Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Si l’île d’Anguilla, dans le nord des Petites Antilles, est une destination secondaire en matière d’arrivées touristiques (moins de 150 000 visiteurs en 2005), il n’en reste pas moins que l’étude des conditions d’émergence du tourisme y est intéressante. Car en la matière, Anguille fait figure d’originalité au sein de son bassin géographique. En revanche, l’analyse des évolutions de la capacité d’hébergement, d’une part, puis des flux de visiteurs, d’autre part, démontre un trait commun à la plupart des îles des Petites Antilles, à savoir une certaine vulnérabilité face à des événements exogènes (catastrophes naturelles et crises géopolitiques). Cet article vise donc à faire le point sur le phénomène touristique (origine, évolution, contraintes) dans une île jusque-là peu étudiée.
Anguilla (91 square kilometres, less than 12 000 inhabitants, 143 200 tourists arrivals in 2005) is a secondary destination in the Lesser Antilles compare to Sint Maarten, Antigua or Barbados. Netherless, tourism development in Anguilla is interesting because it shows that this product is both original (choice of "small and exclusive", majority of excursionnists) and vulnerable (influence of events like cyclone Luis and Lenny in 1995 and 1999, and the terrorist attack of the 2001 september 11th).
Anguilla

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.3492
http://journals.openedition.org/etudescaribeennes/3492

Éditeur(s) : HAL CCSD
Résumé : International audience
This communication reports on a field experiment carried out on a microtidal beach in Camargue, France. The analysis is built on the initial work presented by Sous et al. (2016) on swash-groundwater dynamics. The analysis of a cross-shore network of buried pressure sensors allows to monitor the watertable dynamics over the full 2013-2014 winter season. The pressure head gradients are observed to be primarily seaward, forced by a higher level at the landward boundary. The groundwater flux is driven by the relative fluctuations of Still Water Level and inland elevations. Rain and tides have a little effect. A nearly isolated groundwater circulation is driven by wave activity below the swash zone whatever the overall watertable gradient. Estimations of beach groundwater discharge over the Gulf of Beauduc reveal the importance of beach groundwater in the exchanges between coastal aquifer and open sea.
Coastal Dynamics 2017
Helsingor, Denmark

hal-01562908
https://hal.archives-ouvertes.fr/hal-01562908

Éditeur(s) : Elsevier
Résumé : This study aimed to analyze the role river floods play in triggering gravity flows and to investigate the role of submarine canyon systems as a conduit for terrigenous material to the deep sea. Two years of measurements in the Var canyon at depths ranging from 1200 m to 2350 m indicate that six floods of the Var River triggered hyperpycnal flows, an important mechanism for transporting particulate matter to the deep-sea floor. These sediment gravity flows were characterized by a sudden increase of current velocity that lasted 8 to 22 h and by downward particle fluxes that reached up to 600 g m(-2)d(-1) of particles and 3.1 g m(-2)d(-1) in terms of organic carbon. These large inputs of sediment and organic carbon may have a significant impact on deep-sea ecosystems and carbon storage in the Mediterranean Sea.
Marine Geology (0025-3227) (Elsevier), 2009-07 , Vol. 263 , N. 1-4 , P. 1-6

Droits : 2009 Elsevier Ltd All rights reserved.
http://archimer.ifremer.fr/doc/2009/publication-6640.pdf
DOI:10.1016/j.margeo.2009.03.014
http://archimer.ifremer.fr/doc/00000/6640/

Éditeur(s) : HAL CCSD MDPI
Résumé : International audience
This work investigates the structural formation and analyses of titania membranes (TM) prepared using different vacuum exposure times for molecular weight (MW) cut-off performance and oil/water separation. Titania membranes were synthesized via a sol-gel method and coated on macroporous alumina tubes followed by exposure to a vacuum between 30 and 1200 s and then calcined at 400 °C. X-ray diffraction and nitrogen adsorption analyses showed that the crystallite size and particle size of titania increased as a function of vacuum time. All the TM membranes were mesoporous with an average pore diameter of ~3.6 nm with an anatase crystal morphology. Water, glucose, sucrose, and polyvinylpyrrolidone with 40 and 360 kDa (PVP-40 kDa and PVP-360 kDa) were used as feed solutions for MW cut-off and hexadecane solution for oil filtration investigation. The TM membranes were not able to separate glucose and sucrose, thus indicating the membrane pore sizes are larger than the kinetic diameter of sucrose of 0.9 nm, irrespective of vacuum exposure time. They also showed only moderate rejection (20%) of the smaller PVP-40 kDa, however, all the membranes were able to obtain an excellent rejection of near 100% for the larger PVP-360 kDa molecule. Furthermore, the TM membranes were tested for the separation of oil emulsions with a high concentration of oil (3000 ppm), reaching high oil rejections of more than 90% of oil. In general, the water fluxes increased with the vacuum exposure time indicating a pore structural tailoring effect. It is therefore proposed that a mechanism of pore size tailoring was formed by an interconnected network of Ti-O-Ti nanoparticles with inter-particle voids, which increased as TiO2 nanoparticle size increased as a function of vacuum exposure time, and thus reduced the water transport resistance through the TM membranes. © 2016 by the authors.
ISSN: 1996-1944

hal-01683214
https://hal.univ-antilles.fr/hal-01683214
DOI : 10.3390/ma9110938

Éditeur(s) : HAL CCSD Elsevier
Résumé : The Gulf of Aigues-Mortes (NW Mediterranean Sea) is a midshelf zone whose scale is an intermediate between the nearshore scale (0–10 m depth) and the coastal scale (including the whole continental shelf). Its hydrodynamics is investigated for the first time. ADCP, CTD and thermosalinograph data were collected during three short cruises (HYGAM; March 6–7, 20–21, April 5–6, 2005). They were scheduled approximately every 15 days to sample the gulf circulation under different weather conditions. Moreover, the cruise data were used to validate the Symphonie model, a 3D primitive equations circulation model. The circulation features displayed by in situ data were well reproduced by Symphonie. A downscaling modelling approach was implemented, the largest scale being obtained by the replay of the MFSTEP regional model of the North-Western Mediterranean Sea. The analysis, closely coupling in situ measurements and model results, provides information that would not have been obtained using data separately. The great variability of the oceanic circulation at this scale is well evidenced. Winds are the main forces, not only locally but also at a larger scale. North winds generate coherent structures interacting with the general Mediterranean circulation. The explanation of the induced currents is then not straightforward, some of them being, for example, northward. South and southeast winds reinforce the sloping surface, the latter allowing the geostrophic equilibrium with longshore currents. This study, focused on the end of winter 2004–2005, also enhances the heat fluxes from offshore to nearshore, as well as the initiation of shelf dense waters. The knowledge of the midshelf oceanic circulation is then applied to run a numerical experiment which describes both the dispersion of a fictive contaminant from a point S (at the centre of the GAM), and evaluates the risk of contamination of the beaches along the GAM shores.
ISSN: 0278-4343

hal-00196620
https://hal.archives-ouvertes.fr/hal-00196620
DOI : 10.1016/j.csr.2007.06.006

Éditeur(s) : HAL CCSD Oxford University Press (OUP)
Résumé : In this paper we present the potential of a new compact superconducting gravimeter (GWR iGrav) designed for groundwater monitoring. At first, 3 yr of continuous gravity data are evaluated and the performance of the instrument is investigated. With repeated absolute gravity measurements using a Micro-g Lacoste FG5, the calibration factor (−894.8 nm s−2 V−1) and the long-term drift of this instrument (45 nm s−2 yr−1) are estimated for the first time with a high precision and found to be respectively constant and linear for this particular iGrav. The low noise level performance is found similar to those of previous superconducting gravimeters and leads to gravity residuals coherent with local hydrology. The iGrav is located in a fully instrumented hydrogeophysical observatory on the Durzon karstic basin (Larzac plateau, south of France). Rain gauges and a flux tower (evapo-transpiration measurements) are used to evaluate the groundwater mass balance at the local scale. Water mass balance demonstrates that the karst is only capacitive: all the rainwater is temporarily stored in the matrix and fast transfers to the spring through fractures are insignificant in this area. Moreover, the upper part of the karst around the observatory appears to be representative of slow transfer of the whole catchment. Indeed, slow transfer estimated on the site fully supports the low-flow discharge at the only spring which represents all groundwater outflows from the catchment. In the last part of the paper, reservoir models are used to characterize the water transfer and storage processes. Particular highlights are done on the advantages of continuous gravity data (compared to repeated campaigns) and on the importance of local accurate meteorological data to limit misinterpretation of the gravity observations. The results are complementary with previous studies at the basin scale and show a clear potential for continuous gravity time-series assimilation in hydrological simulations, even on heterogeneous karstic systems.
ISSN: 0956-540X

hal-01526965
https://hal.archives-ouvertes.fr/hal-01526965
https://hal.archives-ouvertes.fr/hal-01526965/document
https://hal.archives-ouvertes.fr/hal-01526965/file/fores2016.pdf
DOI : 10.1093/gji/ggw396

Éditeur(s) : Springer
Résumé : While it is well known that the ocean is one of the most important component of the climate system, with a heat capacity 1,100 times greater than the atmosphere, the ocean is also the primary reservoir for freshwater transport to the atmosphere and largest component of the global water cycle. Two new satellite sensors, the ESA Soil Moisture and Ocean Salinity (SMOS) and the NASA Aquarius SAC-D missions, are now providing the first space-borne measurements of the sea surface salinity (SSS). In this paper, we present examples demonstrating how SMOS-derived SSS data are being used to better characterize key land–ocean and atmosphere–ocean interaction processes that occur within the marine hydrological cycle. In particular, SMOS with its ocean mapping capability provides observations across the world’s largest tropical ocean fresh pool regions, and we discuss from intraseasonal to interannual precipitation impacts as well as large-scale river runoff from the Amazon–Orinoco and Congo rivers and its offshore advection. Synergistic multi-satellite analyses of these new surface salinity data sets combined with sea surface temperature, dynamical height and currents from altimetry, surface wind, ocean color, rainfall estimates, and in situ observations are shown to yield new freshwater budget insight. Finally, SSS observations from the SMOS and Aquarius/SAC-D sensors are combined to examine the response of the upper ocean to tropical cyclone passage including the potential role that a freshwater-induced upper ocean barrier layer may play in modulating surface cooling and enthalpy flux in tropical cyclone track regions.
Surveys In Geophysics (0169-3298) (Springer), 2014-05 , Vol. 35 , N. 3 , P. 681-722

Droits : Springer Science+Business Media Dordrecht 2013
http://archimer.ifremer.fr/doc/00152/26334/24430.pdf
DOI:10.1007/s10712-013-9244-0
http://archimer.ifremer.fr/doc/00152/26334/

Éditeur(s) : Pergamon-elsevier Science Ltd
Résumé : We report rare earth element (REE) and neodymium (Nd) isotope data for the organic fraction of sediments collected from various depositional environments, i.e. rivers (n=25), estuaries (n=18), open-ocean settings (n=15), and cold seeps (n=12). Sedimentary Organic Matter (SOM) was extracted using a mixed hydrogen peroxide/nitric acid solution (20%-H2O2 – 0.02M-HNO3), after removal of carbonate and oxy-hydroxide phases with dilute hydrochloric acid (0.25M-HCl). A series of experimental tests indicate that extraction of sedimentary organic compounds using H202 may be complicated occasionally by partial dissolution of sulphide minerals and residual carbonates. However, this contamination is expected to be minor for REE because measured concentrations in H2O2 leachates are about two-orders of magnitude higher than in the above mentioned phases. The mean REE concentrations determined in the H2O2 leachates for samples from rivers, estuaries, coastal seas and open-ocean settings yield relatively similar levels, with ΣREE = 109 ± 86 ppm (mean ± s; n=58). The organic fractions leached from cold seep sediments display even higher concentration levels (285 ± 150 ppm; mean ± s; n=12). The H2O2 leachates for most sediments exhibit remarkably similar shale-normalized REE patterns, all characterized by a mid-REE enrichment compared to the other REE. This suggests that the distribution of REE in leached sedimentary organic phases is controlled primarily by biogeochemical processes, rather than by the composition of the source from which they derive (e.g. pore, river or sea- water). The Nd isotopic compositions for organic phases leached from river sediments are very similar to those for the corresponding detrital fractions. In contrast, the SOM extracted from marine sediments display εNd values that typically range between the εNd signatures for terrestrial organic matter (inferred from the analysis of the sedimentary detrital fractions) and marine organic matter (inferred from the analysis of local surface seawater). A notable exception is the case of organic matter (OM) fractions leached from cold seep sediment samples, which sometimes exhibit εNd values markedly different from both terrigenous and surface seawater signatures. This suggests that a significant fraction of organic compounds in these sediments may be derived from chemosynthetic processes, recycling pore water REE characterized by a distinct isotopic composition. Overall, our results confirm that organic matter probably plays an important role in the oceanic REE budget, through direct scavenging and remineralization within the water column. Both the high REE abundances and the shape of shale-normalized patterns for leached SOM also suggest that OM degradation in sub-surface marine sediments during early diagenesis could control, to a large extent, the distribution of REE in pore waters. Benthic fluxes of organic-bound REE could hence substantially contribute to the exchange processes between particulates and seawater that take place at ocean margins. Neodymium isotopes could provide useful information for tracing the origin (terrestrial versus marine) and geographical provenance of organic matter, with potential applications in paleoceanography. In particular, future studies should further investigate the potential of Nd isotopes in organic compounds preserved in sedimentary records for reconstructing past variations of surface ocean circulation.
Geochimica Et Cosmochimica Acta (0016-7037) (Pergamon-elsevier Science Ltd), 2014-09 , Vol. 140 , P. 177-198

Droits : 2014 Elsevier Ltd. All rights reserved.
http://archimer.ifremer.fr/doc/00191/30250/28682.pdf
DOI:10.1016/j.gca.2014.05.016
http://archimer.ifremer.fr/doc/00191/30250/

Éditeur(s) : Communication, ICES Conference and Meeting (CM), 2010, Nantes
Résumé : Chlordecone is a very persistent insecticide used in banana plantations of the French West Indies between 1972 and 1993. Chlordecone residues were found in inland water, in agricultural and freshwater products, and in marine organisms. This pollution has become of great concern in 2007. Therefore, a governmental action Plan was launched to better assess the pollution and to improve the consumer’s protection. Within this plan, 1048 samples from 69 different species of marine fishes and crustaceans were collected all around both the Guadeloupe and the Martinique Islands and analyzed. The results confirm the presence of chlordecone in marine organisms, with highly variable concentrations (from the detection limit to 1000 μg.kg-1). In 17.9 % of the samples, concentrations exceeded 20 μg.kg-1, the maximum acceptable level in fish according to the French regulation (Anon, 2008). Two main features of this contamination were characterized. 1) Because of the sedimentation of contaminated suspended soil particles, the sheltered bays are more exposed to chlordecone than the open coast where terrigenous flux are dispersed. 2) Species biology, particularly their lifestyle and diet, appear to influence contamination levels. Thus, the more contaminated species live in relation with sediment or are at high trophic level. These results have directly supported political decisions in order to prevent too high exposure of consumers to chlordecone. Fishing activities in sheltered bays have been forbidden for potentially highly contaminated species like benthic crustaceans and top predators. Further studies are under way to assess the importance of the trophic transport of chlordecone within the foodweb, and to evaluate the historical deposition of this insecticide in sediment and its further bioavailability.

Droits : 2010 ICES/CIEM ; Ifremer
http://archimer.ifremer.fr/doc/00014/12511/9361.pdf
http://archimer.ifremer.fr/doc/00014/12511/

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Although first-order rate constants are basic ingredients of physical chemistry, biochemistry and systems modeling, their innermost nature is derived from complex physical chemistry mechanisms. The present study suggests that equivalent conclusions can be more straightly obtained from simple statistics. The different facets of kinetic constants are first classified and clarified with respect to time and energy and the equivalences between traditional flux rate and modern probabilistic modeling are summarized. Then, a naive but rigorous approach is proposed to concretely perceive how the Arrhenius law naturally emerges from the geometric distribution. It appears that (1) the distribution in time of chemical events as well as (2) their mean frequency, are both dictated by randomness only and as such, are accurately described by time-based and spatial exponential processes respectively.
Physica A: Statistical Mechanics and its Applications

hal-00845518
https://hal-univ-rennes1.archives-ouvertes.fr/hal-00845518
https://hal-univ-rennes1.archives-ouvertes.fr/hal-00845518v2/document
ARXIV : 1307.4583
DOI : 10.1016/j.physa.2013.05.036

Éditeur(s) : Springer
Résumé : The Håkon Mosby mud volcano is a 1.5-km-diameter geological structure located on the Southwest Barents Sea slope at a water depth of 1,270 m. High-definition seabed mapping of the mud volcano has been carried out in 2003 and 2006. A comparative analysis of the bathymetry and backscatter maps produced from the two surveys shows subtle morphological changes over the entire crater of the mud volcano, interpreted to be the consequence of mud eruption events. Mud temperature measurements point to a persistently warm mud at shallow depth in the crater. This is explained by upward fluid advection, rather than conductive cooling of mud flows. The small-scale spatial variability in the temperature distribution may be related to mud outflows or changes in the fluid flow regime. Furthermore, the locations of free gas venting observed in 2006 were found to differ from those of 2003. Our observations of overall similar topographic profiles across the mud volcano in 2003 and 2006 suggest that eruption events would have been modest. Nevertheless, the data bring evidence of significant change in activity even over short time intervals of only 3 years. This may be a characteristic shared by other submarine mud volcanoes, notably those considered to be in a quiescent stage.
Geo-marine Letters (0276-0460) (Springer), 2010-06 , Vol. 30 , N. 3-4 , P. 157-167

Droits : Springer-Verlag 2010
http://archimer.ifremer.fr/doc/00004/11527/10261.pdf
DOI:10.1007/s00367-010-0193-z
http://archimer.ifremer.fr/doc/00004/11527/

Éditeur(s) : HAL CCSD
Résumé : More than 15% of Amazon forest has been converted to pastures these last decades. Some authors argued the world’s permanent pastures (30 % of total land) could potentially offset up to 4% of the global GHG emissions, having a carbon (C) storage potential equal to 0.5 Mg C.ha-1.yr-1(Schulze et al 2009). Accordingly, pastures are good candidates to increase soil uptake C in soil while ensuring a basic food production. Here we would like to assess the effects of tropical forest conversion to cattle pasture in the French Amazonia (French Guiana), by following the long-term dynamics of soil C stocks of permanent tropical pastures (Brachiaria humidicola) after deforestation from 1970. A soil inventory campaign was performed to analyse soil C and N stocks (to 1 m depth) along a pasture chronosequence of 6 months to 36 years old pastures and 4 native forest sites (total 24 sites). The annual C sequestration potential demonstrated by the chronosequence, was compared with eddy covariance flux measurements on 2 pastures and one native forest. Our study shows that old (≥ 24 years) tropical pastures resettle the recurrent C storage observed in native forest. These pastures stored between 1.8 ± 0.5 and 5.3 ± 2.1 tC ha-1 yr-1 compared with 2.6 ± 0.5 tC ha-1 yr-1 for the nearby native forest. Our finding show that old tropical pastures accumulate carbon in soil organic matter, particularly in the deep soil layers (0.2-1 m) and without loss of soil fertility. It suggests that such pastures can be exploited by farmers in the long term with appropriate practices (no fire and no overgrazing, but a mixture of grasses and legumes and a grazing rotation plan). Clearly, efforts to curb deforestation are a priority in order to preserve forest biodiversity and C stocks. But it seems now that, in a climate-smart agriculture way, the current challenge is to manage these deforested areas to maintain the productivity of agricultural ecosystems and in the same time their capacity to mitigate GES.
Building tomorrow’s research agenda and bridging the science-policy gap
Montpellier, France

hal-01204231
https://hal.archives-ouvertes.fr/hal-01204231
PRODINRA : 324147

Éditeur(s) : HAL CCSD
Résumé : International audience
Le nombre de satellites et de capteurs pour la télédétection dédiés à l'observation de la Terre ne cesse d'augmenter, permettant ainsi d'avoir une masse de données importante en particulier en matière d'images. Parallèlement, un effort permanent vise, d'une part, à améliorer l'accès à ces données et, d'autre part, à développer d'avantages d'outils pour les manipuler. De tels efforts sont particulièrement utiles dans des contextes socio-environnementaux très dynamiques spatialement et temporellement, pour lesquels il est nécessaire de suivre et de prédire les événements environnementaux et sociétaux. En revanche, en présence d'un tel flux de données, nous avons besoin de méthodes automatiques d'interprétation d'images. Une solution envisageable pour répondre à ce besoin est de bénéficier des atouts de l'intelligence artificielle pour l'obtention de cartes d'occupation du sol issues d'une classification des régions des images. Afin de contribuer à l'automatisation de la classification, nous proposons une méthode d'induction de règles interprétables par des non-experts et mettant en évidence, explicitement, des connaissances structurelles. Cette méthode s'appuie sur la programmation logique inductive (PLI) et en particulier sur le système inductif ”Aleph”. L'application de la méthode de classification Multi-class Rule Set Intersection (MRSI) permet ensuite de classifier tout nouvel objet au regard des ses caractéristiques intrinsèques et de celles des objets environnants. Nous avons appliqué notre méthodologie à l'étude de la dynamique du littoral de la Guyane Française. Suite à ce travail, nous avons induit 136 règles de classification pour 38 classes d'occupation du sol. Ces règles sont intelligibles et simples à interpréter de par l'utilisation de la logique du premier ordre. Les performances du système ont été évaluées par la validation croisée. En moyenne, la précision, la spécificité et la sensibilité sont, respectivement, égales à 84,62%, 99,57% et 77,22%. Ces résultats quantitatifs montrent une bonne performance de la méthodologie pour la mise à jour automatique de cartes d'occupation du sol et/ou l'assistance aux opérateurs utilisant l'analyse d'image orientée-objet.
11èmes Rencontres des Jeunes Chercheurs en Intelligence Artificielle
Lille, France

hal-01376400
https://hal.archives-ouvertes.fr/hal-01376400
https://hal.archives-ouvertes.fr/hal-01376400/document
https://hal.archives-ouvertes.fr/hal-01376400/file/Bayoudh_RJCIA2013.pdf

Éditeur(s) : HAL CCSD Elsevier
Résumé : We present new analytical data from lavas and associated rocks dredged and/or drilled from the South Fiji Basin, Northland Plateau, Colville Ridge and Havre Trough. These results provide much-needed ground truth about the geology, age and tectonic evolution of the Cenozoic submarine ridges and basins between the active intraoceanic Tonga–Kermadec arc, and rifted continental borderlands of New Zealand, the Norfolk Ridge and New Caledonia. Key results from this study include: (1) Ar–Ar dates on Minerva Abyssal Plain oceanic crust suggest that the ages of magnetic anomalies in the South Fiji Basin have been overestimated by earlier workers; (2) subduction-related lavas are widespread across the region, are not presently organised into arc-like chains, and cluster in the age range 22–18 Ma (Early Miocene); (3) the oldest subduction-related lavas occur in the western part of the region (32–26 Ma: Norfolk and Three Kings Ridge); (4) shoshonites, interpreted as rifted arc lavas, were erupted in a narrow 20–21 Ma interval over a wide area. Put together, these results indicate high magmatic flux and large and rapid horizontal tectonic translations and basin opening from 18–23 Ma in the region immediately north of New Zealand. We explain the Miocene tectonomagmatic development of the region by a model of rapid rollback of a single, east-facing Pacific arc–trench system that became established after Northland Allochthon emplacement. Critical testing of this, versus other, tectonic models must await drilling and dating of thus-far unsampled Kupe Abyssal Plain crust.
ISSN: 0025-3227

hal-00405803
https://hal.archives-ouvertes.fr/hal-00405803
DOI : 10.1016/j.margeo.2006.10.033

Résumé : Penaeus stylirostris shrimp imported from Hawaii for a genetic program and kept at the Saint-Vincent research facility had progressively developed a high sensitivity to IHHNV, the etiological agent of the Infectious, Hypodermic, and Hematopoietic Necrosis. Fears were that the virus could not only be transferred to their offspring, but also that the New Caledonian strain of Penaeus stylirostris, so far considered as resistant, could become sensitive by an off balance of its hosts/pathogen equilibrium. In October 2008, a joint decision between Uprac (shimp owner), Davar (New Caledonian Animal Health Authority) and Ifremer (scientific partner) was taken to terminate all pure breed and hybrid Hawaiian populations remaining in the ponds, and to implement an intensive fallowing protocol, and controlled restocking. IHHNV was also suspected to trouble experiments carried out in the research facility (mortalities, deformities, slow growth), thus affecting research programs. Difficulties pointed out by IHHNV have triggered since 2008 some awareness on biosecurity issues at some level of the New Caledonian shrimp industry. At the St-Vincent research station, it led to a risk assessment and implementation of biosecurity procedures (fallowing, propagation, grow out and use of screened animals) which minimizes the risk of expression of IHHNV. The use of a brand new hatchery building on site also helped in resetting routine hygiene procedures during production and in controlling incoming and outgoing items (shrimp, water, feed, personnel, equipment, pests and wastes). IHHNV has not been detected on analysed samples since then nor have any symptoms been found during experimental or broodstock growout. Keeping this control alive is considered as a useful tool to lower the risk of potential health threats, to get a better understanding in case of an outbreak, and to increase the reliability of experimental results.
Les crevettes originaires d’Hawaii et conservées au LEAD St-Vincent, dans le cadre du programme d’introduction de variabilité génétique dans le cheptel Calédonien, ont progressivement montré une sensibilité importante au virus IHHNV, agent de la Nécrose Hypodermale et Hématopoïétique Infectieuse (mortalité, croissance ralentie, déformations). Les risques d’une transmission génétique de cette sensibilité à leur descendance à moyen terme, et de son développement par rupture de l’équilibre hôte/pathogène sur la souche dite « Calédonienne » jusqu’alors considérée comme résistante à l’IHHN, ont conduit à partir d’octobre 2008, avec l’accord et l’appui de l’UPRAC et de la DAVAR, à la suppression des animaux hawaiiens ou hybrides encore présents dans les bassins de terre du LEAD St-Vincent, au vide sanitaire de ces derniers, et au repeuplement contrôlé du site. D’autre part, le virus IHHN est soupçonné d’avoir pu affecter les animaux utilisés dans les expérimentations menées au LEAD-St-Vincent (mortalités, déformations, croissance réduite), influençant donc potentiellement leur bon déroulement et celui des programmes de recherches. Les obstacles soulevés par l’expression du virus IHHN ont donc initié depuis 2008 une prise de conscience et la mise en place de démarches de biosécurité dans certains points de la filière. A la station de St-Vincent, cette démarche s’est traduite par une identification/évaluation des risques et l’application de mesures (vide sanitaire, reproduction, élevage et utilisation des animaux contrôlés) chacune dotée de procédures qui regroupées, minimisent le risque d’introduction et de dissémination de l’IHHNV. La prise en main de la nouvelle structure d’écloserie sur le site de la SASV a également été mise à profit pour revoir les procédures d’hygiène de routine dans la conduite des productions et dans le contrôle des flux intrants et sortants (animaux, eau, aliments, personnel, équipement, nuisibles, déchets). Aucune détection d’IHHNV sur les échantillons prélevés n’a depuis été observée, de même qu’aucun symptôme de l’expression de cette maladie sur les animaux en élevage sur le site de Saint-Vincent. La poursuite de ces mesures est envisagée comme un outil d’aide à la minimisation des problèmes potentiels, à leur compréhension en cas d’apparition, et à la fiabilisation des résultats.

Droits : 2010 Ifremer
http://archimer.ifremer.fr/doc/00118/22949/20776.pdf
http://archimer.ifremer.fr/doc/00118/22949/

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Le lien entre migration et Antilles françaises est souvent traité en termes d’émigration insulaire vers l’Hexagone. En effet, les flux les plus nombreux correspondent encore à ce mouvement centripète qui s’explique par une situation sociale tendue du fait de l’inadaptation entre l’offre de travail et les jeunes adultes en trop grand nombre. Pourtant les mobilités venant de Métropole existent avec le retour des Antillais au pays. Les Antilles attirent aussi les Métropolitains. La tertiairisation de l’économie, les investissements des grandes sociétés françaises ainsi que les dernières lois de défiscalisation ou celles concernant la création d’entreprises semblent favorisent le mouvement. L’article se propose d’analyser les moteurs de ces nouvelles formes de circulation migratoire entre la France métropolitaine et la Martinique, ainsi que l’insertion économique et les territorialités spécifiques des nouveaux acteurs.
The migration-West Indies nexus is often dealt with in terms of insular emigration towards Metropolitan France. Indeed, most of the flows are still characterised by a centripetal move that can be accounted for by the hiatus between job supply and the demographic importance of the youth. Nonetheless, Metropolitan-origin mobility exist with West Indian return migration as well as Metropolitan French migration. The boom of the service economy, investments from large French firms and recent advantageous fiscal laws favour this pattern. The article seeks to analyse the new driving forces behind the circular movement between Metropolitan France and Martinique, as well as the economic insertion and the specific territorialities of the new actors.

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.932
http://journals.openedition.org/etudescaribeennes/932

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Loin d’être un phénomène nouveau, les mobilités internationales se sont fortement accrues depuis les années 1960. Aujourd’hui, le contexte de mondialisation tend à accélérer les dynamiques migratoires alors que dans le même temps s’observe une élévation des niveaux d’éducation. Ainsi, la soutenabilité de l’augmentation de la fuite des cerveaux dans le monde soulève interrogations et réflexions.Le poids des flux de migrants qualifiés allié à la fragilité relative des données, pose la nécessité d’aborder en profondeur le problème de la fuite des cerveaux. Une analyse au cas par cas s’impose. À partir de données se rapportant à la diaspora caribéenne sur la base statistique de Docquier et Marfouk, cet article propose une réflexion sur les facteurs explicatifs de la fuite des cerveaux dans les territoires insulaires caribéens.
Far from being a new phenomenon, the international motilities have increased since the 60’s. Today, the context of globalization tends to accelerate the migratory dynamics while at the same time observed a rise of the educational levels. The increase of the brain drain has respite to many questions.Nevertheless, image, nature of flows of skilled migrants combined with relative data’s fragility and the necessity to approach the problem and presenting appropriate policies, impose an analysis case by case. Using data relating to the Caribbean diaspora on the statistical basis of Docquier and Marfouk, this article purpose a reflection on the factors that explain the brain drain in the Caribbean islands.
Caraïbes

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.4702
http://journals.openedition.org/etudescaribeennes/4702

Résumé : La thèse est consacrée à la recherche des catastrophes marines (tsunamis, ondes de tempête) dans les Antilles françaises, en utilisant des modèles analytiques et numériques de mécanique des fluides. L'accent est mis sur le développement de modèles de mouvement de glissements de terrain et des vagues causées par ces glissements. Le modèle le plus simple du glissement de terrain «solide block» est utilisé pour évaluer les caractéristiques des flux pyroclastiques du volcan Soufrière-Hills (Montserrat). Un modèle plus complexe de modélisation de glissement de terrain (modèle de Savage-Hutter) a été étudié analytiquement, donnant ainsi une nouvelle famille de solutions exactes décrivant le mouvement de l'écoulement par gravité non linéaire dans une vallée ou dans un canyon sous-marin. Le modèle comprend des ondes simples (Riemann waves),le cas d'un barrage qui cède (dam-break problem), des solutions auto-similaires dans la M-fonne et « chapeaux paraboliques ». Grâce à la théorie linéaire de l'eau peu profonde nous avons étudié le processus de génération de tsunamis par des glissements de terrain de volume variable, se déplaçant à une vitesse variable dans un bassin de profondeur variable. Dans le cas d'un fond marin particulier (cas sans "réflexion"), les phénomènes de résonnance ont été étudiés dans un bassin à profondeur variable. Nous avons utilisé des méthodes numériques pour la résolution non-linéaire des équations des eaux peu profondes afin d'analyser des catastrophes marines réelles (les ondes de tempête causées par le cyclone Lili en 2002, le tsunami volcanique de 2003 à Montserrat) et probables (un tsunami prés des côtes de la Martinique). Des données sur les catastrophes
The dissertation is devoted to research in the field of marine natural hazards (tsunamis, storm surges) in the French West Indies, using analytical and numerical models of fluid mechanics. Emphasis is placed on the development of models of landslide motion and generated tsunami waves. The simple "solid block" model is used to evaluate the characteristics of pyroclastic flow Soufriere Hills volcano (Montserrat). The "fluid model" of a landslide (so called Savage-Hutter model) is studied analytically; within this model a new family of exact solutions that describe the motion of nonlinear gravity flow in a valley or underwater canyon is found: nonlinear Riemann wave, dan break problem, self-similar solutions (M - wave and parabolic cap). In the framework of the linear shallow water theory the process of generation of tsunami waves by landslides of variable volume moving with variable velocity above the basin of variable depth is studied. For the specific bottom profile ("reflectionless" one) the resonant phenomena is investigated in the basin of variable depth. Numerical methods are used to analyze marine hazards: historical (storm surges, caused by Cyclone LILI in 2002; volcanic tsunami 2003 on Montserrat) and possible events (possible tsunami of the coast of Martinique). Various data on marine natural disasters are obtained during field surveys (volcanic tsunami in 2003, stonn surges caused by Hurricane Dean in 2007). Designed catalogs of tsunamis and storm surges are created based on results of numerical modeling and field studies; some statistical analysis is perfomed

http://www.theses.fr/2011AGUY0435/document

Résumé : Les méthodes classiques d'analyse d'images satellites sont inadaptées au volume actuel du flux de données. L'automatisation de l'interprétation de ces images devient donc cruciale pour l'analyse et la gestion des phénomènes observables par satellite et évoluant dans le temps et l'espace. Ce travail vise à automatiser la cartographie dynamique de l'occupation du sol à partir d'images satellites, par des mécanismes expressifs, facilement interprétables en prenant en compte les aspects structurels de l'information géographique. Il s'inscrit dans le cadre de l'analyse d'images basée objet. Ainsi, un paramétrage supervisé d'un algorithme de segmentation d'images est proposé. Dans un deuxième temps, une méthode de classification supervisée d'objets géographiques est présentée combinant apprentissage automatique par programmation logique inductive et classement par l'approche multi-class rule set intersection. Ces approches sont appliquées à la cartographie de la bande côtière Guyanaise. Les résultats démontrent la faisabilité du paramétrage de la segmentation, mais également sa variabilité en fonction des classes de la carte de référence et des données d'entrée. Les résultats de la classification supervisée montrent qu'il est possible d'induire des règles de classification expressives, véhiculant des informations cohérentes et structurelles dans un contexte applicatif donnée et conduisant à des valeurs satisfaisantes de précision et de KAPPA (respectivement 84,6% et 0,7). Ce travail de thèse contribue ainsi à l'automatisation de la cartographie dynamique à partir d'images de télédétection et propose des perspectives originales et prometteuses.
Classical methods for satellite image analysis are inadequate for the current bulky data flow. Thus, automate the interpretation of such images becomes crucial for the analysis and management of phenomena changing in time and space, observable by satellite. Thus, this work aims at automating land cover cartography from satellite images, by expressive and easily interpretable mechanism, and by explicitly taking into account structural aspects of geographic information. It is part of the object-based image analysis framework, and assumes that it is possible to extract useful contextual knowledge from maps. Thus, a supervised parameterization methods of a segmentation algorithm is proposed. Secondly, a supervised classification of geographical objects is presented. It combines machine learning by inductive logic programming and the multi-class rule set intersection approach. These approaches are applied to the French Guiana coastline cartography. The results demonstrate the feasibility of the segmentation parameterization, but also its variability as a function of the reference map classes and of the input data. Yet, methodological developments allow to consider an operational implementation of such an approach. The results of the object supervised classification show that it is possible to induce expressive classification rules that convey consistent and structural information in a given application context and lead to reliable predictions, with overall accuracy and Kappa values equal to, respectively, 84,6% and 0,7. In conclusion, this work contributes to the automation of the dynamic cartography from remotely sensed images and proposes original and promising perpectives

http://www.theses.fr/2013AGUY0671/document

Résumé : La problématique migratoire dans l’ultrapériphérie de l’Union européenne constitue un angle d’approche peu commun dans les études européennes. Espace de réflexion et de concertation qui cherche constamment à s’affirmer, l’ultrapériphérie européenne s’est, pour la première fois de son existence, penchée sur la thématique des flux migratoires. L’intérêt de cette situation sans précédent s’est confirmé lorsque la Commission européenne a officiellement décidé à travers sa communication du 12 septembre 2007 [COM(2007)507] intitulée « Stratégie pour les régions ultrapériphériques : bilan et perspectives », de prêter attention à la situation des régions ultrapériphériques (RUP) face au phénomène d’immigration. Si la plupart des travaux en la matière concernent les espaces nationaux ou transnationaux, rares sont ceux qui traitent d’un espace transrégional aussi éclaté géographiquement et dans sa composition juridico-institutionnelle.L’objet de la thèse porte ainsi sur la problématisation migratoire dans l’ultrapériphérie et l’étude de la fenêtre d’opportunité déclenchée par la communication de 2007. Ce qu’il s’agit d’observer, ce sont les conséquences de cette inscription à l’agenda européen pour l’espace ultrapériphérique sur cette thématique, à savoir la forme d’un processus d’élaboration d’un référentiel européen ultrapériphérique. Pour cela, il est nécessaire de comprendre les paramètres nationaux, régionaux, européens et ultrapériphériques qui englobent cet évènement.Cette étude de politiques publiques prend pour point de départ la notion d’européanisation définie de façon interactionnelle, et débouche sur un cadre théorique basé sur la Théorie du choix rationnel et l’Approche cognitive et normative. A l’aide de la méthode comparative, elle tente de confronter deux régions ultrapériphériques sélectionnées à cet effet : une région française, la Guadeloupe, et une région espagnole, les Iles Canaries. Deux archipels aux réalités juridiques, politiques et sociales différentes, ayant manifesté une inquiétude au sujet du phénomène d’immigration sur leur territoire dans la période précédant la prise en charge de 2007.L’analyse a mis en avant l’enchevêtrement de niveaux d’action publique assez complexe auquel sont confrontées ces régions. La diversité au sein de l’ultrapériphérie complique l’élaboration de bases communes au sujet de la question migratoire. Un processus d’européanisation directe dans l’ultrapériphérie a bien été lancé en 2007, mais reste à développer.L’objectif de la thèse est donc d’apporter des réponses aux difficultés observées, en menant une analyse assez précise de l’évènement de 2007. La démarche s’effectue en deux temps. D’une part, une analyse des paramètres internes (nationaux et régionaux) pouvant conditionner le processus étudié. D’autre part, un décryptage des racines conceptuelles et des premières observations de terrain pour comprendre la teneur du processus.
TraductionDésactiver la traduction instantanéeMigration into the outermost regions of the European Union is an angle unusual approach in European studies. Space for reflection and dialogue that constantly seeks to assert, Outermost Europe has for the first time in its existence, addressed the theme of migration. The advantage of this unprecedented situation is confirmed when the European Commission formally decided through its communication of 12 September 2007 [COM (2007) 507] entitled "Strategy for the outermost regions: achievements and perspectives", pay attention the situation of the outermost regions (OR) face to the immigration phenomenon. If most of the work on the subject relate to national or transnational, few areas are those that deal with cross-regional space also broke geographically and in its legal and institutionnelle.L'objet composition of the thesis and deals with migration in problematisation outermost regions and the study of the window of opportunity triggered by the communication of 2007. what is observed, it is the consequences of this inscription on the European agenda for the outermost space on this theme , namely as a process of developing a European outermost repository. For this it is necessary to understand the national parameters, regional, European and outermost encompassing évènement.Cette this policy study takes as its starting point the notion of Europeanization set of interactional way, and results in a theoretical framework based on Theory of rational choice and cognitive and normative approach. Using the comparative method, she tries to confront two outermost regions selected for this purpose: a French region, Guadeloupe, and one in Spain, the Canary Islands. Two archipelagos legal realities, different political and social, have expressed a concern about the phenomenon of immigration on their territory in the period preceding the care 2007.L'analyse highlighted the tangle of levels rather complex prosecution faced by these regions. The diversity of the outermost regions complicates the common foundations for development on the migration issue. A direct Europeanization process in the outermost regions has been launched in 2007, but remains développer.L'objectif of the thesis is to provide answers to the difficulties observed, leading a fairly accurate analysis of the event 2007. The process is carried out in two stages. On the one hand, an analysis of internal parameters (national and regional) that can condition the studied process. On the other hand, a decryption conceptual roots and the first field observations to understand the content of the process

http://www.theses.fr/2015AGUY0826/document