Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Because many biological processes related to the dynamics of infectious diseases are caused by complex interactions between the environment, the host(s) and the agent(s), the necessity to address the methodological implications of this inherent complexity has recently emerged in epidemiology. Most epidemiologists now acknowledge that most human infectious diseases are likely to have complex dynamics. However, this knowledge still percolates with difficulty in their statistical "modus operandi". Indeed, for the study of complex systems, the traditional first-line statistical toolbox of epidemiologists (mainly built around the Generalized Linear Model family), despite its undeniable practicality and robustness, has structural limitations deprecating its usefulness. Three major sources of complexity neglected or not taken into account by this first-line statistical toolbox and having deep statistical implications are the multi-level organization of data, the non-linear relationships between variables and the complex interactions between variables. Three promising candidates to incorporate along with traditional tools for a new first-line statistical toolbox more suitable to apprehend these sources of complexity are the generalized linear mixed models, the generalized additive models, and the structural equation models. The aforementioned methodologies have the advantage to be generalizations of GLM models and are relatively easy to implement. Their assimilation and implementation would thus be greatly facilitated for epidemiologists. More globally, this text underlines that an improved use of other methods as such described here compared to traditional ones has to be performed to better understand the complexity challenging epidemiologists every day. This is particularly true in the field of infectious diseases for which major public health challenges will have to be addressed in the coming decades.
ISSN: 1567-1348

inserm-00872354
http://www.hal.inserm.fr/inserm-00872354
http://www.hal.inserm.fr/inserm-00872354/document
http://www.hal.inserm.fr/inserm-00872354/file/main_document.pdf
DOI : 10.1016/j.meegid.2013.09.006

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

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

Éditeur(s) : HAL CCSD Springer Verlag/EDP Sciences
Résumé : We characterised the among species variability in leaf gas exchange and morphological traits under controlled conditions of seedlings of 22 tropical rainforest canopy species to understand the origin of the variability in leaf carbon isotope discrimination (Delta) among species with different growth and dynamic characteristics (successional gradient). Our results first suggest that these species pursue a consistent strategy in terms of (Delta) throughout their ontogeny (juveniles grown here versus canopy adult trees from the natural forest). Second, leaf (Delta) was negatively correlated with WUE and N, and positively correlated with gs, but among species differences in (Delta) were mainly explained by differences in WUE. Finally, species belonging to different successional groups display distinct leaf functional and morphological traits. We confirmed that fast growing early successional species maximise carbon assimilation with high stomatal conductance. In contrast, fast and slow growing late successional species are both characterised by low carbon assimilation values, but by distinct stomatal conductance and leaf morphological features. Along the successional gradient, these differences result in much lower (Delta) for the intermediate species (i.e. fast growing late successional) as compared to the two other groups.
ISSN: 1286-4560

hal-01032038
https://hal.archives-ouvertes.fr/hal-01032038
DOI : 10.1051/forest:2006101

Éditeur(s) : HAL CCSD AGU and the Geochemical Society
Résumé : International audience
The ODP/IODP multileg campaign at ODP Site 1256 (Cocos plate, eastern equatorial Pacific) provides the first continuous in situ sampling of fast spreading ocean crust from the extrusive lavas, through the sheeted dikes and down into the uppermost gabbros. This paper focuses on a detailed petrographic and microanalytical investigation of the gabbro section drilled during IODP Expedition 312. The marked patchy and spotty features that can be observed in many Hole 1256D gabbros is mostly due to a close association of two different lithological domains in variable amounts: (1) subophitic domains and (2) a granular matrix. Major and trace element mineral compositions, geothermometry, and petrological modeling suggest that subophitic and granular domains follow one single magma evolution trend formed by in situ fractionation. The subophitic domains correspond to the relative primitive, high-temperature end-member, compositionally similar to the basalts and dikes from the extrusive unit upsection, while the granular domains fit with a magma evolution by crystal fractionation to lower temperatures, up to a degree of crystallization of similar to 80%. Our results support the following scenario for the fossilization of the axial melt lens at ODP Site 1256: relatively primitive MORB melts under near-liquidus conditions fill the melt lens and feed the upper, extrusive crust. Near the melt lens-sheeted dike boundary at lower temperatures, crystallization starts with first plagioclase before clinopyroxene in a mushy zone forming the subophitic domains. At decreasing temperatures, the subophitic domains continue to crystallize, finally forming a well-connected framework. Evolved, residual melt is finally trapped within the subophitic network, crystallizing at near-solidus conditions to the granular matrix. Another important textural feature in Hole 1256D gabbros is the presence of microgranular domains which are interpreted as relics of stoped/assimilated sheeted dikes (transformed to "granoblastic dikes" by contact metamorphism). All these different domains can be observed in close association, often at the thin section scale, demonstrating the extremely complex petrological record of combined crystallization/assimilation processes ongoing in the axial melt lens. Very similar gabbros with a marked spotty/patchy appearance, and bearing the same close association of lithological domains as observed at Site 1256, are known in the so-called "varitextured gabbro" unit from the Oman Ophiolite located at the same structural level, between cumulate gabbros and granoblastic dikes. The close petrological similarity of the gabbro/dike transition between both IODP Hole 1256D and the Oman ophiolite suggests that in situ fractionation and dike assimilation/contamination are major magmatic processes controlling the dynamics and fossilization of the axial melt lens at fast spreading oceanic ridges.
ISSN: 1525-2027

hal-00644798
https://hal.archives-ouvertes.fr/hal-00644798
DOI : 10.1029/2011GC003655

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : L’article examine l’existence précaire des Aloukous de Guyane, descendants d’esclaves marrons. L’étude est basée sur le roman de Roland Brival, Le dernier des Aloukous, un des rares écrivains qui a rendu hommage à ce peuple oublié de l’Histoire et menacé par la modernisation et l’assimilation. Il examine aussi les problématiques de la déforestation, de la déterritorialisation ainsi que l’importance des rituels et des dieux dans la culture des Aloukous.
The article examines the precarious existence of the Alukus, a population based in Guyana, and the descendants of maroons slaves. The study is based on a novel by Roland Brival, one of the few writers from the French Caribbean who has paid a tribute to this ethnic group threatened by modernization and urbanization. It also examines issues of deforestation, deterritorialization, and the importance of rituals and gods in the Alukus' culture.
Guyane française

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.4932
http://journals.openedition.org/etudescaribeennes/4932

Éditeur(s) : HAL CCSD
Résumé :   Diffusion du document : INRA Antilles-Guyane, Documentation, Domaine de Duclos, 97170 Petit-Bourg, Guadeloupe (France) Diplôme : DEA
il s'agit d'un type de produit dont les métadonnées ne correspondent pas aux métadonnées attendues dans les autres types de produit : DISSERTATION
L'objectif de ce travail était d'étudier la plasticité des traits fonctionnels relatifs à la photosynthèse en fonction du type de sol chez Eperua falcata, une espèce forestière de Guyane française. Les individus ont été échantillonnés sur deux sols contrastés : sol de bas-fond (Gleysol) à fort hydromorphisme, et sol de crête (Ferralsol) à drainage vertical libre. Le micro climat lumineux a été quantifié au-dessus de chaque individu. Les capacités photosynthétiques (vitesse maximale de carboxylation du RuBP, Vcmax, et flux maximal d'électrons photosynthétiques, Jmax) ont été estimées en ajustant un modèle biochimique de photosynthèse foliaire (Farquhar et al. 1980), sur des courbes de réponse de l'assimilation nette du C02 en fonction de la concentration interne en CO2, sous fort éclairement (courbe A-Ci). Les résultats obtenus ont montré un effet du type de sol sur les capacités photosynthétiques foliaires et que celles-ci étaient plutôt liées à des modifications des allocations d'azote aux processus de carboxylation Pc et à la bioénergétique Pb plutôt qu'à des changements structuraux foliaires. Les résultats ont également mis en évidence des différentiels dans les seuils de sensibilité à la lumière selon le type de trait foliaire avec, grande sensibilité à de faibles variations du micro climat lumineux pour les capacités de photosynthèse et une absence de sensibilité à ces mêmes variations pour les traits structuraux.
https://hal.archives-ouvertes.fr/hal-01189269

hal-01189269
https://hal.archives-ouvertes.fr/hal-01189269
PRODINRA : 21921

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Deposit feeders are able to process a considerable volume of sediment, containing large 9 quantities of associated bacteria. However, conclusions concerning the trophic role played by 10 benthic bacteria in marine sediments are still not fully elucidated. This study deals with 11 bacterivory by the gastropod Hydrobia ulvae, one of the most abundant deposit-feeding 12 species in intertidal mudflats in Western Europe. Ingestion rates of bacteria were determined 13 during grazing experiments using 15 N pre-enriched bacteria. Grazing experiments were 14 performed in order to measure effects of abiotic (temperature, salinity and luminosity) and 15 biotic (bacterial and algal abundances) factors on ingestion rates of bacteria by H. ulvae of an 16 intertidal mudflat (Brouage, Marennes-Oléron, France). The mean ingestion rate of bacteria 17 by H. ulvae was 1149 ngC ind-1 h-1. The general trend showed a temperature effect with an 18 optimum around 30°C, and the assimilation rate was significantly lower at 5°C. Bacterial 19 assimilation did not significantly differ between salinity 18 and salinity 31. Ingestion was the 20 same in light and in dark conditions. Results were compared with those of other grazing 21 experiments conducted simultaneously in similar conditions with two other grazers with 22 different size and feeding modes: the foraminifera Ammonia tepida and a nematode 23 community from the superficial sediment of the Brouage mudflat. Hydrobia ulvae and 24 nematodes presented a feeding behavior less influenced by environmental changes than A. tepida. Hydrobia ulvae ingested bacteria at a higher rate than smaller meiofaunal grazers and seemed to have a lower ability to selectively ingest diatoms than meiofaunal grazers.
ISSN: 1385-1101

hal-01248039
https://hal.archives-ouvertes.fr/hal-01248039
https://hal.archives-ouvertes.fr/hal-01248039/document
https://hal.archives-ouvertes.fr/hal-01248039/file/Pascal%20et%20al%202008.pdf
DOI : 10.1016/j.seares.2008.05.003

Éditeur(s) : HAL CCSD AGU and the Geochemical Society
Résumé : Mid-ocean ridges magmatism is, by and large, considered to be mostly dry. Nevertheless, numerous works in the last decade have shown that a hydrous component is likely to be involved in ocean ridges magmas genesis and/or evolution. The petrology and geochemistry of peculiar coarse grained gabbros sampled in the upper part of the gabbroic sequence from the northern Oman ophiolite (Wadi Rajmi) provide information on the origin and fate of hydrous melts in fast-spreading oceanic settings. Uncommon crystallization sequences for oceanic settings (clinopyroxene crystallizing before plagioclase), extreme mineral compositions (plagioclase An% up to 99, and clinopyroxene Mg # up to 96), and the presence of magmatic amphibole, imply the presence of a high water activity during crystallization. Various petrological and geochemical constraints point to hydration, resulting from the recycling of hydrothermal fluids. This recycling event may have occurred at the top of the axial magma chamber where assimilation of anatectic hydrous melts is recurrent along mid-ocean ridges or close to segments ends where fresh magma intrudes previously hydrothermally altered crust. In ophiolitic settings, hydration and remelting of hydrothermally altered rocks producing hydrous melts may also occur during the obduction process. Although dry magmatism dominates oceanic magmatism, the dynamic behavior of fast-spreading ocean ridge magma chambers has the potential to produce the observed hydrous melts (either in ophiolites or at spreading centers), which are thus part of the general mid-ocean ridges lineage.
ISSN: 1525-2027

hal-00939400
https://hal.archives-ouvertes.fr/hal-00939400
DOI : 10.1002/ggge.20137

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Volumetrically minor microsyenites, alkali microgranite and related trachytic dykes intrude early Pliocene OIB-like alkali basaltic and basanitic flows of the Meseta del Lago Buenos Aires in Central Patagonia (47 degrees S-71 degrees 30'W), and occur together with scarce trachytic lava flows. Whole-rock K-Ar ages between 3.98 and 3.08 Ma indicate that the emplacement of these felsic rocks occurred more or less synchronously with that of the post-plateau basaltic sequence that they intrude, during a bimodal mafic-felsic magmatic episode devoid of intermediate compositions. Chemically, these rocks have A(1)-type granitoid affinities and are characterized by high silica and alkali contents (60-68 wt.% SiO2; 8.7-10.8 wt.% Na2O+K2O), major and trace elements patterns evidencing evolution by low-pressure fractional crystallization, and Sr and Nd isotopic signatures similar to those of coeval basalts ((Sr-87/Sr-86)o=0.70488-0.70571; (Nd-143/Nd-144)(o)=0.512603-0.512645). Nevertheless, some of them have the most radiogenic Sr values ever reported for a magmatic rock in the Meseta and even in the whole Neogene Patagonian Plateau Lavas province ((Sr-17/Sr-86)(o)= 0.70556-0.70571; (Nd-143/Nd-144)(o)=0.512603-0.512608). In addition, very high contents of strongly incompatible elements in the most evolved rocks, together with Sr isotopic ratios higher than those of coeval basalts, suggest the occurrence of open-system magmatic processes. Continuous fractional crystallization from a primitive basaltic source, similar to post-plateau coeval basalts, towards alkali granites combined with small rates of assimilation of host Jurassic tuffs (AFC) in a shallow magmatic reservoir, best explains the geochemical and petrographic features of the felsic rocks. Therefore, A(1)-type magmatic rocks can be generated by open-system crystallization of deep asthenospheric melts in back-are tectonic settings. In Central Patagonia, these similar to 3-4 Ma old alkaline intrusions occur aligned along a similar to N160-170 trending lineament, the Zeballos Fault Zone, stacking the morphotectonic front of one segment of the Patagonian Cordillera. Intrusion along this fault zone
ISSN: 0024-4937

hal-00412030
https://hal.archives-ouvertes.fr/hal-00412030
DOI : 10.1016/j.lithos.2007.07.002

Résumé : Évoquer la place des libres de couleur en Martinique des origines à 1815, c'est évoqué un curieux paradoxe. Afin d'appréhender ce dernier et aborder la position des libres de couleur dans la société, il a fallu se pencher sur le processus de formation de ce groupe de 1635 à la veille de la Révolution française, en mettant en lumière l'origine de celui-ci, le statut, la condition des personnes, la répartition géographique, la situation socioéconomique et les réseaux de sociabilité qu'ils utilisent dans la société. L'abord de ce processus ne pouvait se faire sans la prise en compte de la politique menée par l'administration envers l'affranchissement. L'utilisation des registres paroissiaux (puis de l'état civil) et du notariat a permis la confrontation entre la théorie (le droit colonial), et, la pratique quotidienne. Il a fallu ensuite mettre en évidence dans un second temps comment, malgré la Révolution française et de ses idéaux, de son impact en Martinique, la ségrégation perdure à l'encontre du groupe des libres de couleur et confirme l'entre-deux de celui-ci dans la société, en dépit de son accroissement numérique (via l'affranchissement principalement) et économique, et ce, jusqu'au début de la Restauration. La politique coloniale menée par les différentes administrations qui se succèdent et les troubles qui perturbent l'ordre établi ont favorisé la compréhension du phénomène. Si, les libres de couleur furent assimilés dès 1685 aux sujets naturels du royaume de France, ils ne purent pourtant exercer comme les Blancs, certaines charges publiques, certaines professions libérales, certains emplois dans la milice (officiers). Cependant, certains d'entre eux réussirent à se hisser économiquement au niveau des négociants blancs avant 1815. Néanmoins, ils demeurèrent cantonnés dans une place mitoyenne entre Blancs et esclaves, une "zone tampon", un entre-deux discriminatoire et ségrégatif. Ces libres de couleur qui étaient aussi bien des noirs que des métis furent rejetés par les Blancs qu'ils souhaitaient égaler et méprisaient en général les esclaves alors qu'ils étaient souvent liés à eux par un ancêtre noir. Comme les Blancs, ils possédaient des esclaves, des terres et des maisons. Pourtant, leur situation dans la société fut très paradoxale.
To evoke the place of free coloureds in Martinic from the earliest times to 1815, it is evoked a curious paradox. In order to apprehend this last and to tackle free coloureds position in the society, it had to look into the process of development of this group from 1635 to the day before french revolution. The access of this process could not become without taking into consideration of the political controlled by the administration on emancipation. The utilization of parish registers (then registers of births, marriages and deaths) and deeds executed by a notary permitted confrontation between the theory (the colonial right) and the daily practical. It had to show how in spite of french revolution and these ideals, and this impact in Martinic, the segregation be continued against free coloureds group and confirmed space in between of this group in the society in spite of these numerical and economic growth (by way of emancipation principally), and those, as far as the beginning of the Restoration. The colonial political controlled by different administrations who followed one another and unrest who perturbed etablished order assisted the comprehension of this phenomenon. If free coloureds were assimilated since 1685 to natural subjects of french kingdom with the same rights, privileges and immunities, they did not exercise as whites some public responsabilities and offices, some liberal trades, some positions in militia (officers). Before the end of observation period (1815), some people were succeded to hoist themselves economically on a level with whites wholesalers. In spite of that, they were limited in a intermediate place between whites and slaves, a "buffer zone". Free coloureds who were as well as blacks than halfcastes have been rejected by whites that they would wish to equal and despised in general slaves even when they had common interests (a mother or a sister in slavery). As whites, they possessed slaves, estates and houses. However, their situation was so paradoxical in the colonial society.

http://www.theses.fr/2011AGUY0395/document

Éditeur(s) : HAL CCSD
Résumé : La Guyane présente une situation linguistique et culturelle exceptionnelle, non pas tant en raison du plurilinguisme qui la caractérise (celui-ci est omniprésent dans le monde) mais de la configuration de ce plurilinguisme, notamment en contexte scolaire : allophonie d'élèves étrangers mais aussi d'élèves français, grande diversité linguistique, écart culturel important entre le monde de l'école et celui de l'environnement familial et quotidien. Cette diversité linguistique et culturelle de l'école en Guyane constitue donc un enjeu essentiel pour une région qui, en tant que département français, est difficilement assimilable aux " pays du Sud ", mais qui pourtant en présente de nombreuses caractéristiques de part son, histoire coloniale . Face à cette situation, l'école française centralisatrice se doit donc d'envisager une transformation de son système éducatif, afin de mieux l'adapter au public qu'elle accueille. Cette transformation peut porter sur différents niveaux : programmes, formation des enseignants, etc. Toutefois elle se heurte à la conception du système éducatif par des décideurs, qui s'appuient sur une réalité fantasmée, une vision holistique de l'éducation en France. De surcroît, l'appartenance de la France au contexte européen suppose une prise en compte des directives élaborées à ce niveau. Aussi, la Guyane est-elle face à un enjeu majeur : celui d'une nécessaire réinterprétation des contenus, des méthodes d'enseignement, et même des principes qui gouvernent cet enseignement. Ses acteurs ne peuvent toutefois agir qu'en se basant sur les textes officiels qui régissent le système éducatif. Comment dans un tel contexte, et face à de tels enjeux, résoudre le paradoxe que constitue une école française dans un département d'Outre-Mer, situé en Amérique du Sud ? C'est à cette question que nous tenterons de répondre en décrivant, dans un premier temps, les caractéristiques de ce contexte éducatif, l'inadaptation des décisions de l'état en matière éducative. Cette description s'appuiera sur des analyses de documents, et sera exemplifiée par des études de cas issus de différents espaces éducatifs de la région. Nous chercherons ensuite à déterminer quels sont les éléments d'adaptation essentiels, en émettant des propositions en termes de contenus d'enseignement, de profil des enseignants et de formation de ces derniers.
Raisons Educatives

halshs-00665368
https://halshs.archives-ouvertes.fr/halshs-00665368
https://halshs.archives-ouvertes.fr/halshs-00665368/document
https://halshs.archives-ouvertes.fr/halshs-00665368/file/raisons_A_ducatives.pdf

Éditeur(s) : Elsevier
Résumé : The uptake and loss kinetics of Cd were determined in two species of scallops from the European coasts, the variegated scallop Chlamys varia and the king scallop Pecten maximus, following exposures via seawater, phytoplankton and sediment using highly sensitive radiotracer techniques (Cd-109). Results indicate that, for seawater and dietary pathways, C. varia displays higher bioaccumulation capacities in terms of uptake rate from water and fraction absorbed from ingested food (assimilation efficiency) than Pecten maximus. Regarding sediment exposure, P. maximus displayed low steady-state Cd transfer factor (TFSS < 1); however, once incorporated, a very large part of Cd transferred from sediment (92%) was strongly retained within R maximus tissues. Both species showed a high retention capacity for Cd (biological half-life, T-b1/2 > 4 months), suggesting efficient mechanisms of detoxification and storage in both species. The digestive gland was found to be the main storage organ of Cd in the two scallops regardless of the exposure pathway. However, Cd was stored differently within this organ according to the species considered: 40% of the total Cd was found in the soluble cellular fraction in C. varia whereas this soluble fraction reached 80% for P. maximus. This suggests that the two species displayed different Cd detoxification/storage mechanisms. Finally, the present study has determined the relative contribution of the different exposure pathways to global Cd bioaccumulation for the two scallop species. Results clearly show that for both species, food constitutes the major accumulation pathway, contributing for >99% and 84% of the global Cd bioaccumulation in C. varia and R maximus, respectively. This work confirms the previous assumption, derived from a bibliographic overview, that dietary pathway plays a prevalent role in metal bioaccumulation in Pectinidae. (C) 2007 Elsevier B.V. All rights reserved.
Journal of Experimental Marine Biology and Ecology (0022-0981) (Elsevier), 2007-12 , Vol. 353 , N. 1 , P. 58-67

Droits : 2007 Elsevier B.V. All rights reserved.
http://archimer.ifremer.fr/doc/2007/publication-3581.pdf
DOI:10.1016/j.jembe.2007.09.001
http://archimer.ifremer.fr/doc/00000/3581/

Éditeur(s) : HAL CCSD Springer Verlag
Résumé :  
Genetic variation for intrinsic water use efficiency (W i) and related traits was estimated in a full-sib family of Quercus robur L. over 3 years. The genetic linkage map available for this F1 family was used to locate quantitative trait loci (QTL) for W i, as estimated by leaf carbon stable isotope composition (δ 13C) or the ratio of net CO2 assimilation rate (A) to stomatal conductance to water vapour (g w) and related leaf traits. Gas exchange measurements were used to standardize estimates of A and g w and to model the sensitivity of g w to leaf-to-air vapour pressure deficit (sgVPD). δ 13C varied by more than 3‰ among the siblings, which is equivalent to 40% variation of W i. Most of the studied traits exhibited high clonal mean repeatabilities (>50%; proportion of clonal mean variability in global variance). Repeatabilities for δ 13C, leaf mass per area (LMA) and leaf nitrogen content were higher than 70%. For δ 13C, ten QTLs were detected, one of which was detected repeatedly for all 3 years and consistently explained more than 20% of measured variance. Four genomic regions were found in which co-localizing traits linked variation in W i to variations in leaf chlorophyll and nitrogen content, LMA and sgVPD. A positive correlation using clonal means between δ 13C and A/g w, as well as a co-localisation of QTL detected for both traits, can be seen as validation of the theoretical model linking the genetic architecture of these two traits.
ISSN: 1614-2942

hal-01032066
https://hal.archives-ouvertes.fr/hal-01032066
DOI : 10.1007/s11295-007-0107-z

Éditeur(s) : HAL CCSD European Geosciences Union
Résumé : International audience
The exchanges of carbon, water and energy between the atmosphere and the Amazon basin have global implications for the current and future climate. Here, the global atmospheric inversion system of the Monitoring of Atmospheric Composition and Climate (MACC) service is used to study the seasonal and interannual variations of biogenic CO 2 fluxes in Amazonia during the period 2002–2010. The system assimilated surface measurements of atmospheric CO 2 mole fractions made at more than 100 sites over the globe into an atmospheric transport model. The present study adds measurements from four surface stations located in tropical South America, a region poorly covered by CO 2 observations. The estimates of net ecosystem exchange (NEE) optimized by the inversion are compared to an independent estimate of NEE upscaled from eddy-covariance flux measurements in Amazonia. They are also qualitatively evaluated against reports on the seasonal and interannual variations of the land sink in South America from the scientific literature. We attempt at assessing the impact on NEE of the strong droughts in 2005 and 2010 (due to severe and longer-than-usual dry seasons) and the extreme rainfall conditions registered in 2009. The spatial variations of the seasonal and in-terannual variability of optimized NEE are also investigated. While the inversion supports the assumption of strong spatial heterogeneity of these variations, the results reveal critical limitations of the coarse-resolution transport model, the surface observation network in South America during the recent years and the present knowledge of modelling uncertainties in South America that prevent our inversion from capturing the seasonal patterns of fluxes across Amazonia. However, some patterns from the inversion seem consistent with the anomaly of moisture conditions in 2009.
ISSN: 1680-7316

hal-01557375
https://hal.univ-lorraine.fr/hal-01557375
https://hal.univ-lorraine.fr/hal-01557375/document
https://hal.univ-lorraine.fr/hal-01557375/file/acp-15-8423-2015.pdf
DOI : 10.5194/acp-15-8423-2015-supplement

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
We present new Sr-Nd-Pb isotope data of the western Alpujárride metamorphic basement and the pre-Miocene Flysch sediments of the Betic Cordillera (southern Spain). Nd model ages are consistent with an increasing detrital input from the Alborán domain to the Flysch Trough in the western Mediterranean during the late Oligocene. The Alpujárride metamorphic crustal rocks derived from Archean-Paleoproterozoic terranes located along the northern margin of Gondwana in the Neoproterozoic. The heterogeneous isotopic signatures of the Alpujárride units indicate that they have different sedimentary protoliths and underwent contrasted Variscan and pre-Variscan tectono-magmatic evolutions. Melts/fluids derived from the western Alpujárride gneisses contaminated the mantle source of the Ronda high-Mg pyroxenite dykes, implying that the Alpujárride lower crust underthrusted the subcontinental lithospheric mantle of the Alborán domain generating subduction-like magmatism in the late Oligocene. The western Alpujárride upper crust is involved in the Neogene volcanism of the Alborán Sea basin, but only contaminated some LREE-enriched calc-alkaline lavas erupted along the continental margins. On the other hand, tholeiitic lavas in the center of the basin show no isotopic evidence of crustal assimilation. This indicates that most of the crust in the central Alborán Sea accreted by Miocene tholeiitic magmatism and that Alpujárride lower crust is absent and likely foundered close to the continental margins of the basin.
ISSN: 0024-4937

hal-01526912
https://hal.archives-ouvertes.fr/hal-01526912
DOI : 10.1016/j.lithos.2016.10.003

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Over the last two decades, climate change has become a major environmental and public health concern due to the increase of the mean temperature on the Earth and its consequences on extreme meteorological events such as floods and droughts. These events induce very low or very high river flows that may impair surface water quality, and therefore result in potential health impacts when used for drinking water production. The present study aims at assessing the impact of hydrologic regime on surface water quality with a particular emphasis on total organic carbon (TOC) and nitrate. Water quality data from three French rivers acquired over a 27 years period, from January 1983 to December 2009, show the influence of extreme flows. Variation in TOC and nitrate concentrations showed opposite patterns for the whole range of flow rate (from less than 10% up to more than 100% of the mean flow). Regarding fluxes, TOC increased continuously with flow rate while nitrate was stable for very high discharges. The C/N ratio expressed from TOC and nitrate concentrations showed high values for extreme flows and particularly for very low flow rates, generally in summer, where nitrate is assimilated by biomass. Considering TOC and nitrate fluxes, it is confirmed that the worst situations were encountered for very high flow rates, namely for TOC exportation during surface runoff which was related to heavy rains or floods. These findings are of great importance with regard to the adaptation for drinking water treatment in facing extreme hydrological conditions, of which the frequency is increasing with climate change.
ISSN: 0022-1694

hal-00878009
https://hal.archives-ouvertes.fr/hal-00878009
DOI : 10.1016/j.jhydrol.2012.11.006

Résumé : L'ouvrage que Verger (1968) a consacré au littoral français en général et au Bassin de Marennes-Oléron en particulier est certainement le plus important document dont nous disposons dans le domaine morpho-sédimentaire. Dans cette étude, l'auteur assimile le littoral charentais aux Wadden de Hollande : cette comparaison est cependant discutable, suivant les arguments développés ci-après qui montrent les principales différences entre vasières littorales charentaises et waddens hollandais.

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/00082/19306/16900.pdf
http://archimer.ifremer.fr/doc/00082/19306/

Éditeur(s) : HAL CCSD Springer
Résumé : International audience
Thiswork examines the relevance of the inclusion of ground-based gravity data in the calibration process of a global rainfall-discharge reservoir model. The analysis is performed for the Durzon karst system (Larzac, France). The first part of the study focuses on the hydrological interpretation of the ground-based gravity measurements. The second part of the study investigates further the information content of the gravity data with respect to water storage dynamics modelling.The gravity-derived information is found unable to either reduce equifinality of the single-objective, dischargebased model calibration process or enhance model performance through assimilation.
ISSN: 1866-6280

hal-00812624
https://hal-brgm.archives-ouvertes.fr/hal-00812624
DOI : 10.1007/s12665-012-1856-z

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
IODP Hole U1309D (Atlantis Massif, Mid-Atlantic Ridge 30 degrees N) is the second deepest hole drilled into slow spread gabbroic lithosphere. It comprises 5.4% of olivine-rich troctolites (->70% olivine), possibly the most primitive gabbroic rocks ever drilled at mid-ocean ridges. We present the result of an in situ trace element study carried out on a series of olivine-rich troctolites, and neighbouring troctolites and gabbros, from olivine-rich intervals in Hole U1309D. Olivine-rich troctolites display poilkilitic textures; coarse-grained subhedral to medium-grained rounded olivine crystals are included into large undeformed clinopyroxene and plagioclase poikiloblasts. In contrast, gabbros and troctolites have irregularly seriate textures, with highly variable grain sizes, and locally poikilitic clinopyroxene oikocrysts in troctolites. Clinopyroxene is high Mg# augite (Mg# 87 in olivine-rich troctolites to 82 in gabbros), and plagioclase has anorthite contents ranging from 77 in olivine-rich troctolites to 68 in gabbros. Olivine has high forsterite contents (82-88 in olivine-rich troctolites, to 78-83 in gabbros) and is in Mg-Fe equilibrium with clinopyroxene. Clinopyroxene cores and plagioclase are depleted in trace elements (e.g., Yb-cpx similar to 5-11 x Chondrite), they are in equilibrium with the same MORB-type melt in all studied rock-types. These compositions are not consistent with the progressively more trace element enriched (evolved) compositions expected from olivine rich primitive products to gabbros in a MORB cumulate sequence. They indicate that clinopyroxene and plagioclase crystallized concurrently, after melts having the same trace element composition, consistent with crystallization in an open system with a buffered magma composition. The slight trace element enrichments and lower Cr contents observed in clinopyroxene rims and interstitial grains results from crystallization of late-stage differentiated melts, probably indicating the closure of the magmatic system. In contrast to clinopyroxene and plagioclase, olivine is not in equilibrium with MORB, but with a highly fractionated depleted melt, similar to that in equilibrium with refractory oceanic peridotites, thus possibly indicating a mantle origin. In addition, textural relationships suggest that olivine was in part assimilated by the basaltic melts after which clinopyroxene and plagioclase crystallized (impregnation). These observations suggest a complex crystallization history in an open system involving impregnation by MORB-type melt(s) of an olivine-rich rock or mush. The documented magmatic processes suggest that olivine-rich troctolites were formed in a zone with large magmatic transfer and accumulation, similar to the mantle-crust transition zone documented in ophiolites and at fast spreading ridges.
ISSN: 0009-2541

hal-00420916
https://hal.archives-ouvertes.fr/hal-00420916
DOI : 10.1016/j.chemgeo.2009.02.013

Éditeur(s) : HAL CCSD Oxford University Press (OUP)
Résumé : In this paper we present the potential of a new compact superconducting gravimeter (GWR iGrav) designed for groundwater monitoring. At first, 3 yr of continuous gravity data are evaluated and the performance of the instrument is investigated. With repeated absolute gravity measurements using a Micro-g Lacoste FG5, the calibration factor (−894.8 nm s−2 V−1) and the long-term drift of this instrument (45 nm s−2 yr−1) are estimated for the first time with a high precision and found to be respectively constant and linear for this particular iGrav. The low noise level performance is found similar to those of previous superconducting gravimeters and leads to gravity residuals coherent with local hydrology. The iGrav is located in a fully instrumented hydrogeophysical observatory on the Durzon karstic basin (Larzac plateau, south of France). Rain gauges and a flux tower (evapo-transpiration measurements) are used to evaluate the groundwater mass balance at the local scale. Water mass balance demonstrates that the karst is only capacitive: all the rainwater is temporarily stored in the matrix and fast transfers to the spring through fractures are insignificant in this area. Moreover, the upper part of the karst around the observatory appears to be representative of slow transfer of the whole catchment. Indeed, slow transfer estimated on the site fully supports the low-flow discharge at the only spring which represents all groundwater outflows from the catchment. In the last part of the paper, reservoir models are used to characterize the water transfer and storage processes. Particular highlights are done on the advantages of continuous gravity data (compared to repeated campaigns) and on the importance of local accurate meteorological data to limit misinterpretation of the gravity observations. The results are complementary with previous studies at the basin scale and show a clear potential for continuous gravity time-series assimilation in hydrological simulations, even on heterogeneous karstic systems.
ISSN: 0956-540X

hal-01526965
https://hal.archives-ouvertes.fr/hal-01526965
https://hal.archives-ouvertes.fr/hal-01526965/document
https://hal.archives-ouvertes.fr/hal-01526965/file/fores2016.pdf
DOI : 10.1093/gji/ggw396