Published in “Geochimica et Cosmochimica Acta” volume 245, pages 316-326. DOI: https://doi.org/10.1016/j.gca.2018.11.010. Use the above information when citing this article. Chlorine and bromine isotope evolution within a fully developed Upper Permian natural salt sequence HGM Eggenkampa,*, P Louvatb, J Griffioenc,d, P Agriniera aÉquipe de Géochimie des Isotopes Stables, Institut de Physique du Globe de Paris, Sorbonne Paris Cité, UMR 7154, CNRS, 1 rue Jussieu, 75238 Paris Cedex 05, France bÉquipe de Géochimie des Enveloppes Externes, Institut de Physique du Globe de Paris, Sorbonne Paris Cité, UMR 7154, CNRS, 1 rue Jussieu, 75238 Paris Cedex 05, France cTNO Geological Survey of the Netherlands, P.O. Box 80015, Utrecht, The Netherlands dCopernicus Institute of Sustainable Development, Utrecht University, P.O. Box 80115, Utrecht, The Netherlands *Corresponding author, email
[email protected] Abstract The behaviour of chlorine and bromine isotopes in evaporite deposits differs significantly. We studied the isotope variations of both elements in a fully developed natural salt sequence from Zechstein evaporite deposits (Wuchiapingian, Upper Permian) in the Northern Netherlands. We observed that the Cl isotope variations follow previously predicted characteristics, showing slightly positive δ37Cl (relative to seawater) in halite (NaCl) dominated layers (up to +0.05 ‰), decreasing to moderately negative values in carnallite (KMgCl3•6H2O) and bischofite (MgCl2•6H2O) dominated layers (down to -0.55 ‰). Bromine isotope variations, the first ever measured in marine evaporite samples, show a different characteristic. δ81Br values 1 of 27 decrease quickly in layers dominated by halite (from +0.2 to -0.5 ‰) and increase again in layers dominated by carnallite and bischofite (up to - 0.1±0.2‰).