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We sequenced two metagenomes from upper sediment layers (0 to 5 and 6 to 10 cm) from the Kanawha River, West Virginia. The watershed includes inputs from the forested Appalachian Mountains, surface coal mining, municipal residues, and extensive chemical manufacturing. The dominant bacterial phyla were Proteobacteria , Bacteriodetes , Firmicutes , Actinobacteria , and Chloroflexi Xenobiotic degradation pathways were present.

Metagenome Sequences of Sediment from a Recovering Industrialized Appalachian River in West Virginia