Soil and Ecosystem Ecology, Lancaster Environment Centre, Lancaster University, Lancaster LA1 4YQ, United Kingdom.
Proc Natl Acad Sci U S A. 2013 Aug 27;110(35):14296-301. doi: 10.1073/pnas.1305198110. Epub 2013 Aug 12.
Intensive land use reduces the diversity and abundance of many soil biota, with consequences for the processes that they govern and the ecosystem services that these processes underpin. Relationships between soil biota and ecosystem processes have mostly been found in laboratory experiments and rarely are found in the field. Here, we quantified, across four countries of contrasting climatic and soil conditions in Europe, how differences in soil food web composition resulting from land use systems (intensive wheat rotation, extensive rotation, and permanent grassland) influence the functioning of soils and the ecosystem services that they deliver. Intensive wheat rotation consistently reduced the biomass of all components of the soil food web across all countries. Soil food web properties strongly and consistently predicted processes of C and N cycling across land use systems and geographic locations, and they were a better predictor of these processes than land use. Processes of carbon loss increased with soil food web properties that correlated with soil C content, such as earthworm biomass and fungal/bacterial energy channel ratio, and were greatest in permanent grassland. In contrast, processes of N cycling were explained by soil food web properties independent of land use, such as arbuscular mycorrhizal fungi and bacterial channel biomass. Our quantification of the contribution of soil organisms to processes of C and N cycling across land use systems and geographic locations shows that soil biota need to be included in C and N cycling models and highlights the need to map and conserve soil biodiversity across the world.
集约化土地利用减少了许多土壤生物区系的多样性和丰度,从而影响了它们所控制的过程和这些过程所支撑的生态系统服务。土壤生物区系与生态系统过程之间的关系主要在实验室实验中发现,而在野外很少发现。在这里,我们在欧洲四个具有不同气候和土壤条件的国家进行了量化研究,研究了由于土地利用系统(集约小麦轮作、粗放轮作和永久草地)导致的土壤食物网组成差异如何影响土壤功能及其提供的生态系统服务。集约小麦轮作在所有国家都一致降低了土壤食物网所有组成部分的生物量。土壤食物网特性在土地利用系统和地理位置之间强烈且一致地预测了碳和氮循环过程,并且它们比土地利用更能预测这些过程。随着与土壤碳含量相关的土壤食物网特性(如蚯蚓生物量和真菌/细菌能量通道比)的增加,土壤碳损失过程增加,并且在永久草地中最大。相比之下,氮循环过程是由独立于土地利用的土壤食物网特性来解释的,例如丛枝菌根真菌和细菌通道生物量。我们对土壤生物在土地利用系统和地理位置之间对碳和氮循环过程的贡献进行了量化,表明需要将土壤生物纳入碳和氮循环模型,并强调需要在全球范围内对土壤生物多样性进行测绘和保护。