Located 100 km west of Key West, Florida, Dry Tortugas National Park (DRTO) is a largely untouched subtropical marine ecosystem that serves as an important developmental habitat, nesting ground, and foraging area for several species of sea turtles, including green turtles. The Park supports a recovering population of green turtles comprised of resident juveniles, subadults, and adults of both sexes; nesting females include residents and migrating females that only return to nest. Stable isotope analysis has been applied widely to describe the trophic ecology of green turtles, from urbanized bays with significant anthropogenic input, to relatively pristine ecosystems with healthy populations at carrying capacity. However, there is a paucity of published literature about the trophic ecology of green turtles in DRTO. This study describes the trophic ecology occupied by two distinct size groups (61 green turtles < 60 cm (SCL) and 98 green turtles > 60 cm (SCL)). Flipper tissue and plasma were analyzed for stable isotopic composition of C and N. Flipper tissue values for δ15N (3.41‰ to 9.69‰) and δ13C (-22.43‰ to -5.38‰) fall within literature values for green turtles, and the wide range of values indicated they could potentially feed at multiple trophic levels. Understanding the trophic ecology of this population of green sea turtles is instrumental to effective management and habitat preservation strategies in DRTO.

No description available.

The present study focuses on the Emsian-Eifelian (Lower-Middle Devonian) carbonate sequences of the Prague Basin. The Třebotov Limestone (Daleje-Třebotov Formation) and the Choteč Limestone (Choteč Formation) and their equivalents represent the stratigraphic units studied. The main goal of this study is to characterize environmental changes, known as Basal Choteč event, that were described from the boundary interval of the Třebotov and Choteč Limestone. In order to do so, sedimentological (microfacies analysis), geochemical (δ13 Ccarb, δ18 Oapatite) and paleontological (taxonomy of conodonts) studies were carried out. Eight microfacies types of carbonate rocks were described and interpreted in this study. Beside that, massive accumulations of calcispheres, peloids, prasinophytes and occurrences of blue-green algae (Girvanella) were recorded especially in the Choteč Limestone. The multidisciplinary approach mentioned resulted in characterization of the sedimentary environment of the studied units as well as their development in time. The main result of the present study is the model of the Basal Choteč event. A hypothesis of enhanced nutrient load is suggested here as a triggering mechanism for intense micritization and peloid formation and prasinophyte blooms, which were together with greater...

Arctic soils contain a large fraction of our planets terrestrial carbon (C) pool. When tundra soils become warmer and permafrost thaws, non-native geoengineering earthworms can enter these soils and ingest organic matter accumulated over long timescales. Previous studies have found that earthworms increase mineralization rates of soil organic matter into carbon dioxide (CO2) when introduced. Yet, this initial mineralization boost seems transient with time and it has been hypothesized that earthworms stimulate the formation of persistent C forms. In this study, I investigated how non-native, geoengineering earthworms affected the relative proportions of seven carbon forms in the O and A1 horizon of tundra soil and if their effect induced a change in pH. I used Nuclear Magnetic Resonance (NMR) spectroscopy to understand what happens to soil carbon compounds in two different tundra vegetation types (heath and meadow), that had been subjected to earthworm treatment for three summers. I found that O-aromatic C increased from 7.22% ± 0.24 (mean ± stderr) in the meadow soil lacking earthworms to 8.98% ± 0.30 in the meadow exposed to earthworms, and that aromatic C increased from 8.71% ± 0.23 to 9.93% ± 0.25. In similar, the result suggested that alkyl C decreased in this vegetation type from 20.43% ± 0.38 to 18.70% ± 0.25 due to earthworm activities. I found no effect on the chemical properties in the heath. I conclude that geoengineering earthworms affect the two vegetation types differently and that earthworms seem to enhance the accumulation of recalcitrant aromatic C forms.

No description available.

Most of microorganisms are ubiquitously able to live in both planktonic and biofilm states, which can be applied to dissolve the energy and environmental issues (e.g., producing biofuels and purifying waste water), but can also lead to serious public health problems. To better harness microorganisms, plenty of studies have been implemented to investigate the metabolism of planktonic and/or biofilm cells via multi-omics approaches (e.g., transcriptomics and proteomics analysis). However, these approaches are limited to provide the direct description of intracellular metabolism (e.g., metabolic fluxes) of microorganisms. Therefore, in this study, I have applied computational modeling approaches (i.e., 13C assisted pathway and flux analysis, flux balance analysis, and machine learning) to both planktonic and biofilm cells for better understanding intracellular metabolisms and providing valuable biological insights. First, I have summarized recent advances in synergizing 13C assisted pathway and flux analysis and metabolic engineering. Second, I have applied 13C assisted pathway and flux analysis to investigate the intracellular metabolisms of planktonic and biofilm cells. Various biological insights have been elucidated, including the metabolic responses under mixed stresses in the planktonic states, the metabolic rewiring in homogenous and heterologous chemical biosynthesis, key pathways of biofilm cells for electricity generation, and mechanisms behind the electricity generation. Third, I have developed a novel platform (i.e., omFBA) to integrate multi-omics data with flux balance analysis for accurate prediction of biological insights (e.g., key flux ratios) of both planktonic and biofilm cells. Fourth, I have designed a computational tool (i.e., CRISTINES) for the advanced genome editing tool (i.e., CRISPR-dCas9 system) to facilitate the sequence designs of guide RNA for programmable control of metabolic fluxes. Lastly, I have also accomplished several outreaches in metabolic engineering. In summary, during my Ph.D. training, I have systematically applied computational modeling approaches to investigate the microbial metabolisms in both planktonic and biofilm states. The biological findings and computational tools can be utilized to guide the scientists and engineers to derive more productive microorganisms via metabolic engineering and synthetic biology. In the future, I will apply 13C assisted pathway analysis to investigate the metabolism of pathogenic biofilm cells for reducing their antibiotic resistance. / Ph. D.

La présence de plantes accélère la décomposition de la matière organique du sol (MOS) au travers de l’apport de composés riches en énergie (rhizodépôts et litières) stimulant les microorganismes ; un phénomène appelé « rhizosphere priming effect » (RPE). Une augmentation de la photosynthèse, activité pourvoyeuse d'énergie rhizodéposée, pourrait augmenter le RPE et l’offre du sol en nutriments. Récemment, le modèle SYMPHONY couplant activités photosynthétiques et microbiennes du sol suggère un ajustement de l'offre du sol en nutriments (delta minéralisation-immobilisation) à la demande des plantes. Cependant, le rôle clé de la photosynthèse sur cet ajustement offre-demande reste à étudier expérimentalement.L’objectif général de la thèse est d'étudier le rôle des interactions des activités photosynthétiques et microbiennes du sol dans les régulations des flux de carbone (C) et d'azote (N) des écosystèmes. Trois écosystèmes types ont été étudiés : la prairie, la monoculture de blé et un nouveau système de culture (NSC) associant blé et plantes pérennes de la prairie. Nous émettons l’hypothèse que les plantes pérennes, via une activité photosynthétique pourvoyant les microorganismes en énergie tout au long de l'année, sont essentielles à l'ajustement offre-demande en N. De nombreux défis techniques ont été relevés afin de construire une plateforme expérimentale de 40 mésocosmes sous éclairage et température naturels. Cette plateforme permet de coupler marquage 13C des plantes, mesures continues des échanges de CO2, du RPE, de la production végétale, du stockage de C du sol, le taux de minéralisation-immobilisation d'N et du lessivage d'N. Ce dispositif nous a permis de déterminer la contribution du RPE dans les flux de C des écosystèmes comprenant la production nette de l’écosystème (NEP), la production primaire brute (GPP) et la respiration de l’écosystème (RE) exprimées en g C m-2 24h-1. Nous avons montré une relation positive linéaire entre (1) RPE et GPP et (2) RPE et biomasse aérienne (AGB) (g C m-2). A partir de ces relations, le RPE peut être prédit en utilisant les équations suivantes : (...). Nous montrons un ajustement offre-demande de l’N au cours des saisons : une forte activité photosynthétique (printemps) est liée à un RPE et un delta minéralisation-immobilisation d’N élevés alors qu’une faible activité photosynthétique (automne) est liée à un RPE et un delta minéralisation-immobilisation d’N faibles. Cet ajustement était observé dans la prairie et dans le NSC mais pas en monoculture de blé. Logiquement, la lixiviation d’N était importante en monoculture de blé alors qu’elle était quasi nulle en prairie et dans le NSC. Après deux années de maintien des trois écosystèmes types, la production aérienne totale du NSC était équivalente à la prairie, tous deux étant supérieurs d’environ un facteur deux à la monoculture de blé. Ces résultats confirment l’importance des plantes pérennes dans la synchronisation offre-demande de l’N. L’ensemble de ces investigations souligne l’importance des activités des plantes et des processus rhizosphériques dans la régulation des cycles CN des écosystèmes. Ces régulations pourront être étudiées in situ et à l'échelle globale grâce aux proxys de ces processus rhizosphériques (RPE, ajustement offre-demande) déterminés dans la thèse. Des activités photosynthétiques et rhizosphériques tout au long de l'année sont essentielles à l'ajustement offre-demande en nutriments conduisant à une forte production primaire, à la fermeture des cycles des nutriments et au stockage de MOS. Ces découvertes offrent l'opportunité de construire de nouveaux systèmes de culture, à l'image de l’association blé-plantes pérennes étudiée, à hautes performances agro-environnementales. / The presence of plants accelerates the decomposition of soil organic matter (SOM) through the supply of energy-rich compounds (rhizodeposits and litter) stimulating microorganisms; a phenomenon called rhizosphere priming effect (RPE). An increase of photosynthesis, supplying soil with rhizodeposited energy, could increase the RPE and soil nutrients offer. Recently, the SYMPHONY model coupling photosynthesis and soil microbial activities suggested an adjustment of the soil nutrient offer (delta mineralization-immobilization) to plant demand. However, the key role of photosynthesis in this offer-demand adjustment needs to be investigated experimentally.The general objective of the thesis is to study the role of interactions between photosynthesis and soil microbial activities in the regulation of carbon (C) and nitrogen (N) fluxes of ecosystems. Three ecosystem types were studied: grassland, wheat monoculture and a new cropping system (NSC) where wheat and perennial grassland species were intercropped. We hypothesize that perennial species, through a continuous photosynthetic activity supplying microorganisms with energy over the year, are essential for offer-demand adjustment.Many technical challenges were overcame to build an experimental platform of 40 mesocosms under natural light and temperature. This platform allows to couple 13C labeling of plants, continuous CO2-exchange measurements, RPE, plant production, soil C storage, N mineralization-immobilization turnover and N leaching.This experimental platform allowed us to determine the contribution of RPE to C fluxes of ecosystems including net ecosystem production (NEP), gross primary production (GPP) and ecosystem respiration (ER) expressed in g C m-2 24h-1. We found positive linear relationships between (1) RPE and GPP and (2) RPE and aboveground biomass (AGB) (g C m-2). Using these relationships, the RPE can be predicted with the following equations: (...).We show an adjustment of soil N-offer to plant N-demand across seasons: a high photosynthetic activity (spring) is linked to high RPE and delta mineralization-immobilization of N whereas a low photosynthetic activity (autumn) is linked to low RPE and delta mineralization-immobilization of N. This adjustment was observed in grassland and NSC but not in wheat monoculture. Consistently, N leaching was high in wheat monoculture while it was almost null in grassland and NSC. After two years of establishment of the three ecosystems, the total aboveground production of the NSC was equivalent to the grassland, each being about twice as high as the wheat monoculture. These results confirm the importance of perennial species in the offer-demand adjustment of N.Our findings underline the importance of plant activities and rhizosphere processes in the regulation of ecosystems C N cycles. Using the proxies of rhizosphere processes (RPE, offer-demand adjustment) provided in the thesis, further studies could investigate these regulations in situ and at the global scale. The presence of photosynthetic and rhizospheric activities over the year are essential for offer-demand adjustment of nutrients leading to high primary production, closing nutrient cycles and SOM storage. These findings offer the opportunity to build new cropping systems such as the wheat-perennial species studied, with high agro-environmental performances.

Der Klimawandel bedroht Ökosysteme auf der ganzen Welt. Besonders der Anstieg in Länge, Intensität und Häufigkeit von Dürren kann bedeutenden Einfluss auf den globalen Kohlenstoffkreislauf haben. Die Frage, ob Pflanzen und Mikroorganismen anfällig gegenüber ökologischem Stress wie Dürren sind, wurde bereits in vielen Studien für verschiedene Ökosysteme und mit verschiedenen Ansätzen untersucht, aber Analysen von Dürreauswirkungen, die ober- und unterirdische Interaktionen von Pflanzen und Mikroorganismen mit einbeziehen, sind eher selten. Deshalb wird in der vorliegenden Studie die Frage erörtert, wie Trockenheit und/oder Hitze die Interaktionen von Pflanzen und Mikroorganismen in Bezug auf ihre Kohlenstoff-Verbindung beeinflussen. Dies dient zur Bestimmung der Stärke der Pflanze-Mikroorganismen-Kohlenstoff-Verbindung, wenn das Ökosystem an seine Grenzen gebracht wird. Der Fokus liegt deshalb auf durch Trockenstress und Hitze hervorgerufenen Veränderungen in der ober-unterirdischen Kohlenstoff-Dynamik in zwei vom Klimawandel bedrohten Ökosystemen. Es wurde untersucht, wie extreme Klimaereignisse, deren Häufigkeit in Zukunft weiter ansteigen soll, die Kohlenstoff-Verbindung zwischen Pflanzen und Mikroorganismen beeinflusst und wie mikrobielle Gemeinschaften unter diesen Umständen reagieren, um die Resistenz und Reaktionsmechanismen von Ökosystemen im zukünftigen Klimawandel besser vorhersagen zu können. In Kapitel 4 wurde ein Buchenwaldunterholz-Ökosystem untersucht. Buchenwaldmonolithen wurden einem extremen Klimaereignis (Trockenheit und/oder Hitze) ausgesetzt. Die Stärke der Pflanze-Mikroorganismen-Kohlenstoff-Verbindung und Veränderungen in der mikrobiellen Gemeinschaftsstruktur und -aktivität wurden mithilfe von stabilen 13C Isotopenmethoden und Ansätzen auf molekularer Basis, wie 16S rRNA- und Phospholipid-Analysen, bestimmt. In Kapitel 5 wurde ein kleines aquatisches Ökosystems untersucht. Zwei emerse aquatische Makrophyten, Phragmites australis und Typha latifolia, wurden in einem Mesokosmos-Experiment mit Sediment aus einem Soll einer einmonatigen Dürre ausgesetzt. Mithilfe einer 13CO2 Pulsmarkierung, sowie PLFA- und nicht-strukturbildenden Kohlenhydrat-Analysen wurde Kohlenstoff von den Blättern in die Wurzeln bis ins Sediment verfolgt, wo er teilweise in mikrobielle Phospholipide eingebaut wird. Diese Studie hat gezeigt, dass die zwei untersuchten Ökosysteme Trockenstress und Hitze relativ gut widerstehen können, zumindest kurzfristig, und dass das Kohlenstoff-Kontinuum, beziehungsweise die Verbindung zwischen ober- und unterirdischen Gemeinschaften, auch unter starkem Stress intakt bleibt. Zusammenfassend scheint es, dass Ökosysteme stark von einem funktionierenden Pflanze-Boden/Sediment-Mikroorganismen Kohlenstoff-Kontinuum abhängen und versuchen, es auch unter starkem Stress zu erhalten, was möglicherweise dazu beiträgt, dem Anstieg von extremen Dürreperioden aufgrund des Klimawandels besser zu widerstehen. / Climate change is threatening ecosystems around the world. Especially the increase in duration, intensity, and frequency of droughts can have a considerable impact on the global carbon cycle. The question whether plants and microbes are susceptible to environmental stress like drought has been assessed in many studies for different ecosystem types and by using numerous approaches, but research on drought effects that includes above- and belowground interactions is rather scarce. Therefore, the present study assesses the question of how drought and/or heat influence the interactions of plants and microbes, especially the carbon coupling, in order to determine the strength of plant-microbe carbon linkages when an ecosystem is pushed to its limits. The focus of this study thus lies on changes in aboveground-belowground carbon dynamics and the subsequent effects on the soil microbial community under drought and/or heat stress in two climate-threatened ecosystems. It was evaluated how extreme climate events, that are predicted to be more frequent in the near future, affect the carbon coupling between plants and microorganisms and how microbial communities respond under these circumstances, in order to be able to better predict ecosystem resistance and response mechanisms under future climate change. In chapter 4 a beech forest understory ecosystem was investigated. An extreme climate event (drought and/or heat) was imposed on beech forest monoliths and the strength of the plant-microbe carbon linkages and changes in the microbial community structure and activity were determined by using stable 13C isotope techniques and molecular-based approaches like 16S rRNA and microbial phospholipid-derived fatty acid (PLFA) analysis. In chapter 5 a small aquatic ecosystems was investigated. Two emergent aquatic macrophytes, Phragmites australis and Typha latifolia, were grown on kettle hole sediment and then exposed to a month-long summer drought in a mesocosm experiment. By conducting a 13CO2 pulse labeling as well as PLFA and non-structural carbohydrate analyses, the fate of carbon was traced from the plant leaves to the roots and into the sediment, where some of the recently assimilated carbon is incorporated into microbial PLFAs. Overall, this study showed that the two investigated ecosystems can endure environmental stress like heat and drought relatively well, at least in the short-term, and that the carbon continuum, or the linkage between above- and belowground communities, remained intact even under severe stress. In conclusion, it seems that ecosystems strongly depend on and try to maintain a functional plant-soil/sediment microorganism carbon continuum under drought, which might help to withstand the increase in extreme drought events under future climate change.

In der vorliegenden Arbeit wurden die Einflüsse der landwirtschaftlichen Nutzung auf die Struktur und Biomasse von Nematoden entlang eines Tiefengradientens und innerhalb zweier Vegetationsperioden an einem Ackerstandort untersucht. Die Freilandanalyse der Nematodengemeinschaft wies auf ein mit Nährstoffen angereichertes und gestörtes Ökosystem, mit einer geringen Diversität, hin. Entlang des Tiefengradienten bildeten die Nematoden Metacommunities, welche Umweltgegebenheiten wie Nahrungsquellen und abiotischen Faktoren widerspiegeln. Signifikant höhere Biomassen wurden unter Weizen im Vergleich zu Mais als Ackerfrucht beobachtet. Die Streuapplikation induzierte einen „bottom-up“ Effekt mit größeren Biomassen in den niedrigen als in den höheren trophischen Stufen. Die Nematoden Biomassen sowie die faunistischen Indizes (Channel Index, Enrichment Index) zeigten, dass der Kohlenstofffluss im Bakterienkanal des Bodens dominierte. Allerdings deckte das 13C Pulse-Labelling Experiment im Feld auf, dass der Kohlenstofffluss durch die Pilzgemeinschaft sowie die pilzfressenden Nematoden wesentlich höhere Umsatzraten aufweist. In einem 14C-Laborexperiment wurde ein vollständiges Budget des Flusses von wurzelbürtigem Kohlenstoff in das Nahrungsnetz der Nematoden bestimmt. Hierbei wiesen die pflanzenparasitären Nematoden die höchsten 14C-Gehalte innerhalb weniger Tage auf, da sie direkt an den Wurzeln fressen und über die Herbivorenkette den Nährstoffzyklus im Boden eröffnen. / The present research considered the effects of agricultural management practice on the nematode community structure and biomass in three different depths and two successive vegetation periods at an arable field site. The resource quality was manipulated by crop plant and organic amendment, to investigate the major soil carbon pathways based on roots, bacteria and fungi. The nematode community analysis pointed to a highly enriched and disturbed ecosystem with low biodiversity. Along the depth gradient the nematodes formed distinct metacommunities, reflecting resource availability and abiotic environmental factors. Wheat supported significantly greater nematode biomass than maize. The litter amendment induced bottom-up effects, with greater biomass allocation at lower than at higher trophic levels. The biomass of nematode families as well as faunal indices (Channel Index, Enrichment Index) revealed a predominance of the bacterial carbon channel in the arable soil. A 13C pulse-labelling experiment investigating the flux of root- derived C into the soil food web revealed high turnover rates in the fungal carbon pathway. This was evident for soil fungi as well as for fungal-feeding nematodes and contradicts general assumptions of a more active bacterial pathway in arable soils. A laboratory experiment with 14C isotope was used to compile a complete budget for the root-derived carbon in the nematode food web. Here plant-feeding nematodes, which feed on living plant roots, thereby opening the root C cycling into the food web, showed highest amounts of 14C allocation within a few days.

Les produits issus de la biomasse végétale connaissent depuis quelques années un succès grandissant dans de nombreuses industries (aromathérapie, cosmétique, parfums, etc.). L’objectif de notre étude était, d’une part de contribuer au développement des méthodes d’identification et de quantification des constituants des mélanges naturels par RMN 13C et RMN 1H (par exemple le squalène dans l’huile d’olive), et d’autre part, de contribuer à la caractérisation chimique de deux conifères introduits en Corse, le pin d’Alep (huile essentielle) et le cèdre de l’Atlas (huile essentielle, huile pyrolytique et résine).La première partie concerne la quantification du squalène présent dans l’huile d’olive. En effet, ce triterpène linéaire participe à la stabilité oxydative de l’huile d’olive et joue un rôle important dans la réduction des risques de certains cancers. Il s’agissait de mettre au point un protocole expérimental basé sur la RMN 1H ou 13C en utilisant un appareil de routine (9,4 Tesla). La quantification par RMN 13C s’est avérée fiable et elle a été appliquée à la quantification du squalène dans 25 échantillons d’huile d’olive de Corse.La seconde partie de nos travaux concerne la caractérisation chimique de l’huile essentielle de pin d’Alep introduit dans trois stations de Corse (Capo di Feno, Saleccia et Tre Padule de Suartone). L’analyse détaillée de l’huile essentielle de cônes, par combinaison des techniques chromatographiques et spectroscopiques, a permis d’identifier 48 composés. La composition chimique est largement dominée par les monoterpènes (Alpha-pinène et myrcène) et un sesquiterpène oléfinique ((E)-Béta-caryophyllène). La RMN 13C a permis d’identifier divers diterpènes, dont le 8,12-époxy-14-labdèn-13-ol. Ce composé est décrit pour la première fois dans l’huile essentielle de pin d’Alep. L’analyse de 15 échantillons d’huile essentielle de cônes a mis en évidence trois types de compositions : Alpha-pinène ; myrcène ; Alpha-pinène/myrcène. Enfin, l’analyse de 47 échantillons d’huile essentielle d’aiguilles, associée à un traitement statistique des données (ACP, AFD), a permis de mettre en évidence une variabilité chimique intraspécifique. Ainsi, les échantillons se répartissent en trois groupes selon leur teneur en (E)-Béta-caryophyllène (groupe I), en E-Béta-caryophyllène/Alpha-pinène/myrcène (groupe II) et en myrcène (groupe III).La dernière partie a été consacrée à l’étude de Cedrus atlantica. L’analyse détaillée d’une huile essentielle commerciale (du Maroc) a permis d’identifier 20 constituants, les composés majoritaires sont les Alpha-, Béta- et Gamma-himachalène. Par ailleurs, 7 composés absents de notre bibliothèque de données spectrales ont été identifiés par RMN 13C. Les compositions chimiques des huiles pyrolytiques artisanales du Maroc sont également dominées par les himachalènes et la (E)-Alpha-atlantone. Enfin, nous avons réalisé l’analyse qualitative et quantitative par RMN 13C, sans séparation préalable, de 28 échantillons de résine de C. atlantica récoltés dans les 5 forêts de Corse référencées par l’ONF (Bavella, Bonifato, Ospedale, Pineta et Vizzavona). A côté des acides résiniques, nous avons également identifié 3 lignanes (pinorésinol, laricirésinol et 9-acétate de laricirésinol). Pour l’ensemble de ces composés, nous avons mis en évidence trois types chimiques. Enfin, nous avons mis au point et validé un protocole expérimental de quantification des lignanes par RMN 1H. / Natural products isolated from plants acquired, in recent years, a growing success in many industries (aromatherapy, cosmetic, perfumes). The objective of our study was to contribute, on the one hand, to the development of methods involving 13C and 1H NMR for the identification and quantification of the components of natural mixtures, and on the other hand, to the chemical characterization of two conifers brought to Corsica, Aleppo pine (essential oil) and atlas cedar (essential oil, pyrolysis oil and resins).The first part concerned the quantification of squalene present in olive oil. Indeed, linear triterpene participated in the oxidative stability of olive oil and play an important role by decreasing some kind of cancers risks. It’s deal with to elaborate an experimental part based on NMR 1H and 13C by using routine apparatus (9.4 Tesla). Quantification by NMR 13C is reliable and have been applied to squalene quantification in 25 samples of Corsican olive oil.The second part of our work concerned the chemical characterization of the essential oil of Aleppo pine brought to Corsica in three different stations (Capo di Feno, Saleccia and Tre Padule de Suartone). A detailed analysis of cone essential oil, using the combination of chromatographic and spectroscopic techniques, leads to the identification of 48 compounds. Chemical composition is extensively dominated by monoterpens (Alpha-pinene and myrcene) and one olefinic sesquiterpen ((E)-Béta-caryophyllene). 13C NMR allowed to the identification of various diterpens, particularly the 8,12-epoxy-14-labden-13-ol. This compound is described for the first time in aleppo pine essential oil. Fifteen samples of cone essential oil were analysed allowing differentiating three kinds of compositions: Alpha-pinene; myrcene; Alpha-pinene/myrcene. Finally, analysis of 47 samples of needles essential oil, associated with statistical treatment of the results (PCA and PFA), suggested the occurrence of an intraspecific chemical variability. Samples are divided into three groups, based on their high contents in (E)-Béta-caryophyllene (groupe I), in (E)-Béta-caryophyllene/Alpha-pinene/myrcene (groupe II) and in myrcene (groupe III).The last part concerned the study of Cedrus atlantica. A detailed analysis of commercial essential oil leads to the identification of 20 constituents. Main compounds are Alpha-, Béta- and Gamma-himachalene. Moreover, seven compounds, not yet referenced in our home-made NMR spectral data library, were identified by NMR 13C. Chemical compositions of handwork pyrolysis oils from Morocco were also dominated by the himachalene’s and (E)--atlantone. Qualitative and quantitative analysis of 28 samples of Cedrus atlantica resins, obtained from the five Corsican forests referenced by the Office National des Forêts of Corsica (Bavella, Bonifato, Ospedale, Pineta and Vizzavona) have been done, without any step of chromatography. Beside resinic acids, we have been identified three lignans (pinoresinol, lariciresinol and lariciresinol-9-acetate). Qualitative and quantitative analysis of these compounds, leads to the occurrence of three types of chemical composition. Finally, we have developed and validated a method for quantification of lignans by 1H NMR.