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Two Different Bacterial Community Types Are Linked with the Low-Methane Emission Trait in Sheep
The potent greenhouse gas methane (CH(4)) is produced in the rumens of ruminant animals from hydrogen produced during microbial degradation of ingested feed. The natural animal-to-animal variation in the amount of CH(4) emitted and the heritability of this trait offer a means for reducing CH(4) emis...
Autores principales: | , , , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Public Library of Science
2014
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4117531/ https://www.ncbi.nlm.nih.gov/pubmed/25078564 http://dx.doi.org/10.1371/journal.pone.0103171 |
Sumario: | The potent greenhouse gas methane (CH(4)) is produced in the rumens of ruminant animals from hydrogen produced during microbial degradation of ingested feed. The natural animal-to-animal variation in the amount of CH(4) emitted and the heritability of this trait offer a means for reducing CH(4) emissions by selecting low-CH(4) emitting animals for breeding. We demonstrate that differences in rumen microbial community structure are linked to high and low CH(4) emissions in sheep. Bacterial community structures in 236 rumen samples from 118 high- and low-CH(4) emitting sheep formed gradual transitions between three ruminotypes. Two of these (Q and S) were linked to significantly lower CH(4) yields (14.4 and 13.6 g CH(4)/kg dry matter intake [DMI], respectively) than the third type (H; 15.9 g CH(4)/kg DMI; p<0.001). Low-CH(4) ruminotype Q was associated with a significantly lower ruminal acetate to propionate ratio (3.7±0.4) than S (4.4±0.7; p<0.001) and H (4.3±0.5; p<0.001), and harbored high relative abundances of the propionate-producing Quinella ovalis. Low-CH(4) ruminotype S was characterized by lactate- and succinate-producing Fibrobacter spp., Kandleria vitulina, Olsenella spp., Prevotella bryantii, and Sharpea azabuensis. High-CH(4) ruminotype H had higher relative abundances of species belonging to Ruminococcus, other Ruminococcaceae, Lachnospiraceae, Catabacteriaceae, Coprococcus, other Clostridiales, Prevotella, other Bacteroidales, and Alphaproteobacteria, many of which are known to form significant amounts of hydrogen. We hypothesize that lower CH(4) yields are the result of bacterial communities that ferment ingested feed to relatively less hydrogen, which results in less CH(4) being formed. |
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