La nutrigénomique dans votre assiette

Formatés par une société qui accorde une place prépondéranze au bien-être et qui nous incite à prendre soin de notre apparence physique, nous sommes paradoxalement confrontés à un monde graduellemet gagné par l'obésité et les maladies qui lui sont associées. Celles-ci reflètent l'inadéquation entre les régimes alimentaires modernes, la sédentarité croissante des populations et le patrimoine génétique que nous avons hérité de nos ancêtres.Comment parvenir à nous nourrir en bonne intelligence avec nos gènes et notre style de vie ? La réponse se trouve peut-être du coté de la génomique, ou nutrigénomique, cette toute nouvelle discipline qui s'intéresse à l'influence de l'alimentation sur les gènes.Médecine, biologie, sciences humaines, industrie pharmaceutique et industrie agroalimentaire trouveront avantage à s'associer pour faire de la nutrigénomique un élément d'innovation scientifique et sociétale dans la prévention et la lutte contre les maladies liées à des régimes inappropriés.

Decision-theoretic reflections on processing a fingermark

A recent publication in this journal [Neumann et al., Forensic Sci. Int. 212 (2011) 32-46] presented the results of a field study that revealed the data provided by the fingermarks not processed in a forensic science laboratory. In their study, the authors were interested in the usefulness of this additional data in order to determine whether such fingermarks would have been worth submitting to the fingermark processing workflow. Taking these ideas as a starting point, this communication here places the fingermark in its context of a case brought before a court, and examines the question of processing or not processing a fingermark from a decision-theoretic point of view. The decision-theoretic framework presented provides an answer to this question in the form of a quantified expression of the expected value of information (EVOI) associated with the processed fingermark, which can then be compared with the cost of processing the mark.

Mineral zoning and geochemistry of epithermal polymetallic Zn-Pb-Ag-Cu-Bi mineralization at Cerro de Pasco, Peru

The large Cerro de Pasco Cordilleran base metal deposit in central Peru is located on the eastern margin of a middle Miocene diatreme-dome complex and comprises two mineralization stages. The first stage consists of a large pyrite-quartz body replacing Lower Mesozoic Pucara carbonate rocks and, to a lesser extent, diatreme breccia. This body is composed of pyrite with pyrrhotite inclusions, quartz, and black and red chalcedony (containing hypogene hematite). At the contact with the pyrite-quartz body, the diatreme breccia is altered to pyrite-quartz-sericite-pyrite. This body was, in part, replaced by pipelike pyrrhotite bodies zoned outward to carbonate-replacement Zn-Pb ores hearing Fe-rich sphalerite (up to 24 mol % Fes). The second mineralization stage is partly superimposed on the first and consists of zoned east-west-trending Cu-Ag-(Au-Zn-Pb) enargite-pyrite veins hosted in the diatreme breccia in the western part of the deposit and well-zoned Zn-Pb-(Bi-Ag-Cu) carbonate-replacement orebodies; in both cases, sphalerite is Fe poor and the inner parts of the orebodies show typically advanced argillic alteration assemblages, including aluminum phosphate Sulfate (APS) minerals. The zoned enargite-pyrite veins display mineral zoning, from a core of enargite-pyrite +/- alunite with traces of Au, through an intermediate zone of tennantite, chalcopyrite, and Bi minerals to a poorly developed Outer zone hearing sphalerite-galena +/- kaolinite. The carbonate-hosted replacement ores are controlled along N 35 degrees E, N 90 degrees E, N 120 degrees E, and N 170 degrees E faults. They form well-zoned upward-flaring pipelike orebodies with a core of famatinite-pyrite and alunite, an intermediate zone with tetrahedrite-pyrite, chalcopyrite, matildite, cuprobismutite, emplectite, and other Bi minerals accompanied by APS minerals, kaolinite, and dickite, and an outer zone composed of Fe-poor sphalerite (in the range of 0.05-3.5 mol % Fes) and galena. The outermost zone consists of hematite, magnetite, and Fe-Mn-Zn-Ca-Mg carbonates. Most of the second-stage carbonate-replacement orebodies plunge between 25 degrees and 60 degrees to the west, suggesting that the hydrothermal fluids ascended from deeper levels and that no lateral feeding from the veins to the carbonate-replacement orebodies took place. In the Venencocha and Santa Rosa areas, located 2.5 km northwest of the Cerro de Pasco open pit and in the southern part of the deposit, respectively, advanced argillic altered dacitic domes and oxidized veins with advanced argillic alteration halos occur. The latter veins are possibly the oxidized equivalent of the second-stage enargite-pyrite veins located in the western part of the deposit. The alteration assemblage quartz-muscovite-pyrite associated with the pyrite-quartz body suggests that the first stage precipitated at slightly, acidic fin. The sulfide mineral assemblages define an evolutionary path close to the pyrite-pyrrhotite boundary and are characteristic of low-sulfidation states; they suggest that the oxidizing slightly acidic hydrothermal fluid was buffered by phyllite, shale, and carbonate host rock. However, the presence in the pyrite-quartz body of hematite within quartz suggests that, locally, the fluids were less buffered by the host rock. The mineral assemblages of the second mineralization stage are characteristic of high- to intermediate-sulfidation states. High-sulfidation states and oxidizing conditions were achieved and maintained in the cores of the second-stage orebodies, even in those replacing carbonate rocks. The observation that, in places, second-stage mineral assemblages are found in the inner and outer zones is explained in terms of the hydrothermal fluid advancing and waning. Microthermometric data from fluid inclusions in quartz indicate that the different ores of the first mineralization stage formed at similar temperatures and moderate salinities (200 degrees-275 degrees C and 0.2-6.8 wt % NaCl equiv in the pyrite-quartz body; 192 degrees-250 degrees C and 1.1-4.3 wt % NaCl equiv in the pyrrhotite bodies; and 183 degrees-212 degrees C and 3.2-4.0 wt % NaCl equiv in the Zn-Pb ores). These values are similar to those obtained for fluid inclusions in quartz and sphalerite from the second-stage ores (187 degrees-293 degrees C and 0.2-5.2 wt % NaCl equiv in the enargite-pyrite veins: 178 degrees-265 degrees C and 0.2-7.5 wt % NaCl equiv in quartz of carbonate-replacement orebodies; 168 degrees-999 degrees C and 3-11.8 wt % NaCl equiv in sphalerite of carbonate-replacement orebodies; and 245 degrees-261 degrees C and 3.2-7.7 wt % NaCl equiv in quartz from Venencocha). Oxygen and hydrogen isotope compositions oil kaolinite from carbonate-replacement orebodies (delta(18)O = 5.3-11.5%o, delta D = -82 to -114%o) and on alunite from the Venencocha and Santa Rosa areas (delta(18)O = 1.9-6.9%o, delta D = -56 to -73%o). Oxygen isotope compositions of quartz from the first and second stages have 6180 values from 9.1 to 1.7.8 per mil. Calculated fluids in equilibrium with kaolinite have delta(18)O values of 2.0 to 8.2 and delta D values of -69 to -97 per mil; values in equilibrium with alunite are -1.4 to -6.4 and -62 to -79 per mil. Sulfur isotope compositions of sulfides from both stages have a narrow range of delta(34)S values, between -3.7 and +4.2 per mil; values for sulfates from the second stage are between 4.2 and 31.2 per mil. These results define two mixing trends for the ore-forming fluids. The first trend reflects mixing between a moderately saline (similar to 10 wt % NaCl equiv) magmatic end member that had degassed (as indicated by the low delta D values) and meteoric water. The second mixing indicates condensation of magmatic vapor with HCl and SO(2) into meteoric water, which formed alunite. The hydrothermal system at Cerro de Pasco was emplaced at a shallow depth (similar to 500 m) in the epithermal and upper part of a porphyry environment. The similar temperatures and salinities obtained for the first stage and second stages, together with the stable isotope data, indicate that both stages are linked and represent successive stages of epithermal polymetallic mineralization in the upper part of a porphyry system.

On the use of IRMS in forensic science: proposals for a methodological approach

The flourishing number of publications on the use of isotope ratio mass spectrometry (IRMS) in forensicscience denotes the enthusiasm and the attraction generated by this technology. IRMS has demonstratedits potential to distinguish chemically identical compounds coming from different sources. Despite thenumerous applications of IRMS to a wide range of forensic materials, its implementation in a forensicframework is less straightforward than it appears. In addition, each laboratory has developed its ownstrategy of analysis on calibration, sequence design, standards utilisation and data treatment without aclear consensus.Through the experience acquired from research undertaken in different forensic fields, we propose amethodological framework of the whole process using IRMS methods. We emphasize the importance ofconsidering isotopic results as part of a whole approach, when applying this technology to a particularforensic issue. The process is divided into six different steps, which should be considered for a thoughtfuland relevant application. The dissection of this process into fundamental steps, further detailed, enablesa better understanding of the essential, though not exhaustive, factors that have to be considered in orderto obtain results of quality and sufficiently robust to proceed to retrospective analyses or interlaboratorycomparisons.

Seroepidemiology of herpes simplex virus type 1 and 2 in pregnant women in Switzerland: an obstetric clinic based study.

OBJECTIVE: To assess the seroprevalence of herpes simplex virus type 1 (HSV-1) and type 2 (HSV-2) IgG antibodies and the seroincidence of HSV-1 and HSV-2 infections in pregnant women attending the maternity clinic of the University Hospital Lausanne. STUDY DESIGN: Blood samples from 1030 women were taken at the usual pregnancy visit in the first trimester to assess the prevalence rate of IgG antibodies against HSV-1 and HSV-2 using a type-specific assay. A second blood sample was taken 6-8 weeks postpartum from returning women who were seronegative for HSV-2 or HSV-1 to assess the incidence of seroconversion (primary infection). RESULTS: The seroprevalence rates were 79.4% (95% CI: 76.9-81.9) for HSV-1 and 21.2% (18.7-23.7) for HSV-2 in women 14-46 years old. Type-specific serostatus patterns were as follows: 17.3% HSV-1/-2: +/+, 62.1% HSV-1/-2: +/-, 3.9% HSV-1/-2: -/+, 16.7% HSV-1/-2: -/-. Two hundred and sixty five women (59 of the 212 seronegative for HSV-1 (27.8%) and 265 of the 812 seronegative for HSV-2 (32.6%)) returned to the outpatient clinic for the post-delivery check and a second blood sample was obtained. One HSV-1 seroconversion was detected (HSV-1 seroconversion rate 2.4%/100 patient×year (95% CI: 0.06-13.4)) in a patient who had symptoms compatible with primary genital herpes. No HSV-2 seroconversion was detected (HSV-2 seroconversion rate: 0/100 patient×year (97.5% one-sided CI: 0-2)). CONCLUSION: Compared to a previous population-based study, our study results suggest a rise in the prevalence of HSV-2 among pregnant women in Switzerland. The low incidence of seroconversion detected during pregnancy is consistent with the very low reported incidence of neonatal herpes in Switzerland. CONDENSATION: This study in a public hospital in Western Switzerland suggests an increasing prevalence of HSV-2, but a low incidence of primary infections in women of childbearing age.

Dynamiques temporelles dans les relations intragroupe et intergroupes

Ce travail de doctorat analyse les dynamiques qui se développent lorsque des personnes discutent en groupe et doivent prendre position sur des enjeux socio-politiques. Notre modèle prédit que les dynamiques positionnelles, relatives aux opinions exprimées, et les dynamiques relationnelles, relatives aux relations affectives et à l'organisation du groupe, sont constamment en interaction et s'imbriquent différemment selon le moment de vie du groupe. Les hypothèses issues de notre modèle ont été testées au moyen de cinq études conduites sur la base d'un paradigme expérimental en plusieurs phases. Les données relatives aux variables dépendantes (attraction interpersonnelle, identification au groupe, perception de cohésion du groupe, choix d'un représentant du groupe, évolution des positions suite aux interactions) ont été récoltées par questionnaire. Les résultats de ces études appuient l'importance d'analyser conjointement les dynamiques relationnelles et positionnelles, dans une perspective temporelle.

Intervention de la pensée représentative de futurs enseignant-e-s dans leurs prises de position envers l'intégration scolaire

In the past two decades, international recommendations have made inclusive education a priority issue. Many countries have adopted school policies inciting players to question their representations about the duties and purposes of schooling and their role therein. In Switzerland, a new national and cantonal framework defines the integration of students with disabilities or special educational needs in the regular classroom as a priority. However, progress in this area is modest and many researchers are left wondering how teachers could be better prepared to meet the special needs of some students. Initial training is thus seen as essential in bringing pre-service teachers to develop open attitudes toward students with disabilities or special educational needs. While many studies have examined the role of training in building professional attitudes, very few deal with teacher representations of inclusive education, let alone those of future teachers. Our research focuses on two samples of pre-service teachers in the beginning, middle or end of their initial training. 261 pre-service teachers for primary education and 212 pre-service teachers for secondaiy education are involved in the study. The research aims to highlight the role of their representative thinking in building their attitudes towards inclusive education. Our results show that objectification remains essentialist and focuses on the prototypes of the most publicized disabilities. They also showed the weakness of the training system as perceived by future teachers. Even though they have maintained or strengthened positive attitudes towards integration, most leave their training with a reinforced sense of apprehension when faced with the disabilities or special educational needs that they expect to encounter in their future work. Although pre-service teachers consider their training insufficient, it nevertheless positively influences their attitudes toward integration. In particular, greater internship practice, however modest it may be, has a significant effect on attitudes of future teachers by increasing their perception of competence and confidence. -- Ces deux dernières décennies, les recommandations internationales ont fait de l'inclusion scolaire une thématique prioritaire. De nombreux pays ont adopté des politiques scolaires obligeant les acteurs scolaires à interroger leurs représentations des missions de l'école et leur rôle au sein de celle-ci. En Suisse, un nouveau cadre national et cantonal a défini comme prioritaire l'intégration dans l'école ordinaire des élèves en situation de handicap ou ayant des besoins éducatifs particuliers. Or, les avancées en la matière restent modestes et de nombreux chercheurs se questionnent sur la manière dont les enseignant-e-s pourraient être mieux préparés à répondre aux besoins éducatifs particuliers de certains élèves. La formation initiale est ainsi perçue comme essentielle pour amener les futurs enseignant-e-s pour développer des attitudes ouvertes envers les élèves en situation de handicap ou ayant des besoins éducatifs particuliers. Si beaucoup d'études portent sur le rôle de la formation dans la construction d'attitudes professionnelles, très peu traitent des représentations des enseignant-e-s à l'égard de l'intégration scolaire et encore moins de celles des futurs enseignant-e-s. Notre recherche porte sur deux populations de futurs enseignant-e-s en début, au milieu ou en fin de formation. Elles sont composées respectivement de 261 étudiant-e-s se destinant à l'enseignement primaire et de 212 étudiant-e-s se destinant à l'enseignement secondaire. La recherche vise à mettre en évidence l'intervention de leur pensée représentative dans leurs prises de position envers l'intégration scolaire. Nos résultats montrent que l'objectivation reste essentialiste et se focalise sur les prototypes de situations de handicap les plus médiatisés. Nos résultats font également fait apparaître la faiblesse du dispositif de formation tel que perçu les futurs enseignant-e-s. Quand bien même ont-ils conservé ou renforcé des attitudes favorables à l'intégration, ils quittent pour la plupart leur formation avec une appréhension renforcée à l'égard des situations de handicap ou de besoins éducatifs particuliers qu'ils s'attendent à rencontrer dans leur future pratique. Bien que la formation soit jugée insuffisante par les étudiant-e-s, elle oriente néanmoins favorablement leurs prises de position envers l'intégration des élèves concernés. En particulier, une plus grande pratique de stage, si modeste soit-elle, a un effet important sur ces prises de position par l'augmentation du sentiment de compétence et la perception d'assurance des futurs enseignant-e-s.

Subclinical thyroid dysfunction and fracture risk: a meta-analysis.

IMPORTANCE: Associations between subclinical thyroid dysfunction and fractures are unclear and clinical trials are lacking. OBJECTIVE: To assess the association of subclinical thyroid dysfunction with hip, nonspine, spine, or any fractures. DATA SOURCES AND STUDY SELECTION: The databases of MEDLINE and EMBASE (inception to March 26, 2015) were searched without language restrictions for prospective cohort studies with thyroid function data and subsequent fractures. DATA EXTRACTION: Individual participant data were obtained from 13 prospective cohorts in the United States, Europe, Australia, and Japan. Levels of thyroid function were defined as euthyroidism (thyroid-stimulating hormone [TSH], 0.45-4.49 mIU/L), subclinical hyperthyroidism (TSH <0.45 mIU/L), and subclinical hypothyroidism (TSH ≥4.50-19.99 mIU/L) with normal thyroxine concentrations. MAIN OUTCOME AND MEASURES: The primary outcome was hip fracture. Any fractures, nonspine fractures, and clinical spine fractures were secondary outcomes. RESULTS: Among 70,298 participants, 4092 (5.8%) had subclinical hypothyroidism and 2219 (3.2%) had subclinical hyperthyroidism. During 762,401 person-years of follow-up, hip fracture occurred in 2975 participants (4.6%; 12 studies), any fracture in 2528 participants (9.0%; 8 studies), nonspine fracture in 2018 participants (8.4%; 8 studies), and spine fracture in 296 participants (1.3%; 6 studies). In age- and sex-adjusted analyses, the hazard ratio (HR) for subclinical hyperthyroidism vs euthyroidism was 1.36 for hip fracture (95% CI, 1.13-1.64; 146 events in 2082 participants vs 2534 in 56,471); for any fracture, HR was 1.28 (95% CI, 1.06-1.53; 121 events in 888 participants vs 2203 in 25,901); for nonspine fracture, HR was 1.16 (95% CI, 0.95-1.41; 107 events in 946 participants vs 1745 in 21,722); and for spine fracture, HR was 1.51 (95% CI, 0.93-2.45; 17 events in 732 participants vs 255 in 20,328). Lower TSH was associated with higher fracture rates: for TSH of less than 0.10 mIU/L, HR was 1.61 for hip fracture (95% CI, 1.21-2.15; 47 events in 510 participants); for any fracture, HR was 1.98 (95% CI, 1.41-2.78; 44 events in 212 participants); for nonspine fracture, HR was 1.61 (95% CI, 0.96-2.71; 32 events in 185 participants); and for spine fracture, HR was 3.57 (95% CI, 1.88-6.78; 8 events in 162 participants). Risks were similar after adjustment for other fracture risk factors. Endogenous subclinical hyperthyroidism (excluding thyroid medication users) was associated with HRs of 1.52 (95% CI, 1.19-1.93) for hip fracture, 1.42 (95% CI, 1.16-1.74) for any fracture, and 1.74 (95% CI, 1.01-2.99) for spine fracture. No association was found between subclinical hypothyroidism and fracture risk. CONCLUSIONS AND RELEVANCE: Subclinical hyperthyroidism was associated with an increased risk of hip and other fractures, particularly among those with TSH levels of less than 0.10 mIU/L and those with endogenous subclinical hyperthyroidism. Further study is needed to determine whether treating subclinical hyperthyroidism can prevent fractures.