Travail et fragilisation : L'organisation et le travail en question

Fragilisé dans son statut et dans son savoir, constamment exposé à une redéfinition de son travail, l'individu contemporain est de moins en moins en mesure de s'assurer de son identité sociale par une identité professionnelle, alors même que les exigences d'implication de soi dans son emploi sont de plus en plus élevées. Comment, en tant que société, ferons-nous face à ce cocktail explosif : d'une part, une extériorité croissante de l'individu à la mission qu'il remplit en tant qu'elle lui est de plus en plus étrangère; et d'autre part, l'exigence, déterminée par l'impératif de rentabilité, de son engagement total dans la réalisation de son travail dont il sait par ailleurs qu'il peut disparaître du jour au lendemain à la faveur d'une restructuration des processus de travail ou de licenciements économiques? Enorme question dans laquelle se joue, sans doute, une part décisive de notre avenir en tant que société : car si, demain, le travail cesse déjouer le rôle intégrateur qu'il a joué depuis la naissance de l'économie industrielle, qu'est-ce qui fera tenir ensemble les individus-travailleurs que nous sommes devenus ?Au travers d'une pluralité de regards disciplinaires allant de la psychologie du travail aux transformations de l'organisation du travail induites par la ©-entreprise en passant par la médecine du travail, la pédagogie, la sociologie des métiers, les contributions réunies ici explorent les mutations récentes advenues dans le travail - en tant qu'il constitue, aujourd'hui encore, le "fait social total ". Le souci commun en est d'interroger la place que le processus organisationnel le plus récent "ménage" à l'individu. Il en est aussi de sonder les stratégies élaborées par celui-ci pour s'y construire et s'y préserver malgré tout, malgré les casses. Sont ainsi offerts différents regards sur la difficulté de l'individu à se forger une place; à conquérir l'estime de soi et de ses semblables par son apport au procès de la production sociale, aussi incontournable qu'impossible. Le présent volume rassemble la majeure partie des contributions présentées dans le cadre d'un cycle de conférences mis sur pied par le Département interfacultaire d'éthique de l'Université de Lausanne et la Haute école de gestion de Neuchâtel au cours des années académiques 2000-2002.

Travertines and volcanic landforms in the eastern pyrenees margin

Travertines and volcanic landforms in the eastern pyrenees margin

Stratigraphy, sedimentology and depositional environments of the Permian to uppermost Cretaceous Batain Group, eastern-Oman

Permian to Late Cretaceous allochthonous sedimentary and volcanic rocks exposed in the Batain area (eastern Oman Margin) have received comparably little attention in the past. They largely were considered as part of the Hamrat Duru Group (Hawasina Complex) of the northern Oman Mountains. Structural, kinematic and biostratigraphic results from our mapping campaign in the Batain area have now revealed, that emplacement of these units occurred in a WNW direction during latest Cretaceous/Early Paleogene time. This clearly contrasts with previous models that postulated a S-ward directed obduction in Campanian times such as recorded from the Hawasina Complex and Semail Ophiolite in the Oman Mountains. We herewith establish the `'Batain Group'' comprising all Permian to Late Cretaceous allochthonous units in the Batain Area. These are: 1.) the Permian Qarari Formation deposited in the toe of a slope setting; 2.) the Late Permian to late Liassic Al Jil Formation comprising periplatform detritus and very coarse breccias; 3.) the Scythian to Norian Matbat Formation formed by slope deposits; 4.) the Early Jurassic to early Oxfordian Guwayza Formation with high energy platform detritus; 5.) the Mid-Jurassic to earliest Cretaceous Ruwaydah Formation seamount; and 6.) the Oxfordian to Santonian Wahrah Formation, mainly radiolarites; and 7.) the Santonian to latest Maastrichtian Fayah Formation built by flysch-type sediments. These sedimentary and volcanic rocks represent deposits of the former ``Batain basin'' off eastern-Oman, destroyed by compressional tectonics at the Cretaceous/Paleogene transition. For tectono-stratigraphic reasons the Batain Group does not form part of the Hawasina Complex.

Vegetation of Lishkmokh mire in Vodlozersky National Park, eastern Karelian republic, Russia

Tiivistelmä: Karjalan tasavallan Vodlajärven kansallispuistossa sijaitsevan Lishkansuon kasvillisuus

Whose DNA is this? How relevant a question? (a note for forensic scientists).

This communication seeks to draw the attention of researchers and practitioners dealing with forensic DNA profiling analyses to the following question: is a scientist's report, offering support to a hypothesis according to which a particular individual is the source of DNA detected during the analysis of a stain, relevant from the point of view of a Court of Justice? This question relates to skeptical views previously voiced by commentators mainly in the judicial area, but is avoided by a large majority of forensic scientists. Notwithstanding, the pivotal role of this question has recently been evoked during the international conference "The hidden side of DNA profiles. Artifacts, errors and uncertain evidence" held in Rome (April 27th to 28th, 2012). Indeed, despite the fact that this conference brought together some of the world's leading forensic DNA specialists, it appeared clearly that a huge gap still exists between questions lawyers are actually interested in, and the answers that scientists deliver to Courts in written reports or during oral testimony. Participants in the justice system, namely lawyers and jurors on the one hand and forensic geneticists on the other, unfortunately talk considerably different languages. It thus is fundamental to address this issue of communication about results of forensic DNA analyses, and open a dialogue with practicing non-scientists at large who need to make meaningful use of scientific results to approach and help solve judicial cases. This paper intends to emphasize the actuality of this topic and suggest beneficial ways ahead towards a more reasoned use of forensic DNA in criminal proceedings.

New considerations on the management of osteoporosis in Central and Eastern Europe (CEE): summary of the "3rd Summit on Osteoporosis-CEE", November 2009, Budapest, Hungary.

INTRODUCTION: In November 2009, the "3rd Summit on Osteoporosis-Central and Eastern Europe (CEE)" was held in Budapest, Hungary. The conference aimed to tackle issues regarding osteoporosis management in CEE identified during the second CEE summit in 2008 and to agree on approaches that allow most efficient and cost-effective diagnosis and therapy of osteoporosis in CEE countries in the future. DISCUSSION: The following topics were covered: past year experience from FRAX® implementation into local diagnostic algorithms; causes of secondary osteoporosis as a FRAX® risk factor; bone turnover markers to estimate bone loss, fracture risk, or monitor therapies; role of quantitative ultrasound in osteoporosis management; compliance and economical aspects of osteoporosis; and osteoporosis and genetics. Consensus and recommendations developed on these topics are summarised in the present progress report. CONCLUSION: Lectures on up-to-date data of topical interest, the distinct regional provenances of the participants, a special focus on practical aspects, intense mutual exchange of individual experiences, strong interest in cross-border cooperations, as well as the readiness to learn from each other considerably contributed to the establishment of these recommendations. The "4th Summit on Osteoporosis-CEE" held in Prague, Czech Republic, in December 2010 will reveal whether these recommendations prove of value when implemented in the clinical routine or whether further improvements are still required.