<div><p>The potent greenhouse gas methane (CH<sub>4</sub>) 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<sub>4</sub> emitted and the heritability of this trait offer a means for reducing CH<sub>4</sub> emissions by selecting low-CH<sub>4</sub> emitting animals for breeding. We demonstrate that differences in rumen microbial community structure are linked to high and low CH<sub>4</sub> emissions in sheep. Bacterial community structures in 236 rumen samples from 118 high- and low-CH<sub>4</sub> emitting sheep formed gradual transitions between three ruminotypes. Two of these (Q and S) were linked to significantly lower CH<sub>4</sub> yields (14.4 and 13.6 g CH<sub>4</sub>/kg dry matter intake [DMI], respectively) than the third type (H; 15.9 g CH<sub>4</sub>/kg DMI; <i>p</i><0.001). Low-CH<sub>4</sub> ruminotype Q was associated with a significantly lower ruminal acetate to propionate ratio (3.7±0.4) than S (4.4±0.7; <i>p</i><0.001) and H (4.3±0.5; <i>p</i><0.001), and harbored high relative abundances of the propionate-producing <i>Quinella ovalis</i>. Low-CH<sub>4</sub> ruminotype S was characterized by lactate- and succinate-producing <i>Fibrobacter</i> spp., <i>Kandleria vitulina</i>, <i>Olsenella</i> spp., <i>Prevotella bryantii</i>, and <i>Sharpea azabuensis</i>. High-CH<sub>4</sub> ruminotype H had higher relative abundances of species belonging to <i>Ruminococcus,</i> other Ruminococcaceae, Lachnospiraceae, Catabacteriaceae, <i>Coprococcus</i>, other Clostridiales, <i>Prevotella</i>, other Bacteroidales, and Alphaproteobacteria, many of which are known to form significant amounts of hydrogen. We hypothesize that lower CH<sub>4</sub> yields are the result of bacterial communities that ferment ingested feed to relatively less hydrogen, which results in less CH<sub>4</sub> being formed.</p></div
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