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Creator:: Briggs, Brandon R., Graw, Michael, Brodie, Eoin L., Bahk, Jang-Jun, Kim, Sung-Han, Hyun, Jung-Ho, Kim, Ji-Hoon, Torres, Marta, and Colwell, Frederick S.
Abstract:: The biogeochemical processes that occur in marine sediments on continental margins are complex; however, from one perspective they can be considered with respect to three geochemical zones based on the presence and form of methane: sulfate-methane transition (SMTZ), gas hydrate stability zone (GHSZ), and free gas zone (FGZ). These geochemical...
Resource Type:: Article
Full Text:: +, Michael Graw3, Eoin L. Brodie4, Jang-Jun Bahk5, Sung-Han Kim6, Jung-Ho Hyun6, Ji-Hoon Kim2,5, Marta

Creator:: Briggs, Brandon R., Inagaki, Fumio, Morono, Yuki, Futagami, Taiki, Huguet, Carme, Rosell-Mele, Antoni, Lorenson, Thomas D., and Colwell, Frederick S.
Abstract:: The degradation of organic carbon in subseafloor sediments on continental margins contributes to the largest reservoir of methane on Earth. Sediments in the Andaman Sea are composed of ~ 1% marine-derived organic carbon and biogenic methane is present. Our objective was to determine microbial abundance and diversity in sediments that...
Resource Type:: Article
Full Text:: untitled R E S EA RCH AR T I C L E Bacterial dominance in

Creator:: Briggs, Brandon R.
Abstract:: Marine sediments contain an abundance of methane that is biologically produced and plays a significant role in the global carbon cycle. Microbes responsible for the carbon cycle in marine sediments, and the processes that they carry out, need to be characterized in order to fully understand the role of this...
Resource Type:: Dissertation
Full Text:: ; Inagaki, et al., 2006; Sorensen & Teske, 2006; Biddle, et al., 2008). These studies indicate that the

ScholarsArchive@OSU