Soil microbial organic nitrogen uptake is regulated by carbon availability
Soil microbial organic nitrogen uptake is regulated by carbon availability
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DOI:
10.1016/j.soilbio.2014.07.003
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发表时间:
2014-10-01
影响因子:
9.7
通讯作者:
Condron, Leo M.
中科院分区:
文献类型:
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作者:
Farrell, Mark;Prendergast-Miller, Miranda;Condron, Leo M.
Plants and microorganisms intensely compete for nitrogen (N) at many stages of the terrestrial N cycle. In particular, the dissolved organic N (DON) pool, and competition for low molecular weight dissolved organic N (LMWDON) compounds such as amino acids and peptides (and LMW dissolved organic matter; LMWDOM as a whole) has received significant recent research interest. However, as LMWDON compounds contain both N and carbon (C), a question that remains is whether soil microorganisms are primarily taking up LMWDON mainly for the C or the N contained therein. We investigated microbial uptake rates of the model peptide L-trialanine as a rapidly cycling LMWDON compound in temperate grassland soils of differing fertility using C-14 labelling to assess how soil fertility status influenced microbial uptake of LMWDON. We then imposed an excess of C as glucose and/or N as NH4Cl to ask whether the uptake of the peptide was affected by C or N excess. Our results demonstrate that L-trialanine is taken up rapidly from the soil solution (t(1/2), < 1.5 min), and that an excess of C, rather than N, resulted in a reduced uptake of the peptide. From this, we conclude that LMWDON is taken up primarily to fulfil the C requirement of soil microorganisms, indicating that they exist in a C-limited state, and are able to respond quickly to a transient influx of an easily metabolisable resource. (C) 2014 The Authors. Published by Elsevier Ltd.