Details zur Publikation

Kategorie Textpublikation
Referenztyp Zeitschriften
DOI 10.1007/s11104-025-07758-z
Lizenz creative commons licence
Titel (primär) Soil water limitation intensity alters nitrogen cycling at the plant-soil interface in Scots pine mesocosms
Autor Solly, E.F.; Jaeger, A.C.H.; Barthel, M.; Six, J.; Mueller, R.C.; Hartmann, M.
Quelle Plant and Soil
Erscheinungsjahr 2025
Department CHS
Sprache englisch
Topic T5 Future Landscapes
Supplements https://static-content.springer.com/esm/art%3A10.1007%2Fs11104-025-07758-z/MediaObjects/11104_2025_7758_MOESM1_ESM.xlsx
https://static-content.springer.com/esm/art%3A10.1007%2Fs11104-025-07758-z/MediaObjects/11104_2025_7758_MOESM2_ESM.xlsx
https://static-content.springer.com/esm/art%3A10.1007%2Fs11104-025-07758-z/MediaObjects/11104_2025_7758_MOESM3_ESM.docx
Keywords Water limitation; Nitrogen cycling; Litter decomposition; 15N labeling; Metagenomics; Soil microbiome; Pinus sylvestris; Nitrogen allocation
Abstract Background and aim
More intense episodes of drought are expected to affect terrestrial nitrogen (N) cycling by altering N transformation rates, the functioning of soil microorganisms, and plant N uptake. However, there is limited empirical evidence of how progressive water loss affects N cycling at the plant-soil interface.
Methods
We adopted 15N tracing techniques and metagenomic analyzes of microbial genes involved in N cycling to assess how different levels of soil water availability influenced the fate of N derived from decomposing litter in mesocosms with Scots pine saplings.
Results
With increasing water limitation, the release of N from decomposing litter into the soil declined rapidly. However, moderate levels of water limitation barely affected the microbial metagenome associated with N cycling and the uptake of N by the saplings. Comparatively, severe levels of water limitation impaired plant N uptake, and increased the prevalence of microbial N-cycling genes potentially involved in mechanisms that protect against water stress. Genes associated with the uptake and release of N during mineralization and nitrification declined under low soil water contents.
Conclusions
When soil water becomes largely unavailable, the cycling of N at the plant-soil interface is slowed down, and microbial and plant tolerance mechanisms may prevail over N uptake and microbial decomposition.
dauerhafte UFZ-Verlinkung https://www.ufz.de/index.php?en=20939&ufzPublicationIdentifier=31155
Solly, E.F., Jaeger, A.C.H., Barthel, M., Six, J., Mueller, R.C., Hartmann, M. (2025):
Soil water limitation intensity alters nitrogen cycling at the plant-soil interface in Scots pine mesocosms
Plant Soil 10.1007/s11104-025-07758-z