Éditeur(s) : HAL CCSD Seismological Society of America
Résumé : International audience
Abstract The continuous record of large surface-rupturing earthquakes along the Dead Sea fault brings unprecedented insights for paleoseismic and archaeoseismic research. In most recent studies, paleoseismic trenching documents the late Holocene faulting activity, while tectonic geomorphology addresses the long-term behavior (>10 ka), with a tendency to smooth the effect of individual earthquake rupture events (Mw >7). Here, we combine historical, archaeological, and paleoseismic investigations to build a consolidated catalog of destructive surface-rupturing earthquakes for the last 14 ka along the left-lateral Jordan Valley fault segment. The 120- km-long fault segment limited to the north and the south by major pull-apart basins (the Hula and the Dead Sea, respectively) is mapped in detail and shows five subsegments with narrow stepovers (width < 3 km). We conducted quantitative geomorphology along the fault, measured more than 20 offset drainages, excavated four trenches at two sites, and investigated archaeological sites with seismic damage in the Jordan Valley. Our results in paleoseismic trenching with 28 radiocarbon datings and the archaeoseismology at Tell Saydiyeh, supplemented with a rich historical seismic record, document 12 surface-rupturing events along the fault segment with a mean interval of ∼1160 yr and an average 5 mm=yr slip rate for the last 25 ka. The most complete part of the catalog indicates recurrence intervals that vary from 280 yr to 1500 yr, with a median value of 790 yr, and suggests an episodic behavior for the Jordan Valley fault. Our study allows a better constraint of the seismic cycle and related short-term variations (late Holocene) versus long-term behavior (Holocene and late Pleistocene) of a major continental transform fault.
ISSN: 0037-1106

hal-00747401
https://hal.archives-ouvertes.fr/hal-00747401
DOI : 10.1785/0120100097

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Comme dans d’autres régions du monde, la croissance démographique et l’aménagement côtier sur le littoral acadien au Nouveau-Brunswick contribuent à une plus grande vulnérabilité et à la détérioration des espaces côtiers et environnements littoraux. L’élévation du niveau marin et les effets des changements climatiques rendent les côtes du Nouveau-Brunswick extrêmement sensibles et entrainent des impacts de plus en plus importants. Ainsi, l’adaptation aux changements climatiques constitue un enjeu de taille pour la province.Nous décrivons ici les résultats d’une étude comparative sur les expériences et les stratégies d’adaptation de deux communautés côtières, les communautés de Cocagne - Grande Digue et de Beaubassin-Est - Cap Pelé. Les deux territoires ont en commun d’avoir des littoraux convoités par le tourisme et le secteur immobilier. Des entretiens semi-dirigés et des groupes de discussion (focus groups) ont permis d’obtenir des informations sur les thématiques suivantes : l’expérience des modifications environnementales, les mesures d’adaptation initiées individuellement ou collectivement, les réactions et les besoins futurs. Les résultats de l’étude mettent en évidence l’enchâssement des aspects économiques et sociétaux dans les enjeux environnementaux et le rôle des représentations et des acteurs qui déterminent le niveau de mobilisation. Enfin, le projet souligne l’importance d’une coordination entre les différentes échelles de gouvernance.
As in other parts of the world, population growth and coastal planning on New Brunswick’s Acadian coastline are contributing to greater vulnerability and deterioration of the natural environment. The rise in sea level and the effects of climate change make the coasts of New Brunswick extremely sensitive, leading to impacts that are increasingly larger. Thus, adaptation to climate change is a major challenge for the province.Here, we describe the results of a comparative study of the experiences and coping strategies of two coastal communities: Cocagne – Grande-Digue and Beaubassin East – Cap-Pelé. Both these territories attract tourism and real estate investors. Semi-structured interviews and focus groups were used to obtain information on the following topics: the experience of environmental change, adaptation measures initiated individually or collectively, reactions and future needs. Results of the study highlight the entrenchment of economic and societal aspects of environmental issues and the role of representations and stakeholders that determine the level of mobilization. Finally, the project emphasizes the importance of coordination between the different levels of governance.
Acadie
Nouveau-Brunswick

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.6663
http://journals.openedition.org/etudescaribeennes/6663

Éditeur(s) : Société Nationale de Protection de la Nature
Résumé : Monitoring of French Polynesia coral reefs and their recent development.-French Polynesia, consisting of 118 islands in the centre of the Pacific Ocean, has more than 15 000 km(2) of reefs and lagoons managed by the local government. Tourism and pearl culture are the two main economic resources of the country. Polynesian coral reefs are extremely diverse and are among those for which we have thorough knowledge. The exploitation of local resources has been recorded for multiple decades and includes : coral materials, fishing, harvest and export of mother-of-pearl molluscs, pearl production, and ornamental fish. All over the country, many monitoring programmes have been launched to measure the health of reefs and the natural and anthropogenic perturbations that they suffer : hurricanes and seismic events, water quality, health of benthic and fish communities, pearl oyster pathology and radiobiology. These data, collected over the last few decades, allowed to define the relative importance of natural and anthropogenic degradation on reefs and lagoons, and to explain the present status of reefs at different spatial scales. Devastating hurricanes are rare (1903-1906, 1982-1983 and occasionally at other times), but they may annihilate outer slope coral communities on some islands. Bleaching events with considerable coral mortality at different geographical scales occurred mainly in 1991, 1994 and 2003. Outbreaks of Acanthaster destroyed numerous reefs (lagoons and outer slopes) from 1978-1982 and a new demographic wave began in 2006 at many Society islands. Eutrophication events only occurred occasionally and only in some lagoons. Whereas natural catastrophic events degrade the coral reef ecosystem across many islands, at the archipelago or even regional scale, anthropogenic degradation is limited to a few Society Islands, occurring rarely on atolls and not at all on those (one third) which are uninhabited. The main causes of reef degradation in some areas of Tahiti and Moorea include the embankment of fringing zones, coral mining, overfishing, absence of urban sewage treatment and the development of leisure and tourism activities. Because of its large geographical extent, one may conclude that major reef degradation in French Polynesia is caused by catastrophic natural events. On the other hand, anthropogenic degradation is more localized. Unfortunately, the synergistic effects of these causes of degradation prevent reefs from recovering. Optimum coral cover on French Polynesian outer reef slopes is between 50-60%. After a major destructive impact (hurricane, bleaching, Acanthaster) a reef is reduced to less than 10% coral cover, however if no more major disturbance events occur a reef will recover in about 12 years. Most of the 15 000 km(2) of reefs and lagoons in French Polynesia are in good health, and along with their neighbouring reefs in East and Central Pacific they are considered as the least degraded reefs worldwide and at a low risk of becoming degraded in the few next decades. However, we are more and more anxious about the future of reefs in the world particularly because present simulations predict that major impacts of climate change would include : elevation of sea surface temperatures, increase in the strength of hurricanes and acidification of seawater which will affect the formation of coral structures.
La Polynésie française, 118 îles au coeur du Pacifique, possède une surface de plus de 15 000 km2 de récifs et lagons gérés par le gouvernement polynésien. Le tourisme et la perliculture représentent les deux ressources économiques majeures du Pays. Les formations récifales très diversifiées sont parmi les mieux connues. Plusieurs suivis d'exploitation des ressources sont opérationnels depuis des décennies : granulats coralliens, pêche pour l'alimentation, collecte et exportation de mollusques nacriers, production de perles, poissons d'ornement. À l'échelle du Pays de très nombreux programmes de surveillance de l'état des récifs et des perturbations qu'ils subissent, naturelles et anthropiques, ont été mis en place : perturbations cycloniques et sismiques, qualité des eaux, état de santé des peuplements benthiques et ichtyologiques, pathologie des nacres, radiobiologie. Toutes ces données recueillies au fi l des décennies ont permis d'établir l'importance relative des dégradations naturelles et anthropiques sur les récifs et lagons polynésiens et d'expliquer leur état de santé actuel en considérant différentes échelles spatiales. Les périodes cycloniques dévastatrices pour les récifs sont rares (1903-1906, 1982-1983 et épisodiquement) mais les cyclones ont parfois anéanti les communautés coralliennes de pentes externes dans certaines îles. Les blanchissements suivis de mortalités importantes à des échelles spatiales diverses, ont été surtout ceux de 1991, 1994 et 2003. Les explosions démographiques d'Acanthaster ont détruit de nombreux récifs (lagons et pentes externes) en 1978-1982 et une nouvelle pullulation s'amplifie depuis 2006 dans plusieurs îles de la Société. Les crises dystrophiques n'ont perturbé qu'épisodiquement certains lagons. [...]
Revue d'Ecologie de la Terre et de la Vie (0249-7395) (Société Nationale de Protection de la Nature), 2008 , Vol. 63 , N. 1-2 , P. 145-177

Droits : 2008 Société Nationale de Protection de la Nature
http://archimer.ifremer.fr/doc/2008/publication-4558.pdf
http://archimer.ifremer.fr/doc/00000/4558/

Éditeur(s) : HAL CCSD Oxford University Press (OUP)
Résumé : International audience
The mantle above a subducting slab is the site of complex interactions between deformation, partial melting, fluid migration and magma transport. To constrain these interactions and their effects on olivine deformation, we analyze microstructures, crystal preferred orientations, and water contents of peridotite xenoliths entrained by andesites of the Avacha volcano, southern Kamchatka arc. These xenoliths are refractory spinel harzburgites that have coarse-grained microstructures with widely spaced subgrain boundaries and sinuous grain boundaries in olivine, consistent with deformation by dislocation creep under low deviatoric stress (< 13 MPa) and with a significant contribution from diffusional processes. Analysis of crystal preferred orientations (CPO) indicates dominant activation of high-temperature, low-stress {0kl}[100] slip systems in olivine and of(100)[001] in orthopyroxene. In most samples, coarse opx crystals, elongated parallel to the lineation, enclose small olivine grains in crystallographic continuity with neighbouring crystals, indicating crystallization of orthopyroxene at the expense of olivine as a result of reactive percolation of Si-rich fluids coeval with the high-temperature deformation. Secondary crystallization of interstitial orthopyroxene led locally to development of opx-rich lenses parallel to the foliation, characterized by a decrease in olivine grain size and dispersion of the olivine CPO without changing the dominant slip systems. Half of the samples also show acicular orthopyroxene aggregates with which is associated a fine-grained matrix composed of rounded strain-free olivine, orthopyroxene, spinel, and rare amphibole crystals. This matrix occurs pervasively along grain boundaries or forms millimeter-scale irregular lenses and anastomosing veinlets that crosscut the coarse crystals and their ductile deformation structures. Both acicular orthopyroxene and the fine-grained matrix are interpreted as resulting from reactive transport of H2O-rich fluids under static conditions, probably in the lithospheric mantle. Infrared analyses show that olivine contains 1-8 center dot 6 ppm by weight of water. These low water contents are similar to those observed in spinel peridotites from other subduction zones and probably record both the low solubility of water in olivine at low pressure and dehydration during exhumation of the xenoliths. Water contents in orthopyroxene are highly variable (25-506 ppm H2O), probably recording spatially heterogeneous interaction with fluids or melts and compositional disequilibrium in the studied samples. Change in the dominant percolation mechanism from porous flow to fracturing suggests cooling, consistent with the low temperatures estimated from pyroxene thermometry (< 800-900 degrees C). The Avacha xenoliths therefore record pervasive deformation of a region of the mantle under asthenospheric conditions, followed by its accretion to the base of the lithosphere, probably as a result of cooling of the mantle wedge. Percolation of Si-rich fluids or hydrous melts is recorded at all stages; this probably enhanced diffusion and lowered deviatoric stresses during ductile deformation, but did not change the dominant slip direction in olivine from [100] to [001].
ISSN: 0022-3530

hal-00456053
https://hal.archives-ouvertes.fr/hal-00456053
DOI : 10.1093/petrology/egp085

Éditeur(s) : HAL CCSD Springer Verlag
Résumé : International audience
We show here that the Amalaoulaou complex, in the Pan-African belt of West Africa (Gourma, Mali), corresponds to the lower and middle sections of a Neoproterozoic intra-oceanic arc. This complex records a 90-130-Ma-long evolution of magmatic inputs and differentiation above a subducting oceanic slab. Early c. 793 Ma-old metagabbros crystallised at lower crustal or uppermost mantle depths (25-30 km) and have geochemical characteristic of high-alumina basalts extracted from a depleted mantle source slightly enriched by slab-derived sedimentary components ((La/Sm)(N) < 1; epsilon(Nd): +5.4-6.2; Sr-87/Sr-86: 0.7027-0.7029). In response to crustal thickening, these mafic rocks were recrystallised into garnet-granulites (850-1,000A degrees C; 10-12 kbar) and subject to local dehydration-melting reactions, forming trondhjemititic leucosomes with garnet-clinopyroxene-rutile residues. Slightly after the granulitic event, the arc root was subject to strong HT shearing during partial exhumation (detachment faults/rifting or thrusting), coeval with the emplacement of spinel- and garnet-pyroxenite dykes crystallised from a high-Mg andesitic parental magma. Quartz and hornblende-gabbros (700-660 Ma) with composition typical of hydrous volcanic rocks from mature arcs ((La/Sm)(N): 0.9-1.8; epsilon(Nd): +4.6 to +5.2; Sr-87/Sr-86: 0.7028-0.7031) were subsequently emplaced at mid-arc crust levels (similar to 15 km). Trace element and isotopic data indicate that magmas tapped a depleted mantle source significantly more enriched in oceanic sedimentary components (0.2%). Exhumation occurred either in two stages (700-660 and 623 Ma) or in one stage (623 Ma) with a final exhumation of the arc root along cold P-T path (550A degrees C, 6-9 kbar; epidote-amphibolite and greenschist facies conditions) during the main Pan-African collision event (620-580 Ma). The composition of magmas forming the Cryogenian Amalaoulaou arc and the processes leading to intra-arc differentiation are strikingly comparable to those observed in the deep section of exposed Mezosoic oceanic arcs, namely the Kohistan and Talkeetna complex. This evolution of the Amalaoulaou oceanic arc and its accretion towards the West African craton belong to the life and closure of the Pharusian Ocean that eventually led to the formation of the Greater Gondwana supercontinent, a similar story having occurred on the other side of the Sahara with the Mozambique Ocean.
ISSN: 0010-7999

hal-00639447
https://hal.archives-ouvertes.fr/hal-00639447
DOI : 10.1007/s00410-011-0624-5

Résumé : On August 18th, 1967, H.M. Arvid Pardo, Malta's delegate at the UN, referred to the General Assembly with the question entitled: "Examination of the question of the reservation exclusively for peaceful purposes of the sea-bed and the ocean floor, and the subsoil thereof, underlying the high seas beyond the limits of present national jurisdiction, and the use of their resources in the interests of mankind." (1) This proposal was not the result of pure abstract thinking, but was, on the contrary, the wording of the necessity to adapt marine legislation to the current development state of the international society. However, this evolutive perspective does not exist only economically and technically speaking: it develops in the political field, especially in the development of the nations claim over marine spaces and the genesis of the principle of freedom of high seas. As in any dialectical perspective, legislation interferes with these de facto situations and imposes a number of directions to the study of a legal regime responding to the needs of a changing international society.
Le 18 août 1967, SE Arvid PARDO, représentant de Malte à l'ONU, saisit l'Assemblée Générale de la question intitulée : "Examen de la question de l'affectation à des fins exclusivement pacifiques du lit des mers ainsi que de leur sous sol, au-delà des limites de la juridiction nationale actuelle et de l'exploitation de leurs ressources dans l'intérêt de l'humanité". (1) Cette proposition n'était pas l'émanation d'une réflexion purement abstraite, mais traduisait au contraire la nécessité d'adapter le droit de la mer à l'état de développement de la société internationale. Cependant, cette perspective évolutive n'existe pas seulement sur le plan économique et technologique : elle se développe au niveau politique, particulièrement dans l'extension des prétentions étatiques sur les espaces maritimes et la genèse du principe de liberté de la haute mer. Comme dans toute perspective dialectique, le droit interfère sur ces situations de fait et impose donc a priori certaines orientations à l'étude d'un régime juridique répondant aux besoins d'une société internationale en pleine mutation. [OCR NON CONTRÔLE]

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/1973/rapport-4803.PDF
http://archimer.ifremer.fr/doc/00000/4803/

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : This paper aims to explore the complex relationships between international tourism and the production and exchange of 'nature' in tropical countries. It is based on data gathered through an ethnographic case study approach on the changing aesthetic, economic and symbolic values attached to the coral reef in the tropical island of La Réunion, Indian Ocean. The analysis of this data shows that, from the point where the collective imaginaries in the Western world associate a 'magic' value with corals, an international institutionalisation process takes place in order to protect and preserve coral reefs and make them touristically accessible. This raises important issues related to the challenges the new value of tropical nature represents for the communication and exchange systems of communities in tropical countries. The paper first explores the meanings of the spiritual and religious value Western societies attribute to coral reefs. It then discusses the institutionalisation of tropical nature by international organisations and the problem of parallel land and natural space ownership systems in La Réunion. After that, it deconstructs the mystification policy of the coral reef operated by local institutions in La Réunion and examines the meaning of protecting the coral reef as a socially embedded 'communicative action' in La Réunion.
L’objectif de cette étude est d’explorer les relations complexes entre d'une part le tourisme international et d'autre part la production et l'échange de 'nature' dans des pays tropicaux. L'étude est basée sur des données recueillies à travers une approche ethnographique des valeurs esthétiques, économiques et symboliques attachées au récif corallien de l'île de La Réunion, dans l'océan Indien. L'analyse de ces données montre qu'à partir du moment où les imaginaires collectifs de l'Occident associent les coraux à une valeur 'magique', un processus d'institutionnalisation internationale s’engage dans le but de protéger, préserver et rendre accessibles au tourisme les récifs coralliens. Ceci implique des problématiques importantes liées à la mise à l'épreuve des systèmes de communication et d'échange des sociétés dans les pays tropicaux. L'étude explore d'abord la signification des valeurs spirituelles et religieuses qu'attribuent les sociétés occidentales aux récifs coralliens. Ensuite, elle discute l'institutionnalisation de la nature tropicale par des organisations internationales ainsi que le problème de l'existence de différents systèmes de gestion foncière à La Réunion. Enfin, l'étude déconstruit la politique de mythification du récif corallien mise en œuvre par des institutions locales à La Réunion et examinera la signification de 'protéger l'environnement' en tant qu'action communicante définie par les systèmes de communication et d'échange réunionnais.
Réunion

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.1112
http://journals.openedition.org/etudescaribeennes/1112

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
During the last decade, the interaction of deep processes in the lithosphere and mantle with surface processes (erosion, climate, sea-level, subsidence, glacio-isostatic readjustment) has been the subject of heated discussion. The use of a multidisciplinary approach linking geology, geophysics, geodesy, modelling, and geotechnology has led to the awareness of coupled deep and surface processes. Deep earth dynamics (topography, erosion, tectonics) are strongly connected to natural hazards such as earthquakes, landslides, and tsunamis; sedimentary mass transfers have important consequences on isostatic movements and on georesources, geothermal energy repartitions. The ability to read and understand the link between deep Earth dynamics and surface processes has therefore important societal impacts. Ground-truthing at carefully-selected sites of investigation is imperative to better understand these connections.Due to its youth (<30 Ma) and its subsidence history, the almost land-locked Gulf of Lion–Sardinia continental margins system provides a unique record of sedimentary deposition from the Miocene to present. Due to its high subsidence rate, palaeoclimatic variations, tectonic events and vertical evolution are all recorded here at very high resolution. The late Miocene isolation and desiccation of the Mediterranean, the youngest and most catastrophic event, the Messinian Salinity Crisis (MSC), induced drastic changes in marine environments: widespread deposition of evaporite (gypsum, anhydrite and halite) in the central basin, and intense subaerial erosion along its periphery. These extraordinary mass transfers from land to sea induced strong isostatic re-adjustments that are archived in the sedimentary record and represent a window to the lithospheric rheology and the deep processes.The GOLD (Gulf of Lion Drilling) project, proposes to explore this unique sedimentary record as well as the nature of the deep crustal structure, providing valuable information about the mechanisms underlying vertical motions in basins and their margins.
ISSN: 0264-8172

insu-01197393
https://hal-insu.archives-ouvertes.fr/insu-01197393
https://hal-insu.archives-ouvertes.fr/insu-01197393/document
https://hal-insu.archives-ouvertes.fr/insu-01197393/file/Rabineau%20et%20al.-final-MPG2014_REVISED-FINAL-No-Marked_FINAL%2BFigures.pdf
DOI : 10.1016/j.marpetgeo.2015.03.018

Éditeur(s) : HAL CCSD Réseau « Développement durable et territoires fragiles »
Résumé : La Trame verte et bleue (TVB), nouveau dispositif d'action publique visant à enrayer la perte de biodiversité traduit un renouvellement des référentiels de justification des politiques de conservation et de leur stratégie territoriale. Il s'agit d'intégrer la planification écologique dans l'aménagement de l'ensemble du territoire. Le processus de territorialisation de la TVB met en rapport de multiples niveaux de décision et d'action imbriqués. Il crée de ce fait des configurations inédites de complexité et d'incertitude et implique des innovations en termes de gouvernance que le cadre analytique de la gouvernance adaptative permet d'appréhender. En nous appuyant sur l'exemple du Parc Naturel Régional des Volcans d'Auvergne, nous analysons le rôle que ces institutions sont susceptibles de jouer dans ces dynamiques de changement et d'apprentissage socio-technique et politique qui conditionnent une mise en œuvre effective de la TVB.
Développement Durable et territoires

hal-00979610
https://hal-agroparistech.archives-ouvertes.fr/hal-00979610

Éditeur(s) : HAL CCSD
Résumé : Genetic structure of Hylesia metabus (Lepidoptera: Saturniidae), moths responsible for lepidopterism outbreaks in French Guiana and Venezuela. . ICE 2016; XXV International Congress of Entomology
ICE 2016; XXV International Congress of Entomology
Orlando, United States

hal-01607289
https://hal.archives-ouvertes.fr/hal-01607289
DOI : 10.1603/ICE.2016.113657
PRODINRA : 396124

Éditeur(s) : HAL CCSD Geological Society of London
Résumé : We have applied transmission electron microscopy (TEM) analyses coupled with viscoplastic self-consistent (VPSC) numerical modelling to identify the active slip systems and to better understand the crystal preferred orientation (CPO) development of the Torridon quartz mylonite (NW Scotland). TEM analyses showed evidence of activation of 1/3〈a〉{π′}, 1/3〈a〉{z} and possible 〈a〉(c) slip systems, as well as dislocation climb and dynamic recrystallization. All the CPOs generated by VPSC models share common characteristics with the Torridon quartz mylonite, but only Models 2 and 3 reproduce the [c]-axes maxima at low angle (<20°) to the foliation pole along the YZ plane, as observed in the mylonite. In Model 2, this concentration only occurs at γ≥2.6, whereas in Model 3 this maxima occurs at lower shear strains. The models that start with a previous preferred orientation acquire very strong CPOs after small-imposed strains, followed by the rapid rotation of the fabric in relation to the new imposed finite strain axes. The combined activation of 〈a〉{π′}, 〈a〉{z} and possibly 〈a〉(c) slip systems, as demonstrated by TEM analyses, suggests that the VPSC model that best predicts CPO development in the Torridon quartz mylonite is Model 2, where the critical resolved shear stress (CRSS) of 〈a〉{π/π′} is assumed to be slightly stronger than 〈a〉(c).
Deformation Mechanisms, Rheology and Tectonics: Microstructures, Mechanics and Anisotropy

hal-00688840
https://hal.archives-ouvertes.fr/hal-00688840

Éditeur(s) : HAL CCSD Geological Society of America
Résumé : International audience
Because of its essential role in coupling climate and tectonics, denudation is a key parameter when constraining the history of Earth’s surface. This is particularly true at the Pliocene-Pleistocene transition, and the potential impact of the onset of Quaternary glaciations remains strongly debated. In the present study, we measured in situ cosmogenic 10Be within continuous late Cenozoic sedimentary sections that had already been dated using magnetostratigraphy. The new data were obtained from four sedimentary basins in the northern and southern Tianshan range (Central Asia). We first thoroughly discuss how in situ cosmogenic 10Be concentrations can be corrected for radioactive decay and for the contribution of postdepositional cosmogenic accumulation to derive the paleo–denudation rates. Our analysis shows that, in the four sedimentary records, the potential bias remains low enough to consider the derived denudation rates reliable. The four records, although likely influenced by local particularities due to lithological heterogeneity and local tectonics, display similar trends of continuously increasing denudation between ca. 9 Ma and the present. These rates have remained relatively high but steady since 4 Ma, ∼1.5 m.y. before the onset of the Quaternary glacial cycles. Though the rejuvenation of the Tianshan range since 11 Ma may explain most of the progressive increase (×5) in denudation, our data suggest that the Quaternary glaciations had only a limited impact on denudation in the Tianshan. Our data, however, indicate an increase in the spatial and high-frequency variability (<1 m.y.) of the denudation rates between 3 and 1 Ma. This may correspond to a transient readjustment of the landscape in response to the onset of Quaternary glacial cycles.
ISSN: 0016-7606

hal-01685766
https://hal.archives-ouvertes.fr/hal-01685766
DOI : 10.1130/B31475.1

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : La vulnérabilité croissante aux aléas extrêmes et les conséquences du changement climatique accentuent l’exposition des Antilles françaises aux risques naturels. Dans ce contexte, la Caisse Centrale de Réassurance par son rôle dans l’indemnisation des Catastrophes naturelles en France cherche à consolider ses connaissances sur les ouragans et les phénomènes induits comme les submersions, les inondations ou les glissements de terrain.À partir des archives antillaises et métropolitaines, une reconstruction de l’intensité des ouragans survenus depuis le début du xviie siècle a été possible. Elle permet ainsi d’évaluer l’exposition des territoires antillais. L’analyse des dommages a permis de proposer une évaluation des enjeux et ainsi saisir la construction de la vulnérabilité. Les réponses apportées en matière de gestion du risque depuis le xviie attestent de la volonté d’assurer la protection des enjeux et des populations et mettent en avant les relations entre risque et aménagement du territoire.
The rising vulnerability to Extreme hazard and the consequences of climate change increase the exposure of French Antilles to natural hazards. Therefore, the French reinsurance company Caisse Centrale de Réassurance aims to develop its scientific knowledge of hurricanes and induced phenomena like storm surges, floods and landslides.With the study of historical archives, located in the Antilles and Metropolitean France, it was possible to build an exhaustive hurricane Severity chronology since the 17th century. Then, a detailed damage analysis in specific strategic areas has offered the opportunity to assess the evolution of the vulnerability of the French Antilles societies. Furthermore, the Risk Management policies, since the 17th century, attest the willingness to protect strategic areas and populations and highlight the link between risk and land use.
Martinique
Guadeloupe
Saint-Martin
Saint-Barthélemy

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.7176
http://journals.openedition.org/etudescaribeennes/7176

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Cette étude originale a vocation à montrer comment un mysticisme authentique s’est formé au fil des siècles en Guadeloupe. Les Antilles sont composées de nombreuses ethnies, aux origines très diversifiées. En Guadeloupe, la société s’est constituée à partir de deux vagues de migrations, qui ont formé une société pluri-ethnique et pluri-culturelle. Ces vagues de migrations se sont inscrites dans un double processus de mondialisation, l’un historique, figé dans le temps, l’autre dynamique, encore effectif de nos jours. La confrontation et la cohabitation de ces ethnies et de ces cultures ont conduit à l’avènement de pratiques mystiques authentiquement guadeloupéennes. Ainsi, le mysticisme est devenu partie prenante de la culture guadeloupéenne, culture encore en construction, qui n’a pas encore soudé en un syncrétisme franc les pratiques des différentes communautés ; chaque individu choisissant, en fonction de ses nécessités, de se référer ou d’appliquer telle ou telle pratique mystique.
This study shows how an authentic mysticism arose in Guadeloupe. The West Indies are made up of many ethnic groups. In Guadeloupe, the society has been constituted by two waves of migrations; so far this society has been pluri-ethnic and pluri-cultural. Those waves reveal a two dimension globalization: the first is historical, likely to be identified in our history, the second is dynamic and is still expanding nowadays. The cohabitation of these ethnic groups and these cultures has led to the creation of an authentic Guadeloupean mysticism. Thus mysticism is important in the Guadeloupean culture. However there has not been syncretism between all the mysticisms of every ethnic group; and every one can choose the mysticism they want, and change whenever they want.
Guadeloupe

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.5940
http://journals.openedition.org/etudescaribeennes/5940

Éditeur(s) : HAL CCSD
Résumé : International audience
La question des langues dans les espaces créoles français n'échappe pas au chercheur qui entreprend de saisir le fonctionnement de ces collectivités humaines singulières pour en proposer une intelligence à ses contemporains. Sans entrer dans un débat scientifique purement linguistique, il apparaît difficile d'éluder le développement général de ce thème dans les départements d'outre-mer, ainsi que ses répercussions dans les espaces publics concernés. L'extension des usages du créole dynamise en l'élargissant, la recherche sur l'objet, même si la diffusion de résultats reste encore trop modeste. L'explosion de phénomènes liés à ce que l'on a pris coutume d'appeler la modernité (urbanisation, communication, etc.) travaillent nos sociétés en profondeur. Une approche fine des processus de changement que connaissent ces aires appelle une élucidation incontournable du réel linguistique. La question des langues dans nos sociétés ne laisse pas le chercheur en Sciences humaines et sociales, indifférent d'autant que le thème déborde les seuls aspects de la recherche en linguistique. Il suffit pour s'en convaincre, d'en observer l'écho médiatique (local/national), la proximité avec les discours sur l'identité culturelle, ou encore les formes du débat sur l'enseignement du créole dans différents champs (presse, discours politique, domaine intellectuel et scientifique). Entamer un travail de déconstruction des statuts et des représentations associés aux langues en présence permettrait sans doute de fournir des éléments de réponse. Dans cette perspective, le présent texte se veut porteur d'une contribution épistémologique. Il pose la question linguistique dans les univers créoles français (et singulièrement aux Antilles) de manière résolument critique. Sa prétention vient de l'urgence de dépassionner un débat d'importance pour nos sociétés dans la mise au jour d'un acteur social créole capable de faire face aux défis toujours plus complexes qui se présentent à lui. L'idée même d'un acteur social créole devrait d'ailleurs, occuper une place essentielle dans notre activité de recherche. Ainsi, à travers le couple langues/sociétés, nous nous proposons d'observer les rapports qu'entretiennent la recherche en linguistique et l'espace public, de cerner les figures diverses que prend le sujet-chercheur et enfin, d'éclairer les enjeux sociaux de la recherche scientifique dans nos aires créoles. 1. La créolistique : un apport de la recherche en linguistique L'ampleur du débat public sur le créole dans nos sociétés, avec parfois ses glissements paroxysmiques a de quoi surprendre. C'est que le débat dont aucun observateur avisé ne se plaindra, demeure intrinsèquement lié aux points de Olivier PULVAR 168 crispation qui se manifestent dans l'opinion (relayée par certains de ses leaders) quant à l'existence d'un créole écrit, aux modalités de son écriture et, aux critères de sa généralisation dans le cadre de son enseignement comme langue. Il renvoie pourtant, aux concepts que pratiquent couramment les chercheurs en linguistique : normalisation, standardisation ou encore aménagement linguistique. On comprend la complexité mais aussi l'impérieuse nécessité d'une clarification pour le non spécialiste. S'initier au travail du linguiste, approcher le contexte sociolinguistique en espaces créolophones, saisir la posture des chercheurs créolistes, représentent autant d'étapes qui, autorisent une approche plus sereine du problème. L’article propose d’interroger les rapports qu’entretiennent la recherche sur les faits de langue et l’espace public dans les Outremers français créolophones.
Philologica Jassyensia

hal-01152995
https://hal.archives-ouvertes.fr/hal-01152995

Éditeur(s) : HAL CCSD Geological Society of America
Résumé : International audience
his study describes the structural setting, petrogenesis, and geochronology of a suite of acidic magmatic rocks that are intruded in the metamorphic core of the Tertiary ophiolitic suture zone of the Sabzevar Range, NE central Iran. These intrusive bodies show tabular geometries with solid-state fabrics documenting syntectonic emplacement during crustal shortening. In the total alkalis-silica (TAS) diagram, their compositions define a medium-K calc-alkaline suite, spanning from basaltic andesite to the dacite and rhyolite fields. They show characteristic low MgO (0.15–0.60 wt%) and Ni (<20 ppm), high Sr contents, a negligible Eu anomaly, and extremely fractionated rare earth element (REEs), with high La/Yb and Sr/Y (up to 900) ratios, but very low Yb and Y contents. They also show zircon Hf isotope compositions compatible with a mid-ocean-ridge basalt (MORB)–type oceanic crust. Inverse and forward thermobarometry constrains conditions of magma crystallization in the upper-pressure field of the amphibolite facies (ca. 1.2–1.5 GPa and 750 °C). Integrated U-Pb zircon and 40Ar/39Ar white mica and amphibole geochronology constrains the Sabzevar magmatism to the late Paleocene (at ca. 58 Ma). Genesis of the Sabzevar magmatic suite is interpreted in terms of prograde, wet amphibolite melting during oceanic subduction, within a pressure-temperature range between a plagioclase-out and a hornblende-out boundary. Magma differentiation and high-pressure amphibole fractionation of pristine slab melts are proposed as the dominant factors that imparted the adakite signature in the Sabzevar structural zone. Implications in terms of the regional tectonic scenario are discussed and framed within the advancing and retreating evolution of the Neotethyan subduction during the Mesozoic–Tertiary time span.
ISSN: 0016-7606

hal-01122824
https://hal.archives-ouvertes.fr/hal-01122824
DOI : 10.1130/B30913.1

Éditeur(s) : Blackwell science
Résumé : The trophic level mean and variance, and the degree of omnivory for five Celtic Sea fish predators were estimated using a database of stomach content records characterized by a high level of taxonomic resolution. The predators occupied a high position in the food web, i.e. 4.75 for Atlantic cod Gadus morhua, 444 for haddock Melanogrammus aeglefinus, 4.88 for European hake Merluccius merluccius, 5.00 for megrim Lepidorhombus whiffiagonis and 5.27 for whiting Merlangius merlangus. The level of taxonomic resolution of the prey did not greatly affect mean T-L predator values; an effect on variance was evident, low resolution masking intra-population variability in T-L. Generalized additive models (GAM) were used to explain the variability of predator T-L caused by environmental variables (international Council for the Exploration of the Sea, ICES, division and season) and predator characteristics (total length, L-T). Significant year, location season and interaction effects were found for some species and with L-T, at the scale of ICES subdivision. The species-specific variability of T-L could be due to spatio-temporal variations in prey availability and in predator selectivity following ontogenetic changes. Omnivorous fish T-L. was less affected by spatio-temporal variations. In addition, results showed that the omnivory index and T-L variability provide dissimilar information on predator feeding strategy. Combining information on T-L. variability and omnivory allowed between within individual and between-individual components contributing to trophic niche width to be separated and the type of generalization of fish predators to be identified. (c) 2008 The Authors Journal compilation (c) 2008 The Fisheries Society of the British Isles.
Journal of Fish Biology (0022-1112) (Blackwell science), 2008-09 , Vol. 73 , N. 4 , P. 763-781

Droits : 2008 Wiley Blackwell Publishing, Inc. The Fisheries Society of the British Isles
http://archimer.ifremer.fr/doc/2008/publication-4699.pdf
DOI:10.1111/j.1095-8649.2008.01938.x
http://archimer.ifremer.fr/doc/00000/4699/

Éditeur(s) : HAL CCSD Réseau « Développement durable et territoires fragiles »
Résumé : The Green and Blue infrastructure (Trame verte et bleue –TVB) is a new conservation policy tool based on the notions of ecological network and corridor. The introduction of this new instrument through the French Grenelle environment commitments brings about some change in the spatial strategy of the conservation policy. Beyond the identification of priority conservation areas, ecological planning of all the territory is concerned. The TVB’s implementation process establishes the connection of multi and nested decisional and action levels. It thus creates specific situations of complexity and uncertainty that require innovation and perpetual change of governance. The study of the Auvergne region case through the adaptive governance analytical framework highlights the potential fruitful role of Regional nature parks in such dynamics of change and learning. Mots-clés : aménagement durable des territoires, biodiversité, réseau écologique, corridor écologique, gouvernance adaptative, socio-écosystème, trame verte et bleue Keywords : Sustainable landplaning, Biodiversity, Ecological network, Adaptive governance, socio-ecosystem
La Trame verte et bleue (TVB), nouveau dispositif d’action publique visant à enrayer la perte de biodiversité traduit un renouvellement des référentiels de justification des politiques de conservation et de leur stratégie territoriale. Il s’agit d’intégrer la planification écologique dans l’aménagement de l’ensemble du territoire. Le processus de territorialisation de la TVB met en rapport de multiples niveaux de décision et d’action imbriqués. Il crée de ce fait des configurations inédites de complexité et d’incertitude et implique des innovations en termes de gouvernance que le cadre analytique de la gouvernance adaptative permet d’appréhender. En nous appuyant sur l’exemple du Parc Naturel Régional des Volcans d’Auvergne, nous analysons le rôle que ces institutions sont susceptibles de jouer dans ces dynamiques de changement et d’apprentissage socio-technique et politique qui conditionnent une mise en œuvre effective de la TVB.
ISSN: 1772-9971

hal-01195370
https://hal.archives-ouvertes.fr/hal-01195370
DOI : 10.4000/developpementdurable.9675
PRODINRA : 269288

Éditeur(s) : HAL CCSD
Résumé : International audience
Up-to-date estimates of the health outcomes of preterm children are needed for assessing perinatal care, informing parents, making decisions about care, and providing evidence for clinical guidelines. To determine survival and neonatal morbidity of infants born from 22 through 34 completed weeks' gestation in France in 2011 and compare these outcomes with a comparable cohort in 1997. The EPIPAGE-2 study is a national, prospective, population-based cohort study conducted in all maternity and neonatal units in France in 2011. A total of 2205 births (stillbirths and live births) and terminations of pregnancy at 22 through 26 weeks' gestation, 3257 at 27 through 31 weeks, and 1234 at 32 through 34 weeks were studied. Cohort data were collected from January 1 through December 31, 1997, and from March 28 through December 31, 2011. Analyses for 1997 were run for the entire year and then separately for April to December; the rates for survival and morbidities did not differ. Data are therefore presented for the whole year in 1997 and the 8-month and 6-month periods in 2011. Survival to discharge and survival without any of the following adverse outcomes: grade III or IV intraventricular hemorrhage, cystic periventricular leukomalacia, severe bronchopulmonary dysplasia, retinopathy of prematurity (stage 3 or higher), or necrotizing enterocolitis (stages 2-3). A total of 0.7% of infants born before 24 weeks' gestation survived to discharge: 31.2% of those born at 24 weeks, 59.1% at 25 weeks, and 75.3% at 26 weeks. Survival rates were 93.6% at 27 through 31 weeks and 98.9% at 32 through 34 weeks. Infants discharged home without severe neonatal morbidity represented 0% at 23 weeks, 11.6% at 24 weeks, 30.0% at 25 weeks, 47.5% at 26 weeks, 81.3% at 27 through 31 weeks, and 96.8% at 32 through 34 weeks. Compared with 1997, the proportion of infants surviving without severe morbidity in 2011 increased by 14.4% (P < .001) at 25 through 29 weeks and 6% (P < .001) at 30 through 31 weeks but did not change appreciably for those born at less than 25 weeks. The rates of antenatal corticosteroid use, induced preterm deliveries, cesarean deliveries, and surfactant use increased significantly in all gestational-age groups, except at 22 through 23 weeks. The substantial improvement in survival in France for newborns born at 25 through 31 weeks' gestation was accompanied by an important reduction in severe morbidity, but survival remained rare before 25 weeks. Although improvement in survival at extremely low gestational age may be possible, its effect on long-term outcomes requires further studies. The long-term results of the EPIPAGE-2 study will be informative in this regard.
ISSN: 2168-6211

hal-01258705
http://hal.univ-brest.fr/hal-01258705
PUBMED : 25621457
DOI : 10.1001/jamapediatrics.2014.3351

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The volume comprises some of the contributions presented during the 10th edition of the Alpine Meeting "CorseAlp 2011". It has been held in Saint Florent (Corsica) between 10th and 16th of April 2011 under the auspices of Societé Geologique de France, Società Geologica Italiana and the INGV (Istituto Nazionale di Geofisica e Vulcanologia) and with the collaboration of colleagues of Université de Corse (M.-M. Spella, M. and J. Ferrandini and L. Ciancaleoni) and the support of the city council of S. Florent. The meeting was framed in the series of "Alpine Workshops" e.g., Siegesmund et al. (2008), Handy and Rosenberg (2011), which are held every two years to develop interdisciplinary research on Alpine-type orogens. It hosted a variety of topical sessions from regional geology to process-oriented field and laboratory studies and gave the opportunity to collect multidisciplinary and multiscale approaches to geodynamic studies including continental rifting and ocean opening, oceanic and continental subduction, late- to post orogenic extension, exhumation of deep seated rocks, back-arc opening and microcontinent rotation, interfering orogenic-scale tectonics and surface processes, tectonics and seismic hazard within the Alpine chain and Mediterranean realms.
ISSN: 0040-1951

hal-00795580
https://hal.archives-ouvertes.fr/hal-00795580