De nombreux organismes marins précipitent des squelettes en calcite magnésienne. Depuis près d’un siècle, il est connu que les concentrations en magnésium de ces squelettes sont influencées par les conditions environnementales, telle la température, régnant au moment de leur dépôt. Dans le contexte actuel de changement climatique, cette propriété a promu l’usage de plusieurs taxons en tant qu’archive naturelle des conditions environnementales du passé. Cependant, les squelettes d’espèces sympatriques, voire d’individus de la même espèce, peuvent présenter des concentrations en magnésium très différentes, attestant de l’influence de facteurs biologiques sur la détermination de la concentration squelettique en cet élément. Une parfaite compréhension des mécanismes d’incorporation du magnésium dans les squelettes est donc requise pour valider l’usage de ce paléotraceur. De plus, la solubilité des calcites augmentant avec leur concentration en magnésium, l’incorporation de cet élément conditionne en partie la stabilité des squelettes calcitiques dans un océan en cours d’acidification.<p>Le présent travail contribue à l’étude des différents facteurs, tant environnementaux que physiologiques et minéralogiques, susceptibles d’affecter l’incorporation du magnésium dans les squelettes en calcite de trois taxons présentant des concentrations en cet élément particulièrement élevées, une éponge hypercalcifiée, Petrobiona massiliana, et deux échinodermes, Paracentrotus lividus et Asterias rubens.<p>Dans une première partie, les effets de plusieurs facteurs environnementaux ont été étudiés, en milieu naturel dans le cas de l’éponge, étant donné son incapacité à survivre en aquarium, et en conditions contrôlées d’aquarium dans le cas des deux échinodermes. Une influence environnementale prépondérante de la température sur la concentration en magnésium squelettique a été mise en évidence dans les 3 modèles biologiques étudiés. Une fois les facteurs génétiques (espèce) et structurels (élément squelettique) fixés, une relation positive liant la température à la concentration en magnésium squelettique a été caractérisée en milieu naturel chez l’éponge hypercalcifiée P. massiliana et en conditions contrôlées chez l’oursin P. lividus. Chez ce dernier, cette relation, non linéaire, se stabilise aux plus hautes températures envisagées, probablement suite à la saturation d’un processus biologique intervenant dans l’incorporation de cet élément. La salinité, un autre facteur environnemental majeur en milieu marin, influence elle aussi positivement la concentration en magnésium dans le squelette de l’étoile de mer A. rubens. A nouveau, il est proposé que cette influence de l’environnement soit modulée par un processus biologique: chez les échinodermes, la concentration en magnésium, contrairement à celle du calcium, n’est pas régulée dans le liquide coelomique. Elle est donc directement influencée par la salinité, et affecte probablement la concentration en cet élément dans le squelette formé. La diffusion depuis l’eau de mer jusqu’au site de calcification par l’intermédiaire des fluides internes a en effet été suggérée sur base du fait que le rapport Mg/Ca de l’eau de mer influence celui des squelettes calcaires<p>Une fois l’influence, directe ou indirecte, des facteurs environnementaux exclue, 44% de la variabilité du rapport Mg/Ca du squelette des échinodermes restent à expliquer. Les expériences de croissance d’échinodermes réalisées en conditions contrôlées indiquent que ce rapport est indépendant de la vitesse de croissance dans ce groupe, contrairement aux hypothèses émises dans la littérature.<p>Dans la seconde partie, la modulation des facteurs minéralogiques par les facteurs biologiques a été investiguée. Pour ce faire, d’une part, les interactions entre rapport Mg/Ca en solution et matrice organique de minéralisation ont été étudiées dans un modèle in vitro. D’autre part, les relations entre soufre et magnésium dans le squelette ont été décryptées.<p>Le rapport Mg/Ca de la solution de précipitation a une influence prépondérante sur la concentration en magnésium du carbonate de calcium précipité in vitro, attestant de l’importance de la régulation de la composition du fluide de calcification et des mécanismes de transport la contrôlant. Deux mécanismes biologiques complémentaires permettent de favoriser l’incorporation, dans les calcites biogéniques, de quantités de magnésium largement supérieures à celles observées dans les calcites inorganiques, et ce, malgré la forte hydratation de ce cation :l’intervention d’agents chélateurs du magnésium et le passage par une phase de carbonate de calcium amorphe (CCA). Les molécules de la matrice organique de minéralisation jouent entre autres le rôle de chélateur du magnésium, réduisant son état d’hydratation et facilitant ainsi son incorporation dans le minéral. Un rôle similaire a été suggéré pour les sulfates en solution, au vu de la corrélation observée dans ce travail entre les rapports Mg/Ca et S/Ca dans la phase minérale des calcites biogéniques étudiées. La matrice organique affecte elle aussi la concentration en magnésium dans le cristal, probablement via la stabilisation de la phase de CCA nécessaire à l’incorporation de concentrations élevées de cet élément: ainsi, les macromolécules de la matrice organique du test d’oursin induisent in vitro la formation de calcites plus riches en magnésium que celles formées en présence de matrice de piquant, un résultat concordant avec le fait que, in vivo, le test contient des concentrations en magnésium plus élevées que les piquants.<p>Cette thèse de doctorat a donc soulevé l’importance des effets biologiques dans la détermination du rapport Mg/Ca dans les calcites biogéniques. Les résultats obtenus montrent que le décryptage des mécanismes impliqués dans l’incorporation du magnésium se doit de considérer la phase amorphe transitoire qui précède la cristallisation. Des effets environnementaux affectent eux aussi la concentration squelettique en magnésium, mais nos résultats suggèrent qu’ils agissent au travers d’une modulation des effets biologiques, et non par une influence thermodynamique directe. Cette hypothèse, si elle est confirmée, impose la plus grande prudence lors de l’utilisation des squelettes en calcite en tant que paléotraceurs.<p><p><p>SUMMARY<p>The magnesium concentration in calcite skeletons produced by marine invertebrates is known to be dependent on several environmental parameters, including temperature, salinity and seawater Mg/Ca ratio. This property prompted the use of this concentration as a proxy of the considered parameters. However, skeletal magnesium contents in sympatric species and even in individuals of the same species may be rather different. These inter and intra-individual variabilities indicate that biological factors also affect magnesium incorporation into biogenic calcites. Magnesium incorporation mechanisms are still unknown in calcifying invertebrates, a fact that questions the validity of this element as a paleoproxy. Moreover, higher magnesium contents increase calcite solubility and could therefore worsen the case of calcifying organisms facing ocean acidification linked to global change.<p>The present thesis is a contribution to the study of the environmental, biological and mineralogical factors affecting magnesium incorporation into the calcitic skeletons of 3 taxa, i.e. one hypercalcified sponge, Petrobiona massiliana, and two echinoderms, Paracentrotus lividus and Asterias rubens.<p>The first part of this work was dedicated to the study of several environmental factors affecting the magnesium concentration in the calcite skeleton of the 3 studied organisms. Consequently to its low survival in aquarium, the sponge was studied using field specimens collected along an environmental gradient. Echinoderms were grown in controlled conditions in aquarium. Once the genetic (species) and structural (skeletal element) factors were fixed, skeletal magnesium concentration was positively related to temperature in the 3 studied species. The Mg/Ca ratio of the test of aquarium-grown P. lividus increased with temperature until a plateau which was probably due to the saturation of a biological process involved in magnesium incorporation. A positive effect of salinity, an other major environmental parameter, on skeletal Mg/Ca was demonstrated in aquarium-grown A. rubens. This influence can also be linked to a biological process: contrary to magnesium, calcium concentration is controlled in the coelomic fluid, from which ions probably diffuse through the living tissues to the calcification site. Thus, the observed positive relation can be explained by the fact that a salinity increase raises the coelomic Mg/Ca ratio, which, according to previous studies, affected the Mg/Ca ratio of the precipitated skeleton.<p>In addition to the reported environmental influences, 44% of the skeletal Mg/Ca ratio variation remained unexplained in echinoderms. The absence of growth rate effect on magnesium incorporation into the echinoderm skeleton was demonstrated in aquarium experiments, contrary to previous literature statements. Other biological factors must therefore affect the incorporation of this element.<p>In the second part of this work, the modulation of mineralogical factors by biological factors was investigated. The interaction between Mg/Ca ratio in the precipitation solution and organic matrix was studied in an in vitro precipitation experiment. In addition, the relation between skeletal Mg/Ca and S/Ca ratios was investigated.<p>A major influence of the precipitation solution Mg/Ca ratio on the magnesium concentration of in vitro precipitated minerals was evidenced, highlighting the importance of transport mechanisms which determine the composition of the calcifying solution. The<p>higher magnesium concentrations presented in some biogenic calcites in comparison to inorganic calcites can be attributed to the action of chelating molecules and to the transition trough an amorphous phase. The strong tendency of magnesium towards hydration can be overcome by the involvement of molecules that can function as magnesium chelators and, therefore, favour the formation of calcite with a high magnesium content. Organic matrix macromolecules have been suggested to proceed as magnesium chelators, reducing the hydration of this ion and facilitating its incorporation into calcite. A similar function was suggested for sulphates that were measured in the echinoderm skeleton. This would explain the positive correlation between skeletal Mg/Ca and S/Ca ratios observed in the studied species. Organic matrix macromolecules also increased the magnesium concentration of minerals precipitated in vitro, probably stabilizing the transient phase of amorphous calcium carbonate, which can incorporate high quantities of magnesium in its structure. The enhancement of magnesium incorporation was more pronounced with the organic matrix extracted from the test of sea urchin than with that extracted from their spines. This result was in agreement with the in vivo skeletal Mg/Ca ratios in P. lividus skeleton that were higher in the test than in the spines.<p>This study demonstrated the importance of the biological effects in the determination of Mg/Ca ratios in biogenic calcites. According to the suggested hypotheses, the understanding of mechanisms involved in magnesium incorporation should take the transient amorphous phase into account. Magnesium concentration in biogenic calcite was also affected by environmental parameters, but these influences could proceed through the indirect modulation of biological rather than a direct thermodynamic control. This hypothesis, if proved correct, would have deep implications for the use of magnesium in calcite skeletons as a paleoproxy. / Doctorat en Sciences / info:eu-repo/semantics/nonPublished

Coral reefs ecosystems are deteriorating and facing dramatic changes. These changes suggest a shift in dominance from corals to other benthic organisms. Particularly in the Caribbean Sea, with corals dying, sponges have become the leading habitat-forming benthic animals. However, little is known about what life-history traits allow organisms to proliferate in a marine system that is undergoing change. Thus, the objective of this dissertation was to try to understand the current increase of encrusting excavating sponges on deteriorating Caribbean coral reefs through the study of reproduction, recruitment and dispersal potential of the widely distributed and currently expanding species, Cliona delitrix. Different methodological approaches were used, such as histology, electron microscopy, quantification of sponges in the field, genetics, and mathematical modeling. Results are presented in four different chapters. It was found that Cliona delitrix has an extended reproductive cycle in Florida, USA, from April - May to around November - December depending on a >25°C sea-water temperature threshold. C. delitrix gametogenesis is asynchronous and it has multiple spawning events. C. delitrix is recruiting abundantly on Caribbean coral reefs, preferentially on recent coral mortality than on old coral mortality. The increase in C. delitrix and other excavating sponges can be explained by the repeated spawning and by the coincidence in time and space of larval production with the availability of new dead coral, which tend to overlap during the warmest months of the year. Eggs or larvae of C. delitrix appear to survive enough to be transported by currents over larger distances. It was found that dispersal ranges for Cliona delitrix may reach as far as ~315 km in the Florida reef track, and over ~971 km in the South Caribbean Sea, between Belize and Panama. Thus, reproduction, dispersal, and recruitment patterns of C. delitrix along with oceanographic currents, and eddies that form at different periods of time, are sustaining the spread of this sponge on coral reefs. According to mathematical models carried out, C. delitrix increase on reefs fluctuates depending of coral mortality events and available space on old dead coral (colonized by algae and other invertebrates). However, under temperature anomalies, these sponges will 2 tend to increase and take over the reef system only if heat stress and coral mortality is moderate. Under massive mortality events both corals and sponges will tend to decline, although sponges at a slower rate than corals. In general, coral excavating sponges have been favored by coral mortality, especially during past few decades. However as bioeroders, their success is also limited by the success of calcifying corals. In a reef management context and based on this dissertation’s findings, it is suggested that excavating sponges, and especially Cliona delitrix, should be more formally included in reef monitoring programs. Their increase can be used to track coral mortality events on reefs (past and future), and also can be used as another major bioindicator of health on coral reefs.

Low light intensity habitats harbor unique sciophilous benthic communities and are a source of novel and unique sponge fauna. However, the community structure of these habitats is poorly studied to date. Thus, this study attempts to understand the composition and structure of sciophilous sponge populations in southeast Florida. Fifty limestone plates were placed on a shallow reef in Fort Lauderdale for two years (2010-2012). To identify the sponge community and their patterns over time, all plates were photographed at the end of each year. Then, samples were taken from each of the live sponge specimens observed on the plates and processed in the laboratory for taxonomical identification. A total of 45 different sponge species were found, the majority corresponding to the Poecilosclerida Order. Eighteen were identified to species level, twenty-two to genus, and five were undetermined. Eight sponges constitute new records to Florida, and four are potentially new species. The most dominant species include Oscarella sp.1, Dysidea etheria, Mycale sp.1, Halisarca caerula and Tedania ignis. Species richness significant varied among years, and species cover among sectors (inner and outer reef). However, sponge assemblages were similar between years with slightly variation between sectors. This study found a diverse and complex composition and structure of sponges that is quite distinct from the sponge assemblages on the open reefs. A guide of the biodiversity of cryptic sponge species was created to facilitate further studies in low light intensity habitats.

Les premières étapes de l’évolution animale restent obscures mais peuvent toutefois être appréhendées par l’étude comparative du développement des animaux basaux comme les éponges, les cnidaires ou les cténophores. Une des innovations majeures dans l’évolution des formes animales est l’apparition de l’épithélium, classiquement considérée comme une synapomorphie des eumétazoaires. Les homoscléromorphes sont les seules éponges à partager avec Eumetazoa la présence d’un véritable épithélium avec notamment une membrane basale contenant du collagène de type IV. Dans ce clade, la recherche des mécanismes épithéliaux sous-tendant le développement a pour enjeu la meilleure compréhension de leur origine et de leur importance dans l’évolution animale. Le travail de cette thèse a consisté à caractériser chez Oscarella lobularis des outils moléculaires responsables des morphogenèses épithéliales. Trois d’entre eux ont été étudiés chez l’adulte. Le premier, la voie WNT canonique, est capable d’induire l’invagination de l’épithélium externe de l’éponge, ce qui n’est pas sans rappeler ce même rôle dans d’autres contextes épithéliaux d’eumétazoaires. Le deuxième est la voie WNT non canonique ou « voie PCP », qui, quand elle est bloquée, empêche l’invagination initiée par la voie canonique. Enfin, le troisième outil est un membre de la famille des gènes à boîte T, OlTbx qui s’exprime spécifiquement dans l’épithélium après l’invagination sus-mentionnée. Cette expression rappelle des expressions d’autres gènes Tbx dans le feuillet endomésodermique invaginé lors de la gastrulation des eumétazoaires. L’invagination semble utiliser une partie d’un même programme génétique dans la gastrula des Eumetazoa et dans l’adulte des Homoscleromorpha. Mes résultats ouvrent des perspectives intéressantes concernant l’éventuelle reconnaissance d’un stade gastrula chez les éponges, point de discorde de la zoologie classique. / The first steps of animal evolution remain obscure but, nevertheless can be better understood by comparative studies of the most basally branching animals, such as sponges, cnidarians and ctenophores. Epithelium is one of the major innovations in the evolution of animal forms and is generally considered as one of the synapomorphies of Eumetazoa. The homoscleromorphs are the only sponges, with Eumetazoa, to have a true epithelium with a basal membrane containing type IV collagen. In this clade, the investigation of epithelial processes underlying development would give insights into their origin and their importance in animal evolution. The aim of my work was to characterize molecular tools involved in epithelial morphogenesis in Oscarella lobularis. I was able to characterize three of those molecular tools. The first one is the canonical WNT pathway inducing invagination of the external epithelium of the sponge, reminiscent of the same function in other epithelial contexts in Eumetazoa. The second one is the non-canonical WNT pathway or “PCP pathway” which blocks invagination when it is inhibited. The third one is a member of the T-box genes family, OlTbx, specifically expressed in the epithelial layer formed by the above-mentioned invagination. Similarly, other Tbx genes are expressed in the endomesodermal layer during eumetazoan gastrulation. Invagination processes involved in both eumetazoan gastrula and homoscleromorph adult tissue seem to share a part (WNT/Tbx) of a common genetical program. My results provide new investigation prospects, in order to answer the difficult question of the origin of gastrulation in sponges.

Globally, methicillin resistant Staphylococcus aureus (MRSA) has become increasingly difficult to manage in the clinic and new antibiotics are required. The structure activity relationship (SAR) study presented in this thesis forms part of an international collaborative effort to identify potent and selective inhibitors of an MRSA pyruvate kinase (PK) enzyme target. In earlier work the known marine natural product bromodeoxytopsentin (1.6), isolated from a South African marine sponge Topsentia pachastrelloides, exhibited selective and significant inhibition of MRSA PK (IC₅₀ 60 nM). Accordingly bromodeoxytopsentin provided the initial chemical scaffold around which our SAR study was developed. Following a comprehensive introduction, providing the necessary background to the research described in subsequent Chapters, this thesis has been divided into three major parts. Part one (Chapter 2) documents the synthesis of two natural imidazole containing topsentin analogues 1.40, 1.46, five new synthetic analogues 1.58—1.61, 2.104. In the process we developed a new method for the synthesis of topsentin derivatives via selenium dioxide mediated oxidation of N-Boc protected 3-acetylindoles to yield glyoxal intermediates which were subsequently cyclized and deprotected to yield the desired products. Interestingly we were able to demonstrate a delicate relationship between the relative equivalents of selenium dioxide and water used during the oxidation step, careful manipulation of which was required to prevent the uncontrolled formation of side products. Synthetic compounds 1.40, 1.46, 1.58—1.61 were found to be potent inhibitors of MRSA PK (IC₅₀ 238, 2.1, 23, 1.4, 6.3 and 3.2 nM respectively) with 1000-10000 fold selectivity for MRSA PK over four human orthologs. In the second part of this thesis (Chapter 3) we report the successful synthesis of a cohort of previously unknown thiazole containing bisindole topsentin analogues 1.62—1.68 via a Hantzsch thiazole synthesis. Bioassay results revealed that these compounds were only moderate inhibitors of MRSA PK (IC₅₀ 5.1—20 μM) which suggested that inhibitory activity was significantly reduced upon substitution of the central imidazole ring of topsentin type analogues with a thiazole type ring. In addition in Chapter 3 we describe unsuccessful attempts to regiospecifically synthesize oxazole and imidazole topsentin analogues through a similar Hantzsch method. As a consequence of our efforts in this regard we investigated three key reactions in depth, namely the synthesis of 2.2, 3.38, 3.40, 3.41 via α-bromination of 3-acetylindole and the synthesis of indolyl-3-carbonylnitriles 2.13, 3.45—3.47 and α-oxo-1H-indole-3-thioacetamides 3.48—3.51. The investigation of the latter led to the isolation and elucidation of two anomalous N,N-dimethyl-1H-indole-3-carboxamides 3.52 and 3.53. Finally the third part of this thesis (Chapter 4) deals with in silico assessment of the binding of both the imidazole and thiazole containing bisindole alkaloids to the MRSA PK protein which initially guided our SAR studies. In this chapter we reveal that there appears to be no correlation between in silico binding predictions and in vitro MRSA PK inhibitory bioassay data. Superficially it seems that binding energy as determined by the docking program used for these studies correlated with the size of the indole substituents and did not reflect IC₅₀ MRSA PK inhibitory data. Although this led us to computationally explore possible alternative binding sites no clear alternative has been identified.

Le devenir des radionucléides naturels et anthropogéniques dans l’environnement demeure une préoccupation majeure des sociétés modernes nucléarisées. Parmi les compartiments environnementaux possiblement impactés, l’hydrosphère est ubiquitaire et peut transporter des composés ou éléments sur de très longues distances. L’évènement récent de Fukushima a démontré que le milieu marin pouvait être également directement impacté ce qui amène à des questionnements tant scientifiques que sociétaux. De nombreuses études ont déjà montré que les radionucléides présents dans l’eau de mer peuvent être fortement accumulés par les organismes marins mais pour autant leur spéciation est inconnue. Or cette connaissance est essentielle afin de maîtriser les mécanismes de transfert entre l’hydrosphère et la biosphère et d'évaluer in fine l’impact global sur l’Homme. Dans ce travail, nous avons choisi de déterminer expérimentalement la spéciation de trois actinides dans l’eau de mer dopée : l’uranium(VI), le neptunium(V) et l’américium(III) (via l’analogue europium(III)) en couplant des calculs de spéciation avec les outils spectroscopiques dont la Spectroscopie Laser Résolue en Temps (SLRT) et la Spectroscopie d'Absorption des Rayons X (EXAFS). Puis nous avons étudié les processus d’accumulation sur l’éponge A. cavernicola, choisi ici car considérée comme un biomoniteur de pollution pour les métaux lourds. L’accumulation de l’europium(III), de l’américium(III) et de l’uranium(VI) dans A. cavernicola a donc été investiguée à l'échelle de traces et ultra traces. Pour l'europium, les techniques d'imagerie X et électronique ont permis de localiser l'élément accumulé et d'en préciser la spéciation. / The fate of natural and anthropogenic radionuclides in the environment remains a major concern in our modern nuclearized societies. Among the environmental compartments, the hydrosphere is ubiquitous and can transport compounds or elements over very long distances. The recent event of Fukushima demonstrated that the marine environment could be directly affected and this raises both scientific and societal questions. Moreover, some studies have already shown that radionuclides present in seawater can be strongly accumulated by marine organisms although their speciation is most of the time unknown. Yet this knowledge is essential to better understand the transfer mechanisms from the hydrosphere to the biosphere and to evaluate their global impact on humans. In this work, we chose to experimentally determine the speciation of three actinides in doped seawater: uranium(VI), neptunium(V) and americium(III) (and the chemical surrogate europium(III)) by coupling speciation modeling with spectroscopic tools among which Time-Resolved Laser-Induced Fluorescence (TRLIF) and X-ray Absorption Spectroscopy (XAS). Then, we have studied the accumulation process in the sponge A. cavernicola, chosen here because it is considered as a biomonitor of heavy metal pollution. The accumulation of europium(III), americium(III) and uranium(VI) in A. cavernicola were investigated at trace and ultra-trace levels. Besides, for europium, X-ray and electronic imaging permit to localize the accumulated element in the sponge and to specify its speciation.

This diploma thesis deals with the preparation of solid hydrophilic sponges made of acetalized PVAl. The sponges were produced by foaming by gaseous reaction by-product. The experimental work also includes the study of active compound immobilization into the sponge (finely ground lignite as a heavy metal sorbent).

Le but de ce travail de doctorat est l’étude chimique et biosynthétique de familles d’alcaloïdes guanidiniques d’origine marine provenant d’éponges de Méditerranée.Le travail est divisé en trois parties successives : 1) l’isolement d’alcaloïdes produits par des éponges marines de l’ordre des Poeciloscerida; 2) l’élucidation de la biosynthèse de la crambescine C1 par des études in vivo d’incorporation de précurseurs marqués au 14C; 3) la synthèse biomimétique de la crambescine A2 448 et de dérivés proches.La famille des alcaloïdes guanidiniques cycliques des crambescines est au coeur de la thèse, ces substances naturelles sont produites par l’éponge incrustante Crambe crambe. Ces alcaloïdes ont été découverts dans les années 1990 et ont suscité beaucoup d’intérêt pour leurs propriétés biologiques et écologiques et leurs synthèses totales. Par contre, leur biosynthèse était encore inconnue à ce jour. La seule synthèse biomimétique disponible était basée sur une hypothèse d’origine polyacétique. Les hypothèses récentes de nos groupes ont permis de mettre en avant une origine mixte: la partie cyclique guanidinique proviendrait d’un pyrrolidinium issu de l’arginine et d’un précurseur “céto-acide” proche des acides gras. Sur la base de cette hypothèse, nous avons mis au point une expérience d’incorporation qui a ensuite inspirée une voie de synthèse biomimétique pour l’accès aux crambescines et dérivés. Les premières conclusions quant à l’origine biosynthétique de ces molécules sont les faits les plus marquants de ce travail. Nous apportons une meilleure compréhension de la biochimie des alcaloïdes guanidiniques marins de structures complexes. / This thesis aims at the study of the chemical and biogenetic origin of specialized guanidine-alkaloid metabolites produced by sponges from the Mediterranean Sea.The work is divided into three main parts: 1) isolation of alkaloids produced by sponges of the Poeciloscerida order; 2) biosynthesis of crambescin C1 by in-vivo 14C-feeding experiments with Crambe crambe sponge; 3) biomimetic synthesis of crambescin A2 448 and derivatives. The main focus of the thesis will be the family of cyclic-guanidine alkaloids "crambescins", produced by the red incrusting sponge Crambe crambe.These alkaloids were discovered in the early 90s and despite the large interest on their biological activities, ecological roles, and synthesis, their biosynthesis is still unknown.The only available biomimetic synthesis of crambescins was based on a fully polyketide origin hypothesis. Recently our groups suggested an alternative biosynthetic hypothesis in which the guanidine-core would be originated from a condensation between a guanidinated pyrrolidinium derived from arginine and a beta-keto fatty acid. Based on this hypothesis, we designed a biosynthesis experiment that inspired a biomimetic synthesis route to access the crambescins and derivatives. The insights from these studies are the first experimental conclusions about the biosynthesis of crambescins. Finally, this work leads to a better comprehension of the biochemistry involved in guanidine marine alkaloids of complex structures.

Natural products offer many possibilities for the treatment of disease. More than 70% of the Earth’s surface is ocean, and recent exploration and access has allowed for new additions to this catalog of natural treasures. The Central Red Sea off the coast of Saudi Arabia serves as a newly accessible location, which provides the opportunity to bioprospect marine sponges with the purpose of identifying novel antiviral scaffolds. Antivirals are underrepresented in present day clinical trials, as well as in the academic screens of marine natural product libraries. Here a high-throughput pipeline was initiated by prefacing the antiviral screen with an Image-based High-Content Screening (HCS) technique in order to identify candidates with antiviral potential. Prospective candidates were tested in a biochemical or cell-based assay for the ability to inhibit the NS3 protease of the West Nile Virus (WNV NS protease) as well as replication and reverse transcription of the Human Immunodeficiency Virus 1 (HIV-1). The analytical chemistry techniques of High-Performance Liquid Chromatograpy (HPLC), Liquid Chromatography-Mass Spectrometry (LC-MS), and Nuclear Magnetic Resonance (NMR) where used in order to identify the compounds responsible for the characteristic antiviral activity of the selected sponge fractions. We have identified a 3-alkyl pyridinium from Amphimedon chloros as the causative agent of the observed WNV NS3 protease inhibition in vitro. Additionally, we identified debromohymenialdisine, hymenialdisine, and oroidin from Stylissa carteri as prospective scaffolds capable of HIV-1 inhibition.

The chemical diversity of the phylum Porifera have provided marine natural products (MNPs) such as alkaloids, terpenoids and peptides with ranging biological activity. Every two days a novel compound deriving from sponges are discovered. The aim of this report is to explore the metabolic diversity of deep-sea sponges collected from five different geographical locations. The metabolome of the deep-sea sponges was studied with tandem mass spectrometry (UPLC- MS/MS) and screened for peptides and other major compounds. The aim also includes the selection, isolation and characterisation of a compound obtained from the metabolic profiling of the sponges. The metabolic profiles of 25 sponges were screened. The specimens analysed in this report displayed great metabolic diversity and peptides, halogenated compounds as well as presumable alkaloids were found. The spectra of some specimens displayed low sensitivity which required optimisation such as increase of volume injection. Nevertheless, the report offers novel discoveries for sponges that have never previously been examined. The brominated compound derived from the sponge Desmacella annexa was analysed using large-scale extraction and different analytical techniques such as preparative-HPLC, Q-Tof-MS and NMR. However, the isolation of the target compound was unsuccessful due to co-extractant compounds and insufficient amount of the compound to perform further purification.  Nevertheless, the discoveries made from the metabolic profiles of the sponges may be of assistance when selecting potential bioactive compounds for further studies. Furthermore, bioassays may be performed in the future on the extracts obtained from the sponge Desmacella annexa.