Éditeur(s) : HAL CCSD American Chemical Society
Résumé : International audience
Four bicyclic and three pentacyclic guanidine alkaloids (1–7) were isolated from a French Polynesian Monanchora n. sp. sponge, along with the known alkaloids monalidine A (8), enantiomers 9–11 of known natural product crambescins, and the known crambescidins 12–15. Structures were assigned by spectroscopic data interpretation. The relative and absolute configurations of the alkaloids were established by analysis of 1H NMR and NOESY spectra and by circular dichroism analysis. The new norcrambescidic acid (7) corresponds to interesting biosynthetic variation within the pentacyclic core. All compounds exhibited antiproliferative and cytotoxic efficacy against KB, HCT116, HL60, MRC5, and B16F10 cancer cells, with IC50 values ranging from 4 nM to 10 μM.
ISSN: 0163-3864

hal-01584556
https://hal.archives-ouvertes.fr/hal-01584556
DOI : 10.1021/acs.jnatprod.6b00168

Éditeur(s) : HAL CCSD SAGE Publications (UK and US)
Résumé : International audience
In this article, we focus on hypomaturation autosomal-recessive-type amelogenesis imperfecta (type IIA2) and describe 2 new causal Matrix metalloproteinase 20 (MMP20) mutations validated in two unrelated families: a missense mutation p.T130I at the expected homozygous state, and a compound heterozygous mutation having the same mutation combined with a nucleotide deletion, leading to a premature stop codon (p.N120fz*2). We characterized the enamel structure of the latter case using scanning electron microscopy analysis and microanalysis (Energy-dispersive X-ray Spectroscopy, EDX) and confirmed the hypomaturation-type amelogenesis imperfecta as identified in the clinical diagnosis. The mineralized content was slightly decreased, with magnesium substituting for calcium in the crystal structure. The anomalies affected enamel with minimal inter-rod enamel present and apatite crystals perpendicular to the enamel prisms, suggesting a possible new role for MMP20 in enamel formation.
ISSN: 0022-0345

hal-01545484
https://hal.archives-ouvertes.fr/hal-01545484
DOI : 10.1177/0022034513488393

Éditeur(s) : HAL CCSD American Society for Microbiology
Résumé : International audience
: We investigated the in vitro effects of four alkyl-galactofuranoside derivatives, i.e. octyl-β-D-galactofuranoside (1), 6-amino-β-D-galactofuranoside (2), 6-N-acetamido-β-D-galactofuranoside (3), and 6-azido-β-D-galactofuranoside (4) on Leishmania donovani. Their mechanism of action was explored using electron paramagnetic resonance spectroscopy (EPR) and nuclear magnetic resonance (NMR), and ultrastructural alterations by transmission electron microscopy (TEM). Compound 1 showed the most promising effects by inhibiting promastigote growth at IC50 8.96 ± 2.5 μM. All compounds exhibit low toxicity towards human macrophages. Compound 1 had a higher selectivity index than the comparative molecule used, i.e. miltefosine (159.7 versus 37.9, respectively). EPR showed that compound 1 significantly reduced membrane fluidity, compared to control promastigotes and to compound 3. The furanose ring was shown to support this effect since the isomer galactopyranose had no effect on parasite membrane fluidity or growth. NMR showed a direct interaction of all compounds (1>2>3>4) with the promastigote membrane, as well as with octyl-galactopyranose and octanol, providing evidence that the n-octyl chain was primarily involved in the anchoring with the parasite membrane, followed by the putative crucial role of furanose ring in the anti-leishmanial activity. A morphologic analysis of compound 1-treated promastigotes by TEM revealed profound alterations on parasite membrane and organelles, but not with compound 3. Quantification of annexinV binding by flow cytometry confirmed that compound 1 induced apoptosis in >90% promastigotes. The effect of compound 1 was also assessed on intra-macrophagic amastigotes, and showed a reduction in amastigote growth associated with an increase of ROS production, thus validating its promising effect.
ISSN: 0066-4804

hal-00941772
https://hal.archives-ouvertes.fr/hal-00941772
PUBMED : 24468785
DOI : 10.1128/AAC.01350-13

Éditeur(s) : HAL CCSD IOP Publishing
Résumé : The use of electron probe microanalysis (EPMA) at low voltage allows improvements in the lateral resolution and surface sensitivity of the technique down to the sub-micrometre scale, and it is also useful in minimizing X-ray absorption (for the analysis of ultra-light elements), charging effects and secondary fluorescence. However, EPMA at low voltage is accompanied by a number of problems which may affect the accuracy of quantitative results. A large number of these problems arise from the need of using low-energy X-ray lines such as L- and M-lines, which have low fluorescence yields, large uncertainties in the mass attenuation coefficients, and are affected by several spectroscopic difficulties (e.g., peak shifts and overlaps). Other factors that play an important role at low voltage are carbon contamination, surface oxidation, the quality of sample polishing, the influence of a conductive coating and the limitations of matrix correction procedures. In this paper, we illustrate the capabilities of EPMA at low voltage and we examine in detail the different sources of uncertainty that may affect the accuracy of quantitative results.
ISSN: 1757-8981

hal-00767564
https://hal.archives-ouvertes.fr/hal-00767564
DOI : 10.1088/1757-899X/32/1/012016

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Four fibers from banana-trees (leaf, trunk) and coconut-tree (husk, fabric) were examined before their incorporation in cementitious matrices, in order to prepare insulating material for construction. Their botanical compositions have been determined following a method described previously. Thermal degradation of these fibers were studied between 200 and 700 °C under nitrogen gas flow. Temperature of pyrolysis was the experimental parameter investigated. The solid residues obtained were analyzed by classical elemental analysis, Fourier Transform Infra Red (FTIR) spectroscopy and were observed by Scanning Electron Microscopy (SEM). This study has shown (1) the relation between botanical, chemical composition with both localization of fibers in the tree and type of tree; (2) the rapid and preferential decomposition of banana fibers with increasing temperature of pyrolysis and (3) the rough samples are made of hollow fibers.
ISSN: 0960-8524

hal-00809780
https://hal.univ-antilles.fr/hal-00809780
DOI : 10.1016/j.biortech.2005.11.030

Éditeur(s) : HAL CCSD Springer Verlag (Germany) Springer Verlag
Résumé : International audience
We have investigated the partitioning of Fe3+ between orthopyroxene (Opx) and garnet (Grt) in well-equilibrated mantle xenoliths using Mössbauer spectroscopy. The samples cover a wide range of P–T conditions (2.1–6.6 GPa, 690–1,412 °C) and geothermal gradients, and are thus representative for Earth’s upper mantle in both on-craton and off-craton continental settings. Garnet has Fe3+/Fetot ratios of 0.03–0.13 and Fe2O3 contents of 0.24–1.00 wt%. Orthopyroxene has, on average, lower Fe3+/Fetot ratios (0.01–0.09) and Fe2O3 contents (0.05–0.63 wt%). In low-pressure, high-temperature samples, however, Opx is systematically richer in Fe2O3 than the coexisting Grt. The Fe3+ Opx/Grt partition coefficient (DOpx/GrtFe3+) shows no obvious relationship with temperature, but increases with decreasing pressure and with increasing NaOpx. The observed Opx/Grt Fe3+ systematics imply that the Opx–Grt Fe–Mg exchange thermometer is not robust against redox changes if total Fe is treated as Fe2+. An approximate evaluation of errors on T estimates due to redox effects predicts negligible deviations for strongly reduced conditions (<65 °C), but potentially large deviations (> to ≫100 °C) for strongly oxidized conditions, especially at very high pressure and when both P and T are calculated by iteration.
ISSN: 0010-7999

hal-01121606
https://hal.archives-ouvertes.fr/hal-01121606
DOI : 10.1007/s00410-014-1101-8

Éditeur(s) : HAL CCSD
Résumé : International audience
The effect of alkaloids extracted from Isertia coccinea plant (AEIC) on the corrosion of C38 steel in 1 M hydrochloric acid was investigated by electrochemical impedance spectroscopy (EIS) and potentiodynamic polarization techniques. Potentiodynamic polarization curves indicated that the extract behave as mixed-type inhibitor. The experimental data obtained from EIS method show a frequency distribution and therefore a modelling element with frequency dispersion behaviour, a constant phase element (CPE) has been used. The inhibition efficiencies of the extract calculated by three methods show the same tendency. Inhibition was found to increase with increasing concentration of the plant extract. The results obtained show that the extract solution of the plant could serve as an effective inhibitor for the corrosion of C38 steel in hydrochloric acid solution. The apparent activation energy of the process taking place in inhibitor presence was determined on the ground of four temperature values in the range from 25 °C to 55 °C using the data obtained by two independent methods. Theoretical fitting of different isotherms, Langmuir, Temkin and Frunkin, were tested to clarify the nature of adsorption.
International journal of electrochemical science

hal-01097030
https://hal-agroparistech.archives-ouvertes.fr/hal-01097030

Éditeur(s) : HAL CCSD European Geosciences Union
Résumé : International audience
An increasing number of field examples in mountain belts show that the formation of passive margins during extreme continent thinning may occur under conditions of high to very high thermal gradient beneath a thin cover of syn-rift sediments. Orogenic belts resulting from the tectonic inversion of distal margins and regions of exhumed continental mantle may exhibit high-temperature, low-pressure (HT-LP) metamorphism and coeval syn-extensional, ductile deformation. Recent studies have shown that the northern flank of the Pyrenean belt, especially the North Pyrenean Zone, is one of the best examples of such inverted hot, passive margin. In this study, we provide a map of HT-LP metamorphism based on a data set of more than 100 peak-temperature estimates obtained using Raman spectroscopy of the carbona-ceous material (RSCM). This data set is completed by previous PT (pressure and temperature) estimates based on mineral assemblages, and new 40 Ar– 39 Ar (amphibole, micas) and U–Pb (titanite) ages from metamorphic and magmatic rocks of the North Pyrenean Zone. The implications on the geological evolution of the Cretaceous Pyrenean paleomar-gins are discussed. Ages range mainly from 110 to 90 Ma, and no westward or eastward propagation of the metamor-phism and magmatism can be clearly identified. In contrast, the new data reveal a progressive propagation of the thermal anomaly from the base to the surface of the continental crust. Focusing on the key localities of the Mauléon basin, Arguenos–Moncaup, Lherz, Boucheville and the Bas-Agly, we analyze the thermal conditions prevailing during the Cre-taceous crustal thinning. The results are synthetized into a series of three regional thematic maps and into two detailed maps of the Arguenos–Moncaup and Lherz areas. The results indicate a first-order control of the thermal gradient by the intensity of crustal thinning. The highest grades of metamor-phism are intimately associated with the areas where subcon-tinental mantle rocks have been unroofed or exhumed.
ISSN: 1869-9510

insu-01161826
https://hal-insu.archives-ouvertes.fr/insu-01161826
https://hal-insu.archives-ouvertes.fr/insu-01161826/document
https://hal-insu.archives-ouvertes.fr/insu-01161826/file/PL03457.pdf
DOI : 10.5194/se-6-643-2015

Éditeur(s) : HAL CCSD IWA Publishing
Résumé : International audience
Anti-cancer drugs are an important class of pharmaceutical products. Methotrexate (MTX) is a folic acid antagonist used in high doses as antimetabolite in anti-cancer treatment as well as in low doses for the treatment of rheumatoid arthritis and adults' psoriasis. In the past, several anti-cancer drugs, including methotrexate, have been found in the environment. Their presence in water, especially if used for the production of drinking water, is even in low concentrations of particular interest, due to the risk to retrieve them in the consumed water and their high activity and grave effects. But prior to usage as drinking water, raw waters are treated and chlorination is a common practice in several countries. As such a treatment can lead to the formation of organochlorine in water, the study of the fate of MTX during chlorination in a batch trial was carried out. The reaction was monitored by dissolved organic carbon (DOC) and by fluorescence and UV spectroscopy. Investigation of by-products formed was done with liquid chromatography/mass spectrometry (LC/MS). Under the given experimental conditions, Methotrexate was eliminated rapidly (t1/2 around 21 min). However, DOC elimination was incomplete. Monitoring with LC-MS showed the formation of a monochlorinated transformation product of MTX. In silico analysis of the proposed transformation products for different carcinogenic, mutagenic and genotoxic endpoints with different software platforms provided no clear evidence that the possible transformation products after chlorination might be more toxic than the parent compound. However, since a number of alerts is altered after chlorination, it cannot be excluded that the toxicity of these transformation products might be modulated compared with the parent compound.
ISSN: 0043-1354

hal-01016617
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01016617
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01016617/document
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01016617/file/Monitoringsur methotrexate_final.pdf
DOI : 10.1016/j.watres.2014.03.008

Éditeur(s) : HAL CCSD Wiley
Résumé : International audience
Sickle cell anemia (SS) is characterized by a reduced cerebral microvascular oxygen saturation (cerebral TOI), which is not associated with hemoglobin concentration. Cerebral TOI has never been studied in sickle cell-hemoglobin C disease (SC). We focused on the relationships between hemorheological alterations and cerebral TOI in sickle cell patients with no cerebral vasculopathy and on the usefulness of TOI variability to assess the cerebral vasomotion activity. The blood rheological profile, the level of cerebral TOI (spatial resolved spectroscopy) and the cerebral TOI variability, which reflects vasomotion activity, were compared between 20 healthy subjects (AA), 21 SC patients, and 21 SS patients. Cerebral TOI exhibited the following order: AA > SC > SS. The low cerebral TOI in SS patients was related to red blood cell aggregation and deformability properties. The cerebral TOI variability of SS and SC patients was increased above healthy values and vasomotion activity was negatively associated with the reduced cerebral TOI in SS patients. We demonstrated that (1) blood rheology could be involved in the reduced cerebral TOI in SS patients but not in SC patients; (2) vasomotion activity is increased in SS and SC patients to compensate for the reduced cerebral TOI.
ISSN: 0361-8609

inserm-00838966
http://www.hal.inserm.fr/inserm-00838966
http://www.hal.inserm.fr/inserm-00838966/document
http://www.hal.inserm.fr/inserm-00838966/file/2013_Waltz_American_Journalsur Hematology.pdf
DOI : 10.1002/ajh.23318

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Alpine Corsica consists of a stack of variably metamorphosed units of continental and Tethys-derived rocks. It represents an excellent example of high-pressure (HP) orogenic belt, such as the Western Alps, exposed over a small and accessible area. Compared to the Western Alps, the geology of Alpine Corsica is poorly unraveled. During the 1970s-80s, based on either lithostratigraphic or metamorphic field observations, various classifications of the belt have been proposed, but these classifications have been rarely matched together. Furthermore, through time, the internal complexity of large domains has been progressively left aside in the frame of large-scale geodynamic reconstructions. As a consequence, major open questions on the internal structure of the belt have remained unsolved. Apart from a few local studies, Alpine Corsica has not benefited of modern developments in petrology and basin research. This feature results in several uncertainties when combining lithostratigraphic and metamorphic patterns and, consequently, in the definition of an exhaustive architecture of the belt. In this paper we provide a review on the geology of Alpine Corsica, paying particular attention to the available lithostratigraphic and metamorphic classifications of the metamorphic terranes. These data are completed by a new and exhaustive metamorphic dataset obtained by means of thermometry based on Raman Spectroscopy of Carbonaceous Material (RSCM). This technique provides reliable insights on the peak temperature of the metamorphic history for CM-bearing metasediments. A detailed metamorphic characterization of metasediments, which have been previously largely ignored due to retrogression or to the lack of diagnostic mineralogy, is thus obtained and fruitfully coupled with the available lithostratigraphic data. Nine main tectono-metamorphic units are defined, from subgreenschist (ca. 280-300 °C) to the lawsonite-eclogite-facies (ca. 500-550 °C) condition. These units are homogeneous in metamorphism, laterally continuous and have characteristic lithostratigraphic features. This study also suggests a direct link between the pre-orogenic extensional setting and the present-day compressional structure of Alpine Corsica, indicating that large sections of subducted lithosphere were subducted and exhumed as coherent domains. These features provide important insight on the mechanism of stacking and exhumation of HP rocks, and make Alpine Corsica a unique reference for mountain-building processes in Tethyan-type orogens.
ISSN: 0012-8252

hal-00814433
https://hal.archives-ouvertes.fr/hal-00814433
DOI : 10.1016/j.earscirev.2012.10.003

Éditeur(s) : HAL CCSD
Résumé : International audience
We present an overview of the Mid-Cretaceous hyper-extended rift systemexposed in the northern part of the Pyrenean mountain range. Itsinversion during the Pyrenean orogeny allows for precious observationsof the deep-seated processes occurring at the foot of distal margins.Some peculiar aspects characterizing the pre-Alpine hyper-extended domainare examined throughout the 400 km long suture that is fossilizedin the North Pyrenean Zone (NPZ). The high temperature/low pressure(HT/LP) thermal imprint of the extensional event is studied thanksto a dataset of more than hundred peak temperature measurementsby Raman spectroscopy of the carbonaceous material (RSCM). Thepre- and syn-rift metasediments are characterized by an intense, synmetamorphicductile deformation. Focusing on several key-localitiesof the NPZ, we examine the emplacement conditions of the peridotitesin response to this extreme crustal thinning. Geological evidencessuch as the occurrence of peridotite bodies directly underlying metamorphicpre-rift sediments indicate an early attenuation of the rifted continentalcrust. Moreover, syn-rift, Albian-Cenomanian flysch sequenceswere deposited synchronously with the syn-metamorphic ductile deformationof the pre-rift sequences. All along the Internal MetamorphicZone (IMZ), the base of the flysch deposits also recorded the HT tectonicevent. Such a synchronicity between geological events, which aregenerally separated in time, is not common in mountain belts. We examinehow tectonics, metamorphism and sedimentation may be activein a single basin during extension. We propose an original mechanismfor the evolution of the basins involving continuous basal extraction ofthe pre-rift metamorphic sediments. This early HT deformation eventrelates to the « phase anté-Cénomanienne » described by Pyrenean geologistssince 1930.
24 ème Réunion des sciences de la Terre 2014
Pau, France

insu-01080795
https://hal-insu.archives-ouvertes.fr/insu-01080795

Éditeur(s) : HAL CCSD Springer Verlag (Germany) Springer Verlag
Résumé : International audience
The Cerro del Almirez massif (Spain) represents a unique fragment of serpentinized oceanic lithosphere that has been first equilibrated in the antigorite stability field (Atg-serpentinites) and then dehydrated into chlorite–olivine–orthopyroxene (Chl-harzburgites) at eclogite facies conditions during subduction. The massif preserves a dehydration front between Atg-serpentinites and Chl-harzburgites. It constitutes a suitable place to study redox changes in serpentinites and the nature of the released fluids during their dehydration. Relative to abyssal serpentinites, Atg-serpentinites display a low Fe3+/FeTotal(BR) (=0.55) and magnetite modal content (=2.8–4.3 wt%). Micro-X-ray absorption near-edge structure (μ-XANES) spectroscopy measurements of serpentines at the Fe–K edge show that antigorite has a lower Fe3+/FeTotal ratio (=0.48) than oceanic lizardite/chrysotile assemblages. The onset of Atg-serpentinites dehydration is marked by the crystallization of a Fe3+-rich antigorite (Fe3+/FeTotal = 0.6–0.75) in equilibrium with secondary olivine and by a decrease in magnetite amount (=1.6–2.2 wt%). This suggests a preferential partitioning of Fe3+ into serpentine rather than into olivine. The Atg-breakdown is marked by a decrease in Fe3+/FeTotal(BR) (=0.34–0.41), the crystallization of Fe2+-rich phases and the quasi-disappearance of magnetite (=0.6–1.4 wt.%). The observation of Fe3+-rich hematite and ilmenite intergrowths suggests that the O2 released by the crystallization of Fe2+-rich phases could promote hematite crystallization and a subsequent increase in fo2 inside the portion of the subducted mantle. Serpentinite dehydration could thus produce highly oxidized fluids in subduction zones and contribute to the oxidization of the sub-arc mantle wedge.
ISSN: 0010-7999

hal-01172310
https://hal.archives-ouvertes.fr/hal-01172310
DOI : 10.1007/s00410-015-1130-y

Éditeur(s) : HAL CCSD Mineralogical Society of America
Résumé : International audience
To test if hydrogen incorporation by ionic diffusion can occur between a volatile-rich kimberlitic liquid and forsterite, results of high-pressure and high-temperature experiments using a piston-cylinder apparatus at 1200–1300 °C and 1 GPa for durations of 1 min, 5 h, and 23 h, are reported here. Kimberlitic liquid in the system CaO-MgO-Al2O3-SiO2-CO2-H2O and synthetic forsterite single crystals were chosen as a first simplification of the complex natural kimberlite composition. Unpolarized Fourier transform infrared spectroscopy was used to quantify the concentrations of OH in the crystallographically oriented forsterite. Scanning electron microscopy, electron backscattered diffraction, electron microprobe analyses, and transmission electron microscopy were performed to identify the run products. After 5 and 23 h, a forsterite overgrowth crystallized with the same orientation as the initial forsterite single crystal. The kimberlitic liquid has crystallized as micrometer-scale euhedral forsterite neocrystals with random crystallographic orientations, as well as a nanoscale aluminous phase and a calcic phase. Despite theoretical water-saturation of the system and long duration, none of the initial forsterite single crystals display signs of hydration such as hydrogen diffusion profile from the border toward the center of the crystal. Most likely, the presence of CO2 in the system has lowered the H2O fugacity to such an extent that there is no significant hydration of the starting forsterite single crystal or its overgrowth. Also, the presence of CO2 enhances rapid forsterite crystal growth. Forsterite growth rate is around 2 × 108 μm3/h at 1250 °C. These experimental results suggest a deep mantle origin of the high OH content found in natural mantle-derived xenoliths transported in kimberlites, as reported from the Kaapvaal craton. In agreement with previous studies, it also points out to the fact that significant hydration must take place in a CO2-poor environment.
ISSN: 0003-004X

hal-01217157
https://hal.archives-ouvertes.fr/hal-01217157
DOI : 10.2138/am-2015-5200

Éditeur(s) : HAL CCSD Wiley-VCH Verlag
Résumé : International audience
Deciphering the assembly history of the Milky Way is a formidable task, which becomes possible only if one can produce high-resolution chrono-chemo-kinematical maps of the Galaxy. Data from large-scale astrometric and spectroscopic surveys will soon provide us with a well-defined view of the current chemo-kinematical structure of the Milky Way, but will only enable a blurred view on the temporal sequence that led to the present-day Galaxy. As demonstrated by the (ongoing) exploitation of data from the pioneering photometric missions CoRoT, Kepler, and K2, asteroseismology provides the way forward: solar-like oscillating giants are excellent evolutionary clocks thanks to the availability of seismic constraints on their mass and to the tight age-initial-mass relation they adhere to. In this paper we identify five key outstanding questions relating to the formation and evolution of the Milky Way that will need precise and accurate ages for large samples of stars to be addressed, and we identify the requirements in terms of number of targets and the precision on the stellar properties that are needed to tackle such questions. By quantifying the asteroseismic yields expected from PLATO for red-giant stars, we demonstrate that these requirements are within the capabilities of the current instrument design, provided that observations are sufficiently long to identify the evolutionary state and allow robust and precise determination of acoustic-mode frequencies. This will allow us to harvest data of sufficient quality to reach a 10% precision in age. This is a fundamental pre-requisite to then reach the more ambitious goal of a similar level of accuracy, which will only be possible if we have to hand a careful appraisal of systematic uncertainties on age deriving from our limited understanding of stellar physics, a goal which conveniently falls within the main aims of PLATO's core science.
ISSN: 0004-6337

hal-01541393
https://hal.archives-ouvertes.fr/hal-01541393
ARXIV : 1706.3778
BIBCODE : 2017AN....338..644M
DOI : 10.1002/asna.201713385

Éditeur(s) : HAL CCSD
Résumé : International audience
Sub-continental lithospheric mantle rocks are exhumed at the foot of magma-poor distal passive margins as aresponse to extreme stretching of the continental crust during plate separation. Remnants of the Northern Iberianpaleo-passive margin are now exposed in the North-Pyrenean Zone (NPZ) and represent field analogues to studythe processes of continental crust thinning and subcontinental mantle exhumation. The NPZ results from theinversion of basins opened between the Iberia and Europa plates during Albo-Cenomanian times. In the westernNPZ, the ‘Chaînons Béarnais’ ranges display a fold-and-thrust structure involving the Mesozoic sedimentarycover, decoupled from its continental basement and associated with peridotite bodies in tectonic contact withPalaeozoic basement lenses of small size. Continental extension developed under hot thermal conditions, asdemonstrated by the syn-metamorphic Cretaceous ductile deformation affecting both the crustal basement and theallochthonous Mesozoic cover.In this study, we present structural and geochemical data providing constraints to reconstruct the evolution ofthe northern Iberia paleo-margin. Field work confirms that the pre-rift Mesozoic cover is intimately associatedto mantle rocks and to thin tectonic lenses of crustal basement. It also shows that the pre-rift cover was detachedfrom its bedrock at the Keuper evaporites level and was welded to mantle rocks during their exhumation atthe foot of the hyper-extended margin. The crust/mantle detachment fault is a major shear zone characterizedby anastomosed shear bands defining a plurimetric phacoidal fabric at the top of the serpentinized mantle. Thedetachment is marked by a layer of metasomatic rocks, locally 20 meters thick, made of talc-chlorite-pyrite-richrocks that developped under greenschist facies conditions. Raman Spectroscopy on Carbonaceous Materials(RSCM), performed on the Mesozoic cover reveal that the entire sedimentary pile underwent temperatures rangingbetween 200C and 480C.We show that: (i) at the site of mantle rocks exhumation, the boudinaged pre-rift sediments have undergone drasticsyn-metamorphic thinning with the genesis of a S0/S1 foliation and, (ii) the Paleozoic basement has been ductilelydeformed, into thin tectonic lenses that remained welded to the exhumed mantle rocks. Therefore the overallcrustal rheology appears dominated by shallow levels having a ductile behavior. This rheology is related to thepresence of a thick pre- and syn-rift decoupled cover acting as an efficient thermal blanket. This new geologicaldata set highlights important characteristics of ductile-type hyper-extended passive margin that cannot be obtainedfrom the study of seismic lines. Finally, we stress that studying field analogues represents a major tool to betterunderstand the mechanisms of extreme crustal thinning associated with mantle exhumation and their structuralinheritance during tectonic inversion.
Geophysical Research Abstracts
Vienne, Austria

insu-01510103
https://hal-insu.archives-ouvertes.fr/insu-01510103

Résumé : En raison de la nature symbiotique des micro-organismes endophytes, cette étude visait à étudier l'activité antibactérienne, antifongique et cytotoxique chez les métabolites secondaires des extraits endophytes foliaires de plantes de l'Amazonie brésilienne et du Cerrado. Dans ce travail de thèse 147 micro-organismes cultivables ont été isolés (130 champignons, 3 bactéries e 14 champignons non-identifiés ou inconnus) à partir de 28 plantes (4 espèces collectées au Brésil et 24 en Guyane Française). Tous les micro-organismes furent identifiés par analyse moléculaire des régions spécifiques de l'ADNr en utilisant des techniques de séquençage génomique. Des champignons endophytes de l’ordre des Xylariales furent ceux de plus importante fréquence d’isolation dans cette étude, représentés par 25 isolats. Des extraits bruts à l’AcOEt furent produits à partir de cultures de chaque micro-organisme isolé. Une proportion relative signifiante (23,1%) des extraits démontra une activité sur Candida albicans ATCC 10213, pendant que 4% furent actifs sur Staphylococcus aureus ATCC 29213. Le potentiel cytotoxique des extraits fut évalué pour des lignées cellulaires humaines KB (carcinome cervical utérin), MDA-MB-435 (mélanome), et MRC-5 (fibroblastes de poumon normal), résultant en proportion signifiante avec activité d’inhibition de la prolifération cellulaire (24,4%, 23,1% e 16,3%, respectivement).Dix-huit métabolites secondaires furent isolés et identifiés à partir du fractionnement des extraits bruts de huit endophytes. Dix-sept de ces substances furent déjà décrites précédemment dans la littérature: l’acide piliformique (24) et la griséofulvine (25) isolés à partir de Xylaria cubensis SNB-GCI02; La phomopirone (26), la pyrenocine (27), l’alterpérilenol (28) et la novae-zelandine (29), isolés de Lewia infectoria SNB-GTC2402; 5-métilmelleina (31) et la dihidrosporothrioride (32) isolées à partir de Xylaria sp. SNB-GTC2501; La mycoleptodiscine (34) et la mycoleptodiscine B (35) isolées à partir de Mycoleptodiscus sp. SNB-GTC2304; le mycoepoxidiène (36) et la altiloxina A (37) isolés à partir de Diaporthe pseudomangiferae SNB-GSS10; L’acremonisol (40), le semicochliodinol (41) et le cochliodinol (42) isolés à partir de Chaetomium globosum SNB-GTC2114; la colletofragarone A2 (43) isolée à partir de Colletotrichum sp. SNB-GTC0201; la flavoglaucine (44) isolée à partir de Eurotium rubrum BBS01. Parmi ces substances, la flavoglaucine (44) isolée à partir de E. rubrum BBS01 démontra une activité comparable au contrôle fluconazol en C. albicans (CIM de 4 µg.mL-1). La substance (44) présenta IC50 >10 µM sur cellules normales MRC-5, ce qui en fait un candidat pour des études ultérieures. Dans ce travail, fut identifié pour la première fois l’activité de la colletofragarone A2 (43) isolée à partir de Colletotrichum sp. SNB-GTC0201. La substance inédite nommée pyrrocidine C (30) fut isolée à partir de L. infectoria SNB-GTC2402 et identifiée par des analyses spectroscopiques (Casella et al., 2013). La pyrrocidine C (30) fut active en S. aureus ATCC 10213 (CIM de 2 µg.mL-1) et ne fut pas considérées cytotoxique pour les cellules normales MRC-5 (IC50 >10 µM), démontrant une sélectivité dans l’action antimicrobienne. Ces résultats démontrent la grande diversité des endophytes fongiques chez les plantes de l'Amazonie brésilienne et du Cerrado et la grande chimiodiversité associée aux métabolites secondaires de ces micro-organismes. Des champignons endophytes tropicaux, comme ceux présentés dans cette étude, peuvent apparaître comme une nouvelle source de substances antimicrobiennes et cytotoxiques.
Because of the symbiotic nature of endophytes, this survey aims to investigate the probality of discovering antibacterial, antifungal and cytotoxic activities in secondary metabolites of leaf endophytes isolated from plants of Amazon and Cerrado biomes. In this study, 147 cultivable microorganisms were isolated (130 fungi, 3 bacteria and 14 unidentified or unknown microbes) from 28 plant species (4 species collected in Brazil and 24 in French Guyana). All endophytes were identified by molecular analyses of specific rDNA regions, with genomic sequencing techniques. Fungal endophytes belonging to Xylariales order were the most frequently isolated in this study, represented by 25 isolates. Crude AcOEt extracts were produced from cultures of each isolated endophyte. A significant relative proportion (23,1%) of extracts showed activity in Candida albicans ATCC 10213, while 4% were active in Staphylococcus aureus ATCC 29213. The cytotoxic potencial of the extracts was evaluated for human cell lines KB (uterin cervical carcinome), MDA-MB-435 (melanoma) and MRC-5 (normal lung fibroblasts), and a significant proportion of them showed cellular proliferation inhibition (24,4%, 23,1% e 16,3%, respectively).Eighteen secondary metabolites were isolated by the fractionation of eight endophytic extracts. Seventeen of these substances had already been previously described in the literature: piliformic acid (24) and griseofulvin (25) isolated from Xylaria cubensis SNB-GCI02; phomopiron A (26), pyrenocin A (27), alterperilenol (28) and novae-zelandin A (29) isolated from Lewia infectoria SNB-GTC2402; 5-metilmellein (31) and dihidrosporothriorid (32) isolated from Xylaria sp. SNB-GTC2501; mycoleptodiscin A (34) and mycoleptodiscin B (35) isolated from Mycoleptodiscus sp. SNB-GTC2304; mycoepoxidien (36) and altiloxin A (37) isolated from Diaporthe pseudomangiferae SNB-GSS10; acremonisol A (40), semicochliodinol A (41) and cochliodinol (42) isolated from Chaetomium globosum SNB-GTC2114; colletofragaron A2 (43) isolated from Colletotrichum sp. SNB-GTC0201; flavoglaucin (44) isolated from Eurotium rubrum BBS01. Among these substances, flavoglaucin (44), isolated from E. rubrum BBS01, showed comparable antifungal activity with the positive control fluconazol in C. albicans (MIC of 4 µg.mL-1). Flavoglaucin (44) also showed IC50 >10 µM in normal MRC-5 cells, becoming a good candidate for further studies. In this work, the cytotoxic activity of colletofragaron A2 (43), isolated from Colletotrichum sp. SNB-GTC0201 was described for the first time. The unpublished substance named pyrrocidin C (30) isolated from L. infectoria SNB-GTC2402 was identified by spectroscopic analyses (Casella et al., 2013). The pyrrocidin C (30) was active in S. aureus ATCC 10213 (MIC of 2 µg.mL-1), and was not considered cytotoxic for normal MRC-5 cells (IC50 >10 µM), showing selectivity in antimicrobial activity. These results demonstrate the great endophytic fungal diversity in plants of Amazon and Cerrado biomes, along with the chemodiversity associated to the secondary metabolites of these endophytes. Tropical fungal endophytes, like those seen in this work, may emerge as a new source of antimicrobial and cytotoxic substances.
Devido à natureza simbiótica dos micro-organismos endofíticos, este estudo teve como objetivo investigar a atividade antibacteriana, antifúngica e citotóxica em metabólitos secundários de extratos de fungos endofíticos foliares de plantas do bioma Amazônia e Cerrado. Neste trabalho de tese foram isolados 147 micro-organismos cultiváveis (130 fungos, 3 bactérias e 14 fungos não-identificados ou desconhecidos) a partir de 28 plantas (4 espécies coletadas no Brasil e 24 na Guiana Francesa). Todos os micro-organismos foram identificados por análise molecular de regiões específicas de DNAr, com uso de técnicas de sequenciamento genômico. Fungos endofíticos da ordem Xylariales foram os de maior frequência de isolamento neste estudo, representados por 25 isolados. Extratos brutos em AcOEt foram produzidos a partir de culturas de cada micro-organismo isolado. Uma proporção relativa significante (23,1%) dos extratos demonstrou atividade em Candida albicans ATCC 10213, enquanto 4% foram ativos em Staphylococcus aureus ATCC 29213. O potencial citotóxico dos extratos foi avaliado para as linhagens celulares humanas KB (carcinoma cervical uterino), MDA-MB-435 (melanoma), e MRC-5 (fibroblastos de pulmão normal), resultando em proporção significante com atividade de inibição da proliferação celular (24,4%, 23,1% e 16,3%, respectivamente). Dezoito metabólitos secundários foram isolados a partir do fracionamento de oito extratos brutos endofíticos. Dezessete destas substâncias já tinham sido descritas anteriormente na literatura: ácido pilifórmico (24) e griseofulvina (25) isoladas de Xylaria cubensis SNB-GCI02; phomopirona A (26), pyrenocina A (27), alterperilenol (28) e novae-zelandina A (29) isoladas de Lewia infectoria SNB-GTC2402; 5-metilmelleina (31) e Dihidrosporothriolida (32) isoladas de Xylaria sp. SNB-GTC2501; mycoleptodiscina A (34) e mycoleptodiscina B (35) isoladas de Mycoleptodiscus sp. SNB-GTC2304; mycoepoxidieno (36) e altiloxina A (37) isoladas de Diaporthe pseudomangiferae SNB-GSS10; acremonisol A (40), semicochliodinol A (41) e cochliodinol (42) isoladas de Chaetomium globosum SNB-GTC2114; colletofragarona A2 (43) isolada de Colletotrichum sp. SNB-GTC0201; flavoglaucina (44) isolada de Eurotium rubrum BBS01. Dentre estas substâncias, a flavoglaucina (44) isolada de E. rubrum BBS01, demonstrou atividade comparável ao controle fluconazol em C. albicans (CIM de 4 µg.mL-1). Esta substância (44) apresentou IC50 >10 µM em células normais MRC-5, tornando-se candidata para estudos posteriores. Neste trabalho foi identificado pela primeira vez a atividade citotóxica da colletofragarona A2 (43), isolada de Colletotrichum sp. SNB-GTC0201. A substância inédita nomeada pyrrocidina C (30) foi isolada a partir de L. infectoria SNB-GTC2402 e identificada através de análises espectroscópicas (Casella et al., 2013). A pyrrocidina C (30) foi ativa em S. aureus ATCC 10213 (CIM de 2 µg.mL-1), e não foi considerada citotóxica para as células normais MRC-5 (IC50 >10 µM), demonstrando seletividade na ação antimicrobiana. Estes resultados demonstram a grande diversidade fúngica endofítica em plantas do bioma Amazônia e Cerrado, e a quimiodiversidade associada aos metabólitos secundários destes micro-organismos. Fungos endofíticos tropicais, como os vistos neste trabalho, podem emergir como uma nova fonte de substâncias antimicrobianas e citotóxicas.

http://www.theses.fr/2014AGUY0836/document

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
A new method to grow large single crystals with stoichiometry close to 1:1:2 of CuInSe2, an important member of the I-III-VI2 family of chalcopyrite semiconductors for optoelectronic device applications, is described. This is called the horizontal varying gradient zone freeze technique and consists of the selenization in the liquid phase of stoichiometric Cu and In and later solidification under programmed varying gradient in a fully automated multiple zone horizontal furnace. All ingots obtained with Se pressure between 15 and 1760 mm of Hg were single phase having chalcopyrite structure and p-type conductivity. X-ray, DTA, optical and electrical characterizations of the samples taken from different parts of the ingots were made. From energy dispersive spectroscopy it is found that the samples of the ingot obtained with Se pressure at 836 mm of Hg were much closer to the ideal stoichiometry 1:1:2.
ISSN: 0022-0248

hal-00808624
https://hal.univ-antilles.fr/hal-00808624
DOI : 10.1016/0022-0248(95)00346-0

Éditeur(s) : HAL CCSD Elsevier Masson
Résumé : International audience
Turbinaria turbinata brown seaweeds were tested as carbon electrode material in symmetric, electrochemical supercapacitors. The electrochemical properties of the carbon materials were characterised for their application as supercapacitors using cyclic voltammetry, galvanostatic charge/discharge method and electrochemical impedance spectroscopic analyses. Our initial results showed that the optimal behaviour was obtained for the sample prepared by pyrolysis at 800 degrees C. The average surface area of the carbon was 812 m(2)/g. Electrochemical tests with an organic electrolyte gave the following interesting results: a capacitance of 74.5 F/g, a specific series resistance of 0.5 Omega cm(2) and an ionic resistivity of 1.3 Omega cm(2). These results show the promising capacitive properties of carbon derived from seaweeds and their application in electrochemical supercapacitors. (C) 2013 Academie des sciences.
ISSN: 1631-0748

hal-00817880
http://hal.upmc.fr/hal-00817880
DOI : 10.1016/j.crci.2012.12.016

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The present work is concerned with the study of the tribological properties of various fluorinated carbon phases obtained at room temperature and then post-treated under fluorine atmosphere at different temperatures. The tribological tests evidence good intrinsic properties for all the compounds (friction coefficient in the range 0.07-0.09). Differences appear after few cycles. Friction measurements after 100 cycles and complementary Raman analyses of the tribofilm remaining in the wear scar point out that long term tribologic properties of the fluorinated compounds strongly depend on the evolution undergone by the materials under friction. The release of HF molecules, the loss of fluorine and partial rebuilding of graphitic phases are at the origin of the degradation of the friction properties. The good properties of the compounds post-treated at temperature in the range 150-300 °C are attributed to the chemical and structural stability of these compounds under friction.
ISSN: 0022-3697

hal-00756133
https://hal.archives-ouvertes.fr/hal-00756133
https://hal.archives-ouvertes.fr/hal-00756133/document
https://hal.archives-ouvertes.fr/hal-00756133/file/Delbe_6346.pdf
DOI : 10.1016/j.jpcs.2006.01.084