6 resultados para Ces deux-là

em Archimer: Archive de l'Institut francais de recherche pour l'exploitation de la mer


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Depuis 2008, des mortalités massives d’huîtres creuses âgées de moins d’un an sont relevées sur le littoral français dès que la température de l’eau de mer atteint le seuil de 16°C. Ces mortalités de naissains sont associées à la détection du virus OsHV-1 μVar. Des travaux de qualification zoo-sanitaire menés depuis 2010 ont montré qu’un lot de naissains issus du captage naturel sur deux était infecté par le virus bien avant l’apparition des mortalités dans le milieu naturel, mais qu’a contrario les naissains d’écloserie expertisés présentaient une fréquence plus faible de portage latent. Dans ce contexte de crise zoo-sanitaire chronique, l’objectif de notre étude consistait à obtenir une information du statut zoo-sanitaire OsHV-1 μVar des populations de naissains du captage 2013 à l’échelle national. Ce travail avait pour finalité de permettre l’identification précoce des zones de captage associées à un risque de mortalité due à l’infection par OsHV-1 μVar. La méthodologie de l’épreuve thermique de laboratoire (ETL) correspond en une période de 1 mois d’isolement des naissains à évaluer en conditions contrôlées de laboratoire. Lors de cette période la température de l’eau de mer est maintenue constante à 21°C et la mortalité est relevée tous les 10 jours. La survie finale associée à des analyses qPCR permettent de qualifier le statut sanitaire en terme de portage OsHV-1 μVar de l’échantillon (statut infecté ou non infecté). Entre février et mars 2014, vingt et un échantillons de naissains âgés de 5 à 7 mois ont été échantillonnés dans six sites du littoral français (étang de Thau, bassin d’Arcachon, pertuis Charentais, baie de Bourgneuf, baie de Vilaine et rade de Brest) pour être qualifiés par ETL au site expérimental Ifremer d’Argenton. Les résultats de la campagne 2014 de qualification zoo-sanitaire confirment qu’en période hivernale, dans le milieu naturel, des naissains de captage peuvent être infectés par OsHV-1 μVar sans développement apparent de maladies ni mortalité. En revanche en ETL, ces lots de naissains infectés par OsHV-1 μVar présentent des taux de mortalité importants. Ainsi, sur les 20 échantillons de naissains de captage étudiés, onze ont révélé des maladies en ETL avec des mortalités cumulées variant de 16 % à 80 %. Ce ratio d’un échantillon sur deux de naissains infectés par OsHV-1 μVar demeure proche de celui observé de 2010 à 2013 lors des travaux précédents qui avaient permis de définir l’ETL. les six sites étudiés ont montré des résultats contrastés. En effet, les résultats se sont révélés favorables pour l’étang de Thau et la baie de Bourgneuf et défavorables dans le cas de la rade de Brest et la Baie de Vilaine. Pour ces deux derniers sites, tous les échantillons de naissains testés ont montré de fortes mortalités pendant l’ETL. Des différences s’observent également intra-site, notamment à Marennes Oléron avec 1 échantillon sur 3 infectés par OsHV-1 μVar ou dans pour Arcachon avec 3 échantillons sur 5. Dans le contexte préoccupant de l’épizootie actuelle, nos résultats confirment que certains lots de naissains de captage sont infectés par OsHV-1 μVar dès les mois de février-mars et pourrait être des acteurs actifs dans le déclenchement annuel du processus infectieux en milieu naturel quand la température de l’eau dépasse 16°C. Par ailleurs, notre étude démontre qu’il serait possible chaque année d’obtenir une qualification sanitaire précoce des zones de captage. Cela permettrait d’améliorer la gestion des risques liés aux transferts de naissains infectés par OsHV-1 μVar dans les différents bassins de production.

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This manuscript presents three approaches : analytical, experimental and numerical, to study the behaviour of a flexible membrane tidal energy converter. This technology, developed by the EEL Energy company, is based on periodic deformations of a pre-stressed flexible structure. Energy converters, located on each side of the device, are set into motion by the wave-like motion. In the analytical model, the membrane is represented by a linear beam model at one dimension and the flow by a 3 dimensions potential fluid. The fluid forces are evaluated by the elongated body theory. Energy is dissipated all over the length of the membrane. A 20th scale experimental prototype has been designed with micro-dampers to simulate the power take-off. Trials have allowed to validate the undulating membrane energy converter concept. A numerical model has been developed. Each element of the device is represented and the energy dissipation is done by dampers element with a damping law linear to damper velocity. Comparison of the three approaches validates their ability to represent the membrane behaviour without damping. The energy dissipation applied with the analytical model is clearly different from the two other models because of the location (where the energy is dissipated) and damping law. The two others show a similar behaviour and the same order of power take off repartition but value of power take off are underestimated by the numerical model. This three approaches have allowed to put forward key-parameters on which depend the behaviour of the membrane and the parametric study highlights the complementarity and the advantage of developing three approaches in parallel to answer industrial optimization problems. To make the link between trials in flume tank and sea trials, a 1/6th prototype has been built. To do so, the change of scale was studied. The behaviour of both prototypes is compared and differences could be explained by differences of boundary conditions and confinement effects. To evaluated membrane long-term behaviour at sea, a method of ageing accelerated by temperature and fatigue tests have been carried out on prototype materials samples submerged in sea water.

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This work presents interactions between quantitative and qualitative river freshwater inputs and the shellfish farming (oyster and mussel) in the Pertuis Charentais. The quantity of freshwater (i.e. salinity) seems to have a weak influence on the shellfish farming contrarily to its quality determined by particulate and dissolved matters contained in the water. In autumn and winter, large precipitations have a "globally positive" effect amending the coastal ecosystem. Associated dissolved nutriments and the organic matter largely determine the quality of the coming spring growth for bred shellfish, itself controlling in turn the annual yield efficiencies. However, in winter their effects are postponed because of strong mineral load, low luminosity and temperature, then limiting the primary production. The spring contributions, directly linked to territorial practices, agriculture and tourism are more variable in quantity and quality from one year to another. They often correspond to high-risk inflows since numerous substances from anthropogenic watersheds can be found diluted in the coastal zone as in the Pertuis Charentais. Their impacts on in situ estuarine ecosystems are still poorly known since these substances are mainly studied and estimated in laboratory in controlled conditions. Several studies showed anthropogenic contaminations (i.e. cadmium, pesticides) could have significant direct or indirect effects on shellfish farming. For instance, the "summer" mortalities between 1990 and 2000 in the South of the Marennes-Oléron bay (MOB), that induced environmental and physiological oyster disorders, could be linked to pesticide effects, measured during consecutive years on the oyster bed of Ronce Perquis in the South of the MOB. The weak results from the spring larval rearing of the IFREMER experimental hatchery in the South of the bay, and chromosomal abnormalities measured on the stocks of wild oysters of the Pertuis could confirm a high-risk spring environment for the shellfish farming. In summer terrestrial inputs are reduced by low precipitations, anthropogenic water removals (drinking water, irrigation) and by plant evapotranspiration. Consequently certain years, a significant salinity increase in water masses of the Pertuis Charentais is observed. However, based on long-term observations, the significant interannual variability noticed in freshwater contributions constitutes one of the most important facts of these last years. When contributions are weak (i.e. 1991 and 2011), the mean annual salinity is 34.5 in the MOB. To the contrary, other years (i.e. 1977, 1981, 1983 and 1988), the mean salinity reduced to 30.5 shows the significant freshwater contributions to the bay. Elsewhere, particularly in the mediterranean region, oyster breeding water conditions characterized by high salinity values show the freshwater does not seem to be necessary for biological functions of the Pacific oyster Crassostrea gigas. Indeed, the oyster embryonic life in particular is well adapted to high salinity values as long as trophic resources are substantial and temperatures remain high. These two factors firstly condition the embryonic survival before the water salinity. Besides, in the Pertuis Charentais, wind conditions and the geographical bloodstock position rather determine the success of the larvae capture than seawater physic-chemical conditions. Finally, a misunderstanding still remains on summer freshwater contributions to the oyster larvae food supply.

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L'enjeu du sous-projet 4 «Gestion des Ressources des Pêches de Poitou-Charentes» est de fournir une information pertinente pour une gestion responsable des ressources des pêches de Poitou-Charentes garante de la durabilité de leur exploitation. Le sous-projet se focalise sur quatre espèces phares de la production halieutique régionale ainsi que sur certaines interactions estimées critiques entre les pêches régionales et d'autres activités. La coquille Saint-Jacques et le pétoncle noir constituent deux ressources majeures pour la pêche dans les pertuis Charentais. Leur importance devrait encore croître avec la limitation la pêche de la civelle envisagée dans le cadre du plan de gestion de l'anguille. Les travaux ont pour objectif le maintien de la pêche des pectinidés pour d'une part, l'adaptation de l'effort de pêche à l'état de ces ressources et d'autre part en progressant dans les capacités de contrôle de l'abondance et de la qualité de ces ressources. La sole et l'anguille sont en valeur les deux premières espèces exploitées du golfe de Gascogne. Elles ont en commun un état préoccupant justifiant des mesures européennes de gestion de leur pêche. Cette partie vise à mieux connaître la contribution des pertuis charentais à la dynamique de ces deux stocks, l'impact sur ceux-ci des diverses activités humaines régionales et aussi d'apprécier l'impact sur les pêches charentaises des mesures de conservation prises pour ces deux ressources majeures au niveau national mais aussi régional.

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The CATARINA Leg1 cruise was carried out from June 22 to July 24 2012 on board the B/O Sarmiento de Gamboa, under the scientific supervision of Aida Rios (CSIC-IIM). It included the occurrence of the OVIDE hydrological section that was performed in June 2002, 2004, 2006, 2008 and 2010, as part of the CLIVAR program (name A25) ), and under the supervision of Herlé Mercier (CNRSLPO). This section begins near Lisbon (Portugal), runs through the West European Basin and the Iceland Basin, crosses the Reykjanes Ridge (300 miles north of Charlie-Gibbs Fracture Zone, and ends at Cape Hoppe (southeast tip of Greenland). The objective of this repeated hydrological section is to monitor the variability of water mass properties and main current transports in the basin, complementing the international observation array relevant for climate studies. In addition, the Labrador Sea was partly sampled (stations 101-108) between Greenland and Newfoundland, but heavy weather conditions prevented the achievement of the section south of 53°40’N. The quality of CTD data is essential to reach the first objective of the CATARINA project, i.e. to quantify the Meridional Overturning Circulation and water mass ventilation changes and their effect on the changes in the anthropogenic carbon ocean uptake and storage capacity. The CATARINA project was mainly funded by the Spanish Ministry of Sciences and Innovation and co-funded by the Fondo Europeo de Desarrollo Regional. The hydrological OVIDE section includes 95 surface-bottom stations from coast to coast, collecting profiles of temperature, salinity, oxygen and currents, spaced by 2 to 25 Nm depending on the steepness of the topography. The position of the stations closely follows that of OVIDE 2002. In addition, 8 stations were carried out in the Labrador Sea. From the 24 bottles closed at various depth at each stations, samples of sea water are used for salinity and oxygen calibration, and for measurements of biogeochemical components that are not reported here. The data were acquired with a Seabird CTD (SBE911+) and an SBE43 for the dissolved oxygen, belonging to the Spanish UTM group. The software SBE data processing was used after decoding and cleaning the raw data. Then, the LPO matlab toolbox was used to calibrate and bin the data as it was done for the previous OVIDE cruises, using on the one hand pre and post-cruise calibration results for the pressure and temperature sensors (done at Ifremer) and on the other hand the water samples of the 24 bottles of the rosette at each station for the salinity and dissolved oxygen data. A final accuracy of 0.002°C, 0.002 psu and 0.04 ml/l (2.3 umol/kg) was obtained on final profiles of temperature, salinity and dissolved oxygen, compatible with international requirements issued from the WOCE program.

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In May, June and July 1996, samples wcre collected along one transect greatly influenced by river discharge (eastern side of the gulf), along one transect slightly influence by river discharge (western side), at one station Iocated in the mouth of the main river (River Daugava), at one station located in the center of the Gulf and at several nearshore locations of the western side. Ratios of rnolecular concentrations of in situ dissolved ioorganic nitrogen, phosphorus and silicon, as weIl as enrichment bioassays were llsed to dctcrrnine which nutrient (s) lirnited the potential biomass of phytoplankton. Both comparison of (NO.d-N02+NJ.L): P04 (DIN: DIP) values with Redfic1d's ratio and bioassay inspection led to the sarne conclusions. Phosphorus was clearly the nutrient most limiting for the potcntial biornass of test species in nitrogen- rich waters, which occurred in mid spring, in the upper layer of the southern-eastern part of the Gulf which is greatly influenced by river discharge. In late spring, with the decrease of the total DIN reserve, nitrogen and phosphorus showed an equallimiting role. In deeper layers of this area and out of the river plume (western side and central part of the gulf), nitrogen was the limiting nutrient. In summer, whcn river discharge was the lowest, a11 DIN concentrations but one ranged between 1.6 and 2.6 µM, and the whole area was nitrogen-limited for both the cyanobacterial and the algal test strains. In 74% of the samples for which nitrogen was the limiting nutrient, phosphorus was recorded to be the second potentially limiting nutrient. In contrast, silicon never appeared as limiting the growth potential of either Microcystis aeruginosa or Phaeodactylum tricornutum; phosphorus was the limiting nutrient when DIN: Si03 values were >1 (in May), but DIN: Si03 was <1 when nitrogen was limiting (June and July). The authors conclude that the recently reported decrease of silicon loading in coastal waters and its subsequent enhanced importance in pushing the outcome of species competition towards harmful species may not yet be the most important factor for the Gulf of Riga. Iron appeared for 12% of the tests in the list of nutrients limiting the potential biomass. Tentative results also indicated that a significant fraction of the nitrogen (~,4 µg-atom N 1(-1) taken up by Microcystis aeruginosa may have been in the form of dissolved organic nitrogen (DON). It is thus also suggested tentatively that more attention be paid to these nitrients during further research in the Gulf of Riga.