Showing 77673–77686 of 78,293 results for "PensoAssathiany Dominique"

Journals 2009 EN

Effective peer assessment processes: Research findings and future directions

Marjo van Zundert · Dominique Sluijsmans · Jeroen J. G. van Merriënboer

Despite the popularity of peer assessment (PA), gaps in the literature make it difficult to describe exactly what constitutes effective PA. In a literature review, we divided PA into variables and then investigated their interrelatedness. We found that (a) PA's psychometric qualities are improved by the training and experience of peer assessors; (b) the development of domain-specific skills benefits from PA-based revision; (c) the development of PA skills benefits from training and is related to students' thinking style and academic achievement, and (d) student attitudes towards PA are positively influenced by training and experience. We conclude with recommendations for future research.

Elsevier BV
Journals 2009 EN

ZAP-70 intron1 DNA methylation status: Determination by pyrosequencing in B chronic lymphocytic leukemia

Sylvain Chantepie · Dominique Vaur · Christoph Grunau +9 more

ZAP-70 expression is a strong prognostic indicator in chronic lymphocytic leukemia. However, ZAP-70 quantification by flow cytometry lacks sufficient standardization. Based upon the correlation between ZAP-70 expression and its gene methylation status, we have developed a quantitative pyrosequencing assay for the determination of ZAP-70 methylation adapted for routine use. Methylation in four CpG pairs (C-223, C-243, C-254, and C-267) in the first intron of ZAP-70 is associated with repression of ZAP-70. Moreover, it correlates with CD38 expression (n=111, p<.0001), IgHv mutation status (n=106, p<.0001), time to treatment (p<.0001), and overall survival (p=.0014). Pyrosequencing of ZAP-70 provides a good alternative to flow cytometry.

Elsevier BV
Journals 2009 EN

The Holocene occurrence of cold water corals in the NE Atlantic: Implications for coral carbonate mound evolution

Norbert Frank · Estelle Ricard · Audrey Lutringer-Paquet +8 more

U-series dating of constructional cold-water corals is a powerful tool to reconstruct the evolution of corals on carbonate mounds. Here we have investigated the time framework of corals such as Lophelia pertusa and Madrepora oculata on five different mound settings of the eastern North Atlantic (on Rockall Bank and in Porcupine Seabight), sampled at variable depth and location (610–880 m water depth). We have found that the past 11 ka reflect a period generally favourable for coral development. We further determined local mound growth rates and identified mound surface erosion (framework collapse) during times of active coral framework construction. “Local” vertical mound growth rates vary between less than 5 cm ka − 1 and up to 220 cm ka − 1 . We interpret rates exceeding 15 cm ka − 1 as representative of densely populated coral reefs. During times of reduced or absent coral development, mound evolution rates are by far smaller (0 to 10 ng g − 1 ) with 232 Th. To complete the coral growth records in cases, a few AMS 14 C ages were measured. Those AMS 14 C ages have been obtained according to the procedures described by ( Frank et al., 2004 ) and have been calibrated using the marine 14 C calibration of CALIB510 ( Stuiver et al., 1998 ) with a mean sub-surface water reservoir age of 500 ± 100 a ( Frank et al., 2004 ). 4 Results 4.1 U-series dating results Results of U-series dating of coral fragments are presented in Table 2 . The U concentration of cold-water species Lophelia pertusa and Madrepora oculata varies strongly between ~ 2.80 and ~ 5.0 μg g − 1 . Initial δ 234 U 0 values range between 140‰ and 155‰ with a mean of 148 ± 3.5‰ ( n = 63; standard deviation = ± 2 σ ) identical to measured present day seawater values of 146.6–149.6‰ ( Delanghe et al., 2002; Robinson et al., 2004 ). Measured 232 Th concentrations are small ( 70 cm ka − 1 ( Fig. 3 a). The initial start of the reef after the Younger Dryas cold reversal (12.9–11.5 ka calibrated BP) is followed by a period of rapid mound growth between 9.5 and 8.5 ka (~ 60 cm ka − 1 ), which is unfortunately poorly dated so far ( Fig. 3 a). Next, VMGR is 4 times lower (~ 15 cm ka − 1 ) until 6 ka followed again by a period of more rapid coral fragment accumulation from 6 to 5 ka. The VMGR is close to zero or at least strongly reduced thereafter at 4.4 ± 0.4 ka, 2.9 ± 0.1 ka, and at 1.9 ± 0.3 ka. In between those intervals of almost absent coral fragment deposition, VMGR are high (40 to 70 cm ka − 1 ). Finally during the past 1.5 ka the reef evolves again at a rate of ~ 30 cm ka − 1 ( Fig. 3 a). Core 55G located in close vicinity of core 54G but at shallower depth of 640 m reveals similar coral ages, but a strongly disturbed age–depth relationship ( Fig. 3 b). Note that the core is composed of mainly Madrepora oculata fragments, a species which construct a thinner and likely more unstable open framework. The dominant age reversal recorded between 70 and 156 cm core depth demonstrates clearly coral debris redistribution likely through physical erosion. This layer corresponds to a core section filled mainly with “coral rubble” (small broken fragments barely visible in the X-ray images) ( Fig. 2 -[3]). Corals in this section are about 9.4 ka to 11 ka old and are thus of equal ages compared to corals obtained at the base of core 54G. Consequently, we may assume that the M. oculata reef started to develop on top of exposed hardgrounds about 11 ka ago as did the Lophelia pertusa reef at deeper water depth (core 54G). During the Holocene, corals have than been displaced as a consequence of physical mound erosion. Below this section corals seem in chronological order and the few fragments dated reveal ages between 8 and 3 ka, but the resulting VMGRs are 15 cm ka − 1 , but local VMGRs can exceed 200 cm ka − 1 . Over the past 11 ka we have found first evidence of temporal changes in reef activity as coral abundances and mound growth rates decline to less than 10 cm ka − 1  at 1.8–2.0 ka, 4.2–4.8 ka and 6–8 ka. Moreover, the onset of the decline of corals activity coincides with a cold climate reversal at 8.2 ka. In addition, we have confirmed that periods favourable for coral growth on SW Rockall Bank and in Porcupine Seabight are related to overall climatic warm phases (MIS 1, 5, 7) and that coral growth is largely reduced or even absent “on mounds” during cold phases such as glacial periods and even MIS 3. Thus, coral growth records follow a glacial/interglacial pattern and are discontinuous in time and space. Detailed chronological studies, however, provide first evidence that those ecosystems are sensitive to even small changes of environmental conditions such as productivity, current activity and potentially water mass density affected by climate change. Finally, the reconstruction of mound evolution during the past 11 ka provides further constrains on mound evolution on geological time scales as it clearly highlights the strong variability of the vertical mound growth rates on solely a few thousand years and on less than a few cm core depth. Acknowledgements This work was funded through the European Union (projects: ECOMOUND, GEOMOUND, and HERMES : EVK3-CT-1999-00013, 00016 and GOCE-CT-2005-511234-1 ) and by the French Centre National de la Recherche Scientifique (CNRS) and the Commisariat à l'Energie Atomique (CEA) . We thank IPEV (Institut Polaire Emile Victor), the members and crew of GEOMOUND Marion Dufresne cruise, for their excellent work recovering these unique sediment cores and deep-water corals presented here. David van Rooij is a post-doctoral fellow of the FWO Flanders. O. Weber, M. Cremer and S. Saint-Paul (DGO, University Bordeaux) are acknowledged for their support with the SCOPIX analyses. Thanks to the constructive comments and critical questions of Augusto Mangini, Christine Hatté and an anonymous reviewer this manuscript has greatly improved. Furthermore, the work is part of the ESF Eurodiversity project MiCROSYSTEMS. References Abrantes, 1998 Abrantes F. Sediment fluxes along the northeastern European Margin: inferring hydrological changes between 20 and 8 kyr Marine Geology 152 1998 7 23 Adkins et al., 1998 Adkins J.F. Cheng H. Boyle E.A. Druffel E.R.M. Edwards R.L. Deep-sea coral evidence for rapid change in ventilation of the deep North Atlantic 15,400 years ago Science 280 1998 725 728 Benito et al., 2008 Benito G. Thorndycraft V.R. Rico M. Sánchez-Moya Y. Sopeña A. Palaeoflood and floodplain records from Spain: evidence for long-term climate variability and environmental changes Geomorphology 101 2008 68 77 Bond, 2001 Bond G. Persistent solar influence on North Atlantic climate during the Holocene Science 294 2130–2136 2001 Cheng et al., 2000a Cheng H. Adkins J.F. Edwards R.L. Boyle E.A. U–Th dating of deep-sea corals Geochimica et Cosmochimica Acta 64 2000 2401 2416 Cheng, 2000b Cheng H. The half-lives of uranium-234 and thorium-230 Chemical Geology 169 2000 17 33 de Haas, 2009 de Haas H. Morphology and sedimentology of (clustered) cold water coral mounds at the south Rockall Trough margins, NE Atlantic Ocean Facies 55 2009 1 26 de Mol, 2002 de Mol B. Large deep-water coral banks in the Porcupine Basin southeast of Ireland Marine Geology 188 2002 193 231 de Mol, 2007 de Mol B. Thérèse Mound: a case study of coral bank development in the Belgica Mound Province, Porcupine Seabight International Journal of Earth Science 96 2007 103 120 Delanghe et al., 2002 Delanghe D. Bard E. Hamelin B. New TIMS constraints on the uranium-238 and uranium-234 in seawaters from the main ocean basins and the Mediterranean Sea Marine Chemistry 80 2002 79 93 Dorschel et al., 2005 Dorschel B. Hebbeln D. Rüggeberg A. Dullo W.-C. Freiwald A. Growth and erosion of a cold-water coral covered carbonate mound in the Northeast Atlantic during the Late Pleistocene and Holocene Earth and Planetary Science Letters 233 2005 33 44 Dorschel et al., 2007 Dorschel B. Hebbeln D. Foubert A. White M. Wheeler A.J. Hydrodynamics and cold-water coral facies distribution related to recent sedimentary processes at Galway Mound west of Ireland Marine Geology 244 2007 184 195 Dullo et al., 2008 Dullo W.-C. Flögel S. Rüggeberg A. Cold-water coral growth in relation to the hydrography of the Celtic and Nordic European Continental Margin Marine Ecology Progress Series 371 2008 165 176 Eisele et al., 2008 Eisele M. Hebbeln D. Wienberg C. Growth history of a cold-water coral-covered carbonate mound — Galway Mound, Porcupine Seabight, NE Atlantic Marine Geology 253 2008 160 169 Ellett and Martin, 1973 Ellett D.J. Martin J.H.A. The physical and chemical oceanography of the Rockall Channel Deep-Sea Research 20 1973 585 625 Fossa, 2003 Fossa H. Report of the Study Group on Cold-Water Corals 2003 International Council for the exploration of the Sea Copenhagen Foubert, 2005 Foubert A. New view of the Belgica Mounds, Porcupine Seabight, NE Atlantic: preliminary results from the Polarstern ARK-XIX/3a ROV cruise A. Freiwald J.M. Roberts Cold-Water Corals and Ecosystems 2005 Springer-Verlag Berlin 403 415 Foubert et al., 2007 Foubert A. van Rooij D. Blamart D. Henriet J.P. X-ray imagery and physical core logging as a proxy of the content of sediment cores in cold-water coral mound provinces: a case study from Porcupine Seabight, SW of Ireland International Journal of the Earth Sciences 96 2007 141 158 Frank, 2004 Frank N. Eastern North Atlantic deep-sea corals: tracing upper intermediate water Delta14C during the Holocene Earth and Planetary Science Letters 219 2004 297 309 Frank, 2005 Frank N. Cold water corals of the northeastern Atlantic margin: carbonate mound evolution and upper intermediate water ventilation during the Holocene A. Freiwald Springer Special Publication 2005 Springer Berlin, Heidelberg Freiwald and Roberts, 2005 Freiwald A. Roberts J.M. Cold-water corals and ecosystems, 1 2005 Springer Heidelberg 1243 pp Freiwald et al., 1997 Freiwald A. Henrich R. Pätzold J. Anatomy of a deep-water coral reef mound from Stjernsund West Finnmark, northern Norway SEPM Special Publications 56 1997 141 162 Gass and Roberts, 2006 Gass S.E. Roberts J.M. The occurrence of the cold water coral Lophelia pertusa (Scleractinia) on oil and gas platforms in the North Seas: colony growth, recruitment and environmental controls on distribution Marine Pollution Bulletin 52 2006 549 559 Henriet, 1998 Henriet J.P. Gas hydrate crystals may help build reefs Nature 391 1998 648 649 Holliday et al., 2000 Holliday N.P. Pollard R.T. Read J.F. Leach H. Water mass properties and fluxes in the Rockall Trough 1975–1998 Deep-Sea Research I 47 2000 1303 1332 Hovland et al., 1994 Hovland M. Croker P.F. Martin M. Fault-associated seabed mounds (carbonate knolls?) off western Ireland and north-west Australia Marine and Petroleum Geology 11 2 1994 232 246 Hovland et al., 1998 Hovland M. Mortensen P.B. Brattegard T. Strass P. Rokoengen K. Ahermatypic coral banks off mid-Norway: evidence for a link with seepage of light hydrocarbons Palaios 13 1998 189 200 Huthnance, 1986 Huthnance J.M. The Rockall Slope Current and shelf edge processes Proceedings of the Royal Society of Edinburgh 88 B 1986 83 101 Huvenne et al., 2003 Huvenne V. de Mol B. Henriet J.P. A 3D seismic study of the morphology and spatial distribution of buried coral banks in the Porcupine Basin, SW of Ireland Marine Geology 198 2003 5 25 Huvenne, 2005 Huvenne V.A.I. The seabed appearance of different coral bank provinces in the Porcupine Seabight, NE Atlantic: results from sidescan sonar and ROV seabed mapping A. Freiwald J.M. Roberts Cold Water Corals and Ecosystems 2005 Springer Verlag Berlin Heidelberg 535 569 Huvenne, 2007 Huvenne V.A.I. The Magellan mound province in the Porcupine Basin International Journal of Earth Sciences 96 2007 85 101 Kano, 2007 Kano A. Age constraints on the origin and growth history of a deep-water coral mound in the northeast Atlantic drilling during integrated Ocean Drilling Program Expedition 307 Geology 35 11 2007 1051 1054 Kenyon, 2003 Kenyon N.H. Giant carbonate mud mounds in the southern Rockall Trough Marine Geology 195 2003 5 30 Kobashia et al., 2007 Kobashia T. Severinghausa J.P. Brookb E.J. Barnolac J.-M. Gracheva A.M. Precise timing and characterization of abrupt climate change 8200 years ago from air trapped in polar ice Quaternary Science Reviews 26 2007 1212 1222 Lomitschka and Mangini, 1999 Lomitschka M. Mangini A. Precise Th/U-dating of small and heavily coated samples of deep sea corals Earth and Planetary Science Letters 170 1999 391 401 Mangini, 1998 Mangini A. Coral provides way to age deep water Nature 392 1998 347 Mangini, 2007 Mangini A. Persistent influence of the North Atlantic hydrography on central European winter temperature during the last 9000 years Geophysical Research Letters 2007 34 L02704. doi: 10.1029/2006GL028600 Manighetti and McCave, 1995 Manighetti B. McCave I.N. Late glacial and Holocene paleocurrents around Rockall Bank, NE Atlantic Ocean Paleoceanography 10 3 1995 611 626 Mienis, 2007 Mienis F. Hydrodynamic controls on cold-water coral growth and carbonate-mound development at the SW and SE Rockall Trough Margin, NE Atlantic Ocean Deep-Sea Research I 54 2007 1655 1674 Mienis, 2009 Mienis F. Carbonate accumulation on a cold water carbonate mound at southwest Rockall Trough margin Marine Geology 265 2009 40 50 Mikkelsen et al., 1982 Mikkelsen N. Erlenkeuser H. Killingley J.S. Berger W.H. Norwegian corals: radiocarbon and stable isotopes in Lophelia pertusa Boreas 11 1982 163 171 Mortensen and Rapp, 1998 Mortensen P. Rapp H.T. Oxgyen and carbon isotope ratios related to growth line patterns in skeletons of Lophelia pertusa ( L. pertusa ) (Anthozoa, Scleractinia): implications for determination of linear extension rates Sarsia 83 1998 433 466 New and Smythe-Wright, 2001 New A.L. Smythe-Wright D. Aspects of the circulation in the Rockall Trough Continental Shelf Research 21 2001 777 810 Olu Le-Roy, 2004 Olu Le-Roy K. Les coraux profonds: une biodiversité à évaluer et à préserver VERTIGO Revue Electronique en Environnement 5 2004 Olu Le-Roy, 2002 Olu Le-Roy K. Shipboard Scientific Crew NO ‘Atalante’ and ROV ‘Victor 6000’ 2 2002 IFREMER Brest Roberts et al., 2006 Roberts M. Wheeler A.J. Freiwald A. Reefs of the deep: the biology and geology of deep-water coral ecosystems Science 312 2006 543 547 Robinson et al., 2004 Robinson L.F. Belshaw N.S. Henderson G.M. U and Th concentrations and isotope ratios in modern carbonates and waters from the Bahamas Geochimica et Cosmochimica Acta 68 8 2004 1777 1789 Roberts et al., 2009 J.M. Roberts A.J. Wheeler A. Freiwald S. Cairns Cold-Water Corals: The Biology And Geology Of Deep-Sea Coral Habitats 2009 Cambridge University Press Cambridge 334 pp Rüggeberg et al., 2003 Rüggeberg A. Dorschel B. Dullo W.-C. Hebbeln D. Environmental control on Propeller Mound (Hovland Mound Province) during the past interglacial–glacial Cycles A. Freiwald C. Schulbert 2nd International Symposium on Deep-Water Corals 2003 Erlanger geologische Abhandlungen Erlangen, Germany 109 Rüggeberg et al., 2007 Rüggeberg A. Dullo C. Dorschel B. Hebbeln D. Environmental changes and growth history of Propeller Mound, Porcupine Seabight: evidence from benthic foraminiferal assemblages International Journal of Earth Sciences 96 2007 57 72 Schröder-Ritzrau et al., 2003 Schröder-Ritzrau A. Mangini A. Lomitschka M. Deep-sea corals evidence periodic reduced ventilation in the North Atlantic during the LGM/Holocene transition Earth and Planetary Science Letters 216 2003 399 410 Schröder-Ritzrau et al., 2005 Schröder-Ritzrau A. Mangini A. Freiwald A. U/Th-dating of deep-water corals from the Eastern North Atlantic and the Mediterranean Sea A. Freiwald C.N. Roberts Cold-Water Corals and Ecosystems 2005 Springer Berlin, Heidelberg 159 174 Smith et al., 1997 Smith J.E. Risk M.J. Schwarcz H.P. McConnaughey T.A. Rapid climate change in the North Atlantic during the Younger Dryas recorded by deep-sea corals Nature 386 1997 818 820 Stuiver, 1998 Stuiver M. Intcal98 radiocarbon age calibration: 24,000–0 cal BP Radiocarbon 40 3 1998 1041 1083 Thornalley et al., 2009 Thornalley D.J.R. Elderfield H. McCave N. Holocene oscillations in temperature and salinity of the surface subpolar North Atlantic Nature 457 2009 711 713 van Aken and Becker, 1996 van Aken H.M. Becker G. Hydrography and through-flow in the north-eastern North Atlantic Ocean: the NANSEN project Progresse in Oceanography 38 1996 297 346 Van Rooij, 2006 Van Rooij D. Quaternary sediment dynamics in the Belgica Mound province, Porcupine Seabight: ice-rafting events and contour current processes International Journal of the Earth Sciences. 2006 doi: 10.1007/s00531-006-0068-6 Van Rooji et al., 2001 Van Rooji D. Blamart D. Unnithan V. Cruise-report MD123 Geosciences: Leg 2, part GEOMOUND Porcupine Basin and Rockall Trough, Off Western Ireland 2001 van Weering et al., 2003 van Weering T. de Haas H. de Stigter H.C. Lykke-Andersen H. Kouvaev I. Structure and development of giant carbonate mounds at the SW and SE Rockall Trough margins, NE Atlantic Ocean Marine Geology 198 2003 67 81 van Weering, 1999 van Weering T. shipboard scientific party Shipboard Cruise Report R.V. Pelagia 64PE143: A Survey Of Carbonate Mud Mounds of Porcupine Bight and S. Rockall Trough Margins, NIOZ, Texel 1999 Vollweiler et al., 2006 Vollweiler N. Scholz D. Müllinghausen C. Mangini A. Spötl C. A precisely dated climate record for the past 9 kyrs from three high alpine stalagmites, Spannagal Cave, Austria Geophysical Research Letters 33 2006 1 5 Wheeler, 2005 Wheeler A.J. Sedimentary processes and carbonate mounds in the Belgica Mound province, Porcupine Seabight, NE Atlantic A. Freiwald J.M. Roberts Cold Water Coral Ecosystems 2005 Springer Verlag Berlin Heidelberg 571 603 Wheeler, 2007 Wheeler A.J. Morphology and environment of cold-water coral carbonate mounds on the NW European margin International Journal of Earth Sciences 96 2007 37 56 White and Bowyer, 1997 White M. Bowyer P. The shelf edge current northwest of Ireland Annals of Geophysics 15 1997 1076 1083 White et al., 2005 White M. Mohn C. De Stigter H.C. Mottram G. Deep-water coral development as a function of hydrodynamics and surface productivity around submarine banks of Rockall Trough, NE Atlantic A. Freiwald J.M. Roberts Cold-Water Corals And Ecosystems 2005 Springer Heidelberg 501 514 Williams et al., 2006 Williams T. Kano A. Ferdelman T. Henriet J.P. party I.E.s. Cold-water coral mounds revealed EOS 87 47 2006 525 526

Elsevier BV
Journals 2009 EN

Microstructure evolution of HP40-Nb alloys during aging under air at 1000 °C

Raluca Voicu · Éric Andrieu · Dominique Poquillon +2 more

Two as-cast HP 40 alloys provided by different manufacturers were aged at 1000 °C under\udlaboratory air. They had the same as-cast microstructure consisting of austenite dendrites\uddelineated by a network of eutectic Nb-rich MC and Cr-rich M7C3 carbides. After aging for\udseveral months, they showed similar microstructures in the bulk materials, though M7C3\udcarbides have been replaced by M23C6 carbides. As expected, a sub-surface zone depleted in\udchromium has appeared where a tetragonal CrNbC could be identified in both materials.\udHowever, the composition of the transition zones between the surface and the bulk\udmaterials differed, mainly because one of the materials underwent significant nitrogen\udpick-up with associated precipitation of M6(C,N) and M2(C,N) phases. On the contrary, the\udother alloy did show only one intermediate zone with a mix of CrNbC, M23C6 and MC\udcarbides. A full account of the microstructures observed in the aged materials is given

Elsevier BV
Journals 2009 EN

Menopause and modifiable coronary heart disease risk factors: A population based study

Nelly Agrinier · Maxime Cournot · Jean Dallongeville +4 more

The aim of our study was to determine the effect of the menopause on various coronary heart disease (CHD) risk factors and on the global risk of CHD in a population based sample of women, making the difference between menopause and age related effects.

Elsevier BV
Journals 2009 EN

Role of the ghrelin/obestatin balance in the regulation of neuroendocrine circuits controlling body composition and energy homeostasis

Jacques Epelbaum · Nawel Bedjaoui · Roland Dardennes +8 more

Ghrelin and obestatin are two peptides isolated from the gastrointestinal tract and encoded by the same preproghrelin gene. They convey to the central nervous system informations concerning the nutritional status and/or the energy stores. Ghrelin, mostly acting through the GH secretagogue receptor GHS-R, is a potent GH secretagogue, an orexigenic peptide and a long-term regulator of energy homeostasis. Obestatin was initially described for its anorexigenic effects and its binding to the G protein-coupled receptor 39 (GPR39). However, the role of obestatin is still controversial and the nature of the obestatin receptor remains an open question. This review is focussed on the possible implication of the ghrelin/obestatin system in psychiatric diseases with particular emphasis on eating disorders.

Elsevier BV
Journals 2009 EN

Développement d’actions de prévention du VIH, des hépatites et des infections sexuellement transmissibles chez les immigrants consultant dans les missions France de Médecins du monde

Marie-Dominique Pauti · Nathalie Simonnot · Pascale Estecahandy

The mission France of Doctors of the World has for objective to facilitate the access to care and to rights in the common law system for vulnerable populations and to bring testimonies out. The objective of the project is to ensure daily actions of prevention: to bring people to screen for HIV and hepatitis as well as obtaining full access to treatment for populations consulting in the Reception centers for Care and Orientation (RCCO). The screening is proposed systematically to all new patients (90% of them are immigrants) after a medical consultation or a special prevention consultation. The prevalence of HIV, hepatitis B and C was respectively 15, 10.5, and 7 times higher than the national average among patients screened in 2007, The centers of Doctors of the World are privileged places to inform, prevent, offer screening, and bring healthcare to this population particularly exposed to risks.

Elsevier BV
Journals 2009 EN

S05-04. Evolutionary diversity and developmental dynamics of X-chromosome inactivation

Ikuhiro Okamoto · Véronique Duranthon · Dominique Thépot +3 more

X-chromosome inactivation ensures dosage compensation for X-linked genes products in mammals. In eutherian mammals, X inactivation is controlled by the non-coding Xist transcript and is believed to be random, with either the paternal or maternal X chromosome being chosen for silencing. In mice, where most studies on the developmental timing of X inactivation have been conducted, Xist expression is initially imprinted and only the paternal X chromosome is inactivated during early mouse development and in extraembryonic tissues. This imprinted form of X inactivation is reversed in the inner cell mass, after which random X inactivation takes place in embryonic lineages. Whether this complex pattern of Xist expression and X-inactivation dynamics exists in other mammals remains unclear. Indeed, the degree to which the X-inactivation process is conserved between different mammals remains an open question. For example, marsupials have no Xist gene and show exclusive paternal X inactivation in all lineages. We have investigated X inactivation during early embryogenesis in other mammals such as rabbits, and find that the kinetics and monoallelic regulation of X inactivation are very different to the situation in mice. Our results suggest that although some molecular mechanisms are shared, there is remarkable evolutionary diversity in the developmental events underlying dosage compensation in different mammals.

Elsevier BV
Journals 2009 EN

Experimental and numerical study on effect of forming rate on AA5086 sheet formability

Cunsheng Zhang · Lionel Leotoing · Dominique Guines +1 more

International audienceWith increasing application of aluminum alloys in automotive or aeronautic industries, it is necessary to characterize their deformation behaviors at large strains, high strain rates and elevated temperatures, which is relatively lacking today. The aim of this paper is to experimentally and numerically investigate the influence of forming rate and temperature on formability of an AA5086 sheet. Firstly, tensile tests are carried out at different temperatures (20, 230, 290 and 350 ◦C) and at different forming rates (10, 750 and 1000 mm/s). A technique of digital image correlation (DIC) associated with a high-speed camera is applied to evaluate the surface strains and a complete procedure is built to detect the onset of localized necking during the experiments. The influences of initial testing temperature and forming rate on the sheet formability are analyzed. Then in order to numerically determine the formability of this sheet, a form of Voce's constitutive law taking into account the temperature and strain rate is proposed. An inverse analysis is carried out to identify the material parameters of the law for the tested aluminum alloy. Finally, with the above identified law, tensile tests are simulated. The experimental and numerical results show that the testing temperature and forming rate have a great influence on sheet formability. At high forming rates, the sheet formability of AA5086 is lowered up to a certain temperature, above this temperature, the formability is greatly enhanced. Furthermore, the agreement between experimental and numerical results indicates that the proposed constitutive law and the identified material parameters can be appropriate to model the sensitivity of AA5086 sheet towards strain rate and temperature

Elsevier BV