Éditeur(s) : CRPLC : Centre de Recherche sur les Pouvoirs Locaux dans la Caraïbe
Extrait de : "Les entités infra-étatiques et les organisations de coopération et d'intégration régionales" : colloque international, les 25 et 26 mars 2013. Université des Antilles et de la Guyane
Description : Après avoir fait rapidement état de la situation des entités infra-étatiques au sein des organisations européennes, Isabelle Vestris axe son intervention autour de trois questionnements centraux. Elle s'interroge sur la façon dont l'Union Européenne et le Conseil de l'Europe ont appréhendé la diversité des entités infra-étatiques. Il est également question de voir comment se traduit concrètement la prise en compte de ces entités au sein de ces organisations. Il est enfin question de se demander dans quelles mesures l'appréhension de la diversité de ces entités contribue-t-elle à enrichir le droit de ces organisations régionales.
Siècle(s) traité(s) : 21
Droits : CC-BY-NC-ND - Attribution - Pas d'utilisation commerciale - Pas de modification
Permalien : http://www.manioc.org/fichiers/V13122
V13122

Résumé : It is about an article presenting the institute, its history, its presence and the projects it leads in New Caledonia. After a first part of general presentation of Ifremer a focus is placed on the strengthening of the presence of the institute in New Caledonia. 3 points are developed by L. Loubersac on the in-house organization, the strategy and examples of works realized within the framework of the buildind up of the lagoons integrated project. Then a spotlight is offered toward 3 projects: DEDUCTION 2 which aims at optimizing the performances of the shrimp aquaculture sector (T. Laugier), AMICAL which focuses on micro-algae aquaculture (L. Chim) and AMBIO centred on the monitoring and the definition of performance indicators for management of Marine Protected Areas and zones Registered on the World heritage (D. Pelletier). The synthesis of this article is realized by S. Chopot of the New Caledonia environment magazine.
Il s’agit d’un article présentant l’institut, son historique, sa présence et les projets qu’il mène en Nouvelle-Calédonie. Après une première partie de présentation générale de l’organisme un focus est placé sur le renforcement de la présence de l’Ifremer en Nouvelle-Calédonie. 3 questions sont posées à L. Loubersac sur l’organisation en interne, la stratégie et des exemples de travaux réalisés dans le cadre du chantier lagons. Puis un coup de projecteur est porté sur 3 projets : Déduction 2 qui vise à optimiser les performances de la filière crevetticole (T. Laugier), AMICAL qui se focalise sur la culture de micro-algues (L. Chim) et AMBIO axé sur le suivi et la définition d’indicateurs de performance des modes de gestion des Aires Marines protégées et des zones Inscrites au Patrimoine Mondial (D. Pelletier). La synthèse de cet article est réalisée par S. Chopot de la revue Environnement Nouvelle-Calédonie.
Environnement Nouvelle-Calédonie, 2013-05 , N. 20 , P. 60-89

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/00200/31093/29501.pdf
http://archimer.ifremer.fr/doc/00200/31093/

Éditeur(s) : HAL CCSD Wiley-Blackwell
Résumé : International audience
This paper aims to decipher the thermal evolution of the Montagne Noire Axial Zone (MNAZ,southern French Massif Central) gneiss core and its metasedimentary cover through determination ofP–T paths and temperature gradients. Migmatitic gneiss from the core of the dome record a clock-wise evolution culminating at 725 25 °C and 0.8 0.1 GPa with partial melting, followed by adecompression path with only minor cooling to 690 25° C and 0.4 0.1 GPa. Field structuralanalyses as well as detailed petrological observations interpreted in a petrogenetic grid indicate thatthe cover sequence experienced LP-HT metamorphism at <0.4 GPa. Apparent thermal gradientswithin the cover were determined with garnet–biotite thermometry and Raman Spectroscopy on Car-bonaceous Matter. High-temperature apparent gradients (e.g. 530 °C km1 along one transect) areexplained by late brittle–ductile extensional shearing evidenced by phyllonites that post-date peakmetamorphism. In areas where normal faults are less abundant and closely spaced, gradients of 20to 50 °C km1 are calculated. These gradients can be accounted for by a combination of domeemplacement and ductile shearing (collapse of isotherms), without additional heat input. Finally, thethermal evolution of the MNAZ is typical for many gneiss domes worldwide as well as with otherLP-HT terranes in the Variscides.
ISSN: 0263-4929

Droits : http://creativecommons.org/licenses/by-nc-nd/
insu-01290388
https://hal-insu.archives-ouvertes.fr/insu-01290388
https://hal-insu.archives-ouvertes.fr/insu-01290388/document
https://hal-insu.archives-ouvertes.fr/insu-01290388/file/jmg12188.pdf
DOI : 10.1111/jmg.12188

Éditeur(s) : HAL CCSD Elsevier
Résumé : We use a triangular representation of the plunges of P, B, and Taxes to compare the different ways tectonic regime is inferred from earthquake focal mechanisms in recent works. We argue that P, B, and Taxes provide a reasonable estimate of principal stress directions when faulting is close to Andersonian conditions, and that this can be estimated from the location on a triangular diagram. We analyze the geometrical relationship between the plunges of P, B, and Taxes on one hand, and the rake of slip and dip of nodal planes on the other hand. We show that the rake and dip level curves correspond to trajectories of the vertical direction along great and small circles with respect to the frame of the P, B. and Taxes. This shows that dip-slip faulting is compatible with vertical P or Taxes, but does not require it, and instead requires horizontal B axes. It also shows that strike-slip faulting does not require vertical B axes, but P and Taxes with equal plunges. This also reveals that focal mechanisms where P, B, and Taxes all have moderate plunge correspond to two very different types of nodal planes: a steeply dipping one with oblique slip and a moderately dipping one with strike-slip. Seismically active and moderately dipping strike-slip faults are to be found among these events.
ISSN: 0040-1951

hal-00486367
https://hal.archives-ouvertes.fr/hal-00486367
DOI : 10.1016/j.tecto.2009.03.006

Éditeur(s) : HAL CCSD Springer Verlag
Résumé : Vertical displacements on the SW-NE T (e) over capt fault (Eastern Pyrenees Axial Zone, France), which separates the Variscan Canigou-Caranca and Mont-Louis massifs, were constrained using a thermochronologic multi-method approach. Ar-40/Ar-39 data from the granitic Mont-Louis massif record its Variscan cooling history and reveal no ages younger than Early Cretaceous, while the Canigou-Caranca gneiss massif records systematically younger Ar-40/Ar-39 ages. These younger Ar-40/Ar-39 ages in the Canigou-Caranca gneiss massif are the result of partial to total rejuvenation of argon isotopic systems related to a thermal flow coeval with the Cretaceous HT-BP metamorphism in the North Pyrenean Zone. Only the deepest rocks from the Canigou-Caranca suffered this extensive Mid-Cretaceous thermal overprint probably due to differential burial around 4 km at that time. The post Mid-Cretaceous vertical displacements along the T (e) over capt fault are recorded by "low" temperature thermochronology using K-feldspar Ar-40/Ar-39, zircon and apatite fission track and (U-Th)/He datings. The Mont-Louis granite samples experienced a long period of protracted cooling reflecting a lack of thermo-tectonic activity in this area from Late Palaeozoic to Early Cenozoic, followed by cooling from 55-60 Ma to Late Eocene at a mean rate of 15-20 degrees C/Ma in the final stage. This cooling stage corresponds to T (e) over capt fault reactivation with a reversed component, promoting exhumation of the Mont-Louis roof zone contemporaneously with the south-vergent Pyrenean thrusting. In the Canigou-Caranca massif, the main cooling event occurred from 32 to 18 Ma at a maximum rate of 30 degrees C/Ma during Early Oligocene followed by a more moderate rate of 3 degrees C/Ma from Late Oligocene to Early Burdigalian, coeval with the normal reactivation of the T (e) over capt fault in brittle conditions that accommodated the final exhumation of the massif during the opening of the Gulf of Lion.
ISSN: 1437-3254

hal-00411442
https://hal.archives-ouvertes.fr/hal-00411442
DOI : 10.1007/s00531-007-0179-x

Éditeur(s) : HAL CCSD Oxford University Press (OUP): Policy P - Oxford Open Option A Oxford University Press (OUP)
Résumé : International audience
The Pyrenean mountain range is a slowly deforming belt with continuous and moderate seismic activity. To quantify its deformation field, we present the velocity field estimated from a GPS survey of the Pyrenees spanning 18 yr. The PotSis and ResPyr networks, including a total of 85 GPS sites, were installed and first measured in 1992 and 1995–1997, respectively, and remeasured in 2008 and 2010. We obtain a deformation field with velocities less than 1 mm yr−1 across the range. The estimated velocities for individual stations do not differ significantly from zero with 95 per cent confidence. Even so, we estimate a maximum extensional horizontal strain rate of 2.0 ± 1.7 nanostrain per year in a N–S direction in the western part of the range. We do not interpret the vertical displacements due to their large uncertainties. In order to compare the horizontal strain rates with the seismic activity, we analyse a set of 194 focal mechanisms using three methods: (i) the ‘r’ factor relating their P and T axes, (ii) the stress tensors obtained by fault slip inversion and (iii) the strain-rate tensors. Stress and strain-rate tensors are estimated for: (i) the whole data set, (ii) the eastern and western parts of the range separately, and (iii) eight zones, which are defined based on the seismicity and the tectonic patterns of the Pyrenees. Each of these analyses reveals a lateral variation of the deformation style from compression and extension in the east to extension and strike-slip in the west of the range. Although the horizontal components of the strain-rate tensors estimated from the seismic data are slightly smaller in magnitude than those computed from the GPS velocity field, they are consistent within the 2σ uncertainties. Furthermore, the orientations of their principal axes agree with the mapped active faults.
ISSN: 0956-540X

hal-01171752
https://hal.archives-ouvertes.fr/hal-01171752
DOI : 10.1093/gji/ggv052

Éditeur(s) : HAL CCSD Wiley-Blackwell
Résumé : International audience
Garnet growth in high-pressure, mafic garnet granulites formed by dehydration melting of hornblende-gabbronorite protoliths in the Jijal complex (Kohistan palaeo-island arc complex, north Pakistan) was investigated through a microstructural EBSD-SEM and HRTEM study. Composite samples preserve a sharp transition in which the low-pressure precursor is replaced by garnet through a millimetre-sized reaction front. A magmatic foliation in the gabbronorite is defined by mafic-rich layering, with an associated magmatic lineation defined by the shape-preferred orientation (SPO) of mafic clusters composed of orthopyroxene (Opx), clinopyroxene (Cpx), amphibole (Amp) and oxides. The shape of the reaction front is convoluted and oblique to the magmatic layering. Opx, Amp and, to a lesser extent, Cpx show a strong lattice-preferred orientation (LPO) characterized by an alignment of [001] axes parallel to the magmatic lineation in the precursor hornblende-gabbronorite. Product garnet (Grt) also displays a strong LPO. Two of the four < 111 > axes are within the magmatic foliation plane and the density maximum is subparallel to the precursor magmatic lineation. The crystallographic relationship < 111 >(Grt)//[001](Opx,Cpx,Amp) deduced from the LPO was confirmed by TEM observations. The sharp and discontinuous modal and compositional variations observed at the reaction front attest to the kinetic inhibition of prograde solid-state reactions predicted by equilibrium-phase diagrams. The P-T field for the equilibration of Jijal garnet granulites shows that the reaction affinities are 5-10 kJ mol.(-1) for the Grt-in reaction and 0-5 kJ mol.(-1) for the Opx-out reaction. Petrographic and textural observations indicate that garnet first nucleated on amphibole at the rims of mafic clusters; this topotactic replacement resulted in a strong LPO of garnet. Once the amphibole was consumed in the reaction, the parallelism of [001] axes of the mafic-phase reactants favoured the growth of garnet crystals with similar orientations over a pyroxene substrate. These aggregates eventually sintered into single-crystal garnet. In the absence of deformation, the orientation of mafic precursor phases conditioned the nucleation site and the crystallographic orientation of garnet because of topotaxial transformation reactions and homoepitaxial growth of garnet during the formation of high-pressure, mafic garnet-granulite after low-pressure mafic protoliths.
ISSN: 0263-4929

hal-00411323
https://hal.archives-ouvertes.fr/hal-00411323
DOI : 10.1111/J.1525-1314.2008.00789.x

Éditeur(s) : HAL CCSD
Résumé : Fault zones are major discontinuities in sedimentary basins. Understanding their role on fluid migrations is an essential issue to (i) characterize the mechanisms and kinematics of deformation and (ii) to determine the parameters which control the distribution of energetic or mineral resources. This work applies to faulting under a temperature range of 200-250°C, corresponding to that of deeply buried reservoirs as well as potentially seismogenic fault zones. The studied faults are normal faults affecting the “Grès d’Annot” Formation, a Priabonian-Rupelian siliclastic turbidite succession of the Alpine foreland basin. They are located in two distinct areas: the Moutière-Restefond area in the eastern part of the basin and the Estrop area in the western part. Vitrinite reflectance outside fault zones indicates maximal temperatures of 240-260°C at Moutière-Restefond and 170-200°C at Estrop, i.e. burial depths around 8 km and 6 km, respectively, assuming a mean geothermal gradient of 30°C/km. Burial was due to underthrusting below the Embrunais-Ubaye Alpine nappes, the difference in burial between the two areas traducing the westward taper of the nappe front.The studied faults affect alternating arkosic sandstone beds and pelite layers with offsets from centimeters to decameters. Two types of core zones are recognized: (1) the foliated core zones of the Moutière-Restefond area, where deformation dominated by pressure solution and synkinematic phyllosilicate neoformation resulted in a foliated fabric, and (2) the core zones of the Estrop area, characterized by dilatant quartz-mineralized veins and breccia. Fault and host rock petrophysical properties were measured on drill plugs, using the water porosity technique and nitrogen permeability technique under 2 Mpa of confining pressure. In the Moutière-Restefond fault zones, plug axes were oriented in three orthogonal directions corresponding to the main deformation axes (X, Y, Z) of the foliated arkose to characterize the effect of structural anisotropy. In the Estrop fault zones, where deformation does not show equivalent anisotropy, the plug axes were oriented according to the main fault plane orientation (i.e., parallel to azimuth, parallel to dip and normal). In each fault zone, the porosity of fault rocks is equivalent to that of host rocks. In the Moutière-Restefond fault zones, the plugs parallel to the X and Z axes of deformation have a permeability similar to that of the host rocks, whereas permeability parallel to the Y axis (i.e. parallel to the foliation and the main fault plane) is one order of magnitude higher. By contrast, the permeability values in the Estrop fault zones are isotropic and equivalent to the host rock values. This study highlights the importance of various types of deformation mechanisms and related fluid-rock interactions in determining different fault rock types within a similar protolith, ultimately controlling distinct petrophysical properties of fault zones.
Les zones de failles constituent des discontinuités majeures dans la croûte supérieure. Ce mémoire s’intéresse aux failles actives à des profondeurs de 5-8 km, i.e. dans des conditions pouvant jouer un rôle important (i) sur le comportement mécanique de de la croûte, en particulier sur son potentiel sismogénique et (ii) sur la compartimentation des réservoirs géologiques profondément enfouis.Les failles étudiées sont des failles normales (rejet jusqu’à 50 mètres) affectant des alternances de bancs de grès arkosiques et de pélites dans les Grès d’Annot, une formation turbiditique d’âge priabonien-rupélien du bassin d’avant-chaine alpin. Les Grès d’Annot ont été enfouis sous les nappes de l’Embrunais-Ubaye peu de temps après leur dépôt et exhumés au Miocène moyen-supérieur. L’étude a été réalisée dans deux secteurs des Alpes de Haute-Provence, (1) le secteur de l’Estrop (chaine des Trois Evéchés, dans la partie occidentale du bassin) et (2) le secteur de Point Vert-Restefond (alentours du col de la Bonette, dans la partie orientale du bassin). La réflectance de la vitrinite dans les Grès d’Annot indique des températures maximales de 160-190°C dans le secteur (1) et de 240-260 °C dans le secteur (2) , soit des profondeurs d’enfouissement de 5-6 km et 8-10 km, respectivement, dans l’hypothèse d’un gradient géothermique moyen de 25-30°C/km. A partir des observations microstructurales, de données d’inclusions de fluides, de modélisations thermodynamiques sur chlorites syncinématiques et des indices de cristallinité de l’illite, on a établi que les failles du secteur (1) ont fonctionné à une température d’environ 200°C pour une pression de 0.6Kbar et celles du secteur (2) dans une gamme de température de 200-220°C et de pression comprise entre 0.6 et 1.1 Kba. L’activité de la faille de Point-Vert a été datée par la méthode 40Ar/39Ar au Miocène inférieur (21 Ma). Ces failles sont interprétées comme associées aux premiers stades du soulèvement résultant de l’activité des chevauchements dans le socle sous-jacent.Deux types principaux de roches de failles caractérisent les failles étudiées. Les brèches dilatantes sont majoritaires dans les zones de failles du secteur (1) alors que les arkoses foliées sont majoritaires dans les zones de failles du secteur (2). Les brèches dilatantes témoignent de mécanismes de déformation dominés par la fracturation transgranulaire et la pression-solution des silicates. Ce dernier mécanisme se manifeste principalement par d’abondantes précipitations cycliques de quartz, les stylolites restant peu développés. Les géométries structurales sont associées à l’activation de plans T de Riedel déterminant l’ouverture de relais extensifs et un régime localement dilatant. Nous associons ce type de roche de faille à une faible pression effective au cours de la déformation.La déformation cisaillante exprimée dans les arkoses foliées témoigne de mécanismes de déformation dominés par (i) la fracturation intragranulaire et transgranulaire, (ii) la pressionsolution/ précipitation des silicates, principalement le quartz, (iii) la néoformation de micas blancs liée à l’altération des feldspaths et (iv) la précipitation de chlorite. Ce travail montre également que les transformations minéralogiques liées aux interactions fluide-roche dans la zone de faille (forte augmentation de la proportion des phyllosilicates au dépend des feldspaths) changent radicalementla composition minéralogique de la roche. Nous associons ce type de roche de faille à une forte pression effective au cours de la déformation.La pétrophysique montre que les brèches de failles (secteur 1) ont une perméabilité isotrope et équivalente à celle du protolithe (10-3mD sous 2 MPa de confinement) tandis que les roches foliées (secteur 2) montrent une augmentation de perméabilité (10-2mD) selon l’axe Y de la déformation, d’un ordre de grandeur supérieure aux perméabilités suivant les axes X et Z et dans la roche hôte (10-3mD). Ce drain préférentiel potentiel est associé à l’orientation des phyllosilicates dans la foliation.
https://hal.archives-ouvertes.fr/tel-01310382

tel-01310382
https://hal.archives-ouvertes.fr/tel-01310382
https://hal.archives-ouvertes.fr/tel-01310382/document
https://hal.archives-ouvertes.fr/tel-01310382/file/Th%C3%A8seCAVAILHES2012.pdf

Éditeur(s) : HAL CCSD
Résumé : National audience
Les semelles métamorphiques sont situées à la base desgrandes ophiolites obductées. Elles sont principalement composéesd’amphibolites (métabasaltes à amphiboles ± grenat,clinopyroxène, plagioclase) fortement cisaillées et dont les conditionsmaximum de métamorphisme sont estimées à 800±100Cet 1.0±0.2 GPa. Leur formation a lieu au cours des 2 Ma suivantl’initiation des zones de subduction. Ces amphibolites sont interprétéescomme des portions de lithosphère océanique subduite,portions qui sont métamorphisées, dis-je, à haute températurepar transfert de chaleur depuis le coin de manteau sus-jacent quiformera la base de l’ophiolite obductée. Leur importante déformationau pic de métamorphisme est interprétée comme synchroneà leur accrétion au manteau de la plaque supérieure. Les semellesmétamorphiques sont donc des témoins directs de la dynamiqueprécoce des zones de subduction océanique. Leur pétrologie etleur déformation fournissent des contraintes majeures, et rares,sur l’évolution de la structure thermique et sur le comportementmécanique de l‘interface de subduction naissante. Cette étudeprésente des données structurales à plusieurs échelles, couplant desanalyses de terrain aux analyses EBSD sur des échantillons à amphibole± plagioclase ± clinopyroxene ± grenat de la semelle métamorphique.Les grains d’amphibole et de plagioclase sont caractériséspar une forte orientation préférentielle parallèle à la foliationet à la linéation. Cette fabrique est accompagnée par une forteorientation cristallographique préférentielle des amphiboles marquéepar un axe [001] marquant la linéation et la normale au plan(001) perpendiculaire à la foliation. Les plagioclases montrentune orientation cristallographique préférentielle faible voire nulle.Cette fabrique est similaire à celle observée dans les amphibolitescisaillées de base de croûte continentale. Les clinopyroxèneset les grenats présentent des degrés d’orientation intermédiaires.Ces deux phases forment des boudins dont l’axe long est orientéparallèlement à la foliation. Les porphyroclastes de clinopyroxèneprésentent une extinction ondulante et le développement de sousgrainsà leur périphérie. Les clinopyroxènes et les grenats agissentdonc comme phases ” dures ”, augmentant la résistance de laroche à la déformation. À l’initiation de la subduction, la partiesupérieure de la plaque plongeante est affectée par l’augmentationprogressive du degré de métamorphisme. Ceci entraîne une fortedéshydratation et la cristallisation de phases ” faibles ” (quartz,amphibole, plagioclase) et ” fortes ” (clinopyroxene, grenat). Larhéologie de l’interface de la subduction en est fortement affectée.Les unités de la semelle métamorphique (avec des minéralogies etdes conditions P-T-t différentes) accrétées aux péridotites de laplaque supérieure témoignent de changements rhéologiques majeuresà l’interface de la subduction au cours de l’histoire précocedes zones de subduction.
RST 2016, livre des résumés
Caen, France

insu-01388730
https://hal-insu.archives-ouvertes.fr/insu-01388730

Éditeur(s) : HAL CCSD American Physiological Society
Résumé : International audience
The IL-33/ST2 axis plays a protective role in T-cell-mediated hepatitis, but little is known about the functional impact of endogenous IL-33 on liver immunopathology. We used IL-33-deficient mice to investigate the functional effect of endogenous IL-33 in concanavalin A (Con A)-hepatitis. IL-33(-/-) mice displayed more severe Con A liver injury than wild-type (WT) mice, consistent with a hepatoprotective effect of IL-33. The more severe hepatic injury in IL-33(-/-) mice was associated with significantly higher levels of TNF-alpha and IL-1 beta and a larger number of NK cells infiltrating the liver. The expression of Th2 cytokines (IL-4, IL-10) and IL-17 was not significantly varied between WT and IL-33(-/-) mice following Con A-hepatitis. The percentage of CD25(+) NK cells was significantly higher in the livers of IL-33(-/-) mice than in WT mice in association with upregulated expression of CXCR3 in the liver. Regulatory T cells (Treg cells) strongly infiltrated the liver in both WT and IL-33(-/-) mice, but Con A treatment increased their membrane expression of ST2 and CD25 only in WT mice. In vitro, IL-33 had a significant survival effect, increasing the total number of splenocytes, including B cells, CD4(+) and CD8(+) T cells, and the frequency of ST2(+) Treg cells. In conclusion, IL-33 acts as a potent immune modulator protecting the liver through activation of ST2(+) Treg cells and control of NK cells.
ISSN: 0193-1857

hal-01366372
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01366372
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01366372/document
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01366372/file/Ablation%20of%20interaction%20between%20IL-33%20and%201%20ST2.pdf
DOI : 10.1152/ajpgi.00097.2016

Éditeur(s) : HAL CCSD Springer Verlag
Résumé : International audience
In this study, the cellular organization of the gill that harbors symbiotic bacteria is described in the thyasirid Thyasira falklandica collected from South Shetlands in Antarctic. Sections of the gills revealed that T. falklandica belongs to the gill type 3, as described by Dufour (Biol Bull, 208:200-212, 2005), with an elongated lateral zone along the frontal-abfrontal axis of the gill Wlaments. The ciliated and intermediary zones looked similar to those described in symbionts-bearing bivalves. The lateral zone is more complex in T. falklandica than in other Thyasiridae already described. Such a zone is composed of four different cell types. Bacteriocytes are abundant in the frontal and abfrontal positions, while the middle part of the lateral zone is occupied mostly by numerous granule cells devoid of bacteria. All along the lateral zone, TEM and SEM observations show some ciliated cells, which are regularly interspersed between bacteriocytes and/or granule cells. Such cells, according to the long double ciliary roots of their cilia, should have a sensory function. Intercalary cells, which have never been observed between bacteriocytes, are restricted to the middle part of the lateral zone where their expansions overlap the adjacent granule cells. Bacterial symbionts occur only extracellularly among long microvilli diVerentiated by the bacteriocytes. They are abundant, usually spherical in shape (around 0.7 m length), and covered by the glycocalix from bacteriocyte microvilli. According to TEM views, the empty vesicles located in the periplasmic space should be sulfur storage, as known for other sulfur-oxidizing symbionts.
ISSN: 0720-213X

hal-00755289
https://hal.univ-antilles.fr/hal-00755289
DOI : 10.1007/s00435-007-0034-4

Éditeur(s) : HAL CCSD Taylor & Francis: STM Behavioural Science and Public Health Titles Taylor & Francis: STM, Behavioural Science and Public Health Titles
Résumé : We have investigated by electron tomography, in a transmission electronic microscope, the interactions between dislocations in olivine single crystals and polycrystals deformed in axial compression at T < 1000 °C (T < 0.5Tm). Dislocations are mostly of the [0 0 1] type, except in the polycrystal where [1 0 0] and [0 0 1] dislocations have been activated. A few 〈1 0 1〉 junctions have been found and characterized. Many collinear interactions have been identified either involving direct interactions between crossing dislocations of opposite Burgers vectors or indirect interactions between dislocations gliding in parallel planes and sessile dislocation loops. We suggest that collinear interaction, already identified as the primary source of strain hardening in FCC metals, is the main dislocation interaction mechanism in olivine deformed at temperatures below 1000 °C.
ISSN: 1478-6443

hal-01174166
https://hal.archives-ouvertes.fr/hal-01174166
DOI : 10.1080/14786435.2014.1000996

Éditeur(s) : HAL CCSD
Résumé : International audience
Kisspeptins are well known as mediators of the coordinated communication between the brain-pituitary axis and the gonads in many vertebrates. To test the hypothesis that gonadal steroids regulate kiss1 and kiss2 mRNA expression in European sea bass (a teleost fish), we examined the brains of gonad-intact (control) and castrated animals, as well as castrated males (GDX) and ovariectomized females (OVX) that received testosterone (T) and estradiol (E2) replacement, respectively, during recrudescence. In GDX males, low expression of kiss1 mRNA is observed by in situ hybridization in the caudal hypothalamus (CH) and the mediobasal hypothalamus (MBH), although hypothalamic changes in kiss1 mRNA levels were not statistically different among the groups, as revealed by real-Time PCR. However, T strongly decreased kiss2 expression levels in the hypothalamus, which was documented in the MBH and the nucleus of the lateral recess (NRLd) in GDX T-Treated sea bass males. Conversely, it appears that E2 evokes lowkiss1mRNAin the CH, while there were cells expressing kiss2 in the MBH and NRLd in these OVX females. These results demonstrate that kisspeptin neurons are presumably sensitive to the feedback actions of sex steroids in the sea bass, suggesting that the MBH represents a major site for sex steroid actions on kisspeptins in this species. Also, recent data provide evidence that both positive and negative actions occur in key factors involved in sea bass reproductive function, including changes in the expression of gnrh-1/gonadotropin, cyp19b, er and ar genes and sex steroid and gonadotropin plasma levels in this teleost fish. © 2016. Published by The Company of Biologists Ltd.
Journal of Experimental Biology

hal-01406072
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01406072
DOI : 10.1242/jeb.137364
PUBMED : 27591305

Éditeur(s) : HAL CCSD
Résumé : 06072 - 89 p.
Projet retenu dans l'appel à projet en 2003. ACI Ecole et Sciences cognitives (Ministère délégué à la recherche et aux nouvelles technologies)
Ce projet vise en particulier à répondre à trois questions : Le niveau de langage en français des enfants créolophones est-il quantitativement et qualitativement différent des enfants de métropole ? Existe t-il une corrélation entre les compétences langagières dans l'une et l'autre langue ? Leur niveau en deux langues exerce t-il un impact sur leurs acquisitions scolaires?
Avant de présenter la méthodologie de l'étude, une revue de questions et d'études en matière de bilinguisme est proposée selon deux champs disciplinaires : psycholinguistique et sociologie de l'éducation.
https://halshs.archives-ouvertes.fr/halshs-00218159

halshs-00218159
https://halshs.archives-ouvertes.fr/halshs-00218159
https://halshs.archives-ouvertes.fr/halshs-00218159/document
https://halshs.archives-ouvertes.fr/halshs-00218159/file/06072.pdf

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : L’objectif de cette étude est d’analyser les impacts et les limites d’une expérience de lutte contre la pauvreté par le tourisme au travers d’une étude de cas dans le village d’Anse-la-Raye, à Sainte-Lucie.Depuis son indépendance en 1979, Sainte-Lucie a tenté de diversifier la structure économique héritée de son passé colonial, en développant notamment des sources alternatives de recettes. Au début, il y a eu un certain succès avec l'industrie de confection et le tourisme qui ont émergé comme des activités viables en dehors de l'agriculture d'exportation.À la fin des années 1980, le pays avait même atteint un taux de croissance qui aurait été considéré comme raisonnable. Sainte-Lucie a d’ailleurs été l’île ayant connu la plus grande croissance économique des Etats du CARICOM. L’exportation de la banane a contribué pour beaucoup à ces résultats, et les nouveaux secteurs ont permis la création d’emplois ainsi que des revenus et des recettes d'exportation supplémentaires.Mais comme tous les Petits Etats Insulaires en Développement (PEID), Sainte-Lucie est caractérisée par sa vulnérabilité économique face aux catastrophes naturelles et crises extérieures. Ainsi, deux des secteurs principaux de son économie se sont affaiblis ces dernières années (l’agriculture et l’industrie), avec pour résultat principal une aggravation de la pauvreté à Sainte-Lucie malgré les bons résultats du secteur touristique devenu le pilier principal de l’économie de l’île.Dans ce contexte de faible croissance économique, le gouvernement et les partenaires sociaux se sont rassemblés pour identifier les politiques susceptibles d’accélérer la croissance économique de Sainte-Lucie. Ainsi, trois axes principaux ont été retenus : l’augmentation de la production locale, la réduction du crime et la réduction de la pauvreté. Dans ce dernier cadre, le gouvernement a lancé plusieurs stratégies de lutte contre la pauvreté notamment l’aide au développement d’activités touristiques.L’étude s’intéresse plus particulièrement au village d’Anse-la-Raye et à une expérience de tourisme pro-pauvre qui y a été développé en 2000 : l’Anse-la-Raye Seafood Friday, une sorte de festival qui permet aux visiteurs de déguster les produits de la mer tous les vendredis. Ce festival a-t-il eu réellement des répercussions sur la population pauvre de la communauté d’Anse-la-Raye ? Est-il viable? Quel est son devenir?
The objective of this study is to analyse the impacts and limitations of attempts to combat poverty using tourism through a case study in the village of Anse-la-Raye, in St. Lucia.Since its independence in 1979, St. Lucia has attempted to diversify the economic structure it inherited from its colonial past, in particular developing alternative sources of revenue. Initially there was some success with the clothing industry and tourism, which emerged as viable business activities outside of agricultural exports.At the end of the 1980s, the country had reached a growth which was considered reasonable. Of all the states of CARICOM, St. Lucia has moreover experienced the greatest economic growth. Banana exports have contributed significantly to these results, and new sectors have led to the creation of jobs and income to supplement export income.But like all Small Island Developing States (SIDS), St. Lucia is characterized by vulnerability to natural disasters and external economic shocks. Two major sectors of the economy have weakened in recent years (agriculture and industry), resulting in an increase in poverty in St. Lucia despite favourable outcomes in the tourism sector, which became the primary pillar of the island.In the context of low economic growth the government and social partners gathered together to identify policies and accelerate economic growth in St. Lucia. Three main themes were identified: Increasing local production; reducing crime and reducing poverty. In this context, the government launched several strategies to combat poverty including assistance for the development of tourism.The study focuses on the village of Anse-la-Raye and the experiences of pro-poor tourism that was developed in 2000: Anse-la-Raye Seafood Friday, a kind of festival that allows visitors to taste the seafood on Fridays. Has this festival really had an impact on the poor of the community of Anse-la-Raye? Is it viable? And what is its future?
Sainte-Lucie

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.6525
http://journals.openedition.org/etudescaribeennes/6525

Éditeur(s) : Pêche thonière et dispositifs de concentration de poissons, Caribbean-Martinique, 15-19 Oct 1999
Résumé : The volcanic island of Mayotte (374 km super(2)) is part of the Comoros Archipelago, which is situated on the North of Mozambic's Canal (Indian Ocean). Mayotte is composed of two islands and some thirty small islands distributed in a lagoon of more than 1,000 km super(2). Being one of the French Republic's Territorial Collectivity, this island is characterized by a very fast demographic evolution (growth rate : 5.8 %), which constitutes the foundation of the development problematic. Most of local halieutic production comes from the reef (nearly 2,000 t in 1999), the technic of "palangrotte" (deep line) is still dominating. The fishing fleet is composed of monoxyl pirogues and polyester fishing boats for the 1,200 fishermen. The first FADs (Fish Aggregating Devices) were installed in 1989. Now, 5 FADs are situated in the lagoon whereas 10 others have been installed out of it. If it is very hard to evaluate economic impact of FAD in Mayotte, their success seems to be limited because of several local constraints : fear to fish out of the lagoon, little interest in tuna, lack of formation. Nevertheless, faced to the demographic evolution and the decrease of the reef ressources, a program of fishing development on FAD has been initiated in 1998, with those following themes : realization of a new prototype of FAD, experimental fishing program with vertical drift "long line", teaching programs for the local fishermen. Today, it is too early to analyze the informations already collected, but the results are very promising, and validate the technical improvement of the new prototype.Original Abstract: L'ile volcanique de Mayotte (374 km super(2)) fait partie de l'archipel des Comores situe au Nord du canal du Mozambique (ocean Indien). Mayotte comprend deux iles et une trentaine d'ilots repartis dans un lagon de plus de 1 000 km super(2). Collectivite territoriale de la Republique francaise, l'ile se caracterise par une evolution demographique tres rapide (taux de croissance: 5,8 %), qui constitue le socle de toutes les problematiques de developpement. L'essentiel de la production halieutique provient du milieu recifal (environ 2 000 t en 1999), la peche a la ligne de fond reste la technique dominante. La flottille de peche est constituee de pirogues monoxyles et de barques polyester pour une population de 1 200 pecheurs. Les premiers DCP mahorais furent installes en 1989. A ce jour, on denombre cinq DCP dans le lagon et dix hors lagon. Il semble que leur succes soit reste limite en raison de plusieurs contraintes locales : peur de la peche hors lagon, peu d'interet pour les poissons pelagiques, manque de formation. Neanmoins, face a l'explosion demographique et a l'appauvrissement des ressources lagonaires, un nouveau programme de developpement de la peche sur DCP a ete initie en 1998. Ce programme comporte trois axes : realisation d'un nouveau prototype de DCP, lancement d'un programme de peches experimentales a la palangre verticale derivante et formation des pecheurs. A ce jour, les informations obtenues sont trop parcellaires pour etre analysees mais les donnees et observations realisees sur les nouveaux dispositifs permettent de valider leur conception technique.

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/00042/15290/12647.pdf
http://archimer.ifremer.fr/doc/00042/15290/

Éditeur(s) : HAL CCSD American Geophysical Union
Résumé : International audience
The reactivation of faults with near-optimal orientations is commonly considered to control the state of stress in the crust. Near the surface, where a principal stress direction is vertical, the attitude of such faults is explained by Anderson's theory. This raises the questions of how prevalent this type of faulting actually is in current seismicity, down to what depth it frequently occurs, and what range of friction angles explains it best. The Global Centroid Moment Tensor catalog is analyzed to address these questions. Dip-slip and strike-slip mechanisms are dominant, and oblique slips are relatively rare for well-constrained events with depths shallower than 30 km. Preferred Andersonian faulting is the simplest, but not the unique, explanation for this dominance. Isolating reverse, strike- slip, and normal events reveals an asymmetry in the distribution of nodal plane dips and plunges of the P, B, and T axes between reverse and normal faulting. Assuming that the most frequent events correspond to reactivation near optimal orientations yields 40-60 degrees and 0-20 degrees friction angles for reverse and normal faults, respectively. This indicates that reverse and normal faulting mechanics are not symmetrical with respect to stress configuration as predicted by Anderson's theory.
ISSN: 8755-1209

hal-00412159
https://hal.archives-ouvertes.fr/hal-00412159
DOI : 10.1029/2007RG000240

Éditeur(s) : HAL CCSD Springer Verlag
Résumé : International audience
Unravelling the detailed pressure–temperature–time-deformation (P–T–t-D) evolution of magmatic and metamorphic rocks provides essential insights into the timing and duration of partial melting and related plutonism during crustal flow and migmatitic dome formation. The Montagne Noire Axial Zone (MNAZ) is a migmatitic dome located within the Variscan orogen in the southern French Massif Central. The timing of the main thermal event that was responsible for intense partial melting is still highly debated. In this study we present new laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) age data on micaschists, migmatites and granites that clarify the P–T–t-D evolution of the MNAZ. Structurally controlled samples were collected in order to constrain the timing of metamorphism, migmatization and plutonism regarding the main structural pattern D1, D2 and D3. D1 and D2 correspond to nappe stacking and dextral transpression, respectively. D3 is related to vertical shortening and coaxial thinning with a preferential NE–SW- to E–W-directed stretching. LA-ICP-MS analyses on the syntectonic Anglès, Soulié and Martys granites yielded U–Th/Pb monazite ages of 305 ± 1.5, 306 ± 1.9 and 314 ± 2 Ma, respectively. Five migmatitic rocks sampled in the eastern and central Espinouse area yielded in situ ages ranging between 312 ± 2 and 301 ± 2 Ma. Along the dome envelope, two garnet–staurolite-bearing micaschists near Saint-Pons-de-Thomières village gave in situ U–Th–Pb ages of 312.1 ± 2.1 and 309.0 ± 3.1 Ma. A fine-grained gneiss with a D3 fabrics in the eastern dome envelope yield a 208Pb/232Th mean age at 305.7 ± 3.9 Ma. All ages obtained in this study for the micaschists, migmatites and granites range between 315 and 301 Ma. We interpret this time span as the record of the high thermal event responsible for intense crustal partial melting within the lower and middle crust. The onset of partial melting occurred at ca. 315 Ma that marked the beginning of transpressional deformation D2. Based on structural and petrological studies, our new U–Th–Pb results suggest that (1) partial melting may have started at ca. 315 Ma and lasted 15–10 Myr and (2) D2 et D3 developed between 315 and 300 Ma and were synchronous. D1 deformation ended at 315 Ma. The onset and duration of D1 related to nappe stacking and crustal thickening is still uncertain.
ISSN: 1437-3254

hal-01526942
https://hal.archives-ouvertes.fr/hal-01526942
DOI : 10.1007/s00531-016-1417-x

Éditeur(s) : HAL CCSD AGU and the Geochemical Society
Résumé : International audience
We analyze focal mechanisms of shallow-intermediate earthquakes in a NW-SE transect along the western Betic Cordillera and Alboran Sea, and deep earthquakes located in the central Betics to constrain the state of stress at the Gibraltar Arc slow convergence area. Shallow earthquakes (< 40 km) are preferably clustered at the mountain front. A general NW-SE horizontal compression is compatible with the convergence, and NW plunging compression axes are in agreement with frontal thrust activity. Toward the Alboran Sea the earthquakes are progressively deeper, reaching intermediate depths (40-120 km) near the coast and supporting the present-day activity of subduction only in this area. The Iberian continental crust concentrates most of the intermediate seismicity and is forced to partially sink into the mantle, probably through the pull of the oceanic slab. This downdip pull together with the buoyancy of the Iberian continental crust produces the slab curvature, downdip extension in the external arc of the continental slab, and downdip compression in the inner arc. T axes highly dipping to the southeast at 90-120 km depth occur at the oceanic/continental transition. Deep earthquakes (> 620 km) show very similar focal mechanisms, fitting the general slab behavior of resistance to further descent at the 660 km discontinuity. Seismicity features evidence the present-day stress distribution in a context of transition from subduction to continental collision.
ISSN: 1525-2027

hal-00669889
https://hal.archives-ouvertes.fr/hal-00669889
DOI : 10.1029/2011GC003824

Éditeur(s) : HAL CCSD
Résumé : International audience
This research aim focused onthe interpretation of the action of pupils for two school professors in mathematics and in physical education. The research is in the field of work concerned with the process of didactic contextalisation (Delcroix, Forissier, Anciaux, 2012). It also mobilizes process of the comparative approach (Mercier, Schubauer-Leoni et Sensevy, 2002). Data processed within the limits of this communication were collected by interview of self-confrontation. The results are used to model the interpretive filters according to three axes: the practical epistemology of the professor through the categories of Shulman (1987), forms of inference employed and his organization. Our study allows us to confront, in this model, the specifics or generics, fruits of disciplinary didactics to the effects of the didactic contextualization. We note that the use of contextualization seems to act as a filter (regardless of the teacher or the discipline concerned) constitutive of a profile kind (in the sense of Clot). Finally, at the end of this research, we discuss the contribution of this type of study for the training of teachers by querying the aspect built of these filters in action-context interaction and by validating the legitimacy of this question: "What is happening in the minds of the students"?Clot, Y. et Faïta, D. (2001). Genre et style en analyse du travail. Concepts et méthodes, Travailler, 6, 7-42Delcroix, A., Forissier, T., & Anciaux, F. (2012). Vers un cadre d’analyse opérationnel des phénomènes de contextualisation didactique. Dans F. Anciaux, T. Forissier et LF. Prudent, Contextualisations didactiques (pp. 141-188). Paris : L’harmattan.Mercier, A., Schubauer-Leoni, ML. & Sensevy, G. (2002). Vers une didactique comparée. Revue française de pédagogie, 141, 5-16.Shulman, L. (1987). « Knowledge and teaching : foundations of the new reform ». Harvard Educational Review, vol. 57, n° 1, p. 1-22.
The Caribbean Academy of Sciences 20th GENERAL MEETING AND BIENNIAL CONFERENCE
Deshaies, Guadeloupe

hal-01618424
https://hal.univ-antilles.fr/hal-01618424