Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
BACKGROUND & AIMS: Nutrients influence non-alcoholic fatty liver disease. Essential fatty acids deficiency promotes various syndromes, including hepatic steatosis, through increased de novo lipogenesis. The mechanisms underlying such increased lipogenic response remain unidentified. METHODS: We used wild type mice and mice lacking Liver X Receptors to perform a nutrigenomic study that aimed at examining the role of these transcription factors. RESULTS: We showed that, in the absence of Liver X Receptors, essential fatty acids deficiency does not promote steatosis. Consistent with this, Liver X Receptors are required for the elevated expression of genes involved in lipogenesis in response to essential fatty acids deficiency. CONCLUSIONS: This work identifies, for the first time, the central role of Liver X Receptors in steatosis induced by essential fatty acids deficiency.
ISSN: 0168-8278

inserm-00872314
http://www.hal.inserm.fr/inserm-00872314
DOI : 10.1016/j.jhep.2013.01.006
PUBMED : 23333450

Éditeur(s) : HAL CCSD Wiley-Blackwell
Résumé : International audience
Search String Advanced > Saved Searches >ARTICLE TOOLS Get PDF (3653K) Save to My Profile E-mail Link to this Article Export Citation for this Article Get Citation Alerts Request PermissionsMore Sharing ServicesShare|Share on citeulikeShare on facebookShare on deliciousShare on www.mendeley.comShare on twitter Abstract Article References Cited ByView Full Article (HTML) Enhanced Article (HTML) Get PDF (3653K)AbstractFor the first time, the crystallized remnant of an oceanic ridge magma chamber is documented in the Oman ophiolite. It exists in the centre of a 40 km long monoclinal ridge (Jebel Dihm, Wadi Tayin massif), exposing a full crustal section perpendicular to the spreading direction. New detailed mapping supported by U-Pb zircon geochronology suggests that the active, fast-spreading ridge that died just prior to detachment of the ophiolite is preserved and largely intact. Our observations provide insights into the crystallizing mush zone of a magma chamber, before it crosses the external walls and solidifies as deformed gabbros. Our data provide new constraints on the shape and internal dynamics of a magma chamber, including gabbro subsidence from the floor of a perched melt lens and the limited contribution of sills to crustal accretion. By locating precisely the palaeo-ridge axis, prior full spreading rate estimates can be increased to ~140 km Ma−1.
ISSN: 0954-4879

hal-01121586
https://hal.archives-ouvertes.fr/hal-01121586
DOI : 10.1111/ter.12130

Éditeur(s) : HAL CCSD
Résumé : International audience
L’agrotourisme, entre identité et développement : éclairages méditerranéens et insulaires
Corte, France

hal-01634312
https://hal.archives-ouvertes.fr/hal-01634312

Éditeur(s) : HAL CCSD
Résumé : National audience
Les flux sédimentaires dans les bassins d'avant-pays dépendent de l'activité érosive des rivières qui drainent en amont les chaînes de montagnes. Les variations du flux sédimentaire sont généralement attribuées à des variations de l'activité érosive en réponse à la tectonique ou aux changements climatiques. À l'aide d'un dispositif expérimental nous étudions les interactions entre la déformation, la pluviométrie et le comportement intrinsèque d'un système géomorphologique que constitue un prisme orogénique soumis à l'érosion. Nous montrons que le réseau de drainage dans un tel prisme évolue toujours depuis un réseau dominé par des drains longitudinaux (parallèles aux structures tectoniques) vers un réseau dominé par des drains transversaux. Au cours de cette réorganisation, les captures de drains longitudinaux par les drains transversaux provoquent des modifications des pentes locales et des flux d'eau. Ces captures entraînent une augmentation subite de la vitesse d'érosion des drains transversaux provoquant celle-là même du flux de sédiment à la sortie du prisme (figure 1), alors que la vitesse de raccourcissement et la pluviométrie sont restées constantes. L'analyse de systèmes naturels montre que cette réorganisation progressive du système de drainage semble être une conséquence inéluctable de la croissance des chaînes de montagnes (Babault et al 2012). On doit par conséquent s'attendre à ce que le flux sédimentaire dans les chaînes soit contrôlé, non seulement par la tectonique et/ou le climat, mais aussi par la dynamique du réseau de drainage.
14 ème congrès français de sédimentologie, Paris, 4-8 novembre 2013, livre des résumés. Publication ASF
Paris, France

insu-00913436
https://hal-insu.archives-ouvertes.fr/insu-00913436

Éditeur(s) : HAL CCSD Nova Science Publishers
Progress in Nonlinear Analysis Research

hal-00514545
https://hal.archives-ouvertes.fr/hal-00514545

Éditeur(s) : HAL CCSD Wiley-Blackwell
Résumé : Combined petrographic study and apatite fission track analysis (apatite FTA) across the Gres d'Annot basin document maximum temperatures reached by this turbiditic sandstone formation, from around 60 degrees C at the SW basin margin up to around 200 degrees C below the Penninic frontal thrust, in relation to burial below the front of Alpine nappes. Increasing diagenetic grade across the basin is primarily expressed by the development of silica transfer by pressure solution and correlated porosity loss. We infer the nappe thickness profile, from the nappe front in the SW up to around 8-10 km in the NE. Apatite FTA dates exhumation of the Gres d'Annot during the Late Miocene, in relation to thrusting of the underlying Argentera and Barrot Palaeozoic massifs. This study illustrates the influence of thrust front propagation on foreland basin diagenesis and exhumation, and highlights potential implications for the evolution of sediment reservoir properties in this context.
ISSN: 0954-4879

hal-00411860
https://hal.archives-ouvertes.fr/hal-00411860
DOI : 10.1111/j.1365-3121.2008.00793.x

Éditeur(s) : HAL CCSD
Résumé : International audience
La lagune de la Manche-à-Eau, écosystème d'eau saumâtre est soumis à la marée, aux alizés et aux ouragans. La carte IGN de 2004 est quadrillée selon une maille de 90 m pour placer 37 points dans un SIG et les borner sur le terrain avec un GPS. D'après les photographies aériennes, le dessin des contours rend possible le suivi morphologique depuis 1950. La profondeur est mesurée à 1437 points avec une perche et une sonde bathymétrique. L'orientation des courants est établie au flot et au jusant avec des penons fixés aux points, et une boussole. Les masses d'eau entrantes et sortantes permettent le calcul du volume d'eau renouvelé à chaque marée. Le suivi cartographique montre, une stabilisation des contours et de l'île due à " l'effet bouclier " et au sol (tourbe racinaire), et une agrégation/désagrégation des îlots selon le passage des ouragans. D'après la bathymétrie actuelle, le comblement de la lagune et le creusement des chenaux sont constatés. Les courants généraux sont gouvernés en surface par les alizés, vent de SSE-NNO et par le va-et-vient de la marée. Les descentes et remontées d'eau obligent ceux-ci à emprunter en profondeur les passages situés le long des berges et autour des dépressions et des hauts-fonds. Le volume d'eau renouvelé à chaque marée (14,8 %) combiné à l'hydrodynamisme actif et varié tend à vivifier cet écosystème.
Proceedings of the 61st Gulf and Caribbean Fisheries Institute
Gosier, Guadeloupe

hal-00755766
https://hal.univ-antilles.fr/hal-00755766
https://hal.univ-antilles.fr/hal-00755766/document
https://hal.univ-antilles.fr/hal-00755766/file/GCFI_61_2009_287-297.pdf

Éditeur(s) : HAL CCSD Universidad autonoma de Queretaro
Résumé : International audience
Algunos de los documentos realizados por o con la colaboración del Consejo de Europa han jugado un papel decisivo en la enseñanza de las lenguas extranjeras, contribuyendo por ejemplo a la introducción del enfoque comunicativo en los años 70, potencialmente más adaptado para favorecer la apropiación operacional de las lenguas y favorecer así mismo la libre circulación de las personas y de las ideas.En esta perspectiva se creó, bajo el liderazgo de John Trim, director del proyecto entre 1975 y 1997, un programa de referencialización para definir las necesidades lingüísticas de los diferentes grupos de aprendices (turistas, inmigrantes, comerciantes…) del cual nacieron Threshold Level (1975) para el inglés, Niveau Seuil (1976) para el francés, y luego Nivel Umbral para el castellano.Relataremos en esta contribución el pasaje de los niveles umbral al programa de “descripción de los niveles de referencia”, DNR, organizado por el Consejo de Europa, haciendo hincapié en la metodología transversal adoptada por los diferentes equipos europeos – análisis de corpus, benchmarking, ultimas teorías de la adquisición del lenguaje, pasaje de los descriptores al referencial, etc. la influencia del Marco europeo común de referencia para las lenguas -, el enfoque orientado a la acción, credibilidad social, autenticidad, etc., las diferentes publicaciones realizadas hoy en día en inglés, español, italiano, alemán y francés (referenciales, DVD…), y los casos específicos de Profile Deutsch, English profile y Un référentiel pour le français, A1-C2.
Revist@ UAQ virtual
Queretaro, Mexico

halshs-01398850
https://halshs.archives-ouvertes.fr/halshs-01398850
https://halshs.archives-ouvertes.fr/halshs-01398850/document
https://halshs.archives-ouvertes.fr/halshs-01398850/file/La_descripcion_y_la_especificacion_de_los%20niveles%20del%20Marco%20comun%20europeo%20para%20los%20idiomas%20aportes%20para%20una%20nueva%20dinamica.pdf

Éditeur(s) : HAL CCSD Cold Spring Harbor Laboratory Press
Résumé : International audience
The genome of male germ cells is actively transcribed during spermatogenesis to produce phase-specific protein-coding mRNAs and a considerable amount of different noncoding RNAs. Ribonucleoprotein (RNP) granule-mediated RNA regulation provides a powerful means to secure the quality and correct expression of the requisite transcripts. Haploid spermatids are characterized by a unique, unusually large cytoplasmic granule, the chromatoid body (CB), which emerges during the switch between the meiotic and post-meiotic phases of spermatogenesis. To better understand the role of the CB in male germ cell differentiation, we isolated CBs from mouse testes and revealed its full RNA and protein composition. We showed that the CB is mainly composed of RNA-binding proteins and other proteins involved RNA regulation. The CB was loaded with RNA, including pachytene piRNAs, a diverse set of mRNAs, and a number of uncharacterized long noncoding transcripts. The CB was demonstrated to accumulate nascent RNA during all the steps of round spermatid differentiation. Our results revealed the CB as a large germ cell-specific RNP platform that is involved in the control of the highly complex transcriptome of haploid male germ cells.
ISSN: 1355-8382

hal-00985894
https://hal-univ-rennes1.archives-ouvertes.fr/hal-00985894
DOI : 10.1261/rna.043729.113
PUBMED : 24554440

Éditeur(s) : HAL CCSD Wiley-Blackwell
Résumé : International audience
Recent field work and review of radiometric data obtained from Neogene lavas and plutonic rocks exposed in the Eastern Central Patagonian Cordillera (46–48ºS), which overlie subducted segments of the South Chile Ridge, suggest important Late Miocene to Pleistocene morphological changes in relation to base level variations and/or tectonic events. We present new field observations from a region south of Lago General Carrera-Buenos Aires, between the main Cordillera and the Meseta del Lago Buenos Aires, demonstrating that normal faulting controlled valley incisions and occurred during lava emplacement at 5–4 Ma and after 3 Ma. We also show that the 12 Ma basaltic flows of the Meseta del Lago Buenos Aires (~2000 m a.s.l.) have been subjected to deep incision, with younger lavas dated at 1.2 Ma partially filling the valleys. These incisions are thought to reflect progressive eastward tilting of the entire meseta. Our new observations, together with additional features from Central Patagonia, strongly suggest that tectonic events led to a regional widespread morphological change after 5 Ma. The coincidence in time and space between the subduction of segments of the South Chile Ridge at 6 and 3 Ma causing opening of a slab window, and strong base level variations in the studied area, suggests a cause-and-effect relationship. In Central Patagonia, compressional tectonics ended well before extensional events reported here. Causes of uplift and further extension are probably completely disconnected. The uplift is purely tectonic in origin and occurred prior to the subduction of the South Chile Ridge. Extension should be a consequence of this subduction.
ISSN: 0954-4879

insu-00272075
https://hal-insu.archives-ouvertes.fr/insu-00272075
DOI : 10.1111/j.1365-3121.2007.00766.x

Éditeur(s) : HAL CCSD Microbiology Society
Résumé : International audience
An actinobacterial strain, designated ViU22(T), was isolated from a natural uranium-rich soil and was studied using a polyphasic approach. Cells formed orange-pigmented colonies, were rod-shaped, Gram-positive (non-staining method), non-motile and non-spore-forming. This organism grew in 0-4.5 % (w/v) NaCl and at 15-37 °C, with optimal growth occurring in 0.5 % (w/v) NaCl and at 30 °C. Comparative 16S rRNA gene sequence analysis revealed that the strain ViU22(T) belonged to the genus Microbacterium. It exhibited highest 16S rRNA gene sequence similarity with the type strains of Microbacterium testaceum (98.14 %) and Microbacterium binotii (98.02 %). The DNA-DNA relatedness of strains ViU22(T) with the most closely related type strains Microbacterium testaceum and Microbacterium binotii DSM 19164(T) was 20.10 % (± 0.70) and 28.05 % (± 0.35), respectively. Strain ViU22(T) possessed a type B2β peptidoglycan with partial substitution of glutamic acid by 3-hydroxy glutamic acid. The major menaquinones were MK-11 and MK-12. Major polar lipids detected in the strain ViU22(T) were diphosphatidylglycerol, phosphatidylglycerol, an unknown phospholipid and unknown glycolipids. The predominant fatty acids were anteiso-C15 : 0, anteiso-C17 : 0 and iso-C16 : 0, a pattern reported for other Microbacterium species. The major cell-wall sugars were galactose, xylose and mannose and the DNA G+C content was 71 mol%. Together, the DNA-DNA hybridization results and the differentiating phenotypic characteristics, showed that strain ViU22(T) should be classified as the type strain of a novel species within the genus Microbacterium, for which the name Microbacterium lemovicicum sp. nov. is proposed. The type strain is ViU22(T) ( = ATCC BAA-2396(T) = CCUG 62198(T) = DSM 25044(T)).
ISSN: 1466-5026

hal-01561095
https://hal-amu.archives-ouvertes.fr/hal-01561095
PUBMED : 23264499
DOI : 10.1099/ijs.0.048454-0

Éditeur(s) : HAL CCSD Cambridge University Press
Résumé : International audience
Genetic variation was examined in two complex cases of Indo-Pacific pygmy angelfishes (genus Centropyge; Pomacanthidae). The lemonpeel pygmy angelfish C. flavissima (Cuvier and Valenciennes) has a geographically disjunct Indian vs. Pacific distribution and the individuals from these two regions differ by their colour patterns. Previous research on C. flavissima has shown mitochondrial introgression from two related species, C. eibli in the eastern Indian Ocean and C. vrolikii in the Pacific Ocean. Using the 16S rDNA and the CO1 gene as phylogeographic markers, we found no mitochondrial haplotypes in common between Indian Ocean C. flavissima and C. eibli, confirming partial genetic isolation, albeit recent. Also, we found substantial genetic differences between Indian and Pacific C. flavissima populations at the nuclear ETS-2 intron locus. The Indian Ocean form of C. flavissima, thus geographically isolated by >2000 km distance from its Pacific Ocean counterpart, is described as a new species, Centropyge cocosensis sp. nov. Centropyge cocosensis sp. nov. differs in appearance from C. flavissima in having a conspicuous blue iris and a fainter, bluish eye ring. We also found that the yellow pygmy angelfish C. heraldi Woods and Schultz consists of two genetically distinct entities, one distributed widely in the northern tropical Indo-West Pacific, the other distributed in the southern Pacific Ocean. The name originally given to the blackfin pygmy angelfish, C. woodheadi Kuiter, is here resurrected to designate the latter.
EISSN: 1755-2672

hal-01340521
https://hal-univ-perp.archives-ouvertes.fr/hal-01340521
DOI : 10.1007/s12526-016-0509-y

Éditeur(s) : HAL CCSD NOVA PUBLISHER,
Résumé : International audience
This paper deals with language practices in nurseries and pre-elementary schools of Martinique. It is focused on the account of modalities concerning everyday interactions and more precisely language distortions that may occur during interactions between adults and children in those structures. The consideration of cultural diversity generated by language distortions is suggested here to be a prerequisite for the development of a reciprocal comprehension leading to adequate mastery of language behavior and learning among young children. This approach proposes new patterns within a didactic agreement considering adult and child differences.
CULTURAL DIVERSITY International Perspectives, Impacts on the Workplace and Educational Challenges,

Droits : info:eu-repo/semantics/OpenAccess
ISBN : 978-1-63321-696-9.
hal-01658930
https://hal.univ-antilles.fr/hal-01658930
https://hal.univ-antilles.fr/hal-01658930/document
https://hal.univ-antilles.fr/hal-01658930/file/Toward%20a%20culture%20of%20diversity.pdf

Éditeur(s) : HAL CCSD
Résumé : This paper presents a collection of wood species with important uses in musical instruments, in reference to historical and geographical cultural specificities, with ranges of viscoelastic vibrational properties by species. Data combine our experimental characterizations and extensive literature review, gathered in a specific relational database. An overview of vibrational properties' distribution on c.400 species is introduced. Two case studies of wood choices for a given function in different epochs or regions are presented: woods for European historical bows, and woods for idiophone bodies in different continents. Trends are contrasted: very different properties associated to historical changes in the first case; some common features over different regions in the second one.
Proceedings of the International Conference of COST Action IE0601 Wood Science for the Preservation of Cultural Heritage
Braga, Portugal

hal-00808403
https://hal.archives-ouvertes.fr/hal-00808403
https://hal.archives-ouvertes.fr/hal-00808403/document
https://hal.archives-ouvertes.fr/hal-00808403/file/Vibrational_properties_tropical_wood_Bremaud_al.pdf

Éditeur(s) : HAL CCSD Wiley-Blackwell
Résumé : This study describes normal fault zones formed in foreland arkosic turbidites (the Grès d'Annot Formation, SW French Alps) under deep diagenesis conditions (~200 °C) and highlights the occurrence of two markedly different fault-rock types: (1) the foliated fault rocks of the Moutière-Restefond area; and (2) the dilatant fault rocks of the Estrop area. The deformation of (1) is dominated by intra- and transgranular fracturing, pressure solution of quartz and feldspar grains and syn-kinematic phyllosilicate precipitation resulting from feldspar alteration. The combination of these mechanisms results in a strongly anisotropic strain with intense shortening normal to the foliation (pressure solution) and extension parallel to the foliation (quartz- and calcite-sealed extension veins). This deformation implies local mass transfer that may be achieved without (or with limited) volume change. The deformation of (2) is expressed as dilatant quartz-sealed veins and breccia textures in which the main mechanisms are transgranular fracturing and quartz precipitation. Type (2) implies fault volume increase, isotropy of deformation and mass transfer at distances larger than in type (1). This study discusses the origins of (1) and (2) and shows that the permeability of (1) is anisotropic, with higher values than the host rocks parallel to the Y main deformation axis (i.e. perpendicular to the slip vector), whereas the permeability of (2) is isotropic and equivalent to that of the host rocks.
ISSN: 0954-4879

hal-01115177
https://hal.archives-ouvertes.fr/hal-01115177
DOI : 10.1111/ter.12100

Éditeur(s) : HAL CCSD Wiley-Blackwell
Résumé : International audience
The frequently observed parallelism between rifts and the pre­ existing orogenic fabric of continents suggests that the inherited tectonic fabric of the lithosphere influences the rupture of continents. We propose that the existence of a pervasive fabric in the lithospheric mantle induces an anisotropie strength in the lithosphere, that guides the propagation of continental rifts. Subcrustal mantle mechanical anisotropy is supported by (i) the anisotropie strength of olivine, (ii) an ubiquitous tectonic fabric in exposed mantle rocks, and (iii) measurements of seismic and electrical anisotropy. During major episodes of continent Rifting parallel to orogenic belts Ocean-opening through rifting and continent break-up is frequently related to the occurrence ofhotspots. There is, howevcr, a discrepancy between hot­ spots acting as pin point sources of heat and the linear extent of rifts over thou­ sands ofkilometres. Moreover rifts tend to parallel pre-existing orogenic fab­
ISSN: 0954-4879

hal-01389721
http://hal.univ-reunion.fr/hal-01389721
http://hal.univ-reunion.fr/hal-01389721/document
http://hal.univ-reunion.fr/hal-01389721/file/Vauchez_TerraNova1997_hal.pdf
DOI : 10.1111/j.1365-3121.1997.tb00003.x

Éditeur(s) : HAL CCSD Geological Society of London
Résumé : Permo-Triassic rift basins offer important hydrocarbon targets along the Atlantic margins. Their fill is dominated by continental red beds, comprising braided fluvial, alluvial fan, aeolian, floodplain and lacustrine facies. These relatively lightly explored basins span both the Atlantic and Tethyan domains and developed above a complex basement with inherited structural fabrics. Sparse data in offshore regions constrain understanding of depositional geometries and sedimentary architecture, further impeded by their deep burial beneath younger strata, combined with the effects of later deformation during continental breakup. This paper provides results from a multidisciplinary analysis of basins along the Atlantic margin. Regional seismic and well data, combined with geochemical provenance analysis from the European North Atlantic margins, are integrated with detailed outcrop studies in Morocco and Nova Scotia. The research provides new insights into regional basin tectonostratigraphic evolution, sediment fill, and reservoir distribution, architecture and quality at a range of scales. Regional seismic profiles, supported by key well data, indicate the presence of post-orogenic collapse basins, focused narrow rifts and low-magnitude multiple extensional depocentres. Significantly, Permo-Triassic basin geometries are different and more varied than the overlying Jurassic and younger basins. Provenance analysis using Pb isotopic composition of detrital K-feldspar yields new and robust controls on the sediment dispersal patterns of Triassic sandstones in the NE Atlantic margin. The evolving sedimentary architecture is characterized by detailed sedimentological studies of key outcrops of age equivalent Permian-Triassic rifts in Morocco and Nova Scotia. The interplay of tectonics and climate is observed to influence sedimentation, which has significant implications for reservoir distribution in analogue basins. New digital outcrop techniques are providing improved reservoir models, and identification of key marker horizons and sequence boundaries offers a potential subsurface correlation tool. Future work will address source and seal distribution within the potentially petroliferous basins.
Petroleum Geology: From Mature Basins to New Frontiers Proceedings of the 7th Petroleum Geology Conf

hal-00590618
https://hal.archives-ouvertes.fr/hal-00590618

Éditeur(s) : HAL CCSD
Atelier Thématique "Loi pour une République Numérique"
Cayenne, French Guiana

hal-01503817
https://hal-agroparistech.archives-ouvertes.fr/hal-01503817

Éditeur(s) : Edinburgh, London
Siècle(s) traité(s) : 19
Provenance : Université Caen Normandie. Service commun de la documentation
Permalien : http://www.manioc.org/patrimon/CAE19033_4
CAE19033_4

Éditeur(s) : HAL CCSD IRD
Résumé : International audience
Malaria remains a major health problem in French Guiana despite the decrease in the number of cases since 2010. A previous study in Camopi, an Amerindian village on the Oyapock River, revealed that Plasmodium falciparum malaria incidence was significantly related to landscape features and that its spatial distribution exhibited some obvious patterns. In the present study, we first identified the spatial patterns that exhibit a significant Moran's index of spatial auto-correlation and that significantly explain P. falciparum malaria incidence within the multiple linear regression framework. Secondly, we linked these patterns with remotely sensed environmental features. The selected model is composed of five spatial components: three patterns, representing 50.7% of the total variance, are associated with large scale variations of the incidence, and the remaining patterns are associated with local scale variations and represent 28.7% of the total variance. Different hamlet clusters that have specificities in terms of P. falciparum malaria incidence rate, environmental characteristics and mosquito control strategies have been identified. The methodology proposed in the present study can provide useful knowledge on the spatial distribution of the P. falciparum malaria incidence in Camopi at different scales and on possible explanation of such distribution, as a function of the scale.
Symposium of the Latin American Society for Remote Sensing and Spatial Information Systems (SELPER)
Cayenne, French Guiana

ird-00797353
http://hal.ird.fr/ird-00797353
http://hal.ird.fr/ird-00797353/document
http://hal.ird.fr/ird-00797353/file/Roux_et_al_SELPER_2012.pdf
IRD : fdi:010058342