Divergent and convergent margins in the north-western Alps - Confrontation to actualistic models

Divergent and convergent margins actualistic models are reviewed and applied to the history of the western Alps. Tethyan rifting history and geometry are analyzed: the northern European margin is considered as an upper plate whereas the southern Apulian margin is a lower plate; the Breche basin is regarded as the former break-away trough; the internal Brianconnais domain represents the northern rift shoulder whilst the more external domains are regarded as the infill of a complex rim basin locally affected by important extension (Valaisan and Vocontain trough). The Schistes lustres and ophiolites of the Tsate nappe are compared to an accretionary prism: the imbrication of this nappe elements is regarded as a direct consequence of the accretionary phenomena already active in early Cretaceous; the Gets/Simme complex could orginate from a more internal part of the accretionary prism. Some eclogitic basements represent the former Apulian margin substratum (Sesia) others (Mont-Rose) are interpreted as the former edge of the European margin. The history of the closing Tethyan domain is analyzed and the remaining problems concerning the cinematics, the presence/absence of a volcanic arc and the eoalpine metamorphism are discussed.

Western Préalpes Médianes Romandes: Timing and structure. A review.

Between the original position and their present day location as klippen, the Prealpes Medianes underwent a complex history of paleotectonics and alpine tectonics. Due to the opening of the Piemont ocean the Brianconnais sedimentation realm of the Prealpes Medianes evolved as a rim basin of the northern passive margin during Jurassic to Eocene times. Different paleotectonic features (normal faults, synsedimentary growth structures, inversion structures) developed and were active above a basal detachment in evaporitic layers. The tectonic movements were a consequence of thermal events in the crust. Isolated from the Iberic continent at the end of the Late Cretaceous, the Brianconnais exotic terrain was incorporated into the accretionary prism of the closing Piemont ocean and the incipient alpine orogeny during the Lutetian-Bartonian. The Prealpes Medianes were detached from their homeland during the Bartonian-Priabonian and were transported onto the foreland. The tectonic style is one of a thin-skinned foreland fold and thrust belt. Fault associated fold development above a main decollement, together with internal deformation, represent the Prealpes Medianes main structural features. The very low-grade metamorphic conditions have their origin in the heat flux induced by tectonic burial by overriding nappes in the accretionary prism. After having been transported on top of the developing Helvetic nappes the Prealpes were emplaced in their present day position in front of the Alpine mountain belt during Oligocene times. Post-emplacement and out of sequence thrusting, possibly younger than Oligocene, is observed and can be related to thrusting in the sedimentary substratum and the basement.

Subduction and obduction processes in the Swiss Alps

The significance of the Brianconnais domain in the Alpine orogen is reviewed in the light of data concerning its collision with the active Adriatic margin and the passive Helvetic margin. The Brianconnais which formerly belonged to the Iberian plate, was located on the northern margin of the Alpine Tethys (Liguro-Piemont ocean) since its opening in the early-Middle Jurassic. Together with the Iberian plate the Brianconnais terrane was separated from the European plate in the Late Jurassic-Early Cretaceous, following the northern Atlantic, Bay of Biscay, Valais ocean opening. This was accompanied by the onset of subduction along the northern margin of Adria and the closure of the Alpine Tethys. Stratigraphic and metamorphic data regarding this subduction and the geohistory of the Brianconnais allows the scenario of subduction-obduction processes during the Late Cretaceous-early Tertiary in the eastern and western Alps to be specified. HP-LT metamorphism record a long-lasting history of oceanic subduction-accretion, followed in the Middle Eocene by the incorporation of the Brianconnais as an exotic terrane into the accretionary prism. Middle to Late Eocene cooling ages of the Brianconnais basement and the presence of pelagic, anorogenic sedimentation lasting until the Middle Eocene on the Brianconnais preclude any sort of collision before that time between this domain and the active Adria margin or the Helvetic margin. This is confirmed by plate reconstructions constrained by magnetic anomalies in the Atlantic domain. Only a small percentage of the former Brianconnais domain was obducted, most of the crust and lithospheric roots were subducted. This applies also to domains formerly belonging to the southern Alpine Tethys margin (Austroalpine-inner Carpathian domain). It is proposed that there was a single Palaeogene subduction zone responsible for the Alpine orogen formation (from northern Spain to the East Carpathians), with the exception of a short-lived Late Cretaceous partial closure of the Valais ocean. Subduction in the western Tethyan domain originated during the closure of the Meliata ocean during the Jurassic incorporating the Austroalpine-Carpathian domain as terranes during the Cretaceous. The subduction zone propagated into the northern margin of Adria and then to the northern margin of the Iberian plate, where it gave birth to the Pyrenean-Provencal orogenic belt. This implies the absence of a separated Cretaceous subduction zone within the Austro-Carpathian Penninic ocean. Collision of Iberia with Europe forced the subduction to jump to the SE margin of Iberia in the Eocene, creating the Apenninic orogenic wedge and inverting the vergence of subduction from south- to north-directed. (C) 1998 Elsevier Science B.V. All rights reserved.

Tethyan margins in space and time

Rifting processes, leading to sea-floor spreading, are characterized by a sequence of events: transtensive phase of extension with syn-rift volcanism; simple shear extension accompanied by lithospheric thinning and asthenospheric up-welling and thermal uplift of the rift shoulder and asymmetric volcanism. The simple shear model of extension leads to an asymmetric model of passive margin: a lower plate tilted block margin and an upper plate flexural, ramp-like margin- Both will be affected by thermal contraction and subsidence, starting soon after sea-floor spreading. Based on these actualistic models Tethyan margins are classified as one type or the other. Their evolution from the first transtensional phase of extension to the passive margin stage are analyzed. Four main rifting events are recognized in the Tethyan realm: an episode of lower Paleozoic events leading to the formation of the Paleotethys; a Late Paleozoic event leading to the opening of the Permotethys and East Mediterranean basin: an early Mesozoic event leading to the opening of the Pindos Neotethys and a Jurassic event related to the opening of the Alpine/Atlantic Neotethys. Type margins are given as example of each rifting event: -Northern Iran (Alborz) as a type area for the Late Ordovician to Silurian rifting of Paleotethys. -Northern India and Oman for the Late Carboniferous to early Permian rifting of Permotethys. -The East Mediterranean (Levant, Tunisia) as a Late Carboniferous rifting event. -The Neotethyan rifting phases are separated in two types: an eastern Pindos system found in Turkey and Greece is genetically linked to the Permotethys with a sea-floor spreading delayed until middle Triassic: a western Alpine system directly linked to the opening of the central Atlantic is characterized by a Late Triassic transtensive phase, an early to Middle Liassic break-away phase and. following sea-floor spreading, a thermal subsidence phase starting in Dogger. Problems related to the closure of the Paleozoic oceanic domains are reviewed. A Late Permian, early Triassic phase of `'docking'' between an European accretionary prism (Chios) and a Paleotethyan margin is supported by recent findings in the Mediterranean area. Back-arc rifting within the European active margin led to the formation of marginal seas during Permian and Triassic times and will contribute to the closure of the Paleozoic oceans.

Religious identity and intercultural dialogue

(Résumé de l'ouvrage) In a world society ruled by economic globalisation, by political interests and theories such as Huntington's «clash of civilisations» that widen the gap between the North and the South, the question should be asked of the role of the religion. To what extent religion and politics can work together? Can faith still be thought as a means of saving the world? Considering that Christianity, Islam and Judaism have much in common, this collection of miscellanies wonders if these religions can join their forces for public benefit. Senior and junior scholars from all over the world, gathered for an interdisciplinary seminar, analyse the contemporary international relationships and geopolitics through the prism of religion, discussing whether it can provide practical solutions to solve conflicts and increase the respect of human rights.

Anti-impérialisme et nouvelle gauche radicale dans la Suisse des années 68

Cette thèse entend apporter un éclairage sur l'histoire politique et sociale de la Suisse des années 68, en étudiant l'articulation entre les mouvements anti-impérialistes et la nouvelle gauche radicale, alors foisonnante. Il s'agit d'analyser cette période de contestation au prisme de l'anti-impérialisme révolutionnaire, lequel, dans le contexte de l'opposition à la guerre du Vietnam, a fortement imprégné le mouvement protestataire, en assignant notamment au tiers-monde le rôle de sujet de l'émancipation mondiale. Combinant une triple approche - chronologique, thématique et biographique - ce travail est structuré en quatre parties. La première partie esquisse un panorama des mouvements anti-impérialistes des années 1960 et 1970 en Suisse, avec une focalisation sur les «années anti-imp», entre 1968 et 1975. La deuxième interroge le rapport entre anti¬impérialisme et nouvelle gauche radicale, en proposant une typologie des principaux courants. La troisième partie s'attache à examiner le système de représentations du monde et de la Suisse véhiculé par le discours de l'extrême gauche. Prenant pour objet le militantisme, la dernière partie esquisse un portrait de groupe de la « génération anti-imp », fondé sur une enquête prosopographique et sur un corpus d'entretiens réalisés avec des militants de l'époque. L'étude révèle que l'anti-impérialisme a fourni à la contestation soixante-huitarde un cadre conceptuel et analytique, un facteur de structuration, ainsi qu'un vecteur de mobilisation. Il a en particulier permis à la gauche radicale suisse d'inscrire sa lutte anticapitaliste locale dans un horizon global d'émancipation. L'analyse de l'anti-impérialisme révolutionnaire, qui a connu son apogée dans les années 68 avant de connaître un déclin rapide et presque total, invite à appréhender cette « décennie mouvementée » comme la fin d'un long cycle politique. -- This thesis aims to shed light on the social and political history of Switzerland in the 1960s and 1970s by studying the relationship between anti-imperialist movements and the emerging new radical left. It analyses this time of rebellion through the prism of revolutionary anti-imperialism. In the context of opposition to the Vietnam War, anti-imperialism strongly influenced protest movements, notably by assigning to the Third World the role of main actor in the fight for global emancipation. Combining a threefold approach - chronological, thematic and biographical - this work is structured in four parts. The first part provides a panorama of the anti-imperialist movements of the long 1960s in Switzerland with a focus on the « anti-imp years » between 1968 and 1975. The second part questions the relationship between anti-imperialism and the new radical left and proposes a typology of its main currents. The third part examines how the radical left's discourse represented the world, and Switzerland in particular. The last part addresses the question of activism and outlines a group portrait of the « anti-imp generation » based on a prosopographical study and on a body of interviews with former activists. This study reveals that anti-imperialism, besides serving as an agent of mobilization, provided a conceptual and ideological framework, as well as a structuring factor, to the protest movements. In particular, it enabled the Swiss radical left to fit its local anti-capitalist struggle into a global horizon of emancipation. This analysis of revolutionary anti- imperialism, which had its heyday in the 1960s and 1970s before experiencing a rapid and almost total decline, thus invites us to see this « turbulent decade » as the end of a long political cycle.

Remodelage des canaux potassiques dépendants de l'ATP lors de l'hypertrophie et de l'insuffisance cardiaque

RESUME :Introduction. Les maladies cardiovasculaires représentent la première cause de mortalité dans les pays développés et l'insuffisance cardiaque (IC) est la plus fréquente. Suite à un infarctus, le coeur des patients subit un remodelage ventriculaire pouvant évoluer vers un état d'IC. L'IC se définit comme un état dans lequel le coeur n'est plus capable d'approvisionner suffisamment les organes et cet état s'accompagne souvent de troubles du rythme cardiaque. Le remodelage ventriculaire touche de nombreux gènes codant à la fois pour les voies métaboliques et pour des canaux ioniques favorisant ainsi l'apparition des arythmies responsables de la mort subite des patients atteints d'IC. Comprendre ce passage entre remodelage et IC est crucial afin de pouvoir un jour prévenir l'IC et les complications médicales qui l'accompagnent. Nous nous sommes intéressés aux canaux potassiques dépendants de l'ATP (KATP) car ces canaux ont la capacité de coupler le métabolisme de la cellule à son activité électrique. En effet, les canaux KATP s'ouvrent quand la charge énergétique (rapport ATP/ ADP) de la cellule chute. Dans les cardiomyocytes, l'ouverture des KATP induit une hyperpolarisation de la membrane cellulaire ce qui diminue indirectement la surcharge calcique et de ce fait préserve la cellule. Les canaux KATp sont formés de 4 sous-unités Kir6.x (Kir6.1 ou Kir6.2) formant le pore du canal associées à 4 sous-unités régulatrices SUR. Les propriétés électrophysiologiques ainsi que la sensibilité pharmacologique des canaux KATP dépendent de leur composition et seuls les canaux KATP formés par la sous-unité Kirô.l sont activés par le diazoxyde.Méthodes et résultats. Nous avons d'abord montré dans un modèle in vivo d'IC chez le rat adulte que les sous-unités Kir6.1 et SUR sont surexprimées dans ces conditions pathologiques. Par ailleurs, les cardiomyocytes issus des coeurs infarcis deviennent sensibles au diazoxyde reflétant la surexpression de Kir6.1. Les potentiels d'action qui sont prolongés dans l'IC et qui sont à l'origine d'arythmies majeures sont normalisés par l'ouverture des canaux KATp induite par le diazoxyde. Ainsi, l'ouverture pharmacologique des canaux KATp contribuerait à la cardio-protection. Dans une seconde partie, nous avons déterminé quels étaient les facteurs de transcription responsables de ce changement d'expression des sous-unités formant les KATP. Dans notre modèle, nous avons pu montrer que la surexpression de Kirô.l est due aux facteurs de transcription Fox03 et FoxF2 qui est aussi responsable de la surexpression des sous-unités SUR. Dans la dernière partie de ce travail, nous avons mis au point un modèle d'IC in vitro en cultivant les cardiomyocytes de rats adultes en présence d'angiotensine II (Angll) ou de TNFa. Ce modèle expérimental nous a non seulement permis de mettre en relation l'importance de L'AnglI et du TNFa sur le remodelage des canaux KATP mais aussi de développer un modèle in vitro présentant les mêmes caractéristiques que le modèle in vivo concernant le remodelage des KATP lors de l'IC. Ce dernier modèle expérimental ouvre des perspectives afin de mieux caractériser les voies de signalisation impliquées dans le remodelage des canaux KATp lors de l'IC.Conclusion. Les canaux KATp subissent un remodelage lors de l'IC et les résultats obtenus montrent le potentiel cardio-protecteur de ces canaux.ABSTRACT :Background and aim. Cardiovascular disease is the leading cause of death in developed countries and heart failure (HF) is the most common. Following myocardial infarction, the heart of the patient undergoes ventricular remodeling which may evolve toward a state of HF. HF is defined as a state in which heart is unable to supply enough blood to organs and this state is often accompanied by cardiac arrhythmias. Ventricular remodeling involves many genes coding for both metabolic enzymes and ion channels. Changes in ion channel expression can promote arrhythmias responsible for sudden death in patients with HF. A better understanding of the transition between remodeling and HF is crucial in order to prevent the complications associated to HF We were interested in ATP-dependent potassium channels (KATp) because they couple cell metabolism to electrical activity of the cell. Indeed, KATP channels open when the energy charge (ratio of ATP / ADP) of the cell collapses. In cardiomyocytes, the opening of KATP channels induces hyper- polanzation of the cell membrane which reduces calcium overload and thereby protects the cell. KATp channels are composed by 4 Kir6.x subumts (Kir6.1 or Kir6.2) forming the pore channel associated with 4 regulatory subunits SUR. The electrophysiological properties as well as pharmacological sensitivity of KATp channels depend on their composition and only KATP channels formed by Kir6.1 subunit are activated by diazoxide.Methods and results. Firstly, using an in vivo model of HF in adult rats, we showed that Kir6.1 and SUR subunits are overexpressed in HF. In addition, cardiomyocytes from post-infarction hearts became sensitive to diazoxide reflecting the overexpression of the Kir6.1 subunit. The opening of KATP by diazoxide tended to reduce the action potential duration (APD) which is extended in HF. This increase in APD is known to be a major source of arrhythmias during HF. Therefore, the opening of KATP channels by diazoxide would be cardio-protective. Secondly, we wanted to determine which transcription factors were responsible for this KATP remodeling. In our model of HF, we showed that overexpression of Kir6.1 is due to the transcription factors Fox03 and FOXF2 which is also responsible for SUR subunits overexpression. Thirdly, we developed an in vitro model of HF by cultivation of adult rat cardiomyocytes in the presence of angiotensin II (Angll) or TNFa. This model is very interesting not only because it underlines the importance of Angll and TNFa in KATp remodeling but also because this in vitro model presents the same KATP remodeling as the in vivo model of HF. These findings show that our in vitro model of HF opens up many possibilities to investigate more precisely the signaling pathways involved in remodeling of the KATP channels in HF.Conclusion. KATP channels undergo remodeling during HF and our results show the cardio¬protective potential of KATP channels in this disease.

Multicenter evaluation of the elecsys® anti-HCV II assay for the diagnosis of hepatitis C virus infection.

Routine screening of patients at risk of hepatitis C virus (HCV) infection has become a priority given recent improvements in therapeutic options and the asymptomatic nature of most chronic infections. The aim of this study was to evaluate the performance of the Elecsys® Anti-HCV II assay, a new qualitative antibody immunoassay, compared with currently available assays, and assess its suitability for routine diagnostic testing. The sensitivity of the Elecsys® Anti-HCV II, ARCHITECT® Anti-HCV, AxSYM® HCV 3.0, PRISM® HCV, Vitros® ECi Anti-HCV, Elecsys® Anti-HCV, and ADVIA Centaur® HCV assays was compared using commercially available seroconversion panels and samples from patients known to be HCV positive and infected with HCV genotypes 1-6. Specificity was investigated using samples from blood donors, unselected hospitalized patients, and patients with potential cross-reacting factors or from high-risk groups. The Elecsys® Anti-HCV II assay detected more positive bleeds than the comparator assays, was more sensitive in recognizing early HCV infection, and correctly identified all 765 samples known to be HCV positive, regardless of genotype. The overall specificity of the Elecsys(®) Anti-HCV II assay was 99.84% (n = 6,850) using blood donor samples, 99.66% (n = 3,922) using samples from unselected hospitalized patients, and 99.66% (n = 2,397) using samples from patients with potentially cross-reacting factors or from high-risk groups. The specificity of the Elecsys® Anti-HCV II assay was superior or equal to the comparator assays. In conclusion, the Elecsys® Anti-HCV II assay is a sensitive and specific assay suitable for routine use in the reliable detection of anti-HCV antibodies. J. Med. Virol. 85:1362-1368, 2013. © 2013 Wiley Periodicals, Inc.

Cruveilhier's legacy to skull base surgery: premise of an evidence-based neuropathology in the 19th century.

OBJECTIVES: Jean Cruveilhier has always been described as a pioneer in pathological anatomy. Almost nothing has been reported concerning his exceptional methodology allying pre-mortem clinical description and syndromic classification of neurological and neurosurgical diseases, and post-mortem meticulous dissections. Cruveilhier's methodology announced the birth of the anatomoclinical method built up by Jean-Martin Charcot and the neurological French school during the 19th century. The aim of our work is to extract the quintessence of Cruveilhier's contributions to skull base pathology through his cogent clinical descriptions coupled with exceptional lithographs of anterior skull base, suprasellar and cerebello-pontine angle tumors. METHODS: We reviewed the masterwork of Jean Cruveilhier on pathological anatomy and we selected the chapters dedicated to central nervous system pathologies, mainly skull base diseases. A systematic review was performed on Pubmed/Medline and Google Scholar using the keywords "Jean Cruveilhier", "Skull base pathology", "Anatomoclinical method". RESULTS: Among his descriptions, Cruveilhier dedicated large chapters to neurosurgical diseases including brain tumors, cerebrovascular pathologies, malformations of the central nervous system, hydrocephalus, brain infections and spinal cord compressions. CONCLUSION: This work emphasizes on the role of Jean Cruveilhier in the birth of the anatomoclinical method particularly in neuroscience during a 19th century rich of epistemological evolutions toward an evidence-based medicine, through the prism of Cruveilhier's contribution to skull base pathology.

Crystallization and preliminary crystallographic characterization of an SH3 domain from the IB1 scaffold protein.

IB1 is a mammalian scaffold protein that interacts with components of the c-Jun N-terminal kinase (JNK) signal-transduction pathway mainly via its protein-protein interaction domains. Crystallization of the key Src homology 3 (SH3) domain of IB1 has been achieved. Crystallization experiments with unmodified protein and deliberately oxidized protein have led to different crystal forms. X-ray data have been collected to 3.0 A resolution from a crystal form with rectangular prism morphology. These crystals are orthorhombic (P2(1)2(1)2(1)), with unit-cell parameters a = 45.9, b = 57.0, c = 145.5 A. These are the first crystallographic data on a scaffold molecule such as IB1 to be reported.

High-precision U-Pb and 40Ar/39Ar dating of an Alpine ophiolite (Gets nappe, French Alps)

Coarse-grained gabbros from two different localities in the Gets nappe (Upper Prealps) have been dated by U-Pb and Ar-40/Ar-39 isotopic analyses. Zircons from both gabbros gave identical concordant U-Pb ages of 166 +/- 1 Ma (Fig. 4). Amphibole from one of them gave an Ar-40/Ar-39 plateau age of 165.9 +/- 2.2 Ma (Fig. 5). This concordance implies that 166 +/- 1 Ma is the age of magmatic crystallization of these gabbros. The Gets wildflysch with its mafic and ultramafic lenses is an ophiolitic melange, that we infer to come from a proximal part of the accretionary prism at the foot of the active SE margin of the Piemont ocean. In this position we can expect to find remnants of the oldest parts of the Piemont oceanic crust. These are the first high-precision dates using modern techniques from an Alpine ophiolite and are in excellent agreement with the following: 1) The few, somewhat younger, reliable ages on ophiolites from the probable continuation of the Piemont basin into the Apennines and Corsica; 2) Recent data on the age of the first supra-ophiolitic sediments (Late Bathonian to Early Callovian radiolarites); 3) The structural and stratigraphic evolution of the Brianconnais (s.s.) domain, the future NW margin of the Piemont ocean. We note a remarkable coincidence, in Late Bajocian time, between: (A) the end of tensile fracturing in the Brianconnais continental crust; (B) the beginning of its subsidence; (C) the age of the Gets ophiolites. This coincidence is consistent with an ocean opening mechanism based on a combination of subhorizontal extension and thermally driven vertical movements of the lithosphere.

Triassic pelagic deposits of Timor: palaeogeographic and sea-level implications

In West Timer, Triassic deposits are found in the Parautochthonous Complex, as well as in the Allochthonous series of Sonnebait. A detailed biostratigraphic investigation integrating field observations and facies analysis, allowed the reconstruction of a synthetic lithostratigraphic succession for the Upper Triassic, a stratigraphic transition from Carnian shales to Upper Norian-Rhaetian limestones is also shown by this study. The fossil content predominantly originates from an open marine environment; lithostratigraphic Units A-E are dated on the basis of radiolaria and palynomorphs, and Unit H, on ammonites and conodonts. The presence of pelagic bioclasts, together with normal grading, horizontal laminations, and current ripples, is indicative of a distal slope to basin environment. The ammonite rich condensed limestone of Unit H was deposited on a `pelagic carbonate plateau' exposed to storms and currents. The organic facies have been used as criteria for biostratigraphy, palaeoenvironmental interpretation, and sequence stratigraphy. The palaeontological analysis of the Triassic succession of West Timer is based on the investigation of radiolaria and palynomorphs, in the marls and limestones of Units A-E, and also on ammonites and conodonts in the condensed limestone of Unit H. Units A and B are Carnian (Cordevolian) in age, based on the occurrence of the palynomorph Camerosporites secatus, associated with `Lueckisporites' cf. singhii, Vallasporites ignacii, Patinosporites densus and Partitisporites novimundanus. Unit C is considered as Norian, on the basis of a relatively high percentage of Gliscopollis meyeriana and Granuloperculatipollis rudis. Unit D contains significant palynomorphs and radiolaria; the organic facies, characterized by marine elements, is dominated by the Norian dinocysts Heibergella salebrosacea and Heibergella aculeata; the radiolaria confirm the Norian age. They range from the lowermost Norian to the lower Upper Norian. Unit E also contains radiolaria, associated in the upper part with the well-known marker of the Upper Norian, Monotis salinaria. For Unit E, the radiolaria attest to a Lower to Upper Norian age based on the occurrence of Capnodoce and abundant Capnuchosphaera; the upper part is Upper Norian to Rhaetian based on the presence of Livarella valida. Finally, the blocks of condensed limestone with ammonites and conodonts of Unit H allowed the reconstruction of a synthetic stratigraphic succession of Upper Carnian to Upper Norian age. Our stratigraphic data lead to the suggestion that the Allochthonous complex, classically interpreted as a tectonic melange of the accretionary prism of the island Arc of Banda. is a tectonically dismembered part of a Triassic lithostratigraphic succession. (C) 2000 Elsevier Science B.V. All rights reserved.

Evidence for middle Cretaceous accretion at Santa Elena Peninsula (Santa Rosa Accretionary Complex), Costa Rica

An oceanic assemblage of alkaline basalts, radiolarites and polymictic breccias forms the tectonic substratum of the Santa Elena Nappe, which is constituted by extensive outcrops of ultramafic and mafic rocks of the Santa Elena Peninsula (NW Costa Rica). The undulating basal contact of this nappe defines several half-windows along the south shores of the Santa Elena Peninsula. Lithologically it is constituted by vesicular pillowed and massive alkaline basaltic flows, alkaline sills, ribbon-bedded and knobby radiolarites, muddy tuffaceous and detrital turbidites, debris flows and polymictic breccias and megabreccias. Sediments and basalt flows show predominant subvertical dips and occur in packages separated by roughly bed-parallel thrust planes. Individual packages reveal a coherent internal stratigraphy that records younging to the east in all packages and shows rapid coarsening upwards of the detrital facies. Alkaline basalt flows, pillow breccias and sills within radiolarite successions are genetically related to a mid-Cretaceous submarine seamount. Detrital sedimentary facies range form distal turbidites to proximal debris flows and culminate in megabreccias related to collapse and mass wasting in an accretionary prism. According to radiolarian dating, bedded radiolarites and soft-sediment- deformed clasts in the megabreccias formed in a short, late Aptian to Cenomanian time interval. Middle Jurassic to Lower Cretaceous radiolarian ages are found in clasts and blocks reworked from an older oceanic basement. We conclude that the oceanic assemblage beneath the Santa Elena Nappe does not represent a continuous stratigraphic succession. It is a pile of individual thrust sheets constituting an accretionary sequence, where intrusion and extrusion of alkaline basalts, sedimentation of radiolarites, turbidites and trench fill chaotic sediments occurred during the Aptian-Cenomanian. These thrust sheets formed shortly before the off-scraping and accretion of the complex. Here we define the Santa Rosa Accretionary Complex and propose a new hypothesis not considered in former interpretations. This hypothesis would be the basis for further research.

Membrane insertion and antibody recognition of a glycosylphosphatidylinositol-anchored protein: an optical study.

The kinetics of binding of a glycolipid-anchored protein (the promastigote surface protease, PSP) to planar lecithin bilayers is studied by an integrated optics technique, in which the bilayer membrane is supported on an optical wave guide and the phase velocities of guided light modes in the wave guide are measured. From these velocities, the optical parameters of the membrane and PSP layers deposited on the waveguide are determined, yielding in particular the mass of PSP bound to the membrane, which is followed in real time. From a comparison of the binding rates of PSP and PSP from which the lipid moiety has been removed, it is shown that the lipid moiety plays a key role in anchoring the protein to the membrane. Specific and nonspecific binding of antibodies to membrane-anchored PSP is also investigated. As little as a fifth of a monolayer of PSP is sufficient to suppress the appreciable nonspecific binding of antibodies to the membrane.