Image_5_Geochemistry of Hydrothermal Fluids From the E2-Segment of the East Scotia Ridge: Magmatic Input, Reaction Zone Processes, Fluid Mixing Regimes and Bioenergetic Landscapes.jpeg

• Main Authors: Samuel I. Pereira, Alexander Diehl, Jill M. McDermott, Thomas Pape, Lukas Klose, Harald Strauss, Gerhard Bohrmann, Wolfgang Bach
• Format: Still Image
• Language: unknown
• Published: 2022
• Subjects: Oceanography; Marine Biology; Marine Geoscience; Biological Oceanography; Chemical Oceanography; Physical Oceanography; Marine Engineering; hydrothermal vents; East Scotia Ridge; back-arc basin; conductive cooling; magmatic water; bioenergetics; Southern Ocean; Scotia Sea
• Online Access: https://doi.org/10.3389/fmars.2022.765648.s006; https://figshare.com/articles/figure/Image_5_Geochemistry_of_Hydrothermal_Fluids_From_the_E2-Segment_of_the_East_Scotia_Ridge_Magmatic_Input_Reaction_Zone_Processes_Fluid_Mixing_Regimes_and_Bioenergetic_Landscapes_jpeg/20071283

The compositions of hydrothermal fluids in back-arc basins (BABs) can be affected by the influx of magmatic fluids into systems that are dominated by reactions between basement rocks and seawater-derived fluids. The East Scotia Ridge (ESR) in the Scotia Sea hosts such hydrothermal systems where the...