Maison des Sciences sociales et des Humanités - Lyon St-Étienne

Abstract. On the basis of a multi-proxy approach and a strategy combining lacustrine and marine records along a north–south transect, data collected in the central Mediterranean within the framework of a collaborative project have led to reconstruction of high-resolution and well-dated palaeohydrological records and to assessment of their spatial and temporal coherency. Contrasting patterns of palaeohydrological changes have been evidenced in the central Mediterranean: south (north) of around 40° N of latitude, the middle part of the Holocene was characterised by lake-level maxima (minima), during an interval dated to ca. 10 300–4500 cal BP to the south and 9000–4500 cal BP to the north. Available data suggest that these contrasting palaeohydrological patterns operated throughout the Holocene, both on millennial and centennial scales. Regarding precipitation seasonality, maximum humidity in the central Mediterranean during the middle part of the Holocene was characterised by humid winters and dry summers north of ca. 40° N, and humid winters and summers south of ca. 40° N. This may explain an apparent conflict between palaeoclimatic records depending on the proxies used for reconstruction as well as the synchronous expansion of tree species taxa with contrasting climatic requirements. In addition, south of ca. 40° N, the first millennium of the Holocene was characterised by very dry climatic conditions not only in the eastern, but also in the central- and the western Mediterranean zones as reflected by low lake levels and delayed reforestation. These results suggest that, in addition to the influence of the Nile discharge reinforced by the African monsoon, the deposition of Sapropel 1 has been favoured (1) by an increase in winter precipitation in the northern Mediterranean borderlands, and (2) by an increase in winter and summer precipitation in the southern Mediterranean area. The climate reversal following the Holocene climate optimum appears to have been punctuated by two major climate changes around 7500 and 4500 cal BP. In the central Mediterranean, the Holocene palaeohydrological changes developed in response to a combination of orbital, ice-sheet and solar forcing factors. The maximum humidity interval in the south-central Mediterranean started ca. 10 300 cal BP, in correlation with the decline (1) of the possible blocking effects of the North Atlantic anticyclone linked to maximum insolation, and/or (2) of the influence of the remnant ice sheets and fresh water forcing in the North Atlantic Ocean. In the north-central Mediterranean, the lake-level minimum interval began only around 9000 cal BP when the Fennoscandian ice sheet disappeared and a prevailing positive NAO-(North Atlantic Oscillation) type circulation developed in the North Atlantic area. The major palaeohydrological oscillation around 4500–4000 cal BP may be a non-linear response to the gradual decrease in insolation, with additional key seasonal and interhemispheric changes. On a centennial scale, the successive climatic events which punctuated the entire Holocene in the central Mediterranean coincided with cooling events associated with deglacial outbursts in the North Atlantic area and decreases in solar activity during the interval 11 700–7000 cal BP, and to a possible combination of NAO-type circulation and solar forcing since ca. 7000 cal BP onwards. Thus, regarding the centennial-scale climatic oscillations, the Mediterranean Basin appears to have been strongly linked to the North Atlantic area and affected by solar activity over the entire Holocene. In addition to model experiments, a better understanding of forcing factors and past atmospheric circulation patterns behind the Holocene palaeohydrological changes in the Mediterranean area will require further investigation to establish additional high-resolution and well-dated records in selected locations around the Mediterranean Basin and in adjacent regions. Special attention should be paid to greater precision in the reconstruction, on millennial and centennial timescales, of changes in the latitudinal location of the limit between the northern and southern palaeohydrological Mediterranean sectors, depending on (1) the intensity and/or characteristics of climatic periods/oscillations (e.g. Holocene thermal maximum versus Neoglacial, as well as, for instance, the 8.2 ka event versus the 4 ka event or the Little Ice Age); and (2) on varying geographical conditions from the western to the eastern Mediterranean areas (longitudinal gradients). Finally, on the basis of projects using strategically located study sites, there is a need to explore possible influences of other general atmospheric circulation patterns than NAO, such as the East Atlantic–West Russian or North Sea–Caspian patterns, in explaining the apparent complexity of palaeoclimatic (palaeohydrological) Holocene records from the Mediterranean area.

Abstract Riparian vegetation responds to hydrogeomorphic disturbances and environmental changes and also controls these changes. Here, we propose that the control of sediment erosion and deposition by riparian vegetation is a key geomorphological and ecological (i.e. biogeomorphic) function within fluvial corridors. In a 3 year study, we investigated the correlations between riparian vegetation and hydrogeomorphic dynamics along a transverse gradient from the main channel to the floodplain of the River Tech, France. Sediment erosion and deposition rates varied significantly along the transverse gradient as a function of the vegetation biovolume intercepting water flow. These effects, combined with the extremely strong mechanical resistance of pioneer woody structures and strong resilience of pioneer labile herbaceous communities, Populus nigra and Salix spp., explain the propensity of biogeomorphic succession (i.e. the synergy between vegetation succession and landform construction) to progress between destructive floods. This geomorphological function newly identified as an ‘ecosystem function’ per se encompasses the coupling of habitat and landform creation, maintenance and change with fundamental ecosystem structural changes in space and in time. Three different biogeomorphic functions, all related to the concept of ecosystem engineering, were identified: (i) the function of pioneer herbaceous communities to retain fine sediment and diaspores in the exposed zones of the active tract near the water resource, facilitating recruitment of further herbaceous and Salicacea species; (ii) the function of woody vegetation to drive the construction of forested islands and floodplains; and (iii) the function of stabilised riparian forests to act as ‘diversity reservoirs’ which can support regeneration after destructive floods. Overall, this study based on empirical data points to the fundamental importance of sediment flow control by pioneer riparian vegetation in defining fluvial ecosystem and landform organisation in time and in space. Copyright © 2009 John Wiley & Sons, Ltd.

EuroRotaNet, a laboratory network, was established in order to determine the diversity of co-circulating rotavirus strains in Europe over three or more rotavirus seasons from 2006/2007 and currently includes 16 countries. This report highlights the tremendous diversity of rotavirus strains co-circulating in the European population during three years of surveillance since 2006/2007 and points to the possible origins of these strains including genetic reassortment and interspecies transmission. Furthermore, the ability of the network to identify strains circulating with an incidence of ≥1% allowed the identification of possible emerging strains such as G8 and G12 since the beginning of the study; analysis of recent data indicates their increased incidence. The introduction of universal rotavirus vaccination in at least two of the participating countries, and partial vaccine coverage in some others may provide data on diversity driven by vaccine introduction and possible strain replacement in Europe.

By documenting how humans adapted to changes in their environment that are often much greater than those experienced in the instrumental record, archaeology provides our only deep-time laboratory for highlighting the circumstances under which humans managed or failed to find to adaptive solutions to changing climate, not just over a few generations but over the longue durée Patterning between climate-mediated environmental change and change in human societies has, however, been murky because of low spatial and temporal resolution in available datasets, and because of failure to model the effects of climate change on local resources important to human societies. In this paper we review recent advances in computational modeling that, in conjunction with improving data, address these limitations. These advances include network analysis, niche and species distribution modeling, and agent-based modeling. These studies demonstrate the utility of deep-time modeling for calibrating our understanding of how climate is influencing societies today and may in the future.

ABSTRACT Riverine ecosystems are recurrently rejuvenated during destructive flood events and vegetation succession starts again. Poplars (i.e. species from Populus genera) respond to hydrogeomorphological constraints, but, in turn, also influence these processes. Thus, poplar development on bare mineral substrates is not exclusively a one‐way vegetative process. Reciprocal interactions and adjustments between poplar species and sediment dynamics during their life cycle lead to the emergence of biogeomorphological entities within the fluvial corridor, such as vegetated islands, benches and floodplains. Based on a review of geomorphological, biological and ecological literature, we have identified and described the co‐constructing processes between riparian poplars and their fluvial environment. We have explored the possibility that the modification of the hydrogeomorphological environment exerted, in particular, by the European black poplar ( Populus nigra L.), increases its fitness and thus results in positive niche construction. We focus on the fundamental phases of dispersal, recruitment and establishment until sexual maturity of P . nigra by describing the hierarchy of interactions and the pattern of feedbacks between biotic and abiotic components. We explicitly relate the biological life cycle of P . nigra to the fluvial biogeomorphic succession model by referring to the ‘biogeomorphological life cycle’ of P . nigra . Finally, we propose new research perspectives based on this theoretical framework. Copyright © 2014 John Wiley & Sons, Ltd.

Abstract Little Ice Age lateral moraines represent one of the most important sediment storages and dynamic areas in glacier forelands. Following glacier retreat, simultaneous paraglacial adjustment and vegetation succession affect the moraine slopes. Geomorphic processes (e.g. debris flows, interrill erosion, gullying, solifluction) disturb and limit vegetation development, while increasing vegetation cover decreases geomorphic activity. Thus, feedbacks between geomorphic and vegetation dynamics strongly control moraine slope development. However, the conditions under which these biogeomorphic feedbacks can occur are insufficiently understood and major knowledge gaps remain. This study determines feedback conditions through the analysis of geomorphic and vegetation data from permanent plots in the Turtmann glacier foreland, Switzerland. Results from multivariate statistical analysis (i) confirm that Dryas octopetala L. is an alpine ecosystem engineer species which influences geomorphic processes on lateral moraines and thereby controls ecosystem structure and function, and (ii) demonstrate that biogeomorphic feedbacks can occur once geomorphic activity sufficiently decreases for D. octopetala to establish and cross a cover threshold. In the subsequent ecosystem engineering process, the dominant geomorphic processes change from flow and slide to bound solifluction. Increasing slope stabilization induces a decline in biogeomorphic feedbacks and the suppression of D. octopetala by shrubs. We conceptualize this relationship between process magnitude, frequency and species resilience and resistance to disturbances in a ‘biogeomorphic feedback window’ concept. Our approach enhances the understanding of feedbacks between geomorphic and alpine vegetation dynamics on lateral moraine slopes and highlights the importance of integrating geomorphic and ecological approaches for biogeomorphic research. Copyright © 2015 John Wiley & Sons, Ltd.

In the post-Soviet space, Georgia and Ukraine are broadly perceived as exceptions to the growing authoritarianism in the region owing to the far-reaching political changes triggered by the so-called Colour Revolutions a decade ago. This article examines Russia's reaction to political changes in Georgia and Ukraine in light of the interplay between the democracy-promotion policies implemented by the EU and US and domestic patterns of democratization. We argue that despite the relatively weak impact of EU and US policies vis-à-vis domestic structures, Russia has responded harshly to (what it perceives as) a Western expansionist agenda in pursuit of reasserting its own hegemonic position in the post-Soviet space. However, coercive pressure from Russia has also unintended, counterproductive effects. We argue that the pressure has actually made Georgia and Ukraine more determined to pursue their pro-Western orientation and has spawned democratization, thereby supporting the objectives of the Western democracy promoters.

Résumé Cet article envisage, à l’échelle de la France, les interrelations entre l’agriculture, les nouvelles fonctions de l’espace rural et l’organisation territoriale. Face aux profondes mutations des campagnes et alors que les recherches des géographes se sont partiellement détournées de la composante agraire puis agricole, quelle est aujourd’hui la place – économique, mais aussi sociale ou culturelle – de l’agriculture ? L’article décline les trois facettes de la territorialisation, dé-territorialisation et re-territorialisation de l’agriculture ; ce dernier processus profitant de l’engouement pour les produits de qualité liés aux terroirs, des soucis de protection de l’environnement, de la « mise en patrimoine » des campagnes et de leurs paysages, ainsi que des nouvelles « politiques de projet » des territoires institutionnels recomposés. L’étude s’achève par une lecture des grands modèles de développement « agri-ruraux » voire « agri-urbains ».

International audience

Abstract Cuwabo (Bantu P34, Mozambique) illustrates a relativization strategy, also attested in some North-Western and Central Bantu languages, whose most salient characteristics are that: (a) the initial agreement slot of the verb form does not express agreement with the subject (as in independent clauses), but agreement with the head noun; (b) the initial agreement slot of the verb form does not express agreement in person and number-gender (or class), but only in number-gender; (c) when a noun phrase other than the subject is relativized, the noun phrase encoded as the subject in the corresponding independent clause occurs in post-verbal position and does not control any agreement mechanism. In this article, we show that, in spite of the similarity between the relative verb forms of Cuwabo and the corresponding independent verb forms, and the impossibility of isolating a morphological element analyzable as a participial formative, the relative verb forms of Cuwabo are participles, with the following two particularities: they exhibit full contextual orientation, and they assign a specific grammatical role to the initial subject, whose encoding in relative clauses coincides neither with that of subjects of independent verb forms, nor with that of adnominal possessors.

Résumé Cet article se propose de comparer la manière dont la question de la reconnaissance du travail est posée dans le modèle de Honneth et dans la psychodynamique de travail. Même si la question du travail a toujours été centrale chez Honneth, elle n’a pas toujours occupé le premier plan de sa réflexion, et elle a été envisagée selon différents points de vue au cours de son évolution intellectuelle. C’est ce cheminement qu’on se propose, dans un premier temps, de retracer afin de fixer les termes de la comparaison. Mais le modèle d’Honneth a également été utilisé de différentes manière par des sociologues du travail et, sur ce point aussi, la confrontation avec la psychodynamique du travail mériterait d’être développée, comme on s’emploie à le suggérer dans un second temps.

Abstract Given the common intuition that consonant lenition occurs more often than fortition, we formulate this as a hypothesis, defining these sound change types in terms of decrease or increase in oral constriction. We then test the hypothesis on allophonic processes in a diverse sample of 81 languages. With the hypothesis confirmed, we examine the input and output of such sound changes in terms of manner and place of articulation and find that while decrease in oral constriction (weakening) affects most consonant types, increase in oral constriction (strengthening) is largely restricted to palatal and labial glides. We conclude that strengthening does not appear to be the simple inverse of weakening. In conclusion we suggest some possible avenues for explaining how glide strengthening may result from articulatory production pressures and speculate that strengthening and weakening can be encompassed under a single theory of sound change resulting from the automatization of production.

:The effects of floods on the radial growth of Populus tremula L. and Quercus robur L. in past decades were studied on a forested island in the Saône River (France). The study considered two stands including both tree species, located above and below the altitude of 169 m, which corresponds to the altitude reached by major river floods. Only the Populus trees closest to water showed a significant growth reduction (narrow rings) in response to recent floods. The reaction of Quercus to prolonged flooding was reflected in the size and distribution of vessels in annual rings. Rings formed in years when trees were flooded have a larger porous zone, including homogeneous small vessels forming a wide earlywood zone. Since 1980, the Saône River floods have shifted from late-winter - early-spring to late-spring flood events (March-April and even early June). Late floods of large magnitude and duration, as in 1983, 1986 and 1989, had precedents only in the 19th century (1856). We hypothesize that such major floods were produced by minor changes in regional atmospheric circulation which favor a higher frequency of rain events of Atlantic influence. Tree-ring signatures of flooded trees are therefore narrow rings in Populus and anomalous structure of porous earlywood in Quercus.

This study overlaps with Johnson’s (1987) ideas about the image schemas underlying thought, but rather than grasping them through the deductive analysis of verbal metaphors, they are approached here through the analysis of the symbolic components of gestures which, accompanying speech, refer to abstract entities. The corpus analyzed was compiled from six television interviews with the French Prime Minister, Lionel Jospin. The interviews averaged thirty minutes and took place over a one-year period. Only symbolic variations along the transverse axis, which is both symmetrical and oriented, are studied. The transverse axis appears to encompass several symbolic axes: a value axis, a spatio-temporal axis, and a logico-temporal axis, themselves derived from the axes of physical progression, which are growth, walking, and writing. A fourth, two-directional symbolic axis depicting an evolving process is added to the above. Successive translations of the upward and forward axes on to the rightward axis, achieved for contextual or ergonomic reasons, are mentally possible, since all three are axes of physical progression. This projection on to the side-toside axis accounts for the semiologically motivated complexity of the symbolic system represented on this major axis.

International audience

AIM: To study the impact of assimilable nitrogen, biotin and their interaction on growth, fermentation rate and volatile formation by Saccharomyces. METHODS AND RESULTS: Fermentations of synthetic grape juice media were conducted in a factorial design with yeast assimilable nitrogen (YAN) (60 or 250 mg l(-1)) and biotin (0, 1 or 10 microg l(-1)) as variables. All media contained 240 g l(-1) glucose + fructose (1 : 1) and were fermented using biotin-depleted Saccharomyces cerevisiae strains EC1118 or UCD 522. Both strains exhibited weak growth and sluggish fermentation rates without biotin. Increased nitrogen concentration resulted in higher maximum fermentation rates, while adjusting biotin from 1 to 10 microg l(-1) had no effect. Nitrogen x biotin interactions influenced fermentation time, production of higher alcohols and hydrogen sulfide (H(2)S). Maximum H(2)S production occurred in the medium containing 60 mg l(-1) YAN and 1 microg l(-1) biotin. CONCLUSIONS: Nitrogen x biotin interactions affect fermentation time and volatile production by Saccharomyces depending on strain. Biotin concentrations sufficient to complete fermentation may affect the organoleptic impact of wine. SIGNIFICANCE AND IMPACT OF THE STUDY: This study demonstrates the necessity to consider nutrient interactions when diagnosing problem fermentations.

Disturbances fundamentally alter ecosystem functions, yet predicting their impacts remains a key scientific challenge. While the study of disturbances is ubiquitous across many ecological disciplines, there is no agreed-upon, cross-disciplinary foundation for discussing or quantifying the complexity of disturbances, and no consistent terminology or methodologies exist. This inconsistency presents an increasingly urgent challenge due to accelerating global change and the threat of interacting disturbances that can destabilize ecosystem responses. By harvesting the expertise of an interdisciplinary cohort of contributors spanning 42 institutions across 15 countries, we identified an essential limitation in disturbance ecology: the word ‘disturbance’ is used interchangeably to refer to both the events that cause, and the consequences of, ecological change, despite fundamental distinctions between the two meanings. In response, we developed a generalizable framework of ecosystem disturbances, providing a well-defined lexicon for understanding disturbances across perspectives and scales. The framework results from ideas that resonate across multiple scientific disciplines and provides a baseline standard to compare disturbances across fields. This framework can be supplemented by discipline-specific variables to provide maximum benefit to both inter- and intra-disciplinary research. To support future syntheses and meta-analyses of disturbance research, we also encourage researchers to be explicit in how they define disturbance drivers and impacts, and we recommend minimum reporting standards that are applicable regardless of scale. Finally, we discuss the primary factors we considered when developing a baseline framework and propose four future directions to advance our interdisciplinary understanding of disturbances and their social-ecological impacts: integrating across ecological scales, understanding disturbance interactions, establishing baselines and trajectories, and developing process-based models and ecological forecasting initiatives. Our experience through this process motivates us to encourage the wider scientific community to continue to explore new approaches for leveraging Open Science principles in generating creative and multidisciplinary ideas.

Abstract This paper evaluates the paraglacial evolution of a sediment‐mantled slope in a polar maritime environment. The intensity of paraglacial processes is estimated through quantification of erosion and dating of field sectors with the help of photographic archives. Gully erosion has been estimated using morphometric parameters and by surveys of vegetation cover. The rapid melting of dead‐ice cores controls gully formation. This leads to slope form modification: gully profile gradients are reduced from a mean of 35° to a mean ranging between 10° and 15°. Profile evolution results from the collapse of glacier lateral moraine. All data (mean slope angle of individual gullies, frequency distribution of slope angles, fractional distance to the apex, gullying index, volume of debris mobilized, vertical erosion rate) tend to increase with increasing deglaciation age and the duration of paraglacial activity. Vegetation colonization is a response to stabilization of the ground surface and the drying up of the ground surface due to dead‐ice melting. The full sequence of paraglacial slope adjustment (gully incision‐stabilization) may occur rapidly at the study site, i.e. within two decades. Finally, a lateral morphogenic sequence is proposed showing the importance of paraglacial processes at the onset of the deglaciation. Copyright © 2009 John Wiley & Sons, Ltd.

Hepatitis C virus (HCV) is a blood-borne pathogen that has a worldwide distribution and infects millions of people. Care-associated HCV infections represented a huge part of hepatitis C burden in the past via contaminated blood and unsafe injections and continue to be a serious problem of public health. The present review proposes a panorama of health care-associated HCV infections via the three mode of contamination that have been identified: (1) infected patient to non-infected patient; (2) infected patient to non-infected health care worker (HCW); and (3) infected HCW to non infected patient. For each condition, the circumstances of contamination are described together with the means to prevent them. As a whole, the more important risk is represented by unsafe practices regarding injections, notably with the improper use of multidose vials used for multiple patients. The questions of occupational exposures and infected HCWs are also discussed. In terms of prevention and surveillance, the main arm for combating care-associated HCV infections is the implementation of standard precautions in all the fields of cares, with training programs and audits to verify their good application. HCWs must be sensitized to the risk of blood-borne pathogens, notably by the use of safety devices for injections and good hygiene practices in the operating theatre and in all the invasive procedures. The providers performing exposed-prone procedures must monitor their HCV serology regularly in order to detect early any primary infection and to treat it without delay. With the need to stay vigilant because HCV infection is often a hidden risk, it can be hoped that the number of people infected by HCV via health care will decrease very significantly in the next years.

Deleuze plonge la critique kantienne transcendantale dans le bain dissolvant d'un empirisme renouvelé. Ce livre se propose de restituer cette entreprise, et d'analyser l'étonnante création de ce concept, que Deleuze mène depuis ses premières monographies (1953) jusqu'à "Différence et Répétition" (1968) dans un dialogue fécond avec l'histoire de la philosophie. Par quelles opérations de distortion et de collage, Deleuze compose-t-il l'empirisme de Hume, la théorie du signe comme force de Nietzsche, le virtuel et les multiplicités de Bergson, les modes de Spinoza, les individualisations impersonnelles de Simondon pour renouveler la théorie kantienne du transcendantal ? C'est tout l'objet de cette enquête, qui permet d'entrer dans le laboratoire du penseur, pour saisir la philosophie se faisant, mais qui permet également d'expliquer l'insistance du transcendantal dans toute son œuvre.