Differential acquisition of amino acid and peptide enantiomers within the soil microbial community and its implications for carbon and nitrogen cycling in soil
Differential acquisition of amino acid and peptide enantiomers within the soil microbial community and its implications for carbon and nitrogen cycling in soil
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DOI:
10.1016/j.soilbio.2015.05.003
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发表时间:
2015-09-01
影响因子:
9.7
通讯作者:
Jones, D. L.
中科院分区:
文献类型:
--
作者:
Broughton, R. C. I.;Newsham, K. K.;Jones, D. L.
L-isomeric amino acids and oligopeptides are thought to represent a key nitrogen (N) source for plants and soil microorganisms, bypassing the need to take up inorganic N, whilst self-cycling of D-enantiomers within peptidoglycan-containing bacteria may provide a further short circuit within the N cycle. Here we use stable isotope profiling (SIP) to identify the fate of organic N within soil microbial communities. We followed the incorporation of C-13-labelled D- or L-labelled amino acids/peptides into phospholipid fatty acids (PLFAs). L-alanine and its peptides were taken up more rapidly than D-enantiomers by Gram-positive bacteria with C-13 incorporation being predominantly into anteiso- and iso-fatty acids typically associated with. Gram-positive bacteria. D-enantiomer uptake was found not to differ significantly between the microbial groups, providing little support for the view that soil bacteria may self-cycle D-forms of amino acids and peptides. There was no consistent association between peptide chain length and incorporation. The concentrations of L- and D-isomeric amino acids in soil solution were 866 nM and 72 nM, respectively. We conclude that Gram-positive bacteria appear to be the primary competitors for L-enantiomeric forms of amino acids and their peptides, but that both D- and L-enantiomers are available N and C sources for bacteria and fungi. (C) 2015 The Authors. Published by Elsevier Ltd.