Oceanography and Atmospheric Sciences and Meteorology Commons^™

Ultra-Diffuse Hydrothermal Venting Supports Fe-Oxidizing Bacteria And Massive Umber Deposition At 5000 M Off Hawaii, Katrina J. Edwards, B. T. Glazer, Olivier J. Rouxel, Wolfgang Bach, D. Emerson, Russ E. Davis, Brandy M. Toner, C. S. Chan, B. M. Tebo, Hubert Staudigel, Craig L. Moyer

Biology Faculty and Staff Publications

A novel hydrothermal field has been discovered at the base of Lōihi Seamount, Hawaii, at 5000 mbsl. Geochemical analyses demonstrate that ‘FeMO Deep’, while only 0.2 °C above ambient seawater temperature, derives from a distal, ultra-diffuse hydrothermal source. FeMO Deep is expressed as regional seafloor seepage of gelatinous iron- and silica-rich deposits, pooling between and over basalt pillows, in places over a meter thick. The system is capped by mm to cm thick hydrothermally derived iron-oxyhydroxide- and manganese-oxide-layered crusts. We use molecular analyses (16S rDNA-based) of extant communities combined with fluorescent in situ hybridizations to demonstrate that FeMO Deep deposits …