74 documents satisfont la requête.
Surface freshwater storage and dynamics in the Amazon basin during the 2005 exceptional drought
Auteur(s) : Frappart, Frédéric Papa, Fabrice Santos Da Silva, Joecila Ramillien, Guillaume Prigent, Catherine Seyler, Frédérique Calmant, Stéphane
Auteurs secondaires : Géosciences Environnement Toulouse (GET) ; Université Paul Sabatier - Toulouse 3 (UPS) - Institut de recherche pour le développement [IRD] - Observatoire Midi-Pyrénées - CNRS Laboratoire d'Etudes en Géophysique et Océanographie Spatiales (LEGOS NOUMEA) ; CNRS - Institut de recherche pour le développement [IRD] : UR065 Centro de Estudos do Tropico Umido (CESTUAv) ; Universidade do Estado do Amazonas Laboratoire d'Etude du Rayonnement et de la Matière en Astrophysique (LERMA) ; CNRS - INSU - Observatoire de Paris - Université de Cergy Pontoise - École normale supérieure - Paris (ENS Paris) - Université Pierre et Marie Curie - Paris 6 (UPMC) 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 Laboratoire d'études en Géophysique et océanographie spatiales (LEGOS) ; CNRS - Institut de recherche pour le développement [IRD] - CNES - INSU - Observatoire Midi-Pyrénées - Université Paul Sabatier - Toulouse 3 (UPS) Projet TOSCA (CNES) 'Variability of terrestrial freshwater storage in the Tropics from multisatellite observations'
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Evaluation of the recovery of microbial functions during soil restoration using near-infrared spectroscopy
Auteur(s) : Schimann, Heidy Joffre, Richard ROGGY, Jean-Christophe Lensi, Robert Domenach, Anne-Marie
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 - Centre National de la Recherche Scientifique (CNRS) 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)
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Statistical classification of log response as an indicator of facies variation during changes in sea level: Integrated Ocean Drilling Program Expedition 313
Auteur(s) : Inwood, Jennifer Lofi, Johanna Davies, Sarah Basile, Christophe Bjerum, Christian Mountain, Gregory, Proust, Jean-Noël Al, Et
Auteurs secondaires : Borehole Research Group (BRG) ; Department of Geology [Leicester] ; University of Leicester - University of Leicester Transferts en milieux poreux ; 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) Tectonique reliefs et bassins ; Institut des Sciences de la Terre (ISTerre) ; Université Joseph Fourier - Grenoble 1 (UJF) - Institut Français des Sciences et Technologies des Transports, de l'Aménagement et des Réseaux (IFSTTAR) - Institut national des sciences de l'Univers (INSU - CNRS) - Institut de recherche pour le développement [IRD] : UR219 - PRES Université de Grenoble - Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry]) - Centre National de la Recherche Scientifique (CNRS) - Université Joseph Fourier - Grenoble 1 (UJF) - Institut Français des Sciences et Technologies des Transports, de l'Aménagement et des Réseaux (IFSTTAR) - Institut national des sciences de l'Univers (INSU - CNRS) - Institut de recherche pour le développement [IRD] : UR219 - PRES Université de Grenoble - Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry]) - Centre National de la Recherche Scientifique (CNRS) 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)
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Comparative modifications in bacterial gill-endosymbiotic populations of the two bivalves Codakia orbiculata and Lucina pensylvanica during bacterial loss and reacquisition
Auteur(s) : Elisabeth, Nathalie H. Caro, Audrey Cesaire, Thierry Mansot, Jean-Louis Escalas, Arthur Sylvestre, Marie-Noelle Jean-Louis, Patrick Gros, Olivier
Auteurs secondaires : Biologie de la Mangrove (BM) ; Systématique, adaptation, évolution (SAE) ; Université Pierre et Marie Curie - Paris 6 (UPMC) - Centre National de la Recherche Scientifique (CNRS) - Université Pierre et Marie Curie - Paris 6 (UPMC) - Centre National de la Recherche Scientifique (CNRS) - Evolution Paris Seine ; Université Nice Sophia Antipolis (UNS) ; Université Côte d'Azur (UCA) - Université Côte d'Azur (UCA) - Centre National de la Recherche Scientifique (CNRS) - Université des Antilles et de la Guyane (UAG) - Université Pierre et Marie Curie - Paris 6 (UPMC) - Université Nice Sophia Antipolis (UNS) ; Université Côte d'Azur (UCA) - Université Côte d'Azur (UCA) - Université des Antilles et de la Guyane (UAG)
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Phylogéographie mondiale des bacilles tuberculeux : contribution des outils moléculaires et bioinformatiques et caractérisation des lignées génotypiques pour des études épidémiologiques et phylogénétiques.
Auteur(s) : Hill, Véronique
Auteurs secondaires : Antilles-Guyane Rastogi, Nalin
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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
0461 : Comparison of cardiovascular responses to nitrogen dioxide and diesel exhausts. An experimental study with controlled exposures to air pollutants
Auteur(s) : Karoui, Ahmed Crochemore, Clément Mekki, Malik Préterre, David Cazier, Fabrice Dewaele, Dorothée Vaugeois, Jean-Marie Corbière, Cécile
Auteurs secondaires : Centre commun de mesure, Dunkerque, France ; Université du Littoral Côte d'Opale Centre de recherche en neurosciences de Lyon ; Université Claude Bernard Lyon 1 (UCBL) - Université Jean Monnet [Saint-Étienne] (UJM) - Université de Lyon - Institut National de la Santé et de la Recherche Médicale (INSERM) - Centre National de la Recherche Scientifique (CNRS) Unité de neuropsychopharmacologie expérimentale (UNE) ; Université de Rouen Normandie (URN) ; Normandie Université (NU) - Normandie Université (NU) - Centre National de la Recherche Scientifique (CNRS) 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 ) Unité d'Epidémiologie [Antananarivo, Madagascar] (IPM) ; Institut Pasteur de Madagascar - Réseau International de Instituts Pasteur Nouvelles Cibles Pharmacologiques de la Protection Endothéliale et de l'Insuffisance Cardiaque (EnVI) ; CHU Rouen - Université de Rouen Normandie (URN) ; Normandie Université (NU) - Normandie Université (NU) - Institut National de la Santé et de la Recherche Médicale (INSERM)
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Baitboat as a tuna aggregating device
Auteur(s) : Hallier, Jean-pierre Delgado De Molina, A
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Molecular biomass and MetaTaxogenomic assessment of soil microbial communities as influenced by soil DNA extraction procedure
Auteur(s) : Terrat, Sebastien Christen, Richard Dequiedt, Samuel Lelievre, Melanie Nowak, Virginie Regnier, Tiffanie Bachar, Dipankar Plassart, Pierre
Auteurs secondaires : Symbiose Marine (SM) ; Systématique, adaptation, évolution (SAE) ; Université Pierre et Marie Curie - Paris 6 (UPMC) - Centre National de la Recherche Scientifique (CNRS) - Université Pierre et Marie Curie - Paris 6 (UPMC) - Centre National de la Recherche Scientifique (CNRS) - Evolution Paris Seine ; Université Nice Sophia Antipolis (UNS) ; Université Côte d'Azur (UCA) - Université Côte d'Azur (UCA) - Centre National de la Recherche Scientifique (CNRS) - Université des Antilles et de la Guyane (UAG) - Université Pierre et Marie Curie - Paris 6 (UPMC) - Université Nice Sophia Antipolis (UNS) ; Université Côte d'Azur (UCA) - Université Côte d'Azur (UCA) - Université des Antilles et de la Guyane (UAG) ADEME (French Environment and Energy Management Agency) Regional Council of Burgundy Genoscope (Evry, France) French Scientific Group of Interest on soils `GIS Sol', involving the French Ministry for Ecology and Sustainable Development (MEDAD) French Ministry of Agriculture French Institute for Environment (IFEN)
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CMV+ Serostatus Associates Negatively with CD4:CD8 Ratio Normalization in Controlled HIV-Infected Patients on cART
Auteur(s) : Poizot-Martin, Isabelle Allavena, Clotilde Duvivier, Claudine Cano, Carla Eliana Guillouet De Salvador, Francine Rey, David Dellamonica, Pierre Cuzin, Lise
Auteurs secondaires : Sciences Economiques et Sociales de la Santé & Traitement de l'Information Médicale (SESSTIM) ; Institut de Recherche pour le Développement (IRD) - Aix Marseille Université (AMU) - ORS PACA - Institut National de la Santé et de la Recherche Médicale (INSERM) Hôpital Sainte-Marguerite [CHU - APHM] (Hôpitaux Sud ) Service des maladies infectieuses et tropicales [CHU Nantes] ; CHU Nantes Infection à VIH, réservoirs, diversité génétique et résistance aux antirétroviraux (ARV) (EA 7327) ; Université Paris Descartes - Paris 5 (UPD5) Centre d’Infectiologie Necker Pasteur ; Assistance publique - Hôpitaux de Paris (AP-HP) - Université Paris Descartes - Paris 5 (UPD5) - CHU Necker - Enfants Malades [AP-HP] Service des maladies infectieuses ; CHU Nice - University Hospital Les Hôpitaux Universitaires de Strasbourg (HUS) Epidémiologie et analyses en santé publique : risques, maladies chroniques et handicaps [Toulouse] ; Université Paul Sabatier - Toulouse 3 (UPS) - Institut National de la Santé et de la Recherche Médicale (INSERM)
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Multi-scale morphodynamics of sand barrier driven by Monsoon/typhoon conditions
Auteur(s) : Campmas, Lucie Sabatier, François Meulé, Samuel Liou, Jying Li Petitjean, Lise Boutin, Frédéric Leroux-Mallouf, Romain Sous, Damien
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) Centre européen de recherche et d'enseignement de géosciences de l'environnement (CEREGE) ; Institut de Recherche pour le Développement (IRD) - Aix Marseille Université (AMU) - Collège de France (CdF) - Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS) thl ; Université du Québec Institut méditerranéen d'océanologie (MIO) ; Institut de Recherche pour le Développement (IRD) - Aix Marseille Université (AMU) - Institut de recherche pour le développement [IRD] : UMR235 - Université de Toulon (UTLN) - Centre National de la Recherche Scientifique (CNRS)
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The Costa Maya: Evolution of a Touristic Landscape
Auteur(s) : Meyer-Arendt, Klaus J.
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Evidence that graft-site candidiasis after kidney transplantation is acquired during organ recovery: a multicenter study in France.
Auteur(s) : Albano, Laetitia Bretagne, Stéphane Mamzer-Bruneel, Marie-France Kacso, Irina Desnos-Ollivier, Marie Guerrini, Patrice Le Luong, Thanh Cassuto, Elisabeth
Auteurs secondaires : Service de néphrologie ; Hôpital Pasteur Nice Service de parasitologie [Mondor] ; Assistance publique - Hôpitaux de Paris (AP-HP) - Hôpital Henri Mondor - Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12) Mycologie Moléculaire ; CNRS - Institut Pasteur de Paris Service de néphrologie adultes ; Assistance publique - Hôpitaux de Paris (AP-HP) - Hôpital Necker - Enfants Malades - Université Paris Descartes - Paris 5 (UPD5) Agence de la Biomédecine ; Agence de la biomédecine Service de transplantation ; Hospices Civils de Lyon - Hôpital Edouard Herriot Service des maladies infectieuses et tropicales ; Assistance publique - Hôpitaux de Paris (AP-HP) - Hôpital Necker - Enfants Malades - Université Paris Descartes - Paris 5 (UPD5) - Centre d'infectiologie Necker-Pasteur Signalisation et Réponses aux Agents Infectieux et Chimiques (SeRAIC) ; Université de Rennes 1 (UR1) - Institut de recherche, santé, environnement et travail [Rennes] (Irset) ; INSERM - École Nationale de la Santé Publique - Université de Rennes 1 (UR1) - Université des Antilles et de la Guyane (UAG) - Structure Fédérative de Recherche en Biologie-Santé de Rennes (Biosit) ; Université de Rennes 1 (UR1) - INSERM - CNRS - INSERM - CNRS - INSERM - École Nationale de la Santé Publique - Université de Rennes 1 (UR1) - Université des Antilles et de la Guyane (UAG) - Structure Fédérative de Recherche en Biologie-Santé de Rennes (Biosit) ; Université de Rennes 1 (UR1) - INSERM - CNRS - INSERM - CNRS - IFR140
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Measuring water accumulation rates using GRACE data in areas experiencing glacial isostatic adjustment: The Nelson River basin
Auteur(s) : Lambert, Adrien Huang, J. Van Derkamp, G. Henton, J. MAZZOTTI, Stephane James, T. S. Courtier, N. Barr, A. G.
Auteurs secondaires : Geological Survey of Canada, Natural Resources Canada, Sidney ; Université du Québec Geodetic Survey Division, Natural Resources Canada, Ottawa ; Université du Québec National Hydrology Research Centre, Environment Canada, Saskatoon ; Université du Québec 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)
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Functional analysis of human RhCG: comparison with E. coli ammonium transporter reveals similarities in the pore and differences in the vestibule
Auteur(s) : Zidi-Yahiaoui, Nedjma Callebaut, Isabelle Genetet, Sandrine Le Van Kim, Caroline Cartron, Jean-Pierre Colin, Yves Ripoche, Pierre Mouro-Chanteloup, Isabelle
Auteurs secondaires : Protéines de la membrane érythrocytaire et homologues non-érythroides ; Université des Antilles et de la Guyane (UAG) - Institut National de la Transfusion Sanguine [Paris] (INTS) - Université Paris Diderot - Paris 7 (UPD7) - Université de la Réunion (UR) - Institut National de la Santé et de la Recherche Médicale (INSERM) Institut de minéralogie et de physique des milieux condensés (IMPMC) ; Université Pierre et Marie Curie - Paris 6 (UPMC) - IPG PARIS - Université Paris Diderot - Paris 7 (UPD7) - Centre National de la Recherche Scientifique (CNRS)
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Local-scale projections of coral reef futures and implications of the Paris Agreement
Auteur(s) : Van Hooidonk, Ruben, Maynard, Jeffrey, Tamelander, Jerker Gove, Jamison, Ahmadia, Gabby, Raymundo, Laurie Williams, Gareth Heron, Scott,
Auteurs secondaires : NOAA Atlantic Oceanographic and Meteorological Laboratory (AOML) ; National Oceanic and Atmospheric Administration (NOAA) Centre de recherches insulaires et observatoire de l'environnement (CRIOBE) ; Université de Perpignan Via Domitia (UPVD) - École pratique des hautes études (EPHE) - Centre National de la Recherche Scientifique (CNRS) United Nations Environment Programme Ecosystems and Oceanography Program ; Pacific Islands Fisheries Science Center World Wildlife Fund Marine Laboratory ; University of Guam School of Ocean Sciences ; Bangor University Marine Geophysical Laboratory ; James Cook University (JCU)
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Effect of heat exposure and exercise on food intake regulation: a randomized crossover study in young healthy men
Auteur(s) : Faure, Cécile Charlot, Keyne Henri, Stéphane Hardy-Dessources, Marie-Dominique Hue, Olivier Antoine-Jonville, Sophie
Auteurs secondaires : Adaptations au Climat Tropical, Exercice et Santé (ACTES) ; Université des Antilles et de la Guyane (UAG) Université des Antilles (Pôle Guadeloupe) ; Université des Antilles (UA) Labex Matisse ANR-11-IDEX-0004-02/10-LABX-0067, MATISSE, MATerials, InterfaceS, Surfaces, Environment(2011)
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Mémoire indienne dans The Swinging Bridge de Ramabai Espinet : la construction d’une identité indo-trinidadienne diasporique
Auteur(s) : Solbiac, Rodolphe
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Measurements of semi-volatile organic compounds in settled dust: influence of storage temperature and duration.
Auteur(s) : Blanchard, Olivier Mercier, Fabien Ramalho, Olivier Mandin, Corinne Le Bot, Barbara Glorennec, Philippe
Auteurs secondaires : Laboratoire d'étude et de recherche en environnement et santé (LERES) ; École des Hautes Études en Santé Publique [EHESP] (EHESP) Centre Scientifique et Technique du Bâtiment (CSTB) ; Centre Scientifique et Technique du Bâtiment (CSTB) 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 ) Agence de l'Environnement et de la Maîtrise de l'Energie, Primequal2/Predit. Grant Number: 0962C0070
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Multi-mode surface waveform tomography of the Pacific Ocean: A closer look at lithospheric cooling
Auteur(s) : Maggi, Alessia Debayle, Eric Priestley, Keith Barruol, Guilhem
Auteurs secondaires : Institut de physique du globe de Strasbourg (IPGS) ; Institut national des sciences de l'Univers (INSU - CNRS) - Université Louis Pasteur - Strasbourg I - Centre National de la Recherche Scientifique (CNRS) Bullard Laboratories ; University of Cambridge [UK] (CAM) 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) Laboratoire de Tectonophysique (Tectonophysique) ; Université Montpellier 2 - Sciences et Techniques (UM2) - Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS)
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