Encyclopedia of Geochemistry

Living Edition
| Editors: William M. White

Ocean Biochemical Cycling and Trace Elements

  • Hein J. W. de Baar
  • Steven M. A. C. van Heuven
  • Rob MiddagEmail author
Living reference work entry
DOI: https://doi.org/10.1007/978-3-319-39193-9_356-1

Definition

Ocean biochemical cycling refers to the distribution of nutrients and bio-essential elements at low concentration that is controlled by their uptake by phytoplankton in surface waters, sinking and remineralization of organic remains in deeper waters, and subsequent redistribution by thermohaline circulation.

Introduction

Dissolved inorganic carbon (C as DIC) varies around ~2 millimoles [mM = 10−3 M] in seawater and is pivotal for life in the sea. Much less abundant are the nutrients nitrate and phosphate that occur in the micromole [μM = 10−6 M] range and are essential for each living organism. Also essential for life are several trace nutrient elements , notably Fe and Zn, that occur in the nanomolar [nM = 10−9 M] range or even lower such as Co in the picomolar [pM = 10−12 M] range. Several other trace elements also occur in the nanomolar [nM] to picomolar [pM] range. Finally a few ultratrace elements occur in the femtomolar [fM = 10−15 M] range in seawater.

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Copyright information

© Springer International Publishing AG 2017

Authors and Affiliations

  • Hein J. W. de Baar
    • 1
  • Steven M. A. C. van Heuven
    • 1
  • Rob Middag
    • 1
    Email author
  1. 1.NIOZ Royal Netherlands Institute for Sea ResearchDepartment of Ocean Systems (OCS), and Utrecht UniversityDen Burg, TexelNetherlands