Water availability is a stronger driver of soil microbial processing of organic nitrogen than tree species composition

Soil organic nitrogen (N) cycling processes constitute a bottleneck of soil N cycling, yet little is known about how tree species composition may influence these rates, and even less under changes in soil water availability such as those that are being induced by climate change. In this study, we us...

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Published inEuropean journal of soil science Vol. 74; no. 1
Main Authors Maxwell, Tania L., Augusto, Laurent, Tian, Ye, Wanek, Wolfgang, Fanin, Nicolas
Format Journal Article
LanguageEnglish
Published Oxford, UK Blackwell Publishing Ltd 01.01.2023
Wiley Subscription Services, Inc
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Subjects
amino acid uptake
Availability
Betula pendula
Biodiversity
Biomass
Climate change
Community composition
Composition
Cycles
Depolymerization
Dilution
Environmental Sciences
France
irrigation
Irrigation water
Isotopes
microbial biomass
microbial carbon
Microorganisms
Moisture content
Nitrogen
Organic nitrogen
Pine trees
Pinus pinaster
plant available water
Plant species
precipitation
protein depolymerisation
Proteins
Soil
soil organic nitrogen
Soil water
Species composition
species diversity
TreeDivNet
trees
Trends
Water
Water availability
France
microbial biomass
precipitation
protein depolymerisation
biodiversity
TreeDivNet
amino acid uptake
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Abstract Soil organic nitrogen (N) cycling processes constitute a bottleneck of soil N cycling, yet little is known about how tree species composition may influence these rates, and even less under changes in soil water availability such as those that are being induced by climate change. In this study, we used a 12‐year‐old tree biodiversity experiment in southwestern France to assess the interactive effects of soil water availability (half of the blocks seasonally irrigated to double precipitation) and tree species composition (monocultural vs. mixed plots of coniferous Pinus pinaster, and of broadleaf Betula pendula). We measured gross protein depolymerisation rates using a novel high‐throughput isotope pool dilution method, along with soil microbial biomass carbon and N to calculate microbial biomass‐specific activities of soil organic N processes. Overall, high soil water availability led to a 42% increase in soil protein depolymerisation rates compared to the unirrigated plots, but we found no effect of species composition on these soil organic N cycling processes. When investigating the interactive effect of tree species mixing and soil water availability, the results suggest that mixing tree species had a negative effect on soil organic N cycling processes in the non‐irrigated blocks subject to dry summers, but that this effect tended to become positive at higher soil water availability in irrigated plots. These results put forth that soil water availability could influence potential tree species mixing effects on soil organic N cycling processes in dry conditions. Highlights Tree species (with different litter C:N ratios) had little effect on protein depolymerisation Increasing water availability via irrigation accelerated depolymerisation rates No interactive effect between tree species mixing and water availability, although trends emerged Positive trend of mixing under high water availability and negative trend under low water
AbstractList Soil organic nitrogen (N) cycling processes constitute a bottleneck of soil N cycling, yet little is known about how tree species composition may influence these rates, and even less under changes in soil water availability such as those that are being induced by climate change. In this study, we used a 12‐year‐old tree biodiversity experiment in southwestern France to assess the interactive effects of soil water availability (half of the blocks seasonally irrigated to double precipitation) and tree species composition (monocultural vs. mixed plots of coniferous Pinus pinaster, and of broadleaf Betula pendula). We measured gross protein depolymerisation rates using a novel high‐throughput isotope pool dilution method, along with soil microbial biomass carbon and N to calculate microbial biomass‐specific activities of soil organic N processes. Overall, high soil water availability led to a 42% increase in soil protein depolymerisation rates compared to the unirrigated plots, but we found no effect of species composition on these soil organic N cycling processes. When investigating the interactive effect of tree species mixing and soil water availability, the results suggest that mixing tree species had a negative effect on soil organic N cycling processes in the non‐irrigated blocks subject to dry summers, but that this effect tended to become positive at higher soil water availability in irrigated plots. These results put forth that soil water availability could influence potential tree species mixing effects on soil organic N cycling processes in dry conditions.HighlightsTree species (with different litter C:N ratios) had little effect on protein depolymerisationIncreasing water availability via irrigation accelerated depolymerisation ratesNo interactive effect between tree species mixing and water availability, although trends emergedPositive trend of mixing under high water availability and negative trend under low water
Soil organic nitrogen (N) cycling processes constitute a bottleneck of soil N cycling, yet little is known about how tree species composition may influence these rates, and even less under changes in soil water availability such as those that are being induced by climate change. In this study, we used a 12‐year‐old tree biodiversity experiment in southwestern France to assess the interactive effects of soil water availability (half of the blocks seasonally irrigated to double precipitation) and tree species composition (monocultural vs. mixed plots of coniferous Pinus pinaster, and of broadleaf Betula pendula). We measured gross protein depolymerisation rates using a novel high‐throughput isotope pool dilution method, along with soil microbial biomass carbon and N to calculate microbial biomass‐specific activities of soil organic N processes. Overall, high soil water availability led to a 42% increase in soil protein depolymerisation rates compared to the unirrigated plots, but we found no effect of species composition on these soil organic N cycling processes. When investigating the interactive effect of tree species mixing and soil water availability, the results suggest that mixing tree species had a negative effect on soil organic N cycling processes in the non‐irrigated blocks subject to dry summers, but that this effect tended to become positive at higher soil water availability in irrigated plots. These results put forth that soil water availability could influence potential tree species mixing effects on soil organic N cycling processes in dry conditions. Highlights Tree species (with different litter C:N ratios) had little effect on protein depolymerisation Increasing water availability via irrigation accelerated depolymerisation rates No interactive effect between tree species mixing and water availability, although trends emerged Positive trend of mixing under high water availability and negative trend under low water
Soil organic nitrogen (N) cycling processes constitute a bottleneck of soil N cycling, yet little is known about how tree species composition may influence these rates, and even less under changes in soil water availability such as those that are being induced by climate change. In this study, we used a 12‐year‐old tree biodiversity experiment in southwestern France to assess the interactive effects of soil water availability (half of the blocks seasonally irrigated to double precipitation) and tree species composition (monocultural vs. mixed plots of coniferous Pinus pinaster, and of broadleaf Betula pendula). We measured gross protein depolymerisation rates using a novel high‐throughput isotope pool dilution method, along with soil microbial biomass carbon and N to calculate microbial biomass‐specific activities of soil organic N processes. Overall, high soil water availability led to a 42% increase in soil protein depolymerisation rates compared to the unirrigated plots, but we found no effect of species composition on these soil organic N cycling processes. When investigating the interactive effect of tree species mixing and soil water availability, the results suggest that mixing tree species had a negative effect on soil organic N cycling processes in the non‐irrigated blocks subject to dry summers, but that this effect tended to become positive at higher soil water availability in irrigated plots. These results put forth that soil water availability could influence potential tree species mixing effects on soil organic N cycling processes in dry conditions. HIGHLIGHTS: Tree species (with different litter C:N ratios) had little effect on protein depolymerisation Increasing water availability via irrigation accelerated depolymerisation rates No interactive effect between tree species mixing and water availability, although trends emerged Positive trend of mixing under high water availability and negative trend under low water
Soil organic nitrogen (N) cycling processes constitute a bottleneck of soil N cycling, yet little is known about how tree species composition may influence these rates, and even less under changes in soil water availability such as those that are being induced by climate change. In this study, we used a 12-year-old tree biodiversity experiment in southwestern France to assess the interactive effects of soil water availability (half of the blocks seasonally irrigated to double precipitation) and tree species composition (monocultural vs. mixed plots of coniferous Pinus pinaster, and of broadleaf Betula pendula). We measured gross protein depolymerisation rates using a novel high-throughput isotope pool dilution method, along with soil microbial biomass carbon and N to calculate microbial biomass-specific activities of soil organic N processes. Overall, high soil water availability led to a 42% increase in soil protein depolymerisation rates compared to the unirrigated plots, but we found no effect of species composition on these soil organic N cycling processes. When investigating the interactive effect of tree species mixing and soil water availability, the results suggest that mixing tree species had a negative effect on soil organic N cycling processes in the non-irrigated blocks subject to dry summers, but that this effect tended to become positive at higher soil water availability in irrigated plots. These results put forth that soil water availability could influence potential tree species mixing effects on soil organic N cycling processes in dry conditions. HighlightsTree species (with different litter C:N ratios) had little effect on protein depolymerisationIncreasing water availability via irrigation accelerated depolymerisation ratesNo interactive effect between tree species mixing and water availability, although trends emergedPositive trend of mixing under high water availability and negative trend under low water.
Author Augusto, Laurent
Tian, Ye
Maxwell, Tania L.
Fanin, Nicolas
Wanek, Wolfgang
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Keywords microbial biomass
precipitation
protein depolymerisation
biodiversity
TreeDivNet
amino acid uptake
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Snippet Soil organic nitrogen (N) cycling processes constitute a bottleneck of soil N cycling, yet little is known about how tree species composition may influence...
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SubjectTerms amino acid uptake
Availability
Betula pendula
Biodiversity
Biomass
Climate change
Community composition
Composition
Cycles
Depolymerization
Dilution
Environmental Sciences
France
irrigation
Irrigation water
Isotopes
microbial biomass
microbial carbon
Microorganisms
Moisture content
Nitrogen
Organic nitrogen
Pine trees
Pinus pinaster
plant available water
Plant species
precipitation
protein depolymerisation
Proteins
Soil
soil organic nitrogen
Soil water
Species composition
species diversity
TreeDivNet
trees
Trends
Water
Water availability
Title Water availability is a stronger driver of soil microbial processing of organic nitrogen than tree species composition
URI https://onlinelibrary.wiley.com/doi/abs/10.1111%2Fejss.13350
https://www.proquest.com/docview/2779249132
https://www.proquest.com/docview/2811977894
https://hal.inrae.fr/hal-04098843
Volume 74
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