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Supplementary Data and figures belongingto the manuscript titled "Tracing timing of growth in cultured mollusks using strontium spiking", published in Frontiers in Marine Science. v2.0: Updated Supplementary File SI7 to include calculations of percentages of trace element peaks cooccurring with peaks in Sr. v2.1: Add latest versions of manuscript figures v2.2: Minor changes to manuscript figures for production of paper

Supplementary Data and figures belongingto the manuscript titled "Tracing timing of growth in cultured mollusks using strontium spiking", in review.

Supplementary files belonging to the paper titled "Temperature dependence of clumped isotopes (∆47) in aragonite" submitted to Geophysical Research Letters. Key points Precise control on carbonate formation temperatures enables more accurate clumped isotope-temperature calibrations Isotopic ordering and acid fractionation in aragonite have a similar temperature dependence as in calcite, enabling combined calibrations The Δ47-relation in carbonates is non-linear, so linear calibrations require temperature-specific calibration data Abstract Clumped isotope thermometry can independently constrain the formation temperatures of carbonates, but a lack of precisely temperature-controlled calibration samples limits its application on aragonites. To address this issue, we present clumped isotope compositions of aragonitic bivalve shells grown under highly controlled temperatures (1‒18°C), which we combine with clumped isotope data from natural and synthetic aragonites precipitated in a wide range of temperatures (1‒850°C). We observe no discernible offset in clumped isotope values between aragonitic foraminifera, mollusks, and abiogenic aragonites or between aragonites and calcites, eliminating the need for a mineral-specific calibration or acid fractionation factor. However, due to non-linear behavior of the clumped isotope thermometer, including high-temperature (>100°C) datapoints in linear clumped isotope calibrations causes them to underestimate temperatures of cold (1‒18°C) carbonates by 2.7 ± 2.0°C (95% confidence level). Therefore, clumped isotope-based paleoclimate reconstructions should be calibrated using samples with well constrained formation temperatures close to those of the samples. &nbsp

Supplementary Information to the manuscript titled: "Optimizing sampling strategies in high-resolution paleoclimate records" in preparation.

Print version and supplementto PhD thesis of Niels J. de Winter, defended on February 22nd 2019 at the Vrije Universiteit Brussel, Brussels, Belgium.

"Shell chemistry of the Boreal Campanian bivalve Rastellum diluvianum (Linnaeus, 1767) reveals temperature seasonality, growth rates and life cycle of an extinct Cretaceous oyster" published in Biogeosciences