Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
To constrain the relations between deformation and metasomatism in the subcratonic lithospheric mantle, we have analyzed the microstructures and crystal preferred orientations in 50 mantle xenoliths from the Kaapvaal craton. Water contents in olivine and pyroxenes were measured in 14 samples equilibrated at different depths. Coarse-granular microstructures recording deformation by dislocation creep followed by annealing predominate. Mylonitic (sheared) peridotites with partially or totally recrystallized microstructures are however common below 140 km. Refractory compositions predominate, but multiple metasomatic events resulted in orthopyroxene enrichment or secondary crystallization of clinopyroxene and phlogopite. Coherent orthopyroxene and olivine CPO in most coarse-grained peridotites implies in pre- to syn-kinematic orthopyroxene enrichment or epitaxial growth on primary orthopyroxene. Undeformed, interstitial orthopyroxene, clinopyroxene, and phlogopite with random orientations in coarse-grained peridotites record post-kinematic modal metasomatic events. Deformation of these phases in the sheared peridotites implies that mylonitization results from a later event, which affected locally the deep cratonic lithosphere. Olivine CPO recording dominant [100] glide predominate at all depths. Only two samples, equilibrated at ~ 3.3 GPa show olivine [001] and orthopyroxene [001] axes subparallel, suggesting dominant [001] glide. Water contents in olivine are maximum (150 wt. ppm H2O) in peridotites equilibrated at ~ 160 km depth. Peridotites equilibrated below 180 km depth are, in contrast, almost dry. Lack of correlation between olivine mg# and water content indicates that the high water contents in olivine record re-hydration after the extensive partial melting, which produced the cratonic root. The vertical variation in water contents in olivine observed in the Kaapvaal peridotites may result from hydrogen addition or loss during extraction by the kimberlites. Comparison with magnetotelluric electrical conductivity data suggests, however, that the observed vertical variation of water contents in olivine may be representative of the present-day state of the Kaapvaal mantle, implying that extensive metasomatism resulted in hydration of the cratonic mantle at intermediate depths. The annealed microstructures of Kaapvaal peridotites indicate however that this metasomatism was not followed by remobilization of the cratonic root.
ISSN: 0024-4937

hal-00750328
https://hal.archives-ouvertes.fr/hal-00750328
DOI : 10.1016/j.lithos.2012.05.001

Éditeur(s) : HAL CCSD
Résumé : The Firouzkuh Fault in most of its extension is located at the southern side of Firouzkuh Valley in west of the Central Alborz. It is a SW - NE prominent structure with a 70 km long on a sinistral -normal fault. It has been known as a south-dipping reverse fault.Paleoseismic analysis and C14 dating along the Firouzkuh left -lateral strike-slip fault indicate that Central Alborz has been shaken by large earthquakes during the Holocene. Here we present the data carried out of one of the two excavated trenches with 15 m long, 2m wide, ~ 4m deep in the east of Firouzkuh, where we found some evidence for last paleoearthquake associated to seismic re-activity on Firouzkuh Fault in the second trench (F2) that dug across a gauge zone. The last event is evidenced by cutting young superficial deposit where this faulted unit stratigrafically covered alluvium deposits yielded dated human bones fragments. The bones found in 60-70cm-deep of trench which a C14 age of 1159 ± 28 BP. Regarding to estimated slips per event on paleoseismological log of eastern wall of trench F1, event magnitudes for each paleoearthquakes are M≈7.
Geosciences Scientific Quarterly Journal

hal-00800375
https://hal.archives-ouvertes.fr/hal-00800375

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : De nombreuses études, dans des domaines variés (économie, statistiques, géographie…), s’attachent en effet à saisir les contraintes que fait peser la géographie sur la réussite économique des îles. Pour la plupart d’entre elles, l’insularité se présente comme une donnée négative qui génère une série de handicaps difficilement surmontables (exiguïté du territoire, faible peuplement, surcoûts, etc.). Cependant les perspectives de développement de ces territoires isolés en permanence par la mer, dotés de possibilités réduites en termes d’espace, de ressources naturelles ou humaines, ou de taille de marché, ne sont pas systématiquement vouées à l’échec.
Numerous studies in various fields (economics, statistics, geography, etc.), have attempted to define the constraints posed by geographic reality on the economic success of the islands. For the most part, these studies present insularity as a handicap difficult to overcome (limited territorial extent, sparse population, higher costs, etc.). Nevertheless the development prospects of these territories permanently isolated by the sea, with reduced opportunities in terms of space, natural resources or human, or market size, are not necessarily doomed to failure

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.509
http://journals.openedition.org/etudescaribeennes/509

Éditeur(s) : HAL CCSD Springer Verlag
Résumé : International audience
Chromitite pods in the Mayarí-Cristal ophiolitic massif (eastern Cuba) were formed in the Late Cretaceous when island arc tholeiites and MORB-like back-arc basin basalts reacted with residual mantle peridotites and generated chromite-rich bodies enclosed in dunite envelopes. Platinum-group minerals (PGM) in the podiform chromitites exhibit important Os-isotope heterogeneities at the kilometric, hand sample and thin section scales. 187Os/188Os calculated at the time of chromitite crystallization (~90 Ma) ranges between 0.1185 and 0.1295 (γOs = −7.1 to +1.6, relative to enstatite chondrite), and all but one PGM have subchondritic 187Os/188Os. Grains in a single hand sample have initial 187Os/188Os that spans from 0.1185 to 0.1274, and in one thin section it varies between 0.1185 and 0.1232 in two PGM included in chromite which are only several millimeters apart. As the Os budget of a single micrometric grain derives from a mantle region that was at least several m3 in size, the variable Os isotopic composition of PGM in the Mayarí-Cristal chromitites probably reflects the heterogeneity of their mantle sources on the 10-100 m scale. Our results show that this heterogeneity was not erased by pooling and mingling of individual melt batches during chromitite crystallization but was transferred to the ore deposits on mineral scale. The distribution of the Os model ages calculated for PGM shows four main peaks, at ~100, 500, 750 and 1,000 Ma. These variable Os model ages reflect the presence of different depleted domains in the oceanic (Pacific-related) upper mantle of the Greater Antilles paleo-subduction zone. The concordance between the age of crystallization of the Mayarí-Cristal chromitites and the most recent peak of the Os model age distribution in PGM supports that Os in several grains was derived from fertile domains of the upper mantle, whose bulk Os isotopic composition is best approximated by that of enstatite chondrites; on the other hand, most PGM are crystallized by melts that tapped highly refractory mantle sources.
ISSN: 0010-7999

hal-00822742
https://hal.archives-ouvertes.fr/hal-00822742
DOI : 10.1007/s00410-010-0575-2

Éditeur(s) : HAL CCSD Springer Verlag
Résumé : International audience
Investigation of an eclogite xenolith, discovered in a Cretaceous granite from the Central Domain of the Dabieshan massif in eastern China, yields new petrological insights into the high to ultrahigh-pressure metamorphism, experienced by the Qinling-Dabie orogen. Prior to inclusion as a xenolith in the granite during the Early Cretaceous, this eclogite xenolith had recorded a complex metamorphic evolution that complies with subduction and exhumation processes experienced by the continental crust of the South China Block. Well-preserved mineral parageneses substantiate the prograde and retrograde stages revealed by inclusions in porphyroblastic garnet and zoned minerals such as garnet, comphacite and amphibole in the matrix. The relatively low P/T re-equilibration during a latemetamorphic stage was textually inferred by the presence of aluminous and calcic-subcalcic amphiboles such as katophorite, edenite, taramite and pargasite as main matrix phases. According to our U/Pb, Rb/Sr and new 40Ar/39Ar geochronological results, namely 109 ± 1 and 112 ± 2 Ma plateau ages for muscovite and amphiboles, respectively, two successive but distinct cooling stages account for the thermal history of the granite–migmatite gneiss dome that forms the Central Dabieshan Domain. We argue that prior to the Cretaceous doming, the Central Dabieshan Domain experienced a tectono-metamorphic evolution similar to that observed in the high-pressure to ultra high-pressure units developed in the Southern Dabieshan Domain and Hong'an massif.
ISSN: 1437-3254

hal-00104224
https://hal-insu.archives-ouvertes.fr/hal-00104224
https://hal-insu.archives-ouvertes.fr/hal-00104224/document
https://hal-insu.archives-ouvertes.fr/hal-00104224/file/Lin-IntJEarthSciences-2007.pdf
DOI : 10.1007/s00531-006-0129-z

Éditeur(s) : HAL CCSD Springer Verlag
Résumé : International audience
North Tanzanian Divergence is the first stage of continental break-up of East African Rift (<6 Ma) and is one of the most concentrated areas of carbonatite magmatism on Earth, with singular Oldoinyo Lengai and Kerimasi volcanoes. Hanang volcano is the southernmost volcano in the North Tanzanian Divergence and the earliest stage of rift initiation. Hanang volcano erupted silica-undersaturated alkaline lavas with zoned clinopyroxene, nepheline, andradite-schorlomite, titanite, apatite, and pyrrhotite. Lavas are low MgO-nephelinite with low Mg# and high silica content (Mg# = 22.4–35.2, SiO2 = 44.2–46.7 wt%, respectively), high incompatible element concentrations (e.g. REE, Ba, Sr) and display Nb–Ta fractionation (Nb/Ta = 36–61). Major elements of whole rock are consistent with magmatic differentiation by fractional crystallization from a parental melt with melilititic composition. Although fractional crystallization occurred at 9–12 km and can be considered as an important process leading to nephelinite magma, the complex zonation of cpx (e.g. abrupt change of Mg#, Nb/Ta, and H2O) and trace element patterns of nephelinites recorded magmatic differentiation involving open system with carbonate–silicate immiscibility and primary melilititic melt replenishment. The low water content of clinopyroxene (3–25 ppm wt. H2O) indicates that at least 0.3 wt% H2O was present at depth during carbonate-rich nephelinite crystallization at 340–640 MPa and 1050–1100 °C. Mg-poor nephelinites from Hanang represent an early stage of the evolution path towards carbonatitic magmatism as observed in Oldoinyo Lengai. Paragenesis and geochemistry of Hanang nephelinites require the presence of CO2-rich melilititic liquid in the southern part of North Tanzanian Divergence and carbonate-rich melt percolations after deep partial melting of CO2-rich oxidized mantle source.
ISSN: 0010-7999

hal-01467390
https://hal.archives-ouvertes.fr/hal-01467390
DOI : 10.1007/s00410-016-1273-5

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Cette étude s’attache à rendre compte des difficultés auxquelles l’île de La Réunion est confrontée de longue date et qui ne trouvent, jusqu’à présent, aucune issue satisfaisante en termes de développement. De crises en conflits, récurrents dans leurs formes comme dans leurs schémas spatiaux, La Réunion demeure enfermée dans des impasses multiples, économiques et sociétales. Aucune issue réelle ne se dessine : la confusion des responsabilités perdure et permet à des schémas éculés, présentés comme des innovations, de se reproduire sans fin.
This study aims to realize the difficulties that the island of Reunion is facing a long time and without satisfactory outcome in terms of development. Crises to conflicts, recurring forms, as in their spatial patterns, Reunion remains locked in an impasse multiple, economic and societal. No actual outcome does is emerging: the responsibilities confusion continues and allows worn patterns, presented as innovations, reproduced endlessly.
Réunion

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.4930
http://journals.openedition.org/etudescaribeennes/4930

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The main political concern in the southern areas of Madagascar is poverty alleviation. To alleviate poverty in the area, the government has chosen to enforce adjustment policies of the World Bank Group. According to the World Bank Group's argument, while artisanal mining is supposed to create significant economic, social and environmental problems, large-scale mining investment results in economic and social prosperity. This paper focuses principally on a re-analysis of the debates regarding the relationship between artisanal and large-scale mining and poverty alleviation in developing countries. Further, the paper offers an alternative viewpoint on these issues based on the example of Madagascar. In the last decade, Madagascar has experienced a significant increase in mining activity. Towards the end of the 90s, informal and artisanal mining emerged as one of the most important economic activities of the area with the development of the Ilakaka frontier. At the same time, foreign investments began to benefit from adjustment policies implemented by the government, and large-scale mining operations also commenced. As the local socio-economic system was deeply affected by these developments, it is wise to monitor the effects of each type of mining operation on poverty alleviation. On the one hand, it appears that governance insufficiency has hampered possibilities for broader economic prosperity through large-scale mining investments. On the other hand, while artisanal mining is frequently condemned by scholars, the negative comments seem to be overly pessimistic, as this activity can be demonstrated to provide considerable economic opportunities for both the native and migrant populations.
ISSN: 0264-8377

hal-01303896
https://hal-univ-perp.archives-ouvertes.fr/hal-01303896
DOI : 10.1016/j.landusepol.2013.08.001

Éditeur(s) : HAL CCSD
Résumé : Subduction is one of the major geodynamical process active during the Earth evolution. The characterization of arc magmas, their evolution through space and time, and the relationship between arc magmatism and continental crust forming processes, constitute the main research topics in petrology and geochemistry since the last three decades. This study focuses on an exhumed portion of the Kohistan Arc (N Pakistan), which is an exceptional ‘in situ' laboratory to study and follow through time the processes active on subduction zones. Based on a pluri-geochemical approach, this study allows unraveling two major issues : 1/ The lack of a cogenetic relationship between the arc root (i.e. ultramafic rocks) and the overlying gabbroic crustal section. The Jijal ultramafic section does not bear a crustal origin and was emplaced at ~117 Ma via a magma-rock reaction between REE-depleted ‘boninite-like' melts and the pre-existing lithospheric mantle with Indian-MORB affinities; 2/ A three-stage geodynamical model covering the arc evolution through ~30 Ma. This model starts with the onset of the subduction followed by the building of the volcanic arc (1st stage). The 2nd stage corresponds to a major thermal event, characterized by abundant magma underplating and by granulitisation of the arc base. Recycling of the residual/cumulative lower crust into the convective asthenospheric mantle was efficient during this stage, and probably related to thermo-mechanical erosion processes. The last stage, between ~95 and 85 Ma, seals the end of the intra-oceanic subduction and corresponds to an “amagmatic” period. This step is followed by a voluminous, but short, magmatic pulse at ~85 Ma, occurring just before the arc-continent collision. At last, this study emphasizes the more mafic composition of the investigated crustal arc section when compared to the bulk continental crust. Nevertheless the arc section composition nicely fits with the lower continental crust average.
Les zones de subduction représentent des zones d'évolution clés dans la compréhension des processus géologiques majeurs actifs sur notre planète. En particulier, la caractérisation et l'évolution des magmas générés dans les zones d'arcs océaniques et la relation entre leur genèse et les processus de croissance crustale sont des axes primordiaux. Cette étude est focalisée sur la portion d'arc océanique exhumée du Kohistan (Nord Pakistan) qui constitue un laboratoire exceptionnel pour appréhender cette problématique. Basée sur une approche géochimique multi-méthodes (éléments majeurs et en trace, isotopes), cette étude a permis d'établir : 1/ l'absence de relation génétique directe entre les roches ultrabasiques de la racine de l'arc et la section crustale sus-jacente. La formation de la séquence ultrabasique de Jijal se produit à ~117 Ma via une réaction de type magma-roche entre des liquides de type boninitique (appauvris en terres rares), et le manteau lithosphérique de type MORB-Indien ; 2/ un modèle géodynamique en trois stades majeurs résumant l'évolution de l'arc océanique et de la subduction sur une période d'environ 30 Ma. Ce modèle débute par l'initiation de la subduction et la formation de l'arc volcanique s.s. (1er stade) ; le 2ème stade correspond à un évènement thermique majeur. Il est représenté par un sous-placage important de magmas et une granulitisation intense de la base de l'arc. Le recyclage de la croûte inférieure cumulative et résiduelle, dans le manteau sous-jacent, se produit durant cette étape vraisemblablement suite à des processus d'érosion thermo-mécanique. Le dernier stade, entre 95 Ma et 85 Ma, scelle la fin du fonctionnement de la zone de subduction et correspond à une période amagmatique suivie par une brève reprise du magmatisme avant la collision de l'arc après 85 Ma. Enfin, une modélisation numérique comparative avec la croûte continentale globale met en évidence la composition significativement plus basique de la croûte de l'arc insulaire du Kohistan. De fortes similitudes sont en revanche observées entre la section d'arc étudiée et la croûte continentale inférieure.
https://tel.archives-ouvertes.fr/tel-00437770

tel-00437770
https://tel.archives-ouvertes.fr/tel-00437770
https://tel.archives-ouvertes.fr/tel-00437770/document
https://tel.archives-ouvertes.fr/tel-00437770/file/thesedhuime.pdf

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Se analiza críticamente al lujo como «concepto» para comprenderlo dentro de la ontologización del sujeto que lo consume y lo ostenta en la actualidad. Estas dos categorías (consumo y ostentación) permiten distinguir al sujeto en dos sentidos: primero, como alguien que busca satisfacer necesidades creadas a partir de relacionar el consumo con la estetización tanto del sujeto como del mundo que lo rodea (el objeto desde un sentido estetizante); segundo, como alguien para quien el lujo es motivo justificante de relación y de des-relación con los otros. Esto a partir de analizar su forma de «hablar» ambivalente (bidireccional): el lujo dice, pero también calla; sugiere, pero no deja de imponer; abre y cierra constantemente; limita y extiende a la vez; en fin, su manera bivalente de comprender la realidad hace que sea más que una simple forma de estar en el mundo. Lo anterior nos permite explicar el por qué de la dicotomía del lujo: para algunos resulta innecesario o superfluo; para otros, en cambio, el lujo es una forma constante de afirmarse como constructo imaginario. De esto se desprende un análisis del lujo como «objeto» y como «idea de objeto»; viendo, así, la forma en que se vuelve base movible de una estetización de comportamientos ambivalentes. En otras palabras, se trata de mirar al lujo pero sin dejar de mirar al sujeto que vive «en» y «desde el lujo».
Analysed critically to the luxury as a “concept” to understand it within the ontologising of the subject that consume it and currently holds it. These two categories (consumption and ostentation) distinguish the subject in two ways: first, as someone who seeks to meet needs created from relate consumption to the aestheticisation of both the subject and the world that surrounds it (the object from a sense aestheticizing); second, as someone for whom luxury is supporting reason of relationship and des-relacion with each other. This starting to analyze his form of “speak” ambivalent (bi-directional): luxury says, but also silent; it suggests, but it doesn't impose; opens and closes constantly; limits and extends at a time; in the end, his bivalent way of understanding reality makes it more than a simple way of being in the world. This allows us to explain the reason for the dichotomy of luxury: for some it is unnecessary or superfluous; for others, on the other hand, the luxury is a constant form of asserting itself as imaginary construct. That is clear from an analysis of the luxury as «object» and «idea of object»; watching, well, how that becomes an aestheticisation of ambivalent behaviour movable base. In other words, it is the luxury look but stop looking at the subject who lives «in» and «luxury».
L’analyse critique du luxe comme « concept » pour comprendre le luxe dans l'ontologisation du sujet qui le consomme et l’occupe actuellement. Les deux catégories (consommation et ostentation) distinguent le rapport à l'objet de deux façons : tout d'abord, comme quelqu'un qui cherche à répondre aux besoins créés dans une relation de consommation et d’esthétisation à la fois du sujet en lui-même et du sujet dans son rapport au monde (l'objet d'une esthétisation de sens) ; deuxièmement, comme quelqu'un pour qui le luxe soutient la construction des relations et non-relations avec les autres. Cela commence dans l’analyser sa forme de « parle » ambivalent (bidirectionnel) : ce que le luxe dit mais aussi les silencieux ; il suggère, mais il n'impose pas ; ouvertures et fermetures ; limites et extensions ; et finalement, son mode bivalent de compréhension de la réalité qui est plus qu'une simple manière d'être au monde. Ceci nous permet d'expliquer les raisons de la dichotomie de luxe : pour certains c'est inutile ou superflu ; pour d'autres, le luxe est une forme constante d'affirmation de soi-même comme construction imaginaire. Il ressort de cette analyse le luxe en tant "objet" et "idée de l'objet"; observant l'observation comment il devient une esthétisation d’un comportement ambivalent évolutif. Autrement dit, il s’agit d’étudier le luxe, mais sans négliger le sujet qui vit dans et à travers le luxe.

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.7315
http://journals.openedition.org/etudescaribeennes/7315

Éditeur(s) : HAL CCSD Société géologique de France
Résumé : International audience
New geodynamical data from West Africa bring consistent informations on the pre-Mesozoic reconstruction within a large area running from the western Sahara to the Colombian cordillera. These new data support a Neoproterozoic Ocean (WANO) between the Amazonian (AMC) and West African (WAC) cratons previously to the Iapetus and Rheic oceans. We delineate 31 blocs detached from the surrounding three continents: NAC (North American Craton), AMC and WAC. 7 came from the WAC margin, 7 from the NAC, 6 from the AMC and 11 from an intermediate volcano sedimentary domain (COB) built on a 1200-1000 Ma oceanic crust. These imbricated blocks formed a tight mosaic by the Hercynian/Alleghanian tectonic event which gave way to the Pangea super-continent. But, during the Atlantic Ocean opening these blocks began to move. They were separated by new oceanic basins. However, previously to the Pangea, blocks from the COB domain formed two sets of garlands located on the northwestern Gondwana margin. The northern one moved to the North until the Silurian to collide the NAC (Taconic tectonic event) meanwhile the southern one remains on the Gondwana margin. All together were gathered by the Carboniferous/Permian time. Then, the framework for the opening of the Atlantic Ocean was not totally disconnected from the "Variscan" collage and many variscan weakness zones were re-used as initial breaking zones. Beyond this tectonic impact, the pre-mesozoic assemblage allows us to compare this "Caribbean" island arc with another one: the Indonesian "Banda" arc. Thus, West Africa is a geological key area for correlations between the Caribbean, the Appalachian, the Brazilian "Nordeste" and the West European domains and for the understanding of the Atlantic Ocean opening process.
EISSN: 1777-5817

hal-00842747
https://hal.archives-ouvertes.fr/hal-00842747
DOI : 10.2113/gssgfbull.184.1-2.5

Éditeur(s) : HAL CCSD American Geophysical Union
Résumé : International audience
We examine absolute gravity (AG) and vertical Global Positioning System (GPS) time series between 1995 and 2010 at eight collocated sites in mid-continent North America. The comparison of AG and GPS rates aligned to ITRF2005 yields a gravity/uplift ratio of -0.17 +/- 0.01 mu Gal mm(-1) (1 mu Gal = 10 nm s(-2)) and an intercept of -0.1 +/- 0.5 mm yr(-1). In contrast, aligning the GPS velocities to ITRF2000 results in a gravity/uplift intercept of -1.3 +/- 0.5 mm yr(-1). The near-zero gravity/uplift offset for the ITRF2005 (or ITRF2008) results shows a good alignment of the GPS vertical velocities to Earth's center of mass, and confirms that GPS velocities in this reference frame can be compared to predictions of geodynamic processes such as glacial isostatic adjustment (GIA) or sea-level rise. The observed gravity/uplift ratio is consistent with GIA model predictions. The ratio remains constant in regions of fast and slow uplift, indicating that GIA is the primary driving process and that additional processes such as local hydrology have a limited impact on a decadal time-scale. Combining AG and GPS measurements can provide significant constraints for geodetic, geodynamic, and hydrological studies. Citation: Mazzotti, S., A. Lambert, J. Henton, T. S. James, and N. Courtier (2011), Absolute gravity calibration of GPS velocities and glacial isostatic adjustment in mid-continent North America, Geophys. Res. Lett., 38, L24311, doi:10.1029/2011GL049846.
ISSN: 0094-8276

hal-00689010
https://hal.archives-ouvertes.fr/hal-00689010
DOI : 10.1029/2011GL049846

Éditeur(s) : HAL CCSD Armand Colin
Résumé : International audience
Located in the heart of the Maritimes in Southeast New Brunswick, Moncton has the highest concentration of Acadians in any urban setting in Canada. Over the years, Acadians have increasingly become part of the New Brunswick society. They have greatly contributed to Moncton's development through the creation of genuine Acadian institutions in the educational and financial sectors, which, as a result, have modified the spatio-linguistic configuration and the cultural identity of the place. This new reality has been the object of a series of spatiotemporal analyses using the Geographic Information System (GIS); they show that the dynamics of the Francophone and Anglophone populations in the agglomeration's different sectors lead to the creation of some isolated linguistic groupings. And that unlike the situation in other regions of New Brunswick, the assimilation process of the French-speaking Acadians into the Anglophone majority has slowed down in the Greater Moncton over the course of thelast few years. These transformations point out to the crucial role of the Universite de Moncton as an educational, cultural and even political nexus for the Acadians in the Greater Moncton, as well as in the Maritime provinces in general.
Située au cœur des Maritimes, dans le sud-est du Nouveau-Brunswick, l'agglomération du Grand Moncton est la région urbaine canadienne qui présente la plus forte concentration d'Acadiens français. Au fil des années, ces derniers furent plus présents dans la société néo-brunswickoise contribuant grandement au développement de Moncton à travers la création d'institutions acadiennes dans le domaine de l'éducation et des services financiers. Les transformations dues à l'émergence d'une influence acadienne modifient la configuration géographique et l'identité culturelle de l'espace en question. Cette réalité apparente fait l'objet d'une série d'analyses spatio-temporelles à l'aide des Systèmes d'Information Géographique (SIG); ces analyses montrent d'abord que la dynamique des populations francophone et anglophone a tendance à créer certains îlots linguistiques tandis que ralentit le processus généralisé d'assimilation des Acadiens à la majorité anglophone dans l'agglomération du Grand Moncton. Ces transformations mettent en évidence le rôle de l'Université de Moncton comme centre d'attraction éducationnel, culturel et même politique pour les Acadiens de Moncton en particulier et des Provinces maritimes en général.
ISSN: 0003-4010

hal-01413577
https://hal.univ-antilles.fr/hal-01413577
https://hal.univ-antilles.fr/hal-01413577/document
https://hal.univ-antilles.fr/hal-01413577/file/2002%20Transformation%20marquante.pdf
DOI : 10.3406/geo.2002.1659

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : En Indonésie orientale, entre l’île de Sumbawa et celle de Florès, se trouve le parc national de Komodo, du nom de la principale île habitée par les fameux varans, un superbe espace naturel désormais préservé par l’UNESCO et entouré de récifs coralliens. Quelques familles de pêcheurs, la plupart musulmans, peuplent ce petit archipel aujourd’hui prisé par les touristes internationaux pour ses dragons et ses lagons. En réalité, les varans géants de Komodo ne sont pas les derniers témoins de la préhistoire, mais d’énormes lézards, impressionnants, très photogéniques et parfois dangereux.Un endroit idéal pour s’adonner à une forme singulière de tourisme d’aventure, même s’il est aujourd’hui plus de masse que de niche. Entre une plage balnéaire et une balade en mini croisière, quelques dizaines de milliers de touristes annuels viennent approcher ces drôles de dragons qui effraient autant qu’ils fascinent les visiteurs. Aussi, promeneurs, baigneurs et excursionnistes se croisent — le temps d’un frisson bien encadré, il est vrai dans un décor de rêve — dans ce parc national, tous animés par les mêmes volontés et curiosité de « voir pour de vrai » cette créature étrange qui stimule notre imaginaire rempli de dinosaures.
In eastern Indonesia, between the island of Sumbawa and Flores that, is the Komodo National Park, named after the main island where the famous lizards are found, a beautiful natural area now protected by UNESCO and surrounded by reefs coral. Some families of fishermen, most Muslims inhabit this small archipelago prized today by international tourists for its dragons and lagoons. In reality, the giant Komodo dragons are the last witnesses of prehistory but huge lizards, impressive, photogenic and sometimes dangerous.An ideal place to indulge in a singular form of adventure tourism, although it is now more mass than niche. Between a seaside beach and a leisurely mini cruise, tens of thousands of annual tourists come to approach these funny dragons that scare as they fascinate visitors. Also, walkers, swimmers and hikers cross - time for a well supported thrill, it is true in a dream setting - in this national park, all driven by the same desire and curiosity to "see for real" this creature strange that stimulates our imagination filled with dinosaurs.
Indonésie
Komodo
Bali

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.7577
http://journals.openedition.org/etudescaribeennes/7577

Éditeur(s) : HAL CCSD
Résumé : Diffusion du document : INRA Documentation de Centre, Domaine de Duclos, 97170 Petitt-Bourg (Guadeloupe, France) Diplôme : DEA
il s'agit d'un type de produit dont les métadonnées ne correspondent pas aux métadonnées attendues dans les autres types de produit : DISSERTATION
Because soil respiration representes 80% of ecosystem respiration, it is a major flux between biosphere and atmosphere. We examined the effects of root and litter exclusion on soil CO! efflux (Rsu1) using trenching and litter exclusion in a tropical plantation constituted of trees seedlings installed in 16 mono-specific stands 20 years ago near Kourou, French Guyana. Soil CO2 efflux was measured using an infra red gas analyser (PP System,EGM4 ) at 16 randomly distributed plot in each treatment: control, root exclusion, litter exclusion and both root and litter exclusion. in the plantation. We measured R'1l1during four periods, and we have collected soil samples, litter biomass and measured moisture at 5 cm depth in the soil. Soil CO, efflux varied significantly among species from 2,8±O,7f1mo l. m''. s' (mean ± standard deviation) to 7.4± 1.7fLmol. n'-' . s ' for Qualea rosea and Vochys ia tomentosa, respectively. 1'0 significant correlation was found between RSIlI variability and soil moisture, which is mostly related to soil texture in the experimental site. Soil CO2 efflux was significantly reduced in litter exclusion treatment and root exclusion plots (6 months litter and/or root exclusion) during ail measurements period and for ail species, compared to control plots. The reduction of soil CO, efflux was higher in plot without root than in plot without litter of control plot (42% and 25%, respectively). There was an import ant specific diversity in these reductions . We estimated the contribution of roof respiration (Rr) to total Rso1 by calculating the difference between Rso1 control and Rsn l root exclusion plot corrected for the decomposition of root that were killed following t re n e h in ~. Thus the heterotrophic component of soil carbon efflux accounts for 46% of total carbon efflux (1,9f1 mol. rn" . s•') while root respiration accounts for 54% of soil carbon release (2,3 ~t mo l. m-2 S-I) . Because there was a negative and significant correlation between microbial respiration (Rrn) and C/N of mature leaves it seemed to be possible to predict Rm if we known the mature leaves quality. In addition a good estimate theorical R ~, values from R~, measured in different treatments.
La respiration du sol en représentant une part de 80% de la respiration de l'écosystème apparaît être un flux majeur entre la biosphère et l'atmosphère. Nous avons étudié les effets de l'exclusion racinaire et de la litière sur le flux de CO, du sol (R ~ , ) en utilisant la méthode de " Trench-plots" et de suppression de litière dans une plantation d'arbres tropicaux. Ces arbres, âgés de 20 ans ont été plantés sur un sol uniforme, près de Kourou en Guyane française, en 16 placeaux mono-spécifiques. Pour mesurer les flux de CO2 provenant du sol, nous avons utilisé un analyseur différentiel de gaz infrarouge portable muni d'une chambre. Les mesures ont été faites sur 4 traitements différents tels que : le contrôle, l'exclusion racinaire, l'exclusion de litière et l'exclusion de litière et de racine et ce, répétés sur chacune des 16 placettes mono-spécifiques. Cette étude comporte 4 campagnes de mesures. Nous avons également effectué des prélèvements de sol de litière et nous avons fait des mesures d’humidité de sol à une profondeur de 5 cm. Les flux de C01 du sol varient fortement entre espèces de 2.8±O.7 ~t m o 1. m-2. sol à 7 A± 1. 7 ~t m o l. m•1 sol pour Qua/ev rosea ct Vochysto tomentasa, respectivement. Il n'existe pas de corrélation significative entre les variations de Rw l ct celles de l'humidité du sol (indication sur la texture du sol de la plantation ). Nous avons observé que Rso1 était significativement plus faible dans les placeaux sans racines et/ou sans litière (6 mois après la mise en place de l'expérimentation) pour toutes les campagnes de mesures et pour toutes les espèces que dans les placeaux contrôlés. Cette réduction du flux de CO2 du sol est plus forte dans les "trench-plots " que dans les traitement s d'exclusion de litière avec 42 et 25% respectivement. Un effet "traitement " et un effet "espèce" important expliquent 3 1"/.. ct 13% de la variabilité totale de R~. Nous avons cherché à connaître la contribution des racines dans les valeurs de R""I. en comparant le flux de CO2 provenant du sol sur des "trench -plot s'' au flux de COl provenant du sol dans les placeaux contrôlés . Cette estimation a été corrigée pour prendre en compte la décomposition des racines tuées par les tranchées. Ainsi, la composante appartenant aux micro -organismes représente 46% du flux total de carbone provenant du sol (1.9Jlmo l. m-2 S•I ) alors que la respiration des racines représente 54% du dégagement de carbone (2 ,3~lmol. m ol . 5-La respiration des micro-organismes pourrait être estimée en mesurant le C/N des feuilles matures puisqu'il existe une corrélation significative et négative entre les deux. Enfin les résultats obtenus sur les différents traitements permettent d'obtenir une bonne estimation de la respiration du sol avec un RSIlI théorique corrélé à 66% avec les valeurs réelles mesurées.
https://hal.archives-ouvertes.fr/hal-01189239

hal-01189239
https://hal.archives-ouvertes.fr/hal-01189239
PRODINRA : 18212

Éditeur(s) : HAL CCSD Société Géologique de France
Résumé : Xenoliths brought up by kimberlite magmas are rare samples of otherwise inaccessible lithospheric mantle. Eclogite xenoliths are found in most cratons and commonly show a range of mineral and chemical compositions that can be used to better understand craton formation. This study focuses on five new kyanite-bearing eclogites from the Udachnaya kimberlite pipe (367±5 Ma). They are fine-to coarse-grained and consist mainly of “cloudy” clinopyroxene (cpx) and garnet (grt). The clinopyroxene is Al,Na-rich omphacite while the garnet is Ca-rich, by contrast to typical bi-mineral (cpx+grt) eclogites that contain Fe- and Mg-rich garnets. The Udachnaya kyanite eclogites are similar in modal and major element composition to those from other cratons (Dharwar, Kaapvaal, Slave, West African). The kyanite eclogites have lower REE concentrations than bi-mineral eclogites and typically contain omphacites with positive Eu and Sr anomalies, i.e. a “ghost plagioclase signature”. Because such a signature can only be preserved in nonmetasomatised samples, we infer that they were present in the protoliths of the eclogites. It follows that subducted oceanic crust is present at the base of the Siberian craton. Similar compositions and textures are also seen in kyanite eclogites from other cratons, which we view as evidence for an Archean, subduction-like formation mechanism related to craton accretion. Thus, contrary to previous work that classifies all kyanite eclogites as type I (IK), metasomatized by carbonatite/kimberlitic fluids, we argue that some of them, both from this work and those from other cratons, belong to the non-metasomatized type II (IIB). The pristine type IIB is the nearest in composition to protoliths of mantle eclogites because it contains no metasomatic enrichments.
ISSN: 0037-9409

hal-01622617
https://hal.archives-ouvertes.fr/hal-01622617
DOI : 10.1051/bsgf/2017008

Éditeur(s) : HAL CCSD
Résumé : HYDRO
The objective of this study was to examine the water relations and hydraulic architecture and vulnerability to cavitation in Virola surinamensis and V. michelii and to compare to similar measurements in Eperua falcata. In several previous reports Virola was seen to have a rather narrow range of xylem pressure potentials ( Yx) near zero in the course of a wet-season day while having water fluxes quite close to Eperua. We tested the hypothesis that the narrow range of Yx might be consistent with very high hydraulic conductivities of stems, roots and shoots and high vulnerability to cavitation in Virola compared to Eperua. When this hypothesis proved false we concluded that the previous determinations of Y x might be wrong in Virola due to latex. We re-examined the determination of Yx in Virola by the pressure chamber technique and compared results to determination of Yleaf by the thermocouple psychrometer technique and found that the likely range of Yx are more negative than previously reported. Problems concerning the determination of Yx in species with latex are discussed.
Journal of Sigmoidal Plant Hydraulics

hal-01032396
https://hal.archives-ouvertes.fr/hal-01032396

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Secondary migration is defined as the movement of hydrocarbons through relatively permeable rocks from source to trap: a two-phase flow within a porous medium. Depending on the geometry and capillary pressure distributions of carrier beds, secondary migration has both vertical and lateral components. The present paper focuses on that part of the migration where the movement is mainly vertical. Its objective is to propose a description of the dynamics governing the vertical part of secondary migration based on the main physical aspects of two-phase flow in a homogeneous porous medium. The study is illustrated by laboratory observations performed in a vertical, 2-D Hele-Shaw cell filled with a transparent porous medium where the flow of dyed oil invading a wetting fluid is visually observed. These observations help us to understand the effect of buoyant, capillary and viscous forces on the resulting flow, the relative importance of which is characterized by non-dimensional numbers. Extrapolating these observations to natural media, it is proposed that vertical secondary migration can be described as a percolation of disconnected and vertically-elongated stringers. These stringers do not move continuously but as a succession of snap-off and re-feeding events which result in a jerky upward movement. Using parameters characterizing the physical properties of the fluid and of the porous medium, the geometry and the dynamic behavior of the stringers are estimated. The width of stringers occurring during secondary migration in geological media is centimetric and their vertical size ranges from several centimeters to a few meters. An upper limit of the mean upward velocity of stringers is proposed, as well as an estimate of their spatial density and of the minimum, average horizontal distance (decametric) between two stringers. The stringers are sparsely distributed, resulting in a low average oil loss and a high efficiency of the vertical migration process.
ISSN: 0264-8172

hal-00831370
https://hal.archives-ouvertes.fr/hal-00831370
https://hal.archives-ouvertes.fr/hal-00831370/document
https://hal.archives-ouvertes.fr/hal-00831370/file/pekins-V-edited.pdf
DOI : 10.1016/j.marpetgeo.2013.04.020

Éditeur(s) : HAL CCSD Wiley
Résumé :  
The complex structure of tree bark reflects its many functions, which include structural support as well as defence against fire, pests and pathogens. Thick bark, however, might limit respiration by the living tissues of the trunk. Nevertheless, little research has addressed community-level variation in bark thickness, and to the best of our knowledge, no one has tested multiple hypotheses to explain variation in bark thickness. We conducted an extensive survey of bark thickness within and among species of trees in the tropical rain forests of French Guiana. Trunk bark thickness increased by 1.2 mm per 10 cm increase in stem diameter, and varied widely at all taxonomic levels. Mean trunk bark thickness was 4.5 mm (range: 0.5-29 mm), which was less that found in two Amazonian rain forests in previous studies. This survey of bark thickness should be of use for forest management since tree survival through fire is strongly predicted by bark thickness. We combined the survey data with multiple datasets to test several functional hypotheses proposed to explain variation in bark thickness. We found bark to provide an average of 10% of the flexural rigidity of tree stems, which was substantially less than that found in the only other study of bark stiffness. Bark thickness was uncorrelated with species' association with fire-prone habitats, suggesting that the influence of fire on bark thickness does not extend into moist Forests. There was also little evidence that bark thickness is affected by its function as a defence against herbivory. Nor was there evidence that thick bark limits trunk respiration. A re-analysis of previously collected anatomical data indicated that variation in rhytidome (non-conducting outer bark) thickness explains much of the variation in overall bark thickness. As rhytidome is primarily involved in protecting the living tissues of the trunk, we suggest that bark thickness is driven mostly by its defensive function. Functional explanations for the variation in bark thickness were not clear-cut. Nevertheless, this study provides a foundation for further investigation of the functional bases of bark in tropical trees.
ISSN: 0269-8463

hal-01032124
https://hal.archives-ouvertes.fr/hal-01032124
DOI : 10.1111/j.1365-2435.2010.01736.x

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Les îles ont longtemps été étudiées comme de simples lieux périphériques, inscrits dans le prolongement de logiques continentales ; des espaces dépourvus de sens en dehors du prisme des puissances métropolitaines. A travers le champ des études insulaires, il s’agit désormais de croiser les différentes expériences insulaires, de poser les contextes de développement et d’étudier les configurations et les temporalités spécifiques des îles. Étudier les îles nécessite de prendre la mesure de ces territoires -loin de toute vision monolithique-, d’analyser leur espace au regard des réalités sociale et politique, de cerner leur poids économique et leur contexte de développement, des héritages de l’histoire à la prise en compte de leur voisinage géographique. Il s’agit de prendre en considération les logiques exogènes qui font l’île et d’interroger les dynamiques internes.Le sujet d’étude est l’île, l’objet «île », l’île dans la gestion de son espace, la définition de son projet territorial, le positionnement de l’île dans son environnement respectif et les opportunités et stratégies dans l’économie mondialisée. La richesse des enseignements des territoires et des sociétés insulaires débordent le simple cadre spatial de l’île qui peut être entendue comme une synecdoque, un microcosme commode et raisonnable du continent.
Islands were studied for a long time as simple peripheral territories, territories which flesh out the seamless continuation of continental logic, meaningless territories without the prism and perspective of metropolitan power. Through the field of the island studies, critical questions cross various island experiences and their context of development and their configurations; or otherwise study specific temporalities, connectivities and materialities, in the context of globalization. To study islands requires taking the measure of these territories, far from any monolithic vision, to analyze their space with regard to their social and political realities, to identify their economic clout and their context of development and the legacies of the history, in consideration of their geographical neighbourhood. It is a question of considering the exogenous logics which make the island and interrogate its internal dynamics.The subject of study is the island, "island" as object, the island in the management of its space, the definition of its territorial project, the positioning of the island in its environmental perspective and the opportunities it enjoys and the strategies it deploys in the globalized economy. The wealth of scholarship of and about islands and island societies extends beyond the simple spatial frame of the island; ‘the Island’ can be understood as a synecdoche, a convenient, manageable and reasonable microcosm of the continent.

Droits : info:eu-repo/semantics/openAccess
http://journals.openedition.org/etudescaribeennes/7272