4.7 Article

Distinct microbial and faunal communities and translocated carbon in Lumbricus terrestris drilospheres

期刊

SOIL BIOLOGY & BIOCHEMISTRY
卷 46, 期 -, 页码 155-162

出版社

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.soilbio.2011.11.024

关键词

Anecic earthworms; Burrow walls; Mesofauna; Microfauna; PLFA; Spatial heterogeneity; Stable isotope probing

资金

  1. Irish Fulbright Commission
  2. Council for International Exchange of Scholars
  3. Environmental ERDTI
  4. Irish Government [2005-S-LS-8]
  5. Natural Environment Research Council [CEH010021] Funding Source: researchfish

向作者/读者索取更多资源

Lumbricus terrestris is a deep-burrowing anecic earthworm that builds permanent, vertical burrows with linings (e.g., drilosphere) that are stable and long-lived microhabitats for bacteria, fungi, micro- and mesofauna. We conducted the first non-culture based field study to assess simultaneously the drilosphere (here sampled as 0-2 mm burrow lining) composition of microbial and micro/mesofaunal communities relative to bulk soil. Our study also included a treatment of surface-applied C-13- and N-15-labeled plant residue to trace the short-term (40 d) translocation of residue C and N into the drilosphere, and potentially the assimilation of residue C into drilosphere microbial phospholipid fatty acids (PLFAs). Total C concentration was 23%, microbial PLFA biomass was 58%, and PLFAs associated with protozoa, nematodes. Collembola and other fauna were 200-to-300% greater in the drilosphere than in nearby bulk soil. Principal components analysis of community PLFAs revealed that distributions of Gram-negative bacteria and actinomycetes and other Gram-positive bacteria were highly variable among drilosphere samples, and that drilosphere communities were distinct from bulk soil communities due to the atypical distribution of PLFA biomarkers for micro- and mesofauna. The degree of microbial PLFA C-13 enrichment in drilosphere soils receiving C-13-labeled residue was highly variable, and only one PLFA, 18:1 omega 9c, was significantly enriched. In contrast, 11 PLFAs from diverse microbial groups where enriched in response to residue amendment in bulk soil 0-5 cm deep. Among control soils, however, a significant delta C-13 shift between drilosphere and bulk soil at the same depth (5-15 cm) revealed the importance of L. terrestris for translocating perennial ryegrass-derived C into the soil at depth, where we estimated the contribution of the recent grass C (8 years) to be at least 26% of the drilosphere soil C. We conclude that L. terrestris facilitates the translocation of plant C into soil at depth and promotes the maintenance of distinct soil microbial and faunal communities that are unlike those found in the bulk soil. (C) 2011 Elsevier Ltd. All rights reserved.

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