Microbial Physiologies Associated with Hydrogenotrophic Metal/Metalloid Reduction from the Crustal Subseafloor of the Juan de Fuca Ridge Flank.
Microbial Physiologies Associated with Hydrogenotrophic Metal/Metalloid Reduction from the Crustal Subseafloor of the Juan de Fuca Ridge Flank.
Jacob Cote1, John Carr2, Jessica Kee Eun Choi2,3, Kaliopi Bousses2, Gabriel Gonsalves-Bertho4, Leah Van Dyke5,6, Olivia Nigro7, Stephanie A Carr8, Michael S Rappe9 and Ileana M. Perez-Rodriguez2, (1)University of Pennsylvania, Graduate Group on Cell and Molecular Biology, Philadelphia, United States, (2)University of Pennsylvania, Department of Earth and Environmental Science, Philadelphia, United States, (3)University of Michigan, Department of Ecology and Evolutionary Biology, Ann Arbor, United States, (4)University of Pennsylvania, Department of Chemical and Biomolecular Engineering, Philadelphia, United States, (5)University of Pennsylvania, Department of Earth and Environmental Science, Philadelphia, PA, United States, (6)University of Pennsylvania, Department of Biology, Philadelphia, PA, United States, (7)Hawaii Pacific University, Department of Natural Science, Kaneohe, United States, (8)Hartwick College, Department of Biology, Oneonta, United States, (9)Hawaiʻi Institute of Marine Biology, University of Hawaiʻi at Mānoa, Kāneʻohe, United States