Phosphate as a limiting resource: introduction

Abstract

Phosphorus (P) is commonly a limiting nutrient for both terrestrial and aquatic productivity, with the consequence that it is considered important in determining the biodiversity and biomass of natural ecosystems. P-limitation of terrestrial plants is not a recent development. Karandashov and Bucher (2005) argued that the evolutionary transition of plants from the aquatic to terrestrial habitats was contingent on the presence of arbuscular mycorrhiza, which facilitated P acquisition. As a consequence of persistent P-limitations, terrestrial plants have evolved a wide range of P acquisition strategies, including mechanisms that increase the range of chemical forms that can be accessed, the range of concentrations that can be taken up and the effective absorbing area of the roots (Lambers et al. 2008). Likewise, plants have a range of strategies for conserving P that enable them to persist in P-deficient habitats, including sclerophyllous leaves and serotinous cones. In order to ensure successful recruitment in P-limited environments they also produce P-rich seeds (e.g. Groom and Lamont 2010, this volume). P is also often a limiting nutrient in agriculture (e.g. Sanchez 2010), deficiency being redressed through applications of P-fertilisers (globally ca. 20×10 kg P annum; Smit et al. 2009). Alarmingly, the finite global stocks of P (2,400×10 kg P) are likely to be depleted within 125 years (Smit et al. 2009; Vaccari 2009). Anthropogenic modification of the global P cycle by fertiliser use as well as waste streams and detergent use have effectively doubled global P cycling since the mid-19th century (Filippelli 2002). A consequence is that many natural ecosystems are threatened by super-abundance of a formerly limiting resource, with resulting biodiversity losses (e.g. Tilman et al. 2001). This is likely to be especially true in systems where P was formerly most-limiting, such as in Mediterranean terrestrial ecosystems (Sala et al. 2000), oligotrophic lakes (Schindler et al. 2008) and nutrient-impoverished oceans (Rabalais et al. 2008). Apart from the direct biodiversity consequences of P-eutrophication, release from P-limitation combined with increased atmospheric CO2 concentration and N deposition may exacerbate the loss of biodiversity.