Abstract
Seafloor methane emission from the Quepos Slide on the submarine segment of the Costa Rica fore-arc margin was estimated by extrapolating flux measurements from individual seeps to the total area covered by bacterial mats. This approach is based on the combination of detailed mapping to determine the abundance of seeps and the application of a numerical model to estimate the amount of benthic methane fluxes. Model results suggest that the majority of the studied seeps transport rather limited amount of methane (on average: ~177 μmol cm−2 a−1) into the water column due to moderate upward advection, allowing for intense anaerobic oxidation of methane (AOM; on average: 53 % of the methane flux is consumed). Depth-integrated AOM rates (56–1,538 μmol CH4 cm−2 a−1) are comparable with values reported from other active seep sites. The overall amount of dissolved methane released into the water column from the entire area covered by bacterial mats on the Quepos Slide is estimated to be about 0.28 × 106 mol a−1. This conservative estimate which relies on rather accurate determinations of seafloor methane fluxes emphasizes the potential importance of submarine slides as sites of natural methane seepage; however, at present the global extent of methane seepage from submarine slides is largely unknown.
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Aloisi G, Wallmann K, Haese R, Saliège J-F (2004) Chemical, biological and hydrological controls on the 14C content of cold seep carbonate crusts: numerical modeling and implications for convection at cold seeps. Chem Geol 213(4):359–383
Berner RA (1980) Early diagenesis. A theoretical approach. Princeton University Press, New York, p 241
Boetius A, Suess E (2004) Hydrate Ridge: a natural laboratory for the study of microbial life fueled by methane from near-surface gas hydrates. Chem Geol 205:291–310
Boetius A, Ravenschlag K, Schubert CJ, Rickert D, Widdel F, Giesecke A, Amann R, Jørgensen BB, Witte U, Pfannkuche O (2000) A marine microbial consortium apparently mediating anaerobic oxidation of methane. Nature 407:623–626. doi:10.1016/j.chemgeo.2004.07.008
Bohrmann G, Heeschen K, Jung C, Weinrebe W, Baranov B, Cailleau B, Heath R, Hühnerbach V, Hort M, Masson D, Trummer I (2002) Widespread fluid expulsion along the seafloor of the Costa Rica convergent margin. Terra Nova 14:69–79
Boudreau BP (1984) On the equivalence of nonlocal and radial-diffusion models for porewater irrigation. J Mar Res 42:731–735
Boudreau BP (1997) Diagenetic models and their implementation: modelling transport and reactions in aquatic sediments. Springer, Berlin, p 414
Brückmann W, Rhein M, Rehder G, Bialas J, Kopf A (2009) SUBFLUX, Cruise No.66, METEOR-Berichte, 09-2, Universität Hamburg, pp 158
de Beer D, Sauter E, Niemann H, Kaul N, Foucher JP, Witte U, Schlueter M, Boetius A (2006) In situ fluxes and zonation of microbial activity in surface sediments of the Hakon Mosby Mud Volcano. Limnol Oceanogr 51(3):1315–1331
Dimitrov LI (2002) Mud volcanoes—the most important pathway for degassing deeply buried sediments. Earth Sci Rev 59:49–76
Etiope G (2004) New directions: GEM—geologic emissions of methane, the missing source in the atmospheric methane budget. Atmos Environ 38(19):3099–3100
Etiope G, Klusman RW (2002) Geologic emissions of methane to the atmosphere. Chemosphere 49(8):777–789
Etiope G, Milkov AV (2004) A new estimate of global methane flux from onshore and shallow submarine mud volcanoes to the atmosphere. Environ Geol 46(8):997–1002
Feseker T, Foucher JP, Harmegnies F (2008) Fluid flow or mud eruptions? Sediment temperature distributions on Hakon Mosby mud volcano, SW Barents Sea slope. Mar Geol 247(3–4):194–207
Flüh ER, Suess E, Söding E (2004) Cruise Report SO1731 and SO173/3+4; Subduction II GEOMAR-Report, 115. GEOMAR, Kiel, p 491
Füri E, Hilton DR, Tryon MD, Brown KM, McMurtry GM, Bruckmann W, Wheat CG (2010) Carbon release from submarine seeps at the Costa Rica fore arc: implications for the volatile cycle at the Central America convergent margin. Geochem Geophy Geosyst 11:Q04s21. doi:10.1029/2009gc002810
Ginsburg GD, Milkov AV, Soloviev VA, Egorov AV, Cherkashev GA, Vogt PR, Crane K, Lorenson TD, Khutorskoy MD (1999) Gas hydrate accumulation at the Haakon Mosby Mud Volcano. Geo-Mar Lett 19:57–67
Greinert J, McGinnis DF, Naudts L, Linke P, De Batist M (2010) Atmospheric methane flux from bubbling seeps: spatially extrapolated quantification from a Black Sea shelf area. J Geophys Res 115:C01002. doi:10.1029/2009JC005381
Grubbs FE (1950) Sample criteria for testing outlying observations. Ann Math Stat 21:27–58
Gubsch S (2010) Detektion und Quantifizierung von subaquatischen Porenwasserfreisetzungen geringer Intensitäten. Shaker Verlag, Reihe Umweltwissenschaft Ph.D Dissertation, Universität Hamburg-Harburg, pp 174
Haese RR, Meile C, Van Cappellen P, De Lange GJ (2003) Carbon geochemistry of cold seeps: methane fluxes and transformation in sediments from Kazan mud volcano, eastern Mediterranean Sea. Earth Planet Sci Lett 212:361–375
Haese R, Hensen C, De Lange GJ (2006) Pore water geochemistry of eastern Mediterranean mud volcanoes: implications for fluid transport and fluid origin. Mar Geol 225:191–208
Henry P, Foucher JP, Lepichon X, Sibuet M, Kobayashi K, Tarits P, Chamotrooke N, Furuta T, Schultheiss P (1992) Interpretation of temperature-measurements from the Kaiko-Nankai Cruise—modeling of fluid-flow in clam colonies. Earth Planet Sci Lett 109(3–4):355–371
Henry P, Le Pichon X, Lallemant S, Lance S, Martin JB, Foucher J-P, Fiala-Médioni A, Rostek F, Guilhaumou N, Pranal V, Castrec M (1996) Fluid flow in and around a mud volcano field seaward of the Barbados accretionary wedge: results from Manon cruise. J. Geophys Res 101(B9):20297–220323
Hensen C, Wallmann K (2004) Methane fluxes and gas hydrate reservoirs in slope sediments along Costa Rica continental margin. EGU 1st General Assembly, Nice, France, EGU04-A-05859
Hensen C, Wallmann K, Schmidt M, Ranero CR, Suess E (2004) Fluid expulsion related to mud extrusion off Costa Rica—a window to the subducting slab. Geology 32:201–204
Hensen C, Nuzzo M, Hornibrook E, Pinheiro LM, Bock B, Magalhães VH , Brückmann W (2007) Sources of mud volcano fluids in the Gulf of Cadiz—indications for hydrothermal imprint. Geochim Cosmochim Acta 71:1232–1248
Hovland M, Judd AG, Burke JRA (1993) The global flux of methane from shallow submarine sediments. Chemosphere 26(Nos. 1–4):559–578
Hovland M, Svensen H, Forsberg CF, Johansen H, Fichler C, Fossa JH, Jonsson R, Rueslatten H (2005) Complex pockmarks with carbonate-ridges off mid-Norway: products of sediment degassing. Mar Geol 218:191–206
Imhoff JF, Sahling H, Suling J, Kath T (2003) 16S rDNA-based phylogeny of sulphur-oxidising bacterial endosymbionts in marine bivalves from cold-seep habitats. Mar Ecol Progress Ser 249:39–51
Judd AG (2004) Natural seabed gas seeps as sources of atmospheric methane. Environ Geol 46(8):988–996
Karaca D (2011) Quantification of methane fluxes and authigenic carbonate formation at cold seeps along the continental margin offshore Costa Rica: a numerical modeling approach. Ph.D. Thesis, University of Kiel, Kiel, pp 117
Karaca D, Hensen C, Wallmann K (2010) Controls on authigenic carbonate precipitation at cold seeps along the convergent margin off Costa Rica. Geochemistry Geophysics Geosystems 11(Q08S27). doi:10.1029/2010GC003062
Kessler JD, Reeburgh WS, Southon J, Seifert R, Michaelis W, Tyler SC (2006) Basin-wide estimates of the input of methane from seeps and clathrates to the Black Sea. Earth Planet Sci Lett 243(3–4):366–375
Kimura G, Silver E, Blum P, a.c. participants (1997) Proceedings of the Ocean Drilling Program, Initial Reports, vol 170. Ocean Drilling Program, College Station, TX, pp 458
Klaucke I, Masson DG, Petersen CJ, Weinrebe W, Ranero CR (2008) Multifrequency geoacoustic imaging of fluid escape structures offshore Costa Rica: implications for the quantification of seep processes. Geochem Geophys Geosyst 9:Q04010. doi:10.1029/2007gc001708
Kopf A (2002) Significance of mud volcanisms. Rev Geophys 40(2):1–52
Kvenvolden KA, Rogers BW (2005) Gaia’s breath—global methane exhalations. Mar Pet Geol 22(4):579–590
Lichtschlag A, Felden J, Wenzhofer F, Schubotz F, Ertefai TF, Boetius A, de Beer D (2010) Methane and sulfide fluxes in permanent anoxia: in situ studies at the Dvurechenskii mud volcano (Sorokin Trough, Black Sea). Geochim Cosmochim Acta 74(17):5002–5018
Linke P, Wallmann K, Suess E, Hensen C, Rehder G (2005) In-situ benthic fluxes from an intermittently active mud volcano at the Costa Rica convergent margin. Earth Planet Sci Lett 235:79–95
Linke P, Sommer S, Rovelli L, McGinnis DF (2010) Physical limitations of dissolved methane fluxes: the role of bottom-boundary layer processes. Mar Geol 272(1–4):209–222
Luff R, Wallmann K (2003) Fluid flow, methane fluxes, carbonate precipitation and biogeochemical turnover in gas hydrate-bearing sediments at Hydrate Ridge, Cascadia Margin: numerical modeling and mass balances. Geochim Cosmochim Acta 67(18):3403–3421
Luff R, Wallmann K, Grandel S, Schlüter M (2000) Numerical modelling of benthic processes in the deep Arabian Sea. Deep Sea Res II 47(14):3039–3072
Luyendyk B, Kennett J, Clark JF (2005) Hypothesis for increased atmospheric methane input from hydrocarbon seeps on exposed continental shelves during glacial low sea level. Mar Pet Geol 22(4):591–596
Mau S, Sahling H, Rehder G, Suess E, Linke P, Soeding E (2006) Estimates of methane output from mud extrusions at the erosive convergent margin off Costa Rica. Mar Geol 225:129–144
Niemann H, Losekann T, de Beer D, Elvert M, Nadalig T, Knittel K, Amann R, Sauter EJ, Schluter M, Klages M, Foucher JP, Boetius A (2006) Novel microbial communities of the Haakon Mosby mud volcano and their role as a methane sink. Nature 443(7113):854–858
Ranero CR, Von Huene R (2000) Subduction erosion along the Middle America convergent margin. Nature 404:748–752
Ranero CR, Grevemeyer I, Sahling H, Barckhausen U, Hensen C, Wallmann K, Weinrebe W, Vannucchi P, von Huene R, McIntosh K (2008) Hydrogeological system of erosional convergent margins and its influence on tectonics and interplate seismogenesis. Geochem Geophys Geosyst 9(3):Q03S04. doi:10.1029/2007GC001679
Reeburgh WS (2007) Oceanic methane biogeochemistry. Chem Rev 107(2):486–513
Sahling H, Masson DG, Ranero CR, Hühnerbach V, Weinrebe W, Klaucke I, Bürk D, Brückmann W, Suess E (2008) Fluid seepage at the continental margin offshore Costa Rica and southern Nicaragua. Geochem Geophys Geosyst 9:Q05S05. doi:10.1029/2008GC001978
Schleicher T (2006) Bestimmung von ventspezifischen Faunenvergesellschaftungen am mittelamerikanischen Kontinentalrand mit Hilfe quantitativer Videoauswertung. Diploma Thesis University of Kiel, Kiel, p 68
Schmidt M, Hensen C, Mörz T, Müller C, Grevemeyer I, Wallmann K, Mau S, Kaul N (2005) Methane hydrate accumulation in “Mound 11” mud volcano, Costa Rica forearc. Mar Geol 216:83–100
Schneider von Deimling J, Rehder G, Greinert J, McGinnnis DF, Boetius A, Linke P (2011) Quantification of seep-related methane gas emissions at Tommeliten, North Sea. Cont Shelf Res 31:867–878
Solomon EA, Kastner M, Jannasch H, Robertson G, Weinstein Y (2008) Dynamic fluid flow and chemical fluxes associated with a seafloor gas hydrate deposit on the northern Gulf of Mexico slope. Earth Planet Sci Lett 270(1–2):95–105
Sommer S, Pfannkuche O, Linke P, Luff R, Greinert J, Drews M, Gubsch S, Pieper M, Poser M, Viergutz T (2006) Efficiency of the benthic filter: biological control of the emission of dissolved methane from sediments containing shallow gas hydrates at Hydrate Ridge. Global Biogeochem Cycles 20(2):Gb2019. doi:10.1029/2004gb002389
Sommer S, Linke P, Pfannkuche O, Schleicher T, von Deimling JS, Reitz A, Haeckel M, Flogel S, Hensen C (2009) Seabed methane emissions and the habitat of frenulate tubeworms on the Captain Arutyunov mud volcano (Gulf of Cadiz). Mar Ecol Progress Ser 382:69–86
Tishchenko P, Hensen C, Wallmann K, Wong CS (2005) Calculation of the stability and solubility of methane hydrate in seawater. Chem Geol 219(1–4):37–52
Torres ME, McManus J, Hammond DE, de Angelis MA, Heeschen KU, Colbert SL, Tryon MD, Brown KM, Suess E (2002) Fluid and chemical fluxes in and out of sediments hosting methane hydrate deposits on Hydrate Ridge, OR, I: hydrological provinces. Earth Planet Sci Lett 201(3–4):525–540
Treude T, Boetius A, Knittel K, Wallmann K, Jørgensen BB (2003) Anaerobic oxidation of methane above gas hydrates. Mar Ecol Prog Ser 264:1–14
Tryon MD, Wheat CG, Hilton DR (2010) Fluid sources and pathways of the Costa Rica erosional convergent margin. Geochemistry Geophysics Geosystems 11:Q04s22. doi:10.1029/2009gc002818
Vannucchi P, Ranero CR, Galeotti S, Straub SM, Scholl DW, McDougall-Ried K (2003) Fast rates of subducting erosion along the Costa Rica Pacific margin: implications for nonsteady rates of crustal recycling at subduction zones. J Geophys Res 108(No. B11). doi:10.1029/2002JB002207
von Huene R, Ranero CR, Weinrebe W, Hinz K (2000) Quaternary convergent margin tectonics of Costa Rica, segmentation of the Cocos Plate, and Central American volcanism. Tectonics 19(2):314–334
von Huene R, Ranero CR, Watts P (2004) Tsunamigenic slope failure along the Middle America Trench in two tectonic settings. Mar Geol 203(3–4):303–317
Wallmann K, Linke P, Suess E, Bohrmann G, Sahling H, Schlüter M, Dählmann A, Lammers S, Greinert J, Mirbach Nv (1997) Quantifying fluid flow, solute mixing, and biogeochemical turnover at cold vents of the eastern Aleutian subduction zone. Geochim Cosmochim Acta 61(24):5209–5219
Wallmann K, Drews M, Aloisi G, Bohrmann G (2006) Fluid expulsion from the Dvurechenskii mud volcano (Black Sea): part II. Methane fluxes and new estimates of global methane discharge into the ocean via submarine mud volcanism. Earth Planet Sci Lett 248:544–559
Acknowledgments
We would like to thank the captains, crew members and the members of the scientific parties of R/V Sonne cruise SO173/2 and R/V Meteor cruise M66/2 for their helpful assistance at sea. Many thanks to Anke Bleyer, Bettina Domeyer and Regina Surberg for having carried out the chemical analyses onboard and at shore-based laboratories. This work was funded by the German Science Foundation (DFG). This publication is contribution no. 235 of the Sonderforschungsbereich 574 “Volatiles and Fluids in Subduction Zones” at Kiel University.
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Karaca, D., Schleicher, T., Hensen, C. et al. Quantification of methane emission from bacterial mat sites at Quepos Slide offshore Costa Rica. Int J Earth Sci (Geol Rundsch) 103, 1817–1829 (2014). https://doi.org/10.1007/s00531-012-0839-3
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DOI: https://doi.org/10.1007/s00531-012-0839-3