Diversity of Hydrothermal Systems on Slow Spreading Ocean Ridges

Published by the American Geophysical Union as part of the Geophysical Monograph Series, Volume 188. Diversity of Hydrothermal Systems on Slow Spreading Ocean Ridges presents a multidisciplinary overview of the remarkable emerging diversity of hydrothermal systems on slow spreading ocean ridges in the Atlantic, Indian, and Arctic oceans. When hydrothermal systems were first found on the East Pacific Rise and other Pacific Ocean ridges beginning in the late 1970s, the community consensus held that the magma delivery rate of intermediate to fast spreading was necessary to support black smoker-type high-temperature systems and associated chemosynthetic ecosystems and polymetallic sulfide deposits. Contrary to that consensus, hydrothermal systems not only occur on slow spreading ocean ridges but, as reported in this volume, are generally larger, exhibit different chemosynthetic ecosystems, produce larger mineral deposits, and occur in a much greater diversity of geologic settings than those systems in the Pacific. The full diversity of hydrothermal systems on slow spreading ocean ridges, reflected in the contributions to this volume, is only now emerging and opens an exciting new frontier for ocean ridge exploration, including * Processes of heat and chemical transfer from the Earth's mantle and crust via slow spreading ocean ridges to the oceans * The major role of detachment faulting linking crust and mantle in hydrothermal circulation * Chemical reaction products of mantle involvement including serpentinization, natural hydrogen, abiotic methane, and hydrocarbon synthesis * Generation of large polymetallic sulfide deposits hosted in ocean crust and mantle * Chemosynthetic vent communities hosted in the diverse settings The readership for this volume will include schools, universities, government laboratories, and scientific societies in developed and developing nations, including over 150 nations that have ratified the United Nations Convention on the Law of the Sea.

Peter Arnold Rona was an American oceanographer. He was also a professor of Earth and planetary sciences at Rutgers University. Colin W. Devey is the editor of Diversity of Hydrothermal Systems on Slow Spreading Ocean Ridges, published by Wiley.

Preface Peter A. Rona, Colin W. Devey, Jérôme Dyment, andBramley J. Murton vii Diversity of Hydrothermal Systems on Slow Spreading OceanRidges: Introduction Peter A. Rona, Colin W. Devey, Jérôme Dyment, andBramley J. Murton 1 Emerging Diversity of Hydrothermal Systems on Slow SpreadingOcean Ridges Peter A. Rona 5 Hydrothermal Circulation at Slow Spreading Ridges: Analysis ofHeat Sources and Heat Transfer Processes Robert P. Lowell 11 Chemical Signatures From Hydrothermal Venting on Slow SpreadingRidges Henrietta N. Edmonds 27 The Magnetic Signature of Hydrothermal Systems in Slow SpreadingEnvironments Maurice A. Tivey and Jérôme Dyment 43 Hydrothermal Activity at the Arctic Mid-Ocean Ridges Rolf B. Pedersen, Ingunn H. Thorseth, Tor Eivind Nygård,Marvin D. Lilley, and Deborah S. Kelley 67 Implications of the Iceland Deep Drilling Project for ImprovingUnderstanding of Hydrothermal Processes at Slow Spreading Mid-OceanRidges Wilfred A. Elders and Gudmundur ÓmarFridleifsson 91 Crustal Structure, Magma Chamber, and Faulting Beneath the LuckyStrike Hydrothermal Vent Field Wayne C. Crawford, Satish C. Singh, Tim Seher, Violaine Combier,Doga Dusunur, and Mathilde Cannat 113 The Relationships Between Volcanism, Tectonism, and HydrothermalActivity on the Southern Equatorial Mid-Atlantic Ridge C. W. Devey, C. R. German, K. M. Haase, K. S. Lackschewitz, B.Melchert, and D. P. Connelly 133 The Ultraslow Spreading Southwest Indian Ridge Daniel Sauter and Mathilde Cannat 153 Deformation and Alteration Associated With Oceanic andContinental Detachment Fault Systems: Are They Similar? Barbara E. John and Michael J. Cheadle 175 Detachment Fault Control on Hydrothermal Circulation Systems:Interpreting the Subsurface Beneath the TAG Hydrothermal FieldUsing the Isotopic and Geological Evolution of Oceanic CoreComplexes in the Atlantic Andrew M. McCaig, Adélie Delacour, Anthony E. Fallick,Teddy Castelain, and Gretchen L. Früh-Green 207 Serpentinization and Associated Hydrogen and Methane Fluxes atSlow Spreading Ridges Mathilde Cannat, Fabrice Fontaine, and Javier Escartín241 High Production and Fluxes of H2 and CH4 and Evidence of AbioticHydrocarbon Synthesis by Serpentinization in Ultramafic-HostedHydrothermal Systems on the Mid-Atlantic Ridge Jean Luc Charlou, Jean Pierre Donval, Cécile Konn,Hélène Ondréas, Yves Fouquet, PhilippeJean-Baptiste, and Elise Fourré 265 Phase Equilibria Controls on the Chemistry of Vent Fluids FromHydrothermal Systems on Slow Spreading Ridges: Reactivity ofPlagioclase and Olivine Solid Solutions and the pH-SilicaConnection W. E. Seyfried Jr., Nicholas Pester, and Qi Fu 297 Geodiversity of Hydrothermal Processes Along the Mid-AtlanticRidge and Ultramafic-Hosted Mineralization: A New Type of OceanicCu-Zn-Co-Au Volcanogenic Massive Sulfide Deposit Yves Fouquet, Pierre Cambon, Joël Etoubleau, Jean LucCharlou, Hélène Ondréas, Fernando J. A. S. Barriga,Georgy Cherkashov, Tatiana Semkova, Irina Poroshina, M. Bohn, JeanPierre Donval, Katell Henry, Pamela Murphy, and Olivier Rouxel321 Hydrothermal Systems: A Decade of Discovery in Slow SpreadingEnvironments Deborah S. Kelley and Timothy M. Shank 369 Chemosynthetic Communities and Biogeochemical Energy PathwaysAlong the Mid-Atlantic Ridge: The Case of BathymodiolusAzoricus N. Le Bris and S. Duperron 409 Index 431