Soil faunal and structural responses to the settlement of a semi-sedentary earthworm Lumbricus terrestris in an arable clay field
Soil faunal and structural responses to the settlement of a semi-sedentary earthworm Lumbricus terrestris in an arable clay field
复制标题
耕地粘土田中半定居蚯蚓 Lumbricus terrestris 沉降的土壤动物和结构响应
DOI:
10.1016/j.soilbio.2017.09.001
复制
发表时间:
2017
影响因子:
9.7
通讯作者:
J. Mikola
中科院分区:
文献类型:
--
作者:
V. Nuutinen;K. Butt;J. Hyväluoma;E. Ketoja;J. Mikola
We studied the soil community and habitat consequences of introducing a deep-burrowing, sedentary life-style earthworm,Lumbricus terrestris(dew-worm) into arable zero-till clay. Seventeen years after introduction, which was originally aimed at improving the macroporosity and permeability of the heavy clay soil, we returned to the gradient ofL. terrestrisdispersal (well established, more recent and no settlement) and investigated the temporal development of the ecosystem engineering impacts on different faunal groups (earthworms, enchytraeids and nematodes) and soil porosity. The faunal responses were examined both atL. terrestrismidden scale (individual living site) and field scale. We found thatL. terrestrismiddens sustained elevated densities of all three faunal groups. In the case of earthworms, there was evidence for temporal development of the engineering impact as the difference between the midden and non-midden areas was more pronounced in the well-established areas than close to the leading edge of dispersal. The earthworm community composition was not altered atL. terrestrismidden sites. The settlement ofL. terrestrishad no discernible effects on field-scale earthworm and nematode abundances, but enchytraeids were practically absent beyond the leading edge of the dispersal. This effect might, however, be partly explained by a gradient of increasing clay content. Soil macroporosity atL. terrestrismidden sites did not increase with the age ofL. terrestrissettlement. Our results suggest thatL. terrestrissettlement in a clay soil can significantly increase the spatial patchiness of soil fauna, but may not, except in the case of enchytraeids, affect their field-scale abundances or the macroporosity of the soil in the vicinity ofL. terrestrisliving sites.