Earthworm impact on the global warming potential of a no-tillage arable soil

Abstract

We studied the effect of the deep-burrowing earthworm Lumbricus terrestris on the greenhouse gas (GHG) fluxes and global warming potential (GWP) of arable no-till soil using both field measurements and a controlled 15 week laboratory experiment. In the field, the emissions of nitrous oxide (N 2 O) and carbon dioxide (CO 2) were on average 43 and 32% higher in areas occupied by L. terrestris (the presence judged by the surface midden) than in adjacent, unoccupied areas (with no midden). The fluxes of methane (CH 4) were variable and had no consistent difference between the midden and non-midden areas. Removing the midden did not affect soil N 2 O and CO 2 emissions. The laboratory results were consistent with the field observations in that the emissions of N 2 O and CO 2 were on average 27 and 13% higher in mesocosms with than without L. terrestris. Higher emissions of N 2 O were most likely due to the higher content of mineral nitrogen and soil moisture under the middens, whereas L. terrestris respiration fully explained the observed increase in CO 2 emissions. The activity of L. terrestris increased the GWP of field and laboratory soil by 50 and 18%, but only 6 and 2% of this increase was due to the enhanced N 2 O emission. Our results suggest that high N 2 O emissions commonly observed in no-tillage soils can partly be explained by the abundance of L. terrestris under no-till management and that L. terrestris can markedly regulate the climatic effects of different cultivation practises.