Sodoma, del Viejo al Nuevo Mundo

Las primeras obras historiográficas castellanas que relatan la “Conquista” de América ofrecen una de las mejores vías para comprender los discursos, religiosos y políticos, en torno a la sexualidad europea a fines de la Edad Media, especialmente relevante si analizamos las representaciones de la sodomía y del homoerotismo. A partir de textos de Bernal Díaz del Castillo, Bernardino de Sahagún, Gonzalo Fernández de Oviedo y Bartolomé de Las Casas, en este artículo se reflexiona sobre las significaciones de Sodoma (como geografía cultural e ideológica) en el contexto ibérico posterior a la “Reconquista”.

Palabras y actitudes de mujeres de la Cataluña bajomedieval ante las violencias e injusticias

En la documentación catalana bajo-medieval abundan los testimonios de mujeres maltratadas, mujeres de todas las edades que sufrían vejaciones y palizas de los hombres que tenían a su alrededor: padres, abuelos, maridos, etc. En este artículo, nos hemos fijado, sobre todo en la documentación judicial y los reque-rimientos notariales, para seguir la pista, no solo a los malos tratos que padecieron algunas muje-res, sino también a las actitudes que adoptaron ante tales agresiones. A través de las diferentes etapas de la vida de las mujeres, se analizan las circunstancias de los malos tratos que sufrían: desde los esponsales de matrimonios forzosos hasta la viudedad y las segundas nupcias.

Molluscan radiations and landscape evolution in Miocene Amazonia

This PhD study aims to exploit the rich archive provided by the Miocene mollusc fauna of the Pebas Formation and other inland Miocene Amazonian formations to reconstruct landscape evolution and biotic development in lowland Amazonia during the Neogene. Over 160 samples from more than 70 Pebas Formation outcrops mostly collected by the author were processed for this study. Additional samples were collected in Andean areas of Colombia and Venezuela and further material from other northwestern South American basins was studied in museums. Pebas Formation samples and well log data made available by Occidental Peru from three wells in the Marañon Basin in Peru were also investigated. During this study four genera and 74 species from the Pebas Formation have been described and a further 13 species have been introduced in open nomenclature, and several species were reported for the first time. The number of mollusc species attributed to the Pebas fauna has increased from around 50 to 156. The Pebas fauna is characterised as aquatic, endemic and extinct, and is a typical representative of a long-lived lake fauna. Fluvial taxa are not common, (marginal) marine taxa are rare. An additional molluscan fauna from the Miocene Solimões Formation of Brazil, containing 13 fresh water species was also described. The newly documented fauna was used to improve biostratigraphic framework of Miocene Amazonian deposits. Twelve mollusc zones were introduced, the upper eleven of which cover a time interval of approximately seven million years covered previously by only three pollen zones. An age model calculated for the borehole data indicates that the Pebas Formation was deposited between c. 24 and 11 Ma. The areal distribution of the outcropping mollusc zones uncovered a broad dome structure, termed here the Iquitos-Araracuara anteclise in the study area. The structure appears to have influenced river courses and also contributed to edaphic heterogeneity that may have been in part responsible for the current high biodiversity in the study area. The Pebas system was a huge system (> one million km2) dominated by relatively shallow lakes, but also containing swamps and rivers. The system was fed by rivers draining the emergent Andes in the west and lowlands and cratons to the east. The Pebas system was located at sea level and was open to marine settings through a northern portal running through the Llanos Basin and East Venezuela Basin towards the Caribbean. Cyclical baselevel changes possibly related to Mylankhovitch cycles, have been documented in depositional sequences of the Pebas Formation. The composition of the Pebasian mollusc fauna implies that the system was mostly a fresh water system. Such an interpretation is matched by strontium isotope ratios as well as very negative δ18O ratios found in the shells, but is at odds with oligohaline and mesohaline ichnofacies found in the same strata. The mollusc fauna of the Pebas Formation diversified through most of the existence of the lake system. The diversification was mostly the result of in-situ cladogenesis. The success of some of the Pebasian endemic clades is explained by adaptation to fresh water, low oxygen, common unconsolidated lake bottoms (soup grounds) as well as high predation intensity. Maximum diversity was reached at the base of the late Middle to early Late Miocene Grimsdalea pollen zone, some 13 Ma. At the time some 85 species co-occurred, 67 of which are considered as Pebasian endemics. A subsequent drop in species richness coincides with indications of elevated salinities, although a causal relation still needs to be established. Apparently the Pebas fauna went (almost) entirely extinct with the replacement of the lake system into a fluvio-tidal system during the Early Late Miocene, some 11 Ma.

Le pouvoir communal et l'émancipation urbaine au XVe siècle : le cas de la ville de Liège (1400-1455)

La ville de Liège, à la fin du Moyen Âge, fut le théâtre de l’affirmation de ses bourgeois par l’entremise des corporations de métier et des institutions communales. Le XIVe siècle fut en effet marqué par des gains communaux importants au détriment, d’une part, du patriciat urbain, d’autre part, du prince-évêque de Liège. À partir de 1384, le Conseil liégeois, entièrement entre les mains des artisans, possédait des prérogatives étendues dans l’administration et la gestion de la ville. Toutefois, la progression du pouvoir bourgeois se trouva brusquement stoppée, pour une dizaine d’années, lors de la défaite liégeoise d’Othée, en 1408. Ce mémoire porte sur l’évolution du pouvoir communal liégeois dans la première moitié du XVe siècle, moins bien connue des historiens. L’étude de la chronique de Jean de Stavelot permet de mettre en lumière cette période trouble. La défaite d’Othée de même que les réformes imposées par les princes-évêques causèrent notamment de grands bouleversements. Des partis politiques entrèrent aussi en scène et la présence voisine du puissant duc de Bourgogne influença la vie des Liégeois. Ces particularités issues du contexte politique et social sont autant d’éléments qui influèrent sur la volonté d’affirmation des bourgeois et l’exercice du pouvoir communal à Liège.

Originalité culturelle au Sylvicole moyen sur le site de Pointe-du-Gouvernement, Haut-Richelieu, Québec

Mémoire numérisé par la Division de la gestion de documents et des archives de l'Université de Montréal.

Les discours de Pierre Plaoul au Parlement de Paris (1406) : un exemple des rhétoriques française et latine au Moyen Âge tardif

Le 27 mai 1406, le théologien parisien Pierre Plaoul comparaît devant la cour du Parlement de Paris en tant que représentant de l’Université de Paris dans une affaire qui l’oppose à l’Université de Toulouse. Il y prononce un sermon en latin, ce que la cour lui reproche instantanément, lui demandant de parler en français pour la prochaine séance. Le 7 juin, lors de sa deuxième comparution, il parle cette fois en langue vernaculaire et prononce un discours extrêmement différent du premier, autant dans son genre que dans son registre de citations. Les deux discours sont conservés dans le registre X1a4787 des Archives nationales de France. L’édition des discours permet de comprendre le raisonnement derrière leurs différences, mais il permet surtout de constater que le discours français fait état d’une érudition encore plus grande que son homologue latin et que son orateur n’était nullement gêné par l’usage de la langue vernaculaire. Remis dans le contexte historiographique actuel, il en ressort que l’utilisation du français par Plaoul concorde parfaitement avec l’abandon du modèle de rapport diglossique entre latin et français pour la fin du Moyen Âge, lui préférant plutôt un rapport de langues en contacts. Ce postulat est soutenu par les nombreuses occurrences d’universitaires médiévaux démontrant une excellente maîtrise d’un registre savant de la langue vulgaire, des poètes, aux prédicateurs en passant par les practiciens du droit. Un examen plus attentif de l’utilisation de la langue française par les docteurs en théologie du règne de Charles VI vient aussi appuyer l’hypothèse selon laquelle les universitaires du bas Moyen Âge considéraient la langue vernaculaire comme un instrument approprié à la transmission de la culture savante.

Ordnung hilffen. Vorreformatorische Geschlechterordnung: Erste deutsche Bibel und Der Ackermann aus Böhmen

Die Dissertation leistet einen Beitrag zur Konstruktion von Geschlechterverhältnissen in der Ehe vor der Reformation. Untersucht werden zwei Texte des 15. Jahrhunderts: Die sogenannte Erste deutsche Bibel (EDB) und die Dichtung Der Ackermann aus Böhmen von Johannes von Tepl. Die Wort-für-Wort-Analyse beider Texte hat aus der zeitgebundenen deutschen Sprachgestalt spezifi-sche Denkfiguren erschlossen. Zentral ist die Gestaltung des Verhältnisses zwischen Gott und Menschen als Rechtsbeziehung Lehen. Das erste Kapitel analysiert und interpretiert die für Ehe- und Geschlechterkonzepte grund-legenden Aussagen von Genesis 1 - 4,1 und den Kanon der fünf Weisheitsbücher der EDB mit folgenden Ergebnissen: 1. Die EDB ist als Rechtsbuch zu lesen, dessen Zentrum die göttliche Herrschaft mit ihrer Rechts-ordnung ist. In diesem Rahmen wird für Mann und Frau die Ordnung Paar definiert. 2. Beide Geschlechter sind gleichwertig. Das kommt in ihren jeweiligen Handlungsfeldern (Werkordnungen) zum Ausdruck. 3. Der Begriff hilffen für die Ehefrau bedeutet Hilfe zum Heil ihres Mannes und eine spezifische Gottesnähe. Dies ist ein entscheidender Unterschied zu Luthers Bibelübersetzung, welche die Frau als untergeordnete Gehilfin des Mannes gestaltet. (Anhang III stellt die EDB-Verse der Lu-therübersetzung von 1545 gegenüber.) 4. Der Sündenfall wird als Rechtsbruch beschrieben, der den Wechsel von der Schöpfungsord-nung im Paradies zur Weltordnung auslöst, die mit den Urteilen Gottes über Frau und Mann beginnt (Genesis 3). Die Urteile fassen die Ehe in einem Diagonalkreuz, welches vier Faktoren untrennbar verbindet: Herrschaft mit Unterordnung sowie hilffen (Gebären) mit Tod. Die Ge-schlechterunterschiede sind konstituierend für die Ehe im Diagonalkreuz. In der EDB lassen sich drei Paarkonstellationen unterscheiden: die Ehe im Diagonalkreuz zwischen dem guten weib und dem weisen Mann, die Ehe ohne Diagonalkreuz zwischen dem un-weib und dem unweisen Mann und die nichteheliche Geschlechterbeziehung zwischen dem gemeinem weib und dem ee-brecher. Das zweite Kapitel der Dissertation vergleicht die alttestamentarischen Ehekonzepte der EDB mit denen der Dichtung Ackermann aus Böhmen. Die rhetorische Form des Streitgesprächs zwischen Witwer und hern Tot zeigt die Struktur eines deutschrechtlichen Prozesses. In diesem Rahmen gewinnen die gegensätzlichen Aussagen über die Ehe die Bedeutung von Rechtspositionen, die in konträren göttlichen Herrschaftsordnungen verortet werden. Die vom Witwer vertretene Herrschaftsordnung beruht auf der alttestamentarischen Rechtsordnung der EDB, während die Positionen des hern Tot diese Rechtsordnung verkehren, indem er die Herrschaftsordnung der Welt als sein Eigen definiert. Ein weiteres Ergebnis des Vergleichs zwischen der EDB und dem Ackermann aus Böhmen ist, dass sowohl die alttestamentarischen Bücher als auch die Dichtung Rechtsfiguren präsentieren. Entscheidend sind in beiden Texten die Urteile Gottes, die jeweils einen Paradigmenwechsel kon-stituieren. In der EDB wird nach dem Sündenfall die (paradiesische) Rechtsordnung in die Rechtsordnung ee gewandelt. Im Ackermann wird die alttestamentarische Rechtsordnung ee der EDB durch die ordenung Tod ersetzt, mit der zugleich die Ordnung Paar nicht mehr gilt. Die Urtei-le Gottes in der EDB definieren das Paar als zweigeschlechtlichen Menschen, das Urteil im Ackermann charakterisiert zwei Einzelmenschen: Mann oder Frau. Damit wird die zentrale Bedeutung der Ehefrau als hilffen zum Heil ihres Mannes aufgehoben, weil die wechselseitige Angewiesenheit von Mann und Frau nicht mehr gegeben ist. Insofern ist hier ein wichtiger Schritt zum reformatorischen Eheverständnis zu erkennen.

Las cuevas prehistóricas de Serinyà (Pla de l’Estany, Girona)

The Reclau Caves, which form part of the Serinyà Prehistoric Caves Park (Pla de l’Estany, Girona), are shelters formed by waterfall travertines which have been in turn affected by karstification phenomena. Though relatively small, these cavities were big enough to held human occupation. Its evolution has seen the falling of blocks and infilling of terrigenous materials. Thus, the caves were completely filled and had most of their original roofs fallen. The first excavations of these caves were made in the mid 1940s and they continued, albeit with some interruptions, until present times. The caves were occupied by humans since the late Middle Pleistocene until the Holocene. Hence, the main occupation periods can be attributed to the Middle Paleolithic and Upper Paleolithic cultures. Given the existence of these sites, the project of an archeological park was started and its first phase opened to the public in the summer of 1997. The creation of this park has led to the protection of the three main caves of the site (Arbreda, Mollet and Reclau Viver Caves). The caves have also been adapted and singposted to open them to the public. Other facilities of the park include a reception building and an activity area. The caves can be visited in guided tours which include the projection of a film, the visit to the permanent exhibition room, the three main caves and the participation in some prehistoric-related activities

Domesticating the calendar: the hours and the almanac in Tudor England

This article examines two genres of text which were extremely popular in the late-medieval and early modern periods, and it pays particular attention to women users. The printed almanacs of sixteenth-century England were enormously influential; yet their contents are so formulaic and repetitive as to appear almost empty of valuable information. Their most striking feature is their astrological guidance for the reader, and this has led to them being considered 'merely' the repository of popular superstition. Only in the last decade have themes of gender and medicine been given serious consideration in relation to almanacs; but this work has focused on the seventeenth century. This chapter centres on a detailed analysis of sixteenth-century English almanacs, and the various kinds of scientific and household guidance they offered to women readers. Both compilers and users needed to chart a safe course through the religious and scientific battles of the time; and the complexities involved are demonstrated by considering the almanacs in relation to competing sources of guidance. These latter are Books of Hours and 'scientific' works such as medical calendars compiled by Oxford scholars in the late middle ages. A key feature of this chapter is that it gives practical interpretations of this complex information, for the guidance of modern readers unfamiliar with astrology.

Quantifying volcanic ash dispersal and impact of the Campanian Ignimbrite super-eruption

1] We apply a novel computational approach to assess, for the first time, volcanic ash dispersal during the Campanian Ignimbrite (Italy) super-eruption providing insights into eruption dynamics and the impact of this gigantic event. The method uses a 3D time-dependent computational ash dispersion model, a set of wind fields, and more than 100 thickness measurements of the CI tephra deposit. Results reveal that the CI eruption dispersed 250–300 km3 of ash over ∼3.7 million km2. The injection of such a large quantity of ash (and volatiles) into the atmosphere would have caused a volcanic winter during the Heinrich Event 4, the coldest and driest climatic episode of the Last Glacial period. Fluorine-bearing leachate from the volcanic ash and acid rain would have further affected food sources and severely impacted Late Middle-Early Upper Paleolithic groups in Southern and Eastern Europe

Marine Isotope Stage 9 environments of fluvial deposits at Hackney, north London, UK

Middle Pleistocene deposits at Hackney, north London comprise a thick unit of organic sands and silts occupying a channel near the confluence of the River Thames in south-eastern England and its left-bank tributary the River Lea. They represent a short time interval, perhaps no more than a few years, within a late Middle Pleistocene interglacial. The organic sediments are overlain by unfossiliferous sands and gravels indicating deposition on the floodplain of a braided river under cool or cold climatic conditions. The fossil plant, insect, mollusc and vertebrate remains from the interglacial deposits all indicate climatic conditions with summers warmer than the present in SE England, and winters with a similar thermal climate. The biostratigraphic evidence suggests that the time period represented by the organic unit is part of MIS 9, although the geochronological evidence for such an age is inconclusive. The palaeontological evidence strongly suggests that this temperate stage was warmer than the succeeding temperate stage MIS 7 or the Holocene, and approaching the Ipswichian (MISs 5e) in its warmth. The multidisciplinary description of the Hackney deposits is one of the first to reconstruct terrestrial conditions in Marine Isotope Stage 9 in Western Europe.

U-Pb zircon and (40)Ar-(39)Ar K-feldspar dating of syn-sedimentary volcanism of the Neoproterozoic Marica Formation: constraining the age of foreland basin inception and inversion in the Camaqua Basin of southern Brazil

New U-Pb zircon and (40)Ar-(39)Ar K-feldspar data are presented for syn-sedimentary volcanogenic rocks from the Neoproterozoic Marica Formation, located in the southern Brazilian shield. Seven (of nine) U-Pb sensitive high-resolution ion microprobe analyses of zircons from pyroclastic cobbles yield an age of 630.2 +/- 3.4 Ma (2 sigma), interpreted as the age of syn-sedimentary volcanism, and thus of the deposition itself. This result indicates that the Marica Formation was deposited during the main collisional phase (640-620 Ma) of the Brasiliano II orogenic system, probably as a forebulge or back-bulge, craton-derived foreland succession. Thus, this unit is possibly correlative of younger portions of the Porongos, Brusque, Passo Feio, Abapa (Itaiacoca) and Lavalleja (Fuente del Puma) metamorphic complexes. Well-defined, step-heating (40)Ar-(39)Ar K-feldspar plateau ages obtained from volcanogenic beds and pyroclastic cobbles of the lower and upper successions of the Marica Formation yielded 507.3 +/- 1.8 Ma and 506.7 +/- 1.4 Ma (2 sigma), respectively. These data are interpreted to reflect total isotopic resetting during deep burial and thermal effects related to magmatic events. Late Middle Cambrian cooling below ca. 200 degrees C, probably related to uplift, is tentatively associated with intraplate effects of the Rio Doce and/or Pampean orogenies (Brasiliano III system). In the southern Brazilian shield, these intraplate stresses are possibly related to the dominantly extensional opening of a rift or a pull-apart basin, where sedimentary rocks of the Camaqua Group (Santa Barbara and Guaritas Formations) accumulated.

The Araguaia fold belt, Brazil: A reactivated Brasiliano-Pan-African cycle (550 Ma) geosuture

The Araguaia-Tocantins geosuture, which separates the Araguaia Fold Belt (AFB) from the Archean Amazonian Craton, was active in the late Middle Proterozoic. The Baixo Araguaia Supergroup was deposited, consisting of the Estrondo Group (lower quartzites with intercalated schists), Xambioá Formation (schists), and Canto da Vazante Formation (upper feldspathic schists); and the Tocantins Group consisting of the Couto Magalhaës Formation (phyllites, quartzites, slates, limestones, and metacherts) and Pequizeiro Formation (upper chlorite schists); and associated mafic-ultramafic bodies. The deformational history includes four regional phases of deformation within this supracrustal sequence: recumbent folds with vergence to the west; refolding with a N-S trend; an intense crenulation episode; and late thrusting from east to west. Metamorphism is of intermediate or intermediate-high pressure type with garnet, biotite, chlorite, and sericite isograds succeeded by a slightly or non-metamorphosed zone, from east to west. Rocks surrounding sparse gneissic-cored domes contain isograds of staurolite, kyanite, and fibrolite. These isograds are believed to be associated with the 1100 Ma Uruaçuano event. The Brasiliano Orogeny strongly affected the AFB with displacements due to transcurrent reactivation of great and old faults of the basement, slight folding in the supracrustal sequence, intrusion of small granite bodies, and development of domes with associated normal faults. The area underlain by the Estrondo Group was uplifted at this time, causing the deposition of the Rio das Barreiras polymictic conglomerate of the central area. K-Ar and Rb-Sr analyses date this thermo-tectonic event at 550 ± 100 Ma. The Archean basement is exposed in the cores of domes as a granite-gneiss association, the Colméia complex, which shows thermo-tectonic features that may be interpreted as polycyclic imprints (Jequié, Transamazonian?, Uruaçuano, and Brasiliano Events). © 1989.