The characterization of microbial assemblages within solid gas hydrate, especially those that may be physiologically active under in situ hydrate conditions, is essential to gain a better understanding of the effects and contributions of microbial activities in Gulf of Mexico (GoM) hydrate ecosystems. In this study, the composition of the Bacteria and Archaea communities was determined by 16S rRNA phylogenetic analyses of clone libraries derived from RNA and DNA extracted from sediment-entrained hydrate (SEH) and interior hydrate (IH). The hydrate was recovered from an exposed mound located in the northern GoM continental slope with a hydrate chipper designed for use on the manned-submersible Johnson Sea Link (water depth, 550 m). Previous geochemical analyses indicated that there was increased metabolic activity in the SEH compared to the IH layer (B. N. Orcutt, A. Boetius, S. K. Lugo, I. R. Macdonald, V. A. Samarkin, and S. Joye, Chem. Geol. 205:239-251). Phylogenetic analysis of RNA-and DNA-derived clones indicated that there was greater diversity in the SEH libraries than in the IH libraries. A majority of the clones obtained from the metabolically active fraction of the microbial community were most closely related to putative sulfate-reducing bacteria and anaerobic methane-oxidizing archaea. Several novel bacterial and archaeal phylotypes for which there were no previously identified closely related cultured isolates were detected in the RNA-and DNA-derived clone libraries. This study was the first phylogenetic analysis of the metabolically active fraction of the microbial community extant in the distinct SEH and IH layers of GoM gas hydrate.Marine gas hydrates, which are ice-like crystalline solids, are composed of rigid water molecules with trapped gas molecules, primarily methane and other hydrocarbons. Gas hydrate reservoirs, which are distributed in the sediments of active and passive continental slope margins, as well as in terrestrial (i.e., permafrost) regions (38), are a proposed fossil fuel energy source (10). Additionally, the estimated global volume of submarine methane hydrates exceeds 10 16 m 3 (7, 10), highlighting the impact of hydrates on global carbon cycling, climate conditions, and seafloor stability (16,18,28,31,35). The formation of gas hydrates is dependent upon suitable gas, temperature, and pressure conditions (reviewed in reference 38). Geological and chemical conditions in the northern continental slope of the Gulf of Mexico (GoM) promote the formation of gas hydrates where seepage of hydrocarbon gases forms extensive surface-breaching mounds on the seafloor, as well as vast veinfilling hydrates in hemipelagic sediments (27).Geochemical characteristics, including gas composition and isotopic ratios of surface breaching hydrate, in the GoM have been well documented (19,33,34,38). Growth and dissolution of GoM hydrate mounds have also been observed, with changes in mound size and shape evident over a period of months (19). Such hydrate growth patterns increase fluid and solid (i.e....