Éditeur(s) : Ieee-inst Electrical Electronics Engineers Inc
Résumé : We validate Soil Moisture and Ocean Salinity (SMOS) sea surface salinity (SSS) retrieved during August 2010 from the European Space Agency SMOS processing. Biases appear close to land and ice and between ascending and descending orbits; they are linked to image reconstruction issues and instrument calibration and remain under study. We validate the SMOS SSS in conditions where these biases appear to be small. We compare SMOS and ARGO SSS over four regions far from land and ice using only ascending orbits. Four modelings of the impact of the wind on the sea surface emissivity have been tested. Results suggest that the L-band brightness temperature is not linearly related to the wind speed at high winds as expected in the presence of emissive foam, but that the foam effect is less than previously modeled. Given the large noise on individual SMOS measurements, a precision suitable for oceanographic studies can only be achieved after averaging SMOS SSS. Over selected regions and after mean bias removal, the precision on SSS retrieved from ascending orbits and averaged over 100 km $times$ 100 km and 10 days is between 0.3 and 0.5 pss far from land and sea ice borders. These results have been obtained with forward models not fitted to satellite L-band measurements, and image reconstruction and instrument calibration are expected to improve. Hence, we anticipate that deducing, from SMOS measurements, SSS maps at 200 km $times$ 200 km, 10 days resolution with an accuracy of 0.2 pss at a global scale is not out of reach.
Ieee Transactions On Geoscience And Remote Sensing (0196-2892) (Ieee-inst Electrical Electronics Engineers Inc), 2012-05 , Vol. 50 , N. 5 , P. 1662-1675

Droits : 2012 IEEE
http://archimer.ifremer.fr/doc/00074/18557/16108.pdf
DOI:10.1109/TGRS.2012.2184546
http://archimer.ifremer.fr/doc/00074/18557/

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The thermal evolution of sediments in the shallowest part of sedimentary basins is challenging to investigate as most of the geothermometers are at their application limits. This is typically the case of the Callovian-Oxfordian claystones at the eastern border of the Paris Basin. A recent 2000 m deep well penetrated the entire Jurassic and Triassic sedimentary series and permitted coring of sediments never reached by previous drilling in this part of the basin. Thanks to the use of several independent geothermometers (apatite fission track thermochronology, fluid inclusion microthermometry, clay mineralogy and sedimentary organic matter evolution) the burial history of the Mesozoic series has been reconstructed, modeled and calibrated using kinetic algorithms relevant to the various paleothermometers used. In addition to these conventional methods, an innovative approach was developed using the temperature-dependence of the magnetic mineral assemblage within clay-rich sediments ("MagEval"). Thermal modeling indicates that the Callovian-Oxfordian and the Lower Triassic experienced maximum burial temperatures of 50 +/- 5 C-circle and 90 +/- 10 C-circle respectively, i.e., about 25 C higher than present-day. This temperature offset implies the erosion of several hundred meters of sediments which, depending on the thermal flux and conductivity considered, most likely constituted Upper Cretaceous chalk deposits. Falling sea level resulted in the exposure and subsequent dismantling of the chalk cover at the beginning of Cenozoic times. The eastern border of the basin was then subjected to slow erosion and discrete tectonic deformation.
ISSN: 0264-8172

hal-01313142
https://hal.archives-ouvertes.fr/hal-01313142
DOI : 10.1016/j.marpetgeo.2013.08.019

Éditeur(s) : HAL CCSD Université des Antilles
Résumé : International audience
The power of attraction of the islands is well established, between the power of intangible resources fed by representations built over time and specific natural and cultural resources of these territories borders. Tourism then appears as an undeniable opportunity. However, the singular territorial context that the island must be considered to weigh the issues of tourism development and opening to the world. In this context it is necessary to develop efficient indicators to measure the sustainability of the tourism project as well as the development of the tourism sector which is only one step (and not an end in itself) in the opening process the island.
Le pouvoir d’attraction des îles n’est plus à démontrer, entre la puissance des ressources intangibles nourries par des représentations construites au fil du temps et les ressources naturelles et culturelles spécifiques de ces territoires de confins. Le tourisme apparait alors comme une opportunité indéniable. Néanmoins le contexte territorial singulier qui fait l’île doit être pris en considération pour bien mesurer les enjeux du développement touristique et l’ouverture sur le monde. Dans ce contexte, il convient de se doter d’indicateurs efficients pour mesurer la soutenabilité du projet touristique sans oublier que le développement du secteur touristique n’est qu’une étape (et non une fin en soi) dans le processus d’ouverture de l’île.
ISSN: 1779-0980

hal-00987544
https://hal-univ-corse.archives-ouvertes.fr/hal-00987544

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Magnetic Resonance Imaging (MRI), a reference examination for cardiac morphology and function in humans, allows to image the cardiac right ventricle (RV) with high spatial resolution. The segmentation of the RV is a difficult task due to the variable shape of the RV and its ill-defined borders in these images. The aim of this paper is to evaluate several RV segmentation algorithms on common data. More precisely, we report here the results of the Right Ventricle Segmentation Challenge (RVSC), concretized during the MICCAI'12 Conference with an on-site competition. Seven automated and semi-automated methods have been considered, along them three atlas-based methods, two prior based methods, and two prior-free, image-driven methods that make use of cardiac motion. The obtained contours were compared against a manual tracing by an expert cardiac radiologist, taken as a reference, using Dice metric and Hausdorff distance. We herein describe the cardiac data composed of 48 patients, the evaluation protocol and the results. Best results show that an average 80% Dice accuracy and a 1cm Hausdorff distance can be expected from semi-automated algorithms for this challenging task on the datasets, and that an automated algorithm can reach similar performance, at the expense of a high computational burden. Data are now publicly available and the website remains open for new submissions (http://www.litislab.eu/rvsc/).
ISSN: 1361-8415

hal-01141170
https://hal.archives-ouvertes.fr/hal-01141170
PUBMED : 25461337

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Le pouvoir d’attraction des îles n’est plus à démontrer, entre la puissance des ressources intangibles nourries par des représentations construites au fil du temps et les ressources naturelles et culturelles spécifiques de ces territoires de confins. Le tourisme apparait alors comme une opportunité indéniable. Néanmoins le contexte territorial singulier qui fait l’île doit être pris en considération pour bien mesurer les enjeux du développement touristique et l’ouverture sur le monde. Dans ce contexte, il convient de se doter d’indicateurs efficients pour mesurer la soutenabilité du projet touristique sans oublier que le développement du secteur touristique n’est qu’une étape (et non une fin en soi) dans le processus d’ouverture de l’île.
The power of attraction of the islands is well established, between the power of intangible resources fed by representations built over time and specific natural and cultural resources of these territories borders. Tourism then appears as an undeniable opportunity. However, the singular territorial context that the island must be considered to weigh the issues of tourism development and opening to the world. In this context it is necessary to develop efficient indicators to measure the sustainability of the tourism project as well as the development of the tourism sector which is only one step (and not an end in itself) in the opening process the island.

Droits : info:eu-repo/semantics/openAccess
http://journals.openedition.org/etudescaribeennes/6363

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The deep structure and deformation mechanisms of the Longmen Shan thrust belt (Sichuan, China), at the eastern border of the Tibetan plateau, were largely debated after the devastating Mw 7.9 Wenchuan earthquake (2008). Recent geophysical studies and field investigations have been focused on the active motion of the major Beichuan fault, which ruptured during the earthquake. However, the total exhumation across the fault still remains unclear. In the hanging wall of the Beichuan fault, the South China block is exhumed in the Pengguan massif. Close to the Beichuan fault, the rocks of the Pengguan massif underwent greenschist facies metamorphism associated with brittle-ductile deformation. No metamorphism is observed in the footwall of the fault. In this study, we characterize and date the metamorphic history recorded in the hanging wall of the Beichuan fault in order to constrain the depth and timing of exhumation of the rocks of the Pengguan massif along the fault. A high-resolution petrological approach involving chemical analyses and X-ray maps was used to analyze the micrometric metamorphic minerals. The P-T conditions of the greenschist facies metamorphic event were estimated by an inverse multi-equilibrium thermodynamic approach. The results, 280 ± 30 °C and 7 ± 1 kbar, suggest that the rocks of the Pengguan massif were exhumed from ca. 20 km depth. Our results underline the importance of the thrusting component in the long-term behavior of the Beichuan fault and provide a minimal depth at which the fault is rooted. In situ laser ablation 40Ar/39Ar dating of metamorphic white mica revealed that the greenschist overprint occurred at 135–140 Ma.The Pengguan massif was therefore partially thrusted along the Beichuan fault during the Lower Cretaceous, long before the Eocene-Miocene exhumation phase which is well-constrained by low-temperature thermochronology. Our results provide the first independent depth information for the exhumation history of the Pengguan massif and reveal a previously undocumented Lower Cretaceous tectonic event that marks the onset of the thick-skinned deformation in the external domain of the Longmen Shan (East of the Wenchuan Fault).
ISSN: 0743-9547

hal-01685556
https://hal.archives-ouvertes.fr/hal-01685556
DOI : 10.1016/j.jseaes.2017.04.003

Éditeur(s) : Littoral 2004, Aberdeen, Scotland, UK, September 2004
Résumé : NAMIBIE (a french acronym for Integrated Multimedia Navigator Within Coastal Environment Data Bases) is a specific tool which first concept has been established by Ifremer and has been developped by an association between research in the field of coastal environment, innovation in the field of new information and communication technologies and services in the field of coastal integrated management and impact studies. The objectives of this tool are to facilitate research, direct access and display of relevant multimedia coastal integrated data and information according to an interactive, widely opened and playfull interface. The principles are based upon the fact that sustainable decision making needs an optimized unterstanding of coastal processes and better consultation between actors. In this purpose the development of the tool has considered that the end-user should and could be free to look after the data and the information he needs for a particular site or environment of interest and for a specific ICZM question according to easy navigation interfaces. That is why NAMIBIE concept is based upon : - a coherent 3D representation of the coasts (i.e. from catchement areas to continental shelf and deep sea), which considers a coherent DEM from land to sea and textural representation of the environment using satellite imagery textural displays, - a 3D navigator which allows the user to fly or dive over and within the coastal environment of interest, - a multimedia database (text, graphs, image, maps, geographic objects, modelling results...) specific to the territory of interest, - an interactive interface which helps in finding relevant information associated to specific questions. The technologies used include VRML data format, integration of standard GIS format (shp, grid, img) within the navigator, integration and display of modelling data. The production chain is realized in C++ and Java scripts allow dialogue between web pages and 3D windows. Applications are presented on the coasts of Languedoc Roussillon region (French Mediterranean border) in the framework of ICZM problematics

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/00089/20055/17696.pdf
http://archimer.ifremer.fr/doc/00089/20055/

Éditeur(s) : HAL CCSD American Geophysical Union (AGU)
Résumé : Extensional fault systems in the Earth's crust can exhibit two end-member geometries that we identify as distributed and localized faulting regimes. A satellite image analysis of fault populations from the Main Ethiopian Rift-Afar area reveals that the rift architecture contains these two faulting regimes. The occurrence of these regimes reveals a jump in the scale of fault segmentation and linkage. Strain localization at rift border zones exhibits particularly large-scale fault linkage and a power law size distribution. This regime replaces prior distributed fault systems, showing small-scale fault linkage and an exponential size distribution. The distributed faulting is interpreted as confined to the thick trap basalt carapace. We show that continental fault systems can develop by a combination of these two geometries, and we demonstrate how to quantitatively decipher the jump between them.
ISSN: 0278-7407

hal-00411147
https://hal.archives-ouvertes.fr/hal-00411147
DOI : 10.1029/2007TC002148

Éditeur(s) : HAL CCSD Taylor & Francis (Routledge)
Résumé : International audience
The Maroni basin, an isolated region delineating the border between Suriname and French Guiana has been affected by the human immunodeficiency virus (HIV) epidemic 10 years after coastal French Guiana. However, the rise in HIV prevalence was sharp, exceeding 1% within 10 years. The aim of the present study is to compare, using the first quantitative data from the general population in remote villages, the knowledge, attitudes, and behaviors regarding HIV between Maroon and Amerindian populations, the two most frequent populations living along the Maroni. Data were collected in 2012 using a structured questionnaire among a random sample of 896 individuals residing in the remote villages on the Maroni river. Proportions were compared between the Maroni and the coastal general population, and between Maroon and Amerindian populations. The present study shows significant differences between territories and between communities living on the Maroni river: the multiple sexual partnerships, more common among population living on the Maroni river, were more frequently reported in Maroons than in Amerindians. Condom use was more frequently reported among men on the Maroni river than on the coast, but these findings were reversed for women. Moreover, among people living on the Maroni river, condom use was more frequently reported among Maroons than among Amerindians. Regarding genital factors that may affect transmission, penile implant seemed to have no ethnic boundaries, steam baths seemed specific to Maroon women. The present results should help to improve community-based specific interventions.
ISSN: 0954-0121

hal-01260915
https://hal.archives-ouvertes.fr/hal-01260915
https://hal.archives-ouvertes.fr/hal-01260915/document
https://hal.archives-ouvertes.fr/hal-01260915/file/2015%2C%20Van%20Melle%20-%20Knowledge%2C%20attitudes%2C%20behaviors%2C%20and%20practices%20differences%20regarding%20HIV.pdf
DOI : 10.1080/09540121.2015.1032203

Éditeur(s) : HAL CCSD Elsevier
Résumé : Different types of fractures and fault rocks occur within the major normal fault zones bordering the NW of the Neogene Penedes basin (NE Spain). In the southwest part of the basin, the main fault is the Baix Penedes fault that places the Upper Jurassic-Lower Cretaceous dolomicrites of the footwall in contact with the Miocene siliciclastic sediments of the hangingwall. Within the footwall damage zone, different fracture systems and their respective associated breccias and cements have been recognized. Using a combination of structural, petrologic and geochemical analyses, we show that these fracture systems evolved from mainly tectonic to mainly karstic features during the progressive development and upward propagation of the fault. The earlier fractures and associated breccias represent the initial stages of the fault propagation, when the process zone formed around the fault tip was dominated by dilatant fracturing (fractures 1 and dilatant breccias B1). The fluid involved in this early deformation precipitated the dolomite cement Cl, in equilibrium with the host-rock in a closed hydrogeological system. Localization of frictional processes generated cataclasites and ultracataclasites along distinct second-order faults (fractures 2). In these fractures, the dolomite cement C2 precipitated in relation to the incipient opening of the hydrological system to percolating meteoric waters. The later fractures and associated breccias represent the late stages of the fault propagation. These structures (fractures 3, fractures 4 and the dilatant breccias B2) were formed when the extensional deformation reached the surface, resulting in an increasingly open hydrogeological system. At these stages, deposition of the dolomitic sediment DS and precipitation of the calcite cements C3, C4 and C5 show the circulation of freshwaters in a vadose meteoric environment, i.e. in karstic conditions.
ISSN: 0375-6742

hal-00512690
https://hal.archives-ouvertes.fr/hal-00512690
DOI : 10.1016/j.gexplo.2009.11.010

Éditeur(s) : HAL CCSD
Résumé : International audience
Suriname is the smallest country in South America. However, in regional academic literature, it has been repeatedly considered one of the largest Caribbean territories for many years (Best 1967; Granger 2008). This territory is generally included in the socio-historical group of the three Guianas (Lézy 2000), or the bio-geographical group of the Guiana Plateau. Additionally, Suriname is frequently considered part of the insular Caribbean (Girvan 2005). The latter consideration implies a geographical paradox that is twofold. In fact, Suriname, French Guiana and Guyana are not directly bordered by the Caribbean Sea. Moreover, like Belize, which is also commonly included in the Caribbean island group, Suriname is not an island in the strict sense of the word, i.e. land surrounded by water, based on the restricted definition of the term. Nevertheless, the Caribbean cannot be defined today on the sole basis of a deterministic relationship with the sea bearing the same name. Further, research conducted on insularity increasingly demonstrates the limitations of the physical nature of the island, in favour of feelings of belonging, alienation, etc. (Taglioni 2003).
Caribbean Atlas

hal-01244081
http://hal.univ-reunion.fr/hal-01244081
http://hal.univ-reunion.fr/hal-01244081/document
http://hal.univ-reunion.fr/hal-01244081/file/Suriname.pdf

Éditeur(s) : HAL CCSD
Résumé : International audience
The increasing development of world trade has promoted the spread of diseases. Recent events, like the H1N1 outbreak and spread, have confirmed this tendency. Everyone could observe that this kind of infectious disease often has the ability to cross countries borders and spread rapidly. Preventing, monitoring and controlling the outbreak of these diseases have appeared to be a public health problem of primary importance for years. However, although numerous works have been conducted in order to understand and study epidemics, this subject remains a topical issue because of the complexity of the phenomena. In this paper, we present new opportunities offered by the field of social networks for understanding the spread of infectious diseases. This work focuses both on techniques already used in epidemiology, and very recent works in social network analysis that open new perspectives. We give an overview of methods currently used to model and study the spread of diseases and future directions that the social network approach allows to glimpse.
2011 Fifth International Conference on Research Challenges in Information Science (RCIS)
Gosier, Guadeloupe

hal-00624364
https://hal.archives-ouvertes.fr/hal-00624364
DOI : 10.1109/RCIS.2011.6006866

Éditeur(s) : Elsevier Science Bv
Résumé : The Danube River Basin–Black Sea area represents a unique natural laboratory for studying the interplay between lithosphere and surface as well as source to sink relationships and their impact on global change. This paper addresses some information on the “active sink” of the system; i.e. the Danube deep sea fan and the Black Sea basin. The present study focuses on the distal sedimentary processes and the evolution of sedimentation since the Last Glacial Maximum. This is investigated through recently acquired long piston coring and shallow seismic data recovered at the boundary of influence of the distal part of the Danube turbidite system (to the north-west) and the Turkish margin (to the south). This dataset provides a good record of the recent changes in the sedimentary supply and climato-eustasy in the Black Sea region during the last 25 ka. This study demonstrates that the deep basin deposits bear the record of the Late Quaternary paleoenvironmental changes and that the western Black Sea constitutes an asymmetric subsident basin bordered by a northern passive margin with confined, mid-size, mud-rich turbidite systems mainly controlled by sea-level, and a southern turbidite ramp margin, tectonically active. Highlights ► Oceanographic results from survey carried out in the western Black Sea are presented. ► The Danube fan distal part: the Black Sea main depositional feature is described. ► This study is on the morphology and gravity sedimentation in the Black Sea deep basin. ► Data were collected at the boundary between the Danube fan and the Turkish margin. ► The dataset provide a good record of sedimentary supply and climato-eustatic changes.
Global And Planetary Change (0921-8181) (Elsevier Science Bv), 2013-04 , Vol. 103 , P. 232-247

Droits : 2012 Elsevier B.V. All rights reserved.
http://archimer.ifremer.fr/doc/00095/20637/18272.pdf
DOI:10.1016/j.gloplacha.2012.05.002
http://archimer.ifremer.fr/doc/00095/20637/

Éditeur(s) : HAL CCSD Elsevier
Résumé : The current interpretation of the Messinian Salinity Crisis (MSC) involves the deposition of the so-called “peripheral or marginal” evaporites in onshore basins, as well as the erosion of the margins and the formation of thick evaporites in the deep parts of the basins. The present study focuses on intermediate depth basins, i.e. located between the onshore outcrops and the deep basins. Indeed, the Balearic Promontory shows small stepped basins filled with MSC deposits between its western extremity on the Alicante shelf and its eastern end around the Menorca block. New and already available seismic reflection profiles and onshore data allow us to investigate the nature and geometrical relationships of these deposits in the area between the islands of Ibiza and Mallorca.Our observations suggest the existence of three MSC-related units in this area. The lowermost transparent seismic unit can be interpreted as a 100 to 200-m-thick salt layer deposited in the deepest part of the Central Mallorca Depression. These evaporites pass laterally and upward into a thin-bedded seismic unit, which could be lithologically equivalent to the Upper Evaporites of the deep basins. All around the borders of the Central Mallorca Depression, this bedded seismic unit onlaps a Slope Unit which shows bedded to chaotic and rafted facies. The Messinian continental shelf is eroded and incised by a valley extending from the Palma onshore area to the Mallorca downslope domain.Our results suggest the presence offshore of at least two generations of diachronous MSC deposits. The observation of salt on a continental high and the widespread MSC deposits on the margins of the Central Mallorca Depression call into question the location of halite preferentially in the deep abyssal basins and the significance of the deep basin MSC units that onlap onto the Margin Erosional Surface (MES), as observed all around the passive margins of the Northwest-Mediterranean Basin. The dual terminology used for peripheral/deep MSC evaporites cannot be applied to any of the MSC units found in the study area.
ISSN: 0025-3227

hal-01115656
https://hal.archives-ouvertes.fr/hal-01115656
DOI : 10.1016/j.margeo.2014.10.001

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Le Bénin, pays de l’Afrique de l’Ouest est confronté à la destruction des terres humides particulièrement dans la partie sud du pays. Les terres humides riches biodiversité sont importantes tant pour les humains que pour milieu naturel. La menace la plus importante est la pression de l’anthropique. Même si ce territoire est reconnu par la Convention Ramsar, la destruction continue. En 1995 le gouvernement a décidé de créer une aire de gestion communautaire pour ces territoires. L’objectif de cette recherche est de comprendre les grands défis liés à la mise en œuvre de la gestion communautaire des milieux humides à travers une étude de cas, en l’occurrence celui de la vallée du Sitatunga. Pour atteindre cet objectif, un séjour de 3 mois a été effectué sur le site. Des entrevues semi-dirigées ont été alors réalisées. Les résultats montrent que la vallée du Sitatunga est considérée comme inutile, voire nuisible, par les populations riveraines rencontrées dans le cadre de l’étude, qui sont davantage préoccupées à se sortir de leur état de pauvreté. Les traditions et valeurs autrefois attribuées à la conservation des milieux humides ont quasiment disparu et l’individualisme est grandissant. Il importe de tenir compte de tous ces facteurs pour espérer véritablement préserver ces milieux. D’un autre côté, parlant de gestion de l’environnement et plus particulièrement de gestion des milieux humides à l’échelle béninoise, le constat n’est pas reluisant. En effet, l’État étant donné son état de sous-développement et donc de manque de ressources, à du mal à coordonner ces activités. Il est de même pour les ONG. La situation est accentuée par l’état des relations entre ONG et structures de l’État qui se considèrent davantage comme des adversaires que comme des partenaires ce qui affecte l’efficacité des activités menées. Pour que la gestion communautaire devienne une réalité, il importe qu’un partenariat soit établi entre les différents acteurs liés à la gestion de la vallée du Sitatunga en particulier et des milieux humides en général : les ONG, l’État et les communautés locales.
Bénin, a country in West Africa is actually facing the destruction of its wetlands, especially those in the southern part of the country. The wetlands which their richness in natural resources are important for both human and wildlife are also threatened by many factors. The most important threat is population pressure. Although recognised as Ramsar sites, the destruction continues. In 1995, the Government has decided to create community protected areas in this part of the country. The objective of this research is to understand the main challenges around the community management of wetlands. The case of the Sitatunga valley, in south Bénin has been studied. The methodology used consisted on interviews with stakeholders during a period of 3 months. The results show that, although the good intentions of community management, its practical application is not easy, and reveal many difficulties in its practical application. The site although rich in biodiversity and used as refuge for several species, is regarded as useless even harmful by the bordering populations, which are more worried by their poverty state. The traditions and values formerly allotted to the wetlands almost disappeared and individualism is growing. It is important to take into account all these factors to truly hope to preserve these wetlands. The study shows that management of the wetlands on a Beninese scale is also difficult. Indeed, the government through its structures struggles to coordinate its activities. It is the same for NGOs. The situation is accentuated by the poor relations between NGOs and government institutions which consider each other more as adversaries than as partners. This affects the effectiveness of the undertaken activities. It is then important for all the stakeholders (NGOs, Government and local communities) to install a partnership to help achieve community management objectives.
Bénin

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.3630
http://journals.openedition.org/etudescaribeennes/3630

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : L’exploitation commerciale des produits forestiers non ligneux a animé et anime encore au plan international les débats sur la gestion durable des forêts, notamment par son apport en matière de conservation, d’amélioration des conditions d’existence des populations locales et de gestion participative. Cependant, l’exploitation commerciale des PFNL soulève la problématique de la durabilité tant au plan écologique, économique que sociopolitique. La présente recherche traite de cette problématique en prenant comme PFNL d’illustration le raphia dans la forêt marécageuse Hlanzoun. Elle vise à analyser la durabilité socio-économique et environnementale de l’exploitation du raphia dans la forêt marécageuse « Hlanzoun ». La méthodologie utilisée est une combinaison d’approches quantitatives et qualitatives. Les outils d’analyse de données utilisés sont entre autre, la statistique descriptive, l’analyse filière des revenus d’exploitation et des valeurs ajoutées et l’analyse du système socio-écologique. Nos résultats montrent que le raphia est une plante à usages multiples. Que ce soit les feuilles, les fibres, la sève ou le tronc, tout ou presque peut être valorisé sur le raphia. Au niveau des villages riverains du Hlanzoun l’exploitation de la sève du raphia et sa transformation en alcool alimentaire est de loin le type d’usage qui procure le plus de revenu malgré le fait que les autres types d’usages mobilisent un nombre plus important d’acteurs. L’exploitation commerciale de ce PFNL se déploie suivant une organisation relativement simple et avec des caractéristiques propres à la plupart des activités de la petite production marchande des économies sous-développées en crise. Cette exploitation est essentiellement articulée autour des coupeurs/collecteurs, des intermédiaires commerciaux, des agents de transformation/conditionnement et des consommateurs des produits finis. La contribution annuelle totale de la filière raphia au développement a été estimée à 192 429 633 Fr. CFA (environ 385 000 dollar) et les revenus d’exploitation de tous les acteurs ont un signe positif malgré le faible niveau de technologie et de formation. Le raphia apporte donc des revenus relativement importants aux divers acteurs en dépit des handicaps de la filière et du déficit d’équité dans la répartition des richesses produites. Au plan de la gouvernance, on note un déficit d’instances, de règles et de procédures, dont l’effectivité et la légitimité sont clairement établies. Cet état de chose laisse le parc à raphia dans un régime d’accès « libre » mais seulement pour les riverains ; nous nous retrouvons donc en présence d’un système de cueillette, caractérisé par l’exploitation de plants immatures et la surexploitation, mettant en péril la capacité de renouvellement de la ressource et même l’avenir de la filière. On note cependant un effort de contrôle de l’accès des non riverains et des tentatives d’adaptation des riverains. En effet, le nombre d’exploitants est passé de 148 à 92 entre 2008 et 2010 et le nombre de pieds de raphia saignés est passé de 15 452 à 8 832 durant la même période. Au total, l’exploitation du raphia dans le Hlanzoun s’inscrit dans un environnement défavorable par rapport aux exigences de développement durable d’une filière de PFNL. Mais les divers acteurs sont à présent conscients de la nécessité d’agir pour une meilleure réglementation de l’accès et de l’exploitation.
The commercial use of non woody forest products is a crucial issue in the international debate on the sustainable management of forests. These products are supposed to contribute to conservation by improving local populations’ livelihood and their involvement in forest management. This study lies within the scope of two South-South Cooperation projects (PSC 22P07 and PSC 03T08) implemented by the CEBEDES NGO with the financial support of the Kingdom of the Netherlands. It aims at analyzing the socioeconomic and environmental sustainability of the raffia stands management in the swamp forest "Hlanzoun ". This small forest is located in one of Benin southern Wetlands in the municipality of Zogbodomey.The methodology to assess raffia socioeconomic performances relies on the estimation of the values added within the raffia value chains. Stakeholders at every segment of the value chains have been surveyed on the incomes obtained out of raffia. The methodology to assess the sustainability of the management relies on a simple indicator measuring the ratio of younger to elder palms. Palms in stands have been counted according to their age group. The survey confirms that raffia is a multi-purpose plant used for its leaves, fibers, sap and trunk. In villages at the borders of the Hlanzoun forest, harvesting the raffia sap on standing palms and processing it into alcohol are a major income generating activity. Alcohol is then marketed through a network of collectors, wholesalers and petty traders up to the consumers. The contribution of raffia to local and regional development was estimated by the total incomes generated at 192.429.633 F CFA. All stakeholders earn positive and significant incomes in spite of the low level of technology and skills, but traders receive a large share of the wealth produced. As regard to governance, "free" access only concerns residents and efforts are made to control the access of non-residents. One notes a deficit of legitimated authorities, rules and procedures for a sustainable use: Restrictions on the harvest of immature palms are not anymore enforced and it endangers the renewal capacity of the resource. But at the same time, the number of operators seems to be decreasing (from 148 to 92 between 2008 and 2010, whereas the number of harvested raffia palms decreased from 15,452 to 8,832 during the same period). A self-regulation might occur, due to the fact that a livelihood of local people relies on a diversity of income generating activities. In total, the operation of Raffia in Hlazoun is in an unfavorable environment with the requirements of sustainable development in a sector of NTFF. But the various actors are now aware of the need for action to better regulate access and operation.
Bénin

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.5556
http://journals.openedition.org/etudescaribeennes/5556

Éditeur(s) : Elsevier Sci Ltd
Résumé : The eastern Demerara Plateau offshore French Guiana was surveyed in 2003 during the GUYAPLAC cruise (multibeam bathymetry and acoustic imagery, 6-channel seismic reflection and 3.5 kHz echo-sounding). The data show the "post-transform" Cenozoic that the series located on the outer part of the plateau (below c. 2000 m) contain at least twelve stacked mass transport deposits (MTDs) that have recorded a history of large-scale slope failure, as well as two main normal fault sets that provide possible pathways for upward fluid migration through the series, reaching at high as the uppermost MTDs. Seabed data show that the area above the failures is characterized by circular-to-elongate (slope-parallel) depressions interpreted as fluid seeps (pockmarks), some of them have been modified by along slope currents. We suggest that the development of the MTDs to results from the combinaiton of the presence of fluid overpressure at depth the geometry of the margin's deep structure, in particular the existence of a 'free borderlateral border' on the outermost plateau. Our results also emphasise the role of stratigraphic decollements within the Cenozoic series.
Marine And Petroleum Geology (0264-8172) (Elsevier Sci Ltd), 2013-09 , Vol. 46 , P. 287-303

Droits : 2013 Elsevier Ltd. All rights reserved.
http://archimer.ifremer.fr/doc/00157/26850/25316.pdf
DOI:10.1016/j.marpetgeo.2013.06.010
http://archimer.ifremer.fr/doc/00157/26850/

Éditeur(s) : HAL CCSD
Résumé :  
The gelatinous layer (G-layer) of tension wood fibres in hardwood contributes to the mechanical function of the living tree and has significant consequences on properties of solid wood. Its size, shape and structure observed by optical or electron microscopy exhibits characteristic anatomical features. However, we found that sectioning of non-embedded wood samples results in an uncontrolled swelling of the G-layer was monitored by serial sections, from an embedded wood sample, from its trimmed transverse face to that located several hundreds of micrometers deep. The results revealed that the initial cutting before embedding produced a border effect responsible for the swollen nature, which is similar to sections from non-embedded material. After a conventional embedding technique was applied, a section of at least 30 micrometres below the trimming surface is required to observe an un-swollen G-layer.
IAWA Journal

hal-01032054
https://hal.archives-ouvertes.fr/hal-01032054

Éditeur(s) : HAL CCSD Oxford University Press (OUP)
Résumé : International audience
We report new structural, microstructural, petrological, and major- and trace-element data on ultramafic rocks from the Kondyor zoned ultramafic complex in Far-East Russia. The ultramafic rocks are subdivided into three subconcentric lithologies, from core to rim: (1) a metasomatic domain where generally phlogopite-rich dykes pervasively intrude dunite; (2) a main dunite core; (3) a pyroxenite rim. The ultramafic rocks have nearly vertical contacts with the surrounding Archaean basement (gneisses, quartzites and marbles) and hornfelsed Riphean sediments. The hornfelsed sediments show a relatively steep ( 60), outward dipping layering, which rapidly flattens to horizontal away from the inner contact. Although the Riphean sediments define a dome-like structure, the inward, shallow dipping foliation of the dunites indicates a synformal structure. Detailed petro-structural investigations indicate that the Kondyor dunites were deformed by solid-state flow under asthenospheric mantle conditions. The outward textural change from coarse- to fine-grained equigranular dunite and the outward-increasing abundance of subgrains and recrystallized olivine grains suggest dynamic recrystallization while fluid circulation was channelized within the core metasomatic zone, with a decreasing melt fraction from core to rim, and also suggest that solid-state deformation induced grain-size reduction towards the cooling border of the Kondyor massif. Based on their geochemistry, the dunites are interpreted as mantle rocks strongly affected by reaction with melts similar to the JurassicCretaceous Aldan Shield lamproites. Rim pyroxenites were formed by a melt-consuming peritectic reaction, implying the existence of at least a small, conductive thermal gradient around the dunite body while the latter was still at near-solidus temperature conditions. This suggests that the zoned structure of Kondyor was initiated at mantle depths, most probably within the subcontinental lithosphere. Upon cooling, the lamproitic melts were progressively focused in the central part of the massif and drained into vein conduits where they reacted with the wall-rock dunite. Two-dimensional numerical modelling based on finite-differences with a marker-in-cell technique incorporates temperature-dependent rheologies for both molten and non-molten host rocks. The modelling consolidates the structural, petrological and geochemical interpretations, which show that the dunites represent the synformal, flat-lying apex of an asthenospheric mantle diapir, triggered by fluid pressure channelized in the core, which nearly reached the Earths surface. We conclude that translithospheric mantle diapirism is an important mode of mass transfer in the Earth.
ISSN: 0022-3530

hal-00424508
https://hal.archives-ouvertes.fr/hal-00424508
DOI : 10.1093/petrology/egn083

Éditeur(s) : Wiley / Blackwell
Résumé : For the first time, a deep seismic data set acquired in the frame of the Algerian-French SPIRAL program provides new insights regarding the origin of the westernmost Algerian margin and basin. We performed a tomographic inversion of traveltimes along a 100-km-long wide-angle seismic profile shot over 40 ocean bottom seismometers offshore Mostaganem (Northwestern Algeria). The resulting velocity model and multichannel seismic reflection profiles show a thin (3-4 km thick) oceanic crust. The narrow ocean-continent transition (less than 10 km wide) is bounded by vertical faults and surmounted by a narrow almost continuous basin filled with Miocene to Quaternary sediments. This fault system, as well as the faults organized in a negative-flower structure on the continent side, marks a major strike-slip fault system. The extremely sharp variation of the Moho depth (up to 45 +/- 3 degrees) beneath the continental border underscores the absence of continental extension in this area. All these features support the hypothesis that this part of the margin from Oran to Tenes, trending N65-N70 degrees E, is a fossil subduction-transform edge propagator fault, vestige of the propagation of the edge of the Gibraltar subduction zone during the westward migration of the Alboran domain.
Geophysical Journal International (0956-540X) (Wiley / Blackwell), 2015-02 , Vol. 200 , N. 2 , P. 1027-1043

Droits : The Authors 2014. Published by Oxford University Press on behalf of The Royal Astronomical Society
http://archimer.ifremer.fr/doc/00255/36670/35278.pdf
http://archimer.ifremer.fr/doc/00255/36670/35279.pdf
DOI:10.1093/gji/ggu454
http://archimer.ifremer.fr/doc/00255/36670/