Late seafloor carbonate precipitation in serpentinites from the Rainbow and Saldanha sites (Mid-Atlantic Ridge)
Ribeiroda Costa, Isabel; Barriga, Fernando J.A.S. Taylor
European Journal of Mineralogy Volume 20 Number 2 (2008), p. 173 - 181
published: Apr 30, 2008
ArtNo. ESP147052002002, Price: 29.00 €
Serpentinized ultramafic rocks recovered during several recent oceanographic missions (1997-2002) on the Rainbow hydrothermal field and on the Saldanha seamount (36°14'N and 36°34'N, Mid-Atlantic Ridge) often exhibit late-stage carbonatization associated to secondary oxidation effects. These carbonate occurrences, mostly vein-filling aragonite, occasionally form dense webs almost completely engulfing and replacing the serpentinite itself.The 87Sr/86Sr (approx. 0.709) and stable isotope signatures (δ13CPDB = 0.2-3.3 ‰; δ18OV-SMOW = 32.2-35.2 ‰) of the carbonate fraction in these serpentinites indicate carbonate precipitation from unmodified seawater, under abiotic conditions, and very low temperatures, close to bottom-water temperatures measured at the sampling stations. These analytical data imply that, unlike the serpentinite-hosted carbonate chimneys in the Lost City hydrothermal field (Ludwig et al., 2006), the vein-filling aragonite in the Rainbow and Saldanha serpentinites has a non-hydrothermal, low-temperature seawater origin.