Éditeur(s) : Université des Antilles et de la Guyane. Service commun de la documentation Université des Antilles et de la Guyane. Service commun de la documentation
Résumé : Lancement officiel de Manioc, la bibliothèque numérique spécialisée sur la Caraïbe, l'Amazonie et le plateau des Guyane, en présence des représentants de la bibliothèque nationale de France et des partenaires de Manioc. Présentation de l'interface, des contenus : ouvrages et illustrations patrimoniaux, catalogue collectif des périodique, revue Etudes caribéennes, TRAMIL (pharmacopée traditionnelle). Présentation de Gallica.
Martinique
21

Droits : Document protégé par le droit d'auteur
fichiers:HASH01d891035183d9bcce1fe085

Éditeur(s) : Université des Antilles et de la Guyane Université des Antilles et de la Guyane. Service commun de la documentation Université des Antilles et de la Guyane. Service commun de la documentation
Extrait de : "Inauguration de la bibliothèque numérique Manioc", le 11 décembre 2009. Université des Antilles et de la Guyane
Résumé : Lancement officiel de Manioc, la bibliothèque numérique spécialisée sur la Caraïbe, l'Amazonie et le plateau des Guyanes, en présence des représentants de la Bibliothèque Nationale de France et des partenaires de Manioc. Présentation de l'interface, des contenus : ouvrages et illustrations patrimoniaux, catalogue collectif des périodiques, revue Etudes caribéennes, TRAMIL (pharmacopée traditionnelle). Présentation de Gallica.
Lancement officiel de Manioc, la bibliothèque numérique spécialisée sur la Caraïbe, l'Amazonie et le plateau des Guyanes, en présence des représentants de la Bibliothèque Nationale de France et des partenaires de Manioc. Présentation de l'interface, des contenus : ouvrages et illustrations patrimoniaux, catalogue collectif des périodiques, revue Etudes caribéennes, TRAMIL (pharmacopée traditionnelle). Présentation de Gallica.
Siècle(s) traité(s) : 21
Droits : CC-BY-NC-ND - Attribution - Pas d'utilisation commerciale - Pas de modification
Provenance : Université des Antilles et de la Guyane. Service commun de la documentation
Permalien : http://www.manioc.org/fichiers/HASH01d891035183d9bcce1fe085
HASH01d891035183d9bcce1fe085
HASH01d891035183d9bcce1fe085
HASH01d891035183d9bcce1fe085

Résumé : This paper calls back the needs of cartography of the interface between lands and sea and assesses the characteristics of this interface in terms of knowledge as spatial and temporal constraints. After a brief typology of the different thematic cartographies of coasts and their applications we develop the contribution of the digital high resolution satellite image and we lean on an example (inventory of aquaculture sites in inter-tropical zone) which meets the three basic needs of localization, quantification and economic planning.
On rappelle les besoins de cartographie de l’interface entre terres et mers et on fait un bilan des caractéristiques de cette interface en termes de connaissances, de contraintes spatiales et temporelles. Après une typologie succincte de la cartographie des littoraux et de leurs applications on développe l‘apport de l’image numérique satellite de haute résolution et on s’appuie sur un exemple (celui de la présélection de sites aquacoles en zone intertropicale) qui répond aux trois besoins fondamentaux besoins de localisation, de quantification (inventaire) et de planification (prévision).

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/00189/29991/28439.pdf
http://archimer.ifremer.fr/doc/00189/29991/

Éditeur(s) : George A. Smathers Libraries, University of Florida George A. Smathers Libraries, University of Florida ( Gainesville, FL )
Résumé : Listing of all terms for translation work for translating the SobekCM interface. This workbook includes 3 spreadsheets: localization strings, external HTML chunks, and general translations. This workbook is set up for ease for translations and ease of programmatic inclusion in SobekCM.

Droits : [cc0] The author dedicated the work to the Commons by waiving all of his or her rights to the work worldwide under copyright law and all related or neighboring legal rights he or she had in the work, to the extent allowable by law.
http://ufdc.ufl.edu/AA00017119/00031

Éditeur(s) : Université Bordeaux 1
Résumé : The mercury cycle was explored in the Petit-Saut reservoir / Sinnamary Estuary continuum in French Guiana. Main processes involve (i) photo-induced reduction, (ii) adsorption and desorption at the particle surfaces, (iii) methylating bacterial activity, (iv) precipitation and dissolution of iron oxyhydroxides and sulfides. Sources of mercury to the Petit-Saut reservoir consist of the partly impacted river-tributaries, the atmospheric deposition and the flooded soils or vegetation. Once into the reservoir, divalent mercury undergoes a large spectrum of transformations including speciation and phase changes. We, here, probe these processes and demonstrate that the Petit-Saut reservoir behaves as a privileged site for atmospheric recycling and in situ methylation. At the air / water interface, the mercury evasion exceeds by 50 % the direct atmospheric deposition. The in situ monomethylmercury (MMHg) production mostly occurs at the water-column chemocline and near the benthic interface. It reaches, for the whole reservoir, 8.1 moles yr-1 which corresponds to a 0.06 % d-1 methylation rate. We calculated that the 2003/04 period MMHg outputs from the reservoir to the Sinnamary Estuary averaged 13.5 moles yr-1 while the inputs were 5.4 moles yr-1. The dynamic Sinnamary Estuary is the genuine geochemical reactor of the continuum. There, the divalent mercury undergoes rapid yet profound partitioning among phases, recycling to the atmosphere and methylation processes. Those mostly originate from the long-scale oxygen paucity of the dam discharged waters. The expression of marked redox gradients and the intense organic matter turnover enhance the production of methylable inorganic mercurial species and tend to favor the sulfate reducing bacteria (methylating agents) activity. As a result, the dynamic Sinnamary Estuary exports 60 % more MMHg than it does import: 27 versus 17 moles yr-1. Further at large, in the saline estuary, we determined: (i) a non conservative behavior of dissolved (< 0.2 µm) mercury, (ii) a lowering of the mercury level of particles during mixing with the Amazon plume and (iii) a gradual dilution of the estuarine mercury concentrations by oceanic waters.
La retenue de Petit-Saut et, à l'aval, l'estuaire du Sinnamary sont deux centres d'altération du cycle naturel du mercure. Les processus sont, entre autres, (i) la photoréduction, (ii) la sorption / désorption en surface des particules, (iii) l'activité méthylante des bactéries, (iv) la dissolution / précipitation des oxyhydroxydes et des sulfures de fer. Les sources de mercure vers la retenue sont variées. Elles regroupent, en premier lieu, les affluents (partiellement orpaillés), l'atmosphère, les sols et la végétation ennoyés. Dans la colonne d'eau, les formes divalentes du mercure subissent un train complet de transformations couplant changements de phase et de spéciation. Nos résultats illustrent ces processus et démontrent que la retenue constitue un site privilégié de recyclage vers l'atmosphère et de méthylation. A l'interface air / eau, les exports en mercure de la retenue excèdent de 50 % le dépôt atmosphérique. La production endogène de monométhylmercure (MMHg) a lieu dans des sites particuliers : la chemocline et l'interface benthique. Elle atteint pour l'ensemble de la retenue 8,1 moles a-1 soit un taux de méthylation de 0,06 % j-1. On estime que la retenue exporte vers l'estuaire du Sinnamary 13,5 moles a-1 de MMHg alors qu'elle n'importe que 5,4 moles a-1. L'estuaire dynamique du Sinnamary constitue le véritable réacteur chimique du système fonctionnant en liaison avec celui de la retenue. Le mercure y décrit un cycle rapide aux processus de partition, de recyclage et de méthylation marqués. Ces processus résultent de l'oxygénation incomplète et durable des masses d'eau anoxiques exportées par la retenue de Petit-Saut. L'expression de gradients rédox prononcés conjuguée à un intense recyclage de la matière organique y favorise la production de formes méthylables de mercure ainsi que l'activité des bactéries sulfatoréductrices (agents de la méthylation). C'est pourquoi, l'estuaire dynamique du Sinnamary exporte 60 % plus de MMHg qu'il n'importe : 27 contre 17 moles a-1. Plus en aval, dans l'estuaire salin, nous avons mis en évidence : (i) un comportement non conservatif du mercure dissous, (ii) un appauvrissement du mercure des particules suite au mélange avec le panache de l'Amazone et (iii) une dilution des concentrations par les masses d'eau océaniques.

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/2006/these-1508.pdf
http://archimer.ifremer.fr/doc/00000/1508/

Éditeur(s) : Université des Antilles et de la Guyane IRD : Institut de Recherche pour le Développement
Extrait de : "Projet CARIBSAT, système caribéen d'information environnementale" : conférence, le 21 mars 2013. Université des Antilles et de la Guyane
Description : A l'interface entre bassins versants et coraux, la mangrove a un rôle fonctionnel primordial. Milieu naturel exceptionnel à la biodiversité importante, la mangrove de Génipa est fortement soumise à des pressions anthropiques, mais aussi aux risques naturels. La télédétection a permis de comparer la structure de la végétation de cette zone, avant et après le cyclone DEAN.
Siècle(s) traité(s) : 21
Droits : CC-BY-NC-ND - Attribution - Pas d'utilisation commerciale - Pas de modification
Permalien : http://www.manioc.org/fichiers/V13093
V13093

Éditeur(s) : Inter-Research
Résumé : On the western coast of the Atlantic, according to the literature, 2 distinct groups of Semibalanus balanoides occur with a distinct interface near the Miramichi Estuary, New Brunswick, in the Gulf of St. Lawrence. On each side of this interface, the groups are characterized by clinal variations for MPI (mannose-6-phosphate isomerase) and GPI (glucose-6-phosphate isomerase). The present study was carried out to determine whether selection occurs at this interface, to establish how early in the sessile life period it occurs and to examine the selecting forces involved. Reciprocal transplant experiments of newly settled individuals to both sides of the interface were carried out. No significant differences specifically linked to source or destination were observed in growth or fecundity for the 2 groups at the sites studied for either control or transplanted individuals. However, differences in survival were observed; individuals transplanted south of the estuary showed lower survival than individuals transplanted north. An allozyme analysis of barnacle survivors for MPI and GPI, 2 alleles whose frequencies are known to vary abruptly in this region, indicated a change of allele frequency in transplanted individuals. The transplants’ allele frequencies came to resemble those of adults from target sites, while no change occurred in transplanted individuals at control sites. Taken together with previous results, our study suggests that selection occurs very early in the newly settled individuals (spat).
Marine Ecology Progress Series (0171-8630) (Inter-Research), 2002-03 , Vol. 229 , P. 173-184

Droits : Inter-Research 2002
http://archimer.ifremer.fr/doc/00048/15970/13410.pdf
DOI:10.3354/meps229173
http://archimer.ifremer.fr/doc/00048/15970/

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : À travers la notion d’interface transnationale, cet article propose une reconceptualisation des formes géographiques observées sur la façade caraïbe de l’Amérique centrale en ce début de XXIe siècle. L’héritage des diverses enclaves – en premier lieu bananières – et des acteurs extérieurs qui leur ont traditionnellement été liés a ici engendré des territoires aux configurations similaires, marqués par des interactions locaux globaux, mais profondément conditionnés par l’échelon national.
Through the concept of transnational interface, this paper proposes a reconceptualization of geographical forms on the Caribbean coast of Central America in the early 21st century. The heritage of the various enclaves - and firstly the banana's - and external actors which have traditionally been linked to them, has led to similar territories, characterized by local-global interactions, deeply conditioned by the national level.
Amérique centrale
Caraïbes

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.6046
http://journals.openedition.org/etudescaribeennes/6046

Éditeur(s) : HAL CCSD Oxford University Press (OUP)
Résumé : International audience
At Cima di Gagnone, garnet peridotite and chlorite harzburgite lenses within pelitic schists and gneisses correspond to eclogite-facies breakdown products of hydrated peridotites and are suitable for studying dehydration of serpentinized mantle. Thermobarometry and pseudosection modelling yield peak temperatures of 750-850°C and pressures <3 GPa. The minimum temperature recorded by the garnet peridotite corresponds to the maximum conditions experienced by the chlorite harzburgite, suggesting that these rocks recrystallized cofacially at ∼800°C. Alternatively, they might have decoupled during subduction, as achieved in tectonically active plate interface boundaries. The major and rare earth element (REE) variability of the peridotites was mostly acquired during pre-subduction mantle evolution as a result of partial melting and reactive melt flow. The ultramafic suite is also characterized by fluid-mobile element enrichments (B, Pb, As, Sb, Cs, Li, U, Be), which confirm derivation from variably serpentinized protoliths. Similarity in the U, Pb, B, Li and Sr contents of the Gagnone peridotites to present-day oceanic serpentinites suggests that these elements were partly taken up during initial serpentinization by seawater-derived fluids. Positive Be, As and Sb anomalies suggest involvement of fluids equilibrated with crustal (metasedimentary) reservoirs during subsequent subduction metamorphism and peridotite entrainment in (meta)sediments. Fluid-mobile element enrichment characterizes all peak eclogitic minerals, implying that multiple hydration events and element influx pre-dated the eclogite-facies dehydration. Peak anhydrous minerals retain B, Li, As and Sb concentrations exceeding primitive mantle values and may introduce geochemical anomalies into the Earth's mantle. The relatively low contents of large ion lithophile elements and light REE in the Gagnone peridotites with respect to much higher enrichments shown by metasomatized garnet peridotite pods hosted in migmatites (Ulten Zone, Eastern Alps) suggest that the crustal rocks at Gagnone did not experience partial melting. The Gagnone garnet peridotite, despite showing evidence for chlorite dehydration, retains significant amounts of fluid-mobile elements documenting that no partial melting occurred upon chlorite breakdown. We propose that the Gagnone ultramafic rocks represent a prime example of multi-stage peridotite hydration and subsequent dehydration in a plate interface setting.
ISSN: 0022-3530

hal-01054319
https://hal.archives-ouvertes.fr/hal-01054319
DOI : 10.1093/petrology/egt068

Éditeur(s) : HAL CCSD
Résumé : International audience
L'avènement des interfaces orientées stylo à conduit au développement de nombreuses applications concernant l'analyse d'une forme dessinée à main levée. Mais un dessin, ce n'est pas uniquement une forme, c'est également l'ensemble des gestes constituant l'activité de tracé ayant donné naissance à la trace. Les interfaces orientées stylo nous donnent la possibilité d'analyser cette dimension du dessin. Nous appelons ce type d'analyse : analyse procédurale. Dans cet article, nous allons montrer comment identifier les procédures de dessin privilégiées des utilisateurs, et ce malgré une grande variabilité intra-scripteur, en utilisant une méthode de filtrage du bruit procédural. Puis nous montrerons un exemple d'application de cette approche en proposant une méthode de reconnaissance de dessinateur basée sur l'analyse procédurale.
Actes du Colloque International Francophone sur l'Écrit et le Document 2012
Bordeaux, France

hal-00698875
https://hal.archives-ouvertes.fr/hal-00698875

Éditeur(s) : HAL CCSD Oxford University Press (OUP): Policy B - Oxford Open Option A Oxford University Press (OUP)
Résumé : International audience
Peridotite xenoliths exhumed by Quaternary alkaline magmatism in the Tahalgha district, southern Hoggar, represent fragments of the subcontinental lithospheric mantle beneath the boundary between the two major structural domains of the Tuareg Shield: the ‘Polycyclic Central Hoggar’ to the east and the ‘Western Hoggar’, or ‘Pharusian Belt’, to the west. Samples were collected from volcanic centres located on both sides of a major lithospheric shear zone at 4°35' separating these two domains. Although showing substantial variations in their deformation microstructures, equilibrium temperatures and modal and chemical compositions, the studied samples do not display any systematic changes of these features across the 4°35' fault. The observed variations rather record small-scale heterogeneities distributed throughout the study area and reflecting the widespread occurrence of vein conduits and metasomatized wall-rocks related to trans-lithospheric melt circulation during the Cenozoic. These features include partial annealing of pre-existing deformation microstructures, post-deformation metasomatic reactions, and trace-element enrichment, coupled with heating from 750–900°C (low-temperature lherzolites) to 900–1150°C (intermediate-T lherzolites and high-T harzburgites and wehrlites). Trace-element modelling confirms that the range of rare earth element (REE) variations observed in the Tahalgha clinopyroxenes may be accounted for by reactive porous flow involving a single stage of basaltic melt infiltration into a light REE (LREE)-depleted protolith. Whole-rock compositions record the final entrapment of disequilibrium metasomatic melts upon thermal relaxation of the veins–wall-rock system. The striking correlations between equilibrium temperatures and trace-element enrichment favor a scenario in which the high-temperature peridotites record advective heat transport along melt conduits, whereas the intermediate- and low-temperature lherzolites reflect conductive heating of the host Mechanical Boundary Layer. This indicates that the lithosphere did not reach thermal equilibrium, suggesting that the inferred heating event was transient and was rapidly erased by thermal relaxation down to the relatively low-temperature present-day geotherm. The low-T (<900°C) deformed lherzolites (porphyroclastic to equigranular) are characterized by only incipient annealing and LREE-depleted clinopyroxene compositions. They were only weakly affected by the Cenozoic events and could represent relatively well-preserved samples from rejuvenated Pan-African lithosphere. Extensive lithospheric rejuvenation occurred either regionally during the Pan-African orogeny, as a result of lithospheric delamination or thermomechanical erosion after thickening, or more locally along the meridional shear zones. The low-T Tahalgha lherzolites are comparable with lherzolites from Etang de Lherz, southern France, interpreted as lithospheric mantle rejuvenated by melt-induced refertilization during a late stage of the Variscan orogeny.
ISSN: 0022-3530

hal-01107410
https://hal.archives-ouvertes.fr/hal-01107410
DOI : 10.1093/petrology/egu056

Éditeur(s) : Springer
Résumé : The Golo Margin in eastern Corsica is dissected by four canyons and two gullies which fed turbidite systems. Study of the dispersal of surficial sediments and flow dynamic in the Golo system is based on Kullenberg and interface cores interpreted in relation to a previously published seismic dataset. Cores were described in detail and interpreted within a sedimentary and stratigraphic framework. During the last 42,000 years, gravity processes which occurred in the large systems with a canyon source were mainly slide-induced, differentiated turbulent surges and hyperpycnal flows. Processes occurring in the small system with a gully source are mainly hyperconcentrated and concentrated flows. Deposits from the Corsican Margin can intercalate with products of processes triggered on the Pianosa Ridge located in the eastern part of the basin. During relative sea-level lowstands or during periods of rapid or high-amplitude sea-level fall, only large canyons (South and North Golo) are supplied by carbonate-rich hyperconcentrated and concentrated flows which are channelled in incised valleys on the shelf. During periods of slow or low-amplitude sea-level fall and during sea-level rise, sediments are trapped on a shelf delta and intensely winnowed by shelf hydrodynamic processes. Sand-rich hyperconcentrated and concentrated flows occur. All the systems fed by a canyon are active simultaneously. Gullies form and are active only during periods of sea-level rise. During relative highstands of sea level (Holocene), all the system is draped by hemipelagic sediments. Relative sea-level changes and canyon location relative to river mouths have a strong influence on the nature of sediment input, and the initiation and type of gravity flows which, in turn, control morphology and geometry.
Geo-Marine Letters (0276-0460) (Springer), 2006-12 , Vol. 26 , N. 6 , P. 373-395

Droits : 2006 Springer
http://archimer.ifremer.fr/doc/2006/publication-3594.pdf
DOI:10.1007/s00367-006-0045-z
http://archimer.ifremer.fr/doc/00000/3594/

Résumé : Le Brésil et la France partagent une frontière commune sur plus de 700 kilomètres, via la Guyane, région monodépartementale d’Outre-Mer française, et l’Amapá, Etat de la République fédérative du Brésil. Réalité socio-spatiale en marges à toutes les échelles malgré le différentiel socio-économique fort qu’elle marque, la frontière franco-brésilienne est devenue, depuis les années 1990, une interface politique, support de la relance des relations internationales franco-brésiliennes et des relations entre Guyane et Amapá.La thèse pose la question de cet écart en se concentrant sur la partie estuarienne de la frontière fluviale de l’Oyapock, autour des bourgs riverains de Saint-Georges (Guyane française) et d’Oiapoque (Brésil), entre lesquels un pont binational d’envergure est en construction, malgré leur rattachement routier à la marge aux polarités régionales de Cayenne et de Macapá.
Brazil and France share a common border of over 700 km via French Guiana, a French Overseas monodepartmental region, and Amapá, State of the Federal Republic of Brazil. Socio-spatial margin at all scales despite the strong socio-economic differential it marks, the Franco-Brazilian border has become since the 1990s a political interface, support for the revival of the Franco-Brazilian international relations and of the relations between French Guiana and Amapá. The thesis raises the question of this gap, focusing on the estuarine portion of the border river of the Oyapock, around the towns of Saint-Georges (French Guiana) and Oiapoque (Brazil) ; a significant bi-national bridge is under construction between these two towns, despite their road connection as margins to the regional polarities of Cayenne and Macapá.
Brasil e França compartilham uma fronteira comum com mais de 700 km através da Guiana Francesa, Região monodepartamental ultramarina francesa, e do Amapá, Estado da República Federativa do Brasil. Realidade sócio-espacial à margem a todas as escalas, apesar do forte diferencial sócio-econômico que a marca, a fronteira franco-brasileira tornou-se, desde os anos 90, uma interface política, suporte para a retomada das relações internacionais franco-brasileiras e das relações entre a Guiana Francesa e o Amapá. A tese expõe a questão deste desnível, centrando-se na porção estuarina da fronteira fluvial do Oiapoque, ao redor das pequenas cidades de Saint-Georges (Guiana Francesa) e de Oiapoque (Brasil), entre as quais uma ponte binacional de grande porte está em construção, apesar da ligação rodoviária delas como margens aos pólos regionais de Caiena e Macapá.

http://www.theses.fr/2012AGUY0504/document

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Afin de mettre en perspective les différents articles du dossier, le texte souligne les différentes étapes qui définissent la situation de la façade caraïbe à la fois au sein des Etats-nations et de la région centraméricaine. Depuis une position de marge ou d’enclave liée à la fois à la géographie et aux logiques de l’empire espagnol, cet ensemble territorial s’est construit à partir de fragments plus ou moins connectés entre eux et aux espaces régionaux maritimes (caribéen ou atlantique). Au cours de leur construction, les différents Etats-nations n’envisagent d’abord la façade caraïbe que dans sa dimension de connexion transisthmique. Pourtant, on constate au vingtième siècle différents processus d’intégration territoriale qui visent à relier espace continental et façade caraïbe, processus qu’il faut associer à de nouvelles dynamiques démographiques. Les sociétés d’interface qui en résultent, voient leurs composantes « ladinas », indiennes, ou afro-descendantes se réorganiser. Enfin, ces fragments qui composent la façade prennent de nouvelles couleurs à la lumière des projections faites par d’autres acteurs (ONG) ou à d’autres échelles (région américaine).
In order to put into perspective the different papers of the issue, this text highlights the successive stages by which the Caribbean coastline of Central American has been constructed, under the several States-nations and as a part of the Central American region. As a margin or enclave due to geographical characters as to the logics of Spanish Empire, these territories have been made from fragments more or less connected between them or to other regional maritime spaces (Caribbean or Atlantic). When growing, the States-nations in the region first exclusively consider their Caribbean coastline as a transisthmic connection. Yet, during the twentieth century, various process of territorial integration aim to connect continental spaces and maritime coastline, associating demographical dynamics. Societies of interface result of these process, where their ladina, indian, afro components are reorganized. Finally, theses fragments as elements of the façade take a new color in the look of new actors (NGO) or from other scales and spaces (Atlantic region, Caribbean Sea).
Para poner en perspectiva los diferentes artículos del numero temático, este texto subraya las varias etapas en que definieron la situación de la costa caribeña, a la vez en cada Estado-Nacion y al nivel de la región. Con una posición de margen o enclave, que se explica tan por motivos geográficos que por las lógicas del imperio español, este conjunto territorial se ha construido a partir de fragmentos más o menos conectados entre sí e con los espacios regionales marítimos (caribeño o atlántico). Cuando se desarrollaron, los Estados-naciones consideraban las costas caribeñas solo por su potencial transístmico. Sin embargo, en el siglo veinte, llevaron a cabo varios procesos de integración territorial que les permiten vincular su espacio continental con la fachada atlántica, y eso asociándose a importantes dinámicas poblacionales. Resultan de estos procesos sociedades de interfaz, cuyos componentes ladinos, indígenas y afros se ven reorganizados. Por fin, los fragmentos que componen la costa caribeña toman otro color a la luz de proyectos llevados por actores ajenos (ONG) o desde espacios y escalas diferentes (Espacio atlántico, región americana).
Amérique centrale
Caraïbes
Livingston
Guatemala

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.6032
http://journals.openedition.org/etudescaribeennes/6032

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
In this study, we report new U-Pb zircon ages and amphibole and biotite 40Ar-39Ar cooling ages for igneous and metaigneous rocks from the eastern portion of the Borborema Province (NE Brazil). We combine these results with preliminary thermobarometric estimates and existing data to place constraints on the timing and duration of the Brasiliano-Pan-African Orogeny in northeastern Brazil and on the subsequent late- to post-orogenic history. The Alcantil orthogneiss contains a complex zircon population, but the youngest concordant analyses yielded an age of 632 ± 17 Ma (2σ). These grains have low Th/U ratios (<0.1), and the age of 632 Ma is therefore interpreted as dating the metamorphic event responsible for the acquisition of the gneissic fabric. In the Caruaru biotite amphibole orthogneiss, concordant analyses provided an age of 618 ± 4 Ma (2σ), which we relate to emplacement of the protolith of the Caruaru orthogneiss. Together with available U-Pb data from the literature, the 632-600 Ma age range is regarded as dating development of a regional flat-lying foliation coeval with high-grade metamorphism (upper amphibolite facies conditions). The 586 ± 3 Ma age (2σ) of the Panelas pluton is similar to those of other granitic plutons associated with a voluminous plutonism of high-K calc-alkaline to shoshonitic nature that occurred at 590-580 Ma. This plutonism slightly predated or was synchronous with development of large strike-slip shear zones. Amphibole grains yielded 40Ar-39Ar ages ranging from 584 ± 4 Ma to about 530 Ma, suggesting that regional temperatures remained near the closing temperature of this mineral (≈500 °C) for a long time. Most 40Ar-39Ar biotite ages range from 552 to 533 Ma, but two samples yielded plateau ages of 519 ± 5 Ma and 509 ± 5 Ma. The inferred rather slow cooling of the studied region possibly reflects low rates of unroofing, allowing persistence of a protracted thermal anomaly caused by the massive injection of magmas at the end of the Neoproterozoic.
ISSN: 0895-9811

hal-00745698
https://hal.archives-ouvertes.fr/hal-00745698
DOI : 10.1016/j.jsames.2012.06.003

Éditeur(s) : Elsevier
Résumé : A field survey was conducted on two intensive shrimp farms using similar technical practices: one (DF) historically affected by a vibriosis, the other (HC) in which the pathogen has been observed although no mortality event has occurred. Because historical data suggest that eutrophication process may directly or indirectly play a role in the disease outbreak, we focussed our research on its dynamics. A higher variability of the phytoplanktonic compartment linked to an imbalance in the molar N:P ratio was observed in farm DF compared to farm HC, implying a modification on the linkage between the bacteria and phytoplankton compartments at DF. The beginning of the mortality outbreak at DF followed a shift from picoto nanophytoplankton. The organic matter mineralization process at the water-sediment interface may explain the disturbance observed in the water column during eutrophication. The consequences of this disturbance on shrimps' health status and pathogen ecology are discussed. (C) 2009 Elsevier Ltd. All rights reserved.
Marine Pollution Bulletin (0025-326X) (Elsevier), 2010-03 , Vol. 60 , N. 3 , P. 402-411

Droits : 2010 Elsevier B.V. All rights reserved.
http://archimer.ifremer.fr/doc/00002/11368/8119.pdf
DOI:10.1016/j.marpolbul.2009.10.012
http://archimer.ifremer.fr/doc/00002/11368/

Éditeur(s) : HAL CCSD Oxford University Press (OUP)
Résumé : International audience
Several studies, both theoretical and experimental, show that sedimentary rocks have a fractal pore-grain interface. In this paper a computer simulated 3-D sedimentary rock structure generated by the Relaxed Ballistic Bidisperse Deposition Model (RBBDM), is investigated to characterize the micro structure of its pores. The pore volume and the rock-pore interface show the same fractal dimension indicating that the pore volume is a fractal. The two point density correlation is computed for the pore space and the results compare favourably with the range reported from experiments. An array of 2-D X-ray tomography micrograph sections of a real sedimentary rock, an oolitic limestone (pure calcite) from the Mondeville formation of Middle Jurassic age (Paris Basin, France), was used to generate a 3-D bitmap. The 3-D real rock sample generated in this manner, was analysed for similar studies as the simulated structure. The results were compared with those obtained from simulation. The simulation results agree qualitatively with the real rock sample. Diffusion through the connected pore space of the simulated structure was studied using a random walk algorithm and the results compared with the similar simulation study done on the 3-D oolitic limestone specimen. In both cases diffusion was found to be anomalous indicating that the sedimentary rock has a fractal geometry. The favourable comparability of results between the simulated and real rock supports the usefulness of the model of sedimentary rock generation which can be applicable to transport phenomena.
ISSN: 0956-540X

hal-00823061
https://hal.archives-ouvertes.fr/hal-00823061
DOI : 10.1093/gji/ggs084

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Properties of composite materials depend on interatomic phenomena occurring between binder crystals. Experimental information of Atomic Force Microscopy (A.F.M.) is of prime importance; however understanding is helped by molecular modeling. As underlined in Section 1, the present study is able to simulate crystal interfaces in presence of a solution within apertures less than 1 Nanometer at a full atomic scale. Section 2 presents the case study of a gypsum solution between (120) gypsum faces, with related boundary conditions and atomic interactions. Section 3 deals with the mass equilibrium of the solution within interfaces <5 angstrom, using the original Semi Analytical Stochastic Perturbations (SASP) approach. This information becomes in Section 4 the key for explaining the peak of adhesion obtained in A.F.M. around an aperture of 3 A and gives enlightenments on gypsum cohesion. In conclusion, this illustration shows the potentialities of full atomic modeling which could not be attained by any numerical approach at a mesoscopic scale.
ISSN: 0008-8846

hal-00411868
https://hal.archives-ouvertes.fr/hal-00411868
DOI : 10.1016/j.cemconres.2007.09.022

Éditeur(s) : Pergamon-elsevier Science Ltd
Résumé : Sites of monomethylmercury (MMHg) production in Amazonian regions have been identified in hydraulic reservoirs, lake sediments and wetlands, but tailings ponds have not yet received sufficient attention for this purpose. This work evidenced high MMHg production within the water column and the interstitial water of two tailings ponds of French Guiana Au mines located; (i) in a small scale exploitation (Combat) where Hg was used for Au amalgamation, and (ii) in an industrial on-going Au mine (Yaoni) processing without Hg. The (MMHg)(D) maximum (2.5 ng L-1) occurred in the oxic water column above the sediment-water interface (SWI) of the most recent tailings pond (Combat), where the substrate was fresh, the redox transition was sharp and the pool of total Hg was large. In the Yaoni pond, the (MMHg)(D) maximum concentration (1.4 ng L-1) was located at the SWI where suboxic conditions prevailed. Using the (MMHg)(D) concentration as a proxy for Hg methylation rates, the present results show that Hg methylation may occur in various redox conditions in tailings ponds, and are favored in areas where the organic matter regeneration is more active. A 3-month long laboratory experiment was performed in oxic and anoxic boxes filled with high turbidity waters from the Combat Au mine to simulate tailings ponds. Slaked lime was added in an experimental set (2 mg L-1)and appeared to be very efficient for the reduction of suspended particulate matter (SPM) to environmentally acceptable concentrations. However, at the end of the experiment, large (MMHg)(D) concentrations were monitored under treated anoxic conditions with the (MMHg)(D) maximum located at the SWI above the Fe-reducing zones. No (MMHg)(D) was detected in oxic experiments. The use of slaked lime for SPM decantation appears to be an efficient and non-onerous process for Au miners to avoid Hg methylation in tailings ponds when it is combined with rapid drainage of the mine waters. A subsequent human intervention is however necessary for the recovery of soil structure through the cover of dried ponds with organic rich materials and reforestation to avoid the stagnation of rain waters and the occurrence of anoxia. (C) 2010 Elsevier Ltd. All rights reserved.
Applied Geochemistry (0883-2927) (Pergamon-elsevier Science Ltd), 2011-02 , Vol. 26 , N. 2 , P. 222-229

Droits : 2010 Elsevier Ltd All rights reserved.
http://archimer.ifremer.fr/doc/00030/14117/12133.pdf
DOI:10.1016/j.apgeochem.2010.11.022
http://archimer.ifremer.fr/doc/00030/14117/

Éditeur(s) : Neidine Editeurs
Résumé : This article of the number 10 of Tai Kona is the natural complement to the article appeared under the number 8, dedicated to the submarine geodiversity of the New Caledonian EEZ. The first article notably put the bases of knowledge on the history, the origins and the specificities of the geodiversity of the maritime spaces of the New Caledonian EEZ. The present article focuses on four of the major stakes which are put: 1/ the scientific ones relative to an exceptional submarine geologic context, 2 /the economic ones connected to such a favorable geologic context and to mineral resources exploitation perspectives which are no more domain of the utopia, 3/ the major environmental ones with the existence of a semi deep and deep major biodiversity and 4/ the stakes on the natural risks of a zone in the active local or regional seismicity. The conclusions of this article underline all the major challenges, in the interface of four main quoted questions, which New Caledonia must know how to raise.
Cet article du numéro 10 de Tai Kona est le complément naturel de l’article paru sous le numéro 8, dédié à la géo diversité sous-marine de la Nouvelle-Calédonie. Le premier article posait notamment les bases de connaissance sur l’histoire, les origines et les spécificités de la géo diversité des espaces maritimes de la ZEE calédonienne. Le présent article se focalise sur quatre des enjeux majeurs qui sont posés aux plans : 1/ scientifique, relatifs à un contexte géologique sous-marin exceptionnel, 2/ économique, liés à un contexte géologique favorable et à des perspectives d’exploitation de ressources qui ne sont plus du domaine de l’utopie, 3/ environnemental avec là encore un contexte totalement original et l’existence d’une biodiversité semi profonde et profonde majeure et 4/ des risques naturels d’une zone à la sismicité locale ou régionale active. Les conclusions de cet article soulignent tous les enjeux majeurs, à l’interface des quatre grands défis cités, que la Nouvelle-Calédonie doit savoir relever.
Tai Kona (2269-7535) (Neidine Editeurs), 2014-09 , N. 10 , P. 24-37

Droits : 2014 Tai Kona
http://archimer.ifremer.fr/doc/00209/32013/30443.pdf
http://archimer.ifremer.fr/doc/00209/32013/