Éditeur(s) : HAL CCSD L'Harmattan
Résumé : International audience
When the European arrived in the Lesser Antilles they have been in contact with their Amerindian inhabitant they will call "Caribs". By this way, an important text corpus concerning those peoples will be constituted between the fifteen and the eighteen centuries. Since the archaeological researches beginnings in the archipelago until today, establish a link between those historic texts and the archaeological findings have been one of the the archaeologists main objectives. We will present here a review of the works about this question. By this way we will be able to observe the progressive transformation of the relationship between the archaeologists and the text sources and this of their utilization mode. This transformation is related to an historians and archaeologist discussion concerning the European text about Lesser Antilles Amerindian real value.
Lors de leur arrivée dans les Petites Antilles les Européens ont été au contact de populations amérindiennes qu'elles ont dénommées "Caraïbes". Ainsi, un important corpus de texte concernant ces groupes a été constitué, entre les XVé et XVIIIé siècles. Dès les débuts de l'archéologie dans l'archipel et jusqu'à aujourd'hui un des enjeux importants de la recherche a été de tenter d'établir un lien entre ces sources historiques et les découvertes effectuées au cours des fouilles. C'est un bilan de ces recherches que nous présenterons ici. Par la mise en évidence des grandes étapes qu'a connues le traitement de cette question, il nous sera possible d'observer la modification progressive du rapport des archéologues aux sources textuelles ainsi que celle de leur mode d'utilisation. Une modification qui s'est effectuée en parallèle d'une discussion, menée tant par les historiens que par les archéologues, sur la valeur des textes des Européens traitant du peuplement amérindien des Petites Antilles.
Les Indiens de Petites Antilles. Des premiers peuplements aux débuts de la colonisation européenne

ISBN : 978-2-296-55079-7
hal-00967529
https://hal.univ-antilles.fr/hal-00967529
https://hal.univ-antilles.fr/hal-00967529/document
https://hal.univ-antilles.fr/hal-00967529/file/A_la_recherche_des.pdf

Éditeur(s) : HAL CCSD Société géologique de France
Résumé : International audience
In this paper, we provide the first structural map of Les Saintes archipelago (Guadeloupe, Lesser Antilles). The finite strain pattern displays four families of fault systems characterized by their statistical structural orientations: N000-N020, N050-N070, N090-N110 and N130-N140 trending fault systems. Our onshore results thus underline a fault network much more complex than the one depicted by the previous offshore geophysical investigations around Les Saintes archipelago, which show only N120-N150 trending system. According to the available K-Ar dating of the volcanic rocks and the relative chronology of the faults defined in the field, we determine the deformation history in Les Saintes islands since the last 3 Ma. The four highlighted trending fault systems are already active since the Pliocene and are consistent with the present-day extensional tectonics in the Guadeloupe archipelago compatible with the reactiva-tion of inherited structures at the active arc scale. We interpret the tectonic evolution of Les Saintes islands as the result of interplay between subduction of aseismic ridges (Tiburon and Barracuda ridges) and oblique convergence. Furthermore , we recognized an exhumed geothermal paleo-system in Terre-de-Haut island which is a good analogue of the present-day active Bouillante geothermal system. Its duration is estimated at 400 k.y. during the Pliocene.
EISSN: 1777-5817

hal-01625778
https://hal.univ-antilles.fr/hal-01625778
https://hal.univ-antilles.fr/hal-01625778/document
https://hal.univ-antilles.fr/hal-01625778/file/VeratIEtAl_Final.pdf
DOI : 10.2113/gssgfbull.187.1.3

Éditeur(s) : Gauthier-Villars
Résumé : The Barbados Ridge composes the major part of the forearc region of the Lesser Antilles magmatic arc. The toe of the ridge is almost certainly the locus of modern accretion of sediment from the subducting Atlantic seafloor. The pre-Pleistocene geology of the island of Barbados, which exposes the crest of the Barbados Ridge, is best explained by accretion, implying that the ridge as a whole is an accretionary prism. Important elements of the island geology in this interpretation are the occurrence of much if not all of the pre-Pleistocene rocks in fault-bounded packets and the juxtaposition of age-overlapping abyssal pelagite and continent-derived fan deposits in such packets. The orientation of tectonic structures on Barbados, however, implies that the Paleogene subduction that created the older part of the prism occurred in a differently configured zone from the present one.
Oceanologica Acta, Special issue (0399-1784) (Gauthier-Villars), 1981

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/00245/35674/34182.pdf
http://archimer.ifremer.fr/doc/00245/35674/

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : L’algue est une ressource marine peu étudiée par la géographie ; elle offre pourtant des potentialités de développement économique. Les macro-algues cultivées à des fins alimentaires sont une alternative à la pêche. Les micro-algues constituent une biomasse valorisable : molécule pharmaceutique, Oméga 3 et biocarburants. De ces différents usages naît la question suivante : les algues sont-elles une ressource marine à exploiter pour développer durablement les territoires de la zone intertropicale ? Nous présenterons tout d’abord l’algoculture à l’échelle mondiale en soulignant le faible poids de cette activité dans le bassin caribéen. Puis nous montrerons que l’algoculture s’inscrit dans un processus de développement durable en assurant un revenu à des communautés rurales (Petites Antilles). Enfin, dans une approche comparative (États-Unis), nous verrons que l’espace caribéen est une région de projets et d’aménagements durables qui a des atouts pour développer l’algoculture : exposition solaire, hautes températures, proximité de la recherche américaine.
Algae as sea resource have not been largely explored in Geography, yet it offers the potential for economic development. Macro-algae are cultivated for food purposes and they can substitute for fishing. Micro-algae can be valued as biomass: “nutraceutics”, Omega 3, biofuel. These various utilizations raise a question: are algae a key to a sustainable development in intertropical islands? We shall present Algaculture on a global scale, while emphasizing its low importance in the Caribbean. Then we shall show how algaculture can be part of a process of sustainable development by providing revenue to rural communities (Lesser Antilles). Finally, in a comparative approach (with the US), we shall see that the Caribbean Region has a number of assets for algaculture that make it suitable for sustainable projects and infrastructures: solar exposure, high temperatures, close to the US research centers.
États-Unis
Caraïbes

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.4389
http://journals.openedition.org/etudescaribeennes/4389

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Durant des siècles, les tortues marines ont procuré une source importante de nourriture, notamment de protéines, pour les populations côtières ainsi qu’une source de revenus. Aujourd’hui, elles sont une composante importante de plusieurs cultures à travers le monde et revêtent une signification symbolique importante pour certaines populations insulaires, notamment dans les Petites Antilles.La raréfaction des populations de tortues de mer octroie à ces dernières un certain intérêt touristique, par exemple dans le cadre d’expériences écotouristiques. Cette espèce emblématique peut d’une certaine manière participer à la protection des océans et des récifs coralliens. Dans ce nouveau contexte, leur valeur économique et environnementale est reconsidérée.
During centuries the marine turtles were considered an important resource for food and protein and for the coastal populations and were also a source of revenue .Today they are a major composition of many cultures around the world and have a very symbolical signification for some island populations in the lesser Antilles.The rarefactions of those turtles give them a certain interest for tourists for example and for ecotourism experiences. This symbolical aspect can participate in the protection of oceans and coral reefs this new context their value economical and environmental is re- considered.
Caraïbes

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.6656
http://journals.openedition.org/etudescaribeennes/6656

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : La récession mondiale de la fin de la décennie 2000 n’épargne pas les pays de la Caraïbe. Si les manifestations économiques de cette crise sont identiques, l’étude menée dans les agglomérations de Pointe-à-Pitre et de Roseau montre que la perception et les réponses des populations face à cet évènement varient, d’un territoire à l’autre, selon le statut politique et le niveau de vie. Dans les Antilles françaises, la réaction a été de rechercher un responsable, en l’occurrence l’État ; tandis que dans l’île indépendante de la Dominique, de manière pragmatique, les populations cherchent collectivement des alternatives.
The global recession at the end of the 2000s did not spare the Caribbean countries. If the economic events of this crisis are the same, the study conducted in urban areas of Pointe-à-Pitre, and Roseau shows that the perception and the responses of people facing this event vary from one jurisdiction to another, depending on the political status and living standards. In the French Antilles, the reaction was to seek a responsible, namely the state, while the independent island of Dominica, in a pragmatic way, people collectively seek alternatives.
Dominique
Guadeloupe
Pointe-à-Pitre
Roseau

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.4909
http://journals.openedition.org/etudescaribeennes/4909

Éditeur(s) : HAL CCSD European Geosciences Union
Résumé : International audience
During the GWADASEIS cruise (Lesser Antilles volcanic arc, February-March 2009) a very high resolution (VHR) seismic-reflection survey was performed in order to constrain Late Quaternary to Present faulting. The profiles we obtained evidence frequent "ponding" of reworked sediments in the deepest areas, similar to the deposition of Mediterranean "homogenites". These bodies are acoustically transparent (few ms t.w.t. thick) and are often deposited on the hanging walls of dominantly normal faults, at the base of scarps. Their thickness appears sufficient to compensate (i.e. bury) co-seismic scarps between successive earthquakes, resulting in a flat and horizontal sea floor through time. In a selected area (offshore Montserrat and Nevis islands), piston coring (4 to 7 m long) was dedicated to a sedimentological analysis of the most recent of these particular layers. It corresponds to non-stratified homogenous calcareous silty sand (reworked calcareous plankton and minor volcanoclastics). This layer can be up to 2 m thick, and overlies finegrained hemipelagites. The upper centimeters of the latter represent the normal RedOx water/sediment interface. 210Pb and 137Cs activities lack in the massive sands, while a normal profile of unsupported 210Pb decrease is observed in the hemipelagite below, together with a 137Cs peak correspond- ing to the Atmospheric Nuclear Experiments (1962). The RedOx level was thus capped by a recent instantaneous major sedimentary event considered as post-1970 AD; candidate seismic events to explain this sedimentary deposits are either the 16 March 1985 earthquake or the 8 October 1974 one (Mw=6.3 and Mw=7.4, respectively). This leads to consider that the syntectonic sedimentation in this area is not continuous but results from accumulation of thick homogenites deposited after the earthquakes (as observed in the following weeks after Haiti January 2010 event, McHugh et al., 2011). The existence of such deposits suggests that, in the area of study, vertical throw likely results from cumulated effects of separated earthquakes rather than from aseismic creep. Examination of VHR profiles shows that all major co-seismic offsets are recorded in the fault growth sequence and that co-seismic offsets can be precisely estimated. By using a sedimentation rate deduced from 210Pb decrease curve (0.5 mm yr−1) and taking into account minor reworking events detected in cores, we show that the Redonda system may have been responsible for five >M6 events during the last 34 000 yr. The approach presented in this work differs from fault activity analyses using displaced sets of isochronous surfaces and postulating co-seismic offsets. Combining VHR seismic imagery and coring we can decipher co-seismic vs. slow continuous displacement, and thus actually estimate the amplitude and the time distribution of major co-seismic offsets.
ISSN: 1561-8633

insu-00844581
https://hal-insu.archives-ouvertes.fr/insu-00844581
https://hal-insu.archives-ouvertes.fr/insu-00844581/document
https://hal-insu.archives-ouvertes.fr/insu-00844581/file/nhess-12-1755-2012.pdf
DOI : 10.5194/nhess-12-1755-2012

Éditeur(s) : HAL CCSD Elsevier
Résumé : LA-ICP-MS and SIMS U–Pb analyses have been performed on detrital zircon grains from four heavy mineral rich metasediments collected at different levels of the Nathorst Land Group (Eleonore Bay Supergroup, Greenland). Zircons from high-grade samples collected in the sillimanite and migmatite zones exhibit modifications to their structure, which are lacking in grains from a low-grade sample (0.3 GPa and 350–400 °C). In the sillimanite zone (0.5 GPa, 650 °C), thin discontinuous rims (<20 μm) plating detrital zircon grains document a metamorphic overgrowth during the Caledonian event dated at 428 ± 25 Ma (2σ). In the migmatite zone (0.4 GPa, 700 °C), zircons underwent severe recrystallisation processes but no new zircon growth. Ilmenite, which constitutes over 50% of the heavy mineral layers, underwent recrystallisation in both high-grade samples and is likely to represent the main source of Zr available for growth of zircon rims in the sillimanite zone. However, in the migmatite zone sample, the metamorphic conditions allowed titanite overgrowth around ilmenite, which acted as a sink for Zr and inhibited new zircon growth. 207Pb/206Pb ages for 152 detrital zircons broadly range between 2800 and 990 Ma. The detrital zircon age signature is characterized by the large predominance of late Paleoproterozoic (1.85–1.60 Ga) grains in all analysed samples and by lesser amounts of Archean (2.7–2.8 Ga) and Mesoproterozoic (1.2–1.0 Ga) zircons. The overall age range indicates that detritus can be sourced from the Labradorian and Makkovikian provinces of northeastern Laurentia. The youngest grain analysed (987 ± 18 Ma) indicates that deposition took place during the Neoproterozoic, in a post-Grenvillian sedimentary environment and was likely coeval with the Mid-Neoproterozoic episode of aborted rifting that affected the eastern margin of Laurentia. The lack of detritus originating from Amazonia or Baltica, placed adjacent to Laurentia during the early stages of Rodinia fragmentation, suggests that these two continental landmasses did not constitute a topographic high during the Neoproterozoic or that the Mid-Neoproterozoic rifting opened toward an open ocean to the north of a combined Laurentia/Baltica, thus resulting in a general south to north direction of transport of the sediments.
ISSN: 0301-9268

hal-00407204
https://hal.archives-ouvertes.fr/hal-00407204
DOI : 10.1016/j.precamres.2007.01.002

Éditeur(s) : HAL CCSD
Résumé : International audience
The INTERREG Caribbean IV program recommends the valorization and protection of the region's environmental core, through collaborative and sustainable management of resources. It uses Martinique as the test case. The French territories of Saint-Martin, Saint-Barthélemy, Guadeloupe, and Martinique, and the member states of the Organization of Eastern Caribbean States are part of a geographic continuum that can easily be identified through its similar landscapes, climates, and natural resources and also through the environmental degradation the states have to face, caused by human activity (pollution and deterioration of ecosystems and habitats), natural hazards, and climate change including sea level rise. Therefore the islands of the Lesser Antilles are faced with an important developmental and environmental challenge, which could be easily summarized as a struggle for balance.
Meteorological Technology International

ird-00742661
http://hal.ird.fr/ird-00742661
http://hal.ird.fr/ird-00742661/document
IRD : fdi:010057442

Éditeur(s) : HAL CCSD Copernicus Publications on behalf of the European Geosciences Union
Résumé : International audience
The 1867 Virgin Island Tsunami reached large magnitude on the coasts of the Caribbean Islands. A maximum tsunami height of 10 m was reported for two coastal locations (Deshaies and Sainte-Rose) in Guadeloupe. Modelling of the 1867 tsunami is performed in the framework of the nonlinear shallow-water theory. The directivity of the tsunami wave source in the Caribbean Sea according to the assumed initial waveform is investigated. The tsunami records at the several coastal regions in the Lesser Antilles, Virgin Islands, Puerto Rico and South America are simulated. The comparison between the computed and observed data is in reasonable agreement.
Natural Hazards and Earth System Science

Droits : info:eu-repo/semantics/OpenAccess
hal-00330900
https://hal.archives-ouvertes.fr/hal-00330900
https://hal.archives-ouvertes.fr/hal-00330900/document
https://hal.archives-ouvertes.fr/hal-00330900/file/nhess-3-367-2003.pdf

Éditeur(s) : HAL CCSD
Résumé : International audience
At the Land-Sea interface, the mangrove forests represent unique but very threatened ecosystems. In the tropical island systems as to the biosphere scale, the mangrove forests and related biocenoses are relevant anthropization markers. The pressures and the direct and indirect damage are also multiple and varied. Generally, the coastal ecosystems of the French West Indies are in constant evolution. The effect of natural factors is increased by human activities. In these small, densely populated and urbanized areas, the mangrove forests are part of the last unoccupied areas. Faced with growing development needs, they represent an area to use, exploit and impact. The human footprint is high and sometimes it has irreversible consequences. The human impact mainly translates into the erosion of biodiversity and ecosystem services. Facing these imbalances, the study of the mangrove ecosystem using conservation ecology stands as an essential approach for the preservation of Martinique’s coastal ecosystems.
ISSN: 2277-8322

hal-01393660
https://hal.univ-antilles.fr/hal-01393660

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Properly assessing the extent and magnitude of fault ruptures associated with large earthquakes is critical for understanding fault behavior and associated hazard. Submarine faults can trigger tsunamis, whose characteristics are defined by the geometry of seafloor displacement, studied primarily through indirect observations (e.g., seismic event parameters, seismic profiles, shipboard bathymetry, coring) rather than direct ones. Using deep-sea vehicles, we identify for the first time a marker of coseismic slip on a submarine fault plane along the Roseau Fault (Lesser Antilles), and measure its vertical displacement of ∼0.9 m in situ. We also map recent fissuring and faulting of sediments on the hangingwall, along ∼3 km of rupture in close proximity to the fault's base, and document the reactivation of erosion and sedimentation within and downslope of the scarp. These deformation structures were caused by the 2004 M w 6.3 Les Saintes earthquake, which triggered a subsequent tsunami. Their characterization informs estimates of earthquake recurrence on this fault and provides new constraints on the geometry of fault rupture, which is both shorter and displays locally larger coseismic displacements than available model predictions that lack field constraints. This methodology of detailed field observations coupled with near-bottom geophysical surveying can be readily applied to numerous submarine fault systems, and should prove useful in evaluating seismic and tsunamigenic hazard in all geodynamic contexts.
ISSN: 0012-821X

insu-01557932
https://hal-insu.archives-ouvertes.fr/insu-01557932
https://hal-insu.archives-ouvertes.fr/insu-01557932/document
https://hal-insu.archives-ouvertes.fr/insu-01557932/file/EPSL-2006-escartin.pdf
DOI : 10.1016/j.epsl.2016.06.024

Éditeur(s) : Pêche thonière et dispositifs de concentration de poissons, Caribbean-Martinique, 15-19 Oct 1999
Résumé : This summary tackles the development of fisheries in the Caribbean using fads. It highlights the principal causes which explain why, in spite of more than thirty years of experimenting, fishing on fads has not developed as much as had been hoped. Whereas the deep-sea production of pelagic fish by the continental countries of the region has considerably increased since the early eighties, that of the Lesser Antilles has grown more slowly. Anchored fads have given the boats of the small-scale fisheries from three islands (Guadeloupe, Martinique and Curacao) access to these pelagic resources. The various modes of development and management of the fads observed in each island are described. The first available data are used to provide some indications of the effects of the various strategies implemented and the changes induced by this new fishing technique.Original Abstract: Cette synthese concerne la region Atlantique Centre-Ouest (FAO 31) mais elle aborde principalement le developpement des DCP ancres de la zone Caraibe. Trois sites principaux font l'objet d'un developpement particulier ; il s'agit des iles pour lesquelles l'activite de peche professionnelle est actuellement effective autour des DCP : la Guadeloupe, la Martinique et Curacao. L'introduction de DCP dans l'Atlantique Centre-Ouest est signalee pour la premiere fois en 1969, a Panama City (Floride). Il s'agit alors de dispositifs cotiers. Les especes ciblees sont des petits poissons pelagiques. Au debut des annees quatre-vingt, l'implantation de DCP ancres autour des petits etats insulaires de la Caraibe pour la peche des grands poissons pelagiques est consideree comme une priorite par les scientifiques reunis lors du 36e congres du Gulf and Caribbean Fisheries Institute (GCFI). Beaucoup d'experiences DCP conduites dans la region ont permis de conclure a une bonne efficacite agregative quels que soient les choix technologiques operes (DCP lourds ou legers). Malgre cela, tres peu d'iles tirent actuellement benefice de l'avantage que procurent les DCP pour l'exploitation des ressources en grands pelagiques frequentant leurs eaux. Les problemes de transfert et les difficultes a passer de la phase experimentale a la phase operationnelle sont probablement a l'origine de ce paradoxe. Le developpement d'une reelle cooperation regionale sur le theme devrait permettre, aux petits etats insulaires notamment, de mieux profiter des migrations des grands poissons pelagiques dans leurs eaux.

Droits : Ifremer
http://archimer.ifremer.fr/doc/00042/15279/12665.pdf
http://archimer.ifremer.fr/doc/00042/15279/

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Tropical islands are characterized by thermal and orographical forcings which may generate microscale air mass circulations. The Lesser Antilles Arc includes small tropical islands (width lower than 50 km) where a total of one-and-a-half million people live. Air quality over this region is affected by anthropogenic and volcanic emissions, or saharan dust. To reduce risks for the population health, the atmospheric dispersion of emitted pollutants must be predicted. In this study, the dispersion of anthropogenic nitrogen oxides (NOx) is numerically modelled over the densely populated area of the Guadeloupe archipelago under weak trade winds, during a typical case of severe pollution. The main goal is to analyze how microscale resolutions affect air pollution in a small tropical island. Three resolutions of domain grid are selected: 1 km, 333 m and 111 m. The Weather Research and Forecasting model (WRF) is used to produce real nested microscale meteorological fields. Then the weather outputs initialize the Lagrangian Particle Dispersion Model (FLEXPART). The forward simulations of a power plant plume showed good ability to reproduce nocturnal peaks recorded by an urban air quality station. The increase in resolution resulted in an improvement of model sensitivity. The nesting to subkilometer grids helped to reduce an overestimation bias mainly because the LES domains better simulate the turbulent motions governing nocturnal flows. For peaks observed at two air quality stations, the backward sensitivity outputs identified realistic sources of NOx in the area. The increase in resolution produced a sharper inverse plume with a more accurate source area. This study showed the first application of the FLEXPART-WRF model to microscale resolutions. Overall, the coupling model WRF-LES-FLEXPART is useful to simulate the pollutant dispersion during a real case of calm wind regime over a complex terrain area. The forward and backward simulation results showed clearly that the subkilometer resolution of 333 m is necessary to reproduce realistic air pollution patterns in this case of short-range transport over a complex terrain area. Globally, this work contributes to enrich the sparsely documented domain of real nested microscale air pollution modelling. This study dealing with the determination of the proper resolution grid and proper turbulence scheme, is of significant interest to the near-source and complex terrain air quality research community.
ISSN: 1352-2310

hal-01349208
https://hal.archives-ouvertes.fr/hal-01349208
DOI : 10.1016/j.atmosenv.2016.05.028

Éditeur(s) : HAL CCSD Springer Verlag
Résumé : International audience
ISSN: 0258-8900

hal-00682343
https://hal.archives-ouvertes.fr/hal-00682343
DOI : 10.1007/s00445-011-0554-0

Éditeur(s) : HAL CCSD Ecological Society of America
Résumé : We investigated the relationship between habitat association and physiological performance in four congeneric species pairs exhibiting contrasting distributions between seasonally flooded and terra firme habitats in lowland tropical rain forests of French Guiana, including Virola and Iryanthera (Myristicaceae), Symphonia (Clusiaceae), and Eperua (Caesalpiniaceae). We analyzed 10-year data sets of mapped and measured saplings (stems 150 cm in height and <10 cm diameter at breast height [dbh]) and trees (stems 10 cm dbh) across 37.5 ha of permanent plots covering a 300-ha zone, within which seasonally flooded areas (where the water table never descends below 1 m) have been mapped. Additionally, we tested the response of growth, survival, and leaf functional traits of these species to drought and flood stress in a controlled experiment. We tested for habitat preference using a modification of the torus translation method. Strong contrasting associations of the species pairs of Iryanthera, Virola, and Symphonia were observed at the sapling stage, and these associations strengthened for the tree stage. Neither species of Eperua was significantly associated with flooded habitats at the sapling stage, but E. falcata was significantly and positively associated with flooded forests at the tree stage, and trees of E. grandiflora were found almost exclusively in nonflooded habitats. Differential performance provided limited explanatory support for the observed habitat associations, with only congeners of Iryanthera exhibiting divergent sapling survival and tree growth. Seedlings of species associated with flooded forest tended to have higher photosynthetic capacity than their congeners at field capacity. In addition, they tended to have the largest reductions in leaf gas exchange and growth rate in response to experimental drought stress and the least reductions in response to experimental inundation. The corroboration of habitat association with differences in functional traits and, to a lesser extent, measures of performance provides an explanation for the regional coexistence of these species pairs. We suggest that specialization to seasonally flooded habitats may explain patterns of adaptive radiation in many tropical tree genera and thereby provide a substantial contribution to regional tree diversity.
ISSN: 0012-9658

hal-01031746
https://hal.archives-ouvertes.fr/hal-01031746

Éditeur(s) : HAL CCSD The International Journal of the Tsunami Society
Résumé : http://library.lanl.gov/tsunami/231/pel.pdf
A strong earthquake (mb = 6.3; Ms = 6.1; Mw = 6.3) occurred on 21 November 2004 in the Dominica Passage separating Guadeloupe and Dominica, in the Lesser Antilles, and generated a weak tsunami with maximum amplitudes of +70 and -80 cm on neighbouring islands. We conducted field surveys on the islands of “Les Saintes”, in the immediate vicinity of the epicenter on November 27, 2004 and February 12, 2005, and report here on the resulting dataset.
ISSN: 8755-6839

hal-00095039
https://hal.archives-ouvertes.fr/hal-00095039

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Le cantonnement de pêche est un outil administratif et juridique français employé pour la gestion de la ressource halieutique et la réglementation de la pêche sur un site marin défini. Cet outil a été mis en place à la Martinique (Petites Antilles) en 1999, à la demande des marins-pêcheurs confrontés à la raréfaction des stocks de poissons au sein de la bande côtière. Les autorités compétentes sur le milieu marin ont installé ce dispositif sur huit zones réparties autour de l’île (de la côte Atlantique à la côte Caraïbes). Le cantonnement de pêche reste peu documenté scientifiquement à ce jour, en dehors d’inventaires ichtyologiques réalisés par des scientifiques-biologistes. Il est donc opportun de retracer les étapes de la mise en place de cet outil et d’analyser les premiers résultats et les enjeux.
Cantonment fishing is a French legal and administrative tool used to manage fisheries resources and the regulation of fishing on marine site defined. This tool was developed in Martinique (Lesser Antilles) in 1999, at the request of fishermen facing depletion of fish stocks in the coastal strip. The competent authorities on the marine environment have installed this device on eight areas spread around the island (the Atlantic coast to the Caribbean coast). Cantonment fishing is little scientifically documented to date, apart from fishery surveys conducted by scientists-biologists. It is therefore appropriate to retrace the steps of the development of this tool and analyze the first results and challenges.
Martinique

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.6800
http://journals.openedition.org/etudescaribeennes/6800

Éditeur(s) : HAL CCSD Copernicus Publications on behalf of the European Geosciences Union
Résumé : International audience
During the GWADASEIS cruise (Lesser Antilles volcanic arc, February–March 2009) a very high resolution (VHR) seismic-reflection survey was performed in order to constrain Late Quaternary to Present faulting. The profiles we obtained evidence frequent " ponding " of reworked sediments in the deepest areas, similar to the deposition of Mediterranean " homogenites ". These bodies are acoustically transparent (few ms t.w.t. thick) and are often deposited on the hanging walls of dominantly normal faults, at the base of scarps. Their thickness appears sufficient to compensate (i.e. bury) co-seismic scarps between successive earthquakes, resulting in a flat and horizontal sea floor through time. In a selected area (offshore Montserrat and Nevis islands), piston coring (4 to 7 m long) was dedicated to a sedimento-logical analysis of the most recent of these particular layers. It corresponds to non-stratified homogenous calcareous silty sand (reworked calcareous plankton and minor volcanoclas-tics). This layer can be up to 2 m thick, and overlies fine-grained hemipelagites. The upper centimeters of the latter represent the normal RedOx water/sediment interface. 210 Pb and 137 Cs activities lack in the massive sands, while a normal profile of unsupported 210 Pb decrease is observed in the hemipelagite below, together with a 137 Cs peak corresponding to the Atmospheric Nuclear Experiments (1962). The RedOx level was thus capped by a recent instantaneous major sedimentary event considered as post-1970 AD; candidate seismic events to explain this sedimentary deposits are either the 16 March 1985 earthquake or the 8 October 1974 one (M w = 6.3 and M w = 7.4, respectively). This leads to consider that the syntectonic sedimentation in this area is not continuous but results from accumulation of thick homogen-ites deposited after the earthquakes (as observed in the following weeks after Haiti January 2010 event, McHugh et al., 2011). The existence of such deposits suggests that, in the area of study, vertical throw likely results from cu-mulated effects of separated earthquakes rather than from aseismic creep. Examination of VHR profiles shows that all major co-seismic offsets are recorded in the fault growth sequence and that co-seismic offsets can be precisely estimated. By using a sedimentation rate deduced from 210 Pb decrease curve (0.5 mm yr −1) and taking into account minor reworking events detected in cores, we show that the Redonda system may have been responsible for five > M 6 events during the last 34 000 yr. The approach presented in this work differs from fault activity analyses using displaced sets of isochronous surfaces and postulating co-seismic offsets. Combining VHR seismic imagery and coring we can decipher co-seismic vs. slow continuous displacement, and thus actually estimate the amplitude and the time distribution of major co-seismic offsets.
Natural Hazards and Earth System Science

insu-01585969
https://hal-insu.archives-ouvertes.fr/insu-01585969
https://hal-insu.archives-ouvertes.fr/insu-01585969/document
https://hal-insu.archives-ouvertes.fr/insu-01585969/file/nhess-12-1755-2012-beck.pdf
DOI : 10.5194/nhess-12-1755-2012

Éditeur(s) : HAL CCSD
Résumé : Meteorological phenomena with scales lower than hurricanes, from extreme rainfalls to pollution peaks, represent important environmental and health risks in the Caribbean. These examples show the need to downscale large-scale meteorological data to island-scale fields.The main goal of the present numerical study is the analysis of the meso- and micro-scale mechanisms inducing diurnal and nocturnal circulations in the Guadeloupe archipelago. The Weather Research and Forecasting model is employed. The micro-scale results are obtained by the coupling of the 1-km simulated fields and the Large Eddy Simulation method. Then, in order to analyze the dispersion of a pollutants plume, the micro-scale outputs with 111 m of resolution are used to force the lagrangian particles dispersion model FLEXPART. The study has been conducted for three real cases of weather types linked with strong, medium and weak trade winds.The results of simulations, validated with available observed data, permitted to simulate all local circulations, including a nocturnal counter-current flow which may induce a pollution peak in the urban area of Pointe-à-Pitre city.These works, which may be applied to other Lesser Antilles islands, suggest many environmental and energy applications.
Les phénomènes météorologiques d'échelles inférieures aux cyclones, depuis les pluies intenses, jusqu'à la dégradation de la qualité de l'air, ont pour les Caraïbes une importance aiguë en termes de risques naturels ou de risques sur la santé. Ces exemples attestent de la nécessité d'utiliser des méthodes de descentes d'échelle pour exploiter l'information météorologique de grande échelle et dériver des scénarios locaux appliqués aux territoires insulaires. Les travaux présentés ont pour principaux objectifs la simulation numérique et l'analyse des mécanismes méso- et micro-échelles qui induisent des circulations locales diurnes et nocturnes sur l'archipel de la Guadeloupe, à l'aide du modèle numérique météorologique Weather Research and Forecasting. Les résultats des simulations micro-échelles sont obtenus par le couplage des champs modélisés à 1 km avec la méthode Large Eddy Simulation. Les sorties micro-échelles, à 111 m, sont ensuite utilisées pour forcer le modèle lagrangien de dispersion de particules FLEXPART afin d'étudier la dispersion d'un panache de polluants. L'étude a été menée pour trois cas réels de situations météorologiques correspondant à des alizés soutenus, moyens et faibles. Les résultats des simulations, après validation, et comparaison aux données d'observation disponibles, permettent de restituer l'ensemble des circulations locales et soulignent l'existence d'un écoulement nocturne à contre courant susceptible d'induire une forte pollution sur la zone urbaine de Pointe-à-Pitre. Cette étude, transposable aux autres îles des petites Antilles, laisse envisager de nombreuses applications environnementales et énergétiques.
https://hal.archives-ouvertes.fr/tel-01074600

Droits : info:eu-repo/semantics/OpenAccess
tel-01074600
https://hal.archives-ouvertes.fr/tel-01074600
https://hal.archives-ouvertes.fr/tel-01074600/document
https://hal.archives-ouvertes.fr/tel-01074600/file/rcece_thesis.pdf