Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The morphogenetic evolution of the Lesser Caucasus has been strongly influenced by Plio-Quaternary volcanic and tectonic events and Pleistocene glaciations. Fluvio-lacustrine environments, indicated by diatomaceous deposits, prevailed in the Syunik region of southern Armenia during the Pliocene and Pleistocene. The Pleistocene diatomaceous deposits studied contain leaf impressions and pollen, allowing local palaeoclimatic reconstructions. The chronology of morphogenetic events has been determined by 17 radiometric dates (K/Ar, Ar/Ar, U/Th), palaeomagnetic investigations and is placed in a spatial context by a detailed geomorphological map and a 24-km geological transect of the Vorotan valley, the main area studied. Before 1.21 Ma, tectonic movements (antecedents of the lower part of the Vorotan valley) generated extensive lake formations with diatomaceous deposits. From 993 ka, volcanic eruptions produced lava flows that covered the fluvio-lacustrine accumulations. During Marine Isotopic Stages 12, 6 and 4, glaciers and fluvio-glacial deposits were probably present overall the principal uplands and valleys of southern Armenia. At 53.68 ka (MIS 3), 12.6 ka, 10.78 ka and 4.14 ka (MIS 1), the development of travertines on some slopes and in some valleys highlights temperate and humid climatic phases. Palaeobotanical studies of leaf and pollen floras show that the vegetation changed several times from forested to steppic phases in response to the climate oscillations of the Lower Pleistocene. This work proposes a first morphogenic and palaeoclimatic reconstruction from the lower Pleistocene to the Postglacial period, when the first settlements of the population in the Lesser Caucasus were influenced by tectono-volcanic events, lake level changes and glacialeinterglacial oscillations forced by the obliquity orbital parameter (41 ky cycles).
ISSN: 1040-6182

hal-00481939
https://hal.archives-ouvertes.fr/hal-00481939
DOI : 10.1016/j.quaint.2010.02.008

Éditeur(s) : HAL CCSD Elsevier
Résumé : Adequate hydrogeophysical monitoring of CO2 geological storage remains a challenge as different parameters might be modified during storage. That implies to compare real-time measurements to an adequate baseline. At the Maguelone shallow experimental site a representative baseline for electrical resistivity was built from a large number of downhole geophysical measurements. At this coastal site this issue is particularly important due to the production of biogenic gas from the subsurface sediments. For this, a modified petrophysical model based on the Waxman-Smits model is proposed to estimate gas saturation found to vary from 2 to 7% within shallow sand layers.
ISSN: 1876-6102

hal-01412685
https://hal.archives-ouvertes.fr/hal-01412685
https://hal.archives-ouvertes.fr/hal-01412685/document
https://hal.archives-ouvertes.fr/hal-01412685/file/pezard2015.pdf
DOI : 10.1016/j.egypro.2015.07.910

Éditeur(s) : HAL CCSD Elsevier Masson
Résumé : National audience
Introduction Les péritonites secondaires à levures représentent une part importante des candidoses profondes et de leur traitement. Peu d’outils sont disponibles afin de prédire au mieux les patients susceptible d’avoir une culture du liquide péritonéal positive. L’étude AMARCAND II (10/202–09/2013) a analysé les patients de réanimation recevant un traitement antifongique pour un candidose invasive prouvée ou suspectée. L’analyse des patients ayant un traitement probabiliste pour péritonite à levure suspectée est présentée ici. Patients et méthodes Cent soixante-douze patients parmi les 835 inclus ont été analysés. Les patients ayant une documentation mycologique (groupe D) ont été comparés à ceux ayant une culture à levure négative (groupe ND). La performance du Candida score [1] et du Peritonitis score [2] ont été évalués dans cette population de candidose profonde suspectée. Résultats Parmi les 172 patients, 51 ont eu une péritonite documentée à levure et 121 un culture à levure négative. Les caractéristiques des groupes sont présentées dans le Tableau 1. L’AUC du Peritonitis score était de 0,63 [0,54–0,72] contre 0,40 [0,31–0,49] pour le Candida score, p = 0,005. Pour un Peritonitis score ≥ 3, la sensibilité était de 39,2 %, la spécificité de 81,8 %, la VPP de 47,6 % et la VPN de 76,2 %. Le Candida score ne permettait pas de classer les patients atteints de péritonite à levure. Discussion Peu d’éléments permettent de différencier les patients qui vont avoir une infection documentée des autres. La localisation sus-mésocolique de l’infection et l’antibiothérapie de plus de 48 heures sont les éléments les plus fiables retrouvés. Le Peritonitis score reste intéressant dans ce contexte mais le Candida score n’a aucune utilité
ISSN: 2352-5800

hal-01244999
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01244999
DOI : 10.1016/j.anrea.2015.07.329

Éditeur(s) : HAL CCSD Elsevier Masson
Résumé : International audience
Antisynthetase syndrome is an inflammatory myopathy frequently associated with pulmonary manifestations, especially interstitial lung diseases, and uncommonly pulmonary hypertension. In the context of a suggestive clinical and radiological picture, positive anti-RNA synthetase antibodies confirm the diagnosis. Anti-Jo1, anti-PL7, and anti-PL12 antibodies are the more commonly encountered. The presence of a number of extra-thoracic manifestations in association with pulmonary disease may suggest the diagnosis. These include: myalgia or muscular deficit, Raynaud's phenomenon, polyarthritis, fever, mechanics hands. Serum creatine kinase levels are usually increased. Electromyogram, muscular magnetic resonance imaging or muscle pathology are not mandatory to make the diagnosis. There is a high variability in symptoms and severity, between patients but also during the course of the disease in the same patient. The presence of an interstitial lung disease is a major prognostic factor and an indication for more intensive treatment, principally with systemic corticosteroids with or without immunosuppressive drugs. Improving respiratory physicians’ knowledge of this disease, which is often revealed by its pulmonary manifestations, should help diagnosis, therapeutic management, and possibly prognosis.
Le syndrome des antisynthétases correspond à une myopathie inflammatoire fréquemment associée à une atteinte pulmonaire, surtout parenchymateuse (pneumopathie infiltrante diffuse) et plus rarement vasculaire (hypertension pulmonaire). Devant un tableau clinique et radiologique évocateur, la présence d’anticorps anti-ARNt synthétases signe le diagnostic. Les plus fréquents de ces auto-anticorps sont les anti-Jo1, les anti-PL7 et les anti-PL12. De nombreuses manifestations cliniques extrathoraciques associées à l’atteinte pulmonaire peuvent orienter le diagnostic : myalgies ou déficit musculaire, phénomène de Raynaud, polyarthrite, fièvre et « mains de mécaniciens ». Une augmentation des créatine-phospho-kinases est quasi constante. Le recours à l’électromyogramme, à l’imagerie musculaire par résonance magnétique ou à l’histologie n’est pas systématique. Néanmoins, il existe une grande variabilité des symptômes et de leur sévérité d’un patient à l’autre ou au long de l’évolution de la maladie. L’atteinte pulmonaire est un facteur pronostic majeur et incite à traiter de manière intensive les patients, principalement par corticothérapie systémique, voire d’emblée par association corticoïdes et immunosuppresseurs. Mieux connaître cette pathologie qui est souvent de révélation pneumologique permettrait d’améliorer le diagnostic et la prise en charge thérapeutique, voire même le pronostic.
ISSN: 0761-8425

hal-01085369
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01085369
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01085369/document
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01085369/file/Manifestations%20pulmonaires%20du%20syndrome%20des%20antisynth%C3%A9tases_accepted.pdf
DOI : 10.1016/j.rmr.2014.07.013

Éditeur(s) : HAL CCSD American Geophysical Union (AGU)
ISSN: 0278-7407

hal-00406419
https://hal.archives-ouvertes.fr/hal-00406419
DOI : 10.1029/2006TC002022

Éditeur(s) : HAL CCSD Dunod
Résumé : Cet ouvrage présente les différents séismes et les origines des soubresauts de la Terre. La sismotectonique est également étudiée : pourquoi, quand et comment se produit la rupture. Chaque faille révèle une histoire (archéosismicité, palésoisismicité, néotectonique) que le géologue, l'architecte et l'urbaniste doivent connaître pour mieux appréhender le risque sismique. Ainsi, les méthodes et les techniques utilisées pour mesurer un risque sismique et le prévenir sont largement étudiées. Le cours fait référence à de nombreux exemples sous la forme d'encarts. Des exercices corrigés permettent à l'étudiant de mettre en oeuvre ses connaissances
https://hal.archives-ouvertes.fr/hal-00408297

hal-00408297
https://hal.archives-ouvertes.fr/hal-00408297

Éditeur(s) : HAL CCSD American Geophysical Union
Résumé : International audience
This study describes a laboratory experiment on rip current circulations over a moveable bed. Rip current characteristics over eight contrasting nature-like beach morphologies are investigated. The seabed varied from reasonably alongshore uniform to strongly alongshore nonuniform with crescentic patterns and bar-rip morphologies, representative of a full morphological down-state sequence. The same offshore shore-normal waves were generated by the wavemaker for the eight situations with the same mean water level to study the sensitivity of rip current characteristics as a function of the beach morphology only. In each case, a 30 to 60 min video run was used to track a large number of drifters released within the surf zone. Results show the presence of classic rip current patterns with counterrotating cells and a relatively narrow offshore-directed jet varying from shore-normal to strongly skewed. Wave-driven circulations were strongly unstable. Computed standard deviations of flow intensity and direction provide high-resolution information on the spatial variability of rip current instabilities. Highly pulsating and weakly directionally variable offshore-directed flow is observed in the rip neck for well-developed bar-rip morphologies that turns into a weakly pulsating and highly directional variable rip current flow with decreasing beach alongshore nonuniformity. Proposing a definition of rip current intensity based on the rip current circulation geometry, rip current intensity was found to linearly increase with increasing measure of beach alongshore nonuniformity within both the low-energy and moderate-energy rip current regimes. To date, our laboratory experiment provides the first extensive quantitative rip current information during a full down-state sequence for a given wave condition.
ISSN: 0148-0227

hal-00602920
https://hal.archives-ouvertes.fr/hal-00602920
DOI : 10.1029/2010JC006343

Éditeur(s) : HAL CCSD World Scientific
Résumé : The present paper presents a laboratory experiment of rip current circulations over a moveable bed. The rip current characteristics over four distinct beach morphologies, exhibiting more or less developed nature-like bar-rip morphology,were investigated. For each video run, the same off shore shore-normal waves were generated by the wave maker with the same mean water level in order to study the sensitivity of the rip current characteristics as a function of the beach morphology only. In each case, a 1-hour video run was used to track a large number (~30) of drifters released within the surf zone. Image coordinates were then rectifie d to still water level Cartesian coordinates to compute drifter velocities, mean characteristics and surf zone rete ntion rates. Results show the presence of classic rip current patterns with counter-rotating cells and a relatively narrowoffshore-directed jet with, for three of the situations, a reasonably symmetric shape. Non-surprisingly, it was found that rip current intensity increases with increasing relative depth of the rip channel. The wave-driven circulations were strongly unstable. Computed standard deviation in fl ow intensity and direction provides high resolution information on the spatial variability of the rip current insta bilities with, for instance, highly-pulsating and weakly directionally variable offshore-directed flow in the rip channel. Conversely to what was previously hypothesized in the literature, there was hardly trace of vortices being shed offs hore and drifters exiting the surf zone compartment were not systematically caught by a pulsating jet. The cause for drifter exiting the semi-enclosed surf zone compartment remains, however, elusive and deserves further investigations. The computed surf zone retention rates (~90%) were of the order of those previously observed in the field, with no clear relationship with the mean rip current velocity or relative depth of the rip channel. Further video-runs will have to be analyzed to explore potential explanations
Proceedings of Coastal Dynamics 2009 Impacts of Human Activities on Dynamic Coastal Processes

ISBN : 978-981-4282-46
hal-00854534
https://hal.archives-ouvertes.fr/hal-00854534

Éditeur(s) : HAL CCSD Elsevier
Résumé : The variability of fluvial activity in the Northwestern Mediterranean coastal lowlands and its relationship with modes of climate change were analysed from the late 9th to the 18th centuries CE. Geochemical analyses were undertaken from a lagoonal sequence and surrounding sediments in order to track the fluvial inputs into the lagoon. An index based on the K/S and Rb/S ratios was used to evidence the main periods of fluvial activity. This index reveals that the Medieval Climate Anomaly (MCA) was a drier period characterized by a lower fluvial activity, while the Little Ice Age (LIA) was a wetter period with an increase of the river dynamics. Three periods of higher than average fluvial activity were evidenced at the end of the first millennium CE (ca. 900–950 cal yr CE), in the first half of the second millennium CE (ca. 1150–1550 cal yr CE), and during the 1600s–1700s CE (ca. 1650–1800 cal yr CE). The comparison of these fluvial periods with other records of riverine or lacustrine floods in Spain, Italy, and South of France seems to indicate a general increase in fluvial and flood patterns in the Northwestern Mediterranean in response to the climate change from the MCA to the LIA, although some episodes of flooding are not found in all records. Besides, the phases of higher than average fluvial dynamics are in good agreement with the North Atlantic cold events evidenced from records of ice-rafted debris. The evolution of fluvial activity in the Northwestern Mediterranean coastlands during the last millennium could have been driven by atmospheric and oceanic circulation patterns.Keywords
ISSN: 0921-8181

hal-01571958
https://hal.archives-ouvertes.fr/hal-01571958
DOI : 10.1016/j.gloplacha.2017.03.008

Éditeur(s) : HAL CCSD
XVIII International Botanical Congress - IBC 2011
Melbourne, Australia

hal-01032388
https://hal.archives-ouvertes.fr/hal-01032388

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Northwest Iran is characterized by a high level of historical and instrumental seismicity related to the ongoing convergence between the Arabian and Eurasian plates. In this region, the main right-lateral strike-slip fault known as the North Tabriz fault (NTF) forms the central portion of a large crustal fault system called the Tabriz fault system (TFS). The NTF is a major seismic source along which at least three strong and destructive earthquakes have occurred since 858 AD. The two most recent destructive seismic events occurred in 1721 AD and 1780 AD, rupturing the SE and NW fault segments, respectively. This paper reports paleoseismological and quantitative geomorphologic investigations on the SE segment of the NTF, between the cities of Bostanabad and Tabriz. These observations help to improve our understanding of the seismic hazard for Tabriz city and its surrounding areas. Our field investigations revealed evidence of successive faulting events since the Late Quaternary. Paleoseismic investigations indicate that since 33.5 kyr, the SE segment of the NTF has experienced at least three major (M>7.5) seismic events, including the 1721 AD earthquake (M=7.6–7.7). Along the NW segment of the fault, however, our results suggest that the amount of strong (M~7.5) seismic events during the same period is significantly greater than along the SE segment. One possible explanation of such a difference in seismic activity is that the Late Quaternary-Holocene coseismic slip rate is decreasing along the NTF from the northwest to the southeast. This explanation contradicts the former hypothesis of a constant slip rate along the whole length of the NTF. In addition, more distributed deformation along several parallel fault branches, in a wider fault zone of the SE segment of the NTF may be considered as additional evidence for the estimation of lower rate of deformation along the fault segment. Such a slip distribution pattern can explain the existence of smaller (~300 m) Pliocene-Quaternary cumulative dextral offsets along the SE fault segment than the measured cumulative offsets along the NW segment (~800 m) of the NTF.
ISSN: 0040-1951

hal-01089420
http://hal.upmc.fr/hal-01089420
http://hal.upmc.fr/hal-01089420/document
http://hal.upmc.fr/hal-01089420/file/Solaymani%20Azad%20et%20al.%2C%202014%20%28accepted%29.pdf
DOI : 10.1016/j.tecto.2014.11.010