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author Deußen, Katharina
Voigt, Claudia
Staubwasser, Michael
Münker, Carsten
El-Shenawy, Mohammed
Klipsch, Swea
Herwartz, Daniel
author_facet Deußen, Katharina
Voigt, Claudia
Staubwasser, Michael
Münker, Carsten
El-Shenawy, Mohammed
Klipsch, Swea
Herwartz, Daniel
collection Datos científicos de ciencias marinas y ambientales
contents Gypsum samples collected in two outcrops located in the Polemi basin, Cyprus, have been analyzed for their triple oxygen and hydrogen isotopic composition. Respective methods are described in the original publication. The oxygen and hydrogen data provided here is derived from the crystal bound H2O within the Gypsum (CaSO4*2H2O), which allows calculating paleo-water isotopic compositions of the mother brine from which this gypsum precipitated during the Messinian Salinity Crisis. Because the isotopic composition of the mother brine is affected by the local hydroclimate at that time, such analyses allow reconstructing paleo-hydroclimate. One aim of the study was to reconstruct paleo-relative humidity of the Messinian Salinity Crisis. For this purpose, the triple oxygen and hydrogen isotope data was fitted to an appropriate isotope model that is based on the Craig and Gordon formula, which provides absolute paleo-relative humidity estimates. Model input and output data are summarized in Table S2.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_967561
institution PANGAEA
language en
publishDate 2024
publisher PANGAEA
record_format pangaea
spellingShingle Triple oxygen and hydrogen isotope data of gypsum from Cyprus
Deußen, Katharina
Voigt, Claudia
Staubwasser, Michael
Münker, Carsten
El-Shenawy, Mohammed
Klipsch, Swea
Herwartz, Daniel
Cyprus; Date of determination; Deuterium excess; Deuterium excess, standard deviation; Event label; Isotope ratio mass spectrometer (IRMS), Thermo Fisher, MAT253; Messinian Salinity Crisis; OUTCROP; Outcrop 1; Outcrop 2; Outcrop ID; Outcrop sample; Oxygen-17 excess; Oxygen-17 excess, standard deviation; Paleoceanography; paleohumidity; Polemi_basin_gypsum_outcrop_1; Polemi_basin_gypsum_outcrop_2; Sample code/label; Sample ID; Seawater δ18O; Sr isotopes; Time point, descriptive; triple oxygen isotopes; δ17O, water; δ17O, water, standard deviation; δ18O, water; δ18O, water, standard deviation; δ Deuterium; δ Deuterium, standard deviation
Gypsum samples collected in two outcrops located in the Polemi basin, Cyprus, have been analyzed for their triple oxygen and hydrogen isotopic composition. Respective methods are described in the original publication. The oxygen and hydrogen data provided here is derived from the crystal bound H2O within the Gypsum (CaSO4*2H2O), which allows calculating paleo-water isotopic compositions of the mother brine from which this gypsum precipitated during the Messinian Salinity Crisis. Because the isotopic composition of the mother brine is affected by the local hydroclimate at that time, such analyses allow reconstructing paleo-hydroclimate. One aim of the study was to reconstruct paleo-relative humidity of the Messinian Salinity Crisis. For this purpose, the triple oxygen and hydrogen isotope data was fitted to an appropriate isotope model that is based on the Craig and Gordon formula, which provides absolute paleo-relative humidity estimates. Model input and output data are summarized in Table S2.
title Triple oxygen and hydrogen isotope data of gypsum from Cyprus
topic Cyprus; Date of determination; Deuterium excess; Deuterium excess, standard deviation; Event label; Isotope ratio mass spectrometer (IRMS), Thermo Fisher, MAT253; Messinian Salinity Crisis; OUTCROP; Outcrop 1; Outcrop 2; Outcrop ID; Outcrop sample; Oxygen-17 excess; Oxygen-17 excess, standard deviation; Paleoceanography; paleohumidity; Polemi_basin_gypsum_outcrop_1; Polemi_basin_gypsum_outcrop_2; Sample code/label; Sample ID; Seawater δ18O; Sr isotopes; Time point, descriptive; triple oxygen isotopes; δ17O, water; δ17O, water, standard deviation; δ18O, water; δ18O, water, standard deviation; δ Deuterium; δ Deuterium, standard deviation
url https://doi.org/10.1594/PANGAEA.967561