Coleman
Max
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Max
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PreprintDiverse styles of submarine venting on the ultraslow spreading Mid-Cayman Rise( 2010-06-24) German, Christopher R. ; Bowen, Andrew D. ; Coleman, Max ; Honig, D. L. ; Huber, Julie A. ; Jakuba, Michael V. ; Kinsey, James C. ; Kurz, Mark D. ; Leroy, S. ; McDermott, Jill M. ; Mercier de Lepinay, B. ; Nakamura, Ko-ichi ; Seewald, Jeffrey S. ; Smith, J. L. ; Sylva, Sean P. ; Van Dover, Cindy L. ; Whitcomb, Louis L. ; Yoerger, Dana R.Thirty years after the first discovery of high-temperature submarine venting, the vast majority of the global Mid Ocean Ridge remains unexplored for hydrothermal activity. Of particular interest are the world’s ultra-slow spreading ridges which were the last to be demonstrated to host high-temperature venting, but may host systems particularly relevant to pre-biotic chemistry and the origins of life. Here we report first evidence for diverse and very deep hydrothermal vents along the ~110 km long, ultra-slow spreading Mid-Cayman Rise. Our data indicate that the Mid- Cayman Rise hosts at least three discrete hydrothermal sites, each representing a different type of water-rock interaction, including both mafic and ultra-mafic systems and, at ~5000 m, the deepest known hydrothermal vent. Although submarine hydrothermal circulation, in which seawater percolates through and reacts with host lithologies, occurs on all mid-ocean ridges, the diversity of vent-types identified here and their relative geographic isolation make the Mid-Cayman Rise unique in the oceans. These new sites offer prospects for: an expanded range of vent-fluid compositions; varieties of abiotic organic chemical synthesis and extremophile microorganisms; and unparalleled faunal biodiversity - all in close proximity.