Articles | Volume 10, issue 4
https://doi.org/10.5194/se-10-1243-2019
https://doi.org/10.5194/se-10-1243-2019
Research article
 | 
31 Jul 2019
Research article |  | 31 Jul 2019

Precipitation of dolomite from seawater on a Carnian coastal plain (Dolomites, northern Italy): evidence from carbonate petrography and Sr isotopes

Maximilian Rieder, Wencke Wegner, Monika Horschinegg, Stefanie Klackl, Nereo Preto, Anna Breda, Susanne Gier, Urs Klötzli, Stefano M. Bernasconi, Gernot Arp, and Patrick Meister

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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Patrick Meister on behalf of the Authors (14 May 2019)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (05 Jun 2019) by Elias Samankassou
RR by Anonymous Referee #2 (17 Jun 2019)
ED: Publish subject to technical corrections (27 Jun 2019) by Elias Samankassou
ED: Publish subject to technical corrections (27 Jun 2019) by Elias Samankassou (Executive editor)
AR by Patrick Meister on behalf of the Authors (30 Jun 2019)  Manuscript 
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Short summary
The formation of dolomite (CaMg(CO3)2), an abundant mineral in Earth's geological record, is still incompletely understood. We studied dolomites embedded in a 100 m thick succession of coastal alluvial clays of Triassic age in the southern Alps. Observation by light microscopy and Sr isotopes suggests that dolomites may spontaneously from concentrated evaporating seawater, in coastal ephemeral lakes or tidal flats along the western margin of the Triassic Tethys sea.