TY - ABST

T1 - Chromium isotope fractionation during coprecipitation with calcium carbonate

AU - Rodler, Alexandra

AU - Sánchez-Pastor, Nuria

AU - Fernández-Díaz, Lurdes

AU - Frei, Robert

PY - 2015

Y1 - 2015

N2 - The chromium (Cr) isotopic composition of carbonates can potentially be used as a paleoclimate proxy to elucidate past fluctuations of oxygen contents in atmosphere and hydrosphere. The use of Cr isotopes to track paleoenvironmental changes, for example related to the rise of oxygen during the Archaean and Protoerozoic, needs careful assessment of the signal robustness and necessitates a thorough understanding of the Cr cycle in Earth system processes. We conducted experiments testing the incorporation and isotopic fractionation of chromate into the calcite lattice. Our experiments indicate enrichment in Cr concentration and preferential incorporation of heavy Cr isotopes in the precipitates. Further, experiments following the procedure of [1], showed an increasing relative isotope difference between precipitate and initial solution (Δ53Cr[p-is]) from +0.06 to +0.18 ‰ with increasing initial Cr solution concentration. Another set of experiments conducted in double diffusion silica hydrogel [2] yielded calcite crystals again significantly enriched in heavy Cr isotopes with [Δ53Cr[p-is]] of +0.29 ± 0.08 ‰ (2σ), whereas silica hydrogel samples show a preferential retention of light Cr isotopes. Previous studies of δ53Cr seawater signals inferred from carbonates may have been too positive. However, considering that seawater Cr concentrations are significantly lower than those chosen for our experiments, a trend towards lower [Δ53Cr[p-is]] at lower initial Cr concentrations could mean marginal to no Cr isotope fractionation in the oceans. These experiments represent a first step toward understanding the Cr isotope signal of carbonates where fractionations will likely be ≤ 0.3 ‰ and as such, pave the way for future work to enable a reliable application of the Cr isotope proxy.References: [1] Hua et al., 2007, Water Air Soil Poll. 179, 381-390. [2] Sánchez-Pastor et al., 2011, Cryst. Growth Des. 11, 3081-3089.

AB - The chromium (Cr) isotopic composition of carbonates can potentially be used as a paleoclimate proxy to elucidate past fluctuations of oxygen contents in atmosphere and hydrosphere. The use of Cr isotopes to track paleoenvironmental changes, for example related to the rise of oxygen during the Archaean and Protoerozoic, needs careful assessment of the signal robustness and necessitates a thorough understanding of the Cr cycle in Earth system processes. We conducted experiments testing the incorporation and isotopic fractionation of chromate into the calcite lattice. Our experiments indicate enrichment in Cr concentration and preferential incorporation of heavy Cr isotopes in the precipitates. Further, experiments following the procedure of [1], showed an increasing relative isotope difference between precipitate and initial solution (Δ53Cr[p-is]) from +0.06 to +0.18 ‰ with increasing initial Cr solution concentration. Another set of experiments conducted in double diffusion silica hydrogel [2] yielded calcite crystals again significantly enriched in heavy Cr isotopes with [Δ53Cr[p-is]] of +0.29 ± 0.08 ‰ (2σ), whereas silica hydrogel samples show a preferential retention of light Cr isotopes. Previous studies of δ53Cr seawater signals inferred from carbonates may have been too positive. However, considering that seawater Cr concentrations are significantly lower than those chosen for our experiments, a trend towards lower [Δ53Cr[p-is]] at lower initial Cr concentrations could mean marginal to no Cr isotope fractionation in the oceans. These experiments represent a first step toward understanding the Cr isotope signal of carbonates where fractionations will likely be ≤ 0.3 ‰ and as such, pave the way for future work to enable a reliable application of the Cr isotope proxy.References: [1] Hua et al., 2007, Water Air Soil Poll. 179, 381-390. [2] Sánchez-Pastor et al., 2011, Cryst. Growth Des. 11, 3081-3089.

M3 - Conference abstract for conference

T2 - Goldschmidt

Y2 - 16 August 2015 through 21 August 2015

ER -