Scotus nouissime cum emendatissimo codice parisino castigatus : additis repo[n]sionibus ad argumenta locis suis, [et] annotationibus opinionum diuerso[rum] doctorum, ac etiam textuum co[m]mento[rum] Aristotelis in marginibus, nec no[n] textu magistri sent

Juan Duns Escoto, Beato, ca. 1266-1308. Scotus super secundo sententiarum. [Venetiis : Bonetus Locatellus, impens. Octauiani Scoti], 18 dic. 1497]. 84 h. : il. Sign.: A-K8, L4

RECONHECENDO-SE SEM-RELIGIÃO NAS PERIFERIAS DA CIDADE: LIBERDADE COMPARTILHADA COMO RESISTÊNCIA

Reconhecendo, a partir da constatação empírica, a multiplicidade de escolhas de crenças no Mundo e em particular na periferia urbana paulistana, reconhecemos, também, a emergência criativa de novas possibilidades de crer e não crer. Tal amplitude não apenas aponta para o crer (segundo as ofertas de um sem número de religiões) e o não crer (ateu e agnóstico), mas para uma escolha que poderia vir a ser silenciada e esquecida, neste binômio arcaico e obsoleto, quando alguém se dá à liberdade crer sem ter religião. Reconhecer interessadamente os sem-religião nas periferias urbanas paulistanas é dar-se conta das violências a que estes indivíduos estão submetidos: violência econômica, violência da cidadania (vulnerabilidade) e proveniente da armas (grupos x Estado). Tanto quanto a violência do esquecimento e silenciamento. A concomitância espaço-temporal dos sem-religião nas periferias, levou-nos buscar referências em teorias de secularização e de laicidade, e, a partir destas, traçar uma história do poder violento, cuja pretensão é a inelutabilidade, enquanto suas fissuras são abertas em espaços de resistências. A história da legitimação do poder que se quer único, soberano, de caráter universal, enquanto fragmenta a sociedade em indivíduos atomizados, fragilizando vínculos horizontais, e a dos surgimentos de resistências não violentas questionadoras da totalidade trágica, ao reconhecer a liberdade de ser com autonomia, enquanto se volta para a produção de partilha de bens comuns. Propomos reconhecer a igual liberdade de ser (expressa na crença da filiação divina) e de partilhar o bem comum em reconhecimentos mútuos (expressa pela ação social), uma expressão de resistência não violenta ao poder que requer a igual abdicação da liberdade pela via da fragmentação individualizante e submissão inquestionável à ordem totalizante. Os sem-religião nas periferias urbanas, nossos contemporâneos, partilhariam uma tal resistência, ao longo da história, com as melissas gregas, os profetas messiânicos hebreus, os hereges cristãos e os ateus modernos, cuja pretensão não é o poder, mas a partilha igual da liberdade e dos bens comuns. Estes laicos, de fato, seriam agentes de resistências de reconhecimento mútuos, em espaços de multiplicidade crescente, ao poder violento real na história.

Westerschelde, Netherlands and Belgium, ca. 1799 (Image 2 of 3) (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Reconnoissance du cours du Hont ou Wester Schelde (Escaut occidental) depuis Anwerpen (Anvers) jusqu'à l'embouchure, faite par ordre du Ministre de la marine et des colonies, en thermidor et fructidor, an VII, vendémiaire et brumaire, an VIII, par Beautemps-Beaupré; assisté des Cens. Daussy et Portier, et de Jh. Raoul. It was published ca. 1799. Scale [ca. 1:41,300]. Covers Westerschelde, Netherlands and Belgium, from Middelburg to Antwerp. This layer is image 2 of 3 total images of the three sheet source map, representing the center portion of the map. Map in French.The image inside the map neatline is georeferenced to the surface of the earth and fit to the RD_New (Rijksdriehoekstelsel), GCS Amersfoort coordinate system. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows coastal features such as rocks, channels, points, ports, coves, islands, flats, canals, and more. Includes also selected land features such as roads, towns, fortification, drainage, land cover, selected buildings, and more. Relief shown pictorially and with hachures. Depths shown by contours and soundings. Includes "Nota" and text with insigne of the Dépôt général de la marine.This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.

Westerschelde, Netherlands and Belgium, ca. 1799 (Image 3 of 3) (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Reconnoissance du cours du Hont ou Wester Schelde (Escaut occidental) depuis Anwerpen (Anvers) jusqu'à l'embouchure, faite par ordre du Ministre de la marine et des colonies, en thermidor et fructidor, an VII, vendémiaire et brumaire, an VIII, par Beautemps-Beaupré; assisté des Cens. Daussy et Portier, et de Jh. Raoul. It was published ca. 1799. Scale [ca. 1:41,300]. Covers Westerschelde, Netherlands and Belgium, from Middelburg to Antwerp. This layer is image 3 of 3 total images of the three sheet source map, representing the eastern portion of the map. Map in French.The image inside the map neatline is georeferenced to the surface of the earth and fit to the RD_New (Rijksdriehoekstelsel), GCS Amersfoort coordinate system. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows coastal features such as rocks, channels, points, ports, coves, islands, flats, canals, and more. Includes also selected land features such as roads, towns, fortification, drainage, land cover, selected buildings, and more. Relief shown pictorially and with hachures. Depths shown by contours and soundings. Includes "Nota" and text with insigne of the Dépôt général de la marine.This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.

Magdeburg, Germany, ca. 1740 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Magdeburgum, ducatus cognominis metropolis ad Albium : sub ditione regis Borussiae, bene munitum ac florens emporium, in quo Tribunal Provinciale, consistorium et camera constituta = Magdeburg, die Haupt Statt eines Herzogthums gleiches Nahmens an der Elb, dem König in Preussen zustaendig, eine wohl fortificierte und florisante Handel Statt in welcher die Magdeburgische Landes Regierung, Consistorium und Camer angelegt, verfetigt von Matthaeus Seutter, Ihro Röm. Kaijserl. Maj. geographo. It was published by M. Seutter ca. 1740. Scale [ca. 1:5,000]. Covers Magdeburg, Germany. Map in Latin and German. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Deutsches Hauptdreiecksnetz (DHDN) 3-degree Gauss-Kruger Zone 4 coordinate system. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as roads, drainage, built-up areas and selected buildings, fortifications, ground cover, and more. Relief shown pictorially. Includes also index and panorama view of Magdeburg.This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.

Ulm, Germany, ca. 1740 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Ulma memorabilis ac permunita libera Imperii Civitas ad Danubium, ubi Ilara et Blavus ei miscentur = Ulm eine considerable Freye Reichs Statt in Schwaben, wo die Flüsse Iler u. Blau in die Donau fallen, verfertigt durch Matthaeum Seutter, Seiner Kayserl. u. Königl. Cathol. Majest. Geogr. in Augspurg. It was published by Matthaeus Seutter, ca. 1740. Scale [ca. 1:4,300]. Covers Ulm, Germany. Map in Latin and German. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Deutsches Hauptdreiecksnetz (DHDN) 3-degree Gauss-Kruger Zone 3 coordinate system. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as roads, drainage, built-up areas and selected buildings, fortifications, ground cover, and more. Relief shown pictorially. Includes also index, text, and panorama of Ulm seen from the North East.This layer is part of a selection of digitally scanned and georeferenced historic maps from the Harvard Map Collection. These maps typically portray both natural and manmade features. The selection represents a range of originators, ground condition dates, scales, and map purposes.

(Table 1) 87Sr/86Sr and Sr/Ca ratios in foraminiferal calcite from DSDP Holes 3-21 and 39-357

The 87Sr/86Sr ratio of ancient seawater, as recorded in marine carbonates, is an important tracer of long-term variations in ocean chemistry (Burke et al., 1982, doi:10.1130/0091-7613(1982)10<516:VOSSTP>2.0.CO;2; Peterman et al., 1970, doi:10.1016/0016-7037(70)90154-7; Dasch and Biscaye, 1971, doi:10.1016/0012-821X(71)90164-6; Veizer and Compston, 1974, doi:10.1016/0016-7037(74)90099-4; Brass, 1976, doi:10.1016/0016-7037(76)90025-9). However, the Sr isotope balance of the oceans has been difficult to constrain; consequently, attempts to evaluate the temporal 87Sr/86Sr changes have been largely qualitative. To constrain the causes of these variations we have measured 87Sr/86Sr ratios in carefully cleaned unrecrystallized foraminifera from DSDP sites 21 and 357. The data presented here have been quantitatively modelled taking advantage of recent advances in understanding of the Sr geochemical cycle. They suggest that whereas hydrothermal fluxes and carbonate recycling are of major importance in defining the marine 87Sr/86Sr ratio, the major control over its variations through the Cenozoic has been changes in the isotope composition of Sr derived from the weathering of silicate rocks.