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Flare-Shaped Acoustic Anomalies in the Water Column Along the Ecuadorian Margin: Relationship with Active Tectonics and Gas Hydrates

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An Erratum to this article was published on 15 March 2016

Abstract

With hull-mounted multibeam echosounder data, we report for the first time along the active Ecuadorian margin, acoustic signatures of water column fluid emissions and seep-related structures on the seafloor. In total 17 flare-shaped acoustic anomalies were detected from the upper slope (1250 m) to the shelf break (140 m). Nearly half of the flare-shaped acoustic anomalies rise 200–500 m above the seafloor. The base of the flares is generally associated with high-reflectivity backscatter patches contrasting with the neighboring seafloor. We interpret these flares as caused by fluid escape in the water column, most likely gases. High-resolution seismic profiles show that most flares occur close to the surface expression of active faults, deformed areas, slope instabilities or diapiric structures. In two areas tectonic deformation disrupts a Bottom Simulating Reflector (BSR), suggesting that buried frozen gas hydrates are destabilized, thus supplying free gas emissions and related flares. This discovery is important as it opens the way to determine the nature and origin of the emitted fluids and their potential link with the hydrocarbon system of the forearc basins along the Ecuadorian margin.

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References

  • Bourgois J (2013) A review on tectonic record of strain buildup and stress release across the andean forearc along the gulf of guayaquil-tumbes basin (GGTB) near ecuador-peru border. Intern Journ Geosc 4:618–635. doi:10.4236/ijg.2013.43057.

  • Collot J-Y, Marcaillou B, Sage F, Michaud F, Agudelo W, Charvis P, Graindorge D, Gutscher MA, Spence G (2004) Are rupture zone limits of great subduction earthquakes controlled by upper plate structures? Evidence form MCS data acquired accross the N-Ecuador-SW Colombia margin. J Geophys Res 109:B11103. doi:10.1029/2004JB003060.

  • Collot J-Y, Migeon, S, Spence, G, Legonidec, Y, Marcaillou, B, Schneider, J-L, Michaud, F, Alvarado, A, Lebrun, J-F, Sosson, M, Pazmiño, A, 2005. Seafloor margin map helps in understanding subduction earthquakes. EOS Transactions, American Geophysical Union, 86(46): 464–466.

  • Collot J-Y, Agudelo W, Ribodetti A, Marcaillou B (2008) Origin of a crustal splay fault and its relation to the seismogenic zone and underplating at the erosional north Ecuador–south Colombia oceanic margin. J Geophys Res 113:B12102. doi:10.1029/2008JB005691.

  • Collot J-Y, Michaud F, Alvarado A, Marcaillou B, Sosson M, Ratzov G, Migeon S, Calahorrano A, Pazmiño A (2009) Visión general de la morfología submarina del margen convergente de Ecuador- Sur de Colombia: implicaciones sobre la transferencia de masa y la edad de la subducción de la Cordillera de Carnegie. In: Collot JY, Sallares V, Pazmiño A (ed) Geologia y Geofisica Marina y Terestre del Ecuador. Publicacion CNDM-INOCAR-IRD, PSE001-09, Guayaquil, Ecuador, pp. 47–74.

  • Dano A, Migeon S, Praeg D, Ceramicola S, Augustin JM, Ketzer JM, Augustin AH, Ducassou E, Mascle J, (2014) Fluid Seepage in Relation to Seabed Deformation on the Central Nile Deep-Sea Fan, Part 1: Evidence from Sidescan Sonar Data S. Krastel et al. (eds.), Submarine Mass Movements and Their Consequences, Advances 129 in Natural and Technological Hazards Research 37, DOI 10.1007/978-3-319-00972-8 12:129–139  .

  • Deniaud Y, Baby P, Basile C, Ordoñez M, Montenegro G, Mascle G (1999) Ouverture et évolution tectono- sédimentaire du Golfe de Guayaquil: bassin d’avant- arc néogène et quaternaire du Sud des Andes équatoriennes. C. R. Acad. Sci. Paris, 328: 181–187.  

  • Deynoux M, Proust JN, Durand J, Merino E (1990) Water transfer cylindrical structures in the Late Proterozoïc eolian sandstones in the Taoudeni Basin, West Africa. Sedim. Geol., 66:227-242.

  • Dominguez S, Lallemand S, Malavieille J, Von Huene R (1998) Upper plate deformations associated with seamount subduction, Tectonophysics, 293: 207–224.

  • Dupré S, Woodside J, Klaucke I, Mascle J, Foucher J-P (2010) Widespread active seepage activity on the Nile Deep Sea Fan (offshore Egypt) revealed by high-definition geophysical imagery. Marine Geology, 275(1–4), 1–19.

  • Dupré S, bERGER L, Le Bouffant N, scalabrin C, bourillet J-F (2014) Fluid emissions at the Aquitaine Shelf (Bay of Biscay, France): A biogenic origin or the expression of hydrocarbon leakage? Continental Shelf Research, 88, 24–33.

  • Dupré S, Scalabrin C, Grall C, Augustin J-M, Henry P, Sengör AMC, Görür N, Çagatay MN, Géli L (2015) Tectonic and sedimentary controls on widespread gas emissions in the Sea of Marmara: Results from systematic, shipborne multibeam echo sounder water column imaging, J. Geophys. Res. Solid Earth, 120, doi:10.1002/2014JB011617.

  • Eguez A, Alvarado A, Yepes H, Machette M, Costa C, Dart R (2003) Database and map of Quaternary faults and folds of Ecuador and its offshore regions. US Geological Survey, Open File Rep, 03–289.

  • Gay A, Lopez M, Berndt C, Séranne M, (2007) Geological controls on focused fluid flow associated with seafloor seeps in the Lower Congo Basin, Marine Geology 244; 68–92.

  • Geli L, Henry P, Zitter T, Dupre S, Tryon M, Cagatay M, De Lepinay B, Le Pichon X, Sengor A, Gorur N, Natalin B, Ucarkus G, Oezeren S, Volker D, Gasperini L, Burnard P, Bourlange S (2008). Gas emissions and active tectonics within the submerged section of the North Anatolian Fault zone in the Sea of Marmara. Earth and Planetary Science Letters, 274(1–2): 34–39.

  • German CR, Parson LM, Mills RA (1996) Mid-ocean ridges and hydrothermal activity. In: Oceanography. An Illustrated Guide. C.P. Summerhayes and S.A. thorpe, eds, p. 152–164.

  • Graindorge D, Calahorrano A, Charvis P, Collot J-Y, Bethoux N (2004) Deep structures of the margin and the Carnegie Ridge, possible consequence on great earthquake recurrence interval. Geoph Res Lett 31. doi:10.1029/2003GL018803.

  • Greinert, J, Artemov, Y, Egorov, V, De Batist, M, Mcginnis, D, (2006) 1300-m-high rising bubbles from mud volcanoes at 2080 m in the Black Sea: Hydroacoustic characteristics and temporal variability. Earth and Planetary Science Letters 244:1–15. doi:10.1016/j.epsl.2006.02.011.

  • Gutscher M-A, Malavieille J, Lallemand S, Collot J-Y (1999) Tectonic segmentation of the North Andean margin: impact of the Carnegie ridge collision. Earth and Planetary Science Letters 168:255–270.

  • Hernández M-J, Michaud F., Collot J-Y, Proust J-N, Ortega R., Aleman A-M (2014) The Neogene Forearc Basins of the Ecuadorian Shelf (1°N-2°20′S): Preliminary Interpretation of a Dense Grid of Mcs Data Abstract T11C-4578 presented at 2014 Fall Meeting, AGU, San Francisco, Calif., 15–19 Dec.

  • Hornafius JS, Quigley D, Luyendyk BP (1999) The world's most spectacular marine hydrocarbon seeps (Coal Oil Point, Santa Barbara Channel, California): Quantification of emissions. Journal of Geophysical Research 104. doi: 10.1029/1999JC900148.

  • Judd AG, Hovland, M (2007) Seabed Fluid Flow. The Impact on Geology, Biology and the Marine Environment. Cambridge University Press, Cambridge.

  • Krabbenhöft A, Netzeband G, Bialas J, Papenberg C (2010) Episodic methane concentrations at seep sites on the upper slope Opouawe Bank, southern Hikurangi Margin, New Zealand, Marine Geology, 272 (1/4):71–78. DOI 10.1016/j.margeo.2009.08.001.

  • Loayza G, Proust J-N, Michaud F, Collot J-Y (2014), Evolution pléistocène du système de canyons du golfe de Guayaquil (Equateur). Contrôles paléo-climatique et tectonique, 14 éme ASF congrés, Paris, page 248.

  • Loncke L., Mascle J., and Fanil Scientific Parties, (2004) Mud volcanoes, gas chimneys, pockmarks and mounds in the Nile deep-sea fan (Eastern Mediterranean): geophysical evidences, Marine and Petroleum Geology 21,6: 669–689.

  • Marcaillou, B, Spence G, Collot J-Y, Wang K (2006) Thermal regime from bottom simulating reflectors along the north Ecuador–south Colombia margin: Relation to margin segmentation and great subduction earthquakes, Journal Geophysisycal Research 111, B12407, doi:10.1029/2005JB004239.

  • Marcaillou B, Collot J-Y., Ribodetti A, d’Acremont E, Mahamat AA, Alvarado A (2016) Seamount subduction at the North-Ecuadorian convergent margin: Effects on structures, inter-seismic coupling and seismogenesis, Earth and Planetary Science Letters 433, 1 January 2016, Pages 146–158.

  • Mascle J, Flore  M, Praeg D, Brosolo L, Camera L, Ceramicola S, Dupre S (2014) Distribution and geological control of mud volcanoes and other fluid/free gas seepage features in the Mediterranean Sea and nearby Gulf of Cadiz. Geo-marine Letters, 34(2–3), 89–110. http://dx.doi.org/10.1007/s00367-014-0356-4.

  • Michaud F, Collot J-Y, Alvarado A, Lopez E y el personal científico y tecnico del INOCAR, (2006) Republica del Ecuador, Batimetría y Relieve Continental, publicación IOA-CVM-02- Post. INOCAR, Guayaquil.

  • Michaud F, Witt C, Royer J-Y (2009) Influence of the Carnegie ridge subduction on Ecuadorian geology: reality and fiction: In: Kay S, Ramos V, and Dickinson WR (eds) Backbone of the Americas: Shallow Subduction, Plateau Uplift and Ridge and terrane Collision. Geol Soc Am Memoir 204:217–228 doi:10.1130/2009.1204.10.

  • Michaud F, Proust J-N, Collot J-Y, the ATACAMES scientific team (2013) Sediments distribution and tectonic faults (Ecuadorian shelf): preliminary results of the ATACAMES Cruise (2012), Abstract T23B-06 presented at 2013 Meeting of the Americas, AGU, Cancun, Mexico, 14-17 May.

  • Michaud F, Proust J-N, Collot J-Y, Lebrun J-F, Witt C, Ratzov G, Pouderoux H, Martillo C, Hernández M-J, Loayza G, Penafiel L, Schenini L, Dano A, Gonzalez M, Barba D, De Min L, Ponce adams G, Urresta A, Calderon M, (2015) Quaternary sedimentation and active faulting along the Ecuadorian shelf: preliminary results of the ATACAMES Cruise (2012), Marine Geophysical Research, 36, 1:81–98.

  • Merewether R, Olsson M-S, Lonsdale P (1985) Acoustically detected hydrocarbon plumes rising from 2-km depths in Guaymas Basin, Gulf of California J. Geophys. Res., 90 (1985), pp. 3075–3085.

  • Nocquet J-M, Mothes P, Alvarado A (2009) Geodesy, geodynamics and earthquake cycle in Ecuador. Geology and marine and onland Geophysics of Ecuador: from the continental coast to the Galapagos Islands. In Collot JY, Sallares V, Pazmiño A (eds) Geologia y Geofisica Marina y Terrestre del Ecuador. Publicacion CNDM-INOCAR-IRD, PSE001-09, Guayaquil, Ecuador pp 83–94.

  • Nocquet J-M, Villegas-Lanza JC, Chlieh M, Mothes PA, Rolandone F, Jarrin P, Cisneros D, Alvarado A, Audin L, Bondoux F, Martin X, Font Y, Régnier M, Vallée M, Tran T, Beauval C, Maguiña Mendoza JM, Martinez W, Tavera H, Yepes H, (2014) Motion of continental slivers and creeping subduction in the northern Andes, Nature Geosciences, 7 (4) (2014), pp. 287–291. http://dx.doi.org/10.1038/ngeo2099

  • Obzhirov A, SHAKIROV R, SALYUK A, SUESS E, BIEBOW N, SALOMATIN A (2004) Relations between methane venting, geological structure and seismo-tectonics in the okhotsk sea, Geo-marine letters, 24:135–139.

  • Paull CK, Borowski WS, Rodrigues N M, (1998) ODP Leg 164 Shipboard Scientific Party, Marine Gas Hydrate Inventory: Preliminary Results of ODP Leg 164 and Implications for Gas Venting and Slumping Associated with the Blake Ridge Gas Hydrate Field. In: Henrient, J. P., Mienert, J., eds., Gas Hydrates: Relevance to World Margin Stability and Climate Change. Geol. Soc. London Spec. Publ., 137: 153–160.

  • Pazmiño A, Zapata C, Michaud F, Martillo C, Loayza G (2010) Reporte Científico a Bordo del B.I.- 91 “Orion” Estudio Geológico del Margen de Plataforma Continental del Golfo de Guayaquil (GEMAC- 1), Diciembre 2010.

  • Pedoja K, Dumont JF, Lamothe M, Ortlieb L, Collot JY, Ghaleb B, Auclair M, Alvarez V, Labrousse B (2006) Plio-quaternary uplift of the manta peninsula and La Plata Island and the subduction of the Carnegie Ridge, central coast of Ecuador. J S Am Earth Sci 22:1–21.

  • Praeg D, Ketzer JM, Augustin AH, Migeon S, Ceramicola S, Dano A, Ducassou E, Dupre S, Mascle J, Rodrigues LF (2014) Fluid seepage in relation to seabed deformation on the central Nile Deep-Sea Fan, part 2: evidence from multibeam and sidescan imagery. Advances in Natural and Technological Hazards Research, 37, 141–150.

  • Proust J-N, Martillo C, Michaud F, Collot J-Y, Dauteuil O (2016) Subduction of seafloor asperities revealed by detailed stratigraphic analysis of the active margin shelf sediments of Central Ecuador. Marine Geology (in press).

  • Ranero CR, Von Huene R (2000) Subduction erosion along the Middle America convergent margin: Nature, v. 404, p. 335–357.

  • Reyes P, Michaud F (2012) Mapa Geologico de la Margen Costera Ecuatoriana (1500000) EPPetroEcuador-IRD (eds), Quito Ecuador.

  • Römer M, Sahling H, Pape Th, dos santos Ferreira C, Wenzhöfer F, Boetius A, Bohrmann G, (2014) Methane fluxes and carbonate deposits at a cold seep area of the Central Nile Deep Sea Fan, Eastern Mediterranean Sea, Marine Geology, 347: 27–42.

  • Sanclemente E (2014) Seismic imaging of the structure of the central Ecuador convergent margin: relationship with the inter-seismic coupling variations, Earth Sciences. Thèse Université de Nice-Sophia Antipolis 2014.

  • Sage F, Collot J-Y , Ranero CR (2006) Interplate patchiness and subduction-erosion mechanisms: Evidence from depth-migrated seismic images at the central Ecuador convergent margin, Geology, v. 34; no. 12; pp. 997–1000; doi: 10.1130/G22790A.1.

  • Schneider Von Deimling J, Brockhoff J, Greinert J (2007) Flare imaging with multibeam systems: Data processing for bubble detection at seeps, Geochem. Geophys. Geosyst., 8, Q06004, doi:10.1029/2007GC001577.

  • Suess E, Torres Ł, M.E., Bohrmann G, Collier RW, Greinert J, Linke P, Rehder G, Trehu A, Wallmann K, Winckler G, Zuleger E, (1999) Gas hydrate destabilization: enhanced dewatering, benthic material turnover and large methane plumes at the Cascadia convergent margin, Earth and Planetary Science Letters 170 (1999) 1–15.

  • Witt C, Bourgois J, Michaud F, Ordoñez M, Jimenez N, Sosson M (2006) Development of the Gulf of Guayaquil (Ecuador) as an effect of the North Andean Block tectonic escape since the lower Pleistocene. Tectonics 25. doi:10.1029/2004TC001723.

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Acknowledgments

We thank the crew of R/V L’Atalante and GE- NAVIR. This work was supported by Institut National des Sciences de l’Univers du Centre National de la Recherche Scientifique (INSU). Thanks to Institut de la Recherche et du Développement (IRD), the Laboratoire Mixte International ‘‘Séismes et Volcans’’(LMI) and to the Instituto Oceanografico de la Armada (INOCAR). This work was partially sponsored by the Ministry of Higher Education, Science, Technology and Innovation of the Republic of Ecuador (SENESCYT). We thank the anonymous reviewers for their constructive comments, which helped us to improve the manuscript.

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Correspondence to Francois Michaud.

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An erratum to this article can be found at http://dx.doi.org/10.1007/s00024-016-1262-7.

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Michaud, F., Proust, JN., Dano, A. et al. Flare-Shaped Acoustic Anomalies in the Water Column Along the Ecuadorian Margin: Relationship with Active Tectonics and Gas Hydrates. Pure Appl. Geophys. 173, 3291–3303 (2016). https://doi.org/10.1007/s00024-015-1230-7

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