4.7 Article

Incorporation of plant carbon and microbial nitrogen into the rhizosphere food web of beech and ash

期刊

SOIL BIOLOGY & BIOCHEMISTRY
卷 62, 期 -, 页码 76-81

出版社

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.soilbio.2013.03.002

关键词

Soil food web; Labeling experiment; Fine roots; Mycorrhizal fungi; Fungal energy channel; Bacterial energy channel

资金

  1. German Research Foundation (DFG)
  2. Ministry of Science and Culture of Lower Saxony
  3. Niedersachsisches Vorab, Cluster of Excellence 'Functional Biodiversity Research'

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We labeled tree saplings of beech and ash with N-15 and C-13 in a greenhouse. Carbon (C) was applied as (CO2)-C-13 to plants and nitrogen (N) was added as (NH4NO3)-N-15-N-15 to the soil. We hypothesized that C will be transferred from plants to the rhizosphere, subsequently in beech to ectomycorrhiza (EM), in ash to arbuscular mycorrhiza (AM) and finally to soil animals. We expected the C signal to be more effectively transferred to soil animals in EM as compared to AM systems since EM forms more extensive extramatrical mycelia as compared to AM. For N-15 we hypothesized that it will be taken up by both saprotrophic microorganisms and mycorrhizal fungi and then channeled to-soil animals. After five month, delta C-13 and delta N-15 signatures of soil animals, EM and fine roots of beech and ash were measured. Litter and soil were hardly enriched in N-15 whereas fine roots of beech and ash were highly enriched suggesting that nitrogen in (NH4NO3)-N-15-N-15 was predominantly taken up by plants and mycorrhizal fungi but little by saprotrophic microorganisms. Roots of beech and ash were highly enriched in C-13 with maximum values in EM proving that C-13 was translocated into roots and mycorrhizal fungi. Soil animals were a priori assigned to primary decomposers, secondary decomposers and predators. Generally, signatures of soil animals did not significantly vary between beech and ash and therefore were pooled. Primary decomposers had low delta C-13 and delta N-15 signatures similar to litter and soil confirming that rhizosphere C and microbial N are of limited importance for primary decomposer taxa. delta C-13 and delta N-15 signatures of secondary decomposers were higher than those of primary decomposers and spanned a large gradient indicating that certain secondary decomposers rely on root derived C and microbial N, however, none of the secondary decomposers had signatures pointing to exclusive feeding on EM. Unexpectedly, delta C-13 and delta N-15 signatures were highest in predators suggesting that they heavily preyed on secondary decomposer species such as the litter dwelling Collembola species Lepidocyrtus cyaneus and species not captured by the heat extraction procedure used for capturing prey taxa, presumably predominantly root associated nematodes. Overall, the results highlight that in particular higher trophic levels rely on carbon originating from other resources than litter with these resources channeled to dominant predators via litter dwelling Collembola species. (C) 2013 Elsevier Ltd. All rights reserved.

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