The severity of stratospheric ozone depletion in the temperate and polar latitudes has raised concerns about the sensitivity of terrestrial vegetation and ecosystems to solar ultraviolet (UV-B) radiation. This dissertation examined the responses of plants and microbes to solar UV-B for 3 years in Tierra de! Fuego, Argentina (55° S). This region is under the influence of the Antarctic "ozone hole" during the austral spring. Additionally, a quantitative review of the UV-B literature was conducted using a set of statistical techniques known as meta-analysis. For the field studies in Tierra de! Fuego, plots were established in a Sphagnum moss peatland and a Carexsedge fen during the spring of 1996. These plots received either near-ambient solar UV-B (90% of ambient) or reduced UV-B (20% of ambient) using specially designed plastic films. At the end of the first field season, no effects of the solar UV-B treatments were apparent on the growth and pigmentation of the plant species in either community The height growth of the moss Sphagnum mageffanicum was less under near-ambient solar UV-B than reduced UV-B during the second and third growing seasons. In contrast, volumetric density of the moss was greater under nearambient UV-B. The growth of the vascular plants did not respond to the solar UV-B treatments even after 3 years although UV-B-absorbing compounds were greater under near-ambient UV-B in some species. Populations of testate amoebae (i.e., shelled amoebae) inhabiting S. magellanicum had greater numbers under near-ambient UV-B than reduced UV-B throughout the 3 years. This response may be an indirect effect of solar UV-B mediated by the direct effect of UV-Bon S. mageffanicum height growth. Fungi on the leaf surfaces of the tree Nothojagus antarctica appeared to be directly inhibited by solar UV-B. The quantitative literature review of plant field studies simulating stratospheric ozone depletion assessed the effects of elevated UV-B on 10 plant response variables from papers published between 1976 and mid-1999. Modest significant inhibitions of leaf area, aboveground biomass, and plant height were apparent due to increased UV-B using meta-analysis. An increase in UV-B-absorbing compounds appears to be the most robust general response to increased UV-B radiation.

Dans un contexte de réchauffement climatique, la fonction puits de carbone des tourbières à sphaignes est susceptible d’être altérée en raison d’une modification des interactions sphaignes-microorganismes, responsables de l’accumulation de carbone. L’objectif de cette thèse a été (1) d’identifier les interactions chimiques entre les polyphénols des sphaignes et les communautés microbiennes des sphaignes et (2) d’évaluer l’impact du réchauffement climatique sur ces relations.Un dispositif expérimental (Open Top Chambers) simulant in situ une hausse modérée des températures (+ 1°C) a été installé sur la tourbière de Frasne (25). La hausse des températures a provoqué une modification du réseau alimentaire microbien avec l’augmentation de la biomasse des bactéries et une baisse importante (-70%) de la biomasse des prédateurs (amibes à thèque). Le réchauffement climatique a également induit une baisse de la production de polyphénols, diminuant ainsi leur effet inhibiteur sur les microorganismes. En parallèle à cette baisse, une hausse des activités enzymatiques phénoloxydases a également été enregistrée. Le réchauffement a ainsi modifié les relations polyphénols – phénoloxydases, deux éléments essentiels du cycle du carbone des tourbières.Les différents changements induits par le réchauffement climatique (polyphénols, phénoloxydases, réseau trophique microbien) ont aussi conduit à une modification des relations « sphaignes-microorganismes » via une accélération potentielle du recyclage des nutriments, ce qui pourrait influencer sur le long terme le fonctionnement de l’écosystème tourbière. / Carbon stocks of Sphagnum-peatlands are likely to be altered by climate warming due to important changes in “Sphagnum-microorganisms” relationships which are responsible for carbon sequestration. The objectives of the thesis are (1) to identify the chemical interactions between Sphagnum-polyphenols and Sphagnum associated microbial communities and (2) to understand the impact of warming on these relationships.An experimental design using Open-Top-Chambers (OTC) was used to simulate an increase of air temperatures (+1°C) on a peatland situated in Jura Mountains (Frasne, 25). Temperature increase induced a modification of the microbial food web with an increase of the biomass of bacteria and a strong decrease of the biomass of top-predators (-70%), i.e. testate amoebae. Warming also induced a decrease of Sphagnum-polyphenols, diminishing their inhibitory effect on microbial communities. In parallel, an increase of phenoloxidase enzymatic activities was recorded in OTC. Climate warming thus modified polyphenol-phenoloxidase interplay, two crucial components of carbon cycle in peatlands. Warming effects on the different components – i.e. polyphenols, phenoloxidases, microbial food web – induced a modification of Sphagnum-microbial communities interplay, favoring carbon and nutrient recycling, which could alter peatland functioning in long-term.