Radium-228 as a tracer of dissolved trace element inputs from the Peruvian continental margin

V. Sanial (1) , L.E. Kipp (1) , P.B. Henderson (1) , P. van Beek (2) , J.-L. Reyss (3, 4) , D.E. Hammond , N.J. Hawco , M.A. Saito , J.A. Resing , P. Sedwick , W.S. Moore , M.A. Charette (1)

1 WHOI - Department of Marine Chemistry and Geochemistry
2 LEGOS - Laboratoire d'études en Géophysique et océanographie spatiales
3 LSCE - Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette]
4 OCEANIS - Océan et Interfaces

Continental margins play a central role in the composition of seawater by being an important source of trace element essentials to the functioning of the ocean ecosystems. Here, we measured long-lived radium isotopes (Ra-226, Ra-228) along a zonal transect at 12 degrees S (US GEOTRACES GP16) in the eastern tropical South Pacific Ocean. We used Ra-228 to quantify the trace element and isotope (TEI) fluxes (DMn, DFe, and DCo) delivered from the Peruvian continental i) shelf and ii) slope. First, elevated Ra-228 activities were measured in surface water over the entire transect (similar to 8500 km), evidence that the continental shelf is an important source of sediment-derived TEIs not only to coastal areas, but to central Pacific Ocean waters. Modeled Ra-228 shelf fluxes combined with water column dissolved TEI/Ra-228 ratios were used to quantify the shelf-ocean input rates (normalized to shelf-area) for DMn (3.3 x 10(3) mu mol m(-2) y(-1)), DFe (1.5 x 10(3) mu mol m(-2) y(-1)), and DCo (1.0 x 10(2) mu mol m(-2) y(-1)). Second, co-occurring plumes of Ra-228, DFe, and DMn extended over 1800 km from the margin at 1000-2500 m depth, indicative of a continental slope sediment TEI input to the intermediate water column. The Ra-228 gradient allowed us to derive an effective horizontal eddy diffusion coefficient (K-h) of 46 m(2) s(-1), which in turn permitted the calculation of slope sediment DMn (6.4 mu mol m(-2) y(-1)) and DFe (5.9 x 10(2) mu mol m(-2) y(-1)) fluxes based on their offshore concentration gradients. On the scale of the South Pacific continental margin between 0-20 degrees S, the DMn shelf flux is approximately 2-3 orders of magnitude higher than the slope flux, while the DFe shelf/slope flux is similar to 3:1. Both shelf and slope sediment derived DMn was transported over a significant distance towards the ocean interior, while DFe concentration gradients were steep, consistent with longer water column residence time for DMn as compared to DFe in marine systems. These findings highlight the importance of considering the continental slope-ocean boundary in the oceanic budgets of biologically-important trace elements.

Mots clés: Radium isotopes; Sediment inputs; Trace elements; GEOTRACES

Domaines: Milieux et Changements globaux; Biodiversité et Ecologie; Ingénierie de l'environnement; Environnement et Société; Géographie

V. Sanial, L.E. Kipp, P.B. Henderson, P. van Beek, J.-L. Reyss, et al.. Radium-228 as a tracer of dissolved trace element inputs from the Peruvian continental margin. Marine Chemistry, 2018, 201, pp. 20-34. ⟨10.1016/j.marchem.2017.05.008⟩. ⟨hal-02007361⟩