(Table 1, 2) Foraminifera biometric data, and boron isotopic composition of Globigerinoides sacculifer of sediments from the Ontong-Java Plateau

Sediment samples from the Ontong-Java Plateau in the Pacific and the 90° east ridge in the Indian Ocean were used to investigate whether shell size and early diagenesis affect d11B of the symbiont-bearing planktonic foraminifer Globigerinoides sacculifer. In pristine shells from both study locations we found a systematic increase of d11B and Mg/Ca with shell size. Shells in the sieve size class 515-865 µm revealed d11B values +2.1 to +2.3 per mil higher than shells in the 250-380 µm class. This pattern is most likely due to differences in symbiont photosynthetic activity and its integrated effect on the pH of the foraminiferal microenvironment. We therefore suggest smaller individuals must live at approximately 50-100 m water depth where ambient light levels are lower. Using the empirical calibration curve for d11B in G. sacculifer, only shells larger than 425 µm reflect surface seawater pH. Partial dissolution of shells derived from deeper sediment cores was determined by shell weight analyses and investigation of the shell surface microstructure by scanning electron microscopy. The d11B in partially dissolved shells is up to 2 per mil lower relative to pristine shells of the same size class. In agreement with a relatively higher weight loss in smaller shells, samples from the Ontong-Java Plateau show a more pronounced dissolution effect than larger shells. On the basis of the primary size effect and potential postdepositional dissolution effects, we recommend the use of shells that are visually pristine and, in the case of G. sacculifer, larger than 500 ?m for paleoreconstructions.

(Table 1) Sample descriptions and results: Carbon, lipid, and kerogen analyses, at DSDP Leg 64 Holes

Pleistocene sediments in the Guaymas Basin, Gulf of California, have been intruded by sills and their organic matter thus subjected to thermal stress. Sediment samples from DSDP/IPOD Sites 477, 478, and 481, and samples of thermally unaltered materials from Sites 474 and 479 were analyzed to characterize the lipids and kerogens and to evaluate the effects of the intrusive thermal stresses. The lipids of the thermally unaltered samples are derived from microbial and terrestrial higher-plant detritus. The samples from the sill proximities contain the distillates, and those adjacent to the sills contain essentially no lipids. The pyrograms of the kerogens from the unaltered samples reflect their predominantly autochthonous microbial origin. When compared with the unaltered samples, the pyrograms of the altered kerogen samples reflect the thermal effects by a reduction in the complexity of the products. Kerogens adjacent to the sills produced little or no pyrolysis products. The effects of intrusions into unconsolidated, wet sediments resulted in in situ pyrolysis of the organic matter, as confirmed by these data.

(Table 1) Lipid yields for samples across the Cretaceous/Tertiary boundary in DSDP Hole 86-577

Core samples of calcareous sediments taken from above and below the proposed Cretaceous/Tertiary boundary (Sample 577-12-5, 130 cm) were examined for geochemical evidence of the mass extinctions and faunal successions that marked this period. The lipid compositions of the six core samples examined were virtually identical and were characterized by a large component of unresolved naphthenic hydrocarbons and a homologous series of an/mo-alkanes, both presumably of bacterial origin. The results of this preliminary study suggest that the lipids of sediments deposited over a several million year period encompassing the Cretaceous-Tertiary extinctions have been almost completely recycled by bacterial metabolism, which occurred under oxic depositional and/or diagenetic conditions and which left a unique bacterial signature with only minor traces of the original sedimentary lipids.

Lipid analytic of environmental and cultural samples

Membrane lipids of marine planktonic archaea have provided unique insights into archaeal ecology and paleoceanography. However, past studies of archaeal lipids in suspended particulate matter (SPM) and sediments mainly focused on a small class of fully saturated glycerol dibiphytanyl glycerol tetraether (GDGT) homologues identified decades ago. The apparent low structural diversity of GDGTs is in strong contrast to the high diversity of metabolism and taxonomy among planktonic archaea. Furthermore, adaptation of archaeal lipids in the deep ocean remains poorly constrained. We report the archaeal lipidome in SPM from diverse oceanic regimes. We extend the known inventory of planktonic archaeal lipids to include numerous unsaturated archaeal ether lipids (uns-AELs). We further reveal i) different thermal regulations and polar headgroup compositions of membrane lipids between the epipelagic (<= 100 m) and deep (> 100 m) populations of archaea; ii) stratification of unsaturated GDGTs with varying redox conditions; and iii) enrichment of tetra-unsaturated archaeol and fully saturated GDGTs in epipelagic and deep oxygenated waters, respectively. Such stratified lipid patterns are consistent with the typical distribution of archaeal phylotypes in marine environments. We thus provide an ecological context for GDGT-based paleoclimatology and bring about the potential use of uns-AELs as biomarkers for planktonic Euryarchaeota. This article is protected by copyright. All rights reserved.

Microbialites and lipid biomarker from coral reefs off the volcanic islands Tahiti and Vanuatu and from the nonvolcanic sites Belize and the Maldives

The occurrence of microbialites in post-glacial coral reefs has been interpreted to reflect an ecosystem response to environmental change. The greater thickness of microbialites in reefs with a volcanic hinterland compared to thinner microbial crusts in reefs with a non-volcanic hinterland led to the suggestion that fertilization of the reefal environment by chemical weathering of volcanic rocks stimulated primary productivity and microbialite formation. Using a molecular and isotopic approach on reef-microbialites from Tahiti (Pacific Ocean), it was recently shown that sulfate-reducing bacteria favored the formation of microbial carbonates. To test if similar mechanisms induced microbialite formation in other reefs as well, the Tahitian microbialites are compared with similar microbialites from coral reefs off Vanuatu (Pacific Ocean), Belize (Caribbean Sea, Atlantic Ocean), and the Maldives (Indian Ocean) in this study. The selected study sites cover a wide range of geological settings, reflecting variable input and composition of detritus. The new lipid biomarker data and stable sulfur isotope results confirm that sulfate-reducing bacteria played an intrinsic role in the precipitation of microbial carbonate at all study sites, irrespective of the geological setting. Abundant biomarkers indicative of sulfate reducers include a variety of terminally-branched and mid chain-branched fatty acids as well as mono-O-alkyl glycerol ethers. Isotope evidence for bacterial sulfate reduction is represented by low d34S values of pyrite (-43 to -42 per mill) enclosed in the microbialites and, compared to seawater sulfate, slightly elevated d34S and d18O values of carbonate-associated sulfate (21.9 to 22.2 per mill and 11.3 to 12.4 per mill, respectively). Microbialite formation took place in anoxic micro-environments, which presumably developed through the fertilization of the reef environment and the resultant accumulation of organic matter including bacterial extracellular polymeric substances (EPS), coral mucus, and marine snow in cavities within the coral framework. ToF-SIMS analysis reveals that the dark layers of laminated microbialites are enriched in carbohydrates, which are common constituents of EPS and coral mucus. These results support the hypothesis that bacterial degradation of EPS and coral mucus within microbial mats favored carbonate precipitation. Because reefal microbialites formed by similar processes in very different geological settings, this comparative study suggests that a volcanic hinterland is not required for microbialite growth. Yet, detrital input derived from the weathering of volcanic rocks appears to be a natural fertilizer, being conductive for the growth of microbial mats, which fosters the development of particularly abundant and thick microbial crusts.

Mean redox potential values in surface sediments along the transect D in the Cretan Sea (Table 1)

The seasonal, spatial and bathymetric changes in the distribution of chloroplastic pigments (Chl a, phaeopigments and CPE), TOC, TON, ATP, bottom water nutrient content and the main biochemical classes of organic compounds (lipids, proteins and carbohydrates) were recorded from May 1994 to September 1995 over the continental margin of northern Crete. The concentration of chloroplastic pigment equivalents (CPE) was always low, dropping dramatically along the shelf-slope gradient. Microbial activity (ATP) also dropped sharply beyond the continental shelf following a distribution pattern similar to TOC and TON. Lipid, protein and carbohydrate concentrations, as well as biopolymeric carbon were comparable to those reported for other more productive areas, however, the quality of the organic matter itself was rather poor. Thus, carbohydrates, the dominant biochemical class, were characterised by being highly (80-99%) refractory, as soluble carbohydrates represented (on annual average) only 6% of the total carbohydrate pool. Protein and lipid concentrations strongly decreased with depth, indicating depletion of trophic resources in the bathyal zone. Proteins appeared to be the more degradable compounds and indeed the protein to carbohydrate ratios were found to decrease strongly in the deeper stations. Organic matter content and quality decreased both with increasing distance from the coast and within the sediment. All sedimentary organic compounds were found to vary between sampling periods, with the changes being more pronounced over the continental shelf. The different temporal patterns of the various components suggest a different composition and/or origin of the OM inputs during the different sampling periods. The amount of material reaching the sediments below 540 m is extremely low, suggesting that most of the organic material is decomposed and/or utilised before reaching the sea floor. In conclusion, the continental shelf and bathyal sediments of the Cretan Sea can be considered, from a trophic point of view, as two different subsystems.

Isotopic composition of diet and tissues, and isotope discrimination factors for pink-footed and barnacle geese, Svalbard

Breeding in the high Arctic is time constrained and animals should therefore start with their annual reproduction as early as possible. To allow for such early reproduction in migratory birds, females arrive at the breeding grounds either with body stores or they try to rapidly develop their eggs after arrival using local resources. Svalbard breeding barnacle geese Branta leucopsis have to fly non-stop for about 1100 km from their last continental staging site to the archipelago making the transport of body stores costly. However, environmental conditions at the breeding grounds are highly unpredictable favouring residual body stores allowing for egg production after arrival on the breeding grounds. We estimated the reliance on southern continental resources, i.e. body stores for egg formation, in barnacle geese using stable isotope ratios in the geese's forage along the flyway and in their eggs. Females adopted mixed breeding strategies by using southern resources as well as local resources to varying extents for egg formation. Southern capital in lipid-free yolk averaged 41% (range: 23-65%), early laid eggs containing more southern capital than eggs laid late in the season. Yolk lipids and albumen did not vary over time and averaged a southern capital proportion of 54% (range: 32-73%) and 47% (range: 25-88%), respectively. Our findings indicate that female geese vary the use of southern resources when synthesizing their eggs and this allocation also varies among egg tissues. Their mixed and flexible use of distant and local resources potentially allows for adaptive adjustments to environmental conditions encountered at the archipelago just before breeding.

(Table 1) Lipid and kerogen content at DSDP Leg 64 Holes

Diatomaceous mud and an organically-rich claystone from holes at Sites 474 and 476 at the mouth of the Gulf of California were analyzed by organic geochemical methods to characterize their organic matter. The lipids of all three samples are primarily marine autochthonous, with the exception of Sample 474-5-3, 105-107 cm, which also contains some vascular plant wax. Based on the lipid composition, the sediment was deposited mainly under oxic environmental conditions. The kerogens were aliphatic and autochthonous marine. Two lignite fragments were also analyzed, and the data indicate that they are driftwood that absorbed marine bitumen from the surrounding sediment during coalification.

(Table 1) Sample descriptions, carbon contents, and lipid yields across the K/T boundary at DSDP Hole 93-605 and at Stevns Klint, Denmark

This reconnaissance study was undertaken to determine whether the mass extinctions and faunal successions that mark the Cretaceous/Tertiary (K/T) boundary left a discernible molecular fossil record in the sediments of this period. Lipid signatures of sediments taken from above and below the K/T boundary were compared in core and outcrop samples taken from two locations: the U.S. east coast continental margin (western Atlantic Ocean, DSDP Site 605) and Stevns Klint, Denmark. Four calcareous sediments taken from above and below the K/T boundary in DSDP Hole 605, Section 605-66-1, revealed changing lipid signatures between above and below that are characterized by a large component of unresolved naphthenic hydrocarbons and a homologous series of n-alkanes ranging from Ci6 to C33. These lipid signatures are attributed to an influx of a terrestrial higher plant component and to bacterial reworking of the sediments under partially anoxic depositional and/or diagenetic conditions. The outcrop samples from Stevns Klint had extremely low concentrations of indigenous lipids. The fish clay at the K/T boundary contained traces of microbial hydrocarbons and fatty acids, whereas the carbonates above and below had only microbial fatty acids and additional terrestrial resin acids. The data from both sites indicate a perturbation in the deposition of lipid compound classes across the K/T boundary.

(Table 1) Composition of lipids in particulate matter and bottom sediments of the Baltic Sea

Lipid contents in the upper layer of bottom sediments in the Baltic Sea range from 0.37 to 2.66 mg/g (1.2-25.8% Corg). It is shown that the main factors determining composition of lipids in bottom precipitates are relative roles of different sources of lipids in sediments and conditions of sediment accumulation. Runoff of the Daugava River into the Gulf of Riga contributes simple low-polarity lipids. Sterols and certain bound fatty acids originate in living organic matter. Polar lipids are formed by inheritance of complex phospholipids and glycolipids from plankton and/or by formation of polycondensates.

Composition of free lipids in bottom sediments in the tropical West Pacific and South Atlantic

Contents of free lipids in the upper layers of slightly siliceous diatomaceous oozes from the South Atlantic and of calcareous foraminiferal oozes, of coral sediments and of red clays from the western tropical Pacific amount varies from 0.014 to 0.057% of dry sediment. Their content is inversely proportional to total content of organic matter. Relative content of low-polar compounds in total amount of lipids and content of hydrocarbons, fatty acids, and sterols in the composition of these compounds can serve as an index of degree of transformation of organic matter in sediment because these compounds are resistant to various degree to microbial and hydrolytic decomposition and, consequently, are selectively preserved under conditions of biodegradation of organic compounds during oxydation-reduction processes.

Elemental composition and petroleum-generating potential of the methylene chloride extracts from DSDP Leg 66 Holes

Organic geochemical studies on samples from Holes 487, 488, and 490 in the southern Mexico Middle America Trench provided an opportunity to characterize the organic fraction of the sedimentary section in an active trench environment and to project the petroleum-producing potential of the extracted lipid fractions. The samples were geologically young and of shallow burial history. Samples from Hole 487, located on the oceanic plate, range in age from late Miocene to middlelate Pleistocene. Samples from Hole 488, representing undifferentiated Quaternary sediment, were collected on the landward side of the lower trench slope. Miocene(?) to Quaternary sediments from Hole 490 were obtained from the upper slope immediately seaward of the inferred location of the continental crust.

Suppression of nuclear factor-κB activity in macrophages by chylomicron remnants: modulation by the fatty acid composition of the particles

Current evidence indicates that chylomicron remnants (CMR) induce macrophage foam cell formation, an early event in atherosclerosis. Inflammation also plays a part in atherogenesis and the transcription factor nuclear factor-kappaB (NF-kappaB) has been implicated. In this study, the influence of CMR on the activity of NF-kappaB in macrophages and its modulation by the fatty acid composition of the particles were investigated using macrophages derived from the human monocyte cell line THP-1 and CMR-like particles (CRLPs). Incubation of THP-1 macrophages with CRLPs caused decreased NF-kappaB activation and downregulated the expression of phospho-p65-NF-kappaB and phospho-IkappaBalpha (pIkappaBalpha). Secretion of the inflammatory cytokines tumour necrosis factor alpha, interleukin-6 and monocyte chemoattractant protein-1, which are under NF-kappaB transcriptional control, was inhibited and mRNA expression for cyclooxygenase-2, an NF-kappaB target gene, was reduced. CRLPs enriched in polyunsaturated fatty acids compared with saturated or monounsaturated fatty acids had a markedly greater inhibitory effect on NF-kappaB binding to DNA and the expression of phospho-p65-NF-kappaB and pIkappaB. Lipid loading of macrophages with CRLPs enriched in polyunsaturated fatty acids compared with monounsaturated fatty acids or saturated fatty acids also increased the subsequent rate of cholesterol efflux, an effect which may be linked to the inhibition of NF-kappaB activity. These findings demonstrate that CMR suppress NF-kappaB activity in macrophages, and that this effect is modulated by their fatty acid composition. This downregulation of inflammatory processes in macrophages may represent a protective effect of CMR which is enhanced by dietary polyunsaturated fatty acids.

A Rare Loss-of-Function Variant in Scavenger Receptor Class B Type I (SCARB1) Raises HDL Cholesterol and Increases Risk of Coronary Disease

Scavenger receptor BI (SR-BI) is the major receptor for high-density lipoprotein (HDL)
cholesterol (HDL-C). In humans, high amounts of HDL-C in plasma are associated with a
lower risk of coronary heart disease (CHD). Mice that have depleted Scarb1 (SR-BI
knockout mice) have markedly elevated HDL-C levels but, paradoxically, increased
atherosclerosis. The impact of SR-BI on HDL metabolism and CHD risk in humans remains
unclear. Through targeted sequencing of coding regions of lipid-modifying genes in 328
individuals with extremely high plasma HDL-C levels, we identified a homozygote for a lossof-function
variant, in which leucine replaces proline 376 (P376L), in SCARB1, the gene
encoding SR-BI. The P376L variant impairs posttranslational processing of SR-BI and
abrogates selective HDL cholesterol uptake in transfected cells, in hepatocyte-like cells
derived from induced pluripotent stem cells from the homozygous subject, and in mice.
Large population-based studies revealed that subjects who are heterozygous carriers of
the P376L variant have significantly increased levels of plasma HDL-C. P376L carriers have
a profound HDL-related phenotype and an increased risk of CHD (odds ratio = 1.79, which is
statistically significant).

Effets préventifs et thérapeutiques des polyphénols dans un modèle in vitro et in vivo de maladie inflammatoire de l’intestin : caractérisation des polyphénols de la pelure de pomme et de la canneberge par spectrométrie de masse

La muqueuse intestinale est exposée à des agents oxydants provenant de l’ingestion d’aliments modifiés, de cellules immuno-inflammatoires et de la flore intestinale. Une diète élevée en fruits et légumes peut diminuer le stress oxydant (SOx) ainsi que l’inflammation via plusieurs mécanismes. Ces effets bénéfiques peuvent être attribuables à leur contenu élevé en polyphénols. La première étude de mon doctorat consistait à tester l’hypothèse que les polyphénols extraits de pelures de pomme (DAPP) pouvaient diminuer le stress oxydant et l'inflammation impliqués dans les maladies inflammatoires de l'intestin (MII). Nous avons caractérisé les polyphénols des DAPP par spectrométrie de masse (LC-MS) et examiné leur potentiel antioxydant et anti-inflammatoire au niveau des cellules intestinales. L’identification des structures chimiques des polyphénols a été effectuée par LC-MS. Le SOx a été induit par l’ajout du complexe fer/ascorbate (Fe/Asc, 200 µM/2 mM) et l’inflammation par la lipopolysaccharide (LPS, 200µg/mL) à des cellules intestinales Caco-2/15 pré-incubées avec les DAPP (250 µg/mL). L’effet du SOx est déterminé par le dosage du malondialdéhyde (MDA), de la composition des acides gras polyinsaturés et de l’activité des enzymes antioxydantes endogènes (SOD et GPx). L’impact des DAPP sur l’inflammation a été testé par l’analyse de l’expression des marqueurs inflammatoires: cyclooxygénase-2 (COX-2), le facteur de nécrose tumorale alpha (TNF-a et l’interleukine-6 (IL-6) et les facteurs de transcription NF-KB, Nrf-2 et PGC1α par immunobuvardage. Nos données ont montré que les flavonols et les flavan-3-ols constituent les composés polyphénoliques majoritaires des DAPP. L’ajout de Fer2+/Asc a provoqué une augmentation de la peroxidation lipidique comparativement aux cellules contrôles, un appauvrissement des acides gras polyinsaturés n-3 et n-6, et une modulation des enzymes antioxydantes, se traduisant par une augmentation de l’activité de la SOD et une diminution de la GPx. En contrepartie, les DAPP ont exhibé leur potentiel à corriger la plupart des perturbations, y compris l’expression protéique anormalement élevée du COX-2 et la production de la prostaglandine E2 (PGE2), ainsi que l’inflammation telle que réflétée par les facteurs NF-κB, TNF-α et IL-6. Par ailleurs, les mécanismes sous-jacents à ces changements bénéfiques des DAPP ont fait intervenir les facteurs de transcription antioxydants (Nrf-2, PGC1α). Vraisemblablement, cette première étude a permis de démontrer la capacité des DAPP à amoindrir le SOx et à réduire l’inflammation, deux processus étroitement impliqués dans les MII. Dans la deuxième étape de mon doctorat, nous avons voulu comparer les résultats de DAPP à ceux des polyphénols dérivant de la canneberge qui est considérée par la communauté scientifique comme le fruit ayant le plus fort potentiel antioxydant. À cette fin, nous avons caractérisé l’effet des composés polyphénoliques de la canneberge (CPC) sur le SOx, la défense antioxydante et l’inflammation au niveau intestinal tout en définissant leur métabolisme intraluminal. Les différents CPC ont été séparés selon leur poids moléculaire par chromatographie et leurs structures chimiques ont été identifiées par LC-MS. Suite à une pré-incubation des cellules Caco-2/15 avec les extraits CPC (250 µg/mL), le Fe/Asc et la LPS ont été administrés comme inducteurs du SOx et de l’inflammation, respectivement. La caractérisation globale des CPC a révélé que les acides phénoliques composaient majoritairement l’extrait de canneberge de petit poids moléculaire (LC) alors que les flavonoïdes et les procyanidines dimériques/trimériques représentaient l’extrait de poids moléculaire moyen (MC) tout en laissant les procyanidines oligo et polymériques à l’extrait de haut poids moléculaire (HC). Les CPC ont permis de restaurer la plupart des perturbations engendrées dans les Caco-2/15 par le Fe/Asc et le LPS. Les CPC exhibaient le potentiel d’abaisser les niveaux de MDA, de corriger la composition des acides gras polyinsaturés n-3 et n-6, d’augmenter l’activité des enzymes antioxydantes (SOD, GPx et CAT) et d’élever l’expression de Nrf2 et PGC1α. En outre, les CPC pouvaient aussi réduire les niveaux élevés des protéines inflammatoires COX-2, TNF-α et IL-6 ainsi que la production des PGE2 par un mécanisme impliquant le NF-κB. Au niveau mitochondrial, les procyanidines oligomériques ont réussi à corriger les dysfonctions reliées à la production d’énergie (ATP), l’apoptose (Bcl-2, Cyt C et AIF) et le statut des facteurs de transcription mitochondriaux (mtTFA, mtTFB1, mtTFB2). Dans le but de bien comprendre les mécanismes d’action des CPC, nous avons défini par LC-MS les composés polyphénoliques qui ont été transportés ou absorbés par l’entérocyte. Nos analyses soulignent le transport (i) des acides cinnamiques et benzoïques (LC); (ii) la quercétine glycosylée et conjuguée et les procyanidines dimériques de type A (MC); et (iii) l’épicatéchine et les procyanidines oligomériques (HC). Les processus de métabolisation (méthylation, glucuronidation et sulfatation) au niveau de l’entérocyte ont probablement permis le transport de ces CPC surtout sous leur forme conjuguée. Les procyanidines oligomériques ayant un degré de polymérisation supérieur à 2 (HC) ont semblé adhérer aux cellules Caco-2/15. L’épicatéchine suivi par les procyanidines dimériques de type A ont été trouvés majoritaires au niveau des mitochondries. Même si nous ignorons encore l’action biologique de chaque composé polyphénolique, nous pouvons suggérer que leurs effets combinatoires exercent des fonctions antioxydantes, anti-inflammatoires et mitochondriales dans le modèle intestinal Caco-2/15. Dans une troisième étape, nous avons procédé à l’évaluation des aspects préventifs et thérapeutique des DAPP tout en sondant les mécanismes sous-jacents dans une étude préclinique. À cette fin, nous avons exploité le modèle de souris avec colite expérimentale provoquée par le Dextran Sulfate de Sodium (DSS). L’induction de l’inflammation intestinale chez la souris C57BL6 a été effectuée par l’administration orale de DSS à 2.5% pendant 10 jours. Des doses physiologiques et supra-physiologiques de DAPP (200 et 400 mg/kg/j, respectivement) ont été administrées par gavage pendant 10 jours pré- et post-DSS. L’inflammation par le DSS a provoqué une perte de poids, un raccourcissement du côlon, le décollement dystrophique de l’épithélium, l’exulcération et les infiltrations de cellules mono et polynucléaires au niveau du côlon. De plus, le DSS a induit une augmentation de la peroxidation lipidique, une régulation à la baisse des enzymes antioxydantes, une expression protéique à la hausse de la myéloperoxidase (MPO), du COX-2 et de la production des PGE2. Par ailleurs, les DAPP ont permis de corriger ou du moins d’alléger la plupart de ces anomalies en situation préventive ou thérapeutique, en plus d’abaisser l’expression protéique de NF-κB et des cytokines inflammatoires (TNF-a et l’IL-6) tout en stimulant les facteurs de transcription antioxydants (Nrf-2, PGC1α). Conséquemment, les polyphénols des DAPP ont exhibé leur puissant pouvoir antioxydant et anti-inflammatoire au niveau intestinal dans un modèle in vivo. Leurs actions sont associées à la régulation des voies de signalisation cellulaire et des changements dans la composition du microbiote. Ces trois projets de recherche permettent d’envisager l’évaluation des effets préventifs et thérapeutiques des DAPP cliniquement chez les patients avec des désordres inflammatoires de l’intestin.