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Global Ca Cycles: Coupling of Continental and Oceanic Processes

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Calcium Stable Isotope Geochemistry

Part of the book series: Advances in Isotope Geochemistry ((ADISOTOPE))

Abstract

Calcium is one of the most important mobile metals that can migrate easily between major geochemical reservoirs at the Earth’s surface; the hydrosphere and the biosphere and crust. In doing so calcium plays a key role in regulating climate over million year time-scales, transferring carbon from the atmosphere and storing it as calcium carbonate. Calcium isotopes potentially provide a way of tracing the mobility of calcium  within the Earth surface environment. This chapter reviews the steps where calcium isotopes are fractionated in the weathering and ocean environments, and how these fractionations can be used to constrain mass transfers on both the continents and in the oceans.

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Authors and Affiliations

  1. Department of Earth Sciences, University of Cambridge, Cambridge, UK

    Edward T. Tipper

  2. LHyGeS/EOST, Université de Strasbourg, Strasbourg, France

    Anne-Désirée Schmitt

  3. Laboratoire Chrono-Environnement, Université Bourgogne Franche-Comté, Besançon, France

    Anne-Désirée Schmitt

  4. Institut für Mineralogie, Universität Münster, Münster, Germany

    Nikolaus Gussone

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Tipper, E.T., Schmitt, AD., Gussone, N. (2016). Global Ca Cycles: Coupling of Continental and Oceanic Processes. In: Calcium Stable Isotope Geochemistry. Advances in Isotope Geochemistry. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-540-68953-9_6

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