Marine Geophysical Research

, Volume 40, Issue 3, pp 357–370 | Cite as

High-resolution seismo-acoustic characterization of Green Canyon 600, a perennial hydrocarbon seep in Gulf of Mexico deep water

  • Arne-R. Diercks
  • Leonardo MacelloniEmail author
  • Marco D’Emidio
  • Samantha Lucker
  • Allison Woolsey
  • Maxwell U. Woolsey
Original Research Paper


Green Canyon Lease Block 600 is a well-documented cold seep site characterized by near-perennial oil and gas slicks large enough to reach the sea surface and to be detected on satellite imagery. This site has been selected by the Ecosystem Impact of Oil and Gas Inputs to the Gulf consortium to study the impacts of natural hydrocarbon seepage versus anthropogenic inputs of hydrocarbons into the Gulf of Mexico ecosystem following the Deepwater Horizon oil spill disaster that occurred in 2010. Here we present the first high-resolution characterization of the site. We investigated the seafloor and shallow subsurface combining autonomous underwater vehicle-borne seismo-acoustics with photo data. Our records show vigorous hydrocarbon flux occurring over a wide area of the complex seafloor morphology. Several mounds, which are the most prominent features of the site, are aligned along a ridge structure and are actively venting hydrocarbons. Detailed bathymetry of the mound’s surface highlights the presence of numerous pockmarks, cones, and micro-mounds of variable sizes and shapes. High reflectivity seafloor backscatter characterizes the entire ridge surface; ground-truthing photo surveys confirm the presence of authigenic carbonate hardgrounds, gas hydrates, and chemosynthetic communities. The shallow stratigraphy indicates that the ridge represents the seafloor expression of normal faults, probably rooted to a deep salt body. Salt tectonics generated a complex network of normal faults, many of which displace the upper part of the Holocene sediments up to the seafloor, forming long linear scars. Acoustic anomalies, interpreted as active migration pathways, underlie mounds and venting structures, suggesting a link between the deep hydrocarbon reservoir and seafloor expulsion features.


Gulf of Mexico Cold seeps Seafloor mounds Hydrocarbon plumbing system Shallow faults Seafloor morphology 



We thank the science parties and the ship’s crews of the RV Pelican and the RV Falkor. Carol B. Lutken is greatly appreciated for reviewing the document and for providing insightful comments. We also are deeply grateful to IHS Kingdom for granting the Academic License of Kingdom Suite 8.8. This work was supported by the NOAA Award NA07AR4300464 to the National Institute for Undersea Science and Technology and by a grant from The Gulf of Mexico Research Initiative to support the ECOGIG-2 research consortium. Data are publicly available through the Gulf of Mexico Research Initiative Information & Data Cooperative (GRIIDC) at [,].


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Copyright information

© Springer Nature B.V. 2018

Authors and Affiliations

  1. 1.School of Ocean Science and EngineeringThe University of Southern MississippiJohn C. Stennis Space CenterUSA
  2. 2.Mississippi Mineral Resources InstituteThe University of MississippiUniversity CampusUSA
  3. 3.US Army ERDC Geotechnical Engineering and Geosciences BranchVicksburgUSA

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