPORT (IN_VIVO)"decreased activity of H2-producing genes"
-
PMID:41582156 - PARTIAL (COMPUTATIONAL)"suppressed H2 production in the PSY rhizosphere"
Reduced Methane Emissions and Proposed H2 Limitation
Greenhouse rice grown in agronomic soil emitted less cumulative CH4 with PSY1 (about 38%) and PSY2 (about 58%) than Kitaake over 70 days. Repeated timepoints were integrated at tub level, not as repeat observations of the same destructively sampled plant. Microbial omics and metabolic modeling focused on PSY1. HYPOTHESIZED - Lower H2 production and greater bacterial consumption restrict hydrogenotrophic methanogenesis; inferred oxygenation and methane oxidation may also contribute. Lower measured CH4 is demonstrated, but the H2-mediated fraction, oxygen concentration and in-situ H2 pool are unresolved.
Metabolites: dihydrogen (CHEBI:18276 · MediaIngredientMech · CMMMech), methane (CHEBI:16183 · MediaIngredientMech · CMMMech)
Biological Processes:
- methanogenesis (GO:0015948 · PathwayMech)
Evidence
-
PMID:41582156 - SUPPORT (IN_VIVO)"reduce cumulative CH4 emissions by 38% (PSY1) and 58% (PSY2) over 70 days of growth compared with controls."
-
PMID:41582156 - PARTIAL (COMPUTATIONAL)"Metabolic modeling using metagenomic and metabolomic data predicts elevated H2 oxidation and suppressed H2 production"
Knowledge gaps & discussions (1)
KNOWLEDGE_GAP OPEN How should the demonstrated whole-exudate methane response be linked without equating it with resolved amino-acid or hydrogen mediation?
Three existing arrows remain explicitly partial or hypothesized. The direct exudate-to-methane link merits extension review; a one-community Edison dry run is not a report or spend authorization. Individual dFBA models are not a coupled methanogen competition experiment. Preserve living-host effects, greenhouse CH4 and soil-exudate perturbations while separating PSY1 omics, seedling sampling, oxygen inference, transcripts and model flux. Specific compounds, H2 addback and field transfer need further evidence.
Attaches to: ecological_interactions#Proposed H2 Oxidation Competition with Methanogenesis, ecological_interactions#PSY Root Exudate Effects and Proposed Bacterial Substrate Preference, ecological_interactions#Reduced H2-Producing Transcripts and Modeled H2 Supply, ecological_interactions#Reduced Methane Emissions and Proposed H2 Limitation
1 evidence item(s)
Soils treated with Kitaake exudates exhibited consistently higher CH4 emissions than those treated with PSY1 or PSY2 exudates
Direct whole-exudate soil amendment supports a methane response, not attribution to individual amino acids.
External Resources
| Name | Repository | Resource ID |
|---|---|---|
|
Primary publication for the PSY rice rhizosphere methane-mitigating community
PubMed record for the Shi et al. 2026 Nature Communications paper linking PSY transgenic rice to altered rhizosphere H2 cycling and reduced methane emissions. |
OTHER | PMID:41582156 |
|
||
|
DOI landing page
DOI link to the Nature Communications paper. |
OTHER | doi:10.1038/s41467-026-68640-9 |
Environmental Factors
| Factor | Value | Unit |
|---|---|---|
| PSY transgene background | PSY1 vs PSY2 vs control rice | N/A |
|
||
| Growth period | 70 days of growth | N/A |
|
||
Growth Media
Cross-Mech Suite Links
Explore related entities across the CultureBotAI X-Mech knowledge bases: