Short-term responses and resistance of soil microbial community structure to elevated CO2 and N addition in grassland mesocosms

Nitrogen (N) addition is known to affect soil microbial communities, but the interactive effects of N addition with otherdrivers of global change remain unclear. The impacts of multiple global changes on the structure of microbial communities may be mediated by specific microbial groups with different life-history strategies. Here, we investigated the combined effects of elevated CO2 and N addition on soil microbial communities using PLFA profiling in a short-term grassland mesocosm experiment. We also examined the linkages between the relative abundance of r- and K-strategist microorganisms and resistance of the microbial community structure to experimental treatments. N addition had a significant effect on microbial community structure, likely driven by concurrent increases in plant biomass and in soil labile C and N. In contrast, microbial community structure did not change under elevated CO2 or show significant CO2 × N interactions. Resistance of soil microbial community structure decreased with increasing fungal/bacterial ratio, but showed a positive relationship with the Gram-positive/Gram-negative bacterial ratio. Our findings suggest that the Grampositive/ Gram-negative bacteria ratio may be a useful indicator of microbial community resistance and that K-strategist abundance may play a role in the short-term stability of microbial communities under global change

Patterns in soil ammonia-oxidizer response to global change

Background/Question/Methods
The Domains Archaea and Bacteria contain the vast majority of Earth’s biodiversity and biomass, and their members play critical, often exclusive, roles in many biogeochemical cycles and ecosystem services. Human-induced global change, particularly with respect to increased nitrogen deposition, has the potential to drastically alter how soil nitrifying communities perform their biogeochemical function. Additionally, multi-factor global change can alter how microbial communities interact with each other and with the associated plant communities. This study, performed in the context of the long-term Jasper Ridge Global Change Experiment (JRGCE) in a California grassland ecosystem, examines how ammonia-oxidizing Archaea and Bacteria (AOA and AOB, respectively) respond to multi-factor global change. Manipulations at the JRGCE include simultaneous increases in CO2, warming, precipitation and nitrogen deposition. Past studies have utilized DNA-fingerprinting methods to assess ammonia-oxidizer response to multi-factor global change. This study compares how seed bank (DNA-based) versus metabolically active (RNA-based) ammonia-oxidizing communities respond to global change manipulations over several seasons. We have employed ultra-deep 454-pyrosequencing techniques to examine these communities using the ammonia monooxygenase (amoA) functional gene marker. Effects of global change have been examined at several phylogenetic levels and linked this community information to gross rates of nitrification using 15N stable isotopic methods. Ammonia-oxidizer and plant communities have been compared using multivariate statistical methods.

Results/Conclusions
Our results show that both AOB and AOA communities are highly influenced by nitrogen deposition in both their abundance and community structure. These changes are linked to increased nitrification rate in the elevated nitrogen deposition plots. Our results further show that the relationship between the AOB and plant communities fundamentally changes under long-term nitrogen deposition manipulation. This positive feedback loop may enhance the rate of change in ammonia-oxidizer communities, which may further elevate nitrification rates. This study provides strong evidence that incorporating microbial community and abundance information into global change predictions is crucial for understanding how ecosystem-level nutrient cycling rates may change.

*The audio track for talks in this symposium may be obtained at the following web address:*

*https://sites.google.com/site/esa2010symposium13audiocontent/esa2010-symposium13-audio-content

Responses of soil nitrite-oxidizers to global environmental changes

Background/Question/Methods
There is increasing evidence that global change can alter the structure of plant
communities with large impacts on the functioning of terrestrial ecosystems. However, little is known about the impact of global change on soil microbial communities. In particular, the response of soil nitrite-oxidizers microorganisms that mediate the second step of nitrification, a key process of the nitrogen cycle, has never been investigated.
Here, we examined the effects of four main global environmental changes on the activity, the abundance and the diversity of soil nitrite-oxidizers in an annual grassland ecosystem as part of the Jasper Ridge Global Change Experiment (CA, USA). This experiment includes four treatments - CO2, temperature, precipitation and nitrogen - with two levels per treatment (ambient and elevated, with elevated treatment based on prediction for the end of the century), and all of their factorial combinations. We measured potential nitrite oxidation, the abundance of soil Nitrobacter- and Nitrospiralike nitrite-oxidizers (using quantitative PCR targeting nxrA and 16S rRNA gene, respectively) and the diversity of soil Nitrobacter-like nitrite-oxidizers (using cloning sequencing targeting the nxrA gene) in each treatment combination at the end of the 7th and 8th growing seasons under treatments. Furthermore, we analyzed to what extent changes in the activity of the soil nitrite-oxidizers result from changes in their abundance or diversity.

Results/Conclusions
Simulated global environmental changes significantly altered the activity, as well as the abundance and the diversity of soil nitrite-oxidizers. Potential nitrite oxidation decreased with increased precipitation and increased with elevated CO2 when combined with added nitrogen or precipitation. The abundance of soil Nitrobacter-like nitrite-oxidizers also decreased with increased precipitation and increased with elevated levels of CO2 and nitrogen. In contrast, the abundance of soil Nitrospira-like nitrite-oxidizers increased with enhanced precipitation and decreased with elevated levels of CO2 and temperature. Finally, the structure of the soil Nitrobacter-like nitrite-oxidizers was significantly altered by the treatments. Consistent with results reported by Attard et al. (2010) for agroecosystems, we found that changes in potential rates of nitrite oxidation in response to treatments were partly explained by changes in the abundance of soil Nitrobacter-like nitrite-oxidizers, but not by changes in the abundance of soil Nitrospiralike nitrite-oxidizers, suggesting that Nitrobacter-like nitrite-oxidizers were the main functional players of the soil nitrite-oxidizing microbial community.
Our study provides evidence that global change could alter the abundance and diversity of soil nitrite-oxidizers, with potential impacts for soil nitrogen cycling.

*The audio track for talks in this symposium may be obtained at the following web address:*

*https://sites.google.com/site/esa2010symposium13audiocontent/esa2010-symposium13-audio-content

Global Change Could Amplify Fire Effects on Soil Greenhouse Gas Emissions

Background: Little is known about the combined impacts of global environmental changes and ecological disturbances on ecosystem functioning, even though such combined impacts might play critical roles in shaping ecosystem processes that can in turn feed back to climate change, such as soil emissions of greenhouse gases.[br/] Methodology/Principal Findings: We took advantage of an accidental, low-severity wildfire that burned part of a long-term global change experiment to investigate the interactive effects of a fire disturbance and increases in CO(2) concentration, precipitation and nitrogen supply on soil nitrous oxide (N(2)O) emissions in a grassland ecosystem. We examined the responses of soil N(2)O emissions, as well as the responses of the two main microbial processes contributing to soil N(2)O production - nitrification and denitrification - and of their main drivers. We show that the fire disturbance greatly increased soil N(2)O emissions over a three-year period, and that elevated CO(2) and enhanced nitrogen supply amplified fire effects on soil N(2)O emissions: emissions increased by a factor of two with fire alone and by a factor of six under the combined influence of fire, elevated CO(2) and nitrogen. We also provide evidence that this response was caused by increased microbial denitrification, resulting from increased soil moisture and soil carbon and nitrogen availability in the burned and fertilized plots. [br/] Conclusions/Significance: Our results indicate that the combined effects of fire and global environmental changes can exceed their effects in isolation, thereby creating unexpected feedbacks to soil greenhouse gas emissions. These findings highlight the need to further explore the impacts of ecological disturbances on ecosystem functioning in the context of global change if we wish to be able to model future soil greenhouse gas emissions with greater confidence

Nitrification, denitrification, and related functional genes under elevated CO2: A meta-analysis in terrestrial ecosystems

International audienceGlobal change may have profound effects on soil nitrogen (N) cycling that can induce positive feedback to climate change through increased nitrous oxide (N2O) emissions mediated by nitrification and denitrification. We conducted a meta-analysis of the effects of elevated CO2 on nitrification and denitrification based on 879 observations from 58 publications and 46 independent elevated CO2 experiments in terrestrial ecosystems. We investigated the effects of elevated CO2 alone or combined with elevated temperature, increased precipitation, drought, and N addition. We assessed the response to elevated CO2 of gross and potential nitrification, potential denitrification, and abundances of related functional genes (archaeal amoA, bacterial amoA, nirK, nirS, and nosZ). Elevated CO2 increased potential nitrification (+28%) and the abundance of bacterial amoA functional gene (+62%) in cropland ecosystems. Elevated CO2 increased potential denitrification when combined with N addition and higher precipitation (+116%). Elevated CO2 also increased the abundance of nirK (+25%) and nirS (+27%) functional genes in terrestrial ecosystems and of nosZ (+32%) functional gene in cropland ecosystems. The increase in the abundance of nosZ under elevated CO2 was larger at elevated temperature and high N (+62%). Four out of 14 two-way interactions tested between elevated CO2 and elevated temperature, elevated CO2 and increased precipitation, and elevated CO2 and N addition were marginally significant and mostly synergistic. The effects of elevated CO2 on potential nitrification and abundances of bacterial amoA and nirS functional genes increased with mean annual temperature and mean annual precipitation. Our meta-analysis thus suggests that warming and increased precipitation in large areas of the world could reinforce positive responses of nitrification and denitrification to elevated CO2 and urges the need for more investigations in the tropical zone and on interactive effects among multiple global change factors, as we may largely underestimate the effects of global change on soil N2O emissions

Impact des changements globaux sur le cycle de l'azote

Au cours de ma thèse, j ai cherché à évaluer l impact des changements globaux sur le cycle de l azote (N) et plus particulièrement sur la nitrification et la dénitrification. Les effets des changements globaux ont été étudiés à travers deux dispositifs : une expérience en serre dans laquelle des monocultures de Dactylis glomerata ont été soumises à une élévation de la teneur en CO2 couplée à une fertilisation azotée et une expérience in situ dans laquelle des parcelles de prairie annuelle ont été soumises aux effets individuels et combinés d une augmentation de la teneur en CO2, de la température, des précipitations et de la déposition d N. De plus, les effets interactifs d un feu accidentel et des traitements ont été explorés. Un résultat intéressant est l absence d effet des traitements sur la nitrification brute, malgré les effets marqués des traitements azotés sur la nitrification potentielle. Les réponses des deux étapes de la nitrification ont été également contrastées : la nitritation a été augmentée par la déposition d N, tandis que la nitratation a été réduite par le traitement précipitation. Des modifications de l abondance et de la structure des communautés impliquées pourraient être à l origine de ces réponses. La dénitrification potentielle a été augmentée dans les parcelles supplémentées en N et en eau, probablement du fait d une augmentation de la disponibilité en substrats et d une diminution de la teneur en oxygène du sol. Enfin, un des résultats les plus impressionnants de cette étude a été l impact très fort du feu sur les émissions de N2O, un puissant gaz à effet de serre, et ce particulièrement dans les parcelles sous fort CO2 et forte déposition d N.In my PhD thesis, I investigated the impact of global change on nitrogen (N) cycle and more specifically on nitrification and denitrification. Impacts of global change were assessed through two experimental designs: a greenhouse experiment in which monocultures of Dactylis glomerata were grown under the interactive effects of elevated CO2 and N supply, and an in situ experiment in which grassland plots were exposed to elevated CO2, temperature, precipitation, N deposition and all their combinations. In addition, the interactive effects of a wildfire and treatments were explored. An interesting result is the non-responsiveness of gross nitrification to global change treatments despite the large effects of N treatments on potential nitrification. The two steps of nitrification also showed contrasting responses to global change treatments: ammonia oxidation increased under high N deposition, while nitrite oxidation decreased in the elevated precipitation treatment. Changes in the abundance and structure of the microbial communities involved could be responsible for these responses. Potential denitrification increased under high N and high precipitation conditions, probably because of higher N availability and lower soil oxygen content. Finally, one of the most striking results of this study was the large impact of fire on soil emissions of N2O, a potent greenhouse gas, especially in the elevated CO2 and increased N deposition plots.ORSAY-PARIS 11-BU Sciences (914712101) / SudocSudocFranceF

Long-term effect of multiple global environmental changes on the retention and distribution of nitrogen in a grassland ecosystem

Long-term effect of multiple global environmental changes on the retention and distribution of nitrogen in a grassland ecosystem. Annual Meeting British Ecological Society and Société Française d'Ecologi

Increasing intraspecific diversity of wheat affects plant nutrient contents but not N recovery in the plant-soil system

Crop homogenization in conventional agriculture has been pervasive while ecology has shown positive effects of biodiversity on ecosystem functioning, that arise from complementarity/facilitation and sampling/selection effects. These effects are well documented for interspecific diversity in both natural ecosystems and agroecosystems but remain less documented at an intraspecific level, particularly for the rates of nutrient uptake by plants and nutrient losses from ecosystems. We conducted a field experiment with 88 experimental plots cultivated with 1, 2, 4 or 8 wheat varieties and 1, 2, 3 or 4 functional groups to assess the effects of the number of varietal and functional diversity of winter wheat on plant biomass production, plant nutrient contents (N, Ca, Cu, Fe, Mg, Mn, P, K, Na and Zn) and fertilizer N recovery in the plant-soil system using a 15N labeling method. We found both negative and positive effects of the number of varieties or number of functional groups on shoot Cu, Fe, Zn, Na and P contents, but no significant effects of intraspecific diversity on biomass production, N content and 15N recovery in the plant-soil system. Our results show differential responses to an increase of intraspecific diversity of wheat on the contents of several essential nutrients in plants and highlight the need to jointly analyze multiple nutrients. Our study also suggests that increasing intraspecific diversity had no overall negative effects on biomass production or N content. Using knowledge on variety functional traits to target specific complementarity mechanisms when designing variety mixtures could thus lead to a positive effect on nutrient absorption and biomass production

Predicting soil bacterial responses to multi-factor global change with trait-based modelling

Predicting soil bacterial responses to multi-factor global change with trait-based modelling. First Global Soil Biodiversity Conferenc

Coupling Between and Among Ammonia Oxidizers and Nitrite Oxidizers in Grassland Mesocosms Submitted to Elevated CO2 and Nitrogen Supply

International audienceMany studies have assessed the responses of soil microbial functional groups to increases in atmospheric CO2 or N deposition alone and more rarely in combination. However, the effects of elevated CO2 and N on the (de)coupling between different microbial functional groups (e.g., different groups of nitrifiers) have been barely studied, despite potential consequences for ecosystem functioning. Here, we investigated the short-term combined effects of elevated CO2 and N supply on the abundances of the four main microbial groups involved in soil nitrification: ammonia-oxidizing archaea (AOA), ammonia-oxidizing bacteria (AOB), and nitrite-oxidizing bacteria (belonging to the genera Nitrobacter and Nitrospira) in grassland mesocosms. AOB and AOA abundances responded differently to the treatments: N addition increased AOB abundance, but did not alter AOA abundance. Nitrobacter and Nitrospira abundances also showed contrasted responses to the treatments: N addition increased Nitrobacter abundance, but decreased Nitrospira abundance. Our results support the idea of a niche differentiation between AOB and AOA, and between Nitrobacter and Nitrospira. AOB and Nitrobacter were both promoted at high N and C conditions (and low soil water content for Nitrobacter), while AOA and Nitrospira were favored at low N and C conditions (and high soil water content for Nitrospira). In addition, Nitrobacter abundance was positively correlated to AOB abundance and Nitrospira abundance to AOA abundance. Our results suggest that the couplings between ammonia and nitrite oxidizers are influenced by soil N availability. Multiple environmental changes may thus elicit rapid and contrasted responses between and among the soil ammonia and nitrite oxidizers due to their different ecological requirements