Evaluation des technologies médicales : travaux présentés pendant le Congrès TEKMED 87 = Assessment of medical technologies : the papers presented during the TEKMED 87 Congress

[Table des matières] Technology assessment in health care in the United States: an historical review / S. Perry. - The aims and methods of technology assessment / JH Glasser. - Evaluation des technologies de la santé / A. Griffiths. - Les données nécessaires pour l'évaluation des technologies médicales / R. Chrzanowski, F. Gutzwiller, F. Paccaud. - Economic issues in technology assessment/DR Lairson, JM Swint. - Two decades of experience in technology assessment: evaluating the safety, performance, and cost effectiveness of medical equipment / JJ Nobel. - Demography and technology assessment / H. Hansluwka. - Méthodes expérimentale et non expérimentale pour l'évaluation des innovations technologiques / R. Chrzanowski, F. Paccaud. - Skull radiography in head trauma: a successful case of technology assessment / NT Racoveanu. - Complications associées à l'anesthésie: une étude prospective en France / L. Tiret et al. - Impact de l'information publique sur les taux opératoires: le cas de l'hystérectomie / G. Domenighetti, P. Luraschi, A. Casabianca. - The clinical effectiveness of acupuncture for the relief of chronic pain / MS Patel, F. Gutzwiller, F. Paccaud, A. Marazzi. - Soins à domicile et hébergement à long terme: à la recherche d'un développement optimum / G. Tinturier. - Economic evaluation of six scenarios for the treatment of stones in the kidney and ureter by surgery or ESWL / MS Patel et al. - Technology assessment and medical practice / F. Gutzwiller. - Technology assessment and health policy / SJ Reiser. - Global programme on appropriate technology for health, its role and place within WHO / K. Staehr Johansen.

Climatic and anthropogenic influence on the stable isotope record from bulk carbonates and ostracodes in Lake Neuchatel, Switzerland, during the last two millennia

Lake Neuchatel is a medium sized, hard-water lake, lacking varved sediments, situated in the western Swiss Lowlands at the foot of the Jura Mountains. Stable isotope data (delta(18)O and delta(13)C) from both bulk carbonate and ostracode calcite in an 81 cm long, radiocarbon-dated sediment core represent the last 1500 years of Lake Neuchatel's environmental history. Comparison between this isotopic and other palaeolimnologic data (mineralogical, geochemical, palynological, etc.) helps to differentiate between anthropogenic and natural factors most recently affecting the lake. An increase in lacustrine productivity (450-650AD ca), inferred from the positive trend in delta(13)C values of bulk carbonate, is related to medieval forest clearances and the associated nutrient budget changes. A negative trend in both the bulk carbonate and ostracode calcite delta(18)O values between approximately 1300 and 1500AD, is tentatively interpreted as due to a cooling in mean air temperature at the transition from the Medieval Warm Period to the Little Ice Age. Negative trends in bulk carbonate delta(18)O and delta(13)C values through the uppermost sediments, which have no equivalent in ostracode calcite isotopic values, are concomitant with the recent onset of eutrophication in the lake. Isotopic disequilibrium during calcite precipitation, probably due to kinetic factors in periods of high productivity is postulated as the mechanism to explain the associated negative isotopic trends, although the effect of a shift of the calcite precipitation towards the warmer months cannot be excluded.

Climate and sea-level variations along the northwestern Tethyan margin during the Valanginian C-isotope excursion: Mineralogical evidence from the Vocontian Basin (SE France)

A high resolution mineralogical study (bulk-rock and clay-fraction) was carried out upon the hemipelagic strata of the Angles section (Vocontian Basin, SE France) in which the Valanginian positive C-isotope excursion occurs. To investigate sea-level fluctuations and climate change respectively, a Detrital Index (DI: (phyllosilicates and quartz)/calcite) and a Weathering Index (WI: kaolinite/(illite + chlorite)) were established and compared to second-order sea-level fluctuations. In addition, the mineralogical data were compared with the High Nutrient Index (HNI, based on calcareous nannofossil taxa) data obtained by Duchamp-Alphonse et al. (2007), in order to assess the link between the hydrolysis conditions recorded on the surrounding continents and the trophic conditions inferred for the Vocontian Basin. It appears that the mineralogical distribution along the northwestern Tethyan margin is mainly influenced by sea-level changes during the Early Valanginian (Pertransiens to Stephanophorus ammonite Zones) and by climate variations from the late Early Valanginian to the base of the Hauterivian (top of the Stephanophorus to the Radiatus ammonite Zones). The sea-level fall observed in the Pertransiens ammonite Zone (Early Valanginian) is well expressed by an increase in detrital inputs (an increase in the DI) associated with a more proximal source and a shallower marine environment, whereas the sea-level rise recorded in the Stephanophorus ammonite Zone corresponds to a decrease in detrital influx (a decrease in the DI) as the source becomes more distal and the environment deeper. Interpretation of both DI and WI, indicates that the positive C-isotope excursion (top of the Stephanophorus to the Verrucosum ammonite Zones) is associated with an increase of detrital inputs under a stable, warm and humid climate, probably related to greenhouse conditions, the strongest hydrolysis conditions being reached at the maximum of the positive C-isotope excursion. From the Verrucosum ammonite Zone to the base of the Hauterivian (Radiatus ammonite Zone) climatic conditions evolved from weak hydrolysis conditions and, most likely, a cooler climate (resulting in a decrease in detrital inputs) to a seasonal climate in which more humid seasons alternated with more arid ones. The comparison of the WI to the HNI shows that the nutrification recorded al: the Angles section from the top of the Stephanophorus to the Radiatus ammonite Zones (including the positive C-isotope shift), is associated with climatic changes in the source areas. At that time, increased nutrient inputs were generally triggered by increased weathering processes in the source areas due to acceleration in the hydrological cycle under greenhouse conditions This scenario accords with the widely questioned palaeoenvironmental model proposed by Lini et al., (1992) and suggests that increasing greenhouse conditions are the main factor that drove the palaeoenvironmental changes observed in the hemipelagic realm of the Vocontian Basin, during the Valanginian positive C-isotope shift. This high-resolution mineralogical study highlights short-term climatic changes during the Valanginian, probably associated to rapid changes in the C-cycle. Coeval Massive Parana-Etendeka flood basalt eruptions may explain such rapid perturbations. (C) 2011 Elsevier B.V. All rights reserved.

A prospective observational safety study on MF59(®) adjuvanted cell culture-derived vaccine, Celtura(®) during the A/H1N1 (2009) influenza pandemic.

BACKGROUND: The present study was a prospective observational study to evaluate the safety profile of Celtura(®), a monovalent, cell culture-derived, inactivated subunit influenza vaccine prepared from A/California/07/2009(H1N1) with the adjuvant MF59(®). Subjects were enrolled prospectively during the H1N1 2009 influenza pandemic at medical centres in Colombia, Chile, Switzerland, and Germany during the period December 2009 to June 2010. METHODS: Subjects ages 18 and older were followed for the occurrence of adverse events (AEs) for six months after vaccination. Adverse events of special interest (AESIs) were neuritis, convulsion (seizure), anaphylaxis, encephalitis, vasculitis, Guillain-Barre syndrome, demyelinating conditions, Bell's palsy, and laboratory-confirmed vaccination failure. RESULTS: Overall, 7348 AEs were reported in 2296 of 3989 enrolled subjects (57.6%). Only two AEs were considered related to injection site reactions. No laboratory-confirmed cases of influenza were reported. There were 108 medically confirmed serious adverse events (SAEs) reported among 73 subjects with 6 such SAEs described as possibly or probably related to vaccination. Three fatal cases were reported and assessed as not related to vaccination. Two AESIs classified as convulsion were reported and assessed as not related to vaccination. Both AESIs occurred well outside the pre-specified 7 day risk window representing the likely timeframe of the occurrence of seizure following vaccination. CONCLUSIONS: The results of this study support the overall good safety profile of MF59 adjuvanted cell culture-derived influenza vaccine as administered in adults during the 2009-2010 H1N1 influenza pandemic. No concern is raised regarding the occurrence of AESIs.

Association between growth and blood pressure during the life course in children and adolescents

Background: Little is known on the relative importance of growth at different periods between birth and adolescence on blood pressure (BP). Objective: To assess the association between birth weight, change in body weight (growth) and BP across the entire span of childhood and adolescence. Methods: School-based surveys were conducted annually between 1998 and 2006 among all children in four school grades (kindergarten, 4th, 7th, and 10th year of compulsory school) in the Seychelles, Indian Ocean. Height and weight and BP were measured. Three cohorts of children examined twice were analyzed: 1606 children surveyed at age 5.5 and 9.1, 2557 at age 9.2 and 12.5, and 2065 at age 12.5 and 15.5, respectively. Weights at birth and at one year were extracted from medical files. Weights were expressed as Z-scores and growth was defined as a change in weight Z-scores (corresponding to weight centile crossing). The association between BP (at age 5.5, 9.2, 12.5, and 15.5) and weight at different times was assessed by linear regression. Using results of regression models of BP on all successive weights, life course plots were drawn by plotting regression coefficients against age at which weight was measured. The figure shows a life course plot of systolic BP in boys aged 15.5. Results: Without adjustment for current weight (at the time of BP measurement), birth weight was not associated with current BP, irrespective of age, excepted for girls at age 15.5 for whom a modest positive association was found. When adjusted for current weight, birth weight was negatively and modestly associated with current BP. BP was strongly associated with current weight, irrespective of age. Life course plots showed that BP was strongly associated with growth during the few preceding years but not with growth during earlier years, except for growth during the first year of life which tended to be associated with systolic BP. Conclusions: Our findings suggest that BP during childhood and adolescence is mainly determined by current body weight and recent growth.

Information and risk management during the first trimester care for pregnant women: Some reflections about the ethical challenges and the legal framework in Switzerland. [L'information et la gestion des risques dans le suivi de la grossesse lors du 1er trimestre : quelques réflexions sur le défi éthique et le cadre légal en Suisse.]

The progress in prenatal medicine raises complex questions with respect to the physician-patient relationship. The physician needs to reconcile medical aspects, ethical principles as well as judicial norms. Already, during the first trimester, the physician has to put into practice the schedule combining for each individual pregnancy physical, laboratory and other appropriate exams. Physicians are under the obligation to inform in a clear and comprehensive way without creating unnecessary anxiety for their patients. Legal requirements include informed consent, the respect for the patient's right to self-determination, and compliance with the Swiss federal law on genetic testing, especially with its articles on prenatal screening and diagnosis. This article discusses the complexity of obstetrical practice when it comes to delivering adequate information within the scope of ethical and legal requirements in Switzerland. L'évolution de la médecine prénatale soulève des enjeux complexes dans la relation médecin-patient. Il s'agit de concilier à la fois les aspects médicaux, les principes éthiques et les normes juridiques. Dès le premier trimestre de la grossesse le médecin doit poser le cadre du suivi et des examens appropriés pour chaque grossesse. Son devoir est d'informer de manière claire et précise sans inquiéter inutilement, en respectant l'exigence légale d'un consentement éclairé et plus largement le droit de la patiente à l'autodétermination ainsi que le cadre de la loi fédérale suisse sur l'analyse génétique humaine dans le domaine du dépistage et du diagnostic prénatal. Cet article discute de la complexité de l'information et de l'application des principes éthiques et légaux dans la pratique obstétricale en Suisse.

Sea-level changes and ammonite faunal turnover during the Lias/Dogger transition in the western Tethys

The aim of this paper was to investigate the possible connections between ammonite faunal turnover and the eustatic events recorded in Tethyan sequences during the middle Toarcian/early Bajocian time interval. For this we have analysed the biostratigraphic ranges, at the subzone level, of approximately 600 ammonite species belonging to 160 genera from several selected sections of the western Tethys (Mediterranean and Submediterranean provinces). The analysis of taxon ranges enabled us to plot curves for ammonite faunal turnovers, inter-subzonal distance, and diversity. Comparing the mentioned curves with Tethyan sequences [Hardenbol et al., 19981, we find that sea-level changes correlate well with origination and extinction events and faunal diversity. Most of the faunal turnovers correlate with stratigraphic events. Extinction events with their corresponding decrease in diversity correlate with regressive intervals and with major or minor sequence boundaries. Origination events and their corresponding increase in diversity were clearly connected with transgressions in Tethyan sequences. In several cases, the major sequence boundary and the subsequent transgressive phase correlate with major ammonite faunal turnover, whereas minor or medium sequence boundaries generally gave rise to minor or medium turnovers.

Energy metabolism during the postexercise recovery in man.

In order to explore the magnitude and duration of the long-term residual effect of physical exercise, a mixed meal (55% CHO, 27% fat and 18% protein) was given to 10 young male volunteers on two occasions: after a 4-h resting period, and on the next day, 30 min after completion of a 3-h exercise at 50% VO2max. Energy expenditure and substrate utilization were determined by indirect calorimetry for 17 h after meal ingestion. The fuel mix oxidized after the meal was characterized by a greater contribution of lipid oxidation to total energy expenditure when the meal was ingested during the post-exercise period as compared with the meal ingested without previous exercise. During the night following the exercise, the stimulation of energy expenditure observed during the early recovery period gradually faded out. However, resting energy expenditure measured the next morning was significantly higher (+4.7%) than that measured without previous exercise. It is concluded that intense exercise stimulates both energy expenditure and lipid oxidation for a prolonged period.

The fixation of metacentric chromosomes during the chromosomal evolution in the common shrew (Sorex araneus, Insectivora)

Rb fusions between acrocentric chromosomes leading to metacentrics tend to become fixed during the chromosomal evolution in the common shrew. Using microsatellite markers preliminary results show that populations are only slightly subdivided and genetic drift seems not to play an important role for the fixation of metacentrics. A significant segregation distortion in favour of metacentric chromosomes was found during male meiosis. This suggests that cytological factors such as facilitated fusion between acrocentric chromosomes or choice-effects at the level of gametes are more likely to play a role for the chromosomal evolution in the common shrew.

Histone H1 expression varies during the Leishmania major life cycle.

The deduced amino acid sequence of Leishmania major sw3 cDNA reveals the presence of characteristic histone H1 amino acid motifs. However, the open reading frame is of an unusually small size for histone H1 (105 amino acids) because it lacks the coding potential for the central hydrophobic globular domain of linker histones present in other eukaryotes. Here, we provide biochemical evidence that the SW3 protein is indeed a L. major nuclear histone H1, and that it is differentially expressed during the life cycle of the parasite. Due to its high lysine content, the SW3 protein can be purified to a high degree from L. major nuclear lysates with 5% perchloric acid, a histone H1 preparative method. Using an anti-SW3 antibody, this protein is detected as a 17 kDa or as a 17/19 kDa doublet in the nuclear subfraction in different L. major strains. The nuclear localization of the SW3 protein is further supported by immunofluorescence studies. During in vitro promastigote growth, both the sw3 cytoplasmic mRNA and its protein progressively accumulate within parasites from early log phase to stationary phase. Within amastigotes, the high level of H1 expression is maintained but decreases when amastigotes differentiate into promastigotes. Together, these observations suggest that the different levels of this histone H1 protein could influence the varying degrees of chromatin condensation during the life-cycle of the parasite, and provide us with tools to study this mechanism.

Regulation of the activity of DnaA and its role during the cell cycle of caulobacter crescentus

The initiation of chromosomal replication must be tightly regulated so that the genome is replicated only once per cell cycle. In most bacteria, DnaA binds to the origin of replication and initiates chromosomal replication. DnaA is a dual-function protein that also acts as an important transcription factor that regulates the expression of many genes in bacteria. Thus, understanding how this protein is regulated during the bacterial cell cycle is of major importance. The α-proteobacterium Caulobacter crescentus is an excellent model to study the bacterial cell cycle, mainly because it is possible to isolate synchronized cell cultures and because it initiates the replication of its chromosome once per cell cycle and at a specific time of the cell cycle. This latest feature is of special interest for the major aim of my thesis work, which focused on the temporal and spatial regulation of the activity of the essential DnaA protein in C. crescentus. In Escherichia coli, the Hda protein converts ATP-DnaA into ADP- DnaA by stimulating the ATPase activity of DnaA, to prevent over-initiation of chromosome replication. We propose that there exists a similar mechanism in C. crescentus, which is not only involved in the temporal control of chromosome replication, but also in the control of gene expression. First, we provided evidences indicating that the hydrolysis of the ATP bound to DnaA is essential for the viability of C. crescentus. Our results suggest that ATP-DnaA promotes the initiation of chromosome replication, since we found that cells over-expressing a DnaA protein with a mutated ATPase domain, DnaA(R357A), over-initiated chromosome replication, unlike cells expressing the wild-type DnaA protein at similar levels. By contrast, the DnaA(R357A) protein was less active than DnaA in promoting the transcription of three essential genes, suggesting that these may be more efficiently activated by ADP-DnaA than ATP-DnaA. We propose that the ATP-DnaA to ADP-DnaA switch down-regulates the initiation of DNA replication while activating the transcription of several essential genes involved in subsequent cell cycle events. Second, we studied the role of the HdaA protein, homologous to Hda, in promoting the ATP- DnaA to ADP-DnaA switch in C. crescentus. HdaA is essential for viability and its depletion in the cell leads to an over-replication of the chromosome, indicating that HdaA is a negative regulator of DNA replication. HdaA dynamically co-localizes with the replisome. In this work, we identified DnaN, the β-clamp of the DNA polymerase, as the replisome component that interacts directly with HdaA and that recruits HdaA to the replisome in live C. crescentus cells. We also showed that a mutant HdaA protein that cannot interact or co-localize with DnaN is not functional, indicating that HdaA is probably activated by DnaN. However, we found that another non-functional HdaA protein, mutated in the conserved Arginine finger of its AAA+ domain, was able to localize at the replisome, suggesting that the AAA+ domain of HdaA exerts its essential function after the recruitment of HdaA to the replisome. We propose that HdaA stimulates the ATPase activity of DnaA once DNA replication is ongoing, via its interaction with DnaN and the activity of the two conserved R fingers of DnaA and HdaA. Finally, we created different strains in which HdaA, DnaN or DnaA were over-produced. We observed that the over-production of HdaA seems to lead to a delay in chromosome replication, while the over-production of DnaN had an opposite effect. Our results also indicate that the over-production of DnaA may intensify the over-initiation phenotype of cells depleted for HdaA. We conclude that the dynamic interplay of HdaA and DnaN in the cell contributes to regulating the ATP-DnaA/ADP-DnaA ratio in the cell, to ensure once per cell cycle initiation of chromosomal replication in C. crescentus. Altogether, our work provided important information on the regulation of the activity of DnaA in C. crescentus. Since DnaA, HdaA and DnaN are well-conserved proteins, most of our findings are useful to understand how chromosome replication and gene expression are controlled by DnaA in many other bacterial species. - L'initiation de la réplication des chromosomes doit être précisément régulée de telle sorte que le génome ne soit répliqué qu'une seule fois par cycle cellulaire. Chez la plupart des bactéries, DnaA se lie à l'origine de réplication du chromosome et en initie sa réplication. DnaA est aussi un facteur de transcription qui régule l'expression de nombreux gènes bactériens. De ce fait, il est très important de comprendre comment DnaA est régulée au cours du cycle cellulaire bactérien. L'a-protéobactérie Caulobacter crescentus est un excellent modèle pour étudier le cycle cellulaire bactérien, essentiellement parce qu'il est aisé d'isoler des populations de cellules synchronisées à la même étape du cycle cellulaire et parce que cette bactérie n'initie la réplication de son chromosome qu'une seule fois et à un moment précis de son cycle. Cette dernière caractéristique est particulièrement pertinente pour l'objectif de mon travail doctoral, qui consistait à comprendre comment l'activité de la protéine essentielle DnaA est régulée dans l'espace et dans le temps chez C. crescentus. Chez Escherichia coli, la protéine Hda convertie DnaA-ATP en DnaA-ADP en stimulant l'activité ATPasique de DnaA, ce qui empêche la sur-initiation de la réplication du chromosome. Nous proposons qu'un mécanisme similaire existe chez C. crescentus. Il serait non seulement nécessaire au contrôle de la réplication du chromosome, mais aussi au contrôle de l'expression de certains gènes. Dans un premier temps, nous avons mis en évidence le fait que l'hydrolyse de l'ATP lié à DnaA est un processus essentiel à la viabilité de C. crescentus. Nos résultats suggèrent que DnaA-ATP initie la réplication du chromosome, comme nous avons observé que des cellules qui sur-expriment une protéine DnaA(R357A) mutée sans domaine ATPasique fonctionnel, sur-initie la réplication de leur chromosome, contrairement aux cellules qui sur-expriment la protéine DnaA sauvage à des niveaux équivalents. Au contraire, la protéine DnaA(R357A) était moins active que la protéine DnaA sauvage pour promouvoir la transcription de trois gènes essentiels, ce qui suggère que ces derniers sont peut-être plus efficacement activés par DnaA-ADP que DnaA-ATP. Nous proposons que la conversion de DnaA-ATP en DnaA-ADP réprime l'initiation de la réplication, tandis qu'elle active la transcription de plusieurs gènes impliqués dans des étapes plus tardives du cycle cellulaire. Dans un deuxième temps, nous avons étudié le rôle de la protéine HdaA, homologue à Hda, dans la conversion de DnaA-ATP en DnaA-ADP chez C. crescentus. Cette protéine est essentielle à la viabilité de C. crescentus et sa déplétion donne des cellules qui sur-initient la réplication de leur chromosome, suggérant que HdaA est un répresseur de la réplication du chromosome. HdaA co-localise de manière dynamique avec le réplisome. Lors de mon travail doctoral, nous avons démontré que DnaN, le β-clamp de l'ADN polymérase, est l'élément qui recrute HdaA au réplisome in vivo. Nous avons aussi montré qu'une protéine HdaA mutante qui ne peut pas interagir ou co-localiser avec DnaN, n'est pas fonctionnelle, ce qui suggère que HdaA est activée par DnaN. Nous avons néanmoins aussi isolé une autre protéine HdaA non fonctionnelle, dont une arginine conservée de son domaine AAA+ était mutée, mais qui pouvait toujours co-localiser avec le réplisome, ce qui suggère que le domaine AAA+ de HdaA est nécessaire après le recrutement de HdaA au réplisome. Nous proposons que HdaA stimule l'activité ATPasique de DnaA qu'une fois que la réplication a commencé, grâce à son interaction avec DnaN et aux deux arginines conservées des protéines HdaA et DnaA. Finalement, nous avons construit différentes souches sur-exprimant HdaA, DnaN ou DnaA. Nous avons observé que la sur-production de HdaA retarde la réplication du chromosome, tandis que la sur-production de DnaN a un effet opposé. Nos observations suggèrent aussi que la sur-expression de DnaA dans des cellules déplétées pour HdaA aggrave leur phénotype de sur-initiation. Nous en concluons que HdaA et DnaN collaborent étroitement et de manière dynamique pour réguler le rapport DnaA-ATP/DnaA-ADP dans la cellule, pour s'assurer que la réplication du chromosome ne soit initiée qu'une seule fois par cycle cellulaire chez C. crescentus. Globalement, notre travail a mis en évidence des informations importantes sur la régulation de l'activité de DnaA chez C. crescentus. Comme DnaA, HdaA et DnaN sont des protéines très conservées, la plupart de nos découvertes sont utiles pour mieux comprendre comment la réplication du chromosome bactérien et l'expression des gènes sont contrôlées par DnaA chez de nombreuses autres espèces bactériennes.

Origin of cadmium enrichments in carbonate rocks deposited in the Alpine Tethys area during the Middle-Late Jurassic

ABSTRACTThe pollution of air, soil and water by heavy metals through anthropogenic activities is an object of numerous environmental studies since long times. A number of natural processes, such as volcanic activity, hydrothermal fluid circulation and weathering of metal-rich deposits may lead to an additional and potentially important input and accumulation of heavy metals in the environment. In the Swiss and French Jura Mountains, anomalous high cadmium (Cd) concentrations (up to 16 ppm) in certain soils are related to the presence of underlying Cd-enriched (up to 21 ppm) carbonate rocks of Middle to Late Jurassic age. The aim of this study is to understand the processes controlling Cd incorporation into carbonate rocks of Middle and Late Jurassic age and to reconstruct the sedimentary and environmental conditions, which have led to Cd enrichments in these sedimentary rocks.Cd concentrations in studied hemipelagic sections in France vary between 0.1 and 0.5 ppm (mean 0.15 ppm). Trace-element behavior and high Mn concentrations suggest that sediment accumulation occurred in a well-oxygenated environment. Increases in Cd contents in the bulk-rock carbonate sediments may be related to increases in surface-water productivity under oxic conditions and important remineralization of organic matter within the water column. In platform settings preserved in the Swiss Jura Mountains, no correlation is observed between Cd contents and evolution of environmental conditions. Cd concentrations in these platform sections are often below the detection limit, with isolated peaks of up to 21 ppm. These important Cd enrichments are associated with peaks in Zn concentrations and are present in carbonate rocks independently of facies and age. The high Cd contents in these shallow-water carbonate rocks are partly related to the presence of disseminated, Cd-rich (up to 1.8%), sphalerite (ZnS) mineralization. The basement rocks are considered to be the source of metals for sulfide mineralization in the overlying Jurassic strata, as the sphalerite Pb isotope pattern is comparable to that of granite rocks from the nearby southern Black Forest crystalline massif. The Rb-Sr ages of sphalerite samples indicate that a main phase of sphalerite formation occurred near the boundary between the late Middle and early Late Jurassic, at around 162 Ma, as a result of enhanced tectonic and hydrothermal activity in Europe, related to the opening of the Central Atlantic and to the tectonic/thermal subsidence during spreading of the Alpine Tethys. I therefore propose to use unusually high Cd concentrations in carbonates as a tracer of tectonic activity in the Jura Mountains area, especially in the case when important enrichments in Zn co-occur. Paleoproductivity reconstructions based on records of authigenic Cd may be compromised not only by post-depositional redistribution, but also by incorporation of additional Cd from hydrothermal solutions circulating in the rock.The circulation of metal-rich hydrothermal fluids through the sediment sequence, in addition to specific environmental conditions during sedimentation, contributes to the incorporation of Cd into the carbonate rocks. However, only hydrothermal activity has led to the unusually high concentrations of Cd in carbonate rocks of Bajocian-Oxfordian age, through the formation of sphalerite mineralization.

Changes in activity of the regulatory glycolytic enzymes and of the pyruvate-dehydrogenase complex during the development of Xenopus laevis.

In this study we investigated the variations of the maximal activities of the rate-controlling glycolytic enzymes (i.e., hexokinase, HK; phosphofructokinase, PFK; pyruvate kinase, PK) and of the pyruvate-dehydrogenase complex (PDHc) during the early embryogenesis of Xenopus laevis (from cleavage through hatching). All the enzymatic assays, using different coupled reactions, were performed spectrophotometrically on cytosolic and mitochondrial fractions. The maximal HK activity increases markedly from neurulation onwards, PFK activity presents a peak around gastrulation, PK activity remains relatively constant throughout the period studied and the highest PDHc activity is observed during cleavage. The specific activities display the same temporal pattern. Furthermore, in the sequence of reactions by which glucose is degraded to form acetyl-CoA, the maximal activities of PFK and PK are not limiting while those of HK and PDHc could be rate-limiting at relatively late developmental stages (hatching).