Chromium isotope cycling in the water column and sediments of the Peruvian continental margin

摘要

Chromium (Cr) isotope fractionation is sensitive to redox changes and the Cr isotopic composition (delta Cr-53) of sedimentary rocks has been used to reconstruct marine redox conditions and atmospheric oxygenation in the past. However, little is known about the behaviour of chromium isotopes across modern marine redox boundaries. We investigated Cr concentrations and delta Cr-53 variations in seawater and sediment across the Peruvian oxygen minimum zone (OMZ) to provide a better understanding of Cr cycling in the ocean. We found that seawater delta Cr-53 values ranged from 0.02 +/- 0.16 parts per thousand to 0.59 +/- 0.11 parts per thousand (2SD) and sediment values from 0.31 +/- 0.07 to 0.92 +/- 0.12 parts per thousand. Neither Cr concentrations nor delta Cr-53 values in the water column revealed significant shifts across the oxic-anoxic boundaries. Instead, processes that operate at a local scale, such as Cr scavenging by Fe-rich particles and Cr release from reducing sediments, are identified as the main controls on Cr concentrations and isotope compositions in the water column. The delta Cr-53 values of sediments deposited in permanently anoxic waters (0.77 +/- 0.19 parts per thousand, n = 5) are significantly different from the delta Cr-53 values of sediments deposited in oxic bottom waters (0.46 +/- 0.19 parts per thousand, n = 4). This suggests that sediment Cr concentrations and delta Cr-53 values are to some extent influenced by water column redox (e.g. reductive dissolution and transport of Fe oxides) and/or early diagenetic (e.g. redistribution of Cr during phosphogenesis) processes as well as biologic activity. Our data demonstrate that local scale water column redox gradients and sediment exchange can lead to a large range of delta Cr-53 values in sediments, comparable to the range found in the entire geologic record to date. Given the increasing prominence of Cr isotope measurements in constraining atmospheric oxygenation in deep time, we argue that th