Chromium Cycling in Redox-Stratified Basins Challenges δ 53 Cr Paleoredox Proxy Applications.

Chromium stable isotope composition (δ53 Cr) is a promising tracer for redox conditions throughout Earth's history; however, the geochemical controls of δ53 Cr have not been assessed in modern redox-stratified basins. We present new chromium (Cr) concentration and δ53 Cr data in dissolved, sinking particulate, and sediment samples from the redox-stratified Lake Cadagno (Switzerland), a modern Proterozoic ocean analog. These data demonstrate isotope fractionation during incomplete (non-quantitative) reduction and removal of Cr above the chemocline, driving isotopically light Cr accumulation in euxinic deep waters. Sediment authigenic Cr is isotopically distinct from overlying waters but comparable to average continental crust. New and published data from other redox-stratified basins show analogous patterns. This challenges assumptions from δ53 Cr paleoredox applications that quantitative Cr reduction and removal limits isotope fractionation. Instead, fractionation from non-quantitative Cr removal leads to sedimentary records offset from overlying waters and not reflecting high δ53 Cr from oxidative continental weathering.