Fluid chemistry of the low temperature hyperalkaline hydrothermal system of Prony Bay (New Caledonia)
Related subject area
Astrobiology and Exobiology: Extreme Environments, Brines & HydrothermalBiodiversity and trophic ecology of hydrothermal vent fauna associated with tubeworm assemblages on the Juan de Fuca RidgeNitrification of archaeal ammonia oxidizers in a high- temperature hot springArctic gypsum endoliths: a biogeochemical characterization of a viable and active microbial communitySaturated CO2 inhibits microbial processes in CO2-vented deep-sea sedimentsActivity and abundance of denitrifying bacteria in the subsurface biosphere of diffuse hydrothermal vents of the Juan de Fuca Ridge
Biogeosciences, 15, 2629–2647,2018
Biogeosciences, 13, 2051–2060,2016
Biogeosciences, 10, 7661–7675,2013
Biogeosciences, 10, 5639–5649,2013
Biogeosciences, 9, 4661–4678,2012
Arcilla, C. A., Pascua, C. S., and Alexander, W. R.: Hyperalkaline groundwaters and tectonism in the Philippines: significance to natural Carbon Capture and Sequestration, in: 10th International Conference on Greenhouse Gas Control Technologies, Energy Procedia, edited by: Gale, J., Hendriks, C. and Turkenberg, W., 5093–5101, 2011.
Avias, J.: Overthrust structure of the main ultrabasic new caledonian massives, Tectonophysics, 4, 531–541, 1967.
Barnes, I. and O'Neil, J.: The relationship between fluids in some fresh alpine-type ultramafics and possible modern serpentinization, Western United States, Geol. Soc. Am. Bull., 80, 1947–1960, 1969.
Barnes, I., O'Neil, J. R., and Trescases, J. J.: Present day serpentinization in New Caledonia, Oman and Yugoslavia, Geochim. Cosmochim. Ac., 42, 144–145, 1978.
Bénézeth, P., Saldi, G. D., Dandurand, J.-L., and Schott, J.: Experimental determination of the solubility product of magnesite at 50 to 200 °C, Chem. Geol., 286, 21–31, 2011.