Inter-mineral Mg isotope fractionation during hydrothermal ultramafic rock alteration: Implications for the global Mg-cycle
MetadataShow full item record
Both riverine and ocean waters are enriched in 24Mg compared to the homogeneous chondritic Mg isotopic composition of the Earth's mantle requiring a fractionation step that is generally attributed to low temperature continental crust weathering. Here we present new observations that indicate that this 24Mg enrichment of surface waters may originate from Mg isotope fractionation during the hydrothermal alteration of primary silicate minerals. Mineral separates of hydrothermally altered ultramafic rocks were collected from three different localities in Norway. Coexisting olivine and serpentine exhibit invariant Mg isotope ratios suggesting that serpentinization does not fractionate Mg isotopes. In contrast, carbonation results in significant inter-mineral Mg isotope fractionation between the antigorite, magnesite, and talc. The carbonation of the natural samples is constrained by O isotope thermometry at ~275°C and hence closes the temperature gap between previous investigations of the natural distribution of Mg isotopes during surface weathering and magmatic processes. The precursor antigorite has an isotopic composition of d26Mg (DSM-3) = - 0.11 ± 0.05‰, whereas the talc is enriched in 26Mg with mean dMg26=0.17±0.08‰ and the magnesite is depleted in 26Mg with mean dMg26=-0.95±0.15‰. As carbonate minerals dissolve faster than silicate minerals, the chemical weathering of carbonated ultramafic and by analogy mafic rocks on the continents will yield isotopically lighter Mg to natural surface waters consistent with field observations. Moreover, the Mg fractionation observed in this study suggests that sub-seafloor hydrothermal carbonation may be a significant contribution to the Mg isotopic composition of ocean water. © 2014 Elsevier B.V.
Showing items related by title, author, creator and subject.
Abiogenic Fischer–Tropsch synthesis of methane at the Baogutu reduced porphyry copper deposit, western Junggar, NW-ChinaCao, M.; Qin, K.; Li, G.M.; Evans, Noreen; Jin, L.Y. (2014)Methane is widely developed in hydrothermal fluids from reduced porphyry copper deposits, but its origin remains enigmatic. The occurrence of methane in fluid inclusions at the Late Carboniferous Baogutu reduced porphyry ...
New insights into the metallogeny of MVT Zn-Pb deposits: A case study from the Nayongzhi in South China, using field data, fluid compositions, and in situ S-Pb isotopesZhou, J.; Wang, Xuan-Ce; Wilde, Simon; Luo, K.; Huang, Z.; Wu, T.; Jin, Z. (2018)© 2018 Walter de Gruyter GmbH, Berlin/Boston. The newly discovered Nayongzhi Zn-Pb deposit ( > 20 Mt ores at 1.11-15.65 wt% Zn and 0.59-0.97 wt% Pb) in NW Guizhou province, South China, is hosted by late Ediacaran and ...
Ore genesis of the Fule Pb–Zn deposit and its relationship with the Emeishan Large Igneous Province: Evidence from mineralogy, bulk C–O–S and in situ S–Pb isotopesZhou, J.; Luo, K.; Wang, Xuan-Ce; Wilde, Simon; Wu, T.; Huang, Z.; Cui, Y.; Zhao, J. (2018)© 2017 International Association for Gondwana Research Magmatic activity plays an important role in mineralization, but little is understood of its role with respect to carbonate-hosted stratabound epigenetic Pb–Zn deposits. ...