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For the first time δ18O and δ13C values from carbonates and δD values of individual n-alkanes were used to reconstruct palaeohydrological conditions in a lagoon at the southern margin of the Central European Zechstein Basin (CEZB). A 12-m core covering the complete Ca2 interval and adjacent anhydrites (A1 and A2) was analyzed for δ18O and δ13C values of dolomitized carbonates and δD values of individual...
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