Netta Shalev
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View article: Insights into stable strontium isotope fractionation in marine gypsum and its geochemical implications
Insights into stable strontium isotope fractionation in marine gypsum and its geochemical implications Open
View article: Reconstructing past seawater δ88/86Sr from calcium-sulfates (gypsum and anhydrite)
Reconstructing past seawater δ88/86Sr from calcium-sulfates (gypsum and anhydrite) Open
Records of the stable-Sr isotope composition of past seawater, δ88/86Srsw, have recently been demonstrated to be good proxies for the evolution of the marine ‘carbonate factory’, the ultimate sink of carbon from the ocean-…
View article: New insights into the Sr isotope budget from stable-Sr isotope fractionation in gypsum
New insights into the Sr isotope budget from stable-Sr isotope fractionation in gypsum Open
The geochemical cycle of strontium (Sr) is closely tied to the long-term inorganic cycle of carbon since the budgets of both elements are controlled by similar natural processes such as volcanism, continental weathering, and carbonates pre…
View article: Magnesium isotope signature of Middle Ordovician dolomites from the Ordos Basin, China
Magnesium isotope signature of Middle Ordovician dolomites from the Ordos Basin, China Open
As a significant sink of seawater magnesium, δ26Mg values of syndepositional marine dolomites can be utilized to reconstruct seawater Mg isotope composition in the past. This, in turn, may serve as a good tracer for the Mg cycle throu…
View article: Exploring Mg-evaporites and sabkha dolomite as archives for seawater Mg isotope composition
Exploring Mg-evaporites and sabkha dolomite as archives for seawater Mg isotope composition Open
Recent studies of seawater compositions of some ‘non-traditional’ stable isotope systems, such as 26Mg/24Mg (reported as δ26Mg), have uncovered great potential to enhance our understanding of the past Earth. However, diffe…
View article: Understanding the role of gypsum in the global Sr cycle using stable-Sr isotopes
Understanding the role of gypsum in the global Sr cycle using stable-Sr isotopes Open
View article: A reconstruction of ocean δ<sup>26</sup>Mg in the Triassic from dolostones and a new model of Earth surface recovery following the End-Permian
A reconstruction of ocean δ<sup>26</sup>Mg in the Triassic from dolostones and a new model of Earth surface recovery following the End-Permian Open
View article: Magnesium isotopes behavior in coastal aquifers
Magnesium isotopes behavior in coastal aquifers Open
View article: Regulation of hydrothermal vent contribution to ocean chemistry by hydrothermally influenced sediments, the Rainbow field case study
Regulation of hydrothermal vent contribution to ocean chemistry by hydrothermally influenced sediments, the Rainbow field case study Open
View article: Precise determination of dolomite content in marine sediments
Precise determination of dolomite content in marine sediments Open
Dolomite (CaMg[CO 3 ] 2 ) is a common rock‐forming mineral. Nevertheless, its mechanisms of formation and the factors that cause dolomite concentration variations within the sedimentary records constitute long‐standing geochemical question…
View article: Using Precambrian carbonates for seawater isotope reconstructions: constraints from LA-ICP-MS U-Pb geochronology of a post-Sturtian cap dolomite, Brazil
Using Precambrian carbonates for seawater isotope reconstructions: constraints from LA-ICP-MS U-Pb geochronology of a post-Sturtian cap dolomite, Brazil Open
<p>Global seawater isotope reconstructions from Precambrian marine carbonates must overcome particular difficulties on two fronts: i) accurate age constraints for global stratigraphic correlations and interpretations, and ii) the rel…
View article: The Mg isotope signature of marine Mg-evaporites
The Mg isotope signature of marine Mg-evaporites Open
View article: Analytical methods for determination of δ<sup>26</sup>Mg and δ<sup>88/86</sup>Sr in evaporites
Analytical methods for determination of δ<sup>26</sup>Mg and δ<sup>88/86</sup>Sr in evaporites Open
Marine evaporites (such as gypsum and halite) precipitate directly from evaporating seawater, and thus are considered to be good recorders of ocean chemistry.Magnesium and strontium are found in gypsum as trace elements in the crystal latt…
View article: Magnesium and Uranium isotope composition of the Sturtian Jacoca Formation cap dolomite, Brazil
Magnesium and Uranium isotope composition of the Sturtian Jacoca Formation cap dolomite, Brazil Open
The Early Cryogenian period is marked by the Sturtian glaciation episode (ca.720-660 Ma) that triggered a global perturbation to ocean chemistry and to the surface cycles of many elements.However, reconstructing variations in seawater chem…
View article: A Characterisation of Dolomitization in Triassic Dolomites of Ticino, Switzerland, Using δ<sup>26</sup>Mg and Clumped Isotopes
A Characterisation of Dolomitization in Triassic Dolomites of Ticino, Switzerland, Using δ<sup>26</sup>Mg and Clumped Isotopes Open
View article: Sabkha dolomite as an archive for the magnesium isotope composition of seawater
Sabkha dolomite as an archive for the magnesium isotope composition of seawater Open
Recent studies have uncovered the potential of Mg isotopes (δ26Mg) for studying past ocean chemistry, but records of such data are still scarce. Dolomite has been suggested as a promising archive for δ26Mg of seawater. However, its enigmat…
View article: Supplemental Material: Sabkha dolomite as an archive for the magnesium isotope composition of seawater
Supplemental Material: Sabkha dolomite as an archive for the magnesium isotope composition of seawater Open
Mg isotope measurements details, Supplemental Figures S1 and S2, and Supplemental Tables S1–S4.
View article: Supplemental Material: Sabkha dolomite as an archive for the magnesium isotope composition of seawater
Supplemental Material: Sabkha dolomite as an archive for the magnesium isotope composition of seawater Open
Mg isotope measurements details, Supplemental Figures S1 and S2, and Supplemental Tables S1–S4.
View article: New isotope constraints on the Mg oceanic budget point to cryptic modern dolomite formation
New isotope constraints on the Mg oceanic budget point to cryptic modern dolomite formation Open
View article: Mg Isotope Interlaboratory Comparison of Reference Materials from Earth‐Surface Low‐Temperature Environments
Mg Isotope Interlaboratory Comparison of Reference Materials from Earth‐Surface Low‐Temperature Environments Open
To enable quality control of measurement procedures for determinations of Mg isotope amount ratios, expressed as δ 26 Mg and δ 25 Mg values, in Earth‐surface studies, the δ 26 Mg and δ 25 Mg values of eight reference materials ( RM s) were…