Depleted arc volcanism in the Alboran Sea and shoshonitic volcanism in Morocco: geochemical and isotopic constraints on Neogene tectonic processes

Samples of volcanic rocks from Alboran Island, the Alboran Sea floor and from the Gourougou volcanic centre in northern Morocco have been analyzed for major and trace elements and Sr-Nd isotopes to test current theories on the tectonic geodynamic evolution of the Alboran Sea. The Alboran Island samples are low-K tholeiitic basaltic andesites whose depleted contents of HFS elements (similar to0.5xN-MORB), especially Nb (similar to0.2xN-MORB), show marked geochemical parallels with volcanics from immature intra-oceanic arcs and back-arc basins. Several of the submarine samples have similar compositions, one showing low-Ca boninite affinity. Nd-143/Nd-144 ratios fall in the same range as many island-arc and back-arc basin samples, whereas Sr-87/Sr-86 ratios (on leached samples) are somewhat more radiogenic. Our data point to active subduction taking place beneath the Alboran region in Miocene times, and imply the presence of an associated back-arc spreading centre. Our sea floor suite includes a few more evolved dacite and rhyolite samples with (Sr-87/Sr-86)(0) up to 0.717 that probably represent varying degrees of crustal melting. The shoshonite and high-K basaltic andesite lavas from Gourougou have comparable normalized incompatible-element enrichment diagrams and Ce/Y ratios to shoshonitic volcanics from oceanic island arcs, though they have less pronounced Nb deficits. They are much less LIL- and LREE-enriched than continental arc analogues and post-collisional shoshonites from Tibet. The magmas probably originated by melting in subcontinental lithospheric mantle that had experienced negligible subduction input. Sr-Nd isotope compositions point to significant crustal contamination which appears to account for the small Nb anomalies. The unmistakable supra-subduction zone (SSZ) signature shown by our Alboran basalts and basaltic andesite samples refutes geodynamic models that attribute all Neogene volcanism in the Alboran domain to decompression melting of upwelling asthenosphere arising from convective thinning of over-thickened lithosphere. Our data support recent models in which subsidence is caused by westward rollback of an eastward-dipping subduction zone beneath the westemmost Mediterranean. Moreover, severance of the lithosphere at the edges of the rolling-back slab provides opportunities for locally melting lithospheric mantle, providing a possible explanation for the shoshonitic volcanism seen in northern Morocco and more sporadically in SE Spain. (C) 2004 Elsevier B.V. All rights reserved.

La gigantomachie de Lousanna-Vidy suivie de considérations sur la transmission du motif de l'anguipède

Considérations méthodologiques Nous avons limité aux précisions indispensables à la compréhension de notre propos les considérations sur la gigantomachie en général. Nous renvoyons aux études signalées plus haut (supra, p. 7, n. 2), principalement pour ce qui concerne les géants avant leur transformation en anguipèdes à partir de l'époque hellénistique. Notre recherche de parallèles reposera sur quelques oeuvres d'art encore existantes : les sculptures décorant les plus importantes d'entre elles feront dès lors figure d'archétype, même si, bien sûr, rien ne permet d'exclure qu'il en ait existé de plus significatives. Parmi les nombreux monuments aujourd'hui disparus, respectivement parmi ceux qui seraient encore à découvrir, il s'en trouvait sans doute qui auraient été susceptibles de servir de modèle pour les sculptures ornant le fanum de Lousonna, duquel bien peu de restes nous sont parvenus. A l'exception de quelques renvois ponctuels, notre démarche s'est appuyée exclusivement sur du matériel et des informations déjà publiés. Pour la reconstitution des bas-reliefs de Lousonna, nous nous sommes inspiré généralement de sculptures hellénistiques et romaines dont l'ornementation présentait des similitudes avec les fragments à notre disposition ; la plupart des parallèles sont mentionnés dans le Lexicon Iconographicum Mythologiae Classicae. L'examen des volumes du Corpus Signorum Imperii Romani et de quelques autres recueils nous a permis de faire des propositions pour les cas restés en suspens. A une exception près, l'échantillonnage aéré formé à partir d'ensembles sculptés qui devaient avoir les mêmes caractéristiques que le matériel que nous tenterons d'identifier : ils comportaient des monstres anguipèdes avec les jambes se terminant par la tête du serpent, remontant au plus tard à la fin de la période romaine et produits dans un atelier gréco-romain. Afin de recréer avec le plus de vraisemblance possible l'environnement du fanum de Lousonna, nous avons recherché des édifices de caractéristiques semblables dans les catalogues de temples gallo-romains dressés par P. D. HORNE et A. C. KING (1980), respectivement I. FAUDUET et P. ARCELIN (1993). Tant l'absence presque complète de restes architecturaux susceptibles d'être rapportés à l'édifice religieux que la nature somme toute modeste du vicus lémanique nous ont fait opter pour une variante minimaliste, se limitant finalement à la structure supportant la gigantomachie devant un temple sans aucune décoration. Pour tenter de préciser les modalités de la transmission du thème des géants, nous envisagerons trois cheminements possibles : la tradition orale, la transmission littéraire et, enfin, la représentation iconographique, qu'il s'agisse de monuments, d'objets mobiliers ou même des quelques rares illustrations de textes antiques. Sauf indication contraire, les textes anciens sont cités dans les traductions des Belles-Lettres, des Sources chrétiennes ou de la Loeb Classical Library dont la liste figure à la page 161. La version française des textes dont aucune traduction n'était disponible est généralement due à François Mottas (traduction F.M.). Nous ne reportons les dates de naissance des auteurs ou des artistes mentionnés que lorsqu'elles sont utiles à la compréhension de notre exposé. En plus du rôle qu'ont pu jouer les oeuvres d'art disparues au cours des deux derniers millénaires, divers facteurs ont dû assurer la constitution et la mise au point d'un imaginaire de plus en plus élaboré des gigantomachies. La mémoire a certes sa part dans l'inspiration des artistes qui réalisèrent les sculptures de la cité lémanique; mais si un mythe ou le récit d'un événement peuvent s'être transmis de bouche à oreille au cours des siècles, certaines ressemblances dans l'attitude des personnages sont trop frappantes, même en tenant compte de ces gestes qu'il n'existe qu'une seule façon de représenter: il n'est dès lors pas possible d'imaginer que la transmission des détails des scènes se serait pratiquée uniquement par voie orale. Si le voyage touristique; tel que nous l'entendons de nos jours, n'a pas existé, les personnes susceptibles d'avoir ramené des informations de leurs déplacements à travers l'Empire sont plus nombreuses qu'on ne le croirait au premier abord. Fonctionnaires allant prendre leur charge ou en mission dans une contrée voisine; soldats, parmi lesquels des mercenaires gaulois; pèlerins ayant visité de grands sanctuaires, comme celui d'Esculape à Pergame, emplacement de la gigantomachie la plus impressionnante, ou d'autres lieux de culte; jeunes fortunés ayant étudié à Athènes; commerçants accompagnés par des muletiers ou des portefaix acheminant leurs marchandises; membres de corporations ou artisans exerçant des métiers itinérants; esclaves, dont l'exportation devait représenter une source de revenus intéressante pour les commerçants romains; en dernier lieu, sans parler des artistes eux-mêmes, ces arpenteurs-géomètres chargés de toutes sortes de relevés qui accompagnaient les empereurs lors de leurs déplacements (infra, p. 36). Il faudra cependant rester prudent quant à l'affirmation d'une connaissance visuelle directe que les sculpteurs de Lousonna auraient eue des réalisations antiques avec lesquelles nous mettrons la gigantomachie en parallèle. Même si elle n'a toujours pas pu être prouvée, la circulation de cahiers de modèles semble bel et bien assurée: dans un atelier, les maîtres ont forcément passé leurs croquis à leurs successeurs et ceci s'est peut-être répété pour plusieurs générations d'artisans. Sans parler des monnaies, d'autres moyens de transmission peuvent encore être mentionnés : éventuelles éditions illustrées de textes antiques, motifs gravés sur des gemmes ou représentés sur des récipients décorés... Une observation s'impose ici : la plupart des monuments que nous utiliserons pour notre reconstitution existaient encore lors de l'érection de notre gigantomachie. Une fois les bas-reliefs de Lousonna reconstitués, restait donc à combler l'absence de toute étude sur la survie de la gigantomachie à travers les âges et à préciser l'emploi qui en serait fait à la Renaissance. Divers recueils d'ouvrages consacrés à la mythologie et remontant à cette période nous ont permis de décrire les modalités de la reprise du récit de la guerre des géants; en l'absence de toute synthèse sur ceux-ci dans la peinture de la Renaissance, c'est en partant de l'examen des nombreux travaux consacrés au Palazzo del Te à Mantoue que nous avons pu établir un lien entre les représentations de géants peintes durant la première moitié du 16ème siècle, au cours duquel la gigantomachie était redevenue un sujet d'actualité. Le monument de la bourgade lémanique comporte encore neuf personnages et constitue, avec celui d'Yzeures-sur-Creuse, l'exemplaire le plus complet découvert dans la partie occidentale de l'Empire romain : il méritait bien d'être à l'origine d'une telle démarche.

Genetics: biased transmission of genomes according to parents of origin.

A new study shows that wood ant queens selectively pass the maternally-inherited half of their genome to their daughters and the paternally-inherited half to their sons. This system, which most likely evolved from ancestral hybridization, creates distinct genetic lineages.

HIV-1 drug resistance transmission networks in southwest Switzerland.

To determine viral subtypes and resistance mutations to antiretroviral treatment (ART) in untreated HIV-1 acutely infected subjects from Southwest Switzerland. Clinical samples were obtained from the HIV primary infection cohort from Lausanne. Briefly, pol gene was amplified by nested PCR and sequenced to generate a 1?kb sequence spanning protease and reverse transcriptase key protein regions. Nucleotide sequences were used to assess viral genotype and ART resistance mutations. Blood specimens and medical information were obtained from 30 patients. Main viral subtypes corresponded to clade B, CRF02_AG, and F1. Resistant mutations to PIs consisted of L10V and accessory mutations 16E and 60E present in all F1 clades. The NNRTI major resistant mutation 103N was detected in all F1 viruses and in other 2 clades. Additionally, we identified F1 sequences from other 6 HIV infected and untreated individuals from Southwest Switzerland, harboring nucleotide motifs and resistance mutations to ART as observed in the F1 strains from the cohort. These data reveal a high transmission rate (16.6%) for NNRTI resistant mutation 103N in a cohort of HIV acute infection. Three of the 5 resistant strains were F1 clades closely related to other F1 isolates from HIV-1 infection untreated patients also coming from Southwest Switzerland. Overall, we provide strong evidence towards an HIV-1 resistant transmission network in Southwest Switzerland. These findings have relevant implications for the local molecular mapping of HIV-1 and future ART surveillance studies in the region.

Stable transmission of targeted gene modification using single-stranded oligonucleotides with flanking LNAs.

Targeted mutagenesis directed by oligonucleotides (ONs) is a promising method for manipulating the genome in higher eukaryotes. In this study, we have compared gene editing by different ONs on two new target sequences, the eBFP and the rd1 mutant photoreceptor betaPDE cDNAs, which were integrated as single copy transgenes at the same genomic site in 293T cells. Interestingly, antisense ONs were superior to sense ONs for one target only, showing that target sequence can by itself impart strand-bias in gene editing. The most efficient ONs were short 25 nt ONs with flanking locked nucleic acids (LNAs), a chemistry that had only been tested for targeted nucleotide mutagenesis in yeast, and 25 nt ONs with phosphorothioate linkages. We showed that LNA-modified ONs mediate dose-dependent target modification and analyzed the importance of LNA position and content. Importantly, when using ONs with flanking LNAs, targeted gene modification was stably transmitted during cell division, which allowed reliable cloning of modified cells, a feature essential for further applications in functional genomics and gene therapy. Finally, we showed that ONs with flanking LNAs aimed at correcting the rd1 stop mutation could promote survival of photoreceptors in retinas of rd1 mutant mice, suggesting that they are also active in vivo.

Apocryphes arméniens. Transmission - traduction - création - iconographie

Ce volume rassemble les contributions présentées au Colloque international sur "La littérature apocryphe en langue arménienne" qui s'est tenu du 18 au 20 sep-tembre 1997 à l'Université de Genève. Cette réunion scientifique a été organisée conjointement par le Centre de recherches arménologiques de Genève et par l'Institut romand des sciences bibliques de l'Université de Lausanne. Il est le fruit d'une première collaboration entre l'Association internationale des études arméniennes (AIEA) et l'Association pour l'étude de la littérature apocryphe chrétienne (AELAC). Les deux associations ont tenté de définir ensemble la place et l'importance des oeuvres apocryphes arméniennes dans l'histoire de l'établissement du canon biblique ainsi que dans le contexte plus général de la diffusion des textes chrétiens et juifs. Après quelques réflexions introductives, les articles de ce volume ont été regroupés en quatre sections autours des thèmes de la transmission, de la traduction, de la création et de l'iconographie. Le débat entre les spécialistes de l'AIEA et de l'AELAC à l'occasion des journées genevoises s'est avéré très stimulants. La publication de ce volume, qui s'adresse également au public des non arménisants, contribue à intensifier et à promouvoir d'autres formes de collaborations interdisciplinaires, indispensables dans un champ de recherche aux implications si vastes.

Cultural transmission can inhibit the evolution of altruistic helping.

The study of culturally inherited traits has led to the suggestion that the evolution of helping behaviors is more likely with cultural transmission than without. Here we evaluate this idea through a comparative analysis of selection on helping under both genetic and cultural inheritance. We develop two simple models for the evolution of helping through cultural group selection: one in which selection on the trait depends solely on Darwinian fitness effects and one in which selection is driven by nonreproductive factors, specifically imitation of strategies achieving higher payoffs. We show that when cultural variants affect Darwinian fitness, the selection pressure on helping can be markedly increased relative to that under genetic transmission. By contrast, when variants are driven by nonreproductive factors, the selection pressure on helping may be reduced relative to that under genetic inheritance. This occurs because, unlike biological offspring, the spread of cultural variants from one group to another through imitation does not reduce the number of these variants in the source group. As a consequence, there is increased within-group competition associated with traits increasing group productivity, which reduces the benefits of helping. In these cases, selection for harming behavior (decreasing the payoff to neighbors) may occur rather than selection for helping.

Transmission disequilibrium of small CNVs in simplex autism.

We searched for disruptive, genic rare copy-number variants (CNVs) among 411 families affected by sporadic autism spectrum disorder (ASD) from the Simons Simplex Collection by using available exome sequence data and CoNIFER (Copy Number Inference from Exome Reads). Compared to high-density SNP microarrays, our approach yielded ∼2× more smaller genic rare CNVs. We found that affected probands inherited more CNVs than did their siblings (453 versus 394, p = 0.004; odds ratio [OR] = 1.19) and that the probands' CNVs affected more genes (921 versus 726, p = 0.02; OR = 1.30). These smaller CNVs (median size 18 kb) were transmitted preferentially from the mother (136 maternal versus 100 paternal, p = 0.02), although this bias occurred irrespective of affected status. The excess burden of inherited CNVs among probands was driven primarily by sibling pairs with discordant social-behavior phenotypes (p < 0.0002, measured by Social Responsiveness Scale [SRS] score), which contrasts with families where the phenotypes were more closely matched or less extreme (p > 0.5). Finally, we found enrichment of brain-expressed genes unique to probands, especially in the SRS-discordant group (p = 0.0035). In a combined model, our inherited CNVs, de novo CNVs, and de novo single-nucleotide variants all independently contributed to the risk of autism (p < 0.05). Taken together, these results suggest that small transmitted rare CNVs play a role in the etiology of simplex autism. Importantly, the small size of these variants aids in the identification of specific genes as additional risk factors associated with ASD.

A stable and 40Ar/39Ar isotope study of a major thrust in the Helvetic nappes (Swiss Alps) - Evidence for fluid-flow and constraints on nappe kinematics

Stable isotope and Ar-40/Ar-39 measurements,were made on samples associated with a major tectonic discontinuity in the Helvetic Alps, the basal thrust of the Diablerets nappe (external zone of the Alpine Belt) in order to determine both the importance of fluids in this thrust zone and the timing of thrusting. A systematic decrease in the delta(18)O values (up to 6 parts per thousand) of calcite, quartz, and white mica exists within a 10- to 70-m-wide zone over a distance of 37 km along the thrust, and they become more pronounced toward the root of the nappe. A similar decrease in the delta(13)C values of calcite is observed only in the deepest sections (up to 3 parts per thousand). The delta D-SMOW (SMOW = standard mean ocean water) values of white mica are -54 parts per thousand +/- 8 parts per thousand (n = 22) and are independent of the distance from the thrust. These variations are interpreted to reflect syntectonic solution reprecipitation during fluid passage along the thrust. The calculated delta(18)O and delta D values (versus SMOW) for the fluid in equilibrium with the analyzed minerals is 12 parts per thousand to 16 parts per thousand and -30 parts per thousand to +5 parts per thousand, respectively, for assumed temperatures of 250 to 450 degrees C. The isotopic and structural data are consistent with fluids derived from the deep-seated roots of the Helvetic nappes where large volumes of Mesozoic sediments were metamorphosed to the amphibolite facies, It is suggested that connate and metamorphic waters, overpressured by rapid tectonic burial in a subductive system escaped by upward infiltration along moderately dipping pathways until they reached the main shear zone at the base of the moving pile, where they were channeled toward the surface, This model also explains the mechanism by which large amounts of fluid were removed from the Mesozoic sediments during Alpine metamorphism. White mica Ar-49/Ar-39 ages vary from 27 Ma far from the Diablerets thrust to 15 Ma along the thrust. An older component is observed in micas far from the thrust, interpreted as a detrital signature, and indicates that regional metamorphic temperatures were less than about 350 degrees C. The;plateau and near plateau ages nearest the thrust are consistent with either neocrystallization of white mica or argon loss by recrystallization during thrusting, which may have been enhanced in the zones of highest fluid flow. The 15 Ma Ar-40/Ar-39 age plateau measured on white mica sampled exactly on the thrust surface dates the end of both fluid flow and tectonic transport.

Female-biased infection and transmission of the gastrointestinal nematode Trichuris arvicolae infecting the common vole, Microtus arvalis.

Previous studies addressing the importance of host gender in parasite transmission have shed light on males as the more important hosts, with the higher transmission potential of males being explained by the fact that they often harbour higher parasite loads than females. However, in some systems females are more heavily infected than males and may be responsible for driving infection under such circumstances. Using a wild population of common voles (Microtus arvalis), we showed that females were more frequently infected by the intestinal nematode Trichuris arvicolae than males (i.e. prevalence based on the presence of eggs in the faeces) and that females were shedding greater numbers of parasite eggs per gram of faeces (EPG) than males. By applying an anthelmintic treatment to either male or female voles, we demonstrated that treating females significantly reduced parasite burdens (i.e. prevalence and EPG) of both male and female hosts, while treating males only reduced parasite burden in males. These findings indicate that in this female-biased infection system females play a more important role than males in driving the dynamics of parasite transmission.

The role of neutralizing antibodies for mouse mammary tumor virus transmission and mammary cancer development.

Mouse mammary tumor virus (MMTV) infection establishes chronic germinal centers and a lifelong neutralizing Ab response. We show that removal of the draining lymph node after establishment of the germinal center reaction led to complete loss of neutralizing Abs despite comparable infection levels in peripheral lymphocytes. Importantly, in the absence of neutralization, only the exocrine organs mammary gland, salivary gland, pancreas, and skin showed strikingly increased infection, resulting in accelerated mammary tumor development. Induction of stronger neutralization did not influence chronic infection levels of peripheral lymphoid organs but strongly inhibited mammary gland infection and virus transmission to the next generation. Taken together, we provide evidence that a tight equilibrium in virus neutralization allows limited infection of exocrine organs and controls cancer development in susceptible mouse strains. These experiments show that a strong neutralizing Ab response induced after infection is not able to control lymphoid MMTV infection. Strong neutralization, however, is capable of blocking amplification of mammary gland infection, tumor development, and virus transmission to the next generation. The results also indicate a role of neutralization in natural resistance to MMTV infection.

Liquid line of descent of a basanitic liquid at 1.5 GPa: Constraints for metasomatic vein formation

The metasomatism observed in the oceanic and continental lithosphere is generally interpreted to represent a continuous differentiation process forming anhydrous and hydrous veins plus a cryptic enrichment in the surrounding peridotite. In order to constrain the mechanisms of vein formation and potentially clarify the nature and origin of the initial metasomatic agent, we performed a series of high-pressure experiments simulating the liquid line of descent of a basanitic magma differentiating within continental or mature oceanic lithosphere. This series of experiments has been conducted in an end-loaded piston cylinder apparatus starting from an initial hydrous ne-normative basanite at 1.5 GPa and temperature varying between 1,250 and 980°C. Near-pure fractional crystallization process was achieved in a stepwise manner in 30°C temperature steps and starting compositions corresponding to the liquid composition of the previous, higher-temperature glass composition. Liquids evolve progressively from basanite to peralkaline, aluminum-rich compositions without significant SiO2 variation. The resulting cumulates are characterized by an anhydrous clinopyroxene + olivine assemblage at high temperature (1,250-1,160°C), while at lower temperature (1,130-980°C), hydrous cumulates with dominantly amphibole + minor clinopyroxene, spinel, ilmenite, titanomagnetite and apatite (1,130-980°C) are formed. This new data set supports the interpretation that anhydrous and hydrous metasomatic veins could be produced during continuous differentiation processes of primary, hydrous alkaline magmas at high pressure. However, the comparison between the cumulates generated by the fractional crystallization from an initial ne-normative liquid or from hy-normative initial compositions (hawaiite or picrobasalt) indicates that for all hydrous liquids, the different phases formed upon differentiation are mostly similar even though the proportions of hydrous versus anhydrous minerals could vary significantly. This suggests that the formation of amphibole-bearing metasomatic veins observed in the lithospheric mantle could be linked to the differentiation of initial liquids ranging from ne-normative to hy-normative in composition. The present study does not resolve the question whether the metasomatism observed in lithospheric mantle is a precursor or a consequence of alkaline magmatism; however, it confirms that the percolation and differentiation of a liquid produced by a low degree of partial melting of a source similar or slightly more enriched than depleted MORB mantle could generate hydrous metasomatic veins interpreted as a potential source for alkaline magmatism by various authors.