Mg isotope fractionation during calcite precipitation: An experimental study

Type : ACL
Nature : Production scientifique
Au bénéfice du Laboratoire : Non
Statut de publication : Publié
Année de publication : 2012
Auteurs (4) : SAULNIER S ROLLION-BARD C VIGIER Nathalie CHAUSSIDON M
Revue scientifique : Geochimica et Cosmochimica Acta
Volume : 91
Fascicule :
Pages : 75-91
DOI : 10.1016/j.gca.2012.05.024
URL : <go to isi>://wos:000307120800006
Abstract : Experimental precipitations of calcite and other carbonate minerals were performed under various conditions of pH, temperature and solution Mg/Ca to determine the Mg partition coefficient and Mg isotope fractionation. Fifteen experiments were performed at pH ranging from 7.41 +/- 0.07 to 8.51 +/- 0.39, temperature ranging from 16.2 +/- 0.7 to 26.5 +/- 0.3 degrees C and Mg/Ca-solution ranging from 0.11 to 0.52 mol/mol. The apparent Mg partition coefficient between calcite and solution (D-Mg) spans a large range of values from 0.018 +/- 0.014 to 0.15 +/- 0.11 and carbonate Mg isotope fractionation (Delta Mg-26) ranges from -2.53 +/- 0.25 parts per thousand to -1.33 +/- 0.14 parts per thousand and does not correlate with either pH or temperature. The range in D-Mg and Delta Mg-26 suggests non-equilibrium partitioning controlled by the processes of calcite growth, i.e. mixing between calcite grown at equilibrium and fluid inclusions, and entrapment of a surface Mg-rich calcite layer in isotopic equilibrium with the solution. The equilibrium Mg isotope fractionation between inorganic calcite and solution is estimated to be -2.13 +/- 0.24 parts per thousand. Additional Mg elemental and isotopic fractionations are observed to occur during biogenic formation of calcite due to variable removal of Mg by the organisms (high-Mg calcite corals, foraminifera) of seawater Mg from their calcification medium. (C) 2012 Elsevier Ltd. All rights reserved.
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Citation :
Saulnier S, Rollion-Bard C, Vigier N, Chaussidon M (2012) Mg isotope fractionation during calcite precipitation: An experimental study. Geochim Cosmochim Ac 91: 75-91 | doi: 10.1016/j.gca.2012.05.024