La distribution de la neige à l'échelle du paysage dans les zones alpines est une des variables les plus importantes contrôlant la structure et la fonction des écosystèmes de montagne. Des changements d'épaisseur neigeuse et de durée d'enneigement peuvent entraîner de grands changements dans les conditions édapho-climatiques, ainsi que dans la composition des communautés végétales et surtout sur les cycles biogéochimiques majeurs et par conséquence la structure et le fonctionnement de l'écosystème. Nous avons utilisé l'approche métatranscriptomique pour essayer de comprendre la diversité fonctionnelle réelle et les activités exprimées dans les sols alpins par les micro-organismes, en réponse à différentes contraintes environnementales. La transcriptomique, et par extension, la métatranscriptomique, peut être vue comme l'analyse quantitative complète de tous les gènes exprimés par un ou plusieurs organismes, ou par l'écosystème entier. L'utilisation de cette approche implique d'abord l'extraction des ARN une bonne qualité et avec un bon rendement, ensuite la conversion de ces ARN en cDNA en ciblant les fractions de ARNm. La capacité d'évaluer le metatranscriptome des communautés microbiennes complexes dans différentes conditions environnementales représente en soi une avancée significative dans notre capacité de relier la structure et les fonctions des communautés avec les génotypes d'ADN (les séquences) et avec la correspondance phénotype. Dans cette étude, nous présentons l'utilisation pour la première fois de l'approche métatranscriptomique concernant les activités des communautés microbiennes des eucaryotes des sols alpins sous deux conditions d'enneigement très contrasté nommés LSM (lately snowmelt) et ESM (early snowmelt), qui sont caractérisés par des gradients climatiques contrastés et des différences de végétations associées. Nous présentons également une analyse des séquences et des procédures d'annotation en utilisant des logiciels publiquement disponibles et des scripts de python en utilisant l'environnent d'Obitools. Nous avons également développé un pipeline d'analyse bio-informatique adapté qui permet d'extraire correctement des renseignements fonctionnels et taxinomiques de ces bases de données. / The distribution of snow across the landscape in the Alps is one of the most important variables controlling the structure and function of mountain ecosystems. Changes in snow depth and duration can cause major changes in soil and climatic conditions, as well as the composition of plant communities and especially on the major biogeochemical cycles and consequently the structure and functioning of the ecosystem. We used the approach métatranscriptomique to try to understand the functional diversity and real activity expressed in Alpine soils by micro-organisms in response to different environmental constraints. Transcriptomics, and by extension, the métatranscriptomique, can be seen as full quantitative analysis of all genes expressed by one or more agencies or by the entire ecosystem. Using this approach involves first extracting RNA in good quality and good yield, then the conversion of RNA into cDNA by targeting mRNA fractions. The ability to assess metatranscriptome complex microbial communities under different environmental conditions is in itself a significant advance in our ability to link the structure and functions of communities with the genotypes of DNA (the sequence) and phenotype correspondence. In this study, we present the first use of the approach métatranscriptomique on the activities of eukaryotic microbial communities of alpine soil in two very contrasting locations called LSM (Lately snowmelt) and ESM (early snowmelt) which are characterized by contrasting climatic gradients and differences in vegetation associated. We present an analysis of sequences and annotation procedures using publicly available software and scripts using python programs and Obitools. We have also developed a pipeline of bioinformatics analysis adapted to correct extraction of information of the functional and taxonomic databases.

It is increasingly being recognized that the soil microbes can mineralize recalcitrant soil organic matter (SOM) by using the fresh carbon (C) as a source of energy, a process called priming effect (PE). It has been shown mostly in lab incubations that PE can have important consequences for sequestration of organic C in soils. However, the importance of PE in C and N dynamics of ecosystems remains little known. The soil-plant interactions and rhizospheric processes can modulate the rates of PE and its consequences on C and N dynamics in an ecosystem. The objective of this thesis was to determine the role of PE in the C and N dynamics of permanent grasslands and the modulation of this role in response to management (plant clipping, fertilization) and global warming. Moreover, it was aimed to identify the microbial groups involved in PE and to unravel the way, e.g. absorption of N, root exudations and litter deposition, by which plant can induce PE. The thesis was based on a new approach allowing continuous dual labelling of multiple grassland plants with 13C- and 14C-CO2. The dual labelling permitted the separation of soil-derived CO2 from plant-derived CO2, the calculation of PE and the determination of mean age of soil-derived CO2-C. Moreover, phospholipids fatty-acids analysis (PLFA) permitted to correlate the variation of PE with changes in microbial community composition. Our work showed that the increased SOM mineralization under grasses was consistently two to three times more than that in bare soils (i.e. PE) over long term (511 days). This reveals that the PE plays key role in ecosystem CO2-C flux and indicates that a very large pool of SOM is under the control of PE. Moreover, we report that 15,000 years old organic C from an undisturbed deep soil can be mineralized after the supply of fresh C by living plants to soil microbes. This result supports the idea that the SOM in deep soils is stable due to the energy-limitation of microbes and the ‘inert' pool of organic C defined in current models is not so ‘inert' finally. The supply of N in soil-plant system through the use of fertilizer or legume decreased the PE suggesting that the C storage in soils is limited by nutrient supply. Similarly, plant clipping reduced the plant N uptake thereby PE. Collectively these results suggest synchronization between plant N uptake and SOM mineralization supporting the idea that soils under permanent plant cover function as a bank of nutrients for the plant, maximizing plant productivity and nutrient retention. An innovative method clearly showed that the root exudation is the major way by which grassland plants induce PE. Moreover, saprophytic fungi are suggested as the key actors in the mineralization of recalcitrant SOM & PE. Lastly, we developed a new theory on temperature response of SOM mineralization by taking into account the energy-limitation of microbes and the temperature-dependent inactivation of enzymes. This theory predicts a negative relationship between temperature and mineralization of recalcitrant SOM, which was supported by experimental results. This finding challenges the classical paradigm of positive relationship between temperature and recalcitrant SOM mineralization. Overall, these investigations on plant-soil systems reinforce the idea that PE and underlying mechanisms play a key role in ecosystem C and N dynamics and even suggest that this role was underestimated in lab experiments. / It is increasingly being recognized that the soil microbes can mineralize recalcitrant soil organic matter (SOM) by using the fresh carbon (C) as a source of energy, a process called priming effect (PE). It has been shown mostly in lab incubations that PE can have important consequences for sequestration of organic C in soils. However, the importance of PE in C and N dynamics of ecosystems remains little known. The soil-plant interactions and rhizospheric processes can modulate the rates of PE and its consequences on C and N dynamics in an ecosystem. The objective of this thesis was to determine the role of PE in the C and N dynamics of permanent grasslands and the modulation of this role in response to management (plant clipping, fertilization) and global warming. Moreover, it was aimed to identify the microbial groups involved in PE and to unravel the way, e.g. absorption of N, root exudations and litter deposition, by which plant can induce PE. The thesis was based on a new approach allowing continuous dual labelling of multiple grassland plants with 13C- and 14C-CO2. The dual labelling permitted the separation of soil-derived CO2 from plant-derived CO2, the calculation of PE and the determination of mean age of soil-derived CO2-C. Moreover, phospholipids fatty-acids analysis (PLFA) permitted to correlate the variation of PE with changes in microbial community composition. Our work showed that the increased SOM mineralization under grasses was consistently two to three times more than that in bare soils (i.e. PE) over long term (511 days). This reveals that the PE plays key role in ecosystem CO2-C flux and indicates that a very large pool of SOM is under the control of PE. Moreover, we report that 15,000 years old organic C from an undisturbed deep soil can be mineralized after the supply of fresh C by living plants to soil microbes. This result supports the idea that the SOM in deep soils is stable due to the energy-limitation of microbes and the ‘inert' pool of organic C defined in current models is not so ‘inert' finally. The supply of N in soil-plant system through the use of fertilizer or legume decreased the PE suggesting that the C storage in soils is limited by nutrient supply. Similarly, plant clipping reduced the plant N uptake thereby PE. Collectively these results suggest synchronization between plant N uptake and SOM mineralization supporting the idea that soils under permanent plant cover function as a bank of nutrients for the plant, maximizing plant productivity and nutrient retention. An innovative method clearly showed that the root exudation is the major way by which grassland plants induce PE. Moreover, saprophytic fungi are suggested as the key actors in the mineralization of recalcitrant SOM & PE. Lastly, we developed a new theory on temperature response of SOM mineralization by taking into account the energy-limitation of microbes and the temperature-dependent inactivation of enzymes. This theory predicts a negative relationship between temperature and mineralization of recalcitrant SOM, which was supported by experimental results. This finding challenges the classical paradigm of positive relationship between temperature and recalcitrant SOM mineralization. Overall, these investigations on plant-soil systems reinforce the idea that PE and underlying mechanisms play a key role in ecosystem C and N dynamics and even suggest that this role was underestimated in lab experiments.

It is increasingly being recognized that the soil microbes can mineralize recalcitrant soil organic matter (SOM) by using the fresh carbon (C) as a source of energy, a process called priming effect (PE). It has been shown mostly in lab incubations that PE can have important consequences for sequestration of organic C in soils. However, the importance of PE in C and N dynamics of ecosystems remains little known. The soil-plant interactions and rhizospheric processes can modulate the rates of PE and its consequences on C and N dynamics in an ecosystem. The objective of this thesis was to determine the role of PE in the C and N dynamics of permanent grasslands and the modulation of this role in response to management (plant clipping, fertilization) and global warming. Moreover, it was aimed to identify the microbial groups involved in PE and to unravel the way, e.g. absorption of N, root exudations and litter deposition, by which plant can induce PE. The thesis was based on a new approach allowing continuous dual labelling of multiple grassland plants with 13C- and 14C-CO2. The dual labelling permitted the separation of soil-derived CO2 from plant-derived CO2, the calculation of PE and the determination of mean age of soil-derived CO2-C. Moreover, phospholipids fatty-acids analysis (PLFA) permitted to correlate the variation of PE with changes in microbial community composition. Our work showed that the increased SOM mineralization under grasses was consistently two to three times more than that in bare soils (i.e. PE) over long term (511 days). This reveals that the PE plays key role in ecosystem CO2-C flux and indicates that a very large pool of SOM is under the control of PE. Moreover, we report that 15,000 years old organic C from an undisturbed deep soil can be mineralized after the supply of fresh C by living plants to soil microbes. This result supports the idea that the SOM in deep soils is stable due to the energy-limitation of microbes and the 'inert' pool of organic C defined in current models is not so 'inert' finally. The supply of N in soil-plant system through the use of fertilizer or legume decreased the PE suggesting that the C storage in soils is limited by nutrient supply. Similarly, plant clipping reduced the plant N uptake thereby PE. Collectively these results suggest synchronization between plant N uptake and SOM mineralization supporting the idea that soils under permanent plant cover function as a bank of nutrients for the plant, maximizing plant productivity and nutrient retention. An innovative method clearly showed that the root exudation is the major way by which grassland plants induce PE. Moreover, saprophytic fungi are suggested as the key actors in the mineralization of recalcitrant SOM & PE. Lastly, we developed a new theory on temperature response of SOM mineralization by taking into account the energy-limitation of microbes and the temperature-dependent inactivation of enzymes. This theory predicts a negative relationship between temperature and mineralization of recalcitrant SOM, which was supported by experimental results. This finding challenges the classical paradigm of positive relationship between temperature and recalcitrant SOM mineralization. Overall, these investigations on plant-soil systems reinforce the idea that PE and underlying mechanisms play a key role in ecosystem C and N dynamics and even suggest that this role was underestimated in lab experiments.

La valeur esthétique des paysages et des espèces est un élément central de la conservation de la biodiversité, puisqu’elle fait intervenir les dimensions affectives et émotionnelles de notre rapport à la nature. Le lien entre biodiversité et perception esthétique demeure cependant peu étudié dans le cadre des services écosystémiques.Suite à un premier travail de synthèse ayant permis de poser les bases conceptuelles et méthodologiques de l’esthétique des paysages, trois études menées sur des systèmes sous-marins à différentes échelles ont permis de mieux comprendre et de quantifier le lien entre les différentes facettes de la biodiversité et la perception esthétique.Les résultats ont permis de mettre en évidence que la nature du lien entre biodiversité et préférences esthétique est dépendante de l’échelle de perception : à une échelle multi-spécifique, la biodiversité et la composition en espèces ont un effet positif sur les préférences esthétiques, tandis que les préférences à l’échelle spécifiques sont déconnectées du fonctionnement écologique des écosystèmes.Ces résultats confirment l’importance de la valeur esthétique dans notre perception de la biodiversité, qui pourrait avoir des conséquences majeures sur la façon dont nous protégeons notre environnement. L’approche fonctionnaliste de l’expérience esthétique est proposée et décrite afin de promouvoir une perception esthétique basée sur la compréhension et la reconnaissance des processus écologiques. Des pistes d’éducation à la biodiversité basée sur une expérience esthétique engagée sont également proposées afin de reconnecter les besoins écologiques et les préférences esthétiques. / The aesthetic value of landscapes and species is a central element for the conservation of biodiversity, since it involves the emotional and emotional dimensions of our relationship to nature. However, the links between biodiversity and aesthetic perception remains poorly studied and recognized within the ecosystem services framework.Following a first critical review, that described the conceptual and methodological bases of landscape aesthetics, three studies on underwater systems at different scales have been computed in order to better understand the link between the different facets of biodiversity and aesthetic perception.The results revealed that the link between biodiversity and aesthetic preferences is dependent on the scale of perception: at a multi-specific scale, biodiversity and species composition have a positive effect on aesthetic preferences, while preferences at a specific scale are disconnected to the ecological functioning of ecosystems.These results confirm the importance of aesthetic value in our perception of biodiversity, which could have major consequences in the way we protect our environment. The aesthetic experience based on the understanding of ecological functioning is proposed and described in order to promote an aesthetic perception relevant to ecological processes. Education to biodiversity based on engaged aesthetic is also proposed, in order to reconnect ecological needs and aesthetic preferences.