Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The formation age of the Siberian cratonic mantle is not well established as yet. Re–Os data on various mantle-derived materials have shown that it contains Archaean components, but the reported Re-depletion ages show a broad variation range (3.4 to 1 Ga) and are commonly ≤ 2 Ga for peridotite xenoliths. We report Hf and Nd isotope data for cpx and garnet separated from nine refractory spinel and garnet peridotite xenoliths from the Udachnaya kimberlite. The cpx from low-opx spinel harzburgites show extremely high εHf values, from + 607 to + 2084, which testify to long-term evolution of these rocks with high Lu/Hf ratios, consistent with their residual origin and near absence of post-melting enrichments in the Lu–Hf system. Such high εHf values are unusual for cpx from other cratonic peridotites and are higher than those reported for depleted cpx in off-cratonic peridotites. The clinopyroxenes from low-opx spinel harzburgites yield Hf model ages from 1.9 to 1.7 Ga while the cpx from high-opx spinel harzburgites yield Hf model ages from 3.0 to 1.9 Ga. When plotted together, they define a Lu/Hf isochron with an age of 1.80 Ga, which we consider as a robust estimate of the formation age (melt extraction event) because it is obtained on residual rocks that show no evidence for HREE and Hf enrichments and because the model ages for three out of four individual samples are similar to each other. The cpx have high εNd of + 94 to + 123, which are inconsistent with their low Sm/NdPM of < 1 and yield no meaningful age estimates. The consistently high, positive εNd in these cpxs can be interpreted in terms of long-term evolution of refractory peridotites with high Sm/Nd, followed by relatively recent LREE enrichments.We infer that a significant part of the lithospheric mantle in the central Siberian craton may have been formed during a major event (or a series of events) at around 1.8 Ga. Older ages reported for the central Siberian craton may refer to less common materials from cratonic or other domains formed in the Archaean that were later incorporated into the cratonic roots. The transition from the “Archaean” to “modern” tectonic regimes in Siberia and possibly elsewhere may have taken place at 1.8–1.9 Ga rather than at ~ 2.5 Ga, i.e. in the second half of the Paleoproterozoic rather than at the Archaean–Proterozoic boundary, at which time the asthenospheric mantle became generally too cold to experience high-degree melting on a large scale. The ~ 1.8 Ga formation age of the Siberian cratonic mantle is coeval with that for a major part of the ancient continental crust in the central Siberian craton. The temporal crust–mantle links may be explained either by the generation of the initial source materials for continental crust in the same melting event that formed the residual peridotites or, alternatively, by subduction and melting of pre-existing proto-lithosphere destabilized by a major mantle upwelling that formed the residual mantle.
ISSN: 0009-2541

hal-01115519
https://hal.archives-ouvertes.fr/hal-01115519
DOI : 10.1016/j.chemgeo.2014.10.018

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Background: Blood Lead Levels (BLLs) have substantially decreased in recent decades in children in France. However, further reducing exposure is a public health goal because there is no clear toxicological threshold. The identification of the environmental determinants of BLLs as well as risk factors associated with high BLLs is important to update prevention strategies. We aimed to estimate the contribution of environmental sources of lead to different BLLs in children in France.Methods: We enrolled 484 children aged from 6 months to 6 years, in a nationwide cross-sectional survey in 2008-2009. We measured lead concentrations in blood and environmental samples (water, soils, household settled dusts, paints, cosmetics and traditional cookware). We performed two models: a multivariate generalized additive model on the geometric mean (GM), and a quantile regression model on the 10th, 25th, 50th, 75th and 90th quantile of BLLs. Results: The GM of BLLs was 13.8 μg/L (=1.38 µg/dL) (95% Confidence Intervals (CI): 12.7-14.9) and the 90th quantile was 25.7 μg/L (CI: 24.2-29.5). Household and common area dust, tap water, interior paint, ceramic cookware, traditional cosmetics, playground soil and dust, and environmental tobacco smoke were associated with the GM of BLLs. Household dust and tap water made the largest contributions to both the GM and the 90th quantile of BLLs. The concentration of lead in dust was positively correlated with all quantiles of BLLs even at low concentrations. Lead concentrations in tap water above 5 µg/L were also positively correlated with the GM, 75th and 90th quantiles of BLLs in children drinking tap water.Conclusions: Preventative actions must target household settled dust and tap water to reduce the BLLs of children in France. The use of traditional cosmetics should be avoided whereas ceramic cookware should be limited to decorative purposes.
ISSN: 0160-4120

Droits : info:eu-repo/semantics/OpenAccess
hal-01099719
https://hal.archives-ouvertes.fr/hal-01099719
https://hal.archives-ouvertes.fr/hal-01099719/document
https://hal.archives-ouvertes.fr/hal-01099719/file/Manuscript_Etchevers_EI_V3_no%20%20changes%20marked.pdf
DOI : 10.1016/j.envint.2014.10.007

Éditeur(s) : HAL CCSD Cambridge University Press (CUP)
Résumé :  
Large seasonal variation in the rate of change in girth of tropical rain-forest tree species has been described, but its origin is still under debate. We tested whether this variation might be related to variation in atmospheric relative humidity through its influence on bark water content and thickness. Variation in trunk circumference of 182 adult trees was measured about twice a month in an undisturbed tropical rain forest over 18mo using dendrometers. Furthermore, a laboratory experiment was conducted to test the direct influence of relative air humidity on bark water content and thickness. In the field, most trees displayed highly positive rates of change in girth at the onset of the wet season, while a quarter of the trees displayed negative changes during long dry seasons, whatever their total annual growth. This variation was correlated with environmental conditions, particularly with atmospheric relative humidity. Trees with high bark water content and thickness displayed a stronger decrease in girth during the dry season. In the chamber experiment, desiccation induced a decrease in the diameter of the trunk sections in tandem with a decrease in bark water content. As a result, seasonal variation in the rate of change in girth of tropical rain-forest trees reflects variation in trunk biophysical properties, through the influence of relative humidity on bark properties, but not directly variation in secondary growth.
ISSN: 0266-4674

hal-01032186
https://hal.archives-ouvertes.fr/hal-01032186
DOI : 10.1017/S0266467410000155

Éditeur(s) : Cnexo
Résumé : Sachons ensuite discerner ce qui peut ou doit changer des éléments permanents qui conditionnent le succès d'une action en profondeur du CNEXO. Il est à cet égard un point fondamental: c'est celui de la position que nous nous assignons dans l'ensemble du dispositif océanologique français. Là, nous ne pouvons fluctuer au gré du temps, des modes ou des opportunités. Nos choix doivent être clairs pour être ratifiés clairement par les textes et pour être compris clairement par nos partenaires. Ils ne seront pas savamment mis en cause s'ils correspondent bien à une réalité ou à un besoin profond et parce qu'ils correspondent à une telle nécessité ils ne sauraient varier sauf à ce que nous soyons accusés d'inconscience ou d'inconsistance. Mais il ne suffit pas que ces choix soient ceux de la Direction Générale pour que la situation du CNEXO soit solide. Il faut encore qu'ils soient profondément compris, vécus, expliqués, joués intelligemment par l'ensemble de notre communauté. Ce n'est pas là une abstraction. Notre avenir est directement lié à la perception concrète et correcte que chacun d'entre vous en aura. Sinon, nous subirons le sort ... des Diplodocus! Le Colloque doit être un moment privilégié pour nous exprimer à ce sujet. Que nous fassions le point à cet égard dans les discussions préparatoires internes est bon et nécessaire. Que nous sachions ensuite en parler clairement avec talent dans un langage conscient des réalités est indispensable. [OCR NON CONTRÔLE]
La Lettre du Cnexo (Cnexo), 1981-09 , N. 8 , P. 1-6

Droits : Cnexo - Ifremer
http://archimer.ifremer.fr/doc/1981/publication-4769.pdf
http://archimer.ifremer.fr/doc/00000/4769/

Éditeur(s) : HAL CCSD Editeur :1022 [SUISSE] : Association de la revue [petite] enfance
Résumé : International audience
En Martinique, comme dans d'autres régions francophones/créolophones, les adultes éduquent et instruisent les enfants en langue française. Ils tendent toutefois, par leurs propres conduites langagières en présence des tout petits, à lever le voile sur l'emploi de la langue créole qu'ils tiennent tant à proscrire au contact des enfants. Cette contradiction dans les conduites langagières des adultes est rapidement repérée par les enfants qui saisissent progressivement les interdits et la dimension confidentielle relatifs à l'emploi du créole, en faisant notamment la part des fréquents échanges créolophones entre adultes et de l'emploi exclusif du français par ces mêmes adultes lorsqu'ils s'adressent à eux. Au contact de son milieu familial et/ou dans les collectivités qu'il fréquente, le tout petit a un rapport plus ou moins direct avec la langue créole qu'emploient des adultes (conversations entendues) ou certains pairs de son entourage. Il surprend par moments ses locuteurs référents lors de l'introduction spontanée d'expressions en créole dans leurs énoncés. Ce n'est qu'au moment de l'intégration des règles liées aux pratiques langagières établies dans le cadre de son éducation que s'instaure une pudeur relative au parler créole en présence des adultes. Dès sa dernière année de crèche (2ans1/2 – 3 ans) et sa première année d'école, il commence à maîtriser le parler français, tout en intériorisant les contradictions des adultes de son entourage. Les distorsions langagières se sont ainsi déplacées d'un espace intersubjectif (entre l'enfant et l'adulte) à un espace intra subjectif (chez l'enfant lui-même) où le jeune locuteur a commencé à s'autocensurer dans ses pratiques langagières, se conformant aux exigences monolingues de l'école où il s'instruit. L'activité du tout petit se situe aussi bien au niveau de la production d'actes langagiers que dans sa position de sujet entendant les productions de ses interlocuteurs, c'est-à-dire que le point de départ de l'investissement personnel de la langue entendue se situe au niveau de l'écoute pratiquée par le locuteur en puissance, le point d'élaboration de cet investissement se manifestant à travers la mise en oeuvre des éléments recueillis durant l'écoute.
ISSN: 1422-8874

Droits : info:eu-repo/semantics/OpenAccess
hal-01658926
https://hal.univ-antilles.fr/hal-01658926
https://hal.univ-antilles.fr/hal-01658926/document
https://hal.univ-antilles.fr/hal-01658926/file/Les%20enfants%20au%20contact%20de%20la%20langue%20proscrite%20RPES.pdf

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Ctenophores are a phylum of non-bilaterian marine (mostly planktonic) animals, characterised by several unique synapomorphies (e.g., comb rows, apical organ). Relationships between and within the nine recognised ctenophore orders are far from understood, notably due to a paucity of phylogenetically informative anatomical characters. Previous attempts to address ctenophore phylogeny using molecular data (18S rRNA) led to poorly resolved trees but demonstrated the paraphyly of the order Cydippida. Here we compiled an updated 18S rRNA data set, notably including a few newly sequenced species representing previously unsampled families (Lampeidae, Euryhamphaeidae), and we constructed an additional more rapidly evolving ITS1 + 5.8S rRNA + ITS2 alignment. These data sets were analysed separately and in combination under a probabilistic framework, using different methods (maximum likelihood, Bayesian inference) and models (e.g., doublet model to accommodate secondary structure; data partitioning). An important lesson from our exploration of these datasets is that the fast-evolving internal transcribed spacer (ITS) regions are useful markers for reconstructing high-level relationships within ctenophores. Our results confirm the paraphyly of the order Cydippida (and thus a ``cydippid-like'' ctenophore common ancestor) and suggest that the family Mertensiidae could be the sister group of all other ctenophores. The family Lampeidae (also part of the former ``Cydippida'') is probably the sister group of the order Platyctenida (benthic ctenophores). The order Beroida might not be monophyletic, due to the position of Beroe abyssicola outside of a clade grouping the other Beroe species and members of the ``Cydippida'' family Haeckeliidae. Many relationships (e.g. between Pleurobrachiidae, Beroida, Cestida, Lobata, Thalassocalycida) remain unresolved. Future progress in understanding ctenophore phylogeny will come from the use of additional rapidly evolving markers and improvement of taxonomic sampling.
ISSN: 0944-2006

hal-01544475
https://hal.archives-ouvertes.fr/hal-01544475
DOI : 10.1016/j.zool.2014.06.004

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
To understand the deep cycle of water, upper mantle water content and distribution between nominally anhydrous minerals (NAMs) and hydrous minerals (e.g., amphibole) must be constrained. We need then to understand H behaviour during mantle melting and metasomatism. Major, minor and trace element compositions including water contents were obtained on ten xenoliths of spinel-bearing peridotites from the Ray Pic locality, in the Southern part of the Massif Central (France). The sample suite investigated here is composed of rather fertile lherzolites (89.4 ≤ Fo ≤ 90.8%; 11.3 ≤ cr# in spinel ≤ 21.1%; 0.942 ≤ [Yb]cpx ≤ 1.90 ppm; cpx: clinopyroxene), which can be best explained by batch melting, with degree of melting between 3 and 10%. These xenoliths contain up to 8% modal amphibole. Three groups are defined as a function of the amphibole modal abundance (above or below 1%) and equilibrium temperature (above or below 1000 °C). Results show no clear positive correlation between modal metasomatism (amphibole) and incompatible element enrichment in cpx. Trace element compositions in cpx show strong enrichments of the most incompatible elements (e.g., (La/Sm)PM as high as 15.7; PM: normalised to primitive mantle values), but strong negative anomalies of the high field strength elements (e.g., (Th/Nb)PM as high as ~ 680). Such trace element fractionations are usually ascribed to the so-called carbonatitic metasomatism involving the percolation of small volume melts which are enriched in volatiles. The hydrogen concentrations in cpx range from 203 to 330 ppm wt. H2O, in orthopyroxene from 66 to 160 ppm wt. H2O and in olivine from 2 to 6 ppm wt. H2O. These values are within the common concentration range of other spinel-bearing peridotites. Amphiboles contain 1.9 ± 0.5 wt.% of H2O.The effect of metasomatism on water abundances in NAMs is not straightforward. Hydrous metasomatism (i.e., leading to the crystallisation of OH-bearing amphibole) has no effect on the water content of the co-existing NAMs. This suggests thus that the occurrence of hydrous minerals, such as amphibole, does not systematically imply that the coexisting NAMs are water-rich (saturated). Further, the percolation of volatile-rich small volume melts, which is fingerprinted by the strong enrichment of the incompatible elements, has also no clear effect on the water content of the NAMs. These data are thus difficult to reconcile with the admitted highly incompatible behaviour of H in upper mantle minerals.
ISSN: 0024-4937

hal-01278062
https://hal.archives-ouvertes.fr/hal-01278062
DOI : 10.1016/j.lithos.2015.08.013

Éditeur(s) : HAL CCSD Elsevier Masson
Résumé : International audience
Alveolar proteinosis (AP) is a rare disease characterized by alveolar accumulation of surfactant components, which impairs gas exchange. AP is classified into three groups: auto-immune AP defined by the presence of plasma autoantibodies anti-GM-CSF, the most frequent form (90 % of all AP); secondary AP, mainly occurring as a consequence of haematological diseases, or following on from toxic inhalation or infections, and genetic AP, which affects almost exclusively children. AP diagnosis is suspected where chest CT-scan demonstrates interstitial lung disease with a crazy paving aspect; and confirmed by bronchoalveolar lavage, which has a milky appearance and contains periodic acid Schiff positive proteinaceous alveolar deposits. The use of surgical lung biopsy to confirm AP is less frequent nowadays. In this context, positive antibodies against GM-CSF indicates an auto-immune etiology of the AP. Concerning management, whole lung lavage is the gold standard therapy. In refractory AP, new treatments are available such as subcutaneous or inhaled GM-CSF supplementation, or rituximab infusions. The clinical course is unpredictable. Spontaneous improvement or even cure can occur, and the 5-year actuarial survival is 95 %. The most frequent complications are infectious etiology.
La protéinose alvéolaire pulmonaire (PAP) est une maladie rare caractérisée par l’accumulation alvéolaire de composants du surfactant qui gêne les échanges gazeux. Les PAP sont séparées en trois groupes : les PAP auto-immunes caractérisées par la présence d’anticorps sériques anti-GM-CSF qui sont les plus fréquentes ; les PAP secondaires à une maladie sous-jacente, le plus souvent hématologique, mais aussi à l’inhalation de toxiques et à des infections ; enfin, les PAP d’origine génétique. Le diagnostic de PAP est évoqué sur le scanner thoracique avec une pneumopathie infiltrante diffuse ayant un aspect classique de crazy paving, puis confirmé par l’aspect laiteux du lavage bronchoalvéolaire, et la présence de matériel lipoprotéinacé PAS positif. La confirmation du diagnostic de PAP par biopsie pulmonaire chirurgicale est désormais rarement nécessaire. La positivité des anticorps sériques anti-GM-CSF signe le caractère auto-immun de la maladie. Le traitement de référence des PAP auto-immunes est le « grand lavage pulmonaire thérapeutique ». En cas de maladie réfractaire, d’autres traitements sont disponibles, tels que le GM-CSF en injection sous-cutanée ou en aérosol et le rituximab. L’évolution de la maladie est imprévisible. Une évolution spontanément favorable ou même une guérison spontanée peuvent survenir et la survie actuarielle à 5 ans est de 95 %. Les principales complications sont infectieuses.
ISSN: 0761-8425

hal-01085907
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01085907
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01085907/document
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01085907/file/Prot%C3%A9inose%20alv%C3%A9olaire%20pulmonaire_accepted.pdf
DOI : 10.1016/j.rmr.2014.08.009

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Tourism in marine and coastal areas is a complex phenomenon. Tourism in coastal areas brings along both positive and negative effects on the environment as a result of activities exerted upon such areas by proponents and tourists. While tourism development results in the modification of coastal environments, it can also flourish where such environments are left unmodified as the pristine nature of the environments attract visitors. Alternatively, in order for marine and coastal tourism to develop and continue to attract tourists, there is the need for an integrated approach that can be translated into a sustainable coastal tourism development. The aim of this paper therefore, is to postulate and develop a framework and guideline to be addressed by decision-makers for coastal areas. Frameworks for sustainable coastal tourism development and coastal zone management (CZM) are suggested taking into account the multifaceted nature of the coastal environment. Although Hong Kong epitomizes a successful tourism destination, alternative tourism is attractive as the diversity of habitats and life forms makes the Hong Kong coastal area unique. For the ecological richness to continue to provide avenues for alternative tourism, it is argued that such frameworks should be adaptable and implemented for a sustainable coastal tourism policy.
La gestion des processus touristique dans des secteurs marins et côtiers est complexe. Les pratiques touristiques et récréatives s’accompagnent d’effets positifs et négatifs sur l'environnement. Le développement de tourisme peut s’épanouir sur des environnements faiblement modifiés mais il n’est pas sans conséquence sur la modification des environnements côtiers. Une gestion intégrée s’impose pour intégrer les pratiques touristiques dans un processus de développement côtier soutenable. Le but de cet article est de proposer un cadre et une orientation pour la gestion intégrée des secteurs côtiers. Des cadres pour le développement côtier soutenable de tourisme et la gestion côtière de zone (CZM) sont suggérés en tenant compte de la nature diversifiée des environnements côtiers. Bien que Hong Kong constitue destination touristique réussie, le tourisme littoral, avec des approches alternatives, est aussi un aspect à promouvoir tant autour de la diversité des habitats et que des formes de vie qui rendent le littoral d’Hong Kong unique.
Hong Kong

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.1373
http://journals.openedition.org/etudescaribeennes/1373

Éditeur(s) : Elsevier
Résumé : The study, which is based on repetitive bathymetric surveys, assesses changes and effects of one of the most important floods recorded in the Rhone Delta area: bottom morphology and sediment distribution in the Rhone outlet after the December 2003 flood are discussed by comparison between Digital Terrain maps (DTMs) of November 2003 and January 2004. The post-flood morphology shows that the whole of the system is active, mainly in the east. The channel of the Rhbne has been hollowed out on the left bank by more than 5 m, the eastern coast of the mouth has retreated 400 m, the mouth-bar has prograded 200 m and the slope of the delta front has increased by 0.19. The overlay of pre- and post-flood DTMs makes it possible to estimate the total volume deposited in the [0 to -20 m] zone as +7.8 X 10(6) m(3) (i.e. 0.88 m(3) m(-2)), which corresponds to 4 X 10(6) t of sediment. These values are compared with the average annual volume of 0.47 X 10(6) m(3) yr(-1) of sediment deposited in this zone between 1995 and 2003, as well as the average sediment load estimated at the Arles station (50 km upstream) for this flood event (3.1 x 10(6) t to 5.3 x 10(6) t). The acquisition of bathymetric measurements immediately before and after a major flood allows more than a simple morphological description; in addition, an analysis of the solid load transfer processes towards the prodelta is achievable. Three mechanisms are highlighted. Most of the material eroded in the channel and supplied to the delta front corresponds to fine sediment that drape homogeneously over the pre-flood morphology of the delta front. The transit of the coarsest sediment (primarily sand) is slowed down in the channel of the Rh6ne: this sediment builds up in relatively small areas, leading to the formation of gullies on the prodelta slope. The gullies have fixed positions and disappear gradually towards the west, following the progressive migration of the active band towards the east. These old features are not reactivated by floods occurring after their formation. During the flood, only a small volume of coarse sediment bypasses through the gullies, and the fine deposits are remobilised rapidly or compacted. Flood input concerns essentially the delta front, which traps 90% of the fluvial solid discharge between 0 and 20 m depth. The coarse prodelta supply is then due mainly to mass movements of unconsolidated material deposited beforehand on the top of the delta front. Consequently, the main nourishment of the prodelta does not occur directly during and/or immediately after a flood event, but is delayed by sediment being temporarily trapped on the delta front.
Marine Geology (0025-3227) (Elsevier), 2006-12 , Vol. 234 , N. 1-4 , P. 159-177

Droits : 2006 Elsevier B.V. All rights reserved
http://archimer.ifremer.fr/doc/2006/publication-2304.pdf
DOI:10.1016/j.margeo.2006.09.025
http://archimer.ifremer.fr/doc/00000/2304/

Éditeur(s) : Gauthier-Villars
Résumé : Coastal lagoons have formed where marine inlets or embayments have become partly or wholly enclosed by depositional spits and barriers, built up as a sequel to the world-wide Holocene marine transgression. Spits and barriers consist of sediment (sand, shingle) derived from the sea floor or carrier alongshore from river mouth or eroding cliff sources; they have been shaped primarily by wave action, some migrating landward while others have remained in position or prograded seaward. A modern prevalence of erosion on barrier coastlines, recession resulting from net losses of sediment offshore, alongshore, or landward has been deomonstrated. This is the outcome partly of rising sea level and partly of diminishing sediment supply. Often the consequence of man's impacts on coastal environments. Examples are given of changes that have resulted from the cutting of artificial entrances through barriers to the building of barriers across tidal inlets to exclude marine penetration.
Oceanologica Acta, Special issue (0399-1784) (Gauthier-Villars), 1982

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/00246/35750/34258.pdf
http://archimer.ifremer.fr/doc/00246/35750/

Éditeur(s) : HAL CCSD
Résumé : Water vapour is highly variable in the atmosphere with concentration reaching saturation in the tropics and with dry areas over elevated continental region. Good knowledge of the amount of integrated water vapour in the air is necessary to predict phase changes and in particular precipitation. Water vapour variability measurements are still insufficient with standard observing systems. Moreover accurate GPS antenna positioning is affected by the refractivity index variation in the troposphere. Consequently, vertical positioning component estimation is difficult. This variation is directly linked to distribution of variables such as pressure, temperature and humidity along the path between satellite and receiver. Here we study more specifically heavy rains et notably Cevenols events. This thesis work consists to check the GPS measurement validity to quantify water vapour in comparison with measurements from radiosoundings and meteorological model outputs. GPS observations and flux surface information have been analysed to see if water vapour quantification by GPS allowed characterising heavy rain events (cumulative rainfall amount greater than 150 mm). Then, we tested the GPS data assimilation impact on cumulative precipitation forecasts using the high resolution Meteo France AROME model (2.5 km). Finally the quality and the contribution of GPS measurement on sea is evaluated for water vapour measurement. This study has been realised in the framework of VAPIMED experiment.
La vapeur d'eau varie largement dans l'atmosphère avec des concentrations allant de la saturation dans les tropiques à des zones presque sèches au-dessus des zones continentales élevées. Une bonne connaissance du contenu en vapeur d'eau dans l'air est nécessaire pour la prévision des changements de phases, notamment les précipitations. La mesure de la variabilité de la vapeur d'eau est une lacune des systèmes d'observation. Par ailleurs, il est apparu que le positionnement précis des antennes GPS était affecté par la variation de l'indice de réfraction dans la troposphère, ce qui rend particulièrement difficile l'estimation de la composante verticale. Cette variation est directement liée à la distribution des variables pression, température et humidité sur les trajets satellite-récepteur. On s'intéresse ici à l'étude des précipitations intenses et notamment aux épisodes Cévenols. Ce travail de thèse consiste à vérifier la validité de la mesure GPS pour la quantification de la vapeur d'eau en la comparant avec des mesures issues de radiosondage et des sorties de modèle météorologique. On cherche à analyser si la quantification de vapeur d'eau par GPS permet de caractériser les forts événements précipitants (cumuls supérieurs à 150 mm) à l'aide d'observations conjointes sur les flux de surface. On étudie ensuite l'impact de l'assimilation de données GPS issues d'un réseau GPS dense sur la prévision des cumuls de pluies dans le modèle à hauterésolution (2.5 km) AROME de Météo France. Finalement on évalue la qualité et l'apport de la mesure de vapeur d'eau par GPS en mer dans le cadre d'une campagne de mesure VAPIMED).
https://tel.archives-ouvertes.fr/tel-00444081

Droits : info:eu-repo/semantics/OpenAccess
tel-00444081
https://tel.archives-ouvertes.fr/tel-00444081
https://tel.archives-ouvertes.fr/tel-00444081/document
https://tel.archives-ouvertes.fr/tel-00444081/file/These_KBoniface.pdf

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Ce numéro de la Revue Études Caribéennes s’intéresse aux liens qui unissent et opposent l’activité touristique et les ressources naturelles, particulièrement dans les pays du Sud. Dans un contexte de médiatisation accrue des enjeux liés à la biodiversité et aux menaces qui pèsent sur elle, le tourisme – et particulièrement l’écotourisme – est souvent présenté comme un moyen de concilier la conservation et le développement. Les autorités locales, malgré l’existence d’un cadre réglementaire propre à l’environnement, ne disposent souvent pas de moyens suffisants (humains, matériels et financiers) pour gérer la croissance de la fréquentation des aires protégées et ses effets potentiels sur l’environnement naturel et humain. En réponse à cette problématique, les institutions financières internationales et les organismes associés proposent aux pays du Sud de trouver un équilibre entre une fréquentation de masse et une fréquentation de bas volume afin de développer « un tourisme de haute qualité ». Même si cela était possible, quels critères peuvent être utilisés pour « cesser » le développement d’un pôle ou d’une région touristique ? L’évolution géographique « naturelle » du tourisme – c’est-à-dire essentiellement basée sur la mise en tourisme de la nature et sur l’accessibilité de ces ressources – pose déjà des problèmes politiques et économiques importants. Les gouvernements (central, régional ou local) sont difficilement en mesure de réaliser un arbitrage de long terme dans ce contexte qui permettrait l’adéquation entre le développement touristique et la préservation des espaces naturels. La relation entre le tourisme et les ressources naturelles s’articule souvent autour de deux objectifs spécifiques, soient : développer un produit à moindre impact, mais aux dépenses élevées et viser un volume de visiteurs qui contribue aux profits économiques, mais qui amène le moins de dégradation écologique/sociale possible. Cette position résume à elle seule à la fois la complexité et les multiples paradoxes dans lesquels s’insère la mise en tourisme de la nature. Les dynamiques sociales et l’extension de l’appropriation privative des espaces naturels et agricoles posent la problématique des modes de gestion des ressources communes et de leur pérennité, particulièrement dans les pays du Sud. Dans ce contexte, les objectifs, les ressources et les stratégies des principaux acteurs concernés sont difficilement conciliables et le système de relation qu’il induit n’est pas nécessairement en phase avec les finalités poursuivies. This edition of Revue Etudes Caribéennes focuses on the links that unite and oppose tourism and natural resources, specifically in southern countries. In a context of increased media coverage of issues related to biodiversity (including threats to it), tourism – particularly ecotourism – is often presented as a mean to reconcile conservation and development. Local authorities, despite the existence of a specific environmental regulatory framework, often have insufficient resources (human, material, financial) to manage the increase of visits to protected areas, and the potential impact of these visits on natural and human environments. In response to this problem, international financial institutions and associated organizations offer to try to find a balance between mass attendance and low volume attendance in order to develop "high quality tourism" in southern countries. Even if this were possible, what criteria can be used to "stop" the development of a tourist site or region for environmental reasons? The “natural” geographic evolution of tourism – in other words, essentially based on the development of nature tourism and accessibility of these resources – already causes huge political and economic problems. Governments (central, regional or local) are hardly able to arbitrate over the long term in a context that would allow finding a balance between tourism development and preservation of natural areas. The relationship between tourism and natural resources often revolves around two specific objectives: to develop a product with less impact, but at high cost and a target volume of visitors that contributes to economic profits, but that causes the least ecological / social degradation possible. This position epitomizes both the complexity and the many paradoxes of nature tourism development. Social interactions and the expansion of private appropriation of natural and agricultural areas highlight the challenges of managing common resources and their sustainability, especially in the southern countries. In this context, development objectives, natural resources and the strategies of key stakeholders are difficult to reconcile, and the relationship between leading actors do not always correspond with these objectives. Esta edición de “Revue Études Caribéennes” se interesa a los lazos que unen y separan la actividad turística y los recursos naturales, particularmente en los países del sur. En un contexto de mediatización en alza sobre los objetivos ligados a la biodiversidad y a las amenazas que pesan sobre ella, el turismo – y particularmente el ecoturismo – está a menudo presentado como un medio de conciliar la conservación y el desarrollo. Las autoridades locales, pese a la existencia de un cuadro propio de reglamentación al medio ambiente, no disponen habitualmente de suficientes medios (humanos, materiales y financieros) para controlar el aumento de visitas en las áreas protegidas y sus efectos potenciales sobre el ambiente natural y humano. En respuesta a esta problemática, las instituciones financieras internacionales y los organismos asociados proponen a los países del sur encontrar un equilibrio entre la frecuentación de masas y una frecuentación de bajo volumen con el objetivo de desarrollar “un turismo de alta calidad”. Incluso si fuese posible, ¿qué criterios podrían ser utilizados para “cesar” el desarrollo de un centro o una región turística? La evolución geográfica “natural” del turismo – esencialmente basada en el desarrollo del turismo de la naturaleza y el acceso de sus recursos – crean problemas políticos y económicos enormes. Los gobiernos (central, regional o local) tienen dificultades para realizar un arbitraje a largo plazo en este contexto que permitiría la adecuación entre el desarrollo turístico y la preservación de los espacios naturales. La relación entre el turismo y los recursos naturales se articula a menudo alrededor de dos objetivos específicos, sean: desarrollar un producto con mínimo impacto, pero con gastos elevados y aspirar a un volumen de visitantes que contribuya a las ganancias económicas, pero que traiga la menor degradación ecológica/social posible. Esta posición resume la complejidad y las múltiples paradojas en las cuales se encaja la puesta del turismo en la naturaleza. Las dinámicas sociales y la extensión de la apropiación privativa de los espacios naturales y agrícolas plantean una problemática en los modos de gestión de los recursos comunes y de su perennidad, particularmente en los países del sur. En este contexto, los objetivos, los recursos y las estrategias de los principales actores concernidos son difícilmente conciliables y el sistema de relación que induce no es necesariamente en la misma fase con los objetivos perseguidos.

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.7884
http://journals.openedition.org/etudescaribeennes/7884

Éditeur(s) : HAL CCSD Oxford University Press
Résumé : International audience
Chronic rhinosinusitis (CRS) rank second at chronic inflammatory diseases in industrialized countries and are an important public health concern. Diagnosis relies on a set of arguments including clinical signs, imaging, histopathologic and mycological analyses of sinus specimens, collected during nasal endoscopy. The sensitivity of fungal cultures is reported to be poor, even when direct examination is positive, thus the epidemiology of fungal chronic sinusitis is ill-known. This study evaluated the sensitivity of molecular diagnosis in 70 consecutive samples (61 patients with CRS) analysed at the University Hospital of Rennes during a 3-year period. DNA detection was performed using a conventional PCR method targeting the ITS1/ITS2 sequence and the resulting amplification products were sequenced. Fungal CRS was proven in 42 patients (69%), of which only 20 (48%) had a positive culture. 37/42 (88%) patients were diagnosed with a fungus ball, 3 with allergic fungal CRS and 2 with undetermined fungal CRS. PCR was positive in all 42 cases and direct sequencing allowed to identify fungi in all cases but one, and detected multiple infection in 3. Aspergillus fumigatus was present in 69% of patients; Cladosporium cladosporoides in 9.5%, Scedosporium sp., A. nidulans and A. flavus in 7% each. In 2/19 patients with negative direct examination, sequencing analysis revealed the presence of Capnobotryella sp. and C. cladosporoides, in clinical settings compatible with fungal sinusitis. In conclusion, ITS1/ITS2 PCR had a twice better sensitivity than culture, and combined sequencing provides accurate epidemiological data on fungal CRS.
ISSN: 1369-3786

hal-01383632
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01383632
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01383632/document
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01383632/file/Contribution%20of%20molecular%20tools%20for%20the%20diagnosis.pdf
DOI : 10.1093/mmy/myw041

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
OBJECTIVES: To investigate whether the glutathione S-transferase polymorphisms GSTM1 and/or GSTT1 contribute to prostate cancer risk in a Caribbean population of African descent in Guadeloupe. METHODS: We performed a hospital-based case-control study with 134 prostate cancer patients and 134 cancer-free, age-matched control subjects. Epidemiologic data were collected using a standard questionnaire. Logistic regression was used to estimate odds ratios (ORs) and compute confidence intervals (CIs). Genotypes were determined by multiplex polymerase chain reaction. RESULTS: The frequency of the GSTM1-positive genotype was 81% in patients and 73% in control subjects, with an adjusted OR of 1.4 (95% CI 0.7 to 2.5). The frequency of the GSTT1-positive genotype was 78% in patients and 63% in control subjects, with an adjusted OR of 2.6 (95% CI 1.4 to 4.9). CONCLUSIONS: A functional GSTT1 polymorphism may be associated with prostate cancer susceptibility in a Caribbean population of African descent.
ISSN: 0090-4295

hal-00688449
https://hal.archives-ouvertes.fr/hal-00688449
DOI : 10.1016/j.urology.2007.02.039
PUBMED : 17572208

Éditeur(s) : HAL CCSD Wiley
Résumé : International audience
BACKGROUND: The RH blood group system has many RHCE variant alleles that have arisen through gene conversion or nucleotide changes. Two probands, with red blood cells (RBCs) that were D+C+E-c+(w) e+ were sent to our laboratories to resolve the weak c expression. STUDY DESIGN AND METHODS: Hemagglutination tests were performed by automated and manual procedures. Genomic DNA analysis was performed by sequencing of Exons 1 to 10 of RHCE and RHD. RESULTS: The probands' RBCs did not react with standard monoclonal anti-E reagents from Bio-Rad, Diagast, DiaMed, Immucor, Ortho, and Quotient. The RBCs reacted variably with anti-c reagents from Diagast, DiaMed, Immucor, or Ortho and did not react with the Quotient anti-c reagent. Surprisingly, sequencing results of RHCE showed the presence of C/G at Position 676 (E/e polymorphism) and the association of the E polymorphism with a 734T>C transition in Exon 5 of the RHCE, encoding a Leu245Pro amino acid substitution in the mature RhcE polypeptide. Replacement of leucine 245 by proline in the eighth transmembrane domain of the RhcE protein may have a steric effect on the protein such that most anti-E reagents do not bind and the interaction between anti-c and c antigen is also affected. CONCLUSION: We report a novel RHCE*cE allele, RHCE*cE734C, which was assigned the provisional ISBT allele name RHCE*cE.14 or RHCE*03.14. It was found in two probands whose RBCs had weakened c expression and typed E- with conventional anti-E reagents. These data, once again, highlight the fact that the genotype does not always reflect the phenotype.
ISSN: 0041-1132

hal-00839022
https://hal.archives-ouvertes.fr/hal-00839022
DOI : 10.1111/j.1537-2995.2012.03860.x
PUBMED : 22958092

Éditeur(s) : HAL CCSD Springer International Publishing
Résumé : International audience
This two-volume book set focuses on the Siberian sturgeon. Acipenser baerii Brandt 1869, one of the 27 “existing” sturgeon species, is a native species of the Siberian catchments, where – as in many other parts of the world – the sturgeon populations are now threatened. Sturgeon farming practices targeting caviar and meat production have been expanding worldwide since the 1990s, and have seen a further increase since the turn of the century. Among the handful of sturgeon species used for significant production, the most dominant is the Siberian sturgeon. Given its peculiar phylogenetic position as a chondrostei and its use as a biological model in e.g. France, the species has also attracted the attention of biologists.
The Siberian Sturgeon (Acipenser baerii, Brandt, 1869)

ISBN : 978-3-319-61925-5
hal-01563969
http://hal.upmc.fr/hal-01563969

Résumé : L'étude de la taxonomie des huîtres est longtemps restée basée sur des critères morphologiques (forme de la coquille et description des organes) et géographiques. Ces considérations sont relativement peu fiables en particulier au niveau interspécifique du fait de la plasticité des caractères morphologiques d'une part de des introductions d'espèces étrangères sur les lieux de culture d'autre part. La biologie moléculaire est donc, depuis quelques années, un outil très utilisé pour différencier les espèces d'huîtres. La phylogéographie des huîtres de la région sud-atlantique a ainsi pu être étudiée grâce à différentes méthodes de recherche du polymorphisme réalisées sur le fragment mitochondrial 16S. La PCR-RFLP, la SSCP et le séquençage ont été utilisés pour déterminer les haplotypes de 9 populations d'huîtres creuses du genre Crassostrea provenant du Sénégal, de Guyane, de Martinique et du Brésil. Ceci a permis par extension à d'autres espèces d'apporter des informations complémentaires à la phylogénie de ce genre. Les résultats obtenus par ces 3 méthodes ont permis de montrer que ces 9 populations se différencient en 2 haplotypes : un africain correspondant à l'espèce Crassostrea gasar et un martiniquais correspondant à l'espèce Crassostrea rhizophorae. De plus,C. gasar, huître caractéristique des côtes africaines, est présente dans 2 sites d'Amérique du sud, ont un en sympatrie avec C. rhizophorae au Brésil, ce qui n'a jamais été décrit jusqu'à présent. L'étude d'un point de vue génétique de cette espèce ainsi que la détermination de sa position phylogénétique, sont également une nouveauté. La sympatrie observée au Brésil permet de s'interroger sur l'existence d'une interfécondité possible et d'un flux de gènes entre les 2 espèces. Des études complémentaires à partir d'un échantillonnage plus vaste réalisé sur toute la côte atlantique sud-américaine permettront de confirmer ces résultats. Par ailleurs, la construction d'un arbre phylogénétique à partir des séquences obtenues dans cette étude et de séquences d'autres espèces du même genre, a permis de préciser les positions de ces espèces les unes par rapport aux autres. Ainsi, C. gasar a une position intermédiaire entre les groupes gigas-angulata et virginica-rhizophorae.

Droits : 1999 Univ; La Rochelle, The author
http://archimer.ifremer.fr/doc/00032/14365/11656.pdf
http://archimer.ifremer.fr/doc/00032/14365/

Éditeur(s) : HAL CCSD Public Library of Science
Résumé : International audience
This study, conducted in the brain of a perciform fish, the European sea bass, aimed at raising antibodies against the precursor of the kisspeptins in order to map the kiss systems and to correlate the expression of kisspeptins, kiss1 and kiss2, with that of kisspeptin receptors (kiss-R1 and kiss-R2). Specific antibodies could be raised against the preprokiss2, but not the preoprokiss1. The data indicate that kiss2 neurons are mainly located in the hypothalamus and project widely to the subpallium and pallium, the preoptic region, the thalamus, the pretectal area, the optic tectum, the torus semicircularis, the mediobasal medial and caudal hypothalamus, and the neurohypophysis. These results were compared to the expression of kiss-R1 and kiss-R2 messengers, indicating a very good correlation between the wide distribution of Kiss2-positive fibers and that of kiss-R2 expressing cells. The expression of kiss-R1 messengers was more limited to the habenula, the ventral telencephalon and the proximal pars distalis of the pituitary. Attempts to characterize the phenotype of the numerous cells expressing kiss-R2 showed that neurons expressing tyrosine hydroxylase, neuropeptide Y and neuronal nitric oxide synthase are targets for kisspeptins, while GnRH1 neurons did not appear to express kiss-R1 or kiss-R2 messengers. In addition, a striking result was that all somatostatin-positive neurons expressed-kissR2. These data show that kisspeptins are likely to regulate a wide range of neuronal systems in the brain of teleosts.
ISSN: 1932-6203

hal-00877315
https://hal.archives-ouvertes.fr/hal-00877315
https://hal.archives-ouvertes.fr/hal-00877315/document
https://hal.archives-ouvertes.fr/hal-00877315/file/Expressionsur Kisspeptins-accepted.pdf
DOI : 10.1371/journal.pone.0070177

Éditeur(s) : HAL CCSD Springer Verlag (Germany)
Résumé : International audience
*Context: Tree orientation is controlled by asymmetric mechanical stresses set during wood maturation. The magnitude of maturation stress differs between longitudinal and tangential directions, and between normal and tension woods. * Aims: We aimed at evaluating patterns of maturation stress on eucalypt plantation trees and their relation with growth, with a focus on tangential stress evaluation. * Methods: Released maturation strains along longitudinal and tangential directions were measured around the circumference of 29 Eucalyptus nitens trees, including both straight and leaning trees. * Results: Most trees produced asymmetric patterns of longitudinal maturation strain but more than half of the maturation strain variability occurred between trees. Many trees produced high longitudinal tensile stress all around their circumference. High longitudinal tensile stress was not systematically associated with the presence of gelatinous layer. The average magnitude of released longitudinal maturation strain was found negatively correlated to the growth rate. A methodology is proposed to ensure reliable evaluation of released maturation strain in both longitudinal and tangential directions. Tangential strain evaluated with this method was lower than previously reported. * Conclusion: The stress was always tensile along longitudinal direction and compressive along tangential direction, and their respective magnitude was positively correlated. This correlation does not result from a Poisson effect but may be related to the mechanism of maturation stress generation.
Annals of Forest Science

hal-00913611
https://hal.archives-ouvertes.fr/hal-00913611
https://hal.archives-ouvertes.fr/hal-00913611/document
DOI : 10.1007/s13595-013-0318-4