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RESEARCH PRODUCT
Depth matters : Effects of precipitation regime on soil microbial activity upon rewetting of a plant-soil system
Romain L. BarnardIlonka C. EngelhardtAmy T. WeltyAmy T. WeltyNadine RouardMarie Christine BreuilSteven J. BlazewiczLucía GalianoAymé SporDavid BruJosé Carlos MirandaArthur Gesslersubject
[SDE] Environmental Sciences0301 basic medicineBiogeochemical cycleRain[SDV]Life Sciences [q-bio]Stable-isotope probingPlant DevelopmentBiologyMicrobiologyArticleprecipitation legacyMesocosmSoil03 medical and health sciencesdry-wetMicrobial ecologyAbundance (ecology)[SDV.BV]Life Sciences [q-bio]/Vegetal Biology[SDV.BV] Life Sciences [q-bio]/Vegetal BiologyPrecipitationPhylogenySoil MicrobiologyEcology Evolution Behavior and Systematicsplant-soil interactionsTopsoilBacteriaFungi04 agricultural and veterinary sciences15. Life on land[SDV] Life Sciences [q-bio]030104 developmental biologyAgronomy13. Climate action[SDE]Environmental Sciences040103 agronomy & agriculture0401 agriculture forestry and fisheriesSoil horizonmicrobial communitydescription
International audience; Climate change is predicted to affect not only the amount but also the temporal distribution of rain. Changes in frequency and amplitude of rain events, i.e. precipitation patterns, result in different water conditions with soil depth, and likely affect plant growth and shape plant and soil microbial activity. Here, we used 18O stable isotope probing (SIP) to investigate bacterial and fungal communities that actively grew or not upon rewetting, at three different depths in plant-soil mesocosms previously subjected to frequent or infrequent watering for 12 weeks (equal total water input). Phylogenetic marker genes for bacteria and fungi were sequenced after rewetting, and plant-soil microbial coupling documented by plant 13C-CO2 labeling. Soil depth, rather than precipitation pattern, was most influential in shaping microbial response to rewetting, and had differential effects on active and inactive bacterial and fungal communities. After rewetting, active bacterial communities were less rich, more even and phylogenetically related than the inactive, and reactivated throughout the soil profile. Active fungal communities after rewetting were less abundant and rich than the inactive. The coupling between plants and soil microbes decreased under infrequent watering in the top soil layer. We suggest that differences in fungal and bacterial abundance and relative activity could result in large effects on subsequent soil biogeochemical cycling.
year | journal | country | edition | language |
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2018-08-12 |