146
Fouquet, Y., Cambon, P., Etoubleau, J., Charlou, J.-L., Ondréas, H., Barriga, F., Cherkashov, G.,
Semkova, T., Poroshina, I., Bohn, M., Donval, J.-P., Henry, K., Murphy, P., & Rouxel, O.
(2010). Geodiversityof hydrothermal processalong the Mid-Atlantic Ridge and ultramafichosted mineralization: a new type of oceanic Cu-Zn-Co-Au volcanogenicmassive sulphide deposit. In P. Rona, C. Devey, J. Dyment, & B. Murton (eds.), Diversity of hydrothermal systems
on slow spreading ocean ridges (pp. 321–367) edited by AGU Geophysical Monograph Series,
188.
Hein, J., Koschinsky, A., Bau, M., Manhein, F., Kang, J. K., & Robert, L. (2000) Cobalt-Rich Ferromanganese Crust in the Pacific. In D. Cronan (ed.), Handbook of marine mineral deposits
(pp. 239–279). CRC Press London.
Hoffert, M., 2008. Les nodules polymétalliques dans les grands fonds océaniques (p. 429). Société
géologique de France, Éditions Vuibert.
Lenoble, J.-P. (1996). Les nodules polymétalliques, bilan de 30 ans de travaux dans le monde.
Chronique de la Recherche Minière, 524, 15–37.
Rona, P. (2003). Resources of the seafloor. Science, 299, 673–674.
Scott, S. D. (2001). Deep Ocean mining. Geoscience Canada, 28(2), 87–94.
Scientific Knowledge and Challenges Related to Hydrogen
Cannat, M., Fontaine, F., & Escartin, J. (2010). Serpentinizationand associated hydrogen and
methane fluxes at slow-spreading Ridges. In P. Rona, C. Devey, J. Dyment, & B. Murton (eds.),
Diversity of hydrothermal systems on slow-spreading ocean ridges (pp. 241–264).
Charlou, J.-L., Bougault, H., Appriou, P., Nelsen, T., & Rona, P. (1991). Different TDM/CH 4 hydrothermal plume signatures: TAG site at 26° N and serpentinized ultrabasic diapir at 15° 05’
N on the Mid-Atlantic Ridge. Geochimica Cosmochimica Acta, 55(11), 3209–3222.
Charlou, J.-L., & Donval, J.-P. (1993). Hydrothermal methane venting between 12° N and 26° N
along the Mid-Atlantic Ridge. Journal of Geophysical Research, 98(B6), 9625–9642.
Charlou, J.-L., Fouquet, Y., Bougault, H., Donval, J.-P., Etoubleau, J., Jean-Baptiste, P., Dapoigny,
A., Appriou, P., & Rona, P. A. (1998). Intense CH 4 plumes generated by serpentinization of
ultramafic rocks at the intersection of the 15° 20’ N Fracture Zone and the Mid-Atlantic Ridge.
Geochimica Cosmochimica Acta, 62(13), 2323–2333.
Charlou, J.L., Donval, J.-P., Douville, E., Jean-Baptiste, P., Radford-Knoery, J., Fouquet, J.,
Dapoigny, A., & Stievenard, M. (2000). Compared geochemical signatures and the evolution
of Menez Gwen (37° 50’ N) and Lucky Strike (37° 17’ N) hydrothermal fluids, south of the
Azores Triple Junction on the Mid-Atlantic Ridge. Chemical Geology, 171, 49–75.
Charlou, J. L., Donval, J.-P., Fouquet, Y., Jean-Baptiste, P., & Holm, N. G. (2002). Geochemistry
of high H 2 and CH 4 vent fluids issuing from ultramafic rocks at the Rainbow hydrothermal
field (36° 14’ N, MAR). Chemical Geology, 191, 345–359.
Charlou, J.-L., Donval, J.-P., Ondreas, H., Fouquet, Y., Jean-Baptiste, P., & Fourré, E. (2010). High
production and fluxes of H 2 and CH 4 and evidence of abiotic hydrocarbon synthesis by serpentinization in ultramafic-hosted hydrothermal systems on the Mid-Atlantic Ridge. In P. Rona, C.
Devey, J. Dyment, & B. Murton (eds.), Diversity of hydrothermal systems on Slow-Spreading
Ocean Ridges (pp. 265–296).
Emmanuel, S., & AgueJ. J. (2007). Implications of present-day abiogenic methane fluxes for the
early Archean atmosphere. Geophysical Research Letters, 34, L-15810.
Holloway, J. R., & O’Day, P. A. (2000). Production of CO 2 and H 2 by diking-eruptive events at
mid-ocean ridges: Implications for abiotic synthesis and global geochemical cycling. International Geology Review, 42, 673–683.
Holm, N. G., & Charlou, J.-L. 2001. Initial indications of abiotic formation of hydrocarbons in
the Rainbow ultramafic hydrothermal system, Mid-Atlantic Ridge. Earth Planetary Science
Letters, 191, 1–8.
Bibliography
Fouquet, Y., Cambon, P., Etoubleau, J., Charlou, J.-L., Ondréas, H., Barriga, F., Cherkashov, G.,
Semkova, T., Poroshina, I., Bohn, M., Donval, J.-P., Henry, K., Murphy, P., & Rouxel, O.
(2010). Geodiversityof hydrothermal processalong the Mid-Atlantic Ridge and ultramafichosted mineralization: a new type of oceanic Cu-Zn-Co-Au volcanogenicmassive sulphide deposit. In P. Rona, C. Devey, J. Dyment, & B. Murton (eds.), Diversity of hydrothermal systems
on slow spreading ocean ridges (pp. 321–367) edited by AGU Geophysical Monograph Series,
188.
Hein, J., Koschinsky, A., Bau, M., Manhein, F., Kang, J. K., & Robert, L. (2000) Cobalt-Rich Ferromanganese Crust in the Pacific. In D. Cronan (ed.), Handbook of marine mineral deposits
(pp. 239–279). CRC Press London.
Hoffert, M., 2008. Les nodules polymétalliques dans les grands fonds océaniques (p. 429). Société
géologique de France, Éditions Vuibert.
Lenoble, J.-P. (1996). Les nodules polymétalliques, bilan de 30 ans de travaux dans le monde.
Chronique de la Recherche Minière, 524, 15–37.
Rona, P. (2003). Resources of the seafloor. Science, 299, 673–674.
Scott, S. D. (2001). Deep Ocean mining. Geoscience Canada, 28(2), 87–94.
Scientific Knowledge and Challenges Related to Hydrogen
Cannat, M., Fontaine, F., & Escartin, J. (2010). Serpentinizationand associated hydrogen and
methane fluxes at slow-spreading Ridges. In P. Rona, C. Devey, J. Dyment, & B. Murton (eds.),
Diversity of hydrothermal systems on slow-spreading ocean ridges (pp. 241–264).
Charlou, J.-L., Bougault, H., Appriou, P., Nelsen, T., & Rona, P. (1991). Different TDM/CH 4 hydrothermal plume signatures: TAG site at 26° N and serpentinized ultrabasic diapir at 15° 05’
N on the Mid-Atlantic Ridge. Geochimica Cosmochimica Acta, 55(11), 3209–3222.
Charlou, J.-L., & Donval, J.-P. (1993). Hydrothermal methane venting between 12° N and 26° N
along the Mid-Atlantic Ridge. Journal of Geophysical Research, 98(B6), 9625–9642.
Charlou, J.-L., Fouquet, Y., Bougault, H., Donval, J.-P., Etoubleau, J., Jean-Baptiste, P., Dapoigny,
A., Appriou, P., & Rona, P. A. (1998). Intense CH 4 plumes generated by serpentinization of
ultramafic rocks at the intersection of the 15° 20’ N Fracture Zone and the Mid-Atlantic Ridge.
Geochimica Cosmochimica Acta, 62(13), 2323–2333.
Charlou, J.L., Donval, J.-P., Douville, E., Jean-Baptiste, P., Radford-Knoery, J., Fouquet, J.,
Dapoigny, A., & Stievenard, M. (2000). Compared geochemical signatures and the evolution
of Menez Gwen (37° 50’ N) and Lucky Strike (37° 17’ N) hydrothermal fluids, south of the
Azores Triple Junction on the Mid-Atlantic Ridge. Chemical Geology, 171, 49–75.
Charlou, J. L., Donval, J.-P., Fouquet, Y., Jean-Baptiste, P., & Holm, N. G. (2002). Geochemistry
of high H 2 and CH 4 vent fluids issuing from ultramafic rocks at the Rainbow hydrothermal
field (36° 14’ N, MAR). Chemical Geology, 191, 345–359.
Charlou, J.-L., Donval, J.-P., Ondreas, H., Fouquet, Y., Jean-Baptiste, P., & Fourré, E. (2010). High
production and fluxes of H 2 and CH 4 and evidence of abiotic hydrocarbon synthesis by serpentinization in ultramafic-hosted hydrothermal systems on the Mid-Atlantic Ridge. In P. Rona, C.
Devey, J. Dyment, & B. Murton (eds.), Diversity of hydrothermal systems on Slow-Spreading
Ocean Ridges (pp. 265–296).
Emmanuel, S., & AgueJ. J. (2007). Implications of present-day abiogenic methane fluxes for the
early Archean atmosphere. Geophysical Research Letters, 34, L-15810.
Holloway, J. R., & O’Day, P. A. (2000). Production of CO 2 and H 2 by diking-eruptive events at
mid-ocean ridges: Implications for abiotic synthesis and global geochemical cycling. International Geology Review, 42, 673–683.
Holm, N. G., & Charlou, J.-L. 2001. Initial indications of abiotic formation of hydrocarbons in
the Rainbow ultramafic hydrothermal system, Mid-Atlantic Ridge. Earth Planetary Science
Letters, 191, 1–8.
Bibliography