A festa nazi em Le Roi des Aulnes. De Michel Tournier: eu-foria e dis-foria

Sugerido para estes encontros interdisciplinares, o tema da Festa reenvia-nos para sentimentos de alegria e plenitude, para algo que traz ao quofidiano a abolição do tempo, uma centelha de renovação e etemidade, que podemos denominar de euforia. De acordo com a etimologia, a palavra foria deriva do grego (popeív e significa trazer, levar, carregar, ao passo que o prefixo eu, (et)) da mesma origem, quer dizer bem. Se juntarmos à mesma palavra, foria, o prefixo Ôya, também de origem grega, obteremos, o confrário de euforia, isto é, disforia que significa carregar mal-estar, dificuldade, desgraça. O romance de Michel Tournier, Le Roi des aulnes,^ que, segundo o autor, esteve para ser intitulado La phorie,^ organiza-se em tomo de núcleos temáticos relacionados com o sentido da palavra ^r/úf. No romance, a euforia é definida pela personagem principal como uma festa, «porter avec bonheur», mas a leitura mostra que euforia (eu-foria) e disforia (dis-foria) são dois estados reversíveis, podendo existir em simultâneo, e que a face de um pode ocultar a do outro.

Les plus anciens mammifères terrestres du Miocène marin de Lisbonne - le gisement du Km 10

For the first time, small mammals were found at the earliest marine level in the northeastern part of the lower Tagus basin, to the NE of Lisbon. At this new locality, at the 10 kilometer of the Lisbon-Oporto A1-IP1 highway,conglomerates yielded, along with marine fossils, more or less abraded teeth and bones from insectivores,lagomorphs, rodents and small artiodactyls (sec Tableau 1). Age may he ascribed to the lower Miocene, MN 2b Neogene mammal unit (about 22 My), but an early MN 3 age cannot be entirely excluded. That corresponds to latest Aquitanian (or less probably earliest Burdigalian) (sec Tableau 2). This is the first hitherto found locality with small mammals of this age as far as Portugal is concerned, as well as the oldest locality so far known in the Tagus basin. Km 10 is somewhat older than the localities of Universidade Católica and Avenida do Uruguay in Lisbon (ANTUNES & MEIN, 1986). Hence we can rather accurately date the age of the first marine transgression in the northeastern part of the lower Tagus basin. This shows that in this region there are no marine equivalents of the "Venus ribeiroi beds" (Aquitanian,Division 1 of the Lisbon Miocene series). Correlation between this unit and the uppermost levels of the essentially paleogene "Complexo de Benfica" may be possible. Fossils at km 10 point out to shallow, coastal, highenergy marine environments. Sedimentological features are compatible with this model. Dry land and swamps with brackish (or ev en fresh) waters were present nearby. From those areas came remains of mammals, crocodylians, as well as oysters and charophytes that were later transported to the sea. Sea was warmer than the extant Atlantic at the same latitudes, even if conditions were not strictly tropical then. These conditions surely influenced climate in the nearby regions. Ecological data concerning mammalian faunas distinctly point out to nearby forest-rich environments, much more so than for Universidade Católica and Avenida do Uruguay localities, from where drier, even steppe environment forms largely prevail.