Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The increased use of pesticides has caused concern over the possible direct association of exposure to combinations of these compounds with bee health problems. There is growing proof that bees are regularly exposed to mixtures of agrochemicals, but most research has been focused on managed bees living in farmland, whereas little is known about exposure of wild bees, both in farmland and urban habitats. To determine exposure of wild bumblebees to pesticides in agricultural and urban environments through the season, specimens of five different species were collected from farms and ornamental urban gardens in three sampling periods. Five neonicotinoid insecticides, thirteen fungicides and a pesticide synergist were analysed in each of the specimens collected. In total, 61% of the 150 individuals tested had detectable levels of at least one of the compounds, with boscalid being the most frequently detected (35%), followed by tebuconazole (27%), spiroxamine (19%), carbendazim (11%), epoxiconazole (8%), imidacloprid (7%), metconazole (7%) and thiamethoxam (6%). Quantifiable concentrations ranged from 0.17 to 54.4 ng/g (bee body weight) for individual pesticides. From all the bees where pesticides were detected, the majority (71%) had more than one compound, with a maximum of seven pesticides detected in one specimen. Concentrations and detection frequencies were higher in bees collected from farmland compared to urban sites, and pesticide concentrations decreased through the season. Overall, our results show that wild bumblebees are exposed to multiple pesticides when foraging in agricultural and urban landscapes. Such mixtures are detected in bee tissues not just during the crop flowering period, but also later in the season. Therefore, contact with these combinations of active compounds might be more prolonged in time and widespread in the environment than previously assumed. These findings may help to direct future research and pesticide regulation strategies to promote the conservation of wild bee populations.
ISSN: 0269-7491

hal-01477203
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01477203
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01477203/file/Quantifying%20exposure%20of%20wild%20bumblebees_accepted.pdf
DOI : 10.1016/j.envpol.2017.01.001
PUBMED : 28087090

Éditeur(s) : HAL CCSD Elsevier
Résumé : Different types of fractures and fault rocks occur within the major normal fault zones bordering the NW of the Neogene Penedes basin (NE Spain). In the southwest part of the basin, the main fault is the Baix Penedes fault that places the Upper Jurassic-Lower Cretaceous dolomicrites of the footwall in contact with the Miocene siliciclastic sediments of the hangingwall. Within the footwall damage zone, different fracture systems and their respective associated breccias and cements have been recognized. Using a combination of structural, petrologic and geochemical analyses, we show that these fracture systems evolved from mainly tectonic to mainly karstic features during the progressive development and upward propagation of the fault. The earlier fractures and associated breccias represent the initial stages of the fault propagation, when the process zone formed around the fault tip was dominated by dilatant fracturing (fractures 1 and dilatant breccias B1). The fluid involved in this early deformation precipitated the dolomite cement Cl, in equilibrium with the host-rock in a closed hydrogeological system. Localization of frictional processes generated cataclasites and ultracataclasites along distinct second-order faults (fractures 2). In these fractures, the dolomite cement C2 precipitated in relation to the incipient opening of the hydrological system to percolating meteoric waters. The later fractures and associated breccias represent the late stages of the fault propagation. These structures (fractures 3, fractures 4 and the dilatant breccias B2) were formed when the extensional deformation reached the surface, resulting in an increasingly open hydrogeological system. At these stages, deposition of the dolomitic sediment DS and precipitation of the calcite cements C3, C4 and C5 show the circulation of freshwaters in a vadose meteoric environment, i.e. in karstic conditions.
ISSN: 0375-6742

hal-00512690
https://hal.archives-ouvertes.fr/hal-00512690
DOI : 10.1016/j.gexplo.2009.11.010

Éditeur(s) : HAL CCSD
Résumé : International audience
MOTIVATION: Imaging mass spectrometry (IMS) is a maturating technique of molecular imaging. Confidence in the reproducible quality of IMS data is essential for its integration into routine use. However, the predominant method for assessing quality is visual examination, a time consuming, unstandardized and non-scalable approach. So far, the problem of assessing the quality has only been marginally addressed and existing measures do not account for the spatial information of IMS data. Importantly, no approach exists for unbiased evaluation of potential quality measures. RESULTS: We propose a novel approach for evaluating potential measures by creating a gold-standard set using collective expert judgements upon which we evaluated image-based measures. To produce a gold standard, we engaged 80 IMS experts, each to rate the relative quality between 52 pairs of ion images from MALDI-TOF IMS datasets of rat brain coronal sections. Experts' optional feedback on their expertise, the task and the survey showed that (i) they had diverse backgrounds and sufficient expertise, (ii) the task was properly understood, and (iii) the survey was comprehensible. A moderate inter-rater agreement was achieved with Krippendorff's alpha of 0.5. A gold-standard set of 634 pairs of images with accompanying ratings was constructed and showed a high agreement of 0.85. Eight families of potential measures with a range of parameters and statistical descriptors, giving 143 in total, were evaluated. Both signal-to-noise and spatial chaos-based measures performed highly with a correlation of 0.7 to 0.9 with the gold standard ratings. Moreover, we showed that a composite measure with the linear coefficients (trained on the gold standard with regularized least squares optimization and lasso) showed a strong linear correlation of 0.94 and an accuracy of 0.98 in predicting which image in a pair was of higher quality. AVAILABILITY AND IMPLEMENTATION: The anonymized data collected from the survey and the Matlab source code for data processing can be found at: https://github.com/alexandrovteam/IMS_quality. CONTACT: theodore.alexandrov@embl.de
Bioinformatics (Oxford, England)

hal-01163754
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01163754
DOI : 10.1093/bioinformatics/btv266
PUBMED : 26072506

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The Massif du Sud is a large ophiolitic complex that crops out in the southern region of New Caledonia (SW Pacific). It is dominated by harzburgite tectonite that locally shows a transitional gradation to massive dunite up section. Clinopyroxene, orthopyroxene and plagioclase progressively appear in dunite up to the transition to layered wehrlite and orthopyroxene-gabbro. The dunite-wehrlite and wehrlite-gabbro contacts are parallel and the latter defines the paleo-Moho.;Highly depleted modal, mineral and bulk rock compositions indicate that harzburgites are residues after high degrees (20-30%) of partial melting mainly in the spinet-stability field. Their relative enrichment in HFSE, LREE and MREE is due to re-equilibration of melting residues with percolating melts. Dunite formed in the Moho transition zone by reaction between residual mantle harzburgite and olivine-saturated melts that led to pyroxene dissolution and olivine precipitation. Rare clinopyroxene and plagioclase crystallized in interstitial melt pores of dunite from primitive, low-TiO2, ultra-depleted liquids with a geochemical signature transitional between those of island arc tholeiites and boninites.;Ascending batches of relatively high-SiO2, ultra-depleted melts migrated through the Moho transition zone and generated wehrlite by olivine dissolution and crystallization of clinopyroxene, orthopyroxene and plagioclase in variable amounts. These liquids were more evolved and were produced by higher degrees of melting or from a more depleted source compared with melts that locally crystallized clinopyroxene in dunite. Ultra-depleted magmas, non-cogenetic with those that formed the Moho transition zone, ascended to the lower crust and generated gabbroic cumulates with subduction-related affinity. Thus, the ultramafic and mafic rocks in the Moho transition zone and lower crust of the Massif du Sud ophiolite are not products of fractional crystallization from a single magma-type but are the result of migration and accumulation of different melts in a multi-stage evolution. The record of high partial melting in the mantle section, and migration and accumulation of ultra-depleted subduction-related melts in the Moho transition zone and lower crust support that the Massif du Sud ophiolite is a portion of forearc lithosphere generated in an extensional regime during the early phases of the subduction zone evolution. Our results show the existence of different types of ultra-depleted melt compositions arriving at the Moho transition zone and lower crust of an infant intraoceanic paleo-arc. Ultra-depleted melts may thus be a significant component of the melt budget generated in oceanic spreading forearcs prior to aggregation and mixing of a large range of melt compositions in the crust.
ISSN: 0009-2541

hal-00429333
https://hal.archives-ouvertes.fr/hal-00429333
DOI : 10.1016/j.chemgeo.2009.06.004

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
BACKGROUND: Evidence of human sexual transmission during Zika virus emergence is a matter of concern, particularly in procreation, but to date, kinetics of seminal shedding and the effects of infection on human reproductive function have not been described. To investigate the effects of Zika virus infection on semen and clearance of Zika virus from semen and body fluids, we aimed to study a cohort of Zika virus-infected men. METHODS: This prospective observational study recruited men presenting with acute Zika virus infection at Pointe-à-Pitre University Hospital in Guadeloupe, French Caribbean, where a Zika virus outbreak occurred between April and November, 2016. Blood, urine, and semen were collected at days 7, 11, 20, 30, 60, 90, and 120 after symptom onset, and semen characteristics, such as total sperm count, sperm motility, vitality, and morphology, and reproductive hormone concentrations, such as testosterone, inhibin, follicle-stimulating hormone, and luteinising hormone, were assessed. At days 7, 11, and 20, semen was processed to isolate motile spermatozoa. Zika virus RNA was detected by RT-PCR using whole blood, serum, urine, seminal plasma, semen cells, and motile spermatozoa fractions. Zika virus was isolated from different sperm fractions on Vero E6 cultures. FINDINGS: 15 male volunteers (mean age 35 years [SD 5; range 25-44) with acute Zika virus infection and positive Zika virus RNA detection in blood or urine were enrolled. Total sperm count was decreased from median 119 × 10(6) spermatozoa (IQR 22-234) at day 7 to 45·2 × 10(6) (16·5-89·6) at day 30 and 70 × 10(6) (28·5-81·4) at day 60, respectively, after Zika virus infection. Inhibin values increased from 93·5 pg/mL (IQR 55-162) at day 7 to 150 pg/mL (78-209) at day 120 when total sperm count recovered. In motile spermatozoa obtained after density gradient separation, Zika virus RNA was found in three of 14 patients at day 7, four of 15 at day 11, and four of 15 at day 20, and replication-competent virus was found in the tested patient. Seminal shedding kinetics seemed heterogeneous among patients. Whole blood was the fluid most frequently positive for Zika virus RNA (62 of 92 samples) and three patients remained positive at day 120. INTERPRETATION: Semen alterations early after acute Zika virus infection might affect fertility and could be explained by virus effects on the testis and epididymis. Frequency of shedding and high viral load in semen, together with the presence of replicative virus in a motile spermatozoa fraction, can lead to Zika virus transmission during sexual contact and assisted reproduction procedures. Whole blood seems to be the best specimen for Zika virus RNA detection, diagnosis, and follow-up. FUNDING: Agence de la Biomédecine/Agence Régionale de Santé de la Guadeloupe/Inserm-REACTing.
ISSN: 0140-6736

hal-01647078
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01647078
DOI : 10.1016/S1473-3099(17)30444-9
PUBMED : 28838639

Éditeur(s) : HAL CCSD
Résumé : International audience
In this work, we focus on the issue of diffusion in dynamic networks. We begin by proposing a generic framework that merges two essential aspects of the problem: diffusion and network dynamics. Then, our framework is used for comparing effects of two aspects of the human behavior, sociability and network dynamics. On the one hand the dynamics of the network is related to the movements of individuals in a social space that lead ephemeral social proximity contacts. On the other hand the diffusion phenomenon is studied through the epidemic paradigm. The results obtained by simulations provide original insight about how and why the "social dynamics" of individuals, related to the proximity in a social space and its evolutions, influences diffusion phenomena through a population.
International Conference on Advances in Social Networks Analysis and Mining
Istanbul, Turkey

hal-00786162
https://hal.archives-ouvertes.fr/hal-00786162
DOI : 10.1109/ASONAM.2012.104

Éditeur(s) : HAL CCSD Public Library of Science
Résumé : International audience
The CoPanFlu-France cohort of households was set up in 2009 to study the risk factors for infection by the pandemic influenza virus (H1N1pdm) in the French general population. The authors developed an integrative data-driven approach to identify individual, collective and environmental factors associated with the post-seasonal serological H1N1pdm geometric mean titer, and derived a nested case-control analysis to identify risk factors for infection during the first season. This analysis included 1377 subjects (601 households). The GMT for the general population was 47.1 (95% confidence interval (CI): 45.1, 49.2). According to a multivariable analysis, pandemic vaccination, seasonal vaccination in 2009, recent history of influenza-like illness, asthma, chronic obstructive pulmonary disease, social contacts at school and use of public transports by the local population were associated with a higher GMT, whereas history of smoking was associated with a lower GMT. Additionally, young age at inclusion and risk perception of exposure to the virus at work were identified as possible risk factors, whereas presence of an air humidifier in the living room was a possible protective factor. These findings will be interpreted in light of the longitudinal analyses of this ongoing cohort.
ISSN: 1932-6203

Droits : http://creativecommons.org/licenses/by-sa/
hal-01122215
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01122215
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01122215/document
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01122215/file/journal.pone.0060127.pdf
PUBMED : 23613718

Éditeur(s) : HAL CCSD
Résumé : International audience
Aux Antilles et en Guyane françaises, comme dans d’autres territoires, les acteurs de l’enseignement, toutes disciplines confondues, sont confrontés à des effets de contextes. Ces derniers peuvent être définis comme les décalages observés entre un objectif d’enseignement et sa réalisation lorsque ces décalages sont attribuables aux différents contextes en présence dans le processus didactique. Ceux-ci peuvent être de natures variées (langagière, culturelle, socio-économique, géographique, géologique, écologique) et mettent en jeu différents objets : objets d’enseignement ou liés au système éducatif, documents pédagogiques, représentations des acteurs, etc.En mettant en scène différentes disciplines d’enseignement et des contextes variés sur le plan sociolinguistique et culturel, ce numéro 5 de la revue Contextes et Didactiques intitulé « Éducation et socialisation en contextes multilingues et pluriculturels » vise à faire émerger des éléments de compréhension des mécanismes menant à l’apparition d’effets de contexte. Les travaux de didactiques contextualisées constituent de fait ici des références convoquées dans les différentes contributions de ce volume.L’une des questions sous-jacente à la thématique et abordée dans ce volume est de savoir dans quelle mesure, à quels niveaux et de quelles manières les processus d’éducation et de socialisation peuvent-ils être adaptés aux contextes sociolinguistiques et culturels dans lesquels ils se déroulent ? L’une des orientations proposées est de décrire et de mesurer les effets de l’environnement sociolinguistique et culturel ainsi que leur prise en compte dans les processus d’apprentissage. Sont ainsi regroupés dans ce volume des travaux centrés sur les langues dites « minorées » au cours des processus d’apprentissage et sur l’utilisation de ces langues dans les processus de socialisation, ainsi que des travaux portant sur les profils linguistiques des locuteurs, les représentations sociolinguistiques, les phénomènes identitaires, les pratiques linguistiques (aspects phonologiques, morphologiques, syntaxiques) et langagières (gestion des langues par les locuteurs, alternance codique), tant chez les élèves que chez les enseignants, dans l’enseignement des langues ou d’autres disciplines. De fait, ces travaux présentent des cadres théoriques et méthodologiques spécifiques basés sur la formulation de problématiques propres à l’identification et à la prise en compte de la diversité sociolinguistique et culturelle des contextes dans l’enseignement. Ces questions sont éclairées par des réflexions d’ordre sociologique, historique et épistémologique sur le processus de contact et de métissage des savoirs locaux et universels. Ainsi, ce numéro 5 de la revue Contextes et Didactiques propose des études quantitatives et qualitatives susceptibles de décrire, de comparer et d’éclairer les processus de contextualisation didactique notamment sur les plans linguistiques, langagiers et culturels. La diversité des contextes évoqués dans les différentes contributions présentes dans ce numéro peut permettre d’envisager des comparaisons de systèmes éducatifs, de situations d’enseignement, de conceptions d’apprenants et de pratiques éducatives. Neuf articles composent ce cinquième numéro de la revue Contextes et Didactiques. Le premier article rédigé par Raphaële FOUILLET et intitulé « Les grammaires du français conçues en Italie : un lieu de contextualisation » vise à mettre en évidence des éléments de contextualisation du discours grammatical écrit observables dans les grammaires du français produites en Italie.Dans le deuxième article, « La géopolitique pour comprendre le contexte socio-culturel libanais et ses pratiques linguistiques », Ludivynn MUNOZ propose une démarche géopolitique en vue d’éclairer le contexte du Liban et de mettre en exergue les contributions de cette discipline dans ce contexte socio-culturel complexe.La troisième contribution, proposée par Christian MICHAUD et intitulée « Disciplines Non Linguistique en Langues Vivantes Étrangères : Quelle prise en compte des effets de contextes pour améliorer les enseignements ? », a comme objectif d’explorer les pratiques pédagogiques de professeurs ayant en charge l’enseignement d’une discipline dite non linguistique en langue vivante étrangère en section européenne en France.Le quatrième article, intitulé « La prise en compte de la dimension linguistique dans les disciplines non-linguistiques : du prescrit au réel ? » et rédigé par Julien BASSO, propose une réflexion sur l’appropriation du français en contexte scolaire, en se focalisant plus précisément sur la prise en compte de la dimension linguistique dans l’enseignement de l’Histoire, de la Géographie et des Sciences de la Vie et de la Terre en Outre-Mer français.La cinquième contribution, de Dominique DÉMOCRITE-LOUISY, s’intitule « Un enseignement bilingue peut-il être une réponse à l’échec scolaire ? Le cas de la collectivité de Saint-Martin ». Cet article porte sur l’enseignement à l’école maternelle à Saint-Martin où la grande majorité des enseignants est essentiellement francophones et où les Agents Territoriaux Spécialisés des Écoles Maternelles sont anglophones.Dans le sixième article, intitulé : « TICE et transposition didactique contextualisée : retour d’expérience dans l’enseignement-apprentissage du français langue 3 en milieu universitaire arabophone », Carine ZANCHI traite du recours aux Technologies de l’Information et de la Communication en Éducation dans le cadre de l’enseignement du français en Jordanie. Elle s’intéresse ainsi à la construction d’outils de formation multimédia à destination d’apprenants arabophones débutants.Le septième article, rédigé par Noël CORDONIER et Sonya FLOREY, a pour titre « Pour un contexte épistémologique du présent. Ou comment se libérer des apories d’une postmodernité généreuse mais fatiguée ». Il relate une expérience scolaire menée en Suisse qui a permis aux élèves d’une classe primaire de créer un imagier plurilingue, en sollicitant l’aide de leurs parents francophones ou allophones, et de l’intégrer dans des tâches d’apprentissage.Dans le huitième article, « Rôle de la langue maternelle et de l’origine sociale des élèves sur l’activité de co-révision à distance d’un texte explicatif en français langue seconde dans le contexte diglossique d’Haïti », Emilien DUVELSON se donne pour objectif d’étudier l’effet de la langue (créole versus français) utilisée dans les textes d’aide, sur la compréhension et la réécriture de textes en langue seconde (français) dans le contexte diglossique d’Haïti chez des lecteurs d’origines sociales différentes.Enfin, dans le neuvième et dernier article, intitulé « La diversité linguistique et culturelle à l’école primaire : quels enjeux pour les enseignants de la Dominique ? », Stella CAMBRONE-LASNES évoque les enjeux culturels, éducatifs et pédagogiques liés à la prise en compte de la diversité linguistique et culturelle en contexte scolaire dominiquais. Elle aborde notamment le statut des langues en présence (anglais, garifuna, kokoy, français, espagnol, chinois, hindi, créole haïtien, créole dominiquais) ainsi que les représentations d’enseignants du primaire sur ces différentes langues, et en particulier le créole dominiquais. De l’Italie au Liban, en passant par la France hexagonale et ses collectivités d’Outre-mer (Saint-Martin, Guadeloupe), la Jordanie, la Suisse, la Dominique et Haïti, ce numéro 5 de la revue Contextes et Didactiques a comme objectif de mettre en évidence les mécanismes qui mènent à l’apparition d’un certain nombre d’effets de contextes en éducation dans des territoires divers et des contextes sociolinguistiques et culturels variés.
Revue « Contextes et Didactiques »

hal-01609280
https://hal.univ-antilles.fr/hal-01609280

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Cold seeps, located on sea floors and frequently fueled with methane, have been much studied for the formation of carbonate nodules, crusts or masses resulting from the activity og communities of anaerobic bacteria. In this paper, we examine the impact of cold seepage on their caging sediments, as far as their geochemical composition and microfaunal content are concerned. To this end, two fossil cold seeps of the Jurassic Beauvoisin site (Vocontian Trough, SE-France) are studied, focusing on the redox-sensitive and/or sulfide-forming trace metals. We observe that: 1) the carbonate edifices of the cold seeps are enriched in specific elements, namely, Sr, Mo As and Sb, compared to their caging marlstones, and 2) the benthic foraminifer populations were present close to the edifices. The Sr enrichment is ascribed to a contamination of the seeping fluids at the contact with underlying evaporites; the Mo-As-Sb enrichment may have several, non-exclusive, origins. We retain two scenarios; in the first one, the enrichment is due to the ascending fluids that could collect these elements when passing through thick shaly formations; in the second scenario, Mo, As and Sb were supplied to the sites of carbonate precipitation together with Fe- and Mn-oxy-hydroxides (the so-called particulate shuttle process). We favor the second scenario (possibly coupled to the first one) because the rather uncommon Mo-As-Sb association is also observed for reducing sediments deposited under the influence of Fe-Mn-shuttling.
ISSN: 0009-2541

hal-00806655
https://hal.archives-ouvertes.fr/hal-00806655
DOI : 10.1016/j.chemgeo.2012.12.012

Éditeur(s) : HAL CCSD American Geophysical Union
Résumé : International audience
Expeditions 304 and 305 of the Integrated Ocean Drilling Program cored and logged a 1.4 km section of the domal core of Atlantis Massif. Postdrilling research results summarized here constrain the structure and lithology of the Central Dome of this oceanic core complex. The dominantly gabbroic sequence recovered contrasts with predrilling predictions; application of the ground truth in subsequent geophysical processing has produced self-consistent models for the Central Dome. The presence of many thin interfingered petrologic units indicates that the intrusions forming the domal core were emplaced over a minimum of 100-220 kyr, and not as a single magma pulse. Isotopic and mineralogical alteration is intense in the upper 100 m but decreases in intensity with depth. Below 800 m, alteration is restricted to narrow zones surrounding faults, veins, igneous contacts, and to an interval of locally intense serpentinization in olivine-rich troctolite. Hydration of the lithosphere occurred over the complete range of temperature conditions from granulite to zeolite facies, but was predominantly in the amphibolite and greenschist range. Deformation of the sequence was remarkably localized, despite paleomagnetic indications that the dome has undergone at least 45 degrees rotation, presumably during unroofing via detachment faulting. Both the deformation pattern and the lithology contrast with what is known from seafloor studies on the adjacent Southern Ridge of the massif. There, the detachment capping the domal core deformed a 100 m thick zone and serpentinized peridotite comprises similar to 70% of recovered samples. We develop a working model of the evolution of Atlantis Massif over the past 2 Myr, outlining several stages that could explain the observed similarities and differences between the Central Dome and the Southern Ridge.
ISSN: 0148-0227

hal-00617528
https://hal.archives-ouvertes.fr/hal-00617528
https://hal.archives-ouvertes.fr/hal-00617528/document
https://hal.archives-ouvertes.fr/hal-00617528/file/2010JB007931.pdf
DOI : 10.1029/2010JB007931

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
ODP (Ocean Drilling Program)/IODP (Integrated Ocean Drilling Program) Site 1256 is located on the Cocos Plate in the Eastern Equatorial Pacific Ocean, in a 15 Ma old oceanic lithosphere formed at the EPR during a period of superfast spreading (>200 mm/yr). ODP/IODP Hole 1256D reached for the first time the contact between sheeted dikes and underlying gabbros. It consequently offers a unique opportunity to study in situ, in present-day oceanic crust, the root zone of the sheeted dike complex. This root zone is a thin, 100 m thick boundary layer between the magmatic system (i.e., the axial melt lens, similar to 1100 degrees C), and the overlying high temperature hydrothermal system (<= 450 degrees C). The understanding of interactions within this boundary layer is critical to that of crustal processes along mid-ocean ridges.;This work focuses on the petrophysical characterization of the root zone of the sheeted dike complex in order to further constrain the hydrothermal circulation system in the vicinity of the axial melt lens, as recorded in non-granoblastic dikes, granoblastic dikes, and varitextured gabbros. The petrophysical properties were determined from sample measurements in the laboratory and were compared to in situ downhole geophysical probing. The porosity structure is bipolar, depending on lithology, resulting in a layered system. Non-granoblastic dikes are generally altered in the greenschist fades (similar to>250 degrees C) with relatively high and interconnected (cementation index m similar to 1.72, electrical tortuosity tau similar to 28.3) porosity (1.5%). In contrast, gabbros are retrogressively metamorphosed in the amphibolite (similar to>450 degrees C) and greenschist facies, with lower porosity (1.3%) that involves numerous fissures and cracks, resulting in a more connected medium (m similar to 1.58, tau similar to 11.8) than non-granoblastic dikes. These cracks are more abundant but also tend to close with increasing depth as indicated in downhole geophysical data. Porosity and alteration, as viewed from surface electrical conductivity, appear to be directly correlated.
ISSN: 0040-1951

hal-00544556
https://hal.archives-ouvertes.fr/hal-00544556
DOI : 10.1016/j.tecto.2010.07.013

Éditeur(s) : HAL CCSD Société des américanistes
Résumé : International audience
A large set of historical documents give us descriptions of Antillean Amerindian boats. These texts constitute a continuous series from the time of first contact to sub-contemporaneous anthropological descriptions. This paper is based on extensive review of the data contained in those early Spanish, Dutch, English, and French sources and also on a review of the few direct archaeological evidences. In this way we tried to analyse not only the nature of the relationship that existed between Antillean Amerindians and the sea but also to obtain an accurate description of their different boat types. Finally we have reconstituted the building process chaîne opératoire of the Kanawa, which were the boat type specifically designed and preferentially used for over-sea navigations.
Nous disposons d'un très grand nombre de descriptions historiques des embarcations amérindiennes antillaises. Ces textes constituent une série continue allant du récit des premiers moments aux études ethnologiques sub-contemporaines. Cet article s'appuie sur une recension d'une ampleur inédite des informations contenues dans ces sources espagnoles, hollandaises, anglaises et françaises précoces ainsi que sur les quelques données archéologiques directes disponibles. Nous avons par ce biais tenté de dégager la nature du rapport entretenu par les populations amérindiennes des Antilles avec l'élément marin, mais aussi d'obtenir la description la plus précise possible des différentes embarcations constituant leur flotte et enfin d'établir la chaîne opératoire de construction des kanawa l'un de ces navires spécifiquement conçu et préférentiellement utilisé pour la navigation en haute mer.
ISSN: 0037-9174

hal-01671136
https://hal.univ-antilles.fr/hal-01671136
https://hal.univ-antilles.fr/hal-01671136/document
https://hal.univ-antilles.fr/hal-01671136/file/JSA102_1_15_art_berard1.pdf
DOI : 10.4000/jsa.14688

Éditeur(s) : HAL CCSD EDP Sciences
Résumé : International audience
Understanding mechanisms in DSSCs is fundamental for their improvement; this includes the nanocrystalline semiconducting layer behaviour. Different mesoporous TiO2 layers are fabricated and analyzed for possible use in DSSC solar cells. The preparations included the addition of P123 triblock copolymer as structuring agent to the synthesized anatase sol. This preparation was also mixed with Degussa P25 TiO2 nanoparticles in one case and polystyrene latex in another. Mesoporous mixed TiO2-SiO2 thin layers were also analyzed. The diverse morphologies and features are studied by microscopic techniques and by means of spectral quantum efficiency of a photoelectrochemical cell (PEC) that uses as photoelectrode the unsensitized porous TiO2 layer. Contact angle measurements are also performed. We have found that a very high specific area due to very small nanocrystals and small pores can hinder electrolyte penetration in the pores formed by TiO2 nanograins, affecting photoelectrodes efficiency. © EDP Sciences, 2015.
ISSN: 1286-0042

hal-01683213
https://hal.univ-antilles.fr/hal-01683213
DOI : 10.1051/epjap/2015150221

Éditeur(s) : HAL CCSD
Résumé : In 1996 the European Commission Humanitarian Office (ECHO) launched a regional approach for disaster preparedness, focusing in its first phase on Central America, Caribbean and Southeast Asia (including Bangladesh). The first step in this process was the preparation of a «diagnostic study» that involved a situation review of the countries in these regions with regard to their vulnerabilities, disaster preparedness capacities and national plans or policies for disaster management.The Centre for Research on the Epidemiology of Disasters of the Université Catholique de Louvain (UCL) served as ECHO’s principal technical support with the collaboration of other institutions in Europe and the regions.The present «diagnostic report», covering Central America and the Caribbean, has been carried out by the Centre International pour la Formation et les Echanges en Géosciences (CIFEG) under the supervision of Professor Robert D’Ercole (Université de Savoie, Chambéry).Mr. Thierry Lesales (Université des Antilles et de la Guyane) participated closely in the drafting of this report and was actively involved in the field missions with Mr D’Ercole where they met and interviewed numerous national officials, non-governmental organisations and regional and international bodies. Further assistance was provided by Claudine Misson (CRED) for the interviews and information collected in the Dominican Republic. The report also draws from an earlier mission undertaken by Dr. Philippe Masure (BRGM, France), Christian Bugnion (CRED) and Alexandra Angulo (CRED) who undertook some of the preparatory work for the diagnostic study.This report presents an analysis of the disaster preparedness situation in Central America and the Caribbean and provides some preliminary recommendations regarding priorities and future programme direction. As such it remains primarily a descriptive study. It is expected to form the basis for the formulation of the ECHO Disaster Preparedness Action Plan.
En 1996, la Oficina Humanitaria de la Comunidad Europea (ECHO) lanzó la iniciativa de un enfoque regional en materia de preparación a los desastres, concentrándose inicialmente en las regiones de América Central, Caribe y Asia del Sureste (incluyendo a Bangladesh). La primera fase de este proceso fue la preparación de un « diagnóstico» que implicaba un examen de la situación de los países de cada una de estas regiones en relación a la vulnerabilidad, la capacidad de preparación a los desastres y las políticas y planes nacionales en materia de gestión de desastres.El Centre for Research on the Epidemiology of Disasters (CRED), de la Université Catholique de Louvain (UCL), ha sido el principal apoyo técnico de ECHO para esta iniciativa, con la colaboración y asistencia de otras instituciones en Europa y en las regiones arriba mencionadasEl presente informe que cubre América Central y el Caribe, fue realizado por el International Centre for Training and Exchanges in Geosciences (CIFEG), bajo la dirección del Profesor Robert D'Ercole (Université de Savoie).Thierry Lesales (Université des Antilles et de la Guyane) participó de cerca a la realización de este documento y estuvo activamente implicado junto al Profesor D'Ercole en las misiones que se realizaron en varios países. En el curso de estas misiones, se entrevistaron con numerosos representantes de gobiernos nacionales, de ONGs y de organizaciones regionales e internacionales Se contó igualmente con la asistencia de Claudine Misson (CRED), quien realizó la misión en República Dominicana. El informe se basa igualmente en una misión anterior llevada a cabo por Philippe Masure (BRGM, France), Alexandra Angulo (CRED) y Christian Bugnion (CRED), la cual realizó parte del trabajo preparatorio para el diagnóstico.El informe presenta un análisis de la situación en América Central y el Caribe y provee recomendaciones preliminares para las prioridades y dirección del futuro programa. En el marco de la segunda fase, está destinado a servir de base para la formulación del Plan de Acción de Preparación a los Desastres de ECHO.
Depuis 1994, ECHO (Office Humanitaire de la Commission Européenne, devenu le service de la Commission européenne à l’aide humanitaire et à la protection civile) a financé, à l'échelle mondiale, de nombreuses opérations pour la prévention et la préparation aux catastrophes (catastrophes naturelles principalement) Ces financements ont répondu aux demandes d'ONG et d'organisations internationales qui ont-elles-mêmes mis en oeuvre les projets correspondants. Les évaluations de ces opérations ont donné des appréciations positives. Cependant, ECHO souhaite s'impliquer davantage dans la prévention et la préparation aux catastrophes et mieux cibler ses actions pour une plus grande cohérence d'ensemble.Au cours de la réunion du 16 juillet 1996, le Comité d'Aide Humanitaire a approuvé la nouvelle approche régionale proposée par ECHO pour son programme de prévention, d'atténuation et de préparation aux catastrophes, le DIPECHO (Dlsaster Preparedness ECHO), pour la période 1996—1998. Ce programme doit s'appliquer dans un cadre régional en concentrant d'abord ses financements sur des plans d'action dans les Caraïbes, en Amérique Centrale, en Asie du Sud-Est et au Bangladesh. Par ailleurs, au lieu de répondre exclusivement aux demandes de financements spécifiques d'ONG, d'organisations internationales et de gouvernements, ECHO souhaite préparer des plans d'action et déterminer les partenaires les plus appropriés pour une mise en oeuvre dirigée par ECHO même. En outre, le DIPECHO a pour objet de rendre plus efficace l'action de l'ensemble de l'Union Européenne, par une étroite coordination de son action avec celles de la Commission et des Etats Membres. Il est enfin prévu de faire précéder la préparation des plans d'action par une phase de diagnostic au cours de laquelle seront identifiés, pour chaque région, les risques, les structures et politiques de prévention existantes aux niveaux communautaire, national et régional, ainsi que les appuis extérieurs en cours et à venir. L'objectif est non seulement de déterminer les lacunes, mais également d'évaluer la cohérence et l'efficacité des systèmes de réponse dans leur ensemble......Dans ce contexte, une première mission exploratoire a été réalisée du 30 septembre au 12 octobre 1996 dans les Caraïbes et l'Amérique Centrale (quatre pays visités) et a débouché sur un premier rapport (A. Angulo, Ch. Bugnion, Ph. Masure, "Rapport de mission exploratoire dans les Caraïbes ct en Amérique Centrale pour DIPECHO").Ce rapport apporte de nombreuses informations et en particulier:(1) il définit le cadre conceptuel, insistant, à juste titre, sur le fait que la prévention et la préparation doivent être distinguées de l'aide d'urgence et qu'elles font partie d'un processus continu au même titre que le développement ;(2) il présente les principales organisations régionales et internationales, et leurs activités dans le domaine de la prévention et de la préparation;(3) il met en évidence les grands types de besoins et fournit les premières orientations pour le programme DIPECHO......Le présent rapport, constituant le diagnostic proprement dit, fait suite à une deuxième série de missions effectuées dans la même région. Il vise à compléter les apports de la mission exploratoire, notamment par:(a) une analyse des catastrophes et de leurs conséquences:(b) une évaluation comparée des risques dans la région;(c) une analyse détaillée des réalisations et des besoins en matière de réduction des risques et des conséquences des catastrophes naturelles ;(d) un examen des conditions actuelles pour un programme DIPECHO cohérent, réalisable et efficace, avec, en particulier, la prise en compte de l’organisation actuelle de la prévention et de la préparation dans la région et un état des appuis extérieurs ;- des propositions de lignes d'actions prioritaires pour le DIPECHO......Le diagnostic s'est appuyé sur une importante documentation : travaux scientifiques, études et rapports recueillis auprès du CRED-Université Catholique de Louvain, du CIFEG, du DHA, de l’IDNDR, de divers organismes sur le terrain (notamment le centre de documentation de San José au Costa Rica), et d'universités européennes (Université de Savoie. Chambéry, Université de Lausanne). Mais ce sont avant tout les nombreux entretiens menés lors des missions (près de 200) qui ont donné corps au diagnostic.Treize pays Ont été visités entre le 22/01 et le 07/03/1997 :- République Dominicaine (C Misson);- Costa Rica, Guatemala, Nicaragua et Cuba (R. D'Ercole) ;- Antigua, Barbade, Haïti, Jamaïque, Ste-Lucie, St-Maarten, St-Vincent et le Guyana (Th. Lesales).Leur choix a été déterminé en concertation avec ECHO, le CRED-UCL et le CIFEG. Ils ne recouvrent pas l'ensemble des pays qu'il aurait été théoriquement possible de visiter. Cependant, le choix de pays-clés, les contacts établis avec de nombreux organismes de portée régionale et la documentation consultée, ont permis de bâtir un diagnostic d'ensemble......L'étude comporte trois parties.La 1e partie constitue une analyse des catastrophes en termes de bilan et de risque. Il s'agit, à l'aide de cartes, notamment, de montrer les effets des catastrophes naturelles en Amérique Centrale et dans les Caraïbes, de présenter la répartition et la fréquence des aléas naturels et de procéder à une analyse de critères de vulnérabilité. L'objectif est, enfin, de déterminer des niveaux de risque, à l'échelle de la région, compte tenu des dangers naturels et des critères de vulnérabilité.La 2° partie est l'étude des actions entreprises dans la région, ces dernières années, afin de réduire les risques et les conséquences des catastrophes. Cette étude permet de dégager des lacunes et des besoins. Les différentes composantes entrant dans le processus de réduction des catastrophes sont retenues : recherche scientifique et technique, prévention stricto sensu, préparation, information / formation. L'accent est également placé sur les modes actuels d'application des politiques de réduction des risques : de l'approche sectorielle à l'approche intégrée.La 3e partie traite des conditions actuelles pour la mise en oeuvre d'un programme DIPECHO cohérent et efficace. Quatre aspects fondamentaux sont analysés: les particularités régionales et nationales (l'hétérogénéité et ses conséquences); les faiblesses et qualités institutionnelles aux différents échelons géographiques: les caractéristiques des organismes susceptibles de contribuer à la mise en oeuvre du DIPECHO; le rôle actuel et en perspective de la Communauté Européenne et des Etats Membres.Chaque partie comporte une conclusion partielle La conclusion générale reprend les idées force des conclusions intermédiaires ct débouche sur des lignes d'actions prioritaires recommandées pour le DIPECHO......L'étude confiée au CIFEG par le CRED-UCL et ECHO a été coordonnée par Robert D'Ercole (Département de Géographie, Université de Savoie, Chambéry, France). Elle a bénéficié de la collaboration de Thierry Lesales (Département de Géographie, Université des Antilles et de la Guyane, Martinique, France) et de Patrick Pigeon (Département de Géographie, Université de Savoie, Chambéry, France). Ont également contribué à la réalisation de celle étude: Claudine Misson (CRED-UCL, Belgique), Jean-Claude Napias (CIFEG, directeur), Jacques Giri (CIFEG, président), Sylvie Orlyk (CIFEG, secrétariat).
https://hal.archives-ouvertes.fr/hal-01196496

hal-01196496
https://hal.archives-ouvertes.fr/hal-01196496
https://hal.archives-ouvertes.fr/hal-01196496/document
https://hal.archives-ouvertes.fr/hal-01196496/file/D%27Ercole%20et%20al%201997%20Diagnostic%20DIPECHO%20Caraibes%20compressed.pdf

Éditeur(s) : HAL CCSD Oxford University Press (OUP)
Résumé : International audience
We report on microstructural data obtained by optical microscopy and transmission electron microscopy concerning the crystallographic relationships of serpentine minerals with their host olivine in two contrasting situations. In the first case, mesh-textured lizardite (liz) is developed in a standard 60% serpentinized oceanic harzburgite from the Oman ophiolite where olivine converts to columnar lizardite. The joined columns are perpendicular to the basal plane (001)(liz), corresponding to the pseudofibres observed optically. The plane (001)(liz) is locally parallel to the narrow boundary ol-liz; thus column orientations register the interface of serpentinization. The ol-liz relationships are not strictly topotactic, but reflect preferred cracking orientations in olivine, parallel to (010)(ol). In the second case, antigorite (atg) develops in a rare sample of antigorite schist in a kimberlite from Moses Rock (Colorado Plateau), representative of a suprasubduction-zone mantle wedge. High-resolution transmission electron microscopy (HRTEM) images along [010](atg) show domains of very regular modulation with a 43 center dot 5 A wavelength (m = 17, where m is the number of silicate tetrahedra along the wave), with few defects, indicative of HP-HT antigorite, and also heavily kinked regions as fingerprints of strong tectonic shear. TEM imaging and electron diffraction patterns reveal two topotactic relationships between antigorite and olivine: [100](atg)//[010](ol) and < 100 >(atg)//< 100 >(ol); the planes in contact are (001)(atg)//(100)(ol) and (001)(atg)//(010)(ol), respectively. The [010](atg)//[001](ol) and antigorite lamellae are parallel to the forsterite b-axis. In both cases, the topography of olivine-serpentine interfaces is controlled by open fluid pathways along microcracks oriented according to the anisotropy of the olivine aggregate. In the cases studied, the serpentine aggregate exhibits a preferred orientation inherited from that of the peridotite. These results have some relevance to the seismic anisotropy of serpentinized mantle. Anisotropy of propagation of seismic waves as a result of the olivine fabric is maintained and reinforced with the development of lizardite. Conversely, the development of antigorite produces a trench-parallel fast S-wave polarization and an anisotropy that is lowered at low degrees of serpentinization and then increased with increasing serpentinization.
ISSN: 0022-3530

hal-00456061
https://hal.archives-ouvertes.fr/hal-00456061
DOI : 10.1093/petrology/egp049

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
We experimentally studied the predatory behavior of Polybia rejecta (Vespidae, Polistinae, Epiponini) towards 2-88 mm-long insects attracted to a UV light trap. Foragers, which began to hunt at 6:30, selected 4-14 mm-long prey insects. Prey detection by sight by hovering wasps was confirmed using decoys. After the wasps landed and walked along a sinuous path, prey were detected by contact or from a distance (1-3cm). This was followed by seizure, stinging (contrarily to most other known cases), prey manipulation and retrieval. Prey that flew off might be caught in flight. The prey load, representing 30.7% of a forager's weight, was optimized by capturing up to six small prey or two medium-sized prey successively (both of which might be consumed in situ). The foragers cut off the wings of larger prey or cut them into two pieces and returned to gather the second piece. The handling time increased exponentially with the weight of the prey. Partial loading (i.e., retrieving a load much inferior to the maximum possible) was likely related to social facilitation, a form of nest-based recruitment that was demonstrated through the experimental elimination of local enhancement by removing foragers (both mechanisms favor the exploitation of favorable patches).
ISSN: 0376-6357

hal-01533217
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01533217
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01533217/document
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01533217/file/Dejean%20et%20al.%20-%20The%20predatory%20behavior%20of%20the%20Neotropical%20social%20w.pdf
DOI : 10.1016/j.beproc.2017.05.011

Éditeur(s) : HAL CCSD
Résumé : International audience
Metamorphic soles correspond to m to 500m thick tectonic slices welded beneath most of the large-scale ophiolites.They typically show a steep inverted metamorphic structure where the pressure and temperature conditions ofcrystallization increase upward (from 500100ºC at 0.50.2 GPa to 800100ºC at 1.00.2 GPa), with isogradssubparallel to the contact with the overlying ophiolitic peridotite. The proportion of mafic rocks in metamorphicsoles also increases from the bottom (meta-sediments rich) to the top (approaching the ophiolite peridotites). Thesesoles are interpreted as the result of heat transfer from the incipient mantle wedge toward the nascent slab (associatedwith large-scale fluid transfer and possible shear heating) during the first My of intra-oceanic subduction(as indicated by radiometric ages). Metamorphic soles provide therefore major constraints on early subductiondynamics (i.e. thermal structure, fluid migration and rheology along the nascent slab interface).We present a detailed structural and petrological study of the metamorphic sole from 4 major cross-sections alongthe Oman ophiolite. We show precise pressure–temperature estimates obtained by pseudosection modelling andEBSD measurements performed on both the garnet-bearing and garnet-free high-grade sole. Results allow quantificationof the micro-scale deformation and highlight differences in pressure–temperature–deformation conditionsbetween the 4 different locations, showing that the inverted metamorphic gradient through the sole is not continuousin all locations.Based on these new constraints, we suggest a new tectonic–petrological model for the formation of metamorphicsoles below ophiolites. This model involves the stacking of several homogeneous slivers of oceanic crust leadingto the present-day structure of the sole. In this view, these thrusts are the result of rheological contrasts between thesole and the peridotite as the plate interface progressively cools down. These slivers later underwent several stagesof retrogression (partly mediated by ascending fluids from the slab) from amphibolite- to prehnite/pumpellite-faciesconditions.
Geophysical Research Abstracts
Vienne, Austria

insu-01309369
https://hal-insu.archives-ouvertes.fr/insu-01309369

Éditeur(s) : HAL CCSD Taylor & Francis
Résumé : International audience
The Jurassic Mirdita ophiolite crops out in the western branch of the Hellenide-Dinaride ophiolite belt in the Balkan Peninsula; it represents a remnant of the Tethyan oceanic lithosphere developed between the Apulian and Pelagonian microcontinents. Emplaced during the Cretaceous on the western margin of Pelagonia, the Mirdita ophiolite was involved in southwestward thrusting of the Hellenide-Dinaride tectonic units during the Eocene alpine tectonics. It was little affected, however, by these alpine events as marked by nearly horizontal Cretaceous limestone deposits overlying the ophiolite. A continuous section of Middle Jurassic oceanic crust, including thin gabbros, a N-S-trending sheeted dike complex, and extrusive rocks, is exposed in the central part of the ophiolite and thickens eastward within a regional, N-S-trending synform. Peridotite massifs exposed along the western and eastern edges of this synform show major structural and petrological differences. The eastern ultramafic domain has a harzburgitic mantle exhibiting a high-temperature asthenospheric foliation dipping steeply to moderately to the west. Major chromite deposits are restricted to these eastern ultramafic massifs. The western ultramafic domain has a zoned mantle, with asthenospheric harzburgite exposed at its western margin, progressively replaced eastward by plagioclase-peridotites that were highly strained at low temperatures, and that are bounded by amphibole-peridotites along with crustal rocks. The occurrence of plagioclase is ascribed to melt impregnation processes that occurred immediately before or during intense lithospheric deformation. The gabbros in the eastern massifs are thicker (1-2 km and layered, whereas they are highly thin and discontinuous in the western massifs. Mantle peridotites of the western massifs locally are in direct contact with the overlying diabase and volcanic rocks along ductile shear zones. Development of epidote-amphibolite facies metamorphism in upper-crustal rocks was produced by hydrothermal alteration in the oceanic realm, and was intense and widespread in the western domain. The Mirdita ophiolite likely originated in a short-lived, narrow ocean basin, which was closed during the Middle Jurassic by eastward overthrusting of the western domain, and westward subduction of the eastern domain. This constrictional phase was followed by dextral oblique convergence between the Pelagonian and Apulian microcontinents. This model implies a parautochtonous origin of the Mirdita ophiolite between these two microcontinents.
ISSN: 0020-6814

hal-00456063
https://hal.archives-ouvertes.fr/hal-00456063
DOI : 10.1080/00206810902823982

Éditeur(s) : HAL CCSD Elsevier
Résumé : Integrated field, LA-MC-ICP-MS geochronology and geochemical data from the Novo Oriente Group have been investigated in order to determine their provenance and possible tectonic setting. This group in the southwestern portion of the Ceara Central Domain, is a well-preserved metavolcanosedimentary sequence, in part exhalative, composed of two distinct formations. The proximal coastal Bonsucesso Formation comprises mainly quartzite and minor basic metavolcanic rocks and is in gradational contact with the distal Caranbas Formation which constitutes a metapelitic-volcanic-carbonate sequence, including metabasic rocks with pillow structure and sheared serpentinized ultrabasic rocks. The youngest detrital zircon found in the quartzite of the Bonsucesso Formation yielded an age of ca. 2.1 Ga and well-defined peaks around 2.2.2.3-2.4 and 2.5 Ga. In addition, zircons from a related metabasalt yielded an upper intercept age of 2083 +/- 28 Ma. We interpret the zircons found in this metabasalt as inherited from the host quartzite. This fact is supported by depleted-mantle Nd model ages (T-DM age) from correlated metabasic and metaultrabasic rocks from other places in the Novo Oriente sequence, which have yielded ages between 1.36 and 1.69 Ga, that is younger than the zircon age obtained in the metabasalt extruded over the Bonsucesso quartzite. Geochemical data of the metasedimentary rocks from the Caraubas Formation indicates a provenance composed of a mixture of felsic and intermediate sources typical of old stable cratons and older continental roots of active tectonic settings. The rocks of the Crania (Medio Coreau Domain) and Bacaja Complexes (southeastern Amazonian Craton) exposed to the west of the Novo Oriente Group, and largely covered by the Phanerozoic Parnaiba intracratonic basin, are the most likely source rocks. Since the precise age of the Novo Oriente Group is not yet well constrained, two distinct settings may be proposed: (1) it may represent a more evolved basin developed from extensional processes during the Mesoproterozoic (ca. 1.5-1.3 Ga); and (2) it could constitute part of the passive margin systems developed during the break-up of the Rodinia crown copyright supercontinent (ca. 0.95-0.8 Ga), associated with a pre-Brasiliano/Pan-African ocean (e.g. Pharusian Ocean). Crown.
ISSN: 1342-937X

hal-00512825
https://hal.archives-ouvertes.fr/hal-00512825
DOI : 10.1016/j.gr.2010.02.001

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Before attaining the mantle wedge, where they trigger partial melting, volatiles released from dehydration reactions in the slab have to migrate across a relatively cold (<750 degrees C), peridotite-layer above the incoming slab. In order to unravel the mechanisms allowing for this initial stage of fluid transport, we performed a detailed field and microstructural study of metamorphic prograde peridotites in the Cerro del Almirez ultramafic massif (Betic Cordillera, Spain), where evidences of one of the most important dehydration reactions in subduction zones, the high-pressure antigorite breakdown (P = 1.6-1.9 GPa and T approximate to 680 degrees C), can be mapped in the field. This reaction led to arborescent growth of centimeter-size olivine and orthopyroxene, producing a chlorite-harzburgite with a spinifex-like texture. Microstructural observations and crystal preferred (CPO) mapping show no evidences of solid-state deformation during the prograde growth of olivine and orthopyroxene at the expenses of antigorite. However, a few tens to a hundred meters away from the reaction front, the metamorphic texture is partially obliterated by grain-size reduction in roughly planar conjugate zones, a few mm to meters wide. Grain size reduction zones (GSRZ) are characterized by (1) sharp contacts with undeformed spinifex-like texture domains, (2) important reduction of the olivine grain size (60-250 mu m), (3) olivine color change from brownish to colorless, (4) decrease in the modal amount of orthopyroxene, and (5) at the mm- to cm-scale, irregular shapes and abrupt terminations. Field and microstructural observations exclude that relative displacement took place across these GSRZ. Changes in modal composition imply reactions with fluids undersaturated in silica. Analysis of olivine crystal-preferred orientations (CPO) in GSRZ shows patterns similar, but more dispersed, than those in neighboring spinifex-like domains. It also reveals mm- to cm-scale discrete domains with rather homogeneous crystallographic orientations suggesting inheritance from the preexisting spinifex-like olivines in the host peridotite. Misorientation angles between neighboring grains in the GSRZ show peaks at similar to 5-10 degrees and similar to 20 degrees, but rotations are not crystallographically controlled. Based on these observations, we rule out the formation of the GSRZ by dynamic recrystallization during dislocation creep and propose that they record brittle deformation (microcraking) of the spinifex-like chlorite-harzburgite, probably induced by hydrofracturing at high pressure and relative low temperature conditions (680-710 degrees C). High-pressure hydrofracturing can, thus, be invoked as an efficient mechanism for fluid flow across the cold top-slab mantle layer, hence allowing the slab-derived fluids to ingress in the wedge.
ISSN: 0012-821X

hal-00534035
https://hal.archives-ouvertes.fr/hal-00534035
DOI : 10.1016/j.epsl.2010.06.029