|
In press: October 6 IN PREPARATION December 2009 • Low-Temperature Metal Stable Isotope Geochemistry During the past decade it has been recognized that the stable isotope compositions of several metallic elements vary significantly in nature due to both biotic and abiotic processing. While this leap in our understanding has been fueled by recent advances in instrumentation and techniques in both thermal ionization and inductively coupled plasma mass spectrometry, the field of metal stable isotope geochemistry has finally moved beyond a focus on development of analytical techniques and toward using the isotopes as source and process tracers in natural and experimental systems. Often termed the “non-traditional stable isotopes,” metal stable isotope systems have found wide application in the geological, hydrological, and environmental research realms and are enjoying a rapidly expanding presence in the scientific literature. This issue of Elements will focus on several intriguing aspects of low-temperature metal stable isotope geochemistry. ____________________________________ A publication of the Mineralogical Society of America, the Mineralogical Society of Great Britain and Ireland, the Geochemical Society, the Mineralogical Association of Canada, The Clay Minerals Society, the International Association of GeoChemistry, the European Association for Geochemistry, the Société Française de Minéralogie et de Cristallographie, the Association of Applied Geochemists, the Deutsche Mineralogische Gesellschaft, the International Association of Geoanalysts, the Società Italiana di Mineralogia e Petrologia, the Polskie Towarzystwo Mineralogiczne (Mineralogical Society of Poland), the Sociedad Española de Mineralogía (Spanish Mineralogical Society), and the Swiss Society of Mineralogy and Petrology) |
|||||