Quantification of dung carbon incorporation in a temperate grassland soil following spring application using bulk stable carbon isotope determinations.

Herbivore dung constitutes a substantial input of C to temperate grassland soils, and its fate must be determined in order to fully understand nutrient cycling in this ecosystem. This experiment used changes in bulk delta13C values of the 0-1 cm and 1-5 cm soil horizons of a dung-treated temperate grassland soil to approximate percentage applied dung C incorporation over 372 days. Natural abundance 13C-labelled C4 dung (delta13C - 12.6%) and C3 dung (delta13C - 31.3% were produced in a monitored diet switch from ryegrass silage (delta13C - 30.1%) to maize silage (delta13C - 11.6%). The dung was applied to a C3 grassland (delta13C 0-1 cm - 29.9%, 1-5 cm - 30.6%), and dung remains and soil cores from beneath the treatments were sampled at intervals. delta13C values were used to estimate a maximum of 12% applied dung C incorporation in the top 5 cm of the soil after 112 days, which declined to around 8% at the end of the experiment. A significant increase in percentage applied dung C was observed in the top 1 cm of soil, compared with the 1-5 cm horizon, after a substantial rain event after 30 days. However, results of forage fibre analyses of the two dung types revealed significant differences in composition which may affect subsequent calculations of percentage dung incorporation based on bulk delta13C values.