La donna diavolo nella grecia antica : Lamia, Circe, Empusa e le stagioni della vita umana

El objetivo de este trabajo es investigar la historia de la monstruosidad femenina en la literatura griega antigua para recuperar algunas estructuras arquetípicas de pensamiento que se ocupan de la antigua y moderna conciencia colectiva sobre el problema del mal, su naturaleza, sus razones y también su falta de razones. De este modo yo repasé las "vidas paralelas" de tres famosas mujeres fatales de la mitología clásica que, colocadas en puntos decisivos de árboles genealógicos horribles llenas de 'maldiciones genéticas', son capaces de formar un tríptico bien definido de "medallones" enmarcados por un fil rouge de la monstruosidad ininterrumpida. Paradigmático de la dialéctica ambigua entre hombre-mujer, bien-mal, víctima-verdugo, normalidad-desviación, y de las dinámicas incontrolables entre los crímenes y los castigos, miedos ancestrales y deseo de descubrimiento, demonios buenos y malos, los mitos de Lamia, Circe y Empusa destacan la atracción irracional que, en la cultura griega antigua, tan racionalista, las personificaciones femeninas del mal son imaginadas moviéndose, con el fin de influir en la conducta humana en las principales etapas de la vida

Organic facies of Cenozoic and Cretaceous sediments at DSDP Leg 80 Holes

The organic facies of Cenozoic sediments cored at DSDP Sites 548-551 along the Celtic Sea margin of the northern North Atlantic (Goban Spur) is dominated by terrestrially derived plant remains and charcoal. Similar organic facies also occur in the Lower and Upper Cretaceous sections at these sites. Mid-Cretaceous (uppermost Albian-Turonian) sediments at Sites 549-551, however, record two different periods of enrichment in organic material, wherein marine organic matter was mixed with terrestrial components. The earlier period is represented only in the uppermost Albianmiddle Cenomanian section at the most seaward site, 550. Here, dark laminated marly chalks rich in organic matter occur rhythmically interbedded with light-colored, bioturbated marly chalks poor in organic matter, suggesting that bottom waters alternated between oxidizing and reducing conditions. A later period of enrichment in organic material is recorded in the upper Cenomanian-Turonian sections at Sites 549 and 551 as a single, laminated black mudstone interval containing biogenic siliceous debris. It was deposited along the margin during a time of oxygen deficiency associated with upwelling-induced intensification and expansion of the mid-water oxygen-minimum layer. In both the earlier and later events, variations in productivity appear to have been the immediate cause of oxygen depletion in the bottom waters.