Diffuse venting in the crater of a shallow seamount inputs stable, organically-complexed dissolved iron to the upper water column of the Australian-Antarctic Ridge bloom region
Patrick Monreal1,2, Pamela Barrett3, Tamara Baumberger4,5, Nathaniel J. Buck6, Jessalyn E Davis1, Sophie E Jenness6, Stevie Walker7, Hope V Jerris8, Elise Herzfeld1, Gert van Dijken9, Kevin R Arrigo9, Randelle M Bundy1 and Joseph A Resing6,10, (1)University of Washington, School of Oceanography, Seattle, United States, (2)University of Washington, Astrobiology Program, Seattle, United States, (3)University of Washington and NOAA/PMEL, Cooperative Institute for Climate, Oceans, and Ecosystem Studies, Seattle, United States, (4)Oregon State University, Corvallis, United States, (5)NOAA Pacific Marine Environmental Laboratory, Newport, Oregon, United States, (6)University of Washington Seattle Campus, School of Oceanography, Seattle, United States, (7)University of Washington, Oceanography, Seattle, United States, (8)Middlebury College, Earth and Climate Sciences, Middlebury, VT, United States, (9)Stanford University, Earth System Science, Stanford, United States, (10)NOAA Pacific Marine Environmental Laboratory, Seattle, United States