Earthworms change the distribution and availability of phosphorous in organic substrates

R.C. Le Bayon^1,2 and F. Binet¹

Abstract
In laboratory controlled soil microcosms, the distribution and availability of phosphorous (P) were determined in the surface-casts and the burrows-linings of the anecic earthworm L. terrestris and were compared with non-ingested soil. To simulate more realistic earthworm community conditions, a combination of L. terrestris plus the endogeic A. caliginosa was tested.

For a 2-month period, the earthworms were given two organic food substrates: rye-grass littered onto the soil surface and sewage sludge mixed with soil. The following treatments were designed: (i) soil alone (S), (ii) soil and sewage sludge (SS), soil and rye-grass litter (SL), and (iv) soil, litter and sludge (SSL). Analyses were performed for P contents (total, available and organic), organic matter content (organic carbon, C_org and total nitrogen, N_tot) and the two acid and alkaline phosphatase activities (AcPA and AkPA).

Earthworms enhanced AcPA and were also responsible for additional AkPA in soil. The two AcPA and AkPA increased not only in surface-casts but also in burrows-linings that paralleled with the decrease of organic P in SL and SSL treatments. The stimulation of AcPA began quickly and declined rapidly in casts (from 19 to 8 µmol phenol g^-1 dry wt h^-1, respectively at week 2 and 8 in the SL treatment) but it was initiated later and maintained at a high level for longer in burrows (more than 10 µmol phenol g^-1 dry wt h^-1 at week 8 in the SL treatment). Significant positive correlations were found between the AkPA activities and Ntot contents (r=0.95, p=0.001) and to a lesser extend with Corg contents (r=0.76, p=0.05) in casts from the SL treatment, while AcPA significantly correlated with N_tot (r=0.91, p=0.004) but not with C_org (r=0.72, p=0.06).

P availability was always highest in casts. However, the available P contents decreased sharply over time in casts and were still low in burrow-linings, suggesting that a large part of inorganic P produced was rapidly immobilized for the microbial growth. Total P content was unchanged except in the SL treatment in which it increased in casts and burrows (ca. 725 µg g^-1, at week 4). Organic P was first the highest in casts and then decreased over time (from 168 at week 1 to 140 µg g^-1 at week 8 in the SL treatment).

This study illustrates that earthworms facilitate P transfer downward increasing a P patchy distribution in the soil, and significantly change the biogeochemical status of P (availability, organic phosphorous pool, AcPA activities) in certain hot spots such as casts and burrow-linings.


Source
Soil Biology & Biochemistry (2006) 38:235–246


Author Locations & Affiliations
(1) UMR 6553 ‘Ecobio’, CNRS/Rennes 1 University, Centre Armoricain de Recherche en ENvironnement (CAREN) F-35042 Rennes Cedex, France
(2) Neuchâtel University, Institute of Botany, Laboratory of Soil and Vegetation, Rue Emile Argand 11, CH-2007 Neuchâtel, Switzerland


Posted March 2010