Contrasting drivers of belowground nitrogen cycling in a montane grassland exposed to a multifactorial global change experiment with elevated CO2, warming, and drought

Tania L. Maxwell, Alberto Canarini, Ivana Bogdanovic, Theresa Bockle, Victoria Martin, Lisa Noll, Judith Prommer, Joana Seneca, Eva Simon, Hans-Peter Piepho, Markus Herndl, Erich M. Potsch, Christina Kaiser, Andreas Richter, Michael Bahn, Wolfgang Wanek (Corresponding author)

Publications: Contribution to journalArticlePeer Reviewed

Abstract

Depolymerization of high-molecular weight organic nitrogen (N) represents the major bottleneck of soil N cycling and yet is poorly understood compared to the subsequent inorganic N processes. Given the importance of organic N cycling and the rise of global change, we investigated the responses of soil protein depolymerization and microbial amino acid consumption to increased temperature, elevated atmospheric CO2, and drought. The study was conducted in a global change facility in a managed montane grassland in Austria, where elevated CO2 (eCO(2)) and elevated temperature (eT) were stimulated for 4 years, and were combined with a drought event. Gross protein depolymerization and microbial amino acid consumption rates (alongside with gross organic N mineralization and nitrification) were measured using N-15 isotope pool dilution techniques. Whereas eCO(2) showed no individual effect, eT had distinct effects which were modulated by season, with a negative effect of eT on soil organic N process rates in spring, neutral effects in summer, and positive effects in fall. We attribute this to a combination of changes in substrate availability and seasonal temperature changes. Drought led to a doubling of organic N process rates, which returned to rates found under ambient conditions within 3 months after rewetting. Notably, we observed a shift in the control of soil protein depolymerization, from plant substrate controls under continuous environmental change drivers (eT and eCO(2)) to controls via microbial turnover and soil organic N availability under the pulse disturbance (drought). To the best of our knowledge, this is the first study which analyzed the individual versus combined effects of multiple global change factors and of seasonality on soil organic N processes and thereby strongly contributes to our understanding of terrestrial N cycling in a future world.
Original languageEnglish
Pages (from-to)2425-2441
Number of pages17
JournalGlobal Change Biology
Volume28
Issue number7
DOIs
Publication statusPublished - 1 Apr 2022

Austrian Fields of Science 2012

  • 106026 Ecosystem research

Keywords

  • amino acid consumption
  • climate warming
  • drought
  • elevated CO2
  • protein depolymerization
  • soil nitrogen cycling
  • T-FACE
  • SOIL ORGANIC NITROGEN
  • EXTRACELLULAR ENZYME-ACTIVITIES
  • PROTEIN DEPOLYMERIZATION
  • N MINERALIZATION
  • MICROBIAL CARBON
  • USE EFFICIENCY
  • AMINO-ACIDS
  • LIMITATION
  • METAANALYSIS
  • RESPONSES
  • elevated CO

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