the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Circum-Arctic Sediment PROvenance Database (CASPROD): A database of mineralogy and geochemistry for the Circum-Arctic surface sediments
Abstract. Arctic amplification is fundamentally reshaping the cryosphere, leading to accelerated sea-ice retreat, permafrost thaw, and intensified riverine discharge. These shifts collectively modify sediment source-to-sink dynamic processes in the Arctic Ocean. While surface sediments in this semi-enclosed basin integrate complex signals from diverse Eurasian and North American source regions, disentangling these provenance signatures requires a robust, multi-proxy framework that has historically been hampered by fragmented, heterogeneous datasets. Here, we present CASPROD (Circum-Arctic Sediment PROvenance Database), a standardized and high-resolution mineralogical and geochemical synthesis of Arctic surface sediments. The dataset integrates multi-proxy records from a broad spatial network, comprising 4308 sampling stations, including bulk sediment Sr-Nd isotopes (n=175 stations), detrital zircon U-Pb ages (n=4671 grains from 21 key stations), clay mineral assemblages (n=1647 stations), and detrital mineral proportions (n=2465 stations). These integrated proxies provide cross-validated sediment provenance constraints: Sr-Nd isotopes discriminate between ancient cratonic shields and juvenile orogenic belts; detrital zircon geochronology yields diagnostic age spectra distinguishing Eurasian versus North American crustal affinities; and clay and detrital mineralogy reflects different circum-Arctic sediment provenances, lithologies and transport processes. By synthesizing these diverse datasets, CASPROD delineates robust pan-Arctic spatial provenance domains and transport pathways. This database thus provides a critical benchmark for reconstructing palaeoceanographic, glacial, and sedimentary dynamics over geological timescales. CASPROD is freely available online (https://doi.org/10.6084/m9.figshare.31926927; Yao et al., 2026) in multiple machine-readable formats (e.g., tabular tables, GIS shapefiles, and GEOTIFF).
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Status: open (until 14 Jun 2026)
- CC1: 'Comment on essd-2026-253', Dennis Darby, 11 May 2026 reply
Data sets
Clay and detrital minerals, Sr-Nd isotopes, and zircon U-Pb ages in Arctic Ocean surface sediments – Circum-Arctic Sediment PROvenance Database (CASPROD): A database of mineralogy and geochemistry for the Circum-Arctic surface sediments Zhengquan Yao et al. https://doi.org/10.6084/m9.figshare.31926927
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 Comment on Yao et al. Provenance preprint.  This paper provides a useful listing of provenance techniques applicable to the Arctic Ocean.  It suffers for two major omissions: 1) The preprint ignores the Fe grain chemical fingerprinting method used in a dozen or more papers.  2) It avoids any scrutiny of the listed methods as to their accuracy.  While the precision of several listed methods might be high, when dealing with multiple sources of ice-rafted sediment in the Arctic Ocean, the accuracy can be quite low.  The Fe grain fingerprinting method has been shown to have an accuracy of less than 2% error of misidentifying the correct source or provenance.