L'étude du système aquifère du Chari Baguirmi vise à améliorer sa connaissance en vue d'une gestion durable etprudente de la ressource en eaux souterraines. Dans la zone d'étude qui couvre 70000 Km2, des campagnes demesures et d'échantillonnages des eaux et de sédiments ont été réalisés. Les eaux échantillonnées ont fait l'objetd'analyses chimiques et isotopiques (O18 et 2H) afin de comprendre le comportement hydrogéochimique dusystème aquifère. La synthèse des données géologiques existantes et la mise en évidence de l'hétérogénéité litho-stratigraphiquepar l'étude granulométrique ont confirmé la complexité hydrogéologique de la zone d'étude. La minéralogie desargiles a montré que le dépôt des différents sédiments se fait de la périphérie vers le centre de la dépression. Cemode de sédimentation permet d'avancer l'hypothèse de l'existence d'une dépression vers laquelle les sédimentsseraient entrainés par l'agent de transport. Cette hypothèse de “ dépression structurale ” réfute l'hypothèseadmise jusqu'à présent d'une origine hydrogéologique (forte évaporation) de cette dépression piézométrique.L'étude basée sur la piézométrie et les données chimiques et isotopiques (O18 et 2H) des eaux a permis decomprendre les processus hydrogéochimiques qui gouvernent la minéralisation des eaux. En plus des isotopes(O18 et 2H), l'utilisation des ratios Br/Cl, Sr/Ca et l'indice d'échanges de bases a permis de mettre en évidenced'une part, l'origine de la salinité des eaux de la dépression piézométrique et d'autre part, les phénomènesd'échanges de bases liés au long temps de séjour des eaux au contact des roches encaissantes et les zones derecharge potentielles de la nappe. / The study of the Chari Baguirmi aquifer system aims to improve the knowledge about this system forsustainable groundwater resource management. In the study area, which covers 70,000 km2, measurementcampaigns and sampling of water and sediments were undertaken. The waters have been sampled for chemicaland isotopic analyzes (18O and 2H) to understand the hydrogeochemical behavior of the aquifer system.The synthesis of existing geological data and highlighting the litho-stratigraphic heterogeneity through thegranulometric study confirmed the hydrogeological complexity of the study area. Clay mineralogy showed thatthe deposition of different sediments occurred from the periphery to the center of the depression. This mode ofsedimentation can hypothesize the existence of a depression into which sediments are trained by the transportagent. This assumption of "structural depression" refutes the hypothesis of a hitherto accepted hydrogeologicalorigin (high evaporation) of the piezometric depression. The study based on the piezometry and chemical and isotopic data (18O and 2H) of water enabled to understand the hydrogeochemical processes that govern the mineralization of the water. In addition to isotopes (2H and 18O), the use of ratios Br/Cl, Sr/Ca and base exchanges index has highlighted on the one hand, the origin of the salinity of waters in the piezometric depression and secondly, the phenomena of base exchanges related to longresidence time of water in contact with rocks and areas of potential groundwater recharge. Numerical modeling of the aquifer was performed in steady state and the results confirm the prevalence of the phenomenon of evaporation in the western p

L’océan Austral est soumis à la redistribution globale des contaminants par les voies atmosphérique et océanique. Cependant, la contamination des écosystèmes austraux est très peu connue, en particulier dans le secteur Indien. De par leur toxicité, leur mobilité et leur capacité à se bioaccumuler dans les tissus des organismes et à se bioamplifier dans les réseaux trophiques, le mercure (Hg) et les polluants organiques persistants (POPs) comptent parmi les contaminants les plus préoccupants. Du fait de leur position élevée dans les réseaux trophiques, les oiseaux marins sont exposés à de grande quantités de contaminants par la voie alimentaire. En conséquence, ils sont souvent utilisés comme bioindicateurs de l’état de contamination des écosystèmes, par le biais des plumes et du sang, qui peuvent être échantillonnés de façon non destructive. Ma thèse s’est intéressée aux nombreuses espèces d’oiseaux marins (plus de 40) qui nichent au sein des Terres Australes et Antarctiques Françaises, au sud de l’Océan Indien, afin de décrire et expliquer les niveaux de contaminants le long d’un large gradient latitudinal, de l’Antarctique à la Zone Subtropicale, et d’identifier les meilleures espèces bioindicatrices pour un suivi à long terme de la contamination de ces écosystèmes. Au cours d’une première étape méthodologique, les manchots et les poussins de toutes les espèces ont été identifiés comme de bons bioindicateurs de contamination puisque, à la différence de la plupart des oiseaux adultes, ils présentent une faible variabilité des niveaux de contaminants dans les plumes. Au cours d’une seconde étape explicative, l’effet de facteurs intrinsèques (traits individuels) et extrinsèques (écologie alimentaire déduite grâce à la méthode des isotopes stables) sur les niveaux de contaminants a été évalué dans les plumes des oiseaux de la communauté de Kerguelen (27 espèces) et dans le sang du grand albatros de Crozet (180 individus dont les traits de vie sont connus). L’écologie alimentaire s’est avérée être le principal facteur explicatif des niveaux de contaminants, tandis que l’âge, le sexe, la phylogénie et le statut reproducteur jouent un rôle mineur. La classe d’âge est néanmoins un facteur à prendre en compte, puisque les poussins montrent souvent des concentrations inférieures aux adultes. Au cours d’une troisième étape, les variations spatio-temporelles de la contamination ont été étudiées en utilisant une sélection d’espèces bioindicatrices et en tenant compte de leur écologie alimentaire. Plusieurs résultats portant sur différentes espèces (oiseaux océaniques) et populations (poussins de skua) ont montré que, contrairement aux prédictions, l’exposition des oiseaux au Hg augmente graduellement des eaux antarctiques aux eaux subantarctiques puis aux subtropicales, alors que l’exposition aux POPs, en accord avec la théorie de la distillation globale, montre la tendance inverse. D’autre part, la comparaison des concentrations en Hg dans les plumes de manchot, effectuée entre des spécimens de musée et des échantillons actuels, indique que leur exposition au Hg n’a pas changée depuis les années 1950-1970. Toutefois, des espèces subantarctiques montrent une tendance à la hausse. De futures études devraient viser à l’utilisation des plumes comme tissu de référence pour l’évaluation et le suivi de la contamination des écosystèmes, en particulier en ce qui concerne les POPs. Parmi les nombreuses espèces étudiées au cours de ces travaux de thèse, les bioindicateurs les plus pertinents se révèlent être le manchot empereur et le pétrel des neiges (Antarctique), le manchot royal, le pétrel bleu et l’albatros à sourcil noirs (subantarctique), le gorfou sauteur subtropical et l’albatros à bec jaune (subtropical). Le suivi à long terme de ces espèces permettra d’évaluer l’évolution temporelle de l’état de contamination de l’océan Austral. / Antarctic and subantarctic marine environments are reached by inorganic and organic contaminants through ocean circulation and atmospheric transport. Yet, environmental contamination is poorly known in the Southern Ocean, in particular in the Indian sector. Among environmental contaminants, mercury (Hg) and persistent organic pollutants (POPs) are primarily of concern, because they are toxic, highly mobile, and they bioaccumulate in the tissues of living organisms and biomagnify up the food web. Seabirds, as upper predators, are exposed to large quantities of contaminants via food intake and have widely served as biomonitors of marine contamination, notably through the non-destructive sampling of their feathers and blood. My doctoral work has focussed on the abundant and diverse seabird species (more than 40) breeding in the French Southern and Antarctic Lands, southern Indian Ocean, in order to describe and explain contaminant concentrations over a large latitudinal gradient, from Antarctica to the subtropics, and to identify the best bioindicator species for contaminant biomonitoring. In a first methodological step, seabirds with synchronous moult of body feathers (adult penguins and chicks of all species) were recognised as good candidates as bioindicators, because, unlike most adult birds, they present low within-individual variation in feather contaminant concentrations. In a second explanatory step, the influence of intrinsic (individual traits) and extrinsic factors (feeding ecology inferred from the stable isotope method) driving variation in contaminant concentrations was evaluated in feathers of the large avian community of the Kerguelen Islands (27 species) and in blood of wandering albatrosses from the Crozet Islands (180 birds of known individual traits). Feeding ecology was the main factor driving variation in contaminant concentrations of blood and feathers, both at the community, population and individual levels, whereas age, sex, phylogeny and breeding status played a minor role. Age-class was however an important intrinsic factor to consider, with chicks usually having lower concentrations than adults. In a third step, spatio-temporal patterns of contamination were studied through selected bioindicator species and by taking into account their feeding habits. Results from different species (oceanic seabirds) and populations (skua chicks) showed that, contrary to predictions, Hg exposure gradually increases from Antarctic to subantarctic and subtropical waters, whereas, in accordance with the global distillation theory, POPs exposure has the opposite pattern. Comparisons between penguin feathers from museum collections and contemporary samples showed that bird exposure to Hg is overall not different today when compared to 50-70 years ago, but subantarctic species are possibly experiencing an increasing trend. Future research efforts should be focussed on the use of feathers as biomonitoring tools, in particular for POPs determination. The best recommended bioindicator species include the emperor penguin and snow petrel (Antarctic), king penguin, blue petrel and black-browed albatross (subantarctic), and northern rockhopper penguin and Indian yellow-nosed albatross (subtropical). Future biomonitoring studies on these species will give invaluable insights into the poorly-known temporal trends of environmental contamination in the Southern Ocean.

L’étude de l’écologie alimentaire d’une espèce est une clé de la compréhension de sa biologie et de son fonctionnement dans l’écosystème. Ainsi, les interactions proies-prédateurs sont une des voies qui structurent et déterminent les dynamiques des populations et le réseau trophique à l’échelle d’un écosystème. Parmi les sites d’étude d’intérêt majeur, le milieu marin est un espace soumis à des forçages naturels et anthropiques. A l’échelle de l’Océan Atlantique Nord-Est, le Golfe de Gascogne est une vaste baie bordée par l’Espagne au sud et la France à l’est. Ce Golfe est le siège historique d’une intense activité de pêches commerciales pour lesquelles les principales espèces de petits poissons pélagiques ciblés sont la sardine, Sardina pilchardus, et l’anchois, Engraulis encrasicolus. L’objectif de ces travaux est d’analyser l’écologie alimentaire printanière, de ces deux petits poissons pélagiques dans le Golfe de Gascogne. Pour ce faire, le premier volet s’est focalisé sur le compartiment des proies mésozooplanctoniques via deux approches : la caractérisation de leurs dynamiques spatio-temporelles sur la décennie 2003-2013 et la mesure de leur contenu énergétique au printemps. Il apparaît, à cette saison, que tous les types de proies ne se valent pas énergétiquement et que notre site d’étude représente une mosaïque d’habitats alimentaires. De plus, la communauté mésozooplanctonique printanière présente une forte structuration spatiale, une évolution temporelle marquée par un changement majeur d’abondance et un contrôle par la biomasse de microphytoplancton. Le second volet de ces travaux est relatif à une approche méthodologique de l’analyse de l’écologie alimentaire de S. pilchardus et E. encrasicolus. Trois traceurs trophiques distincts ont été utilisés : les ratios isotopiques du carbone et de l’azote, la faune parasitaire et les niveaux de contamination en mercure. Pour perfectionner l’utilisation du premier de ces traceurs, une approche expérimentale a été menée sur S. pilchardus pour déterminer un facteur de discrimination trophique. Finalement, il apparaît que l’utilisation de ces trois traceurs a toujours permis de mettre en évidence une variabilité temporelle relative de l’écologie alimentaire des poissons étudiés. En revanche, aucune dynamique spatiale n’a pu être détectée via ces traceurs. / Dietary studies of marine species constitute an important key to improve the understanding of its biology and of its role in the ecosystem. Thus, prey-predator relationships structure and determine population dynamics and the trophic network at the ecosystem scale. Among the major study sites, the marine ecosystem is submitted to natural and anthropogenic constraints. In the North-Eastern part of the Atlantic Ocean, the Bay of Biscay is a large open area surrounded South by Spain and East by France. This bay is an historic place of intense fishery activities for which the main small pelagic species targeted are the pilchard, Sardina pilchardus and the anchovy, Engraulis encrasicolus. The aim of this work is to analyze the trophic ecology of these two small pelagic fish in spring in the Bay of Biscay. To do this, a first section is devoted to their prey composed by the mesozooplanktonic compartment, through a two-fold approach: the characterization of their spatio-temporal dynamics during the decade 2003-2013 and the measurement of their energetic content in spring. For this season, it appears that all prey types are not worth energetically and that the Bay of Biscay represents a mosaic of dietary habitat. Moreover, the spring mesozooplankton community presents a strong spatial structuration, a temporal evolution marked by a major change in abundance and a control by the microphytoplankton biomass. The second section of this work is relative to a methodological approach of the trophic ecology of S. pilchardus and E. encrasicolus. Three different trophic tracers have been used: isotopic ratios of carbon and nitrogen, parasitological fauna and mercury contamination levels. To improve the use of the first of these trophic tracers, an experimental approach has been conducted with S. pilchardus to determine a trophic discrimination factor. Finally, it appears that the use of these three trophic tracers has always been permitted to highlight a temporal variability of the relative trophic ecology of these fish. However, no spatial dynamics could be identified through these three trophic tracers.

Les tendances spatiales et temporelles du mercure en Arctique ont été étudiées au travers de l’analyse de ce métal dans les tissus durs, i.e. dents et poils, des phoques annelés (Phoca hispida) et des ours polaires (Ursus maritimus). Aucune influence du sexe sur les concentrations n’a été détectée dans les tissus de ces deux espèces alors que l’âge est apparu comme un facteur d’influence important.Deux tendances spatiales ont été observées dans les tissus de ces deux espèces : un premier gradient d’augmentation du mercure de l’Est vers l’Ouest de l’Arctique, i.e. de Svalbard, vers le Groenland et enfin, l’Arctique canadien, et un second du Sud vers le Nord de l’Arctique canadien, résultant très probablement de la minéralogie du socle rocheux, mais aussi potentiellement de facteurs biotiques et abiotiques.Une tendance à l’augmentation des concentrations de mercure a été globalement détectée entre la période préindustrielle et la fin du XXe siècle. Cependant, les variations temporelles associées à la seconde partie du XXe siècle révèlent une augmentation continue dans l’Ouest de l’Arctique et une tendance à la diminution dans l’Est de l’Arctique, cette différence étant probablement liée à des apports distincts des masses d’air atmosphériques à ces deux régions. Par ailleurs, une composante de variabilité climatique pourrait contribuer aux variations observées ces dernières décennies en influençant les habitudes alimentaires de ces prédateurs marins arctiques. Ainsi, les isotopes stables d’azote et de carbone s’avèrent être un outil essentiel à coupler aux études sur les tendances de mercure pour permettre de déterminer la part d’un changement dans le régime alimentaire ou dans les niveaux environnementaux.Cette étude a mis en évidence l’importance des poils comme tissu de monitoring non-invasif et pertinent pour un suivi régulier voire annuel tandis que l’utilisation des dents s’avère être plus adaptée à la reconstruction de tendances sur le long-terme. / The spatial and temporal trends of mercury in the Arctic have been studied through the analysis of this metal in hard tissues, i.e. teeth and hair, in ringed seals (Phoca hispida) and polar bears (Ursus maritimus). Sex had no influence on the mercury concentrations while age was a significant factor. Two distinct spatial trends were observed in the tissues of these two species: a first gradient of augmentation from the East to the West of the Arctic, i.e. from Svalbard towards Greenland and the Canadian Arctic, and a second one, from the South to the North of the Canadian Arctic, resulting probably from a combination of the global mineralogy in the Arctic with biotic and abiotic factors. An increasing trend in mercury concentrations has been detected globally between the preindustrial period and the end of the 20th century. However, the temporal trends detected in the second part of the 20th century revealed an increase in the West Arctic while a decrease was observed in the East Arctic. This difference seems to be due to a distinct input of the atmospheric air masses to the two regions. Besides, a climatic variability could contribute to the variations observed these last decennials by influencing the habitat and the feeding habits of the marine predators. Thus, the determination of the stable isotopes seems to be essential to combine to the study of the mercury trends. Finally, this study has showed the importance of hair as a non-invasive and relevant biomonitoring tissue on a regular or annual sampling base, while the use of the teeth seems to be more adequate for reconstructing long-term trends of mercury.

In tropical forests, ants are numerous, diversified and ecologically important, being present from forest floor to upper canopy and exploiting a wide variety of diets. Nearly half of the ant species are directly in contact with the ground stratum, including the leaf-litter and the underlying soil, for nesting or foraging. The main factors known to influence ant distribution and abundance can be environmental (e.g. heterogeneous distribution of microhabitat size, nutrient availability, microclimate, soil properties) or biotic (e.g. inter- and intraspecific competition, prey availability). Some of these factors, such as leaf-litter volume or prey availability, may also vary seasonally. Also, the Ecuadorian Andes are known as being a hotspot of biodiversity for a large array of organisms, but it was not documented until now if this is also the case for ants.<p><p>The general aim of the PhD project was to identify, by both descriptive and experimental approaches, the factors determining the structure of a ground-dwelling ant assemblage at a small-spatial scale and its temporal variation in an evergreen premontane tropical forest of the Ecuadorian Andes.<p><p>In the descriptive part of the project, we studied both horizontal (along a transect) and vertical (across ground layers) species diversity and distribution of ground-dwelling ants. To attempt to explain the observed patterns, we measured a series of environmental factors varying at small spatial scale and/or seasonally: canopy openness, leaf-litter quantity, slope, and a series of soil physico-chemical properties (e.g. texture). The ant assemblage richness appeared to be at least as high as in the Amazonian Basin, with up to 33 species per m². The heterogeneity of species spatial distribution at small spatial scale was high, with distinct species composition (average Jaccard index = 0.2 ± 0.08 SD) and abundance (up to 40 fold) in contiguous plots. We observed a strong seasonal effect on the ant assemblage structure. The higher ant diversity and abundance found at the surface and in the mineral soil during the dry season suggested a seasonal peak of activity on the ground surface and the seasonal migration of drought-sensitive species downwards in the soil. Ant diversity was related to distinct environmental factors according to the ground layer considered. We found strong correlations between litter amount and dominant ant distribution in the leaf-litter layer, while we found no correlation with any factor in the soil layer. The low amount of negative association between dominant species suggested a low interspecific competition.<p><p>In the experimental part of the project, our aim was to identify experimentally the relative importance of habitat size vs. prey availability in structuring the leaf-litter ant assemblage. We studied the response of various ant trophic groups to an increased nutrient availability which boosted the decomposition of their leaf-litter habitat and enhanced the abundance of their prey. Bottom-up effect on the ant fauna (and other predaceous arthropods) regarding species composition and dominance was also studied. Stable isotope analysis was used to distinguish trophic groups among ants and mesofauna. Ants responded differentially according to their trophic group: despite increased prey availability, predatory species were negatively affected by nutrient supply, while other ant trophic group densities did not change. Our results showed that predatory ants are limited by habitat size rather than by prey availability, and that these ants are more affected by habitat loss than their prey, other ant trophic groups and other macrofauna taxa. Furthermore, a taxonomic shift occurred within each ant trophic group, leading to the replacement of dominant genera in fertilized plots.<p><p>As a conclusion, our results emphasize the importance of distinguishing layers among the ground matrix, since both ant faunas and their response to environmental factors vary vertically and seasonally. The distribution of ground-dwelling ants was only weakly explained by both the environmental factors measured and by biotic interactions, at a small spatial scale. Also, our results emphasize the importance of distinguishing trophic groups among the ant assemblage, since the response of these groups under changing conditions was different. In this regard, stable isotope analysis was a useful tool for investigating the trophic ecology of various leaf-litter taxa, and it was successfully used for the first time to assess the diet of leaf-litter ants and their position in the Brown Food Web relative to other taxa. Also, the isotopic approach allowed us to increase the knowledge about the biology of a rare and cryptic ant species, by revealing its top-predatory position. The outstanding local species richness that we observed confirms that the Ecuadorian Andes are also a biodiversity hotspot for ants. / Doctorat en Sciences agronomiques et ingénierie biologique / info:eu-repo/semantics/nonPublished

Water flow and geochemical processes within the unsaturated zone (UZ) in two distinct types of karst environment were investigated using natural tracers (chemistry, stable isotopes 13 C, 18 O, 2 H, and 3 H, 14 C, 87 Sr/86 Sr). The extent of horizontal flow component and the response of drip water chemistry to recharge events were examined in the Moravian Karst (Czech Republic), while the character of water flow and its chemistry were studied in salt diapirs in southeastern part of the Zagros mountains (Iran). Under the conditions of well-developed epikarst, the horizontal flow component, defined as Hmax/T (Hmax = horizontal migration component, T - thickness of VZ) typically reaches values of 0.1 - 0.6 (Moravian and Slovenian Karst). However, in areas where epikarst was stripped off by glacial or human activity, the proportion of horizontal flow component is far greater (Hmax/T 1.6 - 24). This parameter is vital for the design of water source protection zones above caves. Nitrate mean residence time in 120 m thick VZ of the Moravian karst exceeded 16 years. The VZ above the Ochoz Cave (Moravian Karst) represents a semi-open to open system with respect to soil CO2. Under a high drip rate (high flow), the event water only made 5% of the total. During the year, water degassing and so called prior...

L'objectif de cette thèse est d'étudier les réponses adaptatives des métazoaires à une diminution de la disponibilité en nutriments dans leur environnement. Ce travail, couplant des approches d'écologie isotopique et de transcriptomique, est basé sur l'analyse comparative d'isopodes de surface (épigés) et souterrains (hypogés) évoluant depuis plusieurs millions d'années dans des environnements présentant des disponibilités en nutriments très contrastées (absence de photosynthèse en milieu souterrain). Leur histoire évolutive (multiples colonisations indépendantes du milieu souterrain) a permis de définir 13 couples composés d'une espèce épigée et d'une espèce hypogée partageant un ancêtre commun épigé (i.e. 13 réplicats indépendants d'une transition vers un milieu plus pauvre en nutriments). Des adaptations en termes d'amélioration de l'acquisition des nutriments (diminution de la sélectivité trophique, stratégies spécialistes) et de diminution de la demande métabolique (diminution du taux de croissance) ont été mises en évidence chez les isopodes hypogés. En revanche, l'hypothèse d'une sélection _stoechiogénomique_ des nucléotides et acides aminés les plus économes en azote a été réfutée. Il est possible que la sélection naturelle soit inopérante sur la composition des ARN et protéines de par les faibles tailles efficaces de population (Ne) des métazoaires. La sélection pourrait aussi être inexistante à ce niveau, de par l'existence d'interactions entre les différentes réponses adaptatives. Ainsi, l'adoption de certaines réponses adaptatives plus efficaces et/ou rapides à mettre en place pourrait suffire à relâcher la pression de sélection sur les autres réponses / The aim of this PhD project was to investigate the adaptive responses of metazoan to a decrease of nutrient availabilities in their environment.We combined isotopic ecology and Next-Generation Sequencing in a comparative analysis of surface (epigean) and groundwater (hypogean) isopods living in highly contrasted environments in terms of nutrient availabilities (lack of photosynthetic production in groundwater). The original evolutionary history of these isopods (multiple independent colonizations of the subterranean habitat) enabled to define 13 species pairs composed of one epigean and one hypogean species sharing a common epigean ancestor. Using these pairs, we studied 13 independent replicates of an environmental transition towards very low nutrient availabilities. Hypogean isopods display adaptations improving the nutrient acquisition (specialist strategy, decrease of trophic selectivity) as well as adaptations reducing the metabolic needs of organisms (decrease of growth rate). However, hypogean isopods do not display adaptive changes in their macromolecules composition (no evidence for the ’stoichiogenomic’ selection of N-thrifty nucleotides and amino acids). Because of the small effective population size (Ne) of metazoa, natural selection may be inefficient to select N-sparing responses at the level of RNA and protein composition. Selection could also be inexistent at this level in case of interactions between the different adaptive responses. Indeed, some nutrientsaving mechanisms may have been selected more quickly or more efficiently, these adaptations being sufficient to relax the selective pressure on the other response levels

Coastal forest retreat in the Florida Keys during the 20th century has been attributed to a combination of sea level rise and hurricane storm surge impacts, but the interactions between these two disturbances leading to forest decline are not well understood. The goal of my research was to assess their effects over a period spanning more than two decades, and to examine the relationships between these press and pulse disturbances and freshwater availability in pine rockland, hardwood hammock, and supratidal scrub communities. Impacts and recovery from two storm surges, Hurricanes Georges (1998) and Wilma (2005), were assessed with satellite-derived vegetation indices and multiple change detection techniques. Impacts were greater at lower elevations, and in hardwood hammock, spectral signatures indicative of plant stress and productivity returned to pre-disturbance levels within a few years. In pine rockland, impacts were predominately related to Hurricane Wilma, however, a similar return to pre-disturbance conditions was absent, suggesting that trajectories of disturbance recovery differed between the two communities. Long-term monitoring of forest composition, structure, and groundwater salinity showed that compositional shifts in the low shrub stratum were associated with salinization of the freshwater resource attributable to sea level rise. Throughout the course of twelve months of climate and groundwater monitoring (2011-2012), groundwater salinity generally decreased in response to large precipitation events. Modeling of geophysical data indicated that groundwater salinity was an important predictor of community type. Isotopic analysis of d18O in plant stem water and foliar d13C was used to determine temporal and spatial patterns in water use and plant stress in two community dominants, slash pine, Pinus elliottii var. densa, and buttonwood, Conocarpus erectus. Both species relied heavily on groundwater, and plant stress was related to increasing groundwater salinity. The results of this work suggest that the interaction of press and pulse disturbances drive changes in community composition by causing mortality of salt-sensitive species and altering the freshwater resource.

Reconstruction studies of seasonal rainfall utilizing stable isotope based proxy approach suffer from the limitations of time resolutions. Conventional methods and archives limit the achievable resolution to annual scales. However, high resolution reconstruction (seasonal to sub-weekly scale) can be achieved in proxy records where growth rates are high enough to leave spatial signatures in an organically or inorganically deposited layer such as growth bands. In this study, aragonitic skeleton of the gastropod Lissachatina fulica (Bowdich, Giant African Land Snails) is investigated with an aim to achieve sub-weekly scale reconstruction of the Indian monsoon rainfall. These terrestrial gastropods are native of Africa and highly invasive. Their evolution in the geological time period dates back to the Pliocene and is presently distributed across the tropical belt. They exhibit a high growth rate in the presence of water and high relative humidity in the environment. As a result, they are ideally suited for the task of palaeo seasonality reconstruction. The isotopic patterns recorded in their growth bands reveal composition of environmental water at seasonal time scales. In vitro studies were carried out on L. fulica to estimate their growth rates and growth responses to changes in the physical conditions within the culture chamber. The Indian monsoon rainfall exhibits characteristic dry spells that are generally sandwiched between periods of active phases of high rainfall during the South West monsoon season. These dry spells are typically characterized by rainfall with low intensity. Isotope fingerprinting of the rain water at daily time resolution, covering the years of 2007-10 exhibited distinct isotopic ratios for the dry and wet spells. Dry spells were clearly demarcated in the record with isotopically enriched signature. In addition, the study indentified the role of three distinct moisture sources on δ18O of rain water at Bangalore, India. The variability in the oxygen isotopic composition of the Indian monsoon rainfall is predominantly controlled by this source moisture variability at inter annual time scales, while temperature and amount of rainfall tend to dominate the variability in the precipitation isotopes at seasonal and weekly scales. Simultaneous isotopic analyses of both rainwater and shell carbonates growth bands were undertaken to understand their relationship to aid in high resolution reconstruction. Carbonate found in the growth bands of the gastropods, which is precipitated under equilibrium condition from rainwater, preserves the signature of rainfall. This provides an opportunity to reconstruct rainfall parameters (i.e. amount and moisture sources) knowing the variability in shell carbonates. Stable isotopic ratios measured across the growth bands of live shell specimens collected from the southern and eastern Indian regions (Bangalore and Kolkata, respectively) were compared with the rainfall isotope ratios at these two locations; signature of dry spells were clearly identified from the study of isotopic composition in the growth bands of the gastropod specimens. The approach was also extended to older samples from historical archives from eastern Indian region (Kolkata, East India). Individual specimens belonging to the same species of gastropod, which were collected during the monsoon season of the year 1918 were used for reconstructing the seasonal pattern in monsoon rainfall over the region. The record of variation in the isotopic composition seen in the shell was compared with the rainfall data from Indian Metrological Division observatory at Kolkata station. The year 1918 was characterized as a major drought year and the signature of dry period was seen preserved in the specimen. The work under taken in this thesis will widen the scope of seasonality reconstruction using terrestrial shell fossils from palaeo records, which have been rarely investigated in paleoclimate studies from the perspective of understanding the seasonal precipitation variability.

Reconstruction studies of seasonal rainfall utilizing stable isotope based proxy approach suffer from the limitations of time resolutions. Conventional methods and archives limit the achievable resolution to annual scales. However, high resolution reconstruction (seasonal to sub-weekly scale) can be achieved in proxy records where growth rates are high enough to leave spatial signatures in an organically or inorganically deposited layer such as growth bands. In this study, aragonitic skeleton of the gastropod Lissachatina fulica (Bowdich, Giant African Land Snails) is investigated with an aim to achieve sub-weekly scale reconstruction of the Indian monsoon rainfall. These terrestrial gastropods are native of Africa and highly invasive. Their evolution in the geological time period dates back to the Pliocene and is presently distributed across the tropical belt. They exhibit a high growth rate in the presence of water and high relative humidity in the environment. As a result, they are ideally suited for the task of palaeo seasonality reconstruction. The isotopic patterns recorded in their growth bands reveal composition of environmental water at seasonal time scales. In vitro studies were carried out on L. fulica to estimate their growth rates and growth responses to changes in the physical conditions within the culture chamber. The Indian monsoon rainfall exhibits characteristic dry spells that are generally sandwiched between periods of active phases of high rainfall during the South West monsoon season. These dry spells are typically characterized by rainfall with low intensity. Isotope fingerprinting of the rain water at daily time resolution, covering the years of 2007-10 exhibited distinct isotopic ratios for the dry and wet spells. Dry spells were clearly demarcated in the record with isotopically enriched signature. In addition, the study indentified the role of three distinct moisture sources on δ18O of rain water at Bangalore, India. The variability in the oxygen isotopic composition of the Indian monsoon rainfall is predominantly controlled by this source moisture variability at inter annual time scales, while temperature and amount of rainfall tend to dominate the variability in the precipitation isotopes at seasonal and weekly scales. Simultaneous isotopic analyses of both rainwater and shell carbonates growth bands were undertaken to understand their relationship to aid in high resolution reconstruction. Carbonate found in the growth bands of the gastropods, which is precipitated under equilibrium condition from rainwater, preserves the signature of rainfall. This provides an opportunity to reconstruct rainfall parameters (i.e. amount and moisture sources) knowing the variability in shell carbonates. Stable isotopic ratios measured across the growth bands of live shell specimens collected from the southern and eastern Indian regions (Bangalore and Kolkata, respectively) were compared with the rainfall isotope ratios at these two locations; signature of dry spells were clearly identified from the study of isotopic composition in the growth bands of the gastropod specimens. The approach was also extended to older samples from historical archives from eastern Indian region (Kolkata, East India). Individual specimens belonging to the same species of gastropod, which were collected during the monsoon season of the year 1918 were used for reconstructing the seasonal pattern in monsoon rainfall over the region. The record of variation in the isotopic composition seen in the shell was compared with the rainfall data from Indian Metrological Division observatory at Kolkata station. The year 1918 was characterized as a major drought year and the signature of dry period was seen preserved in the specimen. The work under taken in this thesis will widen the scope of seasonality reconstruction using terrestrial shell fossils from palaeo records, which have been rarely investigated in paleoclimate studies from the perspective of understanding the seasonal precipitation variability.