A percepção da ordem e a consciência do tempo em Mari no período Paleo-Babilónico (séc. XIX- XVIII a. C.)

O presente estudo tem como objectivo estudar as questões do tempo e da ordem no reino de Mari. A análise destas questões evidencia dois aspectos importantes: por um lado, a convergência de duas culturas distintas – uma cultura acádica, tipicamente mesopotâmica, e uma cultura amorrita, mais ocidental – num mesmo espaço e, por outro lado, a importância do reino de Mari como um estudo de caso que retrata, por vezes com grande pormenor, a influência da penetração dos povos nómadas nas terras da Mesopotâmia e as suas repercussões nos vários domínios da vida pública. Estudar a ordem implica compreender a organização do mundo e da sociedade, bem como a relação entre as esferas humana e celeste. Estudar o tempo implica, por sua vez, entender como o homem se posiciona no espaço, como entende a sua história e o seu destino. Uma análise focada nestes dois temas permitir-nos-á, pois, compreender qual era o verdadeiro sentido da vida e do mundo para o homem de Mari. Como veremos, para o mariota, a vida assentava numa intensa dinâmica na qual a família detinha o papel principal: era ela que o enquadrava na sociedade, que lhe permitia participar nos destinos da vida pública e receber as devidas honras após a morte. Nesta perspectiva, a família e os laços de sangue adquiriam um papel preponderante em vários domínios da vida humana. Eram os laços consanguíneos que imperavam aquando da escolha de aliados e partidários. Por outro lado, o culto do parentesco impunha uma visão da história segundo a qual o tempo passado se afirmava como o grande modelo teórico das acções desenvolvidas no quotidiano (no presente). Paralelamente à família, o homem de Mari acreditava que no mundo divino residia a sua verdadeira esperança de levar uma vida feliz. A imagem de uma teocracia, onde homem e deus partilhavam o mesmo destino, é transversal a todo o pensamento e acção do homem de Mari. Nesta tese, propomos desenvolver um estudo de conjunto, uma análise transversal que abranja todos os aspectos da vida social e humana: a religião, a política, a cultura e a sociedade

Critical reappraisal of Late Mesozoic-Cenozoic Central and North Atlantic, Caribbean and Mediterranean evolution

(l) The Pacific basin (Pacific area) may be regarded as moving eastwards like a double zip fastener relative to the continents and their respective plates (Pangaea area): opening in the East and closing in the West. This movement is tracked by a continuous mountain belt, the collision ages of which increase westwards. (2) The relative movements between the Pacific area and the Pangaea area in the W-E/E-W direction are generated by tidal forces (principle of hypocycloid gearing), whereby the lower mantle and the Pacific basin or area (Pacific crust = roof of the lower mantle?) rotate somewhat faster eastwards around the Earth's spin axis relative to the upper mantle/crust system with the continents and their respective plates (Pangaea area) (differential rotation). (3) These relative West to East/East to West displacements produce a perpetually existing sequence of distinct styles of opening and closing ocean basins, exemplified by the present East to West arrangement of ocean basins around the globe (Oceanic or Wilson Cycle: Rift/Red Sea style; Atlantic style; Mediterranean/Caribbean style as eastwards propagating tongue of the Pacific basin; Pacific style; Collision/Himalayas style). This sequence of ocean styles, of which the Pacific ocean is a part, moves eastwards with the lower mantle relative to the continents and the upper-mantle/crust of the Pangaea area. (4) Similarly, the collisional mountain belt extending westwards from the equator to the West of the Pacific and representing a chronological sequence of collision zones (sequential collisions) in the wake of the passing of the Pacific basin double zip fastener, may also be described as recording the history of oceans and their continental margins in the form of successive Wilson Cycles. (5) Every 200 to 250 m.y. the Pacific basin double zip fastener, the sequence of ocean styles of the Wilson Cycle and the eastwards growing collisional mountain belt in their wake complete one lap around the Earth. Two East drift lappings of 400 to 500 m.y. produce a two-lap collisional mountain belt spiral around a supercontinent in one hemisphere (North or South Pangaea). The Earth's history is subdivided into alternating North Pangaea growth/South Pangaea breakup eras and South Pangaea growth/North Pangaea breakup eras. Older North and South Pangaeas and their collisional mountain belt spirals may be reconstructed by rotating back the continents and orogenic fragments of a broken spiral (e.g. South Pangaea, Gondwana) to their previous Pangaea growth era orientations. In the resulting collisional mountain belt spiral, pieced together from orogenic segments and fragments, the collision ages have to increase successively towards the West. (6) With its current western margin orientated in a West-East direction North America must have collided during the Late Cretaceous Laramide orogeny with the northern margin of South America (Caribbean Andes) at the equator to the West of the Late Mesozoic Pacific. During post-Laramide times it must have rotated clockwise into its present orientation. The eastern margin of North America has never been attached to the western margin of North Africa but only to the western margin of Europe. (7) Due to migration eastwards of the sequence of ocean styles of the Wilson Cycle, relative to a distinct plate tectonic setting of an ocean, a continent or continental margin, a future or later evolutionary style at the Earth's surface is always depicted in a setting simultaneously developed further to the West and a past or earlier style in a setting simultaneously occurring further to the East. In consequence, ahigh probability exists that up to the Early Tertiary, Greenland (the ArabiaofSouth America?) occupied a plate tectonic setting which is comparable to the current setting of Arabia (the Greenland of Africa?). The Late Cretaceous/Early Tertiary Eureka collision zone (Eureka orogeny) at the northern margin of the Greenland Plate and on some of the Canadian Arctic Islands is comparable with the Middle to Late Tertiary Taurus-Bitlis-Zagros collision zone at the northern margin of the Arabian Plate.