Un horizon infini : paysage, expérience et savoir dans les voyages au Tibet de Jacques Bacot et des explorateurs français (1850-1912)

Résumé de la thèseCette étude repose sur un double constat initial : en premier lieu, les récits français d'explorationau Tibet de la période s'étendant de 1850 à 1912 relèvent d'une tradition particulière du voyagescientifique en partie irréductible aux traditions des autres nations impérialistes de la mêmeépoque, notamment la tradition britannique à laquelle on les a souvent assimilés. En second lieu,ces récits révèlent à la fois la place centrale dégagée à la description du paysage tibétain et uneévolution unique et originale des savoirs et des représentations qui lui sont liés.Ce travail montre la rapide évolution des images du Tibet que s'est façonnées l'Europe,l'interrelation de cette histoire des représentations avec une révision des connaissances sur laterre et l'homme dans les sciences du XIXe siècle, ainsi qu'une dimension différentielle entre lesobjectifs de connaissance émanant des explorateurs français et anglais, différence due à uncontexte géopolitique hétérogène. Sur le fond de cette démarche contextualisante, le recours àl'analyse textuelle met en évidence le rôle qu'ont joué les explorateurs français dans l'histoire dessavoirs sur le Tibet.Pour des raisons inhérentes à la qualité d'écriture de ses récits et à l'acuité remarquable de sonapproche du monde tibétain, une place centrale de ce travail a été ménagée à Jacques Bacot(voyages de 1906 à 1907 - Dans les Marches tibétaines - et de 1909 à 1910 - Le Tibet révolté). Il a dèslors été fructueux de replacer ses récits dans l'histoire des savoirs et des représentations du Tibetet de les comparer aux récits majeurs d'autres explorateurs français au Tibet comme GabrielBonvalot, Fernand Grenard et Henri d'Ollone.Le paysage est une notion-clé pour comprendre le regard que portent les explorateurs sur leTibet. Or le paysage revêt des acceptions variables selon les auteurs et affiche des facettesdifférentes. Il a ainsi été possible de distinguer plusieurs dimensions : une dimension cognitive, unedimension épistémique, une dimension intersubjective et, enfin, une dimension imaginaire et sacrée. Cettedimension sacrée du paysage peut également être actualisée en tant que dimension écosymbolique.C'est là l'aboutissement des voyages de Bacot. L'explorateur, attentif à la culture tibétaine, envient à réaliser la valeur sacrée qui traverse la relation des Tibétains eux-mêmes à leurenvironnement. Le paysage ainsi compris se place au fondement d'une expérience partagée avecdes acteurs issus d'une autre culture et apparaît ainsi comme un opérateur privilégié pour« comprendre les compréhensions » (Clifford Geertz) des explorateurs, mais aussi, de proche enproche, des Tibétains.D'un point de vue épistémologique, la mise au jour de ces dimensions du paysage permetd'éviter certains écueils de la critique historienne et littéraire sur les récits de voyage au Tibet, quin'y a vu tantôt que de simples documents inertes, tantôt que le reflet d'un imaginaire purementet indéfectiblement occidental. La présente étude montre au contraire la part irréductiblequ'occupe la rencontre in situ avec l'autre et l'ailleurs dans l'élaboration conjointe desreprésentations et des savoirs.

Un horizon infini. Explorateurs et voyageurs français au Tibet (1846-1912)

Peu reconnus par la critique postcoloniale, souvent assimilés sans nuances aux enjeux géopolitiques du Grand Jeu en Asie centrale à la même période, les récits des explorateurs français du Tibet manifestent pourtant des traits culturels spécifiques dont on se propose ici de mener l'archéologie. Missionnaires, aventuriers, nobles bannis, scientifiques républicains, diplomates, officiers coloniaux, intellectuels et orientalistes éclairés indiquent tous que la culture de l'exploration dont, de 1846 à 1912, ils sont les représentants se conçoit intrinsèquement comme une culture paysagère. Aussi révèlent-ils une évolution originale des savoirs sur le Tibet et des représentations du paysage tibétain qui se découvre progressivement à eux. La description du paysage participe ainsi globalement d'une histoire des sensibilités et d'une histoire des sciences, ce que l'on peut appeler une géosensibilité. Mais la description scientifique du paysage, liée à la pratique du voyage et à une confrontation à l'ailleurs, ne doit pas masquer le primat expérientiel qui lui donne sens. C'est ainsi que le paysage, en tant qu'expérience vécue, en vient à jouer le rôle d'une médiation interculturelle invitant à un renouvellement des questionnaires des explorateurs. Par ailleurs, la description scientifique participe tout autant de différents orientalismes, de différentes perceptions d'un Tibet associé par les voyageurs à un « paysage sacré ». La diversité dont ceux-ci témoignent, mais aussi les croisements de représentations issues d'autres cultures de l'exploration du Tibet - la tradition anglo-saxonne en premier lieu -, nous plongent aux origines de l'« image du Tibet » qui, au loin de la rencontre vivante des explorateurs - la Première Guerre, la Convention de Simla et l'avènement du Guomindang marquent le terme de la culture française de l'exploration du Tibet -, se cristallisera et s'unifiera dans l'imaginaire occidental du XXe siècle.

Finite horizon bargaining and the consistent field

This paper explores the relationships between noncooperative bargaining games and the consistent value for non-transferable utility (NTU) cooperative games. A dynamic approach to the consistent value for NTU games is introduced: the consistent vector field. The main contribution of the paper is to show that the consistent field is intimately related to the concept of subgame perfection for finite horizon noncooperative bargaining games, as the horizon goes to infinity and the cost of delay goes to zero. The solutions of the dynamic system associated to the consistent field characterize the subgame perfect equilibrium payoffs of the noncooperative bargaining games. We show that for transferable utility, hyperplane and pure bargaining games, the dynamics of the consistent fields converge globally to the unique consistent value. However, in the general NTU case, the dynamics of the consistent field can be complex. An example is constructed where the consistent field has cyclic solutions; moreover, the finite horizon subgame perfect equilibria do not approach the consistent value.

The dark sides of capillary morphogenesis gene 2.

Capillary morphogenesis gene 2 (CMG2) is a type I membrane protein involved in the homeostasis of the extracellular matrix. While it shares interesting similarities with integrins, its exact molecular role is unknown. The interest and knowledge about CMG2 largely stems from the fact that it is involved in two diseases, one infectious and one genetic. CMG2 is the main receptor of the anthrax toxin, and knocking out this gene in mice renders them insensitive to infection with Bacillus anthracis spores. On the other hand, mutations in CMG2 lead to a rare but severe autosomal recessive disorder in humans called Hyaline Fibromatosis Syndrome (HFS). We will here review what is known about the structure of CMG2 and its ability to mediate anthrax toxin entry into cell. We will then describe the limited knowledge available concerning the physiological role of CMG2. Finally, we will describe HFS and the consequences of HFS-associated mutations in CMG2 at the molecular and cellular level.

The case for resequencing studies of Arabidopsis thaliana accessions: mining the dark matter of natural genetic variation.

Ultra-high-throughput sequencing (UHTS) techniques are evolving rapidly and may soon become an affordable and routine tool for sequencing plant DNA, even in smaller plant biology labs. Here we review recent insights into intraspecific genome variation gained from UHTS, which offers a glimpse of the rather unexpected levels of structural variability among Arabidopsis thaliana accessions. The challenges that will need to be addressed to efficiently assemble and exploit this information are also discussed.

Enhanced degradation of metalaxyl in Gley Humic and Dark Red Latosol

Enhanced degradation of the fungicide metalaxyl was investigated in two soils: a gley humic (GH) and a Dark Red Latosol (LE), collected at sites never exposed to the fungicide. The soil samples were treated with successive applications of metalaxyl as a commercial formulation and 14C-metalaxyl in laboratory. Metalaxyl biodegradation was analyzed during 63 days by means of radiometric techniques to verify biomineralization and degradation product formation from the applied 14C-metalaxyl. Although biomineralization (maximum of 14 and 8% in the GH and LE soils, respectively), and partial degradation (about 32 and 48%, respectively) were detected in both soils, enhanced degradation was verified only in the GH soil. Results proved that metalaxyl behaves differently in soils.

Surface and subsurface decomposition of a desiccated grass pasture biomass related to erosion and its prediction with RUSLE

Erosion is deleterious because it reduces the soil's productivity capacity for growing crops and causes sedimentation and water pollution problems. Surface and buried crop residue, as well as live and dead plant roots, play an important role in erosion control. An efficient way to assess the effectiveness of such materials in erosion reduction is by means of decomposition constants as used within the Revised Universal Soil Loss Equation - RUSLE's prior-land-use subfactor - PLU. This was investigated using simulated rainfall on a 0.12 m m-1 slope, sandy loam Paleudult soil, at the Agriculture Experimental Station of the Federal University of Rio Grande do Sul, in Eldorado do Sul, State of Rio Grande do Sul, Brazil. The study area had been covered by native grass pasture for about fifteen years. By the middle of March 1996, the sod was mechanically mowed and the crop residue removed from the field. Late in April 1996, the sod was chemically desiccated with herbicide and, about one month later, the following treatments were established and evaluated for sod biomass decomposition and soil erosion, from June 1996 to May 1998, on duplicated 3.5 x 11.0 m erosion plots: (a) and (b) soil without tillage, with surface residue and dead roots; (c) soil without tillage, with dead roots only; (d) soil tilled conventionally every two-and-half months, with dead roots plus incorporated residue; and (e) soil tilled conventionally every six months, with dead roots plus incorporated residue. Simulated rainfall was applied with a rotating-boom rainfall simulator, at an intensity of 63.5 mm h-1 for 90 min, eight to nine times during the experimental period (about every two-and-half months). Surface and subsurface sod biomass amounts were measured before each rainfall test along with the erosion measurements of runoff rate, sediment concentration in runoff, soil loss rate, and total soil loss. Non-linear regression analysis was performed using an exponential and a power model. Surface sod biomass decomposition was better depicted by the exponential model, while subsurface sod biomass was by the power model. Subsurface sod biomass decomposed faster and more than surface sod biomass, with dead roots in untilled soil without residue on the surface decomposing more than dead roots in untilled soil with surface residue. Tillage type and frequency did not appreciably influence subsurface sod biomass decomposition. Soil loss rates increased greatly with both surface sod biomass decomposition and decomposition of subsurface sod biomass in the conventionally tilled soil, but they were minimally affected by subsurface sod biomass decomposition in the untilled soil. Runoff rates were little affected by the studied treatments. Dead roots plus incorporated residues were effective in reducing erosion in the conventionally tilled soil, while consolidation of the soil surface was important in no-till. The residual effect of the turned soil on erosion diminished gradually with time and ceased after two years.

Broadening the horizon--level 2.5 of the HUPO-PSI format for molecular interactions.

BACKGROUND: Molecular interaction Information is a key resource in modern biomedical research. Publicly available data have previously been provided in a broad array of diverse formats, making access to this very difficult. The publication and wide implementation of the Human Proteome Organisation Proteomics Standards Initiative Molecular Interactions (HUPO PSI-MI) format in 2004 was a major step towards the establishment of a single, unified format by which molecular interactions should be presented, but focused purely on protein-protein interactions. RESULTS: The HUPO-PSI has further developed the PSI-MI XML schema to enable the description of interactions between a wider range of molecular types, for example nucleic acids, chemical entities, and molecular complexes. Extensive details about each supported molecular interaction can now be captured, including the biological role of each molecule within that interaction, detailed description of interacting domains, and the kinetic parameters of the interaction. The format is supported by data management and analysis tools and has been adopted by major interaction data providers. Additionally, a simpler, tab-delimited format MITAB2.5 has been developed for the benefit of users who require only minimal information in an easy to access configuration. CONCLUSION: The PSI-MI XML2.5 and MITAB2.5 formats have been jointly developed by interaction data producers and providers from both the academic and commercial sector, and are already widely implemented and well supported by an active development community. PSI-MI XML2.5 enables the description of highly detailed molecular interaction data and facilitates data exchange between databases and users without loss of information. MITAB2.5 is a simpler format appropriate for fast Perl parsing or loading into Microsoft Excel.

Quels nouveaux médicaments a l'horizon pour te traitement du cancer avancé de la prostate [New drugs at the horizon for men with prostate cancer]

Despite major progress in the understanding of biological mechanisms underlying metastatic prostate cancer, the treatment of men with advanced prostate cancer remains challenging. Several randomized controlled trials with promising or positive results are underway or just released. Here we discuss new treatments which might be used in clinic in the near future: hormonal treatments (Abiraterone and MDV3100), a new chemotherapy (Cabazitaxel), a cellular vaccine (Sipuleucel-T), anti-angiogenic drugs (Bevacizumab, Aflibercept), a new radioactive treatment (Alpharadin) and a new bone-protective agent (Deno-sumab).

Comparação de métodos para a observação de fungos micorrízicos arbusculares e endofíticos do tipo dark septate em espécies nativas de Cerrado

As espécies vegetais de Cerrado sensu stricto apresentam estratégias adaptativas às condições edáficas e climáticas de altos investimentos em fotoassimilados, nutrientes e água para sua estruturação. A simbiose entre fungos e raízes de plantas é uma importante adaptação radicular que auxilia as plantas na absorção de nutrientes e água do solo, sendo determinantes para a sobrevivência no Cerrado. Com o objetivo de estudar fungos micorrízicos arbusculares (FMAs) e fungos endofíticos do tipo dark septate (DSEFs) nas raízes de algumas espécies arbóreas e herbáceas, nativas do Cerrado sensu stricto, foram testados diferentes métodos para melhor observação das estruturas fúngicas em simbiose. O melhor método de clarificação foi observado quando as raízes foram autoclavadas a 121 °C em KOH 2 %, por 20 min, e com a subseqüente transferência para solução nova de KOH 2 %, por 24 h, em temperatura ambiente. Este procedimento foi repetido e, em seguida, essas amostras foram imersas em H2O2 2 % por 2 h. Os arbúsculos foram observados com maiores detalhes após a inclusão em resina, seccionamento e coloração com azul-de-toluidina. Todas as espécies avaliadas encontravam-se colonizadas por FMAs, e apenas em Xylopia aromatica não se observaram os DSEFs. As espécies herbáceas apresentaram maiores freqüências de colonização micorrízica do que as arbóreas. O caráter generalista dos FMAs e DSEFs observado nas espécies vegetais do Cerrado sensu stricto sugere a importância dessas simbioses como mecanismo adaptativo às condições de Cerrado.

Correction of soil acidity in the subsurface of an oxisol with sandy loam texture under no-tillage

In Rio Grande do Sul State (RS), Southern Brazil, aluminum saturation in many areas under no-till system is high and base saturation low in the 0.10-0.20 m layer (subsurface), which may reduce the grain yield of annual crops. The objective of this study was to evaluate if the occurrence of high aluminum saturation and low base saturation in the subsurface, under a no-till system, represents a restrictive environment for crop production, as well as to evaluate forms of lime incorporation for soil acidity correction in the subsurface. For this purpose, an experiment was carried out with soybean (2005/2006), corn (2006/2007), wheat (2007) and soybean (2007/2008) crops, in a Rhodic Hapludox (USDA, 1999) with sandy loam texture, under no-till for four years in the county of Tupanciretã (RS). The six treatments were: no-tillage with and without lime, plowing with and without lime, and chiseling with and without lime. The values of pH-H2O, aluminum saturation and base saturation were evaluated 24 months after treatment application in the layers 0-0.05; 0.05-0.10; 0.10-0.15; 0.15-0.20 and 0.20-0.30 m. The yields of soybean (2005/2006), corn (2006/2007), wheat (2007) and soybean (2007/2008) were evaluated. Soil acidity in the subsurface did not affect crop yield when the acidity in the layer from 0-0.10 m was at levels for which lime application is not recommended, according to CQFSRS/SC (2004). Lime incorporation through plowing was the most efficient way of correcting acidity at deeper levels.

Non-constant discounting in finite horizon: The free terminal time case

This paper derives the HJB (Hamilton-Jacobi-Bellman) equation for sophisticated agents in a finite horizon dynamic optimization problem with non-constant discounting in a continuous setting, by using a dynamic programming approach. A simple example is used in order to illustrate the applicability of this HJB equation, by suggesting a method for constructing the subgame perfect equilibrium solution to the problem.Conditions for the observational equivalence with an associated problem with constantdiscounting are analyzed. Special attention is paid to the case of free terminal time. Strotz¿s model (an eating cake problem of a nonrenewable resource with non-constant discounting) is revisited.

Spodosols pedogenesis under barreiras formation and sandbank environments in the south of Bahia

Morphologically differentiated Spodosols usually occur in the Coastal Plain of the South of Bahia and North of Espírito Santo. They are found in profiles known as "muçungas", i.e. sandy soils that accumulate water. In these areas, two kinds of Spodosols, different from those in the Restinga area, can be found: Spodosols with E albic horizon (white muçunungas) and without this horizon (black muçunungas). Eight soil profiles with spodic characteristics were collected and described in order to evaluate differences in the formation process of Barreiras and Restinga Spodosols in the South of Bahia. The soil profiles were also characterized chemically, physically and mineralogically. Additionally, texture and chemical analysis, Fe and Al extraction by sodium dithionite-citrate-bicarbonate (DBC), acid ammonium oxalate and sodium pyrophosphate, ammonium oxalate extract optic density (DOox), sulphuric acid attack, and X ray difractometry of the clay fraction were performed. In the Spodosols of the Barreiras area, fragipan was found the spodic layers. Cemented B spodic horizon were observed in the white muçunungas, and granular structure and dark color from the surface in the black muçunungas. There was no fragipan or hard spodic horizon in the Restinga Spodosol. This soil is acid, dystrophic and alic, with sandy texture and high clay percentages in the spodic horizons. The CEC, based on H + Al, is predominantly represented by the organic matter. The most representative components of the mineral phase of the clay fraction are kaolinite and possibly vermiculite traces with interlayered hydroxy. Chemical, physical, morphological and mineralogical differences were observed between the Barreiras and Restinga environments. The black and white muçunungas differ in morphologic and chemical properties only.