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Home » Programs & Partnerships » U.S. Science Support Program » Distinguished Lecturer Series » Past Distinguished Lecturer Series » Fluid and Heat Circulation in the Subseafloor Ocean

Fluid and Heat Circulation in the Subseafloor Ocean

dls_spinelliDr. Glenn Spinelli, New Mexico Institute of Mining and Technology


The ocean crust is the largest aquifer on earth, and it hosts vigorous fluid circulation - the entire volume of the world's oceans cycles through the seafloor in less than 500,000 years.  This fluid circulation plays an important role in redistributing heat within the high permeability ocean crust, and can control the crust's thermal state by extracting heat.  The thermal state of the crust, in turn, affects diagenetic, metamorphic, and geodynamic processes.  For example, the thermal state of ocean crust is an important control on subduction zone temperatures, which may affect the updip and downdip limits of the megathrust seismogenic zone.  Results from new thermal models that include coupled fluid and heat transport in a subduction zone show that hydrothermal circulation in subducting basaltic basement rocks can greatly suppress temperatures along the subducting slab relative to cases with no fluid transport.  These results are constrained by seafloor heat flux measurements and observations of temperature and fluid pressure in Ocean Drilling Program boreholes.  Fluid circulation in subducting crust may account for previously unexplained thermal anomalies on the Nankai margin of Japan.

Dr. Spinelli has used sediments and borehole observatory data from Ocean Drilling Program sites on the Juan de Fuca Ridge flank, offshore Costa Rica, and the Nankai margin.  He has also served on the Integrated Ocean Drilling Program Science Steering and Evaluation Panel.

Lecture Schedule

  • August 29, 2008 - University of Missouri-Columbia (Columbia, MO)
  • October 10, 2008 - University of Wisconsin-Madison (Madison, WI)
  • October 17, 2008 - Southern Methodist University (Dallas, TX)
  • January 28, 2009 - Arizona State University (Tempe, AZ)
  • February 19, 2009 - Bowling Green State University (Bowling Green, OH)
  • February 20, 2009 - Indiana University South Bend (South Bend, IN)
  • March 2, 2009 - University of Wyoming (Laramie, WY)
  • March 23, 2009 - Utah State University (Logan, UT)

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Section Contents

Past Distinguished Lecturer Series

  • Microbes and Volcanoes: A Tale from the Seafloor
  • Big Waves, Extreme Aridity, Strange Reefs, and Poisonous Gas in the Cool-Water Carbonate Sediments of the Great Australian Bight
  • Understanding Slow Spreading Ridges: How Do They Work?
  • The Once and Future Warm Earth: A Paleoceanographic View
  • Arctic Coring Expedition (ACEX): A North Pole Discovery
  • Getting Inside the Plate Boundary: Subduction Zone Megathrusts in IODP
  • What Causes Transience in Fluid Flow in Subduction Zones and in Other Oceanic Margin Environments?
  • Linking Tectonics, Climate Change, and Biotic Evolution: The Oceanic Anoxic Events of the Mid-Cretaceous (~120-90 MA)
  • Unraveling the Archive of Climate Change from the Marine Record: Integration of Isotopic and Elemental Proxies in Molluscan Carb
  • Pleistocene Climate Instability: Oceans, Ice and Insolation
  • Greenhouse Gas Emissions, Environment and Biota: The Earth 55 Million Years Ago
  • Methane-Ice in Marine Sediments: Where, How and Why We Study These Deposits
  • The Deep Biosphere: Microbes in the Mud
  • Solar Forcing or Climate System Feedbacks: Who's the Boss of Plio-Pleistocene Variations in Asian Monsoon Strength?
  • Formation of the Kerguelen Large Igneous Province, Gondwana Breakup, Lost Continents and Growth of the Indian Ocean
  • The Pacific Ocean and Climatic Change, from Eocene Extreme Warmth to Pleistocene Glacial Cycles
  • Marine Sediments Go To Prism
  • A Cure for Global Warming? A Critical Look at Iron Fertilization's Role in Climate Change
  • A Rapid Rise in Greenhouse Gas Concentrations 55 Million Years Ago: A Deep Sea Perspective on the Causes and Consequences
  • Estimating the Level and Taking the Temperature of the Tropical Seas over the Past 25,000 Years
  • Exploring Oceanic Magmatism Through Silicate Melt Inclusions
  • Fluid and Heat Circulation in the Subseafloor Ocean
  • Deep-Ocean Circulation During Extremely Warm Climates
  • Pore Pressure, Sedimentation, and Submarine Landslides
  • Discoveries, Hypotheses, and Drilling Surprises: Adventures in Studying the Formation and Evolution of Oceanic Lithosphere
  • One Rock to Change the World: The Story of the Chicxulub Impact Crater
  • The Earth's Turmoil of the Last Deglacial Period
  • Tales of Deep Ocean Circulation Told by Tiny Fish Teeth
  • The Phanerozoic Record of Global Sea-level Change: ODP Constrains the Last 100 Million Years
  • Iceberg-Rafted Sediment in the Deep Ocean — An Ice Volume Story or Not?
  • Formation and Environmental Effects of Giant Oceanic Plateaus
  • Probing the Microbiology of Deeply Buried Marine Sediments
  • Exploring the Application of Foraminiferal Mg/Ca Ratios to Questions of Early Cenozoic Climate Change
  • Unlocking the Secrets of the Deep Subsurface Biosphere
  • Cretaceous Black Shales, Mediterranean Sapropels, and Greenhouse Climate
  • A Cenozoic History of Atmospheric Carbon Dioxide
  • Marine Barite: A Recorder of Ocean Chemistry and Productivity

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