Addition of hydrothermally influenced water relieves iron limitation in surface waters of the Australian-Antarctic Ridge
James Lauer1, Matthew M Mills1, Patrick Monreal2, Pamela Barrett3, Nathaniel J. Buck4, Jessalyn E Davis2, Gert van Dijken1, Sophie E Jenness4, Stevie Walker5, Tamara Baumberger6, Randelle M Bundy2, Joseph A Resing4 and Kevin R Arrigo1, (1)Stanford University, Earth System Science, Stanford, United States, (2)University of Washington, School of Oceanography, Seattle, United States, (3)University of Washington and NOAA/PMEL, Cooperative Institute for Climate, Oceans, and Ecosystem Studies, Seattle, United States, (4)University of Washington Seattle Campus, School of Oceanography, Seattle, United States, (5)University of Washington, Oceanography, Seattle, United States, (6)University of Bergen, Bergen, Norway