09 Vol. 37 — N° 3 13 P.297 – 317 Nickel Isotope Variations in Terrestrial Silicate Rocks and Geological Reference Materials Measured by MC-ICP-MS Bleuenn Gueguen (1, 2)*,OlivierRouxel (1, 2), Emmanuel Ponzevera (2),AndreyBekker (3) and Yves Fouquet (2) (1) Institut Universitaire Europeen de la Mer, UMR 6538, Universite de Bretagne Occidentale, BP 80, F-29280, Plouzane, France (2) IFREMER, Centre de Brest, UniteG eosciences Marines, 29280, Plouzane, France (3) Department of Geological Sciences, University of Manitoba, Winnipeg, R3T 2N2, Canada * Corresponding author. e-mail:
[email protected] Although initial studies have demonstrated the applica- Bien que les premieres etudes demontrent la pertinence bility of Ni isotopes for cosmochemistry and as a potential des isotopes du nickel en cosmochimie et en tant que biosignature, the Ni isotope composition of terrestrial signature biologique, la composition isotopique du nickel igneous and sedimentary rocks, and ore deposits remains des roches ignees et sedimentaires terrestres ainsi que poorly known. Our contribution is fourfold: (a) to detail an celle des dep ots^ de minerais est encore tres peu connue. analytical procedure for Ni isotope determination, (b) to Notre contribution s’organise en quatre axes, (a) detailler determine the Ni isotope composition of various geo- la procedure analytique pour la determination des logical reference materials, (c) to assess the isotope compositions isotopiques en nickel, (b) determiner la composition of the Bulk Silicate Earth relative to the Ni composition isotopique de materiaux geologiques de isotope reference material NIST SRM 986 and (d) to ref erence varies, (c) estimer la composition isotopique de report the range of mass-dependent Ni isotope fractio- la Terre Silicatee Globale (BSE) par rapport au standard nations in magmatic rocks and ore deposits.