Carbon-isotope stratigraphy of the Liesberg Beds Member (Oxfordian, Swiss Jura) using echinoids and crinoids

The Liesberg Beds form the transition between the lower Oxfordian dark coloured marls (Renggeri Member and the Terrain a Chailles Member) and the middle Oxfordian reefal limestones (St-Ursanne Formation). Both lithofacies and biofacies are diverse and evolve rapidly up-section. Stable isotope studies of whole-rock samples are therefore excluded. In search for a convenient isotopic marker, we measured carbon isotope compositions of several fossil groups and chose crinoid stems of Millericrinus spp and echinoid spines of Paracidaris spp because of their abundance throughout the section and the small variations of delta(13)C within one fossil and between fossils from the same stratigraphic level. The delta(13)C values of echinoderms largely reflect earliest diagenetic conditions at the seawatersediment interface. The porous stereome structure secreted of high Mg-calcite by echinoderms has a high reactive surface/volume ratio, which triggers the precipitation of very early syntaxial cements. In the four studied sections reproducible carbon isotope shifts were observed both for Millericrinus spp stems and Paracidaris spp spines. A negative delta(13)C shift of 1-1.5 parts per thousand was observed near the base of the section, just above the transition from Terrain a Chailles Member, where the first corals occur. In the middle and upper part of the four sections, characterised by a stepwise increase of corals and the macrofossils, a positive delta(13)C Shift of about 2 parts per thousand was observed. Despite the highly variable lithologic composition of the Liesberg Beds;Member, carbon isotope shifts seem to be consistent and warrant an interpretation as an original signal, controlled by the isotopic composition of dissolved carbonic acid in seawater. We explain the heavy delta(13)C values (approximate to 2-2.3 parts per thousand) in the lower Liesberg Beds as a transition from an oxygen-limited environment (Terrain a Chailles Member) to the Liesberg Beds Member. The lowest delta(13)C values (approximate to 1-1.5 parts per thousand) correspond to a large input of dissolved nutrients to the platform under oxidizing conditions. The ensuing positive shift (between 2.5 and 3.5 parts per thousand), however, seems to correspond to a general trend of opening up of the platform and connection to open marine waters. Positive delta(13)C values in the upper Liesberg Beds is interpreted as a result of important accelareted extraction of organic carbon from the ocean reservoir, that occurred possibly during periods of warm and humid climate.

Organic geochemistry across the Permian-Triassic transition at the Idrijca Valley, Western Slovenia

Bulk and molecular stable C isotopic compositions and biomarker distributions provide evidence for a diverse community of algal and bacterial organisms in the sedimentary organic matter of a carbonate section throughout the Permian-Triassic (P/Tr) transition at the Idrijca Valley, Western Slovenia. The input of algae and bacteria in all the Upper Permian and Lower Scythian samples is represented by the predominance of C-15-C-22 n-alkanes, odd C-number alkylcyclohexanes, C-27 steranes and substantial contents Of C-21-C-30 acyclic isoprenoids. The occurrence of odd long-chain n-alkanes (C-22-C-30) and C29 steranes in all the samples indicate a contribution of continental material. The decrease of C-org and C-carb contents, increase of Rock-Eval oxygen indices, and C-13-enrichment of the kerogen suggest a decrease in anoxia of the uppermost Permian bottom water. The predominance of odd C-number alkylcycloalkanes, C-27 steranes, and C-17 n-alkanes with delta(13)C values similar to-30parts per thousand, and C-13-enrichment of the kerogens in the lowermost Scythian samples are evidence of greater algal productivity. This increased productivity was probably sustained by a high nutrient availability and changes of dissolved CO2 speciation associated to the earliest Triassic transgression. A decrease Of Corg content in the uppermost Scythian samples, associated to a C-13-depletetion in the carbonates (up to 4parts per thousand) and individual n-alkanes (up to 3.4parts per thousand) compared to the Upper Permian samples, indicate lowering of the primary productivity (algae, cyanobacteria) and/or higher degradation of the organic matter. (C) 2003 Elsevier Ltd. All rights reserved.

Aortic biological valve prosthesis in patients younger than 65 years of age: transition to a flexible age limit?

OBJECTIVES Guidelines proposed bioprosthesis implantation for aortic valve disease if the patients were at least 65 years old at the time of surgery, with a trend towards even younger patients in recent years. Considering the adverse effects of lifetime anticoagulation, new biological valves (less prone to degeneration) and new technologies may lead patients and surgeons to different choices. Therefore, it is interesting to analyse the results of aortic bioprosthetic valve replacement in patients aged <65 years at the time of surgery. METHODS From January 2000 to December 2010, 84 patients aged <65 years at the time of surgery had undergone an aortic bio-prosthetic valve replacement. A mid-term follow-up [(FU) mean FU time: 54.4 ± 39.2 months] was done in August 2011 in all patients (FU completeness: 100%). Results were compared with patients who had a mechanical prosthetic aortic valve replacement during the same period. RESULTS The reoperation rate for structural valve degeneration (SVD) of bioprostheses was 6% and occurred exclusively among patients <56 years. Contraindications for anticoagulation determined the choice of a bioprosthesis among 83% of these patients. The personal preference to avoid anticoagulation was the leading cause in 68% of the older patients (56-65 years). Neurological complications occurred more frequently in the mechanical control group. CONCLUSIONS Reoperations for SVD after bioprosthesis implantation occurred exclusively among younger patients (<56 years), not suitable for systemic anticoagulation. Previous studies, together with our experience, are in favour of an age limit between 56 and 60 years, taking into consideration alternative transcatheter approaches to SVD treatment.

Cenomanian-Turonian transition in a shallow water sequence of the Sinai, Egypt

Environmental and depositional changes across the Late Cenomanian oceanic anoxic event (OAE2) in the Sinai, Egypt, are examined based on biostratigraphy, mineralogy, delta(13)C values and phosphorus analyses. Comparison with the Pueblo, Colorado, stratotype section reveals the Whadi El Ghaib section as stratigraphically complete across the late Cenomanian-early Turonian. Foraminifera are dominated by high-stress planktic and benthic assemblages characterized by low diversity, low-oxygen and low-salinity tolerant species, which mark shallow-water oceanic dysoxic conditions during OAE2. Oyster biostromes suggest deposition occurred in less than 50 m depths in low-oxygen, brackish, and nutrient-rich waters. Their demise prior to the peak delta(13)C excursion is likely due to a rising sea-level. Characteristic OAE2 anoxic conditions reached this coastal region only at the end of the delta(13)C plateau in deeper waters near the end of the Cenomanian. Increased phosphorus accumulations before and after the delta(13)C excursion suggest higher oxic conditions and increased detrital input. Bulk-rock and clay mineralogy indicate humid climate conditions, increased continental runoff and a rising sea up to the first delta(13)C peak. Above this interval, a dryer and seasonally well-contrasted climate with intermittently dry conditions prevailed. These results reveal the globally synchronous delta(13)C shift, but delayed effects of OAE2 dependent on water depth.

Challenge of transition in the socio-professional insertion of youngsters with neurodisabilities.

Objective: To evaluate the activities of patients with neurodisabilities and assess their insertion problems in the professional world. Methods: It is based on medical records of 267 patients (224 with neurodevelopmental diseases and 43 with neuromuscular diseases), aged 16-25 years, followed in the transition clinic of young adults in the neurorehabilitation services of a tertiary center. Results: Nearly half of them (46.8%) were in a protected environment, 37.08% studied and only 3.4% worked. Their studies are much longer and they are less in university than Swiss people of same age. The competitiveness criteria are no mental retardation and to be completely independent. Finally, 29.2% reported work problems, the foremost being the lack of adaptation in the workplace. Conclusion: These results highlight the need to increase the integration of young adults with neuromotor disorders in the labor market.

Epithelial-to-mesenchymal transition mediates docetaxel resistance and high risk of relapse in prostate cancer

Molecular characterization of radical prostatectomy specimens after systemic therapy may identify a gene expression profile for resistance to therapy. This study assessed tumor cells from patients with prostate cancer participating in a phase II neoadjuvant docetaxel and androgen deprivation trial to identify mediators of resistance. Transcriptional level of 93 genes from a docetaxel-resistant prostate cancer cell lines microarray study was analyzed by TaqMan low-density arrays in tumors from patients with high-risk localized prostate cancer (36 surgically treated, 28 with neoadjuvant docetaxel þ androgen deprivation). Gene expression was compared between groups and correlated with clinical outcome. VIM, AR and RELA were validated by immunohistochemistry. CD44 and ZEB1 expression was tested by immunofluorescence in cells and tumor samples. Parental and docetaxel-resistant castration-resistant prostate cancer cell lines were tested for epithelial-to-mesenchymal transition (EMT) markers before and after docetaxel exposure. Reversion of EMT phenotype was investigated as a docetaxel resistance reversion strategy. Expression of 63 (67.7%) genes differed between groups (P < 0.05), including genes related to androgen receptor, NF-k B transcription factor, and EMT. Increased expression of EMT markers correlated with radiologic relapse. Docetaxel-resistant cells had increased EMT and stem-like cell markers expression. ZEB1 siRNA transfection reverted docetaxel resistance and reduced CD44 expression in DU-145R and PC-3R. Before docetaxel exposure, a selected CD44 þ subpopulation of PC-3 cells exhibited EMT phenotype and intrinsic docetaxel resistance; ZEB1/CD44 þ subpopulations were found in tumor cell lines and primary tumors; this correlated with aggressive clinical behavior. This study identifies genes potentially related to chemotherapy resistance and supports evi-dence of the EMT role in docetaxel resistance and adverse clinical behavior in early prostate cancer.

Continent wide response of mountain vegetation to climate change

Climate impact studies have indicated ecological fingerprints of recent global warming across a wide range of habitats. Whereas these studies have shown responses from various local case studies, a coherent large-scale account on temperature-driven changes of biotic communities has been lacking. Here we use 867 vegetation samples above the treeline from 60 summit sites in all major European mountain systems to show that ongoing climate change gradually transforms mountain plant communities. We provide evidence that the more cold-adapted species decline and the more warm-adapted species increase, a process described here as thermophilisation. At the scale of individual mountains this general trend may not be apparent, but at the¦larger, continental scale we observed a significantly higher abundance of thermophilic species in 2008, compared with 2001. Thermophilisation of mountain plant communities mirrors the degree of recent warming and is more pronounced in areas where the temperature increase has been higher. In view of the projected climate change the observed transformation suggests a progressive decline of cold mountain habitats and their biota.

Russian transition in the early 21st century

Tässä tutkimuksessa käsitellään Venäjän talouden kehitystä uudella vuosituhannella. Kylmän sodan aikaan Neuvostoliitto oli suurvalta, jonka asema perustui sotilasmahtiin. Sotateollisuuden konversio palvelemaan nykytarpeita ei ole ollut helppo tehtävä. Vuoden 1998 talouskriisin jälkeen elintaso on toipunut verraten nopeasti, mikä on nähtävissä tarkastellessa kotitalouksien kulutusrakenteita, joita käsitellään tarkemmin luvussa 2. Siirtymätalouksissa vaihtotaseen vajeet ovat yleisiä, mutta luonnonrikkauksiensa ansiosta Venäjän vaihtotaseet ovat olleet huomattavan ylijäämäisiä, mitä pohditaan luvussa 3. Vaihtotaseen ylijäämien heijatusvaikutus on ollut Venäjän rooli pääomien nettoviejänä. Venäjän investointikertymä onedelleen erittäin vaatimaton suhteutettuna maan kehitysvaiheeseen. Jokaisessa menestyksekkäässä taloudessa investoinnit ovat pitkän aikavälintaloudellisen menestyksen avaintekijä. Venäjän erityispiirteitä tähän liittyen on kuvattu luvussa 4. Raportti päättyy talouden nykytilanteen analyysiin (luvut 5 ja 6).

Etude systématique, cladistique et biogéographique des Baetidae (Ephemeroptera) de Madagascar

Les Ephéméroptères constituent un ordre très archaïque d?insectes ailés, comprenant un nombre réduit d?espèces (actuellement environ 2500 espèces). Les larves sont aquatiques; la durée de ce stade est en général d?une année. Le stade adulte est par contre extrêmement bref: de quelques heures à quelques jours. La fonction quasi unique de ce stade est la reproduction. Par sa superficie, Madagascar est la quatrième île du monde. Elle est située dans la partie occidentale de l?Océan Indien à plus de 300 km de la côte africaine. Madagascar faisait partie du super-continent Gondwana. Elle s?est séparée de l?Afrique (-165 M.a.), puis a migré vers le Sud (-125 M.a.) avant de se détacher du sous-continent indien (-65 M.a.). La connaissance des Ephéméroptères malgaches était, jusqu?à très récemment, extrêmement limitée. Grâce au programme Biodiversité et biotypologie des eaux continentales malgaches, lancé conjointement par l?ORSTOM (actuel IRD, France) et le CNRE (Madagascar), un inventaire à large échelle de la macrofaune benthique malgache a été entrepris. La systématique de plusieurs familles d?Ephéméroptères (Tricorythidae, Polymitarcyidae, Palingeniidae,?), ainsi que d?autres groupes d?invertébrés (Trichoptères, Simuliidae, macrocrustacés) a fait l?objet d?études approfondies. La présente étude consistue un des volets de ce programme. Jusqu?au milieu des années 1990, seules quatre espèces valides appartenant à trois genres différents étaient décrites de Madagascar. En 6 ans, ce ne sont pas moins de 25 articles qui sont consacrés à la systématique des Baetidae, permettant de décrire 50 espèces et 8 genres nouveaux. La faune malgache des Baetidae compte actuellement 22 genres et 54 espèces. Malgré sa taille, Madagascar possède une richesse, tant générique que spécifique équivalente à celle d?un continent. Notre connaissance des Baetidae est suffisamment avancée pour mener une étude cladistique et biogéographique. La reconstruction phylogénétique a permis de mettre en évidence cinq lignées principales à Madagascar et de préciser, pour chacune d?elles, les genres inclus et les caractères propres. La faune des Baetidae malgaches présente un taux d?endémicité très élevé: 53 des 54 espèces et un tiers des genres sont endémiques. Elle montre des affinités extrêmement fortes avec la faune africaine, puisque 90% des genres présents à Madagascar ou en Afrique ont une répartition strictement restreinte à cette région. Les autres composantes, notamment orientales et océaniennes, sont négligeables; ces régions n?ont en commun avec Madagascar qu?un nombre restreint de genres cosmopolites. Ces affinités sont en contradiction avec les données géologiques de la dislocation du Gondwana. Plusieurs explications peuvent être données pour résoudre cette contradiction. La plus vraisemblable est que le pouvoir de dispersion des Ephéméroptères, et des Baetidae en particulier, est nettement sous-estimé. L?étude des faunes des îles volcaniques récentes, telles que les Comores, démontre clairement que les Baetidae sont capables de dispersion sur une distance de plus de 300 km. Il est donc possible d?envisager une colonisation de Madagascar à partir de l?Afrique continentale postérieure à la séparation des deux plaques. Nous avons établi des scénarios retraçant l?histoire biogéographique de chacune des cinq lignées. Pour quatre d?entre elles, l?Afrique continentale est le centre d?origine. La cinquième lignée aurait une origine paléarctique; l?Afrique représenterait un centre secondaire de spéciation. Ces lignées auraient secondairement colonisé Madagascar à partir de l?Afrique continentale. Ce travail ouvre donc d?importantes perspectives. Il rend possible l?utilisation à un niveau générique, voire spécifique, des Baetidae pour des travaux de faunistique ou d?écologie, en particulier pour des études liées à la dégradation de la qualité de l?eau. Il devrait également pouvoir servir de base pour l?étude et la compréhension des phénomènes de dispersion et colonisation dans les îles et archipels de l?Ouest de l?Océan Indien.<br/><br/>Mayflies (Ephemeroptera) are among the oldest known flying insects and encompass a very small number of species (ca 2500 species). Larvae are strictly freshwater inhabitants; this stage lasts generally one year. The imaginal stage is extremely short, from few hours to few days, and is devoted almost entirely to reproduction. Madagascar is the fourth largest island in the world by area. It is situated in the western part of the Indian Ocean, at a distance of more than 300 km from the African coast. Madagascar belonged to Gondwana. It was first separated from the African plate (-165 M.y.), then moved to the South (-65 M.y.), before the break-off with the Indian plate (-65 M.y.). Knowledge of the Malagasy mayflies was until recently extremely poor. The program Biodiversity and Biotypology of Malagasy Freshwaters, jointly run by the French ORSTOM and the Malagasy CNRE, began a global survey of the freshwater macroinvertebrates. The systematics of several mayfly families (Tricorythidae, Polymitarcyidae, Palingeniidae,?), and other invertebrate groups (Caddisflies, Blackflies,?) was the subject of ground studies. Our present study is one part of this global program. Until the middle of the nineties, only four baetid species belonging to three different genera had been described from Madagascar. During the last six years, 25 papers were dedicated to the systematics of the Baetidae, allowing the description of 50 new species and 8 new genera. The Malagasy fauna encompasses now 22 genera and 54 species. Despite its size, Madagascar has the same diversity, at specific and generic level, as a continent. Our knowledge of the Baetidae is sufficient to perform a cladistic and biogeographical study. Our phylogenetic reconstruction allows us to propose five main lineages and to indicate, for each of them, the genera included and their features. The Malagasy fauna of Baetidae possesses a high level of endemicity: 53 of the 54 species and one third of the genera are endemic. It shows extremely strong affinities with the African fauna, as more than 90% of the genera present in Madagascar or in Africa have a distribution restricted to this area. Other components, especially Oriental and Oceanian, are negligible. These areas share with Madagascar only a few widespread genera. These African affinities are in contradiction with the geological events, especially the break-off history of Gondwana. Some explanations can be given to solve this contradiction. The most likely is that the dispersal power of the mayflies, especially of the Baetidae, is greatly underestimated. The study of recent volcanic islands, particularly of the Comoros, clearly demonstrates that the Baetidae are able to disperse over more than 300 km. Consequently, a colonisation by the Baetidae, of Madagascar from the continental Africa, after the break-off must be considered as possible. We have established scenarios explaining the biogeographical history of each of the five lineages. For four of them, Africa has to be regarded as the centre of origin. The fifth lineage probably has a Palearctic origin; Africa should be considered as a secondary centre of speciation. These lineages should have secondarily colonised Madagascar from continental Africa. This work opens up new perspectives. It allows the use of the Baetidae for faunistic and ecological studies, especially for problems related to water quality. It must be also considered as a first step for understanding the dispersion and colonisation of the islands of the western part of the Indian Ocean.

Financial convergence in transition economies: EU enlargement

This paper analyses the financial impact of the enlargement of the European Union (EU) to include 10 new Central and Eastern European Nations (CEEN) on firms’ business and financial structures. To this end, we employ quantitative analytic techniques and financial ratios. In this context, we hope to discover whether firms in the new EU member States tend to converge with business in the Europe of the 15 in terms of the structure of firms’ financial statements. We examine the extent to which the increasing integration of the former may foster the convergence of productive structures. The methodology followed consists of an analysis of the evolution of 12 financial ratios in a sample of firms obtained from the AMADEUS data base. To that end, we perform a Dynamic Factor Analysis that identifies the determining factors of the joint evolution of deviations in the financial ratios with respect to the average value of firms in the EU-15. This analysis allows us to analyse the convergence in each of the CEEN nations with respect to the EU-15.