Éditeur(s) : HAL CCSD
Résumé : International audience
Up-to-date estimates of the health outcomes of preterm children are needed for assessing perinatal care, informing parents, making decisions about care, and providing evidence for clinical guidelines. To determine survival and neonatal morbidity of infants born from 22 through 34 completed weeks' gestation in France in 2011 and compare these outcomes with a comparable cohort in 1997. The EPIPAGE-2 study is a national, prospective, population-based cohort study conducted in all maternity and neonatal units in France in 2011. A total of 2205 births (stillbirths and live births) and terminations of pregnancy at 22 through 26 weeks' gestation, 3257 at 27 through 31 weeks, and 1234 at 32 through 34 weeks were studied. Cohort data were collected from January 1 through December 31, 1997, and from March 28 through December 31, 2011. Analyses for 1997 were run for the entire year and then separately for April to December; the rates for survival and morbidities did not differ. Data are therefore presented for the whole year in 1997 and the 8-month and 6-month periods in 2011. Survival to discharge and survival without any of the following adverse outcomes: grade III or IV intraventricular hemorrhage, cystic periventricular leukomalacia, severe bronchopulmonary dysplasia, retinopathy of prematurity (stage 3 or higher), or necrotizing enterocolitis (stages 2-3). A total of 0.7% of infants born before 24 weeks' gestation survived to discharge: 31.2% of those born at 24 weeks, 59.1% at 25 weeks, and 75.3% at 26 weeks. Survival rates were 93.6% at 27 through 31 weeks and 98.9% at 32 through 34 weeks. Infants discharged home without severe neonatal morbidity represented 0% at 23 weeks, 11.6% at 24 weeks, 30.0% at 25 weeks, 47.5% at 26 weeks, 81.3% at 27 through 31 weeks, and 96.8% at 32 through 34 weeks. Compared with 1997, the proportion of infants surviving without severe morbidity in 2011 increased by 14.4% (P < .001) at 25 through 29 weeks and 6% (P < .001) at 30 through 31 weeks but did not change appreciably for those born at less than 25 weeks. The rates of antenatal corticosteroid use, induced preterm deliveries, cesarean deliveries, and surfactant use increased significantly in all gestational-age groups, except at 22 through 23 weeks. The substantial improvement in survival in France for newborns born at 25 through 31 weeks' gestation was accompanied by an important reduction in severe morbidity, but survival remained rare before 25 weeks. Although improvement in survival at extremely low gestational age may be possible, its effect on long-term outcomes requires further studies. The long-term results of the EPIPAGE-2 study will be informative in this regard.
ISSN: 2168-6211

hal-01258705
http://hal.univ-brest.fr/hal-01258705
PUBMED : 25621457
DOI : 10.1001/jamapediatrics.2014.3351

Éditeur(s) : HAL CCSD American Geophysical Union
Résumé : International audience
We recover the Holocene earthquake history of seven seismogenic normal faults in the Fucino system, central Italy. We collected 800 samples from the well-preserved limestone scarps of the faults and modeled their 36Cl concentrations to derive their seismic exhumation history. We found that > 30 large earthquakes broke the faults in synchrony over the last 12 ka. The seven faults released strain at the same periods of time, 12-9 ka, 5-3 ka, and 1.5-1 ka. On all faults, the strain accumulation and release occurred in 3-6 ka supercycles, each included a 3-5 ka phase of slow (≤ 0.5-2 mm/yr) strain accumulation in relative quiescence, followed by a cluster of three to four large earthquakes or earthquake sequences that released most of the strain in < 1-2 ka. The large earthquakes repeated every 0.5 ± 0.3 ka during the paroxysmal phases and every 4.3 ± 0.9 ka between those phases. Earthquakes on the northern faults produced twice larger surface slips (~ 2 m) and had larger magnitudes (Mw 6.2-6.7) than those on the southern faults. On most faults, the relative strain level was found to control the amount of slip and the time of occurrence of the next large earthquake. Faults entered a phase of clustered activity once they had reached a specific relative strain threshold. The Tre Monti fault is identified as the most prone to break over the next century. Our data document earthquake synchrony and clustering at a broader space and time scale than has been reported to date.
ISSN: 0148-0227

hal-00903460
https://hal.archives-ouvertes.fr/hal-00903460
DOI : 10.1002/jgrb.50299

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The ultramafic rocks of the Collo region in northeastern Algeria crop out as “stratified” masses that cut across older metamorphic formations of the Petite Kabylie basement. Based on petrological compositions and mineralogical observations, these rocks are mainly peridotites and serpentinites. The peridotites are identified as lherzolites, but dunites may occur rarely. The lherzolites are composed of olivine, orthopyroxene, clinopyroxene and chromian spinel. Their chemical composition shows high MgO (34.4–37.5 wt%), Cr (0.14–0.27 wt%), Ni (0.14–0.26 wt%) and Co (34–133 ppm) contents and low CaO and Al2O3 concentrations (0.02–2.2 wt% and 0.5 to 2.8 wt%, respectively). The chromite, which represents approximately 1–3% of the rock, is ubiquitous and shows two different generations: primary millimetric euhedral crystals and secondary fine xenomorphic grains and interstitial aggregates. The primary chromites are alumino-ferro-magnesian crystals that show high Al2O3 (25.77%–27.36%) and MgO (10.70%–13.36%). Cr# (100 × Cr/(Al + Cr)) ranges from 45 to 48, and Mg# (100 × Mg/(Mg + Fe2+)) from 49 to 59. The secondary interstitial grains are iron-rich chromites. They show low Al2O3 (4.67%–9.54%) and MgO (4.60%–4.65%). Cr# is relatively high (77–88), whereas Mg# shows relatively low values, ranging from 22 to 25. Primary chromite and whole-rock chemistry show that the Collo ultramafic rocks belong to Alpine-type peridotites that were emplaced within an orogenic setting. The oxygen isotopic composition of both peridotites and chromites is consistent with their derivation from a mantle source (δ18O ranges from +3.0 to +5.9‰). Low δ18O values (<+4.4‰) are recorded in serpentinites and are attributed to the effect of serpentinization processes through high-temperature metasomatic fluids. Magnesite-bearing serpentinites show the lowest δ18O values. These are interpreted as the result of surface water input.
ISSN: 0899-5362

hal-01468003
https://hal.archives-ouvertes.fr/hal-01468003
DOI : 10.1016/j.jafrearsci.2016.10.012

Éditeur(s) : HAL CCSD Springer-Verlag
Résumé : The Chile-Argentina Patagonian Cordillera is a natural laboratory to study the interactions between oceanic and continental lithosphere during the subduction of an active spreading ridge beneath a continent. Subduction of the South Chile spreading ridge, which separates the Nazca plate from the Antarctic plate, started around 15–14 Ma at the southern tip of Patagonia. Presently, the southernmost segment of the Chile Ridge enters the Peru-Chile trench at 46°S, at the site of the Chile Triple Junction (CTJ). We review the main events which occurred on land in the CTJ region (46–47°S), related with processes of ridge subduction. We summarize tectonic, sedimentary, and magmatic features in a 30 Ma-to Present chronological table. A preridge subduction stage, from 30 to 15 Ma, is characterized by the onset and growth of Patagonian relief and by a shift from marine to continental detrital sedimentation in the foreland at 20–22 Ma. The change from pre-ridge subduction to ridge subduction is marked on land by a transition from calc-alkaline to alkaline volcanism, at 14–12 Ma, and by the onset of eruption of very large fl ood basalt provinces (future volcanic plateaus) following rapid erosion of the eastern foreland belt. Post-plateau basaltic volcanism (<4 Ma) is coeval with a period of tectonic and morphological rejuvenation during which the eastern foreland of the Cordillera has been affected by extensional/transtensional tectonics. We place these events in the framework of a tectonomagmatic model involving the opening of slab windows due to both slab tear and ridge axis subduction.
Subduction Zone Geodynamics

hal-00421053
https://hal.archives-ouvertes.fr/hal-00421053
DOI : 10.1007/978-3-540-87974-9_12

Éditeur(s) : HAL CCSD Lippincott, Williams & Wilkins
Résumé : International audience
BACKGROUND:Fever in infants younger than 3 months is generally a cause for concern because of the risk for a serious bacterial infection. The aim of this study was to describe clinical and biological features of Chikungunya infection in infants < 3 months of age hospitalized in Cayenne Hospital during the 2014-2015 outbreak.METHODS:We performed a preliminary retrospective study followed by a prospective study from March 2014 to February 2015. All infants younger than 3 months presenting with fever and hospitalized in Cayenne Hospital were included. The main diagnostic criteria were fever and positive Chikungunya PCR.RESULTS:One hundred and twenty infants were hospitalized with fever. The mean age was 46 days (SD± 22 days). The mean hospitalization duration was 7.4 days (SD± 6.1 days). Chikungunya infection was diagnosed in 26 children. The most important clinical findings were high (80.8% [77.5-84]) and prolonged fever (76.9%, [73.4-80.4]), irritability (96.2% [94.5-97.7]) and skin rash. (69.2%, [65.4-73]). Half of the infants presented edema of the extremities (hands and feet principally). However, in 15 %, Chikungunya infection was associated with a serious bacterial infection. Infants who presented with irritability, high fever and elevated PCT were at high risk for Chikungunya: OR 39, [9.2-243] (p < 0.001), with a specificity of 96.7 % and a negative predictive value of 89.4%. The area of the ROC curve was 0.96 CONCLUSIONS:: Our results confirm that Chikunguyna infection is a cause of high fever in infants younger than 3 months. Our data should be confirmed by larger studies.
ISSN: 0891-3668

inserm-01476019
http://www.hal.inserm.fr/inserm-01476019
http://www.hal.inserm.fr/inserm-01476019/document
http://www.hal.inserm.fr/inserm-01476019/file/2017%2C%20Elenga%20-%20Chikungunya%20Infection%20in%20hospitalized%20febrile%20infants.pdf
DOI : 10.1097/INF.0000000000001541

Résumé : Les 21 et 22 juin 2000, le Département des Ressources Aquacoles a consacré ses journées annuelles à une revue du thème "santé des cheptels" et du dispositif de recherche en pathologie sur les filières poissons, crustacés et mollusques, domaine très stratégique pour l'aquaculture marine française. Les objectifs des ces journées, rappelés par Yves Harache, Directeur du Département, étaient les suivante : • Dresser le bilan des actions de recherche menées par l'Ifremer en pathologie des espèces aquacoles, • Repréciser la stratégie (objectifs/moyens) du Département des Ressources Aquacoles sur le thème "santé des cheptels", • Programmer les actions de recherche à venir, • Stimuler les interactions entre groupes de recherche et laboratoires impliqués. Le présent rapport rend compte du contenu des débats de ces deux journées.

Droits : 2000 Ifremer
http://archimer.ifremer.fr/doc/00164/27547/25711.pdf
http://archimer.ifremer.fr/doc/00164/27547/

Éditeur(s) : HAL CCSD
Résumé : Mon document "Titres et travaux" contient 5 articles au format éditeur.
Mes premiers travaux de recherche, me permettant de soutenir une thèse de doctorat en décembre 1999, ont été effectués au sein du laboratoire du professeur Bernard GRANDCHAMP (unité 409 de l'INSERM) sous la direction du docteur Marie-Christine LECOMTE. Mon travail s'est intégré dans l'étude fonctionnelle et structurale de certains domaines des spectrines érythroïdes et non érythroïdes, principalement le site de tétramérisation et le domaine SH3. Concernant la tétramérisation de la spectrine érythroïde j'ai identifié les régions minimales nécessaires et suffisantes pour former le tétramère puis j'ai mis en évidence une relation entre certaines mutations de la spectrine associées à des anomalies membranaires du globule rouge et la sévérité du défaut de formation du tétramère. J'ai ensuite identifié plusieurs ligands du domaine SH3 de la spectrine non érythroïde. L'un d'entre eux m'a permis de définir une régulation de la protéolyse ciblée de cette spectrine faisant intervenir un mécanisme de phosphorylation/déphosphorylation. Ma formation initiale fut donc celle d'un biochimiste que j'ai étendue peu à peu vers la biologie moléculaire et la biologie cellulaire.
Puis, souhaitant acquérir les connaissances nécessaires au développement de modèles murins, j'ai décidé d'effectuer mon stage post-doctoral à l'Institut COCHIN (unité 567 de l'INSERM) dans une équipe co-dirigée par le docteur Sophie VAULONT et le professeur Axel KAHN. Je me suis ainsi familiarisé avec la souris comme « outil » de recherche (gestion d'un élevage, établissement de nouvelles lignées, génotypage, phénotypage). Je travaillais initialement sur le métabolisme du glucose mais j'ai complètement réorienté ma thématique de recherche au bout d'un an pour finalement identifier et caractériser une hormone, l'hepcidine, contrôlant l'homéostasie du fer.
J'ai été nommé chargé de recherche de grade 2 dans l'unité 409 de l'INSERM en octobre 2002 pour y développer une souche de souris exprimant une spectrine non érythroïde résistante à des mécanismes de protéolyse ciblée. Il s'agit donc toujours d'appréhender certaines fonctions des spectrines mais dans un contexte in vivo. En janvier 2005 j'ai intégré l'unité 665 de l'INSERM dirigée par Yves COLIN afin de poursuivre ce projet. Aujourd'hui, je suis chargé de recherche de grade 1.
Le chapitre scientifique de ce mémoire est divisé en deux parties distinctes : la première traite de mon travail sur la spectrine tandis que la seconde porte sur l'hepcidine. Chaque partie est composée d'une introduction au sujet suivie d'un résumé des travaux que j'ai effectués et/ou dirigés.
https://tel.archives-ouvertes.fr/tel-00285035

Droits : info:eu-repo/semantics/OpenAccess
tel-00285035
https://tel.archives-ouvertes.fr/tel-00285035
https://tel.archives-ouvertes.fr/tel-00285035/document
https://tel.archives-ouvertes.fr/tel-00285035/file/HDR_Titre_et_travaux_-_Gael_Nicolas.pdf