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Short-term carbon input increases microbial nitrogen demand, but not microbial nitrogen mining, in a set of boreal forest soils

Författare:
  • Birgit Wild
  • Saeed Alaei
  • Per Bengtson
  • Samuel Bodé
  • Pascal Boeckx
  • Jörg Schnecker
  • Werner Mayerhofer
  • Tobias Rütting
Publiceringsår: 2017-12
Språk: Engelska
Sidor: 261-278
Publikation/Tidskrift/Serie: Biogeochemistry
Volym: 136
Nummer: 3
Dokumenttyp: Artikel i tidskrift
Förlag: Springer

Abstract english

Rising carbon dioxide (CO2) concentrations and temperatures are expected to stimulate plant productivity and ecosystem C sequestration, but these effects require a concurrent increase in N availability for plants. Plants might indirectly promote N availability as they release organic C into the soil (e.g., by root exudation) that can increase microbial soil organic matter (SOM) decomposition (“priming effect”), and possibly the enzymatic breakdown of N-rich polymers, such as proteins, into bio-available units (“N mining”). We tested the adjustment of protein depolymerization to changing soil C and N availability in a laboratory experiment. We added easily available C or N sources to six boreal forest soils, and determined soil organic C mineralization, gross protein depolymerization and gross ammonification rates (using 15N pool dilution assays), and potential extracellular enzyme activities after 1 week of incubation. Added C sources were 13C-labelled to distinguish substrate from soil derived C mineralization. Observed effects reflect short-term adaptations of non-symbiotic soil microorganisms to increased C or N availability. Although C input promoted microbial growth and N demand, we did not find indicators of increased N mobilization from SOM polymers, given that none of the soils showed a significant increase in protein depolymerization, and only one soil showed a significant increase in N-targeting enzymes. Instead, our findings suggest that microorganisms immobilized the already available N more efficiently, as indicated by decreased ammonification and inorganic N concentrations. Likewise, although N input stimulated ammonification, we found no significant effect on protein depolymerization. Although our findings do not rule out in general that higher plant-soil C allocation can promote microbial N mining, they suggest that such an effect can be counteracted, at least in the short term, by increased microbial N immobilization, further aggravating plant N limitation.

Keywords

  • Geochemistry
  • Ammonification
  • Boreal forest
  • Microbial N mining
  • N mineralization
  • Organic N
  • Priming
  • Protein depolymerization

Other

Published
  • ISSN: 0168-2563
Per Bengtson
E-post: per [dot] bengtson [at] biol [dot] lu [dot] se

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Mikrobiologisk ekologi

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