Éditeur(s) : Pergamon-elsevier Science Ltd
Résumé : We report the northernmost and deepest known occurrence of deep-water pycnodontine oysters based on two surveys along the French Atlantic continental margin to the La Chapelle continental slope (2006) and the Guilvinec Canyon (2008) The combined use of multibeam bathymetry seismic profiling CTD casts and a remotely operated vehicle (ROV) made it possible to describe the physical habitat and to assess the oceanographic control for the recently described species Neopycnodonte zibrowii These oysters have been observed in vivo in depths from 540 to 846 m colonizing overhanging banks or escarpments protruding from steep canyon flanks Especially in the Bay of Biscay such physical habitats may only be observed within canyons where they are created by both long-term turbiditic and contouritic processes Frequent observations of sand ripples on the seabed indicate the presence of a steady but enhanced bottom current of about 40 cm/s The occurrence of oysters also coincides with the Interface between the Eastern North Atlantic Water and the Mediterranean Outflow Water A combination of this water mass mixing internal tide generation and a strong primary surface productivity may generate an enhanced nutrient flux which is funnelled through the canyon When the ideal environmental conditions are met up to 100 individuals per m(2) may be observed These deep-water oysters require a vertical habitat which is often incompatible with the requirements of other sessile organisms and are only sparsely distributed along the continental margins The discovery of these giant oyster banks illustrates the rich biodiversity of deep-sea canyons and their underestimation as true ecosystem hotspots (C) 2010 Elsevier Ltd All rights reserved
Deep-sea Research Part I-oceanographic Research Papers (0967-0637) (Pergamon-elsevier Science Ltd), 2010-12 , Vol. 57 , N. 12 , P. 1561-1572

Droits : 2010 Elsevier Ltd All rights reserved.
http://archimer.ifremer.fr/doc/00023/13419/14034.pdf
DOI:10.1016/j.dsr.2010.09.002
http://archimer.ifremer.fr/doc/00023/13419/

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) : Université de la Méditerranée
Résumé : This study was supported by the Atlantic working site of the « Programme National d’Océanographie Côtière » (PNOC, PNEC since 1999). The objectives were (1) to check the existence and to understand the mechanisms of winter phytoplankton blooms in the bay of Biscay influenced by the Gironde waters (2) to determine the limiting nutrient of the primary production associated to these blooms and to follow the seasonal evolution of the limiting nutrient, (3) to understand the consequences of this early limitation on the structuration of algal populations in spring. Since phosphorus was supposed to be the major limiting nutrient of algal growth in the Gironde plume, the different forms of the phosphorus cycle as well as the bacterial compartment, central in this cycle, were also studied in term of stocks and fluxes. The sampling strategy consisted in three cruises in 1998, BIOMET 2 (January), BIOMET 3 (beginning of March), PEGASE (June) and six cruises in 1999, PLAGIA 1 to 6 (late February, late April, late May, late June, the middle of July and the beginning of October). Winter algal blooms, essentially diatoms, were actually observed both in the typical waters of the plume (S < 34.5) and at the limit of the plume and adjacent atlantic oceanic waters (S > 34.5) in the successives years 1998 and 1999. These blooms were initiated by the occurrence of short anticyclonic windows in winter, acting on physical processes which dominate the evolution and characteristics of the Gironde plume (runoff, wind direction and speed) and, ultimately, on the evolution of the depth of the mixed layer (haline stratification) and available light (decrease of turbidity). The algal growth was actually phosphorus limited in the typical waters of the plume at the end of the winter bloom, in spring and became nitrogen and phosphorus limited in summer until the first autumn gales restored the nutritive balance. More oceanic waters (S > 34.5) were probably N+P limited from the end of the winter-the beginning of spring to autumn. Phosphorus limitation of winter blooms, associated with girondine unbalanced nutritive supplies (high NO3/PO4 ratios) favoured the development of small cells at the beginning of spring and the later presence of spring blooms (June 1998, late May 1999) composed of pico and nanophytoplankton (nanoflagellates), instead of typical diatom spring blooms for temperate waters. This size reduction of algal communities is strongthened by the competition between phytoplankton and bacteria for the phosphate uptake, bacteria being more competitives at low concentrations and being phosphorus limited sometimes in spring. The decreasing size of algal cells probably acted on the structuration of the whole food web. The study of the different forms of phosphorus displayed the importance of the Dissolved Organic Phosphorus (DOP) pool. The potential biological lability and the capacity of algae and bacteria to use the DOP in spring when phosphate are undetectable was shown by the very high specific activities of alkaline phosphatases and the very rapid cycling of phosphate monoesters. According to the few estimations of actual phosphatasic activity and phosphate assimilation fluxes, the hydrolysis of DOP associated with the coupled assimilation of liberated phosphate would represent 91 to 99 % of the phosphorus fluxes into algal and bacterial cells when phosphate were exhausted. In such conditions DOP could satisfy most of microorganisms phosphorus needs.
Cette thèse s’inscrit dans le cadre du Chantier Atlantique du Programme National d’Océanographie Côtière (PNOC, PNEC depuis 1999). Les objectifs de ce travail étaient (1) de vérifier l’existence et comprendre le déterminisme de blooms phytoplanctoniques hivernaux dans les eaux du Golfe de Gascogne influencées par la Gironde, (2) de préciser le facteur limitant de la production primaire associée à ces blooms et de suivre l’évolution saisonnière de ce facteur et (3) de comprendre les conséquences de cette limitation précoce sur la structuration des populations algales au printemps. Le phosphore étant supposé être le principal élément limitant de la croissance algale dans le panache de la Gironde, les différentes composantes du cycle du phosphore ainsi que le compartiment bactérien, central dans ce cycle, ont été étudiés en terme de stock et de flux. La stratégie d’échantillonnage a consisté en trois campagnes en 1998, BIOMET 2 (janvier), BIOMET 3 (début mars), PEGASE (juin) et six campagnes en 1999, PLAGIA 1 à 6 (fin février, fin avril, fin mai, fin juin, mi-juillet et début octobre). Des efflorescences algales hivernales, constituées essentiellement de diatomées, ont effectivement été observées de façon récurrente dans les eaux typiques du panache (S < 34,5) et à la limite du panache et des eaux océaniques atlantiques adjacentes (S > 34,5) au cours des deux années successives 1998 et 1999. Ces blooms ont été engendrés par l’apparition de courtes fenêtres anticycloniques en période hivernale, ces fenêtres interférant sur les processus physiques qui prévalent sur l’évolution et les caractéristiques du panache de la Gironde (régime des débits, orientation et force du vent) et, de façon ultime, sur l’évolution de la profondeur de la couche de mélange (halostratification) et la disponibilité en lumière (diminution de la turbidité). La croissance algale était limitée par le phosphore dans les eaux typiques du panache à la fin du bloom hivernal, au printemps et devint limitée en azote et en phosphore en période estivale et ceci jusqu’à ce que les premières tempêtes automnales rétablissent l’équilibre nutritif des eaux. Les eaux à caractère plus océanique (S > 34,5) étaient plus probablement limitées par N+P dès la fin de l’hiverdébut du printemps et ce jusqu’à l’automne. La limitation des blooms hivernaux par le phosphore, associée à des apports nutritifs girondins déséquilibrés en phosphate (rapports NO3/PO4 élevés) a favorisé le développement de cellules de petite taille au début du printemps et la présence ultérieure de blooms printaniers (juin 1998, fin mai 1999) composés de pico- et de nanophytoplancton (nanoflagellés), blooms « atypiques » pour des eaux tempérées à cette saison. Cette structuration des communautés algales est renforcée par la compétition entre le phytoplancton et les bactéries pour l’acquisition du phosphate, les bactéries étant plus compétitives aux faibles teneurs en phosphate et pouvant être elles-mêmes limitées par le phosphore à certains moments du printemps. La diminution de taille des cellules algales a probablement une incidence sur la structure de taille de l’ensemble du réseau trophique. L’étude des différentes composantes du phosphore montre l’importance du pool de Phosphore Organique Dissous (POD), sa labilité biologique potentielle et la capacité des communautés algales et bactériennes à utiliser ce pool au printemps quand les phosphates sont indétectables (activités spécifiques des phosphatases alcalines très élevées, recyclage très rapide des monoesters de phosphate). Au vu des quelques estimations de l’activité phosphatasique réelle et des flux d’assimilation de phosphate, l’hydrolyse du POD associée à l’assimilation couplée du phosphate libéré représenterait 91 à 99 % des flux de phosphore vers les cellules algales et bactériennes, quand les phosphates du milieu sont déficients. Dans de telles conditions, le POD pourrait satisfaire l’essentiel des besoins des microorganismes en phosphore.

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/00013/12463/9298.pdf
http://archimer.ifremer.fr/doc/00013/12463/

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Mechanism and kinematics of the Late Mesozoic continental extension event of eastern Asia are still debated. In order to better constrain its evolution, two granodioritic plutons of the Jiaodong Peninsula have been chosen as targets for a time-constrained palaeomagnetic study. Indeed, plutons are devoid of visible deformation, did not experience rotation along horizontal axis and are precisely dated by U/Pb and 40Ar/39Ar methods. Multidomain (MD) magnetite has been identified as the principal magnetic remanent carrier. The interpolation of existing and new U/Pb and 40Ar/39Ar ages revealed that characteristic remanent magnetisation was acquired in a narrow range of 116 ± 2 Ma. Twenty out of 27 sites present stable magnetic directions calculated from high-temperature or high-coercive components. The observations of the solo normal magnetic polarity for this palaeomagnetic collection and of the magnetic remanent age consistent with the Cretaceous Normal Superchron (CNS) argue that the characteristic magnetic remanence may be considered as primary. Detailed field observations of the intrusive relationship between the plutons and country rocks and Anisotropy of Magnetic Susceptibility (AMS) study reveal the absence of the subsequent deformation of plutons, or rigid rotation of plutons along a horizontal axis. Two palaeomagnetic poles have been therefore calculated from these plutons. Among 12 out 15 Cretaceous palaeomagnetic poles, including the two new poles provided by this study, from the Jiaodong Peninsula and on both sides of Tan-Lu and Muping-Jimo faults are statistically consistent. As a result, the Jiaodong Peninsula behaved as a rigid block as internal deformation appears negligible. The remaining three derived poles are probably due to the secular variation or/and the vicinity of fault zones near of the palaeomagnetic sampling site. Thus, they can not be applied to the peninsula-scaled tectonics. Comparison of these time52 constrained Cretaceous palaeomagnetic results of the Jiaodong Peninsula with those of North China Block (NCB) indicate that the Jiaodong Peninsula was rigidly attached to NCB since, 3 at least, the Cretaceous as residual difference is clearly insignificant with respect to the error brackets. These new palaeomagnetic results confirm that the relative clockwise (CW) rotation of Eastern Liaoning-Korea Block (ELKB) with respect to NCB does not affect the Jiaodong Peninsula as a rigid block, nevertheless, some tectonic structures have been reactivated since Cenozoic and local rotations could be produced. This palaeomagnetic study reveals that the Late Mesozoic extension in Eastern Asia is heterogeneously expressed in time and space. The complete understanding of the mechanism(s) of this extensional event needs further multidisciplinary investigations.
ISSN: 0031-9201

insu-00599546
https://hal-insu.archives-ouvertes.fr/insu-00599546
https://hal-insu.archives-ouvertes.fr/insu-00599546/document
https://hal-insu.archives-ouvertes.fr/insu-00599546/file/Charles_et_al_PEPI2011.pdf
DOI : 10.1016/j.pepi.2011.05.006

Résumé : Les deux principaux objectifs de ce travail sont de proposer des outils pour la selection d'animaux résistants aux strongles gastro-intestinaux, parasites du tube digestif, et de faire progresser la compréhension des mécanismes de résistance chez la chèvre créole. La variabilité génétique du caractère de résistance au parasitisme digestif a été étudiée afin de vérifier quels critères décrivant le mieux la résistance, peuvent être utilisés pour la sélection. L'ensemble des résultats obtenus suggèrent que le critère d'excrétion d'oeufs et le critère d'éosinophilie sont les plus adaptés pour un schéma de sélection puisqu'ils possèdent une héritabillté moyenne et représentent le mieux la résistance. De plus, ils ne semblent pas en opposition avec le poids, principal critère de production. Le déterminisme génétique de la résistance aux strongles gastro-intestinaux a été étudié et a permis de mettre en évidence l'existence d'un gène majeur pour la résistance chez la population de chèvre créole. De plus, la primo-détection de qtl a permis d'identifier 13 régions du génome ayant un effet sur les critères de résistance. Les mécanismes responsables de la résistance aux strongles gastro-intestinaux ont également été à l'étude. L'ensemble des résultats met en évidence le rôle des éosinophiles dans la mise en place de la résistance aux strongles gastro-intestinaux. L'activité des immunogobulines e semblent dirigés vers les larves l3 d'haemonchus contortus et suggère la mise en place d'une réaction protectrice. Chez la chèvre créole. Ces deux mécanismes semblent donc jouer un rôle important dans la mise en place de la résistance aux strongles gastro-intestinaux
The two main objectives of this work are to propose tools for the selection of resistant animals to gastrointestinal nematodes and advance knowledge on mechanisms of resistance of creole goats. this work has analysed the genetic variability of resistance to digestive parasitism in order to determine which criteria best describes the resistance and can be use for selection. the overall results suggest that the egg excretion and the eosinophilia are the criteria most suitable for a breeding scheme because they have moderate heritability estimates and best represent the resistance. moreover, they do not seem in conflict with the weight, the main criterion of production. the genetic determinism of resistance to gastrointestinal parasites has been studied and has highlighted the existence of a major gene for resistance in creole goats. in addition, the primodetection of qtl identified 13 genomic regions that affect the resistance. the mechanisms behind the resistance to gastrointestinal parasites were also studied and first hypothesis regarding the involvment of the immune response in resistance have been made in goats. the overall results highlighted the role of eosinophils in the development of resistance to gastrointestinal nematodes. the activity of immunoglobulin e seems directed toward l3 larvae of haemonchus contortus and may be imply in the establishment of a protective response agasint nematode parasites. in creole goats, these two mechanisms seem to play an important role in the development of resistance to gastrointestinal nematode infections

http://www.theses.fr/2011AGUY0407/document

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
To constrain the relations between deformation and metasomatism in the subcratonic lithospheric mantle, we have analyzed the microstructures and crystal preferred orientations in 50 mantle xenoliths from the Kaapvaal craton. Water contents in olivine and pyroxenes were measured in 14 samples equilibrated at different depths. Coarse-granular microstructures recording deformation by dislocation creep followed by annealing predominate. Mylonitic (sheared) peridotites with partially or totally recrystallized microstructures are however common below 140 km. Refractory compositions predominate, but multiple metasomatic events resulted in orthopyroxene enrichment or secondary crystallization of clinopyroxene and phlogopite. Coherent orthopyroxene and olivine CPO in most coarse-grained peridotites implies in pre- to syn-kinematic orthopyroxene enrichment or epitaxial growth on primary orthopyroxene. Undeformed, interstitial orthopyroxene, clinopyroxene, and phlogopite with random orientations in coarse-grained peridotites record post-kinematic modal metasomatic events. Deformation of these phases in the sheared peridotites implies that mylonitization results from a later event, which affected locally the deep cratonic lithosphere. Olivine CPO recording dominant [100] glide predominate at all depths. Only two samples, equilibrated at ~ 3.3 GPa show olivine [001] and orthopyroxene [001] axes subparallel, suggesting dominant [001] glide. Water contents in olivine are maximum (150 wt. ppm H2O) in peridotites equilibrated at ~ 160 km depth. Peridotites equilibrated below 180 km depth are, in contrast, almost dry. Lack of correlation between olivine mg# and water content indicates that the high water contents in olivine record re-hydration after the extensive partial melting, which produced the cratonic root. The vertical variation in water contents in olivine observed in the Kaapvaal peridotites may result from hydrogen addition or loss during extraction by the kimberlites. Comparison with magnetotelluric electrical conductivity data suggests, however, that the observed vertical variation of water contents in olivine may be representative of the present-day state of the Kaapvaal mantle, implying that extensive metasomatism resulted in hydration of the cratonic mantle at intermediate depths. The annealed microstructures of Kaapvaal peridotites indicate however that this metasomatism was not followed by remobilization of the cratonic root.
ISSN: 0024-4937

hal-00750328
https://hal.archives-ouvertes.fr/hal-00750328
DOI : 10.1016/j.lithos.2012.05.001

Éditeur(s) : Gauthier-Villars
Résumé : Fish communities from two lagoon ecosystems, Ria Formosa (Portugal) and Grand Cul-de-Sac Marin (Guadeloupe), show interesting similarities of spatial and temporal organization. On the temporal scale, three community changes are observed in both systems, corresponding to massive arrivals and/or departures of migratory species. However, these migrations are more conspicuous in the Ria Formosa than in the Grand Cul-de-Sac Marin. On a spatial scale, the community structure is also largely determined by migratory species, whose abundance is a factor of homogenization. This is clearly observed in Ria Formosa, where the lagoon selection applies on a regional scale. Conversely, the community of sedentary fish identifies remarkable stations affected by chronic aggressions such as tourism or pollution. An explicative analysis, comprising a discriminant analysis and multiple regressions was realized on the data collected in the Grand Cul-de-Sac Marin. This analysis made it possible to determine the important environmental descriptors in the two complementary processes involved in recruitment: migrant availability, which determines the temporal organization of the fish assemblage. These migrations are explained by water temperature and salinity, two descriptors controlled by climatic conditions; the settlement process, which determines the spatial organization of the fish assemblage. This is explained by habitat descriptors such as visibility and turtlegrass blade length, or trophic descriptors, such as primary production, zooplankton density or nitrate concentration.
Oceanologica Acta (0399-1784) (Gauthier-Villars), 1993 , Vol. 16 , N. 3 , P. 291-301

Droits : info:eu-repo/semantics/openAccess
http://archimer.ifremer.fr/doc/00099/21056/18682.pdf
http://archimer.ifremer.fr/doc/00099/21056/

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The mycotoxin enniatin B (EnnB) is predominantly produced by species of the Fusarium genera, and often found in grain. The cytotoxic effect of EnnB has been suggested to be related to its ability to form ionophores in cell membranes. The present study examines the effects of EnnB on cell death, differentiation, proliferation and pro-inflammatory responses in the murine monocyte-macrophage cell line RAW 264.7. Exposure to EnnB for 24 h caused an accumulation of cells in the G0/G1-phase with a corresponding decrease in cyclin D1. This cell cycle-arrest was possibly also linked to the reduced cellular ability to capture and internalize receptors as illustrated by the lipid marker ganglioside GM1. EnnB also increased the number of apoptotic, early apoptotic and necrotic cells, as well as cells with elongated spindle-like morphology. The Neutral Red assay indicated that EnnB induced lysosomal damage; supported by transmission electron microscopy (TEM) showing accumulation of lipids inside the lysosomes forming lamellar structures/myelin bodies. Enhanced levels of activated caspase-1 were observed after EnnB exposure and the caspase-1 specific inhibitor ZYVAD-FMK reduced EnnB-induced apoptosis. Moreover, EnnB increased the release of interleukin-1 beta (IL-1β) in cells primed with lipopolysaccharide (LPS), and this response was reduced by both ZYVAD-FMK and the cathepsin B inhibitor CA-074Me. In conclusion, EnnB was found to induce cell cycle arrest, cell death and inflammation. Caspase-1 appeared to be involved in the apoptosis and release of IL-1β and possibly activation of the inflammasome through lysosomal damage and leakage of cathepsin B.
ISSN: 0041-008X

inserm-00871698
http://www.hal.inserm.fr/inserm-00871698
DOI : 10.1016/j.taap.2012.03.014
PUBMED : 22483798

Éditeur(s) : HAL CCSD American Society for Investigative Pathology (ASIP)
Résumé : International audience
Semen represents the main vector of HIV dissemination worldwide, yet the origin of HIV in semen remains unclear. Viral populations distinct from those found in blood have been observed in semen, indicating local viral replication within the male genital tract. The seminal vesicles, the secretions of which constitute more than 60% of the seminal fluid, could represent a major source of virus in semen. This study is the first to investigate the susceptibility of human seminal vesicles to HIV infection both in vitro and in vivo. We developed and characterized an organotypic culture of human seminal vesicles to test for target cells and HIV infection, and, in parallel, analyzed the seminal vesicle tissues from HIV-infected donors. In vitro, in contrast to HIV-1 X4, HIV-1 R5 exposure induced productive infection. Infected cells consisted primarily of resident CD163(+) macrophages, often located close to the lumen. In vivo, HIV protein and RNA were also detected primarily in seminal vesicle macrophages in seven of nine HIV-infected donors, some of whom were receiving prolonged suppressive highly active antiretroviral therapy. These results demonstrate that human seminal vesicles support HIV infection in vitro and in vivo and, therefore, have the potential to contribute virus to semen. The presence of infected cells in the seminal vesicles of treated men with undetectable viremia suggests that this organ could constitute a reservoir for HIV.
American Journal of Pathology

inserm-00626549
http://www.hal.inserm.fr/inserm-00626549
DOI : 10.1016/j.ajpath.2011.08.005
PUBMED : 21925468

Éditeur(s) : HAL CCSD Elsevier Masson
Résumé : International audience
Mussels of the subfamily Bathymodiolinae thrive around chimneys emitting hot fluids at deep sea hydrothermal vents, as well as at cold seeps and on sunken organic debris (sunken wood, whale falls). Despite the absence of light-driven primary production in these deep-sea ecosystems, mussels succeed reaching high biomasses in these harsh conditions thanks to chemosynthetic, carbon-fixing bacterial symbionts located in their gill tissue. Since the discovery of mussel symbioses about three decades ago our knowledge has increased, yet new findings are published regularly regarding their diversity, role and evolution. This article attempts to summarize current knowledge about symbiosis in Bathymodiolinae, focusing on mussel species for which information is available regarding both hosts and symbionts. Moreover, new data obtained from small mussels inhabiting sunken woods around the Philippines are provided. Indeed, mussel species from organic falls remain poorly studied compared to their vent and seep relatives despite their importance for the understanding of the evolution of symbiosis in the subfamily Bathymodiolinae.
ISSN: 1631-0691

hal-00750422
https://hal.univ-antilles.fr/hal-00750422

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Saline aquifers in deep sedimentary formations are considered the primary candidates for geological storage of CO2, due to their large volumetric capacity that would be sufficient to meet the needs for CCS storage space in a global scale. In comparison to depleted oil and gas reservoirs the deep saline aquifers are, however, less investigated as there has previously been little economic interest in them. Effective methods for characterizing the storage aquifers are crucial for a successful implementation of any CCS project and therefore being developed and transferred from other applications in a various CCS projects.The objective of EU FP7 funded project MUSTANG project (A multiple space and time scale approach for the quantification of deep saline formations for CO2 storage, www.co2mustang.eu) has been to develop methods for characterizing saline aquifers and for understanding their properties. An essential part of this was establishment of a CO2 injection site at Heletz, Israel, where small-scale scientifically motivated injection experiments are planned to be carried out in presently ongoing continuation projects TRUST (http://trust-co2.org/) and CO2QUEST (www.co2quest.eu).While a large number of publications has been already produced based on the work in the MUSTANG project and its successors, and published in different journals, including this one, the objective of this Special Edition has been to gather some of the concluding work in the same journal issue. The focus has in particular been in summarizing the site characterization work carried out at the Heletz site, thereby providing readers an easy overview of the findings and characteristics of the site. In addition, some related work from some of the other sites investigated in MUSTANG project is also included, namely work from the sites Hontomin, Maguelone and a natural analog site in the North Sea. The results are intended to add to our understanding on relevant properties of geological formations as candidates for CO2 geological storage.
ISSN: 1750-5836

hal-01356326
https://hal.archives-ouvertes.fr/hal-01356326
DOI : 10.1016/j.ijggc.2016.02.007

Éditeur(s) : HAL CCSD American Geophysical Union
Résumé : International audience
The Yakutat-St. Elias collision in SE Alaska and adjacent Canada represents a prime example of present-day tectonics associated with an indentor corner. Its eastern syntaxis is marked by high exhumation, a sharp structural bend, and strain concentration at the transition from shortening to oblique transpression. Here we present GPS velocity and strain rate fields that cover the syntaxis, including 11 new stations in the core of the St. Elias Mountains. These data are corrected for transient deformation (glacial isostatic adjustment and postseismic and interseismic loading) to produce residual velocities and strain rates representative of long-term tectonics. The main features of these velocity and strain rate fields are a peak in strain rates (strain knot) in the syntaxis at the junction between the main fault systems and a rapid rotation from convergence-parallel to convergence-normal orientations of the velocities and shortening axes around the syntaxis, leading to shortening across the southern Denali Fault. These features are consistent with the strain and tectonic patterns expected near an indentor corner at the transition from shortening to transpression, with a combination of diffuse and localized deformation. The GPS velocities and strain rates show diffuse deformation around the syntaxis, from pure convergence-parallel shortening in the orogenic wedge to oblique extension that accommodates the strain rotation at the front of the syntaxis. This indentor-corner model also results in a near-zero strike-slip rate on the southern Denali Fault and shows no clear evidence for a throughgoing fault hypothesized to link the Fairweather and Totschunda Faults.
ISSN: 0148-0227

hal-01243510
https://hal.archives-ouvertes.fr/hal-01243510
DOI : 10.1002/2014JB011842

Éditeur(s) : HAL CCSD Public Library of Science
Résumé : International audience
In 2008 a fatal case of primary amoebic meningoencephalitis, due to the amoeboflagellate Naegleria fowleri, occurred in Guadeloupe, French West Indies, after a child swam in a bath fed with geothermal water. In order to improve the knowledge on free-living amoebae in this tropical part of France, we investigated on a monthly basis, the presence of Naegleria spp. in the recreational baths, and stream waters which feed them. A total of 73 water samples, 48 sediments and 54 swabs samples were collected from 6 sampling points between June 2011 and July 2012. The water samples were filtered and the filters transferred to non-nutrient agar plates seeded with a heat-killed suspension of Escherichia coli while sediment and swab samples were placed directly on these plates. The plates were incubated at 44°C for the selective isolation of thermophilic Naegleria. To identify the Naegleria isolates the internal transcribed spacers, including the 5.8S rDNA, were amplified by polymerase chain reaction and the sequence of the PCR products was determined. Thermophilic amoebae were present at nearly all collection sites. The pathogenic N. fowleri was the most frequently encountered thermophilic species followed by N. lovaniensis. The concentration of N. fowleri was rather low in most water samples, ranging from 0 to 22 per liter. Sequencing revealed that all N. fowleri isolates belonged to a common Euro-American genotype, the same as detected in the human case in Guadeloupe. These investigations need to be continued in order to counsel the health authorities about prevention measures, because these recreational thermal baths are used daily by local people and tourists.
ISSN: 1932-6203

pasteur-00782031
https://hal-riip.archives-ouvertes.fr/pasteur-00782031
https://hal-riip.archives-ouvertes.fr/pasteur-00782031/document
https://hal-riip.archives-ouvertes.fr/pasteur-00782031/file/article_naegleria_plos_one.pdf
DOI : 10.1371/journal.pone.0054414

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Carbonation of peridotite is a widespread process in nature, with emerging societal and environmental implications through geological storage of CO2. We studied the micro- and nano-scale structures associated with the carbonation of peridotite pervaded by a CO2-rich water and the induced changes of its hydrodynamic properties. Focused ion beam (FIB) nanotomography was coupled with scanning electron microscopy (SEM) and transmission electron microscopy (TEM) observations. An experimental sample of dunite core percolated by a CO2-rich fluid (pCO2 = 11 MPa) at 160 °C was compared with a naturally carbonated sample from the Atlantic Ridge (Exp. IODP 304). Results of the 8-days percolation experiment show continuous alteration of olivine into magnesite locally associated with a poorly crystalline serpentine-type mineral referred to as proto-serpentine. The experiment is also characterized by an overall decrease in rock porosity (from 7.7 to 6.4%) and permeability (from 8.5 × 10− 16 to 1.7 × 10− 16 m2). The primary inter-granular porosity (1 to 10 μm) is progressively filled with magnesite, leading to the overall decrease of permeability. At the same time, a secondary small-scale porosity (10 nm to 1 μm) is created at the tip of the dissolution features along the (010) cleavage planes of olivine grains. Carbonate crystals grow within these etch-pit structures behind the dissolution front. Dissolution and precipitation occur at a relative rate that maintains the secondary porosity over the timescale of the experiment (i.e. carbonate growth has to be the slowest one). This process is interpreted as an interface coupled dissolution-precipitation mechanism of olivine carbonation. Proto-serpentine is only formed in highly reduced flow areas, such as small olivine etch-pits (10 to 500 nm wide), which are more isolated from CO2 input. SEM-FIB analyses show the 3D preferential orientation of the dissolution-precipitation planes within a given olivine grain. It suggests the formation of lateral connections between the etch-pits (infra-micrometric “channels”) providing access to reactants and removing reaction products at the reaction sites. The experimental results show that olivine dissolution and magnesite precipitation converge to a quasi-steady state resulting in a constant carbonation rate controlled by reaction kinetics and not by mass transfer for this flow regime. The system self-regulates, independently of the porosity change at least during this incipient stage of olivine carbonation. Similar textures are observed in natural samples collected at 170 m-depth in the vicinity of veinlets driving late fluids down into the cooling oceanic lithosphere. This suggests that similar mechanisms are active in nature and can play an important role in the late, low temperature alteration stages of fractured peridotite. These results also highlight the critical role of nm-scale spatial arrangement of dissolution and precipitation features on mass transfers and on the sustainability of olivine carbonation through coupled dissolution-precipitation processes.
ISSN: 0009-2541

hal-01684733
https://hal.archives-ouvertes.fr/hal-01684733
DOI : 10.1016/j.chemgeo.2017.11.013