Quantifying trace element and isotope fluxes at the ocean-sediment boundary - a review

• Published in: Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences
• Main Authors: Homoky, W, Weber, T, Berelson, W, Conway, T, Henderson, G, van Hulten, M, Jeandel, C, Severmann, S, Tagliabue, A
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: Royal Society 2016
• Subjects: North Atlantic
• Online Access: https://doi.org/10.1098/rsta.2016.0246; https://ora.ox.ac.uk/objects/uuid:cf50c5de-6cf5-4cfb-99a2-060ebf947a6b

Quantifying fluxes of trace elements and their isotopes (TEIs) at the ocean’s sediment-water boundary is a preeminent challenge to understand their role in the present, past and future ocean. There are multiple processes that drive the uptake and release of TEIs and properties that determine their rates are unevenly distributed (e.g. sediment composition, redox conditions and (bio)physical dynamics). These factors complicate our efforts to find, measure, and extrapolate TEI fluxes across ocean basins. GEOTRACES observations are unveiling the oceanic distributions of many TEIs for the first time. These data evidence the influence of the sediment-water boundary on many TEI cycles, and underline the fact that our knowledge of the source-sink fluxes that sustain oceanic distributions is largely missing. Present flux measurements provide low spatial coverage and only part of the empirical basis needed to predict TEI flux variations. Many of the advances and present challenges facing TEI flux measurements are linked to process studies that collect sediment cores, pore waters, sinking material or seawater in close contact with sediments. However, such sampling has not routinely been viable on GEOTRACES expeditions. In this article 13 we recommend approaches to address these issues. Firstly, with an interrogation of emergent data using isotopic mass balance and inverse modelling techniques, and secondly, by innovating pursuits of direct of TEI flux measurements. We exemplify the value of GEOTRACES data with a new inverse model estimate of benthic Al flux in the North Atlantic Ocean. Further we review viable flux measurement techniques tailored to the sediment-water boundary. We propose such activities are aimed at regions that intersect the GEOTRACES Science Plan on the basis of seven criteria that may influence TEI fluxes: sediment provenance, composition, organic carbon supply, redox conditions, sedimentation rate, bathymetry, and the benthic nepheloid inventory.