Articles | Volume 7, issue 2
Biogeosciences, 7, 469–480, 2010
Biogeosciences, 7, 469–480, 2010

  03 Feb 2010

03 Feb 2010

Benthic phosphorus and iron budgets for three NW African slope sediments: a balance approach

K. Küster-Heins1, G. J. de Lange2, and M. Zabel3 K. Küster-Heins et al.
  • 1Department of Geosciences, University of Bremen, Klagenfurter Strasse, 28359 Bremen, Germany
  • 2Department of Earth Sciences – Geochemistry, Faculty of Geosciences, Utrecht University, 3508 TA Utrecht, The Netherlands
  • 3Marum – Center for Marine Environmental Sciences, University of Bremen, Leobener Strasse, 28359 Bremen, Germany

Abstract. Despite intensive research on the different domains of the marine phosphorus (P) cycle during the last decades, frequently discussed open questions still exist especially on controlling factors for the benthic behaviour of P and its general distribution in sediment-pore water systems. Steady state or the internal balance of all relevant physical and (bio)geochemical processes are amongst the key issues. In this study we present and discuss an extended data set from surface sediments recovered from three locations on the NW African continental slope. Pore water data and results from sequential sediment extractions give clear evidence to the well-known close relationship between the benthic cycles of P and iron. Accordingly, most of the dissolved phosphate must have been released by microbially catalyzed reductive dissolution of iron (oxhydr)oxides. However, rates of release and association of P and iron, respectively, are not directly represented in profiles of element specific sediment compositions. Results from steady-state based transport-reaction modelling suggest that particle mixing due to active bioturbation, or rather a physical net downward transport of P associated to iron (oxyhydr)oxides, is an essential process for the balance of the inspected benthic cycles. This study emphasizes the importance of balancing analytical data for a comprehensive understanding of all processes involved in biogeochemical cycles.

Final-revised paper