Éditeur(s) : Edinburgh : Adam and Charles Black
Siècle(s) traité(s) : 19
Provenance : Université Caen Normandie. Service commun de la documentation
Permalien : http://www.manioc.org/patrimon/CAE19033_1
CAE19033_1

Éditeur(s) :  :
Siècle(s) traité(s) : 19
Droits : Domaine public
Provenance : Collectivité territoriale de Martinique. Bibliothèque Schoelcher
Permalien : http://www.manioc.org/patrimon/SCH13244
SCH13244

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Les effets de la crise du capitalisme se sont traduits en Guadeloupe en janvier 2009 par un mouvement social sans précédent, dirigé par un collectif qui a suscité l’adhésion en raison de son expression du malaise social et de la gestion des revendications adressées au gouvernement. Ce mouvement social est innovant en Guadeloupe en raison de la pluralité des acteurs et de la nature de ses revendications. C’est donc sur son sens qu’il convient de s’interroger. Une société civile s’est réveillée créant de nouveaux espaces de débat.
Capitalism’s crisis effects resulted in social movement unprecedented led by a group that mobilized in the style of expressing unrest and managing demands that were sent to French government. This social movement is new in Guadeloupe because of variety actions and type of demands. It’s therefore necessary to consider its meaning: a civil society woke up creating new spaces for debate.
Guadeloupe

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.4898
http://journals.openedition.org/etudescaribeennes/4898

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Les longues grèves qui ont paralysé la Guadeloupe et la Martinique en 2009 sont en partie liées à la crise qui touche les économies insulaires. L’agriculture est menacée par les nouvelles négociations avec l’OMC qui sont très défavorables aux exportations de la banane et du sucre. Le secteur touristique est lui aussi au plus bas. Dans ces conditions, le chômage, le sous-emploi sont difficiles à accepter quand les prix augmentent et que les perspectives de développement ne sont pas vraiment définies.
The long strikes that paralyzed Guadeloupe and Martinique in 2009 are partly related to the crisis in the island economies. Agriculture is threatened by the new WTO negotiations that are unfavorable to exports of bananas and sugar. Tourism sector is also low. Under these conditions, unemployment and underemployment are difficult to accept when prices rise and development prospects are not really defined.
Guadeloupe
Martinique

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.4880
http://journals.openedition.org/etudescaribeennes/4880

Éditeur(s) : Elsevier Science Bv
Résumé : The overexploitation of fishery resources has led to a major fisheries crisis. In this context, artisanal fisheries, and in particular small-scale coastal fisheries, appear as relevant alternatives for a sustainable use of coastal resources. Marine Protected Areas (MPA) are more and more used as management tools for these fisheries, as protection effects and targeted access regulations may benefit to commercial fishers. Managers and scientists need then quantitative information not only to adapt their management to the fishing activity present on their territory, but also to estimate the effects of MPA management on it. This study provides catch and effort estimates that are essential for appraising and managing the artisanal fishery in the Côte Bleue Marine Park (CBMP), a French Mediterranean MPA including two No-Take Zones of different age and size. A field protocol was defined and implemented between July 2009 and June 2010 within the CBMP. Seven métiers were identified and characterized by target species, gear type, fishing grounds and fishing periods. During the one-year studied period, 3512 fishing trips and 4645 fishing operations were performed by 30 active boats in the Côte Bleue fishing territory, amounting to 9500 km of immersed nets. In total, approximately 130 tons of catch were landed in the six CBMP harbors, out of which 58% depend on the three main species caught on the Côte Bleue: hake (Merluccius merluccius), gilthead seabream (Sparus aurata) and common sole (Solea solea). The presented methodology could be part of a long term monitoring requiring close collaboration with local fishers. It enables adaptive management with respect to changes in fishing pressure (from inside and outside the MPA) that may impact the environment and its resources.
Fisheries Research (0165-7836) (Elsevier Science Bv), 2014-06 , Vol. 154 , P. 93-101

Droits : 2014 Elsevier B.V. All rights reserved.
http://archimer.ifremer.fr/doc/00180/29120/29367.pdf
DOI:10.1016/j.fishres.2014.02.006
http://archimer.ifremer.fr/doc/00180/29120/

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Le conflit social aux Antilles en 2009 a été très médiatisé en métropole où il est apparu exceptionnel, première épreuve dans le champ social susceptible de faire vaciller l’autorité d’un gouvernement jusqu’alors inflexible dans ce domaine. Au regard de l’historien, le conflit social antillais n’a rien de bien neuf. Il se glisse dans une histoire du mouvement social antillais qui reste encore un champ bien peu traité par l’histoire la plus contemporaine. Un rapide retour en arrière sur deux conflits sociaux majeurs, en 1959 et 1961, permet de resituer l’impact des pulsions sociales sur les politiques françaises pour l’outre-mer. Le regard de l’historien ici porté vient nuancer le caractère « exceptionnel » du moment 2009 et rappelle que les sorties de crise trouvées en 2009 rappellent étrangement celles retenues un demi-siècle plus tôt !
Social conflict in the West Indies in 2009 was highly publicized in France where it seemed exceptional, as a first event in the social field likely to shake the authority of a government previously inflexible in this area. In view of the historian, social conflict Caribbean has nothing new. He slips into a West Indian social history of the movement which is still a field little studied by the more contemporary history. A quick look back at two major social conflicts in 1959 and 1961 can relocate the impact of the social instincts of the French policy for overseas. The eye of the historian here has brought nuance to the "exceptional" at the time and recalls that out of the crisis in 2009 found strangely reminiscent of those used half a century ago!
Martinique

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.4881
http://journals.openedition.org/etudescaribeennes/4881

Éditeur(s) : Santiago de los Caballeros : Pontificia Universidad Católica Madre y Maestra Santiago de los Caballeros : Pontificia Universidad Católica Madre y Maestra
Résumé : (Funding) Digitized with funding from the Digital Library of the Caribbean grant awarded by TICFIA.
República Dominicana

Droits : All rights reserved by the source institution.
RD 303.69 N972e

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Les crises environnementales ont de profondes répercussions sur les économies et les sociétés insulaires, et ceci de manière exacerbée en Haïti, après le terrible tremblement de terre du 12 janvier 2010. Les petites îles de la Caraïbe et de l’Océan Indien sont confrontées à de nombreuses crises qui ont des origines locales, mais le plus souvent exogènes. Par delà le marasme mondial actuel, l’insularité et l’exiguïté sont autant de facteurs qui aggravent la crise économique et accroissent les tensions dans ces territoires. Dans les DROM (Département et Région d’Outre-mer), les mouvements sociaux ont été très importants.
Environmental crises have a profound impact on island economies and societies, and this so exacerbated in Haiti after the devastating earthquake of January 12, 2010. Small islands in the Caribbean and in the Indian Ocean endured numerous crises sometimes of local origin but more often due to external factors. Beyond the current global downturn, insularity and small size are factors that aggravate the economic crisis and increasing tensions in these areas. In DROM (Department Region Overseas), social movements have been very important.
Caraïbes
Guadeloupe
Guyane française
Martinique
Réunion

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.5013
http://journals.openedition.org/etudescaribeennes/5013

Éditeur(s) : HAL CCSD Société géologique de France
Résumé : International audience
The Messinian salinity crisis (MSC) is characterized by gigantic erosion that remodels the margins while a thick, essentially evaporitic and detrital, sedimentary sequence forms in the deep basins. Based on recent (MAURESC, 2003) and earlier (MESEA 1, 1990; MAGIRAA, 1996; GEOBREST, 2002) seismic reflection data, this work brings to light the record of the MSC on the Provençal margin, which has until now been rarely explored from this perspective. Beyond its strictly regional interest, this study fits into a larger synthesis of MSC seismic markers in the Mediterranean and Black Sea marine domain [Lofi et al., 2011] and employs the new nomenclature established on this occasion. The results obtained reveal a Messinian detrital body (CU unit) of 625 metres maximum thickness at the foot of the margin, accumulating at the mouths of the principal canyons. Its form, facies and extension assimilate it to clastic fans, fed by subaerial erosion linked to the MSC. The relative geometry of CU and the Messinian units MU and UU deposited in the deep basin give indications to their chronostratigraphic relations. The deposition of the CU unit is posterior to the basal part of the mobile unit consisting of halite (MU), but contemporary to its top. These results agree with the recent scenarii, which propose that the precipitation of MU in the basin began early, during the lowering of the sea level, and ended at a low level during the MSC [Blanc, 2000; Martin et al., 2001; Sage et al., 2005; Ryan, 2009]. The UU unit surmounts MU and is subdivided into two sub-units with perceptibly different seismic facies : UU1 at the base and UU2 at the summit. UU1 could correspond to a unit containing more halite and/or more clastic material than UU2. The UU1 sub-unit could be partially contemporary to the CU unit. Concerning salt tectonics and its markers, three structural provinces have been evidenced in the sector of study, respectively : an upslope domain in extension (normal faults), an intermediary domain in translation (tabular MU) and a downslope domain in contraction (salt diapirs). These domains are directly linked to the gravity spreading and/or gliding of the brittle sedimentary cover formed by the CU, UU and Plio-Quatenary units and of the mobile level, MU. In the study area, a close relation between the distribution and thickness of CU and salt tectonics has additionally been evidenced at the mouths of the large Messinian canyons, being best expressed where CU is thick.
EISSN: 1777-5817

hal-00622998
https://hal-brgm.archives-ouvertes.fr/hal-00622998
DOI : 10.2113/gssgfbull.182.2.181

Éditeur(s) : HAL CCSD Société géologique de France
Résumé : International audience
The Messinian salinity crisis (MSC) is characterized by gigantic erosion that remodels the margins while a thick, essentially evaporitic and detrital, sedimentary sequence forms in the deep basins. Based on recent (MAURESC, 2003) and earlier (MESEA 1, 1990; MAGIRAA, 1996; GEOBREST, 2002) seismic reflection data, this work brings to light the record of the MSC on the Provençal margin, which has until now been rarely explored from this perspective. Beyond its strictly regional interest, this study fits into a larger synthesis of MSC seismic markers in the Mediterranean and Black Sea marine domain [Lofi et al., 2011] and employs the new nomenclature established on this occasion. The results obtained reveal a Messinian detrital body (CU unit) of 625 metres maximum thickness at the foot of the margin, accumulating at the mouths of the principal canyons. Its form, facies and extension assimilate it to clastic fans, fed by subaerial erosion linked to the MSC. The relative geometry of CU and the Messinian units MU and UU deposited in the deep basin give indications to their chronostratigraphic relations. The deposition of the CU unit is posterior to the basal part of the mobile unit consisting of halite (MU), but contemporary to its top. These results agree with the recent scenarii, which propose that the precipitation of MU in the basin began early, during the lowering of the sea level, and ended at a low level during the MSC [Blanc, 2000; Martin et al., 2001; Sage et al., 2005; Ryan, 2009]. The UU unit surmounts MU and is subdivided into two sub-units with perceptibly different seismic facies : UU1 at the base and UU2 at the summit. UU1 could correspond to a unit containing more halite and/or more clastic material than UU2. The UU1 sub-unit could be partially contemporary to the CU unit. Concerning salt tectonics and its markers, three structural provinces have been evidenced in the sector of study, respectively : an upslope domain in extension (normal faults), an intermediary domain in translation (tabular MU) and a downslope domain in contraction (salt diapirs). These domains are directly linked to the gravity spreading and/or gliding of the brittle sedimentary cover formed by the CU, UU and Plio-Quatenary units and of the mobile level, MU. In the study area, a close relation between the distribution and thickness of CU and salt tectonics has additionally been evidenced at the mouths of the large Messinian canyons, being best expressed where CU is thick.
EISSN: 1777-5817

hal-00498286
https://hal.archives-ouvertes.fr/hal-00498286

Éditeur(s) : HAL CCSD
Résumé : Le projet METYSS (Messinian Event in the Tyrrhenian from Seismic Study) concerne le bassin tyrrhénien occidental le long de la côte est-sarde et s'intègre dans le cadre d'une étude comparative des marqueurs sismiques de la Crise de Salinité Messinienne (CSM) à l'échelle du bassin méditerranéen. La mer tyrrhénienne est un bassin arrière-arc néogène lié à la subduction calabraise. Le rifting débute sur la marge est-sarde au cours du Tortonien et du Messinien, impliquant au moins localement une contemporanéité des dépôts de la CSM avec les processus de rifting qui segmente la marge en plusieurs sous-bassins. Cette région est donc particulièrement adaptée à la caractérisation et à l'organisation des dépôts messiniens en contexte de tectonique active. L'identification des marqueurs de la CSM et la détermination de leurs caractéristiques spatio-temporelles (faciès, géométrie, distribution et relations) ont été effectuées à partir de l'interprétation de 1200 km de profils sismiques multitraces HR acquis en 2009 lors de la campagne METYSS-1 sur le N/O "Téthys II". L'un des premiers résultats est que l'on retrouve dans cette zone les marqueurs caractéristiques de la CSM, comparables à ceux déjà observés dans le bassin méditerranéen occidental : surfaces d'érosion (MES, TES, BES) et unités messiniennes typiques (UU: Upper Unit; MU: Mobile Unit). La réalisation des cartes de répartition de ces unités sismiques permet d'en déterminer la variabilité spatiale, et notamment d'affiner celle de la couche de sel (MU), par rapport aux données pré-existantes. Ainsi, le long de la partie haute de la marge est-sarde, la rareté de l'unité MU et la présence des UU semblent indiquer que cette zone se situait à une profondeur intermédiaire pendant la crise. Inversement, plus profondément dans le bassin, l'épaisseur importante de la couche de sel sous les UU, témoigne d'une profondeur déjà conséquente de cette zone durant la CSM. On remarque également que dans le secteur nord de la zone d'étude, la répartition de MU est contrainte par les blocs basculés, le sel étant confiné dans les sous-bassins qui segmentent la marge. Dans le secteur sud, la répartition de la couche de sel est plus homogène dans le bassin profond, et est déformée par une tectonique salifère active. A terme, nous souhaitons utiliser les marqueurs de la CSM pour reconstituer les paléo-connexions et paléo-profondeurs des différents bassins de la zone, mais également comprendre les interactions entre tectonique crustale, tectonique salifère, et sédimentation. L'objectif est aussi de restituer l'évolution tectono-sédimentaire de la marge est-sarde depuis 6Ma.
13ème Congrès Français de Sédimentologie
Dijon, France

hal-00657315
https://hal-brgm.archives-ouvertes.fr/hal-00657315

Éditeur(s) : HAL CCSD
Résumé : Le projet terre-mer METYSS a pour objectif de comprendre les effets immédiats et différés de la Crise de Salinité Messinienne (CSM) ainsi que les relations tectonique et sédimentation sur la marge est-sarde. Cette marge résulte de l'ouverture de la Mer Tyrrhénienne à partir du Tortonien et jusqu'au Messinien (c. 9 à 5 Ma). Des bassins profonds existaient déjà au Messinien dans le domaine tyrrhénien, comme l'atteste l'identification, à partir des données sismiques, d'épaisses séries évaporitiques messiniennes (Gaullier et al., 2009). Le principal canyon creusé dans la marge est connecté en amont avec le golfe d'Orosei, où affleurent à terre les seuls dépôts pliocènes connus. Dans la région d'Orosei, ces dépôts correspondraient donc potentiellement au remplissage de la partie amont des incisions liées à la CSM, lors de la remise en eau de la Méditerranée, comme c'est le cas en de nombreux endroits du pourtour méditerranéen (Clauzon, 1982). Les investigations de terrain MeTySar-2010 montrent que le principal fleuve actuel, le Cedrino, suit le cours d'une paléovallée qui incise le soubassement granitique et ses altérites. Ces dépôts ont été érodés (au Messinien ?) puis remaniés lors d'une transgression marine. Les microfaunes, présentes dans les faciès marins fins, indiquent un âge Pliocène supérieur (Giresse et al., ce congrès). Cette série marine présente des pendages de l'ordre de 20 à 30 ° qui s'organisent selon une direction NNE-SSW, subparallèle aux structures tectoniques majeures associées au rifting de la marge est-sarde. Le basculement des séries pliocènes est scellé par un ensemble de coulées volcaniques dont les plus anciennes sont datées du Quaternaire ancien. La cartographie et la caractérisation des dépôts mettent en évidence un paléo-relief orienté NNE-SSW qui contrôle la répartition des unités sédimentaires. Ces résultats suggèrent que l'activité tectonique post-messinienne participe au contrôle de l'architecture et de la paléogéographie des séries pliocènes dans ce secteur. Aucune trace de dépôts marins du Pliocène Inférieur, ni de Gilbert deltas s.s. n'a été relevée à terre. La transgression observée au Pliocène supérieur sur cette bordure du bassin implique 1) une position haute de la marge au Pliocène inférieur, et 2) une forte subsidence de ce secteur de la marge au Pliocène moyen. Cette subsidence serait la conséquence de l'activité tectonique post-rift, par ailleurs mise en évidence en mer grâce à deux campagnes récentes (METYSS 1 et 3, Gaullier et al., ce congrès).
13ème Congrès Français de Sédimentologie
Dijon, France

hal-00657307
https://hal-brgm.archives-ouvertes.fr/hal-00657307

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
We report preliminary results of a seismological experiment, SEISMOTANZ'07, which consisted in the deployment of a local network (35 stations) in the East African Rift System (EARS), North Tanzania, during 6 months in 2007. We compare two earthquake sequences (Gelai and Manyara) occurring respectively in the southern end of the Kenya rift and in the North Tanzanian Divergence (NTD). Only distant of 150 km, their triggering mechanisms are different. None of the sequences depicts typical swarm or mainshock-aftershock patterns. They highlight the change in the magmatic/tectonic nature of the rift where the eastern branch of the EARS enters the Tanzanian craton. The similar shape and long-axis of the elongate sequences emphasize the preferred locus of active strain release along NE-SW discontinuities which probably root at depth into steep Proterozoic shear zones. At Gelai, the deformation is dominated by aseismic process involving slow slip on normal fault and dyke intrusion within the upper crust Calais_et_al_2008. The spatial and temporal earthquake distribution indicates a possible correlation between the Gelai crisis and the eruption of the nearby Oldoinyo Lengai volcano. At Manyara, the sequence is more uncommon, revealing a long-lasting seismic activity deepely rooted (20-35 km depth) possibly related to stress loading transmitted laterally. The yield stress envelope modelled from the depth frequency distribution of earthquakes in the NTD is consistent with the presence of a mafic lower crust and further supports the strength increase of the rifted crust from south Kenya to the NTD.
ISSN: 0899-5362

hal-00420599
https://hal.archives-ouvertes.fr/hal-00420599
DOI : 10.1016/j.jafrearsci.2009.09.005

Éditeur(s) : HAL CCSD American Society of Hematology
Résumé : International audience
Sickle cell disease is characterized by painful vaso-occlusive crises during which abnormal interactions between erythroid adhesion molecules and vessel-wall proteins are thought to play a critical role. Hydroxyurea, the only drug with proven benefit in sickle cell disease, diminishes these interactions, but its mechanism of action is not fully understood. We report that, under hydroxyurea, expression of the unique erythroid laminin receptor Lu/BCAM was increased, but red blood cell adhesion to laminin decreased. Because Lu/BCAM phosphorylation is known to activate cell adhesion to laminin, it was evaluated and found to be dramatically lower in hydroxyurea-treated patients. Analysis of the protein kinase A pathway showed decreased intracellular levels of the upstream effector cyclic adenosine monophosphate during hydroxyurea treatment. Using a cellular model expressing recombinant Lu/BCAM, we showed that hydroxyurea led to decreased intracellular cyclic adenosine monophosphate levels and diminished Lu/BCAM phosphorylation and cell adhesion. We provide evidence that hydroxyurea could reduce abnormal sickle red blood cell adhesion to the vascular wall by regulating the activation state of adhesion molecules independently of their expression level.
ISSN: 0006-4971

inserm-00821117
http://www.hal.inserm.fr/inserm-00821117
http://www.hal.inserm.fr/inserm-00821117/document
http://www.hal.inserm.fr/inserm-00821117/file/Bartolucci_Blood_2010.pdf
DOI : 10.1182/blood-2009-12-257444

Résumé : Dans le cas des DOM, singulièrement la Guadeloupe, qui sont à l'aube de l'expérimentation de réformes profondes de politiques économiques, l'élaboration d'un outil de simulation macroéconomique tel qu'un MEGC apparaît naturellement comme une exigence plus que souhaitable. Ce recours à la construction de modèles spécifiques pour les DOM est en parfaite cohérence avec l'une des principales conclusions du rapport d'information diligenté par le Sénat aux lendemains de la crise sociale du début de l'année 2009. Les appels à projet de la Commission europèenne et du Ministère de l'Outre-mer vont justement dans le sens de pallier celte carence puisque la politique économique des RUP de façon générale est conduite à vue sans aucun outil d'investigation ex ante. Nous avons conçu plusieurs modèles. Parmi eux, CloDyn est le premier modèle macroéconomique pour les DOM à vocationopérationnelle. Composée de plus de 2000 équations, ce modèle d'équilibre général calculable tient compte de nombreuses rigidités sur les marchés des biens et services et du travail et se décline sous deux versions: statique et dynamique. Les élasticités ont fait l'objet d'estimations économétriques. Il tient compte de nombreuses spécificités tant au niveau de la fiscalité de ces régions (octroi de mer, taxe sur les carburants, subventions à l'exportation) que du coût des facteurs (exonérations des charges sur les bas salaires, sur rémunératio des fonctionnaires). Il repose sur une formalisation des mécanismes en oeuvre dans ces économies que nous avons appelé le DOM disease pour expliquer les dysfonctionnements persistants sur le plan macroéconomique.
In the case of the French overseas regions, particularly of Guadeloupe, which are just beginning to experiment with economic policies radical reforrns, the development of a macroeconomic simulation tool such as a CGE model appears naturally as a highly desirable requirement. The use of the construction of specifie models for DOM is fully consistent with a major finding of the report commissioned by the Senate in the aftermath of the social crisis of the early 2009. As a malter of facts, the purpose of the calls for project initiated by the European Commission and the Ministry of Overseas is to remedy this deficiency, since the RUP economie policy is generally to conduct no investigation tool ex ante. We designed several models. Among them, CloDyn is the first operational DOM-based macroeconomic rnodel. Composed of more than 2000 equations, this computable general equilibrium model takes into account many rigidities in the markets for goods and services and labor and is available in two versions: static and dynamic. Elasticities have been econometrically estimated. lt rests on many features of both taxation (dock dues, fuel tax, export subsidies) and the cost factors (exemption from charges on low wages, remuneration of civil servants). Il is based on a formalization of the mechanisms at work in these economies we calied the DOM disease to explain the persistent failures in such economies. lt also evaluates the monetary poverty among households with the use of a block of microsimulation model and we allow a profane in GAMS to use this tool and conduct its own analytical work thanks to a user friendly interface.

http://www.theses.fr/2011AGUY0411/document

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : La perspective d’un classement en « cœur de parc » des îlets Pigeon, haut lieu de la plongée sous-marine, relance les débats autour de la place des sports de nature dans le Parc national de la Guadeloupe. Faut-il craindre une interdiction de la plongée sous-marine en cœur de parc, comme ce fut le cas pour le canyoning, suite au conflit environnemental entourant cette pratique ? La réglementation est-elle toujours de mise, alors que la loi sur les parcs de 2006 exhorte les parcs à s’engager dans des démarches partenariales, afin de bâtir un projet de territoire reposant sur les principes du développement durable et de solidarité écologique entre le cœur de parc et ses espaces environnants ? Parallèlement, si le Parc doit passer d’une gestion de crises, souvent hésitante et parfois arbitrale, à une gestion concertée, de quel potentiel de coopération dispose-t-il pour dépasser des situations de conflits potentiels comme celle des îlets Pigeon ? Existe-t-il un effet d’apprentissage du conflit du canyoning capable de modeler ce potentiel de coopération ?
The probability that the Pigeon Islands, a Mecca for diving, will be classified as a protected “heart of park”, reopens the debate about outdoor sports in the National Park of Guadeloupe. Should we be worried about the prohibition of diving in this “heart of park”, as has happened in the case of canyoning, following an environmental conflict around this practice? Are regulations always acceptable, when at the same time the law on the national parks of 2006 exhorts the parks to make a commitment to participatory initiatives, and to create projects based on the principles of sustainable development and ecological solidarity between the heart of park and its surrounding spaces? At the same time, if the Park has to develop from a crisis management style, with hesitating and arbitrary decisions, to a more cooperative management style, what potential is there to use cooperation to overcome possible conflict situations such as the Pigeon Islands? Are there lessons to be learned from the conflict surrounding the canyoning, which would help model the process and benefits of cooperation?
Guadeloupe

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.3608
http://journals.openedition.org/etudescaribeennes/3608

Éditeur(s) : Macon : Protat frères
Siècle(s) traité(s) : 19
Droits : Domaine public
Provenance : Collectivité territoriale de Martinique. Bibliothèque Schoelcher
Permalien : http://www.manioc.org/patrimon/SCH13269
SCH13269

Éditeur(s) : HAL CCSD
Résumé : International audience
The Corinth Rift is the most seismically active zone in Europe. The area is characterized by very localized NSextension at a rate of1.5cm/year, the occurrence of frequent and intensive microseismic crises and occasionalmoderate to large earthquakes like in 1995 (Mw=6.1).Since the year 2000, the Corinth Rift Laboratory (CRL, http://crlab.eu) consisting in a multidisciplinary naturalobservatory, aims at understanding the mechanics of faulting and earthquake nucleation in the Rift. Recent studieshave improved our view about fault geometry and mechanics within CRL, but there is still a critical need for a betterknowledge of the structure at depth both for the accuracy of earthquake locations and for mechanical interpretationof the seismicity.In this project, we aim to analyze the complete seismological database (13 years of recordings) of CRL by usingrecently developed methodologies of structural imaging, in order to determine at the same time and with highresolution, the local 3D structure and the earthquake locations.We perform an iterative joint determination of 3D velocity model and earthquake coordinates. In a first step, Pand S velocity models are determined using first arrival time tomography method proposed by Taillandier et al.(2009). It consists in the minimization of the cost function between observed and theoretical arrival times which isachieved by the steepest descent method (e.g. Tarantola 1987). This latter requires computing the gradient of thecost function by using the adjoint state method (Chavent 1974). In a second step, earthquakes are located in thenew velocity model with a non-linear inversion method based on a Bayesian formulation (Gesret et al. 2015). Step1 and 2 are repeated until the cost function no longer decreases.We present preliminary results consisting in: (1) the adjustement of a 1D velocity model that is used as initialmodel of the 3D tomography and (2) a first attempt of the joint determination of 3D velocity model and earthquakelocation.In addition to the tomographic imaging, we perform a preliminary receiver function analysis of teleseismic datarecorded by the broadband stations of the CRL network. The RF analysis should provide the interface depthsbeneath seismometers and increase the imaging resolution of the upper crustal structures provided by the 3Dtomography. In this first attempt, we adjust the 1D velocity model that produces a synthetic RF as similar aspossible to the observed RF for a subset of data. We compare the identified interfaces with structures imaged bythe tomography.
EGU general assembly 2016
Vienne, Austria

hal-01306224
https://hal-mines-paristech.archives-ouvertes.fr/hal-01306224

Éditeur(s) : HAL CCSD
Résumé : International audience
The « METYSS » cruise was carried out in June 2009 onboard the R/V « Téthys II » along the eastern Sardinian and south-eastern Corsican margins, western Tyrrhenian Sea, in order to better constrain the potential links between deformation related to either crustal tectonics or salt tectonics and sediment accumulation, especially during the Messinian and Plio-Quaternary times. We acquired 15 high-resolution seismic reflection profiles (about 1200 km in cumulative length) along the south-eastern Corsican margin, immediately north of the Bonifacio Strait and along the upper and middle parts of the eastern Sardinian margin, from the continental slope to the Cornaglia Terrace. The Tyrrhenian Sea is considered as a Neogene back-arc basin that opened during continental rifting and oceanic spreading related to the eastward migration of the Apennine subduction system from Tortonian to Pliocene times (Jolivet et al., 2006). Rifting of the Tyrrhenian Sea started first along the Eastern Sardinian margin during the Tortonian-Messinian times and therefore the series of that age should be considered as syn-rift sediments (Sartori et al., 2004). The « METYSS » seismic profiles clearly illustrate that this part of the Tyrrhenian was highly segmented during the rifting stage by N-S trending normal faults delineating ridges (e.g., Baronie Ridge) and basins (e.g., Sardinian Basin and Cornaglia Terrace), as previously described for example by Thommeret (1999) and Sartori et al. (2004). The Messinian sedimentary units and especially the « Upper Unit » (UU, Lofi et al., this congress, corresponding to the « Upper Evaporites » in the previous literature) are, without any doubt, of syn-rift age, as they display a fan-shaped stratal geometry. The Mobile Unit (MU, Lofi et al., this congress), i.e. the Messinian halite, is clearly imaged in the study area and its spatial repartition can be outlined. The highly-variable thickness of the confined salt basins could be due to the initial basin geometry (i.e. before the Messinian salinity Crisis) or to the syn-rift character of the deposition. Southeastward of the study area, in the vicinity of the Cornaglia Seamount, salt tectonics appears surprisingly vigorous. More surprisingly, several normal faults seem to have remained active in recent times, if not even at present time. Fault slip has been recorded by bathymetric scarps and associated footwall debris flows interfingered within the Plio-Quaternary sequence, even though the eastern Sardinian margin is usually considered to be passive now. Moreover, some amount of tectonic inversion is visible on some normal faults that show contractional or transpressional components of late slip. In addition, this “post-rift” deformation can be illustrated within the Plio-Quaternary sequence by a regional unconformity. Consequently, numerous mass-transport deposits and channel-levees systems observed in the Plio-Quaternary cover could be partly controlled by tectonic activity. These very preliminary results require further investigations in order to better decipher the role of crustal tectonics and salt tectonics, salt-related structures being very efficient markers to discriminate between the respective contribution of gravity-driven, salt tectonics and deep-seated, crustal tectonics (Gaullier et al., 2010). Finally, we aim to precisely determine the relative vertical movements (tilting, subsidence, magmatism. . . ) and geodynamical history of the different segments of the area since 6 Ma.
Geophysical Research Abstracts
Vienne, Austria

hal-00537828
https://hal-brgm.archives-ouvertes.fr/hal-00537828
https://hal-brgm.archives-ouvertes.fr/hal-00537828/document
https://hal-brgm.archives-ouvertes.fr/hal-00537828/file/EGU2010-15469_ref6821.pdf

Éditeur(s) : Monachii ; Lipsiae : apud Frid. Fleischer in comm.
Extrait de : Flora brasiliensis : enumeratio plantarum in Brasilia hactenus detectarum quas suis aliorumque botanicorum studiis descriptas et methodo naturali digestas partim icone illustratas
Résumé : Édition : 1883-1885
Siècle(s) traité(s) : 19
Droits : Domaine public
Provenance : Université Toulouse III - Paul Sabatier. Service Commun de la Documentation
Permalien : http://www.manioc.org/patrimon/TLS17091
TLS17091