The importance of the microbial food web and how it interplays with the classical food chain has gained considerable attention in temperate lakes. However its role in carbon transfer from pico- and nanoplankton to zooplankton and planktivores is relatively unknown in tropical lakes. Sampling of the microbial food web and experiments to estimate the growth rate and fate of its components were performed in Lake Victoria, East Africa, during the mixing season (May to August) 2002. Bacterioplankton and ciliate densities in Napoleon Gulf ranged from 6. 2 to 14. 9 cells x 10⁶&bull;mL^-1 and 51. 9 to 75. 2 cells&bull;mL^-1, respectively. Flagellate abundance was high, ranging from 70. 4 to 127. 9 cells x 10³&bull;mL^-1. Small flagellates, tentatively called Choanoflagellida, dominated the flagellate community by abundance and biomass. Bacterial growth rates were low, yet high abundance and cell size resulted in high bacterial production representing 24 to 38% of phytoplankton production. Protozoan growth rates and production are similar to values reported for other African lakes and the Laurentian Great Lakes. Protozoa were the dominant grazers of bacteria with grazing pressure switching from protozoa > 5 ??m in June to protozoa < 5 ??m (presumably flagellates) in July. In July, grazing on flagellates was from predators < 40 ??m, probably ciliates, while the ciliate community was grazed by > 40-??m plankton. Given that plankton of Lake Victoria is dominated by colonial cyanobacteria and raptorial zooplankton, protozoa could be an important pathway in the pelagic food web of Lake Victoria, East Africa.

The importance of the microbial food web and how it interplays with the classical food chain has gained considerable attention in temperate lakes. However its role in carbon transfer from pico- and nanoplankton to zooplankton and planktivores is relatively unknown in tropical lakes. Sampling of the microbial food web and experiments to estimate the growth rate and fate of its components were performed in Lake Victoria, East Africa, during the mixing season (May to August) 2002. Bacterioplankton and ciliate densities in Napoleon Gulf ranged from 6. 2 to 14. 9 cells x 10⁶&bull;mL^-1 and 51. 9 to 75. 2 cells&bull;mL^-1, respectively. Flagellate abundance was high, ranging from 70. 4 to 127. 9 cells x 10³&bull;mL^-1. Small flagellates, tentatively called Choanoflagellida, dominated the flagellate community by abundance and biomass. Bacterial growth rates were low, yet high abundance and cell size resulted in high bacterial production representing 24 to 38% of phytoplankton production. Protozoan growth rates and production are similar to values reported for other African lakes and the Laurentian Great Lakes. Protozoa were the dominant grazers of bacteria with grazing pressure switching from protozoa > 5 µm in June to protozoa < 5 µm (presumably flagellates) in July. In July, grazing on flagellates was from predators < 40 µm, probably ciliates, while the ciliate community was grazed by > 40-µm plankton. Given that plankton of Lake Victoria is dominated by colonial cyanobacteria and raptorial zooplankton, protozoa could be an important pathway in the pelagic food web of Lake Victoria, East Africa.

Environmental heterogeneity in both space and time has significant repercussions for community structure and ecosystem processes. Dimictic lakes provide examples of vertically structured ecosystems that oscillate between stable and mixed thermal layers on a seasonal basis. Vertical patterns in abiotic conditions vary during both states, but with differing degrees of variation. For example, during summer thermal stratification there is high spatial heterogeneity in temperature, nutrients, dissolved oxygen and photosynthetically active radiation. The breakdown of stratification and subsequent mixing of the water column in fall greatly reduces the stability of the water column to a vertical gradient in light. Nutrients and biomass that were otherwise constrained to the depths are also suspended, leading to a boom in productivity. Freshwater lakes are teeming with microbial diversity that responds to the dynamic environment in a seemingly predictable manner. Although such patterns have been well studied for nanoplanktonic phototrophic and heterotrophic populations, less work has been done to integrate the influence of mixotrophic nutrition to the protistan assemblage. Phagotrophy by phytoplankton increases the complexity of nutrient and energy flow due to their dual functioning as producers and consumers. The role of mixotrophs in freshwater planktonic communities also varies depending on the relative balance between taxon-specific utilization of carbon and energy sources that ranges widely between phototrophy and heterotrophy. Therefore, the role of mixotrophy in the microbial food web is difficult to predict because functional types of mixotrophs along a gradient of nutritional strategies contribute differently to nutrient cycling and carbon sequestration. The overall objective of this work was to advance existing knowledge of the abundance and activity of phagotrophy phytoplankton in lacustrine systems. The incorporation of mixotrophy into the microbial food web requires the complement of physiological studies in culture (as described in chapter 2) and quantification of activity (including abundance and bacterivory) in relation to strict phototrophs and heterotrophs in situ (as described in chapter 3 and 4). Information on the physiological ecology of mixotrophic protists is crucial to understanding their role in planktonic food webs and influence on the dynamic microbial community structure in lake ecosystems. An understanding of the ecological functioning of lakes has ultimate consequences for management of water resources, particularly in the face of global climate change. / Biology

Ce travail de thèse focalise sur le fonctionnement du réseau microbien de la lagune de Thau à travers une approche « Réseau » ayant permis l’étude simultanée de l’ensemble des groupes microbiens (21 groupes) des virus au microzooplancton. La croissance et la mortalité des micro-organismes ont été étudiées expérimentalement lors de plusieurs saisons puis d’une étude en mésocosme. Nous avons déterminé les proportions de mortalité dont sont responsables le microzooplancton et les virus au travers de la lyse virale. Un suivi in situ puis en mésocosme dans la lagune de Thau nous a permis d'observer la réponse des composantes du réseau microbien à un forçage typiquement Méditerranéen, la crue.Il apparait que les bactéries hétérotrophes ont les plus fortes croissances allant jusqu’à 2,18 jour-1. La croissance pour divers groupes pico- et nano-phytoplanctoniques était inférieure à 1,5 jour-1. La cause majeure de mortalité des différents groupes de micro-organismes étudiés est la prédation du microzooplancton (> 90% en moyenne), tandis que la lyse virale semble être un processus sporadique et nettement moins important. Le fait que les taux de prédation observés soient très proches des taux de croissance de différents micro-organismes suggère que le réseau microbien étudié présente une forte efficacité de transfert de la biomasse vers les niveaux trophiques supérieurs.Dans ce contexte, la crue provoque à court terme une diminution de la croissance microbienne et du broutage, alors qu’elle déclenche la lyse virale chez certains groupes. Cependant, la réactivité de ce réseau permet un rétablissement rapide indiquant une forte capacité de résilience de ce système. / The aims of this thesis work were to shed new lights on the functioning of the microbial food web (MFW) in the Thau coastal lagoon through a “global approach” that permit us to study simultaneously the entire MFW components (21 groups) from viruses to microzooplankton. Growth and mortality of microorganisms were studied experimentally along seasons and during a mesocosm experiment. We particularly focus on mortality due to microzooplankton (<200µm) grazing and viral lysis. Responses of the different components of the MFW under a typical Mediterranean forcing, flash flood, was also studied during an in situ monitoring and a mesocosm experiment in the Thau Lagoon.In conclusion, it appears that heterotrophic bacteria show the highest growth rates (until 2.18 day-1). Growth rates of pico- and nanophytolankton groups were always lower than 1.5 day-1. The major cause of mortality of the different group studied, reaching on average 90%, was due to the predation by the microzooplankton. Mortality due to viral lysis appeared to be a “sporadic processes”, less important than microzooplankton grazing indeed. In addition, the observed grazing rates or bacterivory were close to growth rates of microorganisms, suggesting an efficient trophic transfer of the microbial biomass towards higher trophic levels.River flash flood; an important forcing in the Mediterranean coastal zone; triggered on a short time scale, a decrease in growth and grazing rates of microorganisms whereas viral lysis was enhanced. However, the important dynamics of this studied MFW allowed the rapid reestablishment of growth and grazing rates, indicating a strong resilience capability of this system.

Les interactions entre les végétaux et les organismes telluriques sont déterminantes pour la décomposition des matières organiques et la nutrition minérale des plantes. L’objectif général de la thèse était de comprendre comment les interactions multi-trophiques dans la rhizosphere agissent sur la disponibilité en azote minéral et l’allocation en carbone dans la plante. Nous avons mis au point des dispositifs de culture de plante, permettant de contrôler l’environnement biotique des racines (inoculation par des espèces symbiotiques modèles : un protozoaire bactériophage et/ou une espèce mycorhizienne à arbuscules). Nous avons utilisé l’azote 15N et le carbone 13C pour tracer le cheminement de l’azote du sol vers la plante et le carbone assimilé par photosynthèse, de la plante vers le sol et les microorganismes du sol. L’allocation de C vers les racines et la rhizosphère est dépendante de la qualité de la litière foliaire enfouie. La structure de la communauté microbienne déterminée par l’analyse des profils d’acides gras (PLFA) est modifiée par la présence de protozoaires pour la litière à C/N élevé. Les mycorhizes à arbuscules et les protozoaires présentent une complémentarité pour l’acquisition du C et de N par la plante. Les protozoaires remobilisent l’azote de la biomasse microbienne par leur activité de prédation. Les hyphes fongiques transportent du C récent issu de la plante vers des sites riches en matière organique non accessibles aux racines. Ainsi, l’activité de la communauté microbienne est stimulée et la disponibilité en N augmentée lorsque des protozoaires sont présents. Les perspectives de ce travail sont de déterminer si (i) les interactions étudiées dans ce dispositif modèle peuvent être généralisées à d’autres interactions impliquant d’autres espèces de champignons mycorhiziens et de protozoaires (ii) la phénologie de la plante et la composition des communautés végétales influence la nature et l’intensité des réponses obtenues / Plants interact with multiple root symbionts for fostering uptake of growth-limiting nutrients. In turn, plants allocate a variety of organic resources in form of energy-rich rhizodeposits into the rhizosphere, stimulating activity, growth and modifying diversity of microorganisms. The aim of my study was to understand how multitrophic rhizosphere interactions feed back to plant N nutrition, assimilate partitioning and growth. Multitrophic interactions were assessed in a single-plant microcosm approach, with arbuscular mycorrhizal fungi (Glomus intraradices) and bacterial feeding protozoa (Acanthamoeba castellanii) as model root symbionts. Stable isotopes enabled tracing C (13C) and N (15N) allocation in the plant and into the rhizosphere. Plant species identity is a major factor affecting plant-protozoa interactions in terms of N uptake and roots and shoot morphology. Plants adjusted C allocation to roots and into the rhizosphere depending on litter quality and the presence of bacterial grazers for increasing plant growth. The effect of protozoa on the structure of microbial community supplied with both, plant C and litter N, varied with litter quality added to soil. AM-fungi and protozoa interact to complement each other for plant benefit in C and N acquisition. Protozoa re-mobilized N from fast growing rhizobacteria and by enhancing microbial activity. Hyphae of AM fungi acted as pipe system, translocating plant derived C and protozoan remobilized N from source to sink regions. Major perspectives of this work will be to investigate whether (i) multitrophic interactions in our model system can be generalized to other protozoa-mycorrhiza-plant interactions (ii) these interactions are depending on plant phenology and plant community composition

科学研究費補助金 研究種目:一般研究(C) 課題番号:03640552 研究代表者:浜 健夫 研究期間:1991-1992年度