Éditeur(s) : Université des Antilles Études caribéennes
Résumé : L’étude des représentations de la drépanocytose dans une population scolarisée de l’île de Marie-Galante (N=267), en Guadeloupe, est ici réalisée à partir du traitement des réponses à une question d’association libre qui s’inscrivait dans un questionnaire plus large. L’analyse des occurrences et des co-occurrences spontanément associées à la drépanocytose montre le flou qui entoure cette maladie dans la population étudiée, attestant d’une faible maîtrise des représentations biomédicales. Ce sont finalement le statut et la signification du sang, ainsi que la notion même de maladie génétique, qui paraissent mal assurés, car réinscrits dans l’univers des représentations culturelles et sociales liées à l’identité/altérité et à la filiation.
This paper presents a part of the results of a research on the representation on SCD (Sickle Cell Disease) among a schooled population living in Marie-Galante (Guadeloupe). It treats free associations of the respondents concerning SCD. The analysis of occurrencies and co-occurrencies spontaniously associated to the disease reveals the incertitude surrounding it, attesting thus of a small control of biomedical representations. The status and signification of blood, even as the notion of genetic disease, seem to be ambigious in their answers. They are in fact imbedded in the universe of social and cultural representations related to identity/alterity and filiation problematics.
Guadeloupe

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.3684
http://journals.openedition.org/etudescaribeennes/3684

Éditeur(s) : HAL CCSD IOS Press
Résumé : International audience
Purpose: The aim of this study was to clarify whether exercising in a tropical climate induces blood rheology alterations despite ad libitum hydration. Methods: Hematological, biochemical and hemorheological changes were investigated in young healthy adults (N = 9 men, 20.7 ± 0.8 yrs) after a 10-km race in hot and humid conditions. Subjects' maximal aerobic abilities were tested using a maximal ramp exercise. Blood was sampled at rest (T R), at the end of the race (T Ex), and after 24 hours of recovery (T 24). Ad libitum hydra-tion was allowed during the race. Blood viscosity (b), red blood cell deformability (EI), aggregation (AI) and disaggregation shear rate (␥) were measured. Results: Hematocrit, hemoglobin and plasma concentration of chlorine, sodium and potassium did not change in response to exercise. No functional consequence was observed on RBC deformability since EI remained unchanged. Percentages of echinocytes, schizocytes and stomatocytes remained in the subclinical range at all times. AI, µ and ßb did not present change. Conclusion: Running exercise in tropical climate with ad libitum hydration does not alter the main rheological properties of blood.
ISSN: 1386-0291

hal-01163975
https://hal.univ-antilles.fr/hal-01163975
DOI : 10.3233/CH-2011-1388

Éditeur(s) : HAL CCSD Springer/Terra Scientific Publishing Company
Résumé : International audience
This study of the Cajati deposit provides evidence that the ore was neither purely hydrothermal, nor volcanic in origin, as previous workers have proposed. The ores were formed from magnetite-rich magmas, hydrothermally altered and intruded at an indicated crustal depth in excess of 500 m. The mineralogical and textural association between magnetite and magnesioferrite in the carbonatite, and between the titanomagnetite and magnesioferrite-Ti mineralization in the pyroxenite of hedenbergite, seems to be analog mineralizations strongly related to the ionic substitution of Fe2+ by Mg. Relatively high Q ratios (>= 5) for Jacupirangite-pyroxenite may indicate a thermo remanent magnetization (TRM) by the ore during post-metamorphic cooling, however it call also be developed from chemical remanent magnetization (CRM). Vector plots for the pyroxenite samples show reasonably linear and stable magnetic components. The intensity decay Curves show that only two components of magnetizations are likely present. Continuous susceptibility measurements with increasing temperature show that the main magnetic phase seems to be magnetite. Maghemite is probably produced during the cooling process. Susceptibility recorded from low temperature (liquid nitrogen (- 196 degrees C)) to room temperature produces typical Curves. indicating Verwey transition of magnetite. Hysteresis parameters point Out that nearly all values fill in a novel region of the Day plot, parallel to but below magnetite SD + MD mixing curves.
ISSN: 1343-8832

hal-00420922
https://hal.archives-ouvertes.fr/hal-00420922

Éditeur(s) : HAL CCSD
Résumé : This work focus on the characterization of the source and dynamic of compactional fluids during sedimentary burial, through two complementary examples of late orogenic oil‐field half‐grabens: The exhumed Lodève Permian Basin and a deep buried Jurassic basin in the North Viking Graben (North Sea).Constituting the main part of the thesis, a multi‐disciplinary approach was conducted in the Lodève Basin where Ba‐F‐Cu‐Pb polymetallic mineralized systems are trapped into synrift faults and paleokarsts in the carbonate basement at the hinge point of the rollover. The source, timing and P/T conditions of fluid migration were deduced from the analysis of the microfabric, the fluid inclusions microthermometry, and the isotopic (Sr, S, O, H) and Rare Earth Element (REE) signature. Results are then crossed with a structural and thermal modeling that consolidates the sequence and dynamics of fluid during burial.A similar approach was conducted in the North Viking Graben where fluid markers are restricted to 3D seismic and well core data. Comparable Ba‐Pb‐Zn veins are reported in basin margin, plugging one of the most important siliciclastic hydrocarbon reservoir in the substratum. This analysis provides additional constraints on basinal fluid behavior and allows us to propose a global dynamic model for various compositions of fluids and reservoirs.We conclude to a polyphase fluid sequence history including:(a) In the carbonate basement of the Lodève Basin, karstic paleocanyon incisions and associated cavities coupled to synrift fault, act as major drain for fluids. These structures are early affected by hypogen‐sulfuric karstification in response to the interaction between bacterial oxidation of sulfides entrapped within Lower Permian blackshales and the basement oxidizing aquifer.(b) Disequilibrium compaction initiates overpressure‐driven basinal fluid migration towards basin margins, characterized by temperatures around 150‐180°C and salinities between 9 et 18wt%eq.NaCl. Isotopic (Sr, S, O) and REE analyses reveal that Ba‐M+‐rich mineralizing fluids derived mainly from buried blackshales diagenesis. External fluids coming from the lower crust are also identified that play a key role in fluorite precipitation by the leaching of late hercynian granites (mean temperature of 250°C and salinity > 20wt%eq.NaCl).(c) During the synrift period, fluid overpressure is responsible for the periodic reactivation of fault plane according to seismic‐valve process, bedded‐control shearing and hydraulic brecciation at the basement‐seal interface. These mechanisms induce cyclic polymetallic mineralization by the mixing between in‐situ formation water and deep ascending basinal fluids.(d) Thermogenic fluids expulsion starts with last basinal fluids during late burial stage. Hydrocarbons thus migrate along the same regional pathways up to the rollover crest, where they are partly rerouted by the previous mineralized baffle.(e) In the Lodève basin, post‐rift exhumation of the margins led to the remobilization of synrift deposits by subaerial biochemical processes at the sulfate‐methane transition. The latter results from the interaction between the still active hydrocarbon dysmigration with a playa lake sulfate‐rich aquifer. Secondary low‐temperature barite fronts precipitate then within basement meteoric karsts.In addition to the « source to sink » model of basinal fluids, this work provides new insights on the early plugging of hydrocarbon reservoirs and for the metallogenesis of Mississippi Valley‐Type deposits.
Ce travail porte sur la caractérisation de la source et de la dynamique des fluides de bassin au cours de leur chargement à travers deux exemples complémentaires de demi‐grabens tardi‐orogéniques pétroliers : Le Bassin Permien de Lodève, aujourd’hui à l’affleurement et un bassin jurassique enfouis dans le North Viking Graben (Mer du Nord).Le coeur de la thèse concerne le Bassin de Lodève où, à partir d’une approche pluridisciplinaire intégrée, nous avons caractérisé l’architecture des minéralisations (Ba, F, Cu, Pb) piégées dans un réseau paléokarstique alimenté par les failles syn‐rift, dans le substratum carbonaté à l’apex du roll‐over. La source, le calendrier et les conditions de migration des fluides ont été approchés à partir de l’analyse de la micro‐fabrique, la microthermométrie sur inclusions fluides, les analyses isotopiques (Sr, S, O, H) et de Terres Rares. Les résultats analytiques ont été enfin croisés avec un modèle thermique et structural du bassin qui conforte la séquence et la dynamique du système fluide en cours d’enfouissement.Une démarche similaire, mais plus limitée, a été conduite dans le bassin du North Viking Graben où l’accès aux marqueurs fluides est restreint aux données de sismique 3D et de carottes. Comme à Lodève, les minéralisations Ba‐Pb‐Zn colmatent un réservoir dans le substratum à l’apex du roll‐over. Elles se présentent sous forme de ciments dans des grès ou des fractures. Cette analyse apporte des contraintes complémentaires et permet de proposer un modèle dynamique général avec des variantes en fonction de la nature des fluides et des réservoirs.On retiendra donc la séquence fluide suivante :(a) Dans le cas du bassin de Lodève sur substratum carbonaté, les chemins préférentiels de drainage se développent dans des paléocanyons N‐S couplés à un réseau de fractures et d’endokarsts météoriques. Ces derniers sont élargis en début de rifting par la dissolution hypogène sulfurique produite par l’oxydation bactérienne des sulfates et des pyrites des blackshales, au contact de l’aquifère oxydant du Cambrien.(b) Le déséquilibre de compaction initie la migration des fluides interstitiels en surpression vers les marges avec des températures autour de 150‐180°C et des salinités entre 9 et 18wt%eq.NaCl. Les analyses isotopiques (Sr, S, O) révèlent que la majorité des fluides provient de l’altération diagénétique des blackshales riches en métaux. Des interactions sont également mises en évidence avec des fluides profonds (entre 240°C et 260°C ; salinités > à 20wt%eq.NaCl), qui lessivent les granites tardi‐hercyniens.(c) Pendant le syn‐rift, les conditions de surpression de fluide permettent la réactivation cyclique des failles, les décollements stratigraphiques et la formation de brèches hydrauliques, favorisant la mise en connexion avec les réservoirs superficiels à l’apex du rollover. Le modèle de Sibson ajusté aux fluides de bassins est alors le moteur de la migration verticale.(d) Les fluides thermogéniques commencent à être expulsés avec les derniers fluides de compaction au cours d’un stade plus évolué de l’enfouissement en empruntant les mêmes chemins jusqu’à l’apex du roll over. Ils sont alors partiellement freinés et déviés par les colmatages minéralisés antérieurs.(e) A Lodève, la continentalisation des minéralisations antérieures au cours de l’exhumation post‐rift conduit à leur remaniement partiel au niveau de la transition sulfate‐méthane induite par l’interaction entre une playa évaporitique et la dysmigration des hydrocarbures. Des barytines secondaires de basse température, déprimées en Sr sont alors précipitées de manière synsédimentaire dans des karsts météoriques du socle.Outre l’illustration d’un modèle complet (source to sink) de dynamique des fluides dans un bassin, ce travail apporte de nouvelles contraintes dans l’approche du colmatage des réservoirs à hydrocarbures sur les têtes de blocs basculés et sur la genèse des gîtes miniers de type Mississippi Valley‐Type.
https://hal.archives-ouvertes.fr/tel-01457583

tel-01457583
https://hal.archives-ouvertes.fr/tel-01457583
https://hal.archives-ouvertes.fr/tel-01457583/document
https://hal.archives-ouvertes.fr/tel-01457583/file/th%C3%A8seLaurent2015V2.pdf

Éditeur(s) : HAL CCSD Nature Publishing Group
Résumé : International audience
Cancer cells display alterations in many cellular processes. One core hallmark of cancer is the Warburg effect which is a glycolytic reprogramming that allows cells to survive and proliferate. Although the contributions of environmental contaminants to cancer development are widely accepted, the underlying mechanisms have to be clarified. Benzo[a]pyrene (B[a]P), the prototype of polycyclic aromatic hydrocarbons, exhibits genotoxic and carcinogenic effects, and it is a human carcinogen according to the International Agency for Research on Cancer. In addition to triggering apoptotic signals, B[a]P may induce survival signals, both of which are likely to be involved in cancer promotion. We previously suggested that B[a]P-induced mitochondrial dysfunctions, especially membrane hyperpolarization, might trigger cell survival signaling in rat hepatic epithelial F258 cells. Here, we further characterized these dysfunctions by focusing on energy metabolism. We found that B[a]P promoted a metabolic reprogramming. Cell respiration decreased and lactate production increased. These changes were associated with alterations in the tricarboxylic acid cycle which likely involve a dysfunction of the mitochondrial complex II. The glycolytic shift relied on activation of the Na+/H+ exchanger 1 (NHE1) and appeared to be a key feature in B[a]P-induced cell survival related to changes in cell phenotype (epithelial-to-mesenchymal transition and cell migration).
ISSN: 2045-2322

Droits : http://creativecommons.org/licenses/by/
hal-01359569
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01359569
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01359569/document
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01359569/file/The%20environmental%20carcinogen-CCBY%20%281%29.pdf
DOI : 10.1038/srep30776

Éditeur(s) : HAL CCSD Springer Verlag (Germany)
Résumé : International audience
The influence of magnetic interactions on the anisotropy of magnetic susceptibility (AMS) have been largely studied by several theoretical models or experiments. Numerical models have shown that when magnetostatic interactions occur, the distributions of particles over the volume rather than their individual orientations control the AMS. We have shown recently from a comprehensive rock magnetic study and from a theoretical 2-dimensional (2-D) model that single domain particles closely packed in globule aggregates could produce strong local random interaction magnetic fields which could influence the magnetic susceptibility and decrease the degree of anisotropy. In this paper, we first present in detail this 2-D theoretical model and then we extend it to the 3-D case. The possible distribution function of the magnetostatic interaction fields comprises two extreme states: it is either isotropic or ordered. The former case corresponds to the thermal-demagnetized state while the second case corresponds to the alternating field (AF) demagnetized state. We show that when easy axes of magnetization are not uniformly distributed, the degree of anisotropy decreases as the interaction field increases in both AF- and thermal-demagnetized states in 2-D and 3-D geometry. Thus we conclude that random magnetic fields generated by a random arrangement of magnetic particles over the sample volume decrease the degree of anisotropy of AMS and may alter the magnetic fabric.
ISSN: 0039-3169

hal-00758113
https://hal.archives-ouvertes.fr/hal-00758113
https://hal.archives-ouvertes.fr/hal-00758113/document
https://hal.archives-ouvertes.fr/hal-00758113/file/SGEG-2012-HAL.pdf
DOI : 10.1007/s11200-010-9097-7

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The Maghrebides, Betics and some parts of the Calabrian, NE Sicilian and Tuscan allochtons constitute dismembered fragments of the Alpine belt that resulted from the Cenozoic collision between Africa and Eurasia and the opening of the Western Mediterranean basin. Mineral and whole-rock geochemical analyses have been performed on three distinct outcrops of mantle material from the Edough Massif of NE Algeria, namely the Bou Maiza (BM) gabbros, the La Voile Noire (LVN) amphibolites and the Sidi Mohamed (SM) peridotites. In all samples, Sr isotopes are largely affected by seawater alteration (87Sr/86Sract. > 0.70384 and up to 0.70888) and cannot be used to evaluate the nature of the source reservoirs. SM peridotites display variable depleted mantle Nd isotopic signatures (εNdact. from + 7.0 to + 12.2) and geochemical features suggesting no significant chemical depletion as a result of partial melting and melt extraction (Mg# < 90; slightly LREE-depleted patterns with La/YbN = 0.33-0.39). These rocks are interpreted as parts of the subcontinental lithospheric mantle incorporated into the crustal units of the Edough Massif during the early stages of opening of the Algerian basin. BM gabbros and LVN amphibolites show geochemical signatures indicating derivation from a common Depleted Mantle reservoir (εNd > + 7.9) and are likely cogenetic, but without filiation with the SM peridotites. Pb isotopes indicate a contribution of sediments in the source reservoir, which is attributed to contamination solely by hydrous fluids released from a sedimentary component. This observation, together with a LILE-enrichment, suggests a back-arc basin environment. These results indicate that BM and LVN units were obducted onto the North African margin and subsequently fragmented, probably during doming and exhumation of the lower continental crust of the Edough massif. Doming resulted in opposite movements of the overlying oceanic units, southward for the BM units and northward for LVN amphibolites.
ISSN: 0040-1951

hal-01122777
https://hal.archives-ouvertes.fr/hal-01122777
DOI : 10.1016/j.tecto.2014.03.031

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : In this paper, we consider the consolidation of consumption as prime stage of the production process and the diffusion of new forms of commerce in the city, as foundations for analyzing the urban space reproduction process in the contemporary period. Having as research place the metropolis of Sao Paulo - Brazil, we conducted an analysis and some thoughts on the place of commerce and consumption of luxury goods in the urban space reproduction process, analyzed from the perspective of the extended reproduction of capital.
En este trabajo, consideramos que la consolidación del consumo como etapa primaz del proceso de producción y la difusión de las nuevas formas de comercio en la ciudad, están en la base para analizar el proceso de reproducción del espacio urbano en el período contemporáneo. La metrópolis de São Paulo – Brasil, es el local de los análisis y reflexiones sobre el lugar del comercio y el consumo de bienes de lujo en la reproducción del espacio urbano, considerando la reproducción del capital.
São Paulo

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.7378
http://journals.openedition.org/etudescaribeennes/7378

Éditeur(s) : HAL CCSD BioMed Central
Résumé : International audience
BACKGROUND: Homologous recombination is the key process that generates genetic diversity and drives evolution. SPO11 protein triggers recombination by introducing DNA double stranded breaks at discreet areas of the genome called recombination hotspots. The hotspot locations are largely determined by the DNA binding specificity of the PRDM9 protein in human, mice and most other mammals. In budding yeast Saccharomyces cerevisae, which lacks a Prdm9 gene, meiotic breaks are formed opportunistically in the regions of accessible chromatin, primarily at gene promoters. The genome-wide distribution of hotspots in this organism can be altered by tethering Spo11 protein to Gal4 recognition sequences in the strain expressing Spo11 attached to the DNA binding domain of the Gal4 transcription factor. To establish whether similar re-targeting of meiotic breaks can be achieved in PRDM9-containing organisms we have generated a Gal4BD-Spo11 mouse that expresses SPO11 protein joined to the DNA binding domain of yeast Gal4. RESULTS: We have mapped the genome-wide distribution of the recombination initiation sites in the Gal4BD-Spo11 mice. More than two hundred of the hotspots in these mice were novel and were likely defined by Gal4BD, as the Gal4 consensus motif was clustered around the centers in these hotspots. Surprisingly, meiotic DNA breaks in the Gal4BD-Spo11 mice were significantly depleted near the ends of chromosomes. The effect is particularly striking at the pseudoautosomal region of the X and Y chromosomes -- normally the hottest region in the genome. CONCLUSIONS: Our data suggest that specific, yet-unidentified factors influence the initiation of meiotic recombination at subtelomeric chromosomal regions.
ISSN: 1471-2164

inserm-00849779
http://www.hal.inserm.fr/inserm-00849779
http://www.hal.inserm.fr/inserm-00849779/document
http://www.hal.inserm.fr/inserm-00849779/file/1471-2164-14-493.pdf
DOI : 10.1186/1471-2164-14-493

Éditeur(s) : HAL CCSD Cerimes
Résumé : L'ensemble des articles est archivé sur ArchiveTémaTice. Les actes sont aussi accessibles sur le site du colloque http://www.cerimes.fr/colloquefrancomexicain
Les textes qui composent ces actes ont été présentés à l'occasion du premier colloque franco-mexicain en sciences de la communication, organisé par la Asociación mexicana en Ciencias de la comunicación (AMIC) et la Société Française des Sciences de l'Information et de la Communication (SFSIC), à Mexico, du 8 au 10 avril 2002.

Les médias classiques: radio, télévision (8 avril 2002)
Introduction . La coopération scientifique bilatérale et l'interculturel dans l'activité de recherche, Bruno Ollivier
La recherche française sur le média et les discours télévisuels: éléments pour un bilan prospectif, Guy Lochard
Parcours de la programmation télévisée au Mexique, Florence Toussaint
El regimen de la television hertziana en Mexico, Claudia I. Garcia Rubio
La question de l'éthos et du genre en communication politique, Simone Bonnafous
L'exposition de la vie privée dans les médias, André Vitalis

Identités, culture, communication (9 avril 2002)
Reconfiguraciones cimunicativas de la socialidad y reencantamientos de la communication identidad, Jesus Martin-Barbero
Identité, culture et communication, Jean François Tetu
Las organizaciones civiles en las radiodifusoras comerciales, Dr. José Cisneros E.
Les SIC et l'altérité: démarches d'une recherche sur la Chine. réflexions épitstémologiques sur les analyses de corpus à base communicationnelles de langue et de culture non-maternelles, Dominique Colomb
Transicion, reforma del estado y medios de comunicacion en Mexico, Dr. Javier Esteinou Madrid
Medios masivos y formacion psicosocial, Enrique Guinsberg

Technologies d'information et de communication ( 10 avril 2002)
Quoi de nouveau dans la recherche française en informatique et communication ? Bernard Miege
Convergencia tecnologica: perspectivas de investigacion en Mexico, Delia Crovi Druetta
Medias, technologies et public: la notion de projet au cœur d'une éventuelle médiation, Claire Noy
La formacion de profesores de educacion superior en el uso de la computadora y la internet. reflexioànes sobre el tema, Luz Maria Garay Cruz
Vers un retour à une lecture non linéaire, Schmidt C. T, Roxin I.(), Mercier D, Hufschmitt B. & Cotten J.-P
NTIC et éducation à distance. Le cas d'Edusat au Mexique face au cas français, Norma Veronica Fernandez Arriaga.
Les sciences de l'éducation et les sciences de la communication en dialogue: à propos des médias et des technologies éducatives, Geneviève Jacquinot-Delaunay
Internet et Intranet dans les organisations "un scénario récurrent", Jean-Antoine Corbalan
De l'université virtuelle au campus numérique : simple effet de traduction ou changement de paradigme, Françoise Thibault
Competencias mediacionales de los sujetos en programas educativos en entornos digitales, Maria Elena Chan Nunez
Le journal quotidien sur le Web. L'identité éditoriale au risque du formatage, Annelise Touboul
Conclusion, Carmen Gomez-Mont
Premier colloque franco-mexicain de sciences de la communication
Mexico, France

Droits : info:eu-repo/semantics/OpenAccess
ISBN : http://www.cerimes.education.fr
edutice-00000362
https://edutice.archives-ouvertes.fr/edutice-00000362
https://edutice.archives-ouvertes.fr/edutice-00000362/document
https://edutice.archives-ouvertes.fr/edutice-00000362/file/actes.pdf

Éditeur(s) : HAL CCSD Springer Verlag
Résumé : International audience
We report new textural and chemical data for 10 garnet peridotite xenoliths from the Udachnaya kimberlite and examine them together with recent data on another 21 xenoliths from the 80-220 km depth range. The samples are very fresh (LOI near zero), modally homogeneous and large (>100 g). Some coarse-grained peridotites show incipient stages of deformation with <10 % neoblasts at grain boundaries of coarse olivine. Such microstructures can only be recognized in very fresh rocks, because fine-grained interstitial olivine is strongly affected by alteration, and may have been overlooked in previous studies of altered peridotite xenoliths in the Siberian and other cratons. Some of the garnet peridotites are similar in composition to low-opx Udachnaya spinel harzburgites (previously interpreted as pristine melt extraction residues), but the majority show post-melting enrichments in Fe and Ti. The least metasomatized coarse peridotites were formed by 30-38 % of polybaric fractional melting between 7 and 4 GPa and ≤1-3 GPa. Our data together with experimental results suggest that garnet in these rocks, as well as in some other cratonic peridotites elsewhere, may be a residual mineral, which has survived partial melting together with olivine and opx. Many coarse and all deformed garnet peridotites from Udachnaya underwent modal metasomatism through interaction of the melting residues with Fe-, Al-, Si-, Ti-, REE-rich melts, which precipitated cpx, less commonly additional garnet. The xenoliths define a complex geotherm probably affected by thermal perturbations shortly before the intrusion of the host kimberlite magmas. The deformation in the lower lithosphere may be linked to metasomatism.
ISSN: 0010-7999

hal-00941252
https://hal.archives-ouvertes.fr/hal-00941252
DOI : 10.1007/s00410-013-0855-8

Éditeur(s) : Elsevier Science Bv
Résumé : Shrimp aquaculture in New Caledonia is subject to seasonal mortalities during grow-out due to highly virulent Vibrio nigripulchritudo (Vn). To understand the mechanisms affecting shrimp resistance and leading to significant mortality, a shrimp ecophysiology and immunology survey was conducted on two farms, the first considered as a "control" farm (HC), the second affected by the disease (DF). Mortality observed during the survey at DF started 50 days after stocking and was typical of this disease. The main observations regarding shrimp were: (a) growth was not affected by the disease and was faster in the DF than in the HC pond; (b) disease did not affect one sex more than the other, or a specific part of the population in terms of weight; (c) the physical condition of shrimp did not specifically allow us to foresee disease outbreak; (d) shrimp at late premolt stage D-2 and early postmolt stage A appeared to be at some points of the mortalities - but not continuously - the most sensitive to disease; (e) physiological, immunological and nutritional parameters of uninfected shrimp in the DF pond were altered, suggesting that environmental stress occurred just before the first mortalities; (f) data suggest that Vn-infected shrimp are more stressed than the presumed healthy shrimp. Combined with pathological and environmental knowledge gained in parallel during this survey, a conceptual model is proposed. Results suggest that an unstable environment induced conditions (i) stressful for the shrimp, increasing their susceptibility to bacterial infections and (ii) favoring the proliferation of the pathogen in the pond. The combination of these two processes could lead to significant mortality.
Aquaculture (0044-8486) (Elsevier Science Bv), 2013-04 , Vol. 388 , P. 105-114

Droits : 2013 Elsevier B.V. All rights reserved.
http://archimer.ifremer.fr/doc/00176/28764/27567.pdf
DOI:10.1016/j.aquaculture.2013.01.010
http://archimer.ifremer.fr/doc/00176/28764/

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Subcutaneous fat tissues from an indigenous fat-type breed and an intensively-lean selected breed were studied in juvenile pigs. Combining DIGE with bioinformatics and target analyses of key genes, enzymes or terminal routes, this study identifies metabolic and homeostatic processes, response to organic substances, and acute-phase responses as the main pathways whose proteins were regulated in association with adiposity. Breed-related differences in abundance and activities of malic enzyme and glucose-6-phosphate dehydrogenase NADPH-supplying enzymes suggested up-regulation of the lipogenic pathway to dispose for a greater adiposity. Over-abundance in the lipolytic protein carboxylesterase-1 was revealed in fat-type piglets. A panel of pro- and anti-inflammatory proteins such as serpins, had an altered abundance in the fat-type piglets, suggesting adverse consequences of fat accumulation even in early post-weaning stages. Propensity to low-grade inflammation in fat pigs was reinforced by the up-regulation of genes encoding pro-inflammatory cytokines IL6 and TNF-α in these piglets. Differential abundance in annexin-A5 and pericentrin suggested a positive regulation of cell apoptosis in lean piglets. Our results are relevant in the context of data linking the accretion of body lipids to the physiology and pathology of adipose tissue in models other than rodents for a better control of human health and nutrition.
ISSN: 1874-3919

hal-01122161
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01122161
PUBMED : 22061664
DOI : 10.1016/j.jprot.2011.10.012

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The replenishment and persistence of marine species is contingent on dispersing larvae locating suitable habitatand surviving to a reproductive stage. Pelagic larvae rely on environmental cues to make behavioural decisionswith chemical information being important for habitat selection at settlement. We explored the sensory worldof crustaceans and fishes focusing on the impact anthropogenic alterations (ocean acidification, red soil, pesti-cide) have on conspecific chemical signals used by larvae for habitat selection. Crustacean (Stenopus hispidus)and fish (Chromis viridis) larvae recognized their conspecifics via chemical signals under control conditions. Inthe presence of acidified water, red soil or pesticide, the ability of larvae to chemically recognize conspecificcues was altered. Our study highlights that recruitment potential on coral reefs may decrease due to anthropo-genic stressors. If so, populations of fishes and crustaceans will continue their rapid decline; larval recruitmentwill not replace and sustain the adult populations on degraded reefs
ISSN: 0025-326X

hal-01491052
https://hal-univ-perp.archives-ouvertes.fr/hal-01491052
DOI : 10.1016/j.marpolbul.2016.08.083

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : La question que pose cet article est : comment un individu cosmopolite, à partir du geste réflexif de s’éprouver dans le regard de l’autre, peut-il saisir et se représenter son appartenance à une commune humanité ? Nous proposons que la socialisation cosmopolite soit intimement liée à la nature du groupe d’accueil dans lequel se fait l’immersion dans un ailleurs. Or, cette rencontre ne peut se faire avec l’humanité en général, mais elle prend forme dans l’interrelation entre deux ou plusieurs entités culturelles spécifiques. Ce qui nous ouvre à d’autres questions : de quelle altérité parle-t-on ? Pour qui ? Pourquoi ? Pour quoi ? De ce fait, le sentiment d’appartenance à une commune humanité, s’il est, au moins dans une certaine mesure, partagé par tout individu cosmopolite, l’est à entendre d’un point de vue utopique. Si la socialisation cosmopolite dans des enclaves backpacker ou des dispositifs d’échanges universitaires est réalisée dans une logique d’intégration principalement dirigée vers une communauté occidentale cosmopolite, une autre forme de socialisation, par l’expérience de la grande itinérance, serait ainsi possible. Cette dernière serait immergée dans les cultures locales, elle serait éphémère, aléatoire, hétérogène et principalement réalisée dans le rite des hospitalités, et peut ainsi représenter une forme différente d’élaboration du sentiment cosmopolite. En effet, celle-ci ne serait pas élaborée dans la tension entre deux modèles (intégration), mais dans une réaction en chaine de multiples modèles, qui, par sérendipités, se travaillent les unes les autres, dans de multiples directions, sans pouvoir se fixer, ouvrant ainsi à la diversité de l’humanité. S’il faut ici parler de socialisation cosmopolite, elle serait plutôt à entendre sur le plan anthropologique qu’ethnologique.
The question raised by this article is: how a cosmopolitan individual, from the reflective gesture of experiencing himself in the gaze of the other, can grasp and represent his belonging to a common humanity. We propose that cosmopolitan socialization be intimately linked to the nature of the host group in which the immersion takes place. However, this encounter cannot be made with humanity in general, but it takes shape in the interrelationship between two or more specific cultural entities. What opens us to others questions: what kind of otherness are we talking about? For whom? Why? In which purpose? As a result, the feeling of belonging to a common humanity, if it is shared, at least to some extent, by each cosmopolitan individual, is to be understood from a utopian point of view. If cosmopolitan socialization in backpacker enclaves or academic exchanges is carried out in the logic of integration mainly directed towards a cosmopolitan Western community, then another form of socialization through the experience of itinerancy would be possible. The latter would be immersed in local cultures, it would be ephemeral, random and heterogeneous and mainly carried out in the rite of hospitalities, and may thus represent a different form of elaboration of cosmopolitan feeling. Indeed, this would not be elaborated in the tension between two models (integration), but in a chain reaction of multiple models, which by serendipities, work one another, in multiple directions, without being able to stabilized, opening to the diversity of humanity. If we speak here of cosmopolitan socialization, it would rather be understood on the anthropological level than on an ethnological one.

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.11283
http://journals.openedition.org/etudescaribeennes/11283

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Les consommateurs des services touristiques, en particulier les touristes fortunés, sont aussi des consommateurs de services hôteliers de luxe. Dans le cas d’Haïti, la nouvelle orientation de l’hôtellerie haut de gamme semblerait augurer un tel principe. Cependant, notre analyse montre qu’à ce stade, et pour des raisons essentiellement socio-institutionnelles, il n’est pas exact de parler d’une industrie du luxe, même s’il y a de plus en plus d’hôtels haut de gamme dans le pays.
Consumers of tourism services, especially wealthy tourists, are also consumers of luxury hotel services. In the case of Haiti, the new orientation of the upscale hotels seems to augur such a principle. However, our analysis shows that at this stage, mainly for socio-institutional reasons, it is not correct to consider the fact that there are more and more top hotels range in the country a luxury industry.
Haïti

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.7397
http://journals.openedition.org/etudescaribeennes/7397

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
In the Oman ophiolite, the horizon where the melt lens pinched during drifting away from the ocean ridge axis has been identified. Starting in the Root Zone of the Sheeted Dike Complex (RZSDC) located above this horizon, 18 Sections down to the upper gabbros unit have been mapped in great detail, in selected areas of the southern massifs of this ophiolite. They are complemented by 133 sites, located throughout the entire ophiolite, where the transition from the RZSDC to the uppermost foliated gabbros is well exposed. Altogether, half the sites and 11 cross sections display, within a few tens of meters beneath the RZSDC, a magmatic foliation which is parallel to the overlying sheeted dikes. In the other sites and cross sections, the gabbro foliation is either flat-lying or steep but not parallel to the sheeted dikes. Compared to the RZSDC isotropic ophitic gabbros where clinopyroxene is interstitial between plagioclase laths, in the topmost steeply foliated gabbros, clinopyroxene is idiomorphic, becoming rapidly granular and tabular down section by recrystallization and peripheral alteration to hornblende. Moving down from these uppermost gabbros and over one hundred meters, the steep foliation becomes stronger and the poorly recovered top gabbros grade into the recrystallized, granular gabbros of the gabbro unit. These repeated observations indicate to ascribe these gabbros to subsidence of a compacting mush from the floor of the melt lens into the underlying, main magma chamber. The topmost gabbros beneath RZSDC, which were expelled from the melt lens by drifting very soon after settling on the melt lens floor, display in plagioclase a spectacular zoning pointing to a fast cooling. Moving downwards, stronger foliation, increased compaction and recovery-recrystallization are explained by the time spent by the subsiding mush inside the magma chamber increasing by one order of magnitude (similar to 50 to 500 yr) over this vertical distance. This field-based study brings compelling field evidence supporting the former models of subsidence which were based on the assumption that the mush that settled onto the floor of the melt lens is sucked downwards during drifting of the crust away from the ridge axis.
ISSN: 0012-821X

hal-00420903
https://hal.archives-ouvertes.fr/hal-00420903
DOI : 10.1016/j.epsl.2009.04.012

Éditeur(s) : Springer
Résumé : Interannual variability of subtropical sea-surface-height (SSH) anomalies, estimated by satellite and tide-gauge data, is investigated in relation to wintertime daily North-Atlantic weather regimes. Sea-level anomalies can be viewed as proxies for the subtropical gyre intensity because of the intrinsic baroclinic structure of the circulation. Our results show that the strongest correlation between SSH and weather regimes is found with the so-called Atlantic-Ridge (AR) while no significant values are obtained for the other regimes, including those related to the North Atlantic Oscillation (NAO), known as the primary actor of the Atlantic dynamics. Wintertime AR events are characterized by anticyclonic wind anomalies off Europe leading to a northward shift of the climatological wind-stress curl. The latter affects subtropical SSH annual variability by altered Sverdrup balance and ocean Rossby wave dynamics propagating westward from the African coast towards the Caribbean. The use of a simple linear planetary geostrophic model allows to quantify those effects and confirms the primary importance of the winter season to explain the largest part of SSH interannual variability in the Atlantic subtropical gyre. Our results open new perspectives in the comprehension of North-Atlantic Ocean variability emphasizing the role of AR as a driver of interannual variability at least of comparable importance to NAO.
Climate Dynamics (0930-7575) (Springer), 2013-09 , Vol. 41 , N. 5-6 , P. 1159-1171

Droits : Springer-Verlag Berlin Heidelberg 2012
http://archimer.ifremer.fr/doc/00161/27248/25480.pdf
DOI:10.1007/s00382-012-1578-7
http://archimer.ifremer.fr/doc/00161/27248/

Éditeur(s) : HAL CCSD Springer Verlag
Résumé : International audience
Interleukin-33 (IL-33), a cytokine belonging to the IL-1 family, is crucially involved in inflammatory pathologies including liver injury and linked to various modes of cell death. However, a link between IL-33 and necroptosis or programmed necrosis in liver pathology remains elusive. We aimed to investigate the regulation of IL-33 during necroptosis-associated liver injury. The possible regulation of IL-33 during liver injury by receptor-interacting protein kinase 1 (RIPK1) and poly(ADP-ribose) polymerase 1 (PARP-1) was investigated in mice in vivo and in hepatic stellate cells in vitro. The liver immunohistopathology, flow cytometry, serum transaminase measurement, ELISA, and qPCR-based cytokine measurement were carried out. By using a chemical approach, we showed that pretreatment of mice with Necrostatin-1 (Nec-1) (inhibitor of RIPK1) and/or PJ34 (inhibitor of PARP-1) significantly protected mice against concanavalin A (ConA) liver injury (aspartate amino-transferase (AST)/alanine amino-transferase (ALT)) associated with down-regulated hepatocyte-specific IL-33 expression. In contrast, the expression level of most systemic cytokines (except for IL-6) or activation of liver immune cells was not altered by chemical inhibitors rather an increased infiltration of neutrophils in the liver. During polyinosine-polycytidylic acid (Poly(I:C))-induced acute hepatitis, liver injury and hepatocyte-specific IL-33 expression was also inhibited by PJ34 without any protective effect of PJ34 in CCl4-induced liver injury. Moreover, PJ34 down-regulated the protein expression of IL-33 in activated hepatic stellate cells by cocktail of cytokines or staurosporine in vitro. In conclusion, we evidenced that the Nec-1/PJ34 is a potent inhibitor of liver injury and Nec-1/PJ34 down-regulated hepatocyte-specific IL-33 expression in the liver in vivo or in hepatic stellate cells in vitro, suggesting IL-33 as a possible readout of necroptosis-involved liver pathologies. Necroptosis inhibitors can protect mice against liver injury induced by ConA or Poly(I:C). IL-33 expression in liver injury in vivo is inhibited by PJ34. IL-33 expression in hepatic stellate cells in vitro is inhibited by PJ34. Hepatocyte-specific IL-33 expression is down-regulated by Nec-1/PJ34 during hepatitis. IL-33 is a new marker of necroptosis-associated liver injuries.
ISSN: 0946-2716

hal-01134319
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01134319
DOI : 10.1007/s00109-015-1270-6
PUBMED : 25747661

Éditeur(s) : HAL CCSD Wiley
Résumé : International audience
In the Caribbean, Pterocarpus officinalis swamp forest, a coastal freshwater wetland, has been locally transformed by human activities into Colocasia esculenta monoculture (under the swamp forest) or pasture (where deforestation has occurred). The aim of this study was to evaluate the impact of three land uses of this tropical wetland (swamp forest, C. esculenta monoculture and pasture) on soil abiotic and biological features. We hypothesized that increasing the level of ecosystem alteration by agricultural intensification would negatively impact soil chemical characteristics, soil fauna diversity and carbon mineralization. As expected, land use significantly affected soil characteristics and changes followed the increasing intensity of land use. The ‘undisturbed system’, that is swamp forest, was characterized by a large soil organic matter content, a high level of soil moisture, a small phosphorus content and a slightly lower pH. These characteristics were correlated with a small faunal abundance and diversity and slow carbon (C) mineralization. The ‘low disturbance system’, that is C. esculenta monoculture, was the closest to swamp forest characteristics and changes between the both systems principally concerned a very slight decrease in organic matter content and very small increase in C mineralization and Coleoptera diversity. By contrast, all parameters (soil chemical characteristics, C mineralization and faunal abundance and diversity) were impacted in the most intensive land-use, pasture. Our study confirmed that agricultural practices have an influence on soil fauna and C mineralization processes in wetlands. Moreover, our study suggested that a C. esculenta traditional agroecosystem under swamp forest cover could be considered as an ‘eco-friendly’ agricultural practice.
ISSN: 0266-0032

hal-01562423
https://hal.archives-ouvertes.fr/hal-01562423
DOI : 10.1111/sum.12273