Geo-Marine Letters

, Volume 25, Issue 5, pp 281–292

ROV study of a giant pockmark on the Gabon continental margin


    • Département GéosciencesIFREMER
  • K. Olu
    • Département Environnement ProfondIFREMER
  • Y. Fouquet
    • Département GéosciencesIFREMER
  • J. L. Charlou
    • Département GéosciencesIFREMER
  • A. Gay
    • Laboratoire GTS, place BataillonUniversité Montpellier II
  • B. Dennielou
    • Département GéosciencesIFREMER
  • J. P. Donval
    • Département GéosciencesIFREMER
  • A. Fifis
    • Département Environnement ProfondIFREMER
  • T. Nadalig
    • Laboratoire de Microbiologie et de GénétiqueUniversité Louis Pasteur, CNRS-FRE 2326, Institut de Botanique
  • P. Cochonat
    • Département GéosciencesIFREMER
  • E. Cauquil
    • TOTAL
  • J. F. Bourillet
    • Département GéosciencesIFREMER
  • M. Le Moigne
    • Direction Environnement LittoralIFREMER
  • M. Sibuet
    • Département Environnement ProfondIFREMER

DOI: 10.1007/s00367-005-0213-6

Cite this article as:
Ondréas, H., Olu, K., Fouquet, Y. et al. Geo-Mar Lett (2005) 25: 281. doi:10.1007/s00367-005-0213-6


A giant, 800-m wide pockmark, called Regab, was discovered along the Equatorial African margin at 3160-m water depth and was explored by remote operated vehicle (ROV) as part of the Zaiango (1998–2000) and Biozaire (2001–2003) projects carried out conjointly by TOTAL and a number of French research institutes. A microbathymetric map obtained using the ROV sensors shows that the pockmark actually consists of a cluster of smaller pockmarks aligned N70 along a 15-m deep depression. Methane was recorded all over the pockmark, the highest values along the axis of the depression where massive carbonate crusts and dense seep communities were also found. Several faunal species belong to the Vesicomyidae and Mytilidae bivalve families, as well as to Siboglinidae (Vestimentifera) tubeworms. Preliminary analyses confirm their association with symbiotic bacteria, thus documenting their dependence on fluid seeps. The pockmark appears to be related to an infilled channel, visible on the seismic data 300 m below the seafloor, which may act as a reservoir for biogenic fluids supplied to the trap from the surrounding sediments.

Copyright information

© Springer-Verlag 2005