Early diagenesis of trace metals (V, Mo, U) in sediments of the Peruvian upwelling area: response to oxygen dynamics in the water column

• Main Authors: Scholz, Florian, Hensen, Christian, Noffke, Anna, Rhode, Anne, Wallmann, Klaus
• Format: Conference Proceeding
• Language: English
• Published: Copernicus 2011
• Subjects: Geochemistry

The upwelling area in the eastern equatorial Pacific off Peru is one of the most pronounced oxygen minimum zones(OMZs) of the modern ocean. Modeling scenarios predict an expansion of the OMZs in the course of global changein the coming decades. As a consequence, the Peruvian continental margin represents a key locality for studies onbiogeochemical dynamics in the future ocean.We present pore water and sediment data for redox-sensitive metals (Fe, Mn, V, Mo, and U) that have been collectedalong a transect across the Peruvian margin at 11°S. The results are used to evaluate the behavior of trace metalsin a wide range of biogeochemical and hydrodynamic settings.In the core of the OMZ, where permanently anoxic conditions prevail, redox sensitive metals exhibit diageneticbehaviors largely consistent with previous studies. Vanadium and Mo are released from Fe oxihydroxides andsubsequently recycled through diffusion across the benthic boundary or trapped through formation of authigenicV phases and sequestration of Mo by authigenic pyrite. Some U is delivered through diffusion across the benthicboundary, reduction and precipitation of UO2 and incorporation into phosphorites. The utmost part of the buried U,however, is delivered in particulate form, most likely as bioauthigenic U which cannot be recycled in the suboxicwaters overlying the anoxic sediments. In contrast to sediments in the core of the OMZ, sediments on the shelfexperience frequent oxygenation episodes related to the passage of internal waves and the regular recurrence ofEl Niño events. These oxygenation episodes lead to the re-oxidation and remobilization of authigenic U and V. Incontrast to that, the authigenic accumulation of Mo is favored by the occasional occurrence of slightly oxidizingconditions. This is most likely due to enhanced formation of sulfur intermediates necessary for pyrite formationand the increased stability of pyrite, the major Mo sink, under oxidizing conditions, compared to authigenic V andU phases. Redox oscillations in the Peruvian OMZ thus lead to a discrimination of U against Mo, a mechanism thatshould be considered in the interpretation of U/Mo systematics in paleo redox studies. Overall our results providevaluable constraints on how trace metal inventories of marginal sediments may respond to expanding shelf anoxiaand to short term perturbations of sediment redox conditions.