Éditeur(s) : Pêche thonière et dispositifs de concentration de poissons, Caribbean-Martinique, 15-19 Oct 1999
Résumé : The length frequency distribution of blackfin tunas (Thunnus atlanticus) shows a significant difference between fishes caught with a longline, during Ifremer experimental surveys and fishes landed by fishermen who exploit martinican FADs. The fishing technique used could probably explain this. In fact, diving surveys have confirmed the presence of great concentrations of adult blackfin tunas under FADs. Big individuals stay during long periods between 20 and 50 meters under the FAD while small ones go up to the surface to feed on little flying fishes, at dawn principally. The bait and the line used at the moment around martinican FADs do not fit to adult blackfin tunas fishing. From these observations and following the tests realized by Ifremer in La Reunion in 1990, we proposed to martinican fishermen to test a new technique based on the utilization of live bait locally called "coulirous" (Selar crumenophthalmus). In La Reunion, this technique has been successful. Live baits are hooked on a vertical longline. In Martinique, the tests to catch live bait during the night near the shore have been already successful and the first fishing experiences with vertical line are also encouraging. This paper aims at proposing and transfering this technique to martinican fishermen but technical exchanges and discussions are needed to improve this new fishing technique.Original Abstract: Une analyse des compositions en taille des thons noirs (Thunnus atlanticus) captures, d'une part, lors des peches experimentales realisees par l'Ifremer a la palangre derivante et, d'autre part, debarques par les pecheurs exploitant les DCP martiniquais montre une difference significative de la taille moyenne des individus. Les techniques de peche utilisees peuvent probablement expliquer cette difference. En effet, des observations sous-marines ont confirme a plusieurs reprises la presence de larges concentrations de thons noirs adultes sous les dispositifs. Les gros individus se tiennent preferentiellement entre 20 et 50 m de profondeur a proximite du DCP alors que les petits individus montent plus frequemment en surface pour chasser, notamment au lever du jour. L'appat et les caracteristiques des engins actuellement utilises autour des DCP martiniquais ne sont pas bien adaptes a la capture des thons noirs adultes. A partir de ce constat et sur la base des essais de palangres verticales realises au laboratoire de l'Ifremer de La Reunion en 1990, qui ont abouti a une generalisation de cette technique de peche autour des DCP reunionnais, nous avons propose aux pecheurs martiniquais de tester cette nouvelle technique basee sur l'utilisation de " coulirous " vivants (Selar crumenophthalmus). Les essais de peche de l'appat vivant, la nuit a la palangrotte, se sont reveles positifs dans plusieurs baies de la Martinique et les premiers tests sur la palangre verticale a thons noirs sont encourageants. Cette communication fait le point sur le transfert vers les pecheurs martiniquais en identifiant les mises au point necessaires pour ameliorer l'efficacite de la technique proposee.

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/00042/15293/12651.pdf
http://archimer.ifremer.fr/doc/00042/15293/

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
We present the 1998-2009 GPS-derived velocity field for the Armenia region based on a survey-mode observation network of 31 GPS sites.We combine our results with previous GPS studies of the region to better assess the deformation of the Lesser Caucasus and Kura basin region. The results show that the Kura basin and the Lesser Caucasus regions are two different blocks, and that the main fault (Pambak-Sevan-Sunik) between these two regions has a right-lateral slip rate of 2±1 mm/yr. This is consistentwithmorphotectonic estimates and suggests a fairly constant slip rate over the last 120-300 ka. The right-lateral slip rate on one of the southern branch of the Pambak-Sevan-Sunik fault is lower than 1 mm/yr and the good agreementwith a geologically estimated slip rate suggests a constant slip rate over the last 1.4 Myr. The Sardarapat and Akhurian faults experience some shortening. This shortening is consistentwith someindependent geological estimates and shows the Arabian push.However, NNW-SSE-orientated faults have an extensional fault normal component instead of the expected shortening due to the Arabia-Eurasia convergence. This substantial extensive strain, and the sharp azimuth change of the velocity vectors between the Arabia promontory and the Lesser Caucasus suggest that processes other than "extrusion", possibly related to old subduction or delamination, contribute to the geodynamics of the region.
ISSN: 0040-1951

hal-00812623
https://hal.archives-ouvertes.fr/hal-00812623
DOI : 10.1016/j.tecto.2013.02.002

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
We report concentrations of hydrogen (H) in upper mantle minerals of peridotites (olivine and pyroxenes) transported by alnöitic lavas, which erupted on the southwestern border of the Ontong Java Plateau (Malaita, Solomon Islands, West Pacific). Unpolarized FTIR analyses show that olivine, orthopyroxene, and diopside contain 2–32 ppm, 162–362 ppm and 159–459 ppm wt H2O, respectively. In the studied lherzolites, garnets are anhydrous. The concentration of hydrogen within individual olivine and pyroxene grains is almost homogeneous, indicating no evidence of dehydration or hydration by ionic diffusion. In the lherzolite, the concentration of hydrogen in olivine tends to increase weakly with depth (based on geothermobarometry), consistent with the increase of water solubility with increasing water fugacity as a function of pressure, but concentrations remain well below water-saturation values determined experimentally. The highest concentration of H in olivine (32 ppm wt H2O) is, however, found in refractory spinel harzburgites, which equilibrated at depths of 85 km., while deeper specimens as the high-temperature spinel harzburgites, and some of the garnet lherzolites, contain less hydrogen in olivine. Olivines from pyroxene- or pargasite-rich peridotites have also lower hydrogen concentrations. We interpret the high hydrogen concentrations in olivine from the refractory spinel harzburgites as due to (1) simultaneous hydration and metasomatism of the lithospheric mantle by a water-rich silicate melt/fluid, during which hydrogen follows MREE and where spinel harzburgite have experienced ‘stealth’ metasomatism, and/or (2) to a late ‘fleeting’ hydrogen metasomatism, which would hydrate the rock after this first ‘stealth’ metasomatism event. In the second case, the composition of the ‘fleeting’ percolating fluid (small volume fraction of very evolved fluids, with high volatiles concentration and transient properties) is likely to be linked to the decrease of the plume activity and resulting in the downwelling of the lithosphere asthenosphere boundary. The difference in hydrogen concentration between harzburgites and lherzolites could be linked to variation in trace elements in olivine induced by the first ‘stealth’ metasomatism alone or associated to the late ‘fleeting’ hydrogen metasomatism, triggered by the lack of secondary crystallization of clinopyroxenes in the harzburgite. To conclude, H concentrations in upper mantle minerals may thus be correlated to metasomatic events, with the later yielding variation of the mineral assemblage and trace element composition that constitute the peridotites.
ISSN: 0024-4937

hal-01143385
https://hal.archives-ouvertes.fr/hal-01143385
DOI : 10.1016/j.lithos.2014.11.005

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Although ants may induce community-wide effects via changes in physical habitats in terrestrial environments, their influence on aquatic communities living in plant-held waters remains largely underexplored. The neotropical tank-bromeliad Aechmea mertensii (Bromeliaceae) occurs along forest edges in ant-gardens initiated by Camponotus femoratus or by Pachycondyla goeldii. Its leaves form wells that hold rainwater and provide suitable habitats for many aquatic organisms. We postulated that these ant-plant mutualisms indirectly affect the microbial community structure via changes in the environmental conditions experienced by the plants. To test this hypothesis, we analyzed the protist communities from 63 tank-bromeliads associated with either C. femoratus or P. goeldii (hereafter Cf-Aechmea and Pg-Aechmea) along a forest edge in French Guiana. For each plant, a large number of environmental variables (including habitat structure, food resources, incident radiation and the presence of aquatic invertebrates) were quantified to determine their relative importance in driving any observed differences across ant-associated plants. Pg-Aechmea are located in sun-exposed areas and hold low volumes of water and low amounts of detritus, whereas Cf-Aechmea are located in partially shaded areas and accumulate higher amounts of water and detritus. Protists (i.e., protozoa and algae) inhabiting Cf-Aechmea exhibit greater richness and abundances than those in Pg-Aechmea. Variations in detritus content, number of leaves, incident radiation, and the epiphyte richness of the ant-garden were the main factors explaining the variation in protist richness. A shift in the functional group composition of protists between bromeliads tended by different ant species suggested that mutualistic ants indirectly mediate changes in the microbial food web.
Basic and Applied Ecology

hal-00913126
https://hal.archives-ouvertes.fr/hal-00913126
https://hal.archives-ouvertes.fr/hal-00913126/document
DOI : 10.1016/j.baae.2012.10.002
OATAO : 10190

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : En Haïti, l’accès difficile à des services spécialisés et la rareté des hôpitaux psychiatriques amènent l’aggravation des problèmes d’adaptation (IESM-OMS, 2011 ; Lecomte et Raphaël, 2010a; Nicolas et al.,). Certains services d’intervention tentent de répondre aux besoins complexes des enfants de la rue, comme par exemple le Centre d’accueil de Delmas 3. Au Québec, le modèle psychoéducatif guide les interventions spécialisées auprès de jeunes ayant des troubles de comportements. Le présent projet de recherche vise d’une part à évaluer si une approche collaborative favoriserait la pérennité d’un programme d’intervention en Haïti et d’autre part si le modèle psychoéducatif pourrait répondre aux besoins du milieu d’intervention du Centre d’accueil de Delmas. Pour favoriser la mobilisation des partenaires, le projet met de l’avant une méthode qualitative et collaborative (Hamel, Cousineau et Vézina, 2010). D’abord, une formation adaptée aux besoins du milieu a été présentée aux intervenants. Ensuite, l’équipe de recherche et les intervenants du centre d’accueil ont animé des activités psychoéducatives. Ce projet pilote a montré qu’une approche collaborative favorise la participation et le niveau de satisfaction de tous les acteurs impliqués. Cette expérience a également permis de constater que le modèle psychoéducatif pourrait être utilisé dans les centres d’accueil en Haïti. En effet, ce modèle permet d’adapter la réponse aux besoins des personnes selon les caractéristiques des milieux (Renou, 2005).
In Haiti, accessibility to specialized services and the lack of psychiatric hospitals exacerbates adaptation problems (Lecompte and Raphael 2010a; Nicolas et al, 2012; WHO-AIMS, 2011). The health professionals at the Centre d’accueil de Delmas 3 respond to the complex needs of young street children. In Quebec, several evidence-based intervention models have shaped our clinical practice for young children with behavior disorders. In fact, rehabilitation interventions are based on the psychoeducational model. The current research project had two goals: 1) Examine whether a collaborative approach would facilitate and ensure that the implementation of an intervention program would be ongoing and long-lasting in Haiti; 2) Explore whether the psychoeducational model could respond to the needs of a Haitian youth center. Qualitative methods were used to bring together partners in the research (Hamel, Cousineau and Vézina, 2010). First, educators followed a two days training developed to respond the specific needs. Second, interventions were implemented by researchers in collaboration with the stakeholders. This pilot project has shown that a collaborative approach encourages training and the level of participants' satisfaction. Futher, this experience showed that the psychoeducational model could very well fit the needs of a Haitian youth center. The psychoeducative model can yield responses adapted to the needs of people accounting for the characteristics of the environment (Renou, 2005).
Haïti

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.10295
http://journals.openedition.org/etudescaribeennes/10295

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Tsavorite, the vanadian variety of green grossular, is a high value economic gemstone. It is hosted exclusively in the metasedimentary formations from the Neoproterozoic Metamorphic Mozambique Belt. The deposits are mined in Kenya, Tanzania and Madagascar and other occurrences are located in Pakistan and East Antarctica. They are located within metasomatized graphitic rocks such as graphitic gneiss and calc-silicates, intercalated with meta-evaporites. Tsavorite is found as primary deposits either in nodule (type I) or in quartz vein (type II), and in placers (type III). The primary mineralizations (types I and II) are controlled by lithostratigraphy and/or structure. For the African occurrences, the protoliths of the host-rocks were deposited at the beginning of the Neoproterozoic within a marine coastal sabkha environment, located at the margin of the Congo-Kalahari cratons in the Mozambique Ocean. During the East African-Antarctican Orogeny, the rocks underwent high amphibolite to granulite facies metamorphism and the formation of tsavorite deposits occurred between 650 and 550 Ma. The nodules of tsavorite were formed during prograde metamorphism, calcium coming from sulphates and carbonates, whereas alumina, silicates, vanadium and chromium probably came from clays and chlorite. The veins were formed during the deformation of the metasedimentary platform units which experienced shearing, leading to the formation of fault-filled veins. Metasomatism developed during retrograde metamorphism. The metasedimentary sequences are characterized by the presence of evaporitic minerals such as gypsum and anhydrite, and scapolite. Evaporites are essential as they provide calcium and permit the mobilization of all the chemical elements for tsavorite formation. The H2S-S8 metamorphic fluids characterized in primary fluid inclusions of tsavorites and the δ11B values of coeval dravite confirm the evaporitic origin of the fluids. The V2O3 and Cr2O3 contents of tsavorite range respectively from 0.05 to 7.5 wt.%, while their δ18O values are in the range of 9.5-21.1‰. The genetic model proposed for tsavorite is metamorphic, based on chemical reactions developed between an initial assemblage composed of gypsum and anhydrite, carbonates and organic matter deposited in a sabkha-like sedimentary basin.
ISSN: 0169-1368

hal-00853279
https://hal.archives-ouvertes.fr/hal-00853279
DOI : 10.1016/j.oregeorev.2013.01.016

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Les îles ont longtemps été étudiées comme de simples lieux périphériques, inscrits dans le prolongement de logiques continentales ; des espaces dépourvus de sens en dehors du prisme des puissances métropolitaines. A travers le champ des études insulaires, il s’agit désormais de croiser les différentes expériences insulaires, de poser les contextes de développement et d’étudier les configurations et les temporalités spécifiques des îles. Étudier les îles nécessite de prendre la mesure de ces territoires -loin de toute vision monolithique-, d’analyser leur espace au regard des réalités sociale et politique, de cerner leur poids économique et leur contexte de développement, des héritages de l’histoire à la prise en compte de leur voisinage géographique. Il s’agit de prendre en considération les logiques exogènes qui font l’île et d’interroger les dynamiques internes.Le sujet d’étude est l’île, l’objet «île », l’île dans la gestion de son espace, la définition de son projet territorial, le positionnement de l’île dans son environnement respectif et les opportunités et stratégies dans l’économie mondialisée. La richesse des enseignements des territoires et des sociétés insulaires débordent le simple cadre spatial de l’île qui peut être entendue comme une synecdoque, un microcosme commode et raisonnable du continent.
Islands were studied for a long time as simple peripheral territories, territories which flesh out the seamless continuation of continental logic, meaningless territories without the prism and perspective of metropolitan power. Through the field of the island studies, critical questions cross various island experiences and their context of development and their configurations; or otherwise study specific temporalities, connectivities and materialities, in the context of globalization. To study islands requires taking the measure of these territories, far from any monolithic vision, to analyze their space with regard to their social and political realities, to identify their economic clout and their context of development and the legacies of the history, in consideration of their geographical neighbourhood. It is a question of considering the exogenous logics which make the island and interrogate its internal dynamics.The subject of study is the island, "island" as object, the island in the management of its space, the definition of its territorial project, the positioning of the island in its environmental perspective and the opportunities it enjoys and the strategies it deploys in the globalized economy. The wealth of scholarship of and about islands and island societies extends beyond the simple spatial frame of the island; ‘the Island’ can be understood as a synecdoche, a convenient, manageable and reasonable microcosm of the continent.

Droits : info:eu-repo/semantics/openAccess
http://journals.openedition.org/etudescaribeennes/7272

Éditeur(s) : HAL CCSD Association des Géographes Français
Résumé : International audience
The international symposium on Urban Growth and Natural Hazards, in particular in Developing Countries was held in the Université Blaise-Pascal, Clermont-Ferrand (France) on December 2 and 3, 1994. This meeting brought together about 70 researchers, Ph. D. students, and professionals from France and 12 other countries, representing universities, research agencies, as well as government and private companies. The symposium aimed to gather specialists who are engaged and acting in programmes on hazard appraisal, risk prevention and urban management in the city environment. These people compared experiences acquired in two different fields: on the one hand urban growth and its consequences, and on the other hand, natural hazards and their effects, in particular in developing countries.Three themes correspond to the three sessions of the symposium. (1) Natural hazards and environmental factors: inventory, diagnostic and classification, (2) Vulnerability of urban society and environment: concepts, approaches, and classification, (3) Tools for urban risk prevention and risk management in case of crisis and catastrophes.
ISSN: 0004-5322

hal-01165465
https://hal.archives-ouvertes.fr/hal-01165465

Éditeur(s) : HAL CCSD De Gruyter
Résumé : COST Action E35 : Fracture mechanics and micromechanics of wood and wood composites with regard to wood machining
The data available in the literature concerning wood cutting forces permits to build models or to simulate the main wood machining processes ( milling, sawing, peeling, etc.). This approach contributes to a better understanding of formation of wood surfaces and chips and the data may be helpful to optimise cutting geometry, reduce tool wear, improve tool material, and to size tool-machines. The models may also be useful for industrial application in two ways: ( 1) providing data to optimise the settings for a given operation ( batch approach), and ( 2) building predictive models that could be the basis of an online control system for the machining processes ( interactive approach). A prerequisite for this is that numerous machining tests on different wood materials are performed based on experiences with different kind of tools and experimental devices. With a focus on potential industrial applications, the emphasis of this review was on the wood peeling process, which is a very demanding special case of wood cutting. Although not so many industrial machines are equipped with expensive force sensors, there is a lot of high quality information available about cutting forces which may be useful to improve the scientific or technological knowledge in wood machining. Alternative parameters, such as vibration or sound measurements, appear to be promising substitutes in the praxis, particularly to feed online control systems of any wood cutting process.
ISSN: 0018-3830

hal-01032121
https://hal.archives-ouvertes.fr/hal-01032121
DOI : 10.1515/HF.2009.014

Éditeur(s) : HAL CCSD
Résumé : International audience
La présente recherche s’intéresse aux termes créoles utilisés dans le domaine des activités physiques et sportives en Guadeloupe. Ce vocabulaire est tiré de la littérature créole, de situations réelles de pratiques sportives et d’entretiens passés auprès d’entraîneurs, d’enseignants d’EPS et de sportifs antillais. Une traduction en français a été assignée à chacun des termes recensés par les participants eux-mêmes. Ce travail s’adresse à ceux qui souhaitent comprendre, connaître ou découvrir les mots créoles en rapport avec le sport en général et le corps en mouvement. Son ambition est de favoriser la communication et le partage d’expériences au sein des pratiques sportives en Guadeloupe, mais aussi l’identification d’un patrimoine culturel et linguistique dans le sport aux Antilles françaises.
ISSN: 1762-598X

hal-01609294
https://hal.univ-antilles.fr/hal-01609294

Éditeur(s) : HAL CCSD
Résumé : Red blood cell hemodynamics influence blood rheology and thus circulatory function. Different authors showed that red blood cells are heterogeneous in blood flow. This heterogeneity could be explained by physical characteristics such as morphology, aggregability and deformability, but also by cellular and molecular environment. All these notions are found in sickle cell disease where sickle red blood cells become more rigid, leading to vascular occlusions, increased with an inflammatory context. In a preceding study, our results showed that velocity heterogeneity allow RBC classification, leading to different RBC sub-groups, using a dynamical approach and flow studies. In order to have a better understanding of the physiological meaning of such an heterogeneity, dynamical velocity experiences have been conducted in the case of normal and sickle red blood cells with different endothelial activations by proinflammatory cytokines, under a constant venular flow. Thus, normal and sickle red blood cells are classified into different sub-groups, showing their heterogeneity. Moreover, sub-population velocities and distribution evolve differently according to vascular state or treatment. These results show that red blood cell velocities and rheology depend on vascular environment and red blood cell morphology. However, the physiological meaning of this behavior should be explained by cellular and molecular effects of such activation.
https://hal.archives-ouvertes.fr/hal-00201461

hal-00201461
https://hal.archives-ouvertes.fr/hal-00201461
https://hal.archives-ouvertes.fr/hal-00201461/document
https://hal.archives-ouvertes.fr/hal-00201461/file/RBCV_Marianne_v1.pdf

Éditeur(s) : HAL CCSD L'Harmattan
Résumé : International audience
Dès le 18e siècle, l'Église africaine-américaine a été un espace de liberté pour les Noirs aux États-Unis. Tantôt conservatrice, tantôt force de progrès social, elle a clairement participé à la construction de l'expérience africaine-américaine en influençant la région Caraïbe. Qui veut comprendre la communauté africaine-américaine doit passer par la porte de l'église. Cet ouvrage s'intéresse à la manière dont cette dynamique s'est matérialisée dès le 18e siècle jusqu'à son impact sur la personnalité de Barack Obama, le premier président africain-américain.
https://hal.univ-antilles.fr/hal-01380128

ISBN : 978-2-343-06492-5
hal-01380128
https://hal.univ-antilles.fr/hal-01380128

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The main political concern in the southern areas of Madagascar is poverty alleviation. To alleviate poverty in the area, the government has chosen to enforce adjustment policies of the World Bank Group. According to the World Bank Group's argument, while artisanal mining is supposed to create significant economic, social and environmental problems, large-scale mining investment results in economic and social prosperity. This paper focuses principally on a re-analysis of the debates regarding the relationship between artisanal and large-scale mining and poverty alleviation in developing countries. Further, the paper offers an alternative viewpoint on these issues based on the example of Madagascar. In the last decade, Madagascar has experienced a significant increase in mining activity. Towards the end of the 90s, informal and artisanal mining emerged as one of the most important economic activities of the area with the development of the Ilakaka frontier. At the same time, foreign investments began to benefit from adjustment policies implemented by the government, and large-scale mining operations also commenced. As the local socio-economic system was deeply affected by these developments, it is wise to monitor the effects of each type of mining operation on poverty alleviation. On the one hand, it appears that governance insufficiency has hampered possibilities for broader economic prosperity through large-scale mining investments. On the other hand, while artisanal mining is frequently condemned by scholars, the negative comments seem to be overly pessimistic, as this activity can be demonstrated to provide considerable economic opportunities for both the native and migrant populations.
ISSN: 0264-8377

hal-01303896
https://hal-univ-perp.archives-ouvertes.fr/hal-01303896
DOI : 10.1016/j.landusepol.2013.08.001

Éditeur(s) : HAL CCSD Lippincott, Williams & Wilkins
Résumé : PURPOSE OF REVIEW: Malaria represents one of the most important selective factors affecting human populations. Several inherited diseases of red blood cells lead to resistance at the erythrocytic stage. Among patients who experience hereditary elliptocytosis related to mutations of erythrocyte membrane proteins, molecular studies have shown the prevalence of particular spectrin mutations in patients from black ethnic extraction, leading one to question the selection of new malaria-resistant genes. RECENT FINDINGS: Prospective epidemiological and molecular studies in West Africa have confirmed the prevalence (between 0.6 and 1.6%) of particular spectrin mutations related to hereditary elliptocytosis. These studies have also revealed the frequency of alpha-spectrin chain polymorphisms, associated in cis with elliptocytogenic spectrin mutations and defining particular spectrin allele haplotypes. Culture studies of Plasmodium falciparum in elliptocytes bearing such elliptocytogenic alleles of spectrin showed that these alleles are supplementary genetic factors of malaria resistance in vitro. SUMMARY: Certain instances of spectrin mutations or polymorphisms have not yet been shown to constitute new factors of innate resistance to malaria in vivo. Epidemiological surveys of hereditary elliptocytosis and parasite culture studies, however, have argued that the relationships between parasite and spectrin-based skeleton should be examined more closely and the molecular interactions between parasite ligands and particular spectrin chain domains should be characterized.
ISSN: 1065-6251

inserm-00128119
http://www.hal.inserm.fr/inserm-00128119
http://www.hal.inserm.fr/inserm-00128119/document
http://www.hal.inserm.fr/inserm-00128119/file/Dhermy_et_al_figures.pdf
DOI : 10.1097/MOH.0b013e3280d21afd

Éditeur(s) : HAL CCSD Public Library of Science
Résumé : International audience
BACKGROUND: While a great number of papers have been published on the short-term effects of air pollution on mortality, few have tried to assess whether this association varies according to the neighbourhood socioeconomic level and long-term ambient air concentrations measured at the place of residence. We explored the effect modification of 1) socioeconomic status, 2) long-term NO2 ambient air concentrations, and 3) both combined, on the association between short-term exposure to NO2 and all-cause mortality in Paris (France).METHODS: A time-stratified case-crossover analysis was performed to evaluate the effect of short-term NO2 variations on mortality, based on 79,107 deaths having occurred among subjects aged over 35 years, from 2004 to 2009, in the city of Paris. Simple and double interactions were statistically tested in order to analyse effect modification by neighbourhood characteristics on the association between mortality and short-term NO2 exposure. The data was estimated at the census block scale (n=866).RESULTS: The mean of the NO2 concentrations during the five days prior to deaths were associated with an increased risk of all-cause mortality: overall Excess Risk (ER) was 0.94% (95%CI=[0.08;1.80]. A higher risk was revealed for subjects living in the most deprived census blocks in comparison with higher socioeconomic level areas (ER=3.14% (95%CI=[1.41-4.90], p extless0.001). Among these deprived census blocks, excess risk was even higher where long-term average NO2 concentrations were above 55.8 μg/m3 (the top tercile of distribution): ER=4.84% (95%CI=[1.56;8.24], p for interaction=0.02).CONCLUSION: Our results show that people living in census blocks characterized by low socioeconomic status are more vulnerable to air pollution episodes. There is also an indication that people living in these disadvantaged census blocks might experience even higher risk following short-term air pollution episodes, when they are also chronically exposed to higher NO2 levels
ISSN: 1932-6203

hal-01187406
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01187406
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01187406/document
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01187406/file/journal.pone.0131463.PDF
DOI : 10.1371/journal.pone.0131463

Éditeur(s) : HAL CCSD Société géologique de France
Résumé : International audience
– The 300 km long allochthonous sheet of oceanic mantle forming the New Caledonia ophiolite displays three specific characters: 1) the ophiolite pile lacks concordant sheeted dykes and pillow basalt layers; 2) the ophiolite, refered to as the Peridotite nappe, is thrusted over the basaltic formations of the Poya terrane which are classicaly thought to originate from a different oceanic environment; 3) The basal contact of the ultramafic sheet is remarkably flat all along New-Caledonia and the Peridotite nappe has not been thickened during obduction, rather it experienced significant extension. This suggests that the peridotites have not been emplaced by a tectonic force applied to the rear. New petrological and geochemical results obtained from mantle rocks finally show that the Poya terrane may originate from the same oceanic basin as the peridotites. In this article, we consider such possible cogenetic links and we propose a simple model for the obduction of the New Caledonia ophiolite in which the Poya basalts represent the original cover of the Peridotite nappe. We infer that continuous uplift of the subducted units buried beneath the oceanic lithosphere in the northern part of New Caledonia drove passive uplift of the ophiolite and led to erosion and to initiation of sliding of the basaltic layer. During the Priabonian (latest Eocene), products of the erosion of the basaltic layer were deposited together with sediments derived from the Norfolk passive oceanic margin. These sediments are involved as tectonic slices into an accretionary wedge formed in response to plate convergence. The volcaniclastic sedimentation ends up with the emplacement of large slided blocks of basalts and rafted mafic units that progressively filled up the basin. Obduction process ended with the gravity sliding of the oceanic mantle sheet, previously scalped from its mafic cover. This process is contemporaneous with the exhumation of the HP-LT units of Pouebo and Diahot. Gravity sliding was facilitated by the occurrence of a continuous serpentine sole resulting from metasomatic hydratation of mantle rocks, which developed during the uplift of the Norfolk basement and overlying Diahot and Pouébo units. Progressive emersion of the obducted lithosphere allowed subsequent weathering under subaerial, tropical conditions. Obduction passive et mise en place gravitaire des grandes nappes ophiolitiques : les ophiolites de Nouvelle-Calédonie (SW Pacifique) sont-elles un cas d'école ? Résumé. – La nappe de manteau de Nouvelle-Calédonie, s'étendant sur 300 km de long montre trois caractéristiques im-portantes: 1) La succession ophiolitique ne contient ni dykes, ni basaltes en coussin, 2) l'ophiolite est charriée sur des formations basaltiques (nappe de Poya) que l'on considère classiquement comme originaires d'un bassin océanique dif-férent de celui d'où est issu le manteau, et 3) le contact basal de la nappe ultrabasique est remarquablement plat tout le long de l'île et celle-ci n'a pas été épaissie durant l'obduction. Cela suggère que les péridotites n'ont pas été mises en place en réponse à une poussée tectonique arrière. De nouveaux résultats pétrologiques et géochimiques obtenus sur l'ophiolite montrent en réalité que les basaltes de Poya peuvent être extraits de la fusion du manteau de l'ophiolite. Nous proposons donc un nouveau modèle pour l'obduction, dans lequel les basaltes de Poya forment la couver-ture initiale primitive du manteau de la nappe des péridotites. La surrection progressive des unités profondes enfouies lors de la subduction de la lithosphère du bassin sud-Loyauté à l'Eocène, a permis le soulèvement passif de l'ophiolite et l'érosion puis le glissement des unités basaltiques. Durant le Priabonien, l'accumulation des produits de l'érosion de la couche des basaltes et de la marge passive de Norfolk ont formé les séquences de flysch comprenant localement des débris basaltiques grossiers. Ces sédiments font partie d'un prisme d'accrétion tectonique construit en réponse à la convergence au front de la subduction. La sédimentation détritique se termine par la mise en place de grandes unités ba-saltiques glissées qui comblent le bassin. Le processus de l'obduction se termine par le glissement gravitaire de l'écaille de manteau océanique sur les basaltes. Cet événement est contemporain de l'exhumation des unités HP-BT de Pouébo et du Diahot. Le glissement gravitaire a été facilité par la présence sous l'ophiolite, d'une semelle continue de serpentines résultant de l'interaction du manteau avec des fluides métasomatiques remontant durant l'exhumation des unités en-fouies pendant la subduction continentale. L'émersion progressive de la lithosphère obduite a placé le manteau dans des conditions d'altération supergène tropicale.
EISSN: 1777-5817

hal-01257702
https://hal.archives-ouvertes.fr/hal-01257702
https://hal.archives-ouvertes.fr/hal-01257702/document
https://hal.archives-ouvertes.fr/hal-01257702/file/Lagabrielleetal-BSGF-2012-revised-light.pdf
DOI : 10.2113/gssgfbull.184.6.545

Éditeur(s) : HAL CCSD American Geophysical Union
Résumé : International audience
We analyze the kinematics of fault tip folding at the front of a fold-and-thrust wedge using a sandbox experiment. The analog model consists of sand layers intercalated with low-friction glass bead layers, deposited in a glass-sided experimental device and with a total thickness h = 4.8 cm. A computerized mobile backstop induces progressive horizontal shortening of the sand layers and therefore thrust fault propagation. Active deformation at the tip of the forward propagating basal décollement is monitored along the cross section with a high-resolution CCD camera, and the displacement field between pairs of images is measured from the optical flow technique. In the early stage, when cumulative shortening is less than about h/10, slip along the décollement tapers gradually to zero and the displacement gradient is absorbed by distributed deformation of the overlying medium. In this stage of detachment tip folding, horizontal displacements decrease linearly with distance toward the foreland. Vertical displacements reflect a nearly symmetrical mode of folding, with displacements varying linearly between relatively well defined axial surfaces. When the cumulative slip on the décollement exceeds about h/10, deformation tends to localize on a few discrete shear bands at the front of the system, until shortening exceeds h/8 and deformation gets fully localized on a single emergent frontal ramp. The fault geometry subsequently evolves to a sigmoid shape and the hanging wall deforms by simple shear as it overthrusts the flat ramp system. As long as strain localization is not fully established, the sand layers experience a combination of thickening and horizontal shortening, which induces gradual limb rotation. The observed kinematics can be reduced to simple analytical expressions that can be used to restore fault tip folds, relate finite deformation to incremental folding, and derive shortening rates from deformed geomorphic markers or growth strata.
ISSN: 2169-9313

hal-00138061
https://hal.archives-ouvertes.fr/hal-00138061
https://hal.archives-ouvertes.fr/hal-00138061/document
https://hal.archives-ouvertes.fr/hal-00138061/file/Bernard_et_al-2007-Journalsur Geophysical_Research__Solid_Earth_%281978-2012%29.pdf
DOI : 10.1029/2005JB004149

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Acknowledging the high exposure of the region to natural and man-made disasters, this article emphasizes the need for the Institutions of Higher Education operating in the Caribbean to improve their level of preparedness and develop efficient mitigation plans. Based on their experience of the Disaster Resistant Universities initiative, the authors suggest a methodology to develop such plans adapted to the Caribbean context. A four-step risk assessment allows the definition and implementation of a hazard mitigation plan for the universities, along with table-top exercises critical for capacity building within the institution.
Reconnaissant le niveau d’exposition élevé de la zone Caraïbe aux catastrophes d’origines naturelle et anthropique, l’article souligne la nécessité pour les établissements d’enseignement supérieur implantés dans la région à la fois d’optimiser leur niveau de préparation face aux catastrophes, et de définir des plans opérationnels de réduction des risques. Sur la base de leur expérience de l’initiative « Universités Résistantes aux Catastrophes », les auteurs suggèrent une méthodologie de planification préventive adaptée au contexte caraïbe. Une évaluation des risques en 4 étapes autorise la mise en place d’un plan de réduction des risques ; le plan ainsi adopté par les universités devra être associé à la mise en œuvre de simulations essentielles au développement des savoir-faire au sein même de l’établissement
Reconociendo la alta exposición de la región a los desastres naturales y artificiales, este artículo da énfasis a la necesidad para las instituciones de educación superior que funcionan en la zona Caribe de mejorar su nivel del estado de preparación, y desarrollar planes eficientes de mitigación. De acuerdo con su experiencia de la iniciativa « Universidades Resistentes a los Desastres », los autores sugieren una metodología para desarrollar tales planes adaptados al contexto Caribeño. Una evaluación de los riesgos en cuatro etapas autoriza la implementación de un plan de reducción de los riesgos para las universidades, junto con las simulaciones esenciales al desarrollo de los conocimientos técnicos dentro del establecimiento.
Caraïbes

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.294
http://journals.openedition.org/etudescaribeennes/294

Éditeur(s) : HAL CCSD IOP Publishing
Résumé : The Bureau International des Poids et Mesures (BIPM), Sevres, France, hosted the 7th International Comparison of Absolute Gravimeters (ICAG) and the associated Relative Gravity Campaign (RGC) from August to September 2005.;ICAG 2005 was prepared and performed as a metrological pilot study, which aimed:;(1) To determine the gravity comparison reference values;;(2) To determine the offsets of the absolute gravimeters; and;(3) As a pilot study to accumulate experience for the CIPM Key Comparisons.;This document presents a complete and extensive review of the technical protocol and data processing procedures. The 1st ICAG-RGC comparison was held at the BIPM in 1980-1981 and since then meetings have been organized every 4 years.;In this paper, we present an overview of how the meeting was organized, the conditions of BIPM gravimetric sites, technical specifications, data processing strategy and an analysis of the final results. This 7th ICAG final report supersedes all previously published reports.;Readings were obtained from participating instruments, 19 absolute gravimeters and 15 relative gravimeters. Precise levelling measurements were carried out and all measurements were performed on the BIPM micro-gravity network which was specifically designed for the comparison.
ISSN: 0026-1394

hal-00644529
https://hal.archives-ouvertes.fr/hal-00644529
DOI : 10.1088/0026-1394/48/5/003

Éditeur(s) : HAL CCSD American Geophysical Union (AGU)
Résumé : International audience
The Pyrenean peridotites (lherzolites) form numerous small bodies of subcontinental mantle, a few meters to 3 km across, exposed within the narrow north Pyrenean zone (NPZ) of Mesozoic sediments paralleling the north Pyrenean Fault. Recent studies have shown that mantle exhumation occurred along the future NPZ during the formation of the Albian-Cenomanian Pyrenean basins in relation with detachment tectonics. This paper reviews the geological setting of the Pyrenean lherzolite bodies and reports new detailed field data from key outcrops in the Bearn region. Only two types of geological settings have to be distinguished among the Pyrenean ultramafic bodies. In the first type (sedimented type or S type), the lherzolites occur as clasts of various sizes, ranging from millimetric grains to hectometric olistoliths, within monogenic or polymictic debris flow deposits of Cretaceous age, reworking Mesozoic sediments in dominant proportions as observed around the Lherz body. In the second type (tectonic type or T type), the mantle rocks form hectometric to kilometric slices associated with crustal tectonic lenses. Both crustal and mantle tectonic lenses are in turn systematically associated with large volumes of strongly deformed Triassic rocks and have fault contacts with units of deformed Jurassic and Lower Cretaceous sediments belonging to the cover of the NPZ. These deformed Mesozoic formations are not older that the Aptian-early Albian. They are unconformably overlain by the Albian-Cenomanian flysch formations and have experienced high temperature-low pressure mid-Cretaceous metamorphism at variable grades. Such a tectonic setting characterizes most of the lherzolite bodies exposed in the western Pyrenees. These geological data first provide evidence of detachment tectonics leading to manle exhumation and second emphasize the role of gravity sliding of the Mesozoic cover in the preorogenic evolution of the Pyrenean realm. In the light of such evidence, a simple model of basin development can be inferred, involving extreme thinning of the crust, and mantle uprising along a major detachment fault. We demonstrate coeval development of a crust-mantle detachment fault and generalized gravitational sliding of the Mesozoic cover along low-angle faults involving Triassic salt deposits as a tectonic sole. This model accounts for the basic characteristics of the precollisional rift evolution in the Pyrenean realm.
ISSN: 0278-7407

hal-00512818
https://hal.archives-ouvertes.fr/hal-00512818
DOI : 10.1029/2009TC002588