Various aspects of the ecophysiology of rootless carnivorous Utricularia plants were assessed, with focus on nutrient acquisition and mutualistic interactions within trapping organs. The study includes extracellular enzyme measurements, the evaluation of commensal microbial community structure and function, stable isotope labelling to determine plant carbon allocation, and ion chromatography analyses of trap fluid composition

Coarse particulate organic matter (CPOM) is an essential part of the food chain in aquatic ecosystems because it represents a readily available carbon and energy source. The process by which it decomposes in rivers has been well studied and documented. However, the rate and extent of biodegradability of various CPOM components (i.e., twigs, leaves, grass, etc.) in storm drains is not well understood. The Jordan River TMDL study identified storm water generated CPOM as a likely cause of low dissolved oxygen levels in the lower Jordan River, but recent investigations have suggested that dissolved organic matter generated from this CPOM in storm drains and culverts entering into the Jordan River, rather than the CPOM itself, is the main driver of oxygen impairment. The degradability of CPOM components transported and stored in the storm drain system was studied to understand its relative impact on dissolved oxygen and nutrient status in the Jordan River. Results indicate the generation of highly degradable organic material is a function of the starting CPOM, and oxygen consumption is associated with the dissolved portion of organic material leached from CPOM in water. Leaves and grass produced the highest levels of all parameters studied. Between 93% to 95% of total oxygen demand is generated within the first 1 to 3 hours of the 24 hour test. Chemical oxygen demand and dissolved organic carbon proved to be the best indicator of biochemical oxygen demand. By using the results of the leaching study an estimate of water quality indicator levels in the Jordan River was made, and was compared to levels in samples collected from the Jordan River. The estimate proved accurate for dissolved organic carbon but not for total or volatile suspended solids. Results of this study were used to discuss possible solutions to reduce oxygen demand in the Jordan River.

Les systèmes côtiers pélagiques sont caractérisés par de multiples apports de matière organique particulaire (MOP) d’origine autochtone (phytoplancton) ou allochtone (continentale, benthique) dont la variabilité spatiale et temporelle peut être forte. L’objectif de ma thèse était 1) de quantifier la composition de la MOP des systèmes côtiers pélagiques, 2) de déterminer les forçages à sa dynamique spatio-temporelle et 3) d’investiguer le lien entre bactéries et composition de la MOP. Cette étude a été menée sur douze systèmes (estuaire, lagune, rias, baies, littoraux) distribués sur les trois façades maritimes françaises, en combinant rapports isotopiques et élémentaires (composition), acides gras (lien MOP-bactéries) et statistiques multivariées (forçages).A l’échelle multi-systémique et/ou intra-systémique, deux grands gradients sont observés :- un gradient côte (plus forte contribution continentale et benthique) – large (MOP phytoplanctonique), principalement lié à l’hydrodynamique sédimentaire (débits des fleuves, remise en suspension du matériel benthique) et à la proximité des sources allochtones- un gradient Sud (présence de MOP issue de la diazotrophie) – Nord (absence de cette MOP), en lien avec le statut trophique (oligo vs méso/eutrophie) des systèmes.La saisonnalité de la dynamique temporelle de la composition de la MOP est fortement variable selon les sites. Elle est généralement plus forte près de la côte et plus faible au large et en zone amont de l’estuaire étudié. Cette dynamique est également reliée à l’hydrodynamique sédimentaire.Enfin, l’étude a révélé que la biomasse bactérienne est principalement associée à la MOP continentale et benthique. / Pelagic coastal systems are characterized by multiple inputs of particulate organic matter (POM) from autochthonous (phytoplankton) and allochthonous (continental, benthic) origin whose spatial and temporal variability can be high. The aims of my PhD were to 1) quantify POM composition in pelagic coastal systems, 2) determine the forcings to its spatio-temporal dynamics and 3) investigate the link between bacteria and POM composition. This study was conducted on twelve systems (estuary, lagoon, bays, rias, littoral) distributed over the three maritime facades of France by combining the use of elemental and isotopic ratios (composition), fatty acids (POM-bacteria link) and multivariate analysis (forcings).At multi-systems and/or intra-system scale, two main gradients are observed:- an inshore (higher continental and benthic contribution) - offshore gradient (phytoplanktonic POM) mainly related to hydrodynamics and sedimentary hydrodynamics (river flow, resuspension of benthic material) and to the proximity to allochthonous sources- a South (POM related to diazotrophy) – North (absence of this POM) gradient, associated to the trophic status (oligo vs meso/eutrophy) of the studied systems.The seasonality of spatio-temporal dynamics of POM composition is highly variable depending on the station. It is in general higher near the coast and lower offshore and upstream in the studied estuary. This dynamic is also strongly associated to sedimentary hydrodynamics.Finally, this study highlight that bacterial biomass is mainly associated to continental and benthic POM.