How fertile are earthworm casts? A meta-analysis

• Published in: Geoderma
• Main Authors: van Groenigen, J.W., van Groenigen, Kees Jan, Koopmans, G.F., Stokkermans, Lotte, Vos, M.J., Lubbers, I.M.
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2019
• Subjects: Concentration processes; Earthworms; Nitrogen; Phosphorus; Relative cast fertility; Transformation processes; Antarc*; Antarctica
• Online Access: https://research.wur.nl/en/publications/how-fertile-are-earthworm-casts-a-meta-analysis; https://doi.org/10.1016/j.geoderma.2018.11.001

It has long been established that earthworms beneficially affect plant growth. This is to a large extent due to the high fertility of their casts. However, it is not clear how fertile casts are compared to bulk soil, and how their fertility varies between earthworm feeding guilds and with physico-chemical soil properties. Using meta-analysis, we quantified the fertility of earthworm casts and identified its controlling factors. Our analysis included 405 observations from 81 articles, originating from all continents except Antarctica. We quantified cast fertility by determining the enrichment of earthworm casts relative to the bulk soil (“relative cast fertility”; RCF) for total organic carbon (TOC), total phosphorus (P) and total nitrogen (N) concentrations, as well as for plant available pools of N (total mineral N) and P (available P: P-Olsen, P-Bray or comparable metrics), C-to-N ratio and microbial biomass C. In addition to these response variables, we studied four additional ones closely related to soil fertility: pH-H2O, clay content, cation exchange capacity (CEC), and base saturation. With the exception of C-to-N ratio, microbial C and clay content, all studied response variables were significantly increased in casts compared to the bulk soil. Increases in total elemental concentrations (TOC, total P and total N), which are the result of preferential feeding or concentration processes, were comparable and ranged between 40 and 48%. Nutrient availability, which is to a large extent the result of (bio)chemical transformation processes in the earthworm gut, was increased more strongly than total elemental concentrations (241% and 84% for mineral N and available P, respectively). Increases in pH (0.5 pH units), cation exchange capacity (40%), and base saturation (27%) were also large and significant. None of the soil-related possible controlling factors could satisfactorily explain thevariation in RCF; plant presence (or other sources of organic C input such as residue application) was the only controlling ...