Proximité à distance : les fonctions critiques de la mimêsis dans la pensée de Theodor W. Adorno

La présente thèse entend donner sens à un concept qui occupe une place centrale au sein de la pensée de Theodor W. Adorno mais qui, parce que notoirement difficile à définir, n’a pas reçu l’attention qu’il mérite : la mimêsis (Mimesis). Il s’agira, plus exactement, de comprendre la mimêsis comme un point nodal de la critique adornienne, qui nous permet de comprendre au nom et en vue de quoi elle se déploie. Car sous toutes ses acceptions – et nous verrons qu’elles sont fort variées – la mimêsis adornienne est toujours invoquée dans le but de contrecarrer les tendances hétéronomes (c’est-à-dire : déshumanisantes) propres aux sociétés capitalistes avancées. Surtout, elle est constamment présentée comme un correctif matérialiste au type de rationalité abstraite qui sous-tend ces sociétés. Cette tâche s’avère d’autant plus lourde que, malgré son important poids normatif, la mimêsis ne fait pas l’objet, chez Adorno, d’une théorisation explicite. Il nous faudra pallier cette indétermination, en identifiant d’abord les assises normatives les plus premières de la critique adornienne (0.0. Introduction : les fondements normatifs de la critique adornienne), pour ensuite rendre compte des fonctions particulières qu’occupe la mimêsis au sein de cette critique (1.0. Les fonctions critiques de la mimêsis adornienne). Ce travail de débroussaillage exégétique et interprétatif nous permettra de constater que la mimêsis adornienne recèle trois types de potentiels critiques distincts. D’abord, en ce qu’elle est présentée – dans les travaux des années 1930 et 1940 surtout – comme une impulsion psychosomatique à même de trahir, l’instant d’une brève résistance, la violence infligée à la nature intérieure et extérieure de l’homme par les forces réificatrices de la rationalité instrumentale (Instrumentelle Vernunft), la mimêsis adornienne peut être comprise comme un mimétisme (Mimikry) bioanthropologique dont la valeur est principalement expressive (2.O. Mimikry : le potentiel bioanthropologique de la mimêsis). Ensuite, lorsqu’elle sera pensée – à partir de la fin des années 50 surtout – comme une compétence proprement épistémique qui permet au sujet connaissant de rencontrer à nouveau puis de redéterminer les objets de son expérience, la mimêsis adornienne peut être comprise comme un correctif critique à la logique appropriative de la pensée identifiante (identifizierendes Denken) (3.O. Affinität et Entäusserung : le potentiel épistémique de la mimêsis). Enfin, dans la mesure où elle informe le modus operandi de l’oeuvre d’art d’avant-garde telle que défendue par Adorno dans la Théorie esthétique, et qui consiste à détourner, en les retournant contre elles-mêmes, les contraintes imposées par le monde totalement administré (total verwaltete Welt), la mimêsis peut être comprise comme une Methexis subversive, c’est-à-dire comme une stratégie séditieuse à même de conjurer l’hétéronomie sociale en l’anticipant et en l’incorporant (4.0. Methexis subversive : le potentiel stratégique de la mimêsis). Ainsi, tout en voulant rendre justice à la très grande polysémie du concept, nous aimerions démontrer que la mimêsis adornienne pointe constamment vers une forme ou une autre de résistance : comme expression, comme extériorisation ou comme subversion.

Solar radiation over and under sea ice during the POLARSTERN cruise ARK-XXVI/3 (TransArc) in summer 2011

Arctic sea ice has declined and become thinner and younger (more seasonal) during the last decade. One consequence of this is that the surface energy budget of the Arctic Ocean is changing. While the role of surface albedo has been studied intensively, it is still widely unknown how much light penetrates through sea ice into the upper ocean, affecting sea-ice mass balance, ecosystems, and geochemical processes. Here we present the first large-scale under-ice light measurements, operating spectral radiometers on a remotely operated vehicle (ROV) under Arctic sea ice in summer. This data set is used to produce an Arctic-wide map of light distribution under summer sea ice. Our results show that transmittance through first-year ice (FYI, 0.11) was almost three times larger than through multi-year ice (MYI, 0.04), and that this is mostly caused by the larger melt-pond coverage of FYI (42 vs. 23%). Also energy absorption was 50% larger in FYI than in MYI. Thus, a continuation of the observed sea-ice changes will increase the amount of light penetrating into the Arctic Ocean, enhancing sea-ice melt and affecting sea-ice and upper-ocean ecosystems.

Lithologic, mineral, chemical and isotopic compositions of altered rocks with increasing distance across the eastern flank of the Juan de Fuca Ridge, ODP Leg 168 data

During ODP Leg 168, 10 sites were drilled across the eastern flank of the Juan de Fuca Ridge (JdFR), to examine the conditions of fluid-rock interaction in three distinct hydrothermal regimes (referred to as the Hydrothermal Transition (HT), Buried Basement (BB) and Rough Basement (RB) transects), extending over a ~120 km linear transect perpendicular to the spreading ridge. This was carried out in an attempt to constrain the conditions and processes that control the location, style and magnitude of low temperature (<150°C) fluid-rock interaction within this setting. This paper presents new data on the petrology, mineral chemistry and whole rock strontium and oxygen isotopic compositions of basalts from the eastern flank of the JdFR, in order to investigate the extent, style and sequence of low-temperature hydrothermal alteration and to establish how the hydrothermal regime evolved with time. Throughout the flank, a progressive sequence of low-temperature hydrothermal alteration has been identified, marked by changes in the dominant secondary mineral assemblage, changing from: chlorite+chlorite/smectite; to iron oyxhydroxide+celadonite; to saponite+/-pyrite; culminating at present with Ca- to CaMg(+/-Fe,Mn)-carbonate. The changes in secondary mineralogy have been used to infer a series of systematic shifts in the conditions of alteration that occurred as the basement moved off-axis and was progressively buried by sediment. In general, hydrothermal alteration of the uppermost oceanic crust commenced under open, oxidative conditions, with interaction between unmodified to slightly modified seawater and basaltic crust, to a regime in which circulation of a strongly modified seawater-derived fluid was more restricted, and alteration occurred under non-oxidative conditions. Across the flank, petrological observations and microprobe analyses indicate that the observed ranges in secondary mineral composition are directly related to changes in the geochemical and textural characteristics of the basement, as well as to interaction between fluids and phases from the four stages of alteration. This is suggestive of an increase in fluid-rock increased with time. Whole rock 87Sr/86Sr and d18O analyses of basalts from across the eastern flank of the JdFR reinforce petrological observations, with 87Sr/86Sr and d18O values slightly elevated above accepted pristine MORB values for this region. These results are consistent with an increase in the amount of fluid-rock interaction with time. Across the flank, enrichment in the 87Sr/86Sr and d18O relative to MORB, is influenced by a number of factors, including: local and regional variations in the crustal lithology and structure; the age of the crust; the extent of bulk rock alteration; and theoretically, the relative abundance of different isotopically-enriched secondary mineral phases in the crust.

State Street. South West [southwest] Corner of Campus. Methodist Church in distance

Gentleman posing by lamppost

Sight distance requirements at lane closure work zones on urban freeways. Interim report.

Texas State Department of Highways and Public Transportation, Transportation Planning Division, Austin

Distance requirements for ramp metering.

Texas Department of Transportation, Austin

Repeatability of visibility tests. Final report.

National Highway Traffic Safety Administration, Washington, D.C.

Decision sight distance for highway design and traffic control requirements. Final report.

Federal Highway Administration, Office of Research, Washington, D.C.

Improved visibility for school buses during adverse weather - summary report. Final report.

National Highway Traffic Safety Administration, Washington, D.C.

Improved visibility for school buses during adverse weather - volume I. Final report.

National Highway Traffic Safety Administration, Washington, D.C.

Improved visibility for school buses during adverse weather - volume II: appendixes. Final report.

National Highway Traffic Safety Administration, Washington, D.C.