96 documents satisfont la requête.
Tourism planning in small tropical islands: methodological considerations and development issues in Samoa
Auteur(s) : Pearce, Douglas G.
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Investigating trophic-level variability in Celtic Sea fish predators
Auteur(s) : Chassot, E Rouyer, Tristan Trenkel, Verena Gascuel, D
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Spatial variability of soil microbial functioning in a tropical rainforest of French Guiana using nested sampling
Auteur(s) : Fromin, Nathalie Saby, Nicolas Lensi, Robert Brunet, Didier Porte, Benjamin Domenach, Anne-Marie ROGGY, Jean-Christophe
Auteurs secondaires : Centre d’Ecologie Fonctionnelle et Evolutive (CEFE) ; Institut de Recherche pour le Développement (IRD [France-Sud]) - Centre National de la Recherche Scientifique (CNRS) - Université de Montpellier (UM) - Institut national de la recherche agronomique [Montpellier] (INRA Montpellier) - École pratique des hautes études (EPHE) - Centre international d'études supérieures en sciences agronomiques (Montpellier SupAgro) - Université Paul-Valéry - Montpellier 3 (UM3) - Institut national d’études supérieures agronomiques de Montpellier (Montpellier SupAgro) Unité INFOSOL ; Institut National de Recherche Agronomique Ecologie fonctionnelle et biogéochimie des sols et des agro-écosystèmes (Eco&Sols) ; Centre international d'études supérieures en sciences agronomiques (Montpellier SupAgro) - Institut National de la Recherche Agronomique (INRA) - Institut de Recherche pour le Développement (IRD) - Centre de Coopération Internationale en Recherche Agronomique pour le Développement (CIRAD) - Institut national d’études supérieures agronomiques de Montpellier (Montpellier SupAgro) Ecologie des forêts de Guyane (ECOFOG) ; Centre de Coopération Internationale en Recherche Agronomique pour le Développement (CIRAD) - Institut National de la Recherche Agronomique (INRA) - Université des Antilles et de la Guyane (UAG) - AgroParisTech - Centre National de la Recherche Scientifique (CNRS) ACI/Ecosphere Continentale; Fonctionnement et Dynamique de la Biosphere Continentale: Processus; Echanges de Matieres et d'Energie; Modelisation (Centre National de la Recherche Scientifique, France) program DIPROTROFLUX
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Proceedings of the 1st International Workshop on Semantics for Biodiversity
Auteur(s) : Larmande, Pierre Arnaud, Elizabeth Mougenot, Isabelle Jonquet, Clement Libourel, Thérèse Ruiz, Manuel
Auteurs secondaires : Diversité, adaptation, développement des plantes (DIADE) ; Université Montpellier 2 - Sciences et Techniques (UM2) - Institut de recherche pour le développement [IRD] Institut de Biologie Computationnelle (IBC) ; Institut national de la recherche agronomique (INRA) - Institut de recherche pour le développement [IRD] - Centre de coopération internationale en recherche agronomique pour le développement [CIRAD] - INRIA - CNRS - Université de Montpellier (UM) Bioversity International ; Consultative Group on International Agricultural Research [CGIAR] Espace pour le Développement (ESPACE-DEV) ; Université Montpellier 2 - Sciences et Techniques (UM2) - Université des Antilles et de la Guyane (UAG) - Institut de recherche pour le développement [IRD] - Université de la Réunion SMILE: Système Multi-agent, Interaction, Langage, Evolution (INFO/SMILE) ; Département Informatique (INFO/LIRMM) ; Laboratoire d'Informatique de Robotique et de Microélectronique de Montpellier (LIRMM) ; Université de Montpellier (UM) - CNRS - Université de Montpellier (UM) - CNRS - Laboratoire d'Informatique de Robotique et de Microélectronique de Montpellier (LIRMM) ; Université de Montpellier (UM) - CNRS - Université de Montpellier (UM) - CNRS Amélioration Génétique et Adaptation des Plantes Méditerranéeennes et Tropicales (AGAP) ; Centre international d'études supérieures en sciences agronomiques (Montpellier SupAgro) - Institut national de la recherche agronomique (INRA) - CIRAD-BIOS Pierre Larmande and Elizabeth Arnaud and Isabelle Mougenot and Clement Jonquet and Thérèse Libourel and Manuel Ruiz ANR : IBC, SIFR
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Socio-historical approach of the disabled sport movement in Guadeloupe: social, identity and sports stakes in associations dynamics (1978-2010) ; APPROCHE SOCIO-HISTORIQUE DU MOUVEMENT HANDISPORT EN GUADELOUPE : ENJEUX SOCIAUX, IDENTITAIRES ET SPORTIFS DES DYNAMIQUES ASSOCIATIVES (1978-2010).
Auteur(s) : Villoing, Gael
Auteurs secondaires : Adaptations au Climat Tropical, Exercice et Santé (ACTES) ; Université des Antilles et de la Guyane (UAG) Université Montpellier I Anne Marcellini
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Monitoring deformation from hydrologic processes in a karst aquifer using long-baseline tiltmeters
Auteur(s) : Jacob, Thomas Chery, Jean Boudin, Frederick Bayer, Roger
Auteurs secondaires : Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)
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Aromatase, estrogen receptors and brain development in fish and amphibians
Auteur(s) : Coumailleau, Pascal Pellegrini, Elisabeth Adrio, Fátima Diotel, Nicolas Cano-Nicolau, Joel Nasri, Ahmed Vaillant, Colette Kah, Olivier
Auteurs secondaires : Institut de recherche, santé, environnement et travail [Rennes] (Irset) ; Université d'Angers (UA) - Université des Antilles et de la Guyane (UAG) - Université de Rennes 1 (UR1) - École des Hautes Études en Santé Publique [EHESP] (EHESP) - Institut National de la Santé et de la Recherche Médicale (INSERM) - Structure Fédérative de Recherche en Biologie et Santé de Rennes ( Biosit : Biologie - Santé - Innovation Technologique ) Department of Cell Biology and Ecology ; university of Santigo de Compostela Groupe d'Etude sur l'Inflammation Chronique et l'Obésité (GEICO) ; Université de la Réunion (UR)
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Online Sketch Recognition with Incremental Fuzzy Models
Auteur(s) : Tencer, Lukas Režnáková, Marta Cheriet, Mohamed
Auteurs secondaires : Département de génie de la production automatisée ; Ecole de Technologie Supérieure [Montréal] (ETS) International Graphonomics Society (IGS) Université des Antilles (UA) Céline Rémi Lionel Prévost Eric Anquetil
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Condicionantes del turismo sustentable en el caribe mexicano
Auteur(s) : F. Borja Cervantes, Jorge Gómez Uzeta, Rosalía
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La lecture publique a l’épreuve du territoire, un défi pour la Guyane de demain ?
Auteur(s) : Manga, Blaise Bitegue Dit
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Tuna fishing and a review of payaos in the Philippines
Auteur(s) : Dickson, J Natividad, Ac
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Trade-offs in an ant–plant–fungus mutualism
Auteur(s) : Orivel, Jérôme Malé, Pierre-Jean Lauth, Jérémie Roux, Olivier Petitclerc, Frédéric Dejean, Alain Leroy, Céline
Auteurs secondaires : Ecologie des forêts de Guyane (ECOFOG) ; Centre de Coopération Internationale en Recherche Agronomique pour le Développement (CIRAD) - Institut National de la Recherche Agronomique (INRA) - Université des Antilles et de la Guyane (UAG) - AgroParisTech - Université de Guyane (UG) - Centre National de la Recherche Scientifique (CNRS) UMR Evolution et Diversité Biologique ; Université de Toulouse CNRS : programme Amazonie II ; programme Convergence ; La Région Guyane : Europe : FSE - projet Bi-Appli - 115/SGAR-DE/2011/052274 ; Fondation pour la Recherche sur la Biodiversité : AAP-IN-2009-050 ; Investissement d'avenir : ANR-10-LABX-25-01 - ANR-10-LABX-0041
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Quantification of erosion and sedimentation using time-lapse gravimetry and Lidar in southern Taiwan
Auteur(s) : Mouyen, Maxime Steer, Philippe Croissant, Thomas Lemoigne, Nicolas Hwang, Cheinway Cheng, Ching-Chung Masson, Frédéric Davy, Philippe
Auteurs secondaires : Géosciences Rennes (GR) ; Université de Rennes 1 (UR1) - Institut national des sciences de l'Univers (INSU - CNRS) - Observatoire des Sciences de l'Univers de Rennes (OSUR) - Centre National de la Recherche Scientifique (CNRS) Risques ; Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) - Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) Department of Civil Engineering [Hsinchu] ; National Chiao Tung University (NCTU) Institut de physique du globe de Strasbourg (IPGS) ; Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS) European Geosciences Union
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Joint inversion of teleseismic and GOCE gravity data: application to the Himalayas
Auteur(s) : Basuyau, Clemence Diament, M. Tiberi, Christel Hetenyi, G. Vergne, J. Peyrefitte, A.
Auteurs secondaires : Institut de Physique du Globe de Paris (IPGP) ; Université Pierre et Marie Curie - Paris 6 (UPMC) - Institut national des sciences de l'Univers (INSU - CNRS) - IPG PARIS - Université Paris Diderot - Paris 7 (UPD7) - Université de la Réunion (UR) - Centre National de la Recherche Scientifique (CNRS) Manteau et Interfaces ; Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) - Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) Eidgenössische Technische Hochschule [Zürich] (ETH Zürich) Sismologie ; Ecole et Observatoire des sciences de la terre de Strasbourg (EOSTS) ; Institut national des sciences de l'Univers (INSU - CNRS) - Université Louis Pasteur - Strasbourg I - Centre National de la Recherche Scientifique (CNRS) - Institut national des sciences de l'Univers (INSU - CNRS) - Université Louis Pasteur - Strasbourg I - Centre National de la Recherche Scientifique (CNRS) - Institut de physique du globe de Strasbourg (IPGS) ; Centre National de la Recherche Scientifique (CNRS) - Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS) Bureau de Recherches Géologiques et Minières (BRGM) (BRGM)
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Rutas Alimentarias: una estrategia de negocios inclusivos que vincula las políticas agrarias y turísticas
Auteur(s) : Barrera, Ernesto Bringas Alvarado, Olivia
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La lecture publique à l’épreuve du territoire, un défi pour la Guyane de demain ?
Auteur(s) : Manga, Blaise Bitegue Dit
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Les bénéfices de la protection des mangroves de l’outre-mer français par le Conservatoire du littoral : une évaluation économique à l’horizon 2040
Auteur(s) : Giry, Florent Binet, Thomas Keurmeur, Nastasia
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Du tourisme et de la pauvreté en Afrique : duel ou duo ?
Auteur(s) : Hillali, Mimoun
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Superfast Spreading Rate Crust 4 Integrated Ocean Drilling Program Expedition 335 Scientific Prospectus
Auteur(s) : Teagle, D. Ildefonse, Benoit Blum, P.
Auteurs secondaires : National Oceanography Centre, Southampton ; Université du Québec Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) Texas A&M University [College Station]
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200 mm/y) to exploit the observed relationship between spreading rate and depth to axial low velocity zones, thought to be magma chambers, seismically imaged at active mid-ocean ridges. This was a deliberate strategy to reduce the drilling distance to gabbroic rocks because thick sequences of lavas and dikes have proved difficult to penetrate in past. ODP Leg 206 (2002) initiated operations at Site 1256, including the installation in Hole 1256D of a reentry cone with 16 inch casing inserted through the 250 m thick sedimentary cover and cemented into basement to facilitate deep drilling. The hole was then cored ~500 m into basement. IODP Expeditions 309 and 312 (2005) successfully completed the first sampling of an intact section of upper oceanic crust from lavas, through the sheeted dikes, and into the upper gabbros. Hole 1256D now penetrates >1500 meters below seafloor (mbsf) and >1250 m subbasement and currently resides in the dike–gabbro transition zone. The first gabbroic rocks were encountered at 1407 mbsf. Below this lies a ~100 m complex zone of fractionated gabbros intruded into contact metamorphosed dikes. Although previous cruises achieved the benchmark objective of reaching gabbro in intact ocean crust, critical scientific questions remain. These include the following: 1. Does the lower crust form by the recrystallization and subsidence of a high-level magma chamber (gabbro glacier), crustal accretion by intrusion of sills throughout the lower crust, or some other mechanism? 2. Is the plutonic crust cooled by conduction or hydrothermal circulation? 3. What is the geological nature of Layer 3 and the Layer 2/3 boundary at Site 1256? 4. What is the magnetic contribution of the lower crust to marine magnetic anomalies? Hole 1256D is poised at a depth where samples that should conclusively address these questions can be obtained, possibly with only a few hundred meters of drilling. Importantly, as of the end of Expedition 312, the hole was clear of debris and open to its full depth. Increased rates of penetration (1.2 m/h) and enhanced core recovery (>35%) in the gabbros indicate that this return to Hole 1256D could deepen the hole >300 m into plutonic rocks, past the transition from dikes to gabbro, and into a region of solely cumulate gabbroic rocks."> 200 mm/y) to exploit the observed relationship between spreading rate and depth to axial low velocity zones, thought to be magma chambers, seismically imaged at active mid-ocean ridges. This was a deliberate strategy to reduce the drilling distance to gabbroic rocks because thick sequences of lavas and dikes have proved difficult to penetrate in past. ODP Leg 206 (2002) initiated operations at Site 1256, including the installation in Hole 1256D of a reentry cone with 16 inch casing inserted through the 250 m thick sedimentary cover and cemented into basement to facilitate deep drilling. The hole was then cored ~500 m into basement. IODP Expeditions 309 and 312 (2005) successfully completed the first sampling of an intact section of upper oceanic crust from lavas, through the sheeted dikes, and into the upper gabbros. Hole 1256D now penetrates >1500 meters below seafloor (mbsf) and >1250 m subbasement and currently resides in the dike–gabbro transition zone. The first gabbroic rocks were encountered at 1407 mbsf. Below this lies a ~100 m complex zone of fractionated gabbros intruded into contact metamorphosed dikes. Although previous cruises achieved the benchmark objective of reaching gabbro in intact ocean crust, critical scientific questions remain. These include the following: 1. Does the lower crust form by the recrystallization and subsidence of a high-level magma chamber (gabbro glacier), crustal accretion by intrusion of sills throughout the lower crust, or some other mechanism? 2. Is the plutonic crust cooled by conduction or hydrothermal circulation? 3. What is the geological nature of Layer 3 and the Layer 2/3 boundary at Site 1256? 4. What is the magnetic contribution of the lower crust to marine magnetic anomalies? Hole 1256D is poised at a depth where samples that should conclusively address these questions can be obtained, possibly with only a few hundred meters of drilling. Importantly, as of the end of Expedition 312, the hole was clear of debris and open to its full depth. Increased rates of penetration (1.2 m/h) and enhanced core recovery (>35%) in the gabbros indicate that this return to Hole 1256D could deepen the hole >300 m into plutonic rocks, past the transition from dikes to gabbro, and into a region of solely cumulate gabbroic rocks."> 200 mm/y) to exploit the observed relationship between spreading rate and depth to axial low velocity zones, thought to be magma chambers, seismically imaged at active mid-ocean ridges. This was a deliberate strategy to reduce the drilling distance to gabbroic rocks because thick sequences of lavas and dikes have proved difficult to penetrate in past. ODP Leg 206 (2002) initiated operations at Site 1256, including the installation in Hole 1256D of a reentry cone with 16 inch casing inserted through the 250 m thick sedimentary cover and cemented into basement to facilitate deep drilling. The hole was then cored ~500 m into basement. IODP Expeditions 309 and 312 (2005) successfully completed the first sampling of an intact section of upper oceanic crust from lavas, through the sheeted dikes, and into the upper gabbros. Hole 1256D now penetrates >1500 meters below seafloor (mbsf) and >1250 m subbasement and currently resides in the dike–gabbro transition zone. The first gabbroic rocks were encountered at 1407 mbsf. Below this lies a ~100 m complex zone of fractionated gabbros intruded into contact metamorphosed dikes. Although previous cruises achieved the benchmark objective of reaching gabbro in intact ocean crust, critical scientific questions remain. These include the following: 1. Does the lower crust form by the recrystallization and subsidence of a high-level magma chamber (gabbro glacier), crustal accretion by intrusion of sills throughout the lower crust, or some other mechanism? 2. Is the plutonic crust cooled by conduction or hydrothermal circulation? 3. What is the geological nature of Layer 3 and the Layer 2/3 boundary at Site 1256? 4. What is the magnetic contribution of the lower crust to marine magnetic anomalies? Hole 1256D is poised at a depth where samples that should conclusively address these questions can be obtained, possibly with only a few hundred meters of drilling. Importantly, as of the end of Expedition 312, the hole was clear of debris and open to its full depth. Increased rates of penetration (1.2 m/h) and enhanced core recovery (>35%) in the gabbros indicate that this return to Hole 1256D could deepen the hole >300 m into plutonic rocks, past the transition from dikes to gabbro, and into a region of solely cumulate gabbroic rocks."> 200 mm/y) to exploit the observed relationship between spreading rate and depth to axial low velocity zones, thought to be magma chambers, seismically imaged at active mid-ocean ridges. This was a deliberate strategy to reduce the drilling distance to gabbroic rocks because thick sequences of lavas and dikes have proved difficult to penetrate in past. ODP Leg 206 (2002) initiated operations at Site 1256, including the installation in Hole 1256D of a reentry cone with 16 inch casing inserted through the 250 m thick sedimentary cover and cemented into basement to facilitate deep drilling. The hole was then cored ~500 m into basement. IODP Expeditions 309 and 312 (2005) successfully completed the first sampling of an intact section of upper oceanic crust from lavas, through the sheeted dikes, and into the upper gabbros. Hole 1256D now penetrates >1500 meters below seafloor (mbsf) and >1250 m subbasement and currently resides in the dike–gabbro transition zone. The first gabbroic rocks were encountered at 1407 mbsf. Below this lies a ~100 m complex zone of fractionated gabbros intruded into contact metamorphosed dikes. Although previous cruises achieved the benchmark objective of reaching gabbro in intact ocean crust, critical scientific questions remain. These include the following: 1. Does the lower crust form by the recrystallization and subsidence of a high-level magma chamber (gabbro glacier), crustal accretion by intrusion of sills throughout the lower crust, or some other mechanism? 2. Is the plutonic crust cooled by conduction or hydrothermal circulation? 3. What is the geological nature of Layer 3 and the Layer 2/3 boundary at Site 1256? 4. What is the magnetic contribution of the lower crust to marine magnetic anomalies? Hole 1256D is poised at a depth where samples that should conclusively address these questions can be obtained, possibly with only a few hundred meters of drilling. Importantly, as of the end of Expedition 312, the hole was clear of debris and open to its full depth. Increased rates of penetration (1.2 m/h) and enhanced core recovery (>35%) in the gabbros indicate that this return to Hole 1256D could deepen the hole >300 m into plutonic rocks, past the transition from dikes to gabbro, and into a region of solely cumulate gabbroic rocks."> | 200 mm/y) to exploit the observed relationship between spreading rate and depth to axial low velocity zones, thought to be magma chambers, seismically imaged at active mid-ocean ridges. This was a deliberate strategy to reduce the drilling distance to gabbroic rocks because thick sequences of lavas and dikes have proved difficult to penetrate in past. ODP Leg 206 (2002) initiated operations at Site 1256, including the installation in Hole 1256D of a reentry cone with 16 inch casing inserted through the 250 m thick sedimentary cover and cemented into basement to facilitate deep drilling. The hole was then cored ~500 m into basement. IODP Expeditions 309 and 312 (2005) successfully completed the first sampling of an intact section of upper oceanic crust from lavas, through the sheeted dikes, and into the upper gabbros. Hole 1256D now penetrates >1500 meters below seafloor (mbsf) and >1250 m subbasement and currently resides in the dike–gabbro transition zone. The first gabbroic rocks were encountered at 1407 mbsf. Below this lies a ~100 m complex zone of fractionated gabbros intruded into contact metamorphosed dikes. Although previous cruises achieved the benchmark objective of reaching gabbro in intact ocean crust, critical scientific questions remain. These include the following: 1. Does the lower crust form by the recrystallization and subsidence of a high-level magma chamber (gabbro glacier), crustal accretion by intrusion of sills throughout the lower crust, or some other mechanism? 2. Is the plutonic crust cooled by conduction or hydrothermal circulation? 3. What is the geological nature of Layer 3 and the Layer 2/3 boundary at Site 1256? 4. What is the magnetic contribution of the lower crust to marine magnetic anomalies? Hole 1256D is poised at a depth where samples that should conclusively address these questions can be obtained, possibly with only a few hundred meters of drilling. Importantly, as of the end of Expedition 312, the hole was clear of debris and open to its full depth. Increased rates of penetration (1.2 m/h) and enhanced core recovery (>35%) in the gabbros indicate that this return to Hole 1256D could deepen the hole >300 m into plutonic rocks, past the transition from dikes to gabbro, and into a region of solely cumulate gabbroic rocks.">Plus
Patterns of variations in large pelagic fish: A comparative approach between the Indian and the Atlantic Oceans
Auteur(s) : Corbineau, A. Rouyer, Tristan Fromentin, Jean-marc Cazelles, B. Fonteneau, Alain Menard, Frederic
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