Abstract
Hydrothermal fluids at the Galapagos Spreading Center (GSC) and at 21°N on the East Pacific Rise were enriched in methane, hydrogen and carbon monoxide by orders of magnitude over ambient bottom water. Nitrous oxide showed both enrichment and depletion in warm vent waters. Each GSC vent field exhibited unique dissolved gas to silica ratios indicating that complex source — sink mechanisms operated within a small geographic region. The CH4/3 He ratio at 21°N was 6.1 × 106 whereas at the GSC, a range of 12.4 to 42 × 106 was seen. At 21°N the H2/3 He ratio was on the order of 100 times that at the GSC. Microbial data showed as many as 109 organisms ml−1 in GSC samples and 105 ml−1 in the hot 21°N waters. These microbial communities are complex and include organisms known to produce and consume the gases discussed here. We conclude that microbial activity in the warm GSC vents is a significant contributing factor in determining the final gas concentrations in the vent waters.
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References
Aminuddin, M. and Nicholas, D. J. D., 1973, Sulphide oxidation linked to the reduction of nitrate and nitrite in Thiobacillus denitrif icans, Biochim. Biophys. Acta, 325:81–93.
Arrhenius, G. (1981) Interaction of ocean-atmosphere with planetary interior. Adv. Space Res., 1: 37–48.
Ballard, R. D., van Andel, T. H. and Holcomb, R. T., 1982, The Galapagos Rift at 86°W 5. Variations in volcanism, structure, and hydrothermal activity along a 30–kilometer segment of the rift valley. J. Geophys. Res., 87: 1149–1161.
Baross, J. A., Lilley, M. D. and Gordon, L. I., 1982a, Is the CH4, I2 and CO venting from submarine hydrothermal systems produced by thermophilic bacteria ? Nature 298: 366–368.
Baross, J. A., Dahm, C. N., Ward, A. K., Lilley, M. D. and Sedell, J. R., 1982b, Initial microbial response in lakes to the Mt. St. Helens eruption. Nature 296: 49–52.
Baross, J. A., Lilley, M. D., Dahm, C. N., and Gordon, L. I., 1982c, Evidence for microbial linkages between CH+ and CO in aquatic environments. EOS, Trans. Am. Geophys.Union , 63: 155.
Cicerone, R. J., Shetter, J. D., Stedman, D. H., Kelly, T. J. and Liu, S. C., 1978, Atmospheric N20: measurements to determine its sources, sinks, and variations. J. Geophys Res., 83: 3042–3050.
Cohen, Y., 1977, Shipboard measurement of dissolved nitrous oxide in seawater by electron capture gas chromatography, Anal. Chem., 49: 1238–1240.
Cohen, Y., 1978, Consumption of dissolved nitrous oxide in an anoxic basin, Saanich Inlet, British Columbia. Nature 272: 235–237.
Cohen, Y. and Gordon, L. I., 1978, Nitrous oxide in the oxygen minimum of the eastern tropical North Pacific: evidence for its consumption during denitrification and possible mechanisms for its production. Deep-Sea Res. 25: 509–524.
Cole, J. A., 1976, Microbial gas metabolism. Adv. Microbial Phys. 14: 1–92.
Corliss, J. B., Dymond, J., Gordon, L. I., Edmond, J. M., von Herzen, R. P., Ballard, R. D., Green, K., Williams, D., Bainbridge, A., Crane, K. and van Andel, T. H., 1979, Submarine thermal springs on the Galapagos Rift. Science 203: 1073–1083.
Craig, H., Welhan, J. A., Kim, K., Poreda, R. and Lupton, J. E., 1980, Geochemical studies of the 21°N EPR hydrothermal fluids. EOS, Trans. Am. Geophys. Union 61: 992.
Craig, H., 1981, Hydrothermal plumes and tracer circulation along the East Pacific Rise: 20°N to 20°S. EOS, Trans. Am. Geophys. Union 62: 893.
Edmond, J. M., Measures, C., McDuff, R. E., Chan, L. H., Collier, R., Grant, B., Gordon, L. I. and Corliss, J. B., 1979a, Ridge crest hydrothermal activity and the balances of the major and minor elements in the ocean: the Galapagos data. Earth Planet. Sci. Lett., 46: 1–18.
Edmond, J. M., Measures,C., Mangum, B., Grant, B., Sclater, F. R., Collier, R., Hudson, A., Gordon, L. I. and Corliss, J. B., 1979b, On the formation of metal-rich deposits at ridge crests. Earth Planet.Sci. Lett., 46: 19–30.
Edmond, J. M., Von Damm, K. L., McDuff, R. E. and Measures, C. I., 1982, Chemistry of hot springs on the East Pacific Rise and their effluent dispersal. Nature 297: 187–191.
Fuchs, G., Thauer, R., Ziegler, H. and Stichler, W., 1979, Carbon isotope fractionation by Methanobacterium thermoautotrophium. Archiv. Microbiol. 120:135–139.
Games, L. M., Hayes, J. M., and Gunsalus, R. P., 1978, Methane-producing bacteria: natural fractionations of the stable carbon isotopes. Geochim. Cosmochim. Acta, 42:1295–1297.
Gerlach, T. M., 1980a, Evaluation of volcanic gas analyses from Kilauea volcano. J. Volcanol. Geotherm. Res., 1:295–317.
Gerlach, T. M., 1980b, Evaluation of volcanic gas analyses from Surtsey volcano, Iceland, 1964–1967. J. Volcanol. Geotherm Res., 8:191–198.
Gerlach, T. M. and Nordlie, B. E., 1975, The C-O-H-S gaseous system, part II: temperature, atomic composition, and molecular equilibria in volcanic gases. Am. J. Sci., 275: 377–394.
Goering, J. J., 1978, Denitrification in marine systems. in: “Microbiology-1978”, D. Schlessinger, ed., American Society for Microbiology, Washington D.C. p. 357–361.
Hallam, N. and Eugster, H. P., 1976, Ammonium silicate stability relations. Contrib. Miner. Petrol. 57:227–244.
Jannasch, H. W. and Wirsen, C. O., 1979, Chemosynthetic primary production at East Pacific sea floor spreading centers. BioSci. 29: 592–598.
Jannasch, H. W. and Wirsen, C. O., 1981, Morphological survey of microbial mats near deep-sea thermal vents. Appl. Environ. Microbiol. 41: 528–538.
Jenkins, W. J., Edmond, J. M. and Corliss, J. B., 1978, Excess 3He and 4He in Galapagos submarine hydrothermal waters. Nature 272: 156–158.
Karl, D. M., Wirsen, C. O. and Jannasch, H. W., 1980, Deep-sea primary production at the Galapagos hydrothermal vents. Science 207: 1345–1347.
Karl, D. M., Burns, D. J., and Orrett, K., 1983, Biomass and in situ growth characteristics of deep sea hydrothermal vent microbial communities, Abs. annual meeting Am. Soc. Microbiol. p. 235, Abs. N 69.
LaZerte, B. D., 1981, The relationship between total dissolved carbon dioxide and its stable carbon isotope ratio in aquatic sediments. Geochim. Cosmochim. Acta, 45:647–656.
Lilley, M. D. and Gordon, L. I., 1979, Methane, nitrous oxide, carbon monoxide, and hydrogen in the hydrothermal vents of the Galapagos Spreading Center. EOS, Trans. Am. Geophys. Union 60:863.
Lilley, M. D., de Angelis, M. A. and Gordon, L. I., 1982, Methane, hydrogen, carbon monoxide and nitrous oxide in submarine hydrothermal vent waters. Nature 300: 48–50.
Lupton, J. E., Weiss, R. F. and Craig, H., 1977, Mantle helium in hydrothermal plumes in the Galapagos Rift. Nature 267: 603–604.
McDuff, R. E. and Edmond, J. M., 1982, On the fate of sulfate during hydrothermal circulation at mid-ocean ridges. Earth Planet. Sci. Lett., 57: 117–132.
Rau, G. H., 1981a, Hydrothermal vent clam and tube worm 13C/12C: further evidence of nonphotosynthetic food sources. Science 213: 338–339.
Rau, G. H., 1981b, Low 15N/14N in hydrothermal vent animals: ecological implications. Nature 289: 484–485.
Rau, G. H. and Hedges, J. I., 1979, Carbon-13 depletion in a hydrothermal vent mussel: suggestion of a chemosynthetic food source. Science 203: 648–649.
Richet, P., Bottinga, Y. and Javoy, M., 1977, A review of hydrogen, carbon, nitrogen, oxygen, sulfur and chlorine stable isotope fractionation among gaseous molecules. Ann. Rev. Earth Planet. Sci., 5: 65–110.
Rosenfeld, W. D. and Silverman, R. S., 1959, Carbon isotope fractionation in bacterial production of methane. Science 130: 1658–1659.
Schink, D. R., Fanning, K. A. and Piety, J., 1966, A sea-bottom sampler that collects both bottom water and sediment simultaneously. J. Mar. Res., 24: 365–373.
Schoell, M., 1980, The hydrogen and carbon isotopic composition of methane from natural gases of various origins. Geochim. Cosmochim. Acta, 44:649–661.
Welhan, J. A. and Craig, H., 1979, Methane and hydrogen in East Pacific Rise hydrothermal fluids. Geophys. Res. Lett., 6: 829–831.
Williams, P. M., Smith, K. L., Druffel, E. M. and Linick, T. W., 1981, Dietary carbon sources of mussels and tubeworms from Galapagos hydrothermal vents determined from tissue 14C activity. Nature 292: 448–449.
Wolery, T. J. and Sleep, N. H., 1976, Hydrothermal circulation and geochemical flux at mid-ocean ridges. J. Geol., 84: 249–275.
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Lilley, M.D., Baross, J.A., Gordon, L.I. (1983). Reduced Gases and Bacteria in Hydrothermal Fluids: The Galapagos Spreading Center and 21°N East Pacific Rise. In: Rona, P.A., Boström, K., Laubier, L., Smith, K.L. (eds) Hydrothermal Processes at Seafloor Spreading Centers. NATO Conference Series, vol 12. Springer, Boston, MA. https://doi.org/10.1007/978-1-4899-0402-7_18
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