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Fertilität und Macht: Die Reproduktionspflicht mittelalterlicher Herrscherinnen und Herrscher
(2021)
Fertility was a key theme of medieval rulership. To conceive and give birth to sons – and thus to ensure the succession to the throne – was one of the foremost duties of medieval kings and queens. But what happened when a male child died in infancy, no male child was born, or no pregnancy ever came about? Barrenness could have dramatic consequences in the Middle Ages, for example expulsion, divorce or conflicts over royal succession. Against this historical background, it seems logical that the fate of the childless ruler would be recounted in the form of a ‘Passion narrative’. In the German literature of the Middle Ages, however, there are also interpretative models of a contrary vein to be found. In the year 1220, for instance, Ebernand of Erfurt construed the wedded life of the imperial couple Henry and Kunigunde as a tale of resistance against the royal obligation to reproduce. In his versified legend, composed in the vernacular, the couple secretly agrees not to fulfil society’s expectations, but to lead a chaste marriage. Yet above and beyond legend, childless rulers were also subject to the impact of multifarious legal, religious, medical, narrative and discursive factors. Taking Michel Foucault as a point of departure, this contribution shows how fertility became a field of power on which hierarchies between rulers and subjects, men and women were negotiated, while also shedding light on how religious and secular ideals clashed in the assessment of infertility.
Fulgurites (= natural glasses formed by lightning strikes to the ground) are indicators of thunderstorms (e.g. Julien 1901). The distribution pattern of fulgurites in the study area (Grand Erg de Bilma and Erg de Tenere between 11.5°E and 16.5° and 18.5°N) shows decreasing fulgurite concentration from south to north. The fulgurite sites are concentrated in the area of fossil dune complexes, where they occur topographically above palaeolimnic deposits in mid-slope position of interdune depressions.
Various amphibolites, metagabbros and eclogitic relics of the Mariimske Lazne complex, and amphibolites from the Cerna Hora Massif exhibit an uniform geochemical character which compares well with modern mid-ocean ridge basalts. Geochemically these metabasites are similar to the amphibolites of the My to area and to schistose. partly striped amphibolites of the neighbouring Tirschenreuth-Mahring Zone and the Erbendorf-Vohenstrauss Zone (Bavaria). Greenschists and amphibolites from the Domailice metamorphic complex show an alkaline-basaltic tendency conforming to modern within-plate basalts or basalts from anomalous midocean ridge segments. In their chemical character, these metabasites compare well with the flaseramphibolites of the Erbendorf-Vohenstrauss Zone. Fine-grained amphibolites in the Warzenrieth area and gabbroic amphiboltes in the Blatterberg-Hoher Bogen area show normal MORB character. The metamorphosed gabbroic rocks in the southern part of the Neukirchen-Kdyne (meta-) igneous complex are subalkaline-tholeiitic and exhibit a magmatic differentiation trend. They differ from the neighbouring amphibolites by generally lower contents of incompatible elements.
Various amphibolites, metagabbros and eclogitic relics of the Mariänske Läzne complex, and amphibolites from the Cernä Hora Massif exhibit an uniform geochemical character which compares weil with modern mid-ocean ridge basalts. Geochemically these metabasites are similar to the amphibolites of the Myto area and to schistose, partly striped amphibolites of the neighbouring Tirschenreuth-Mähring Zone and the Erbendorf-Vohenstrauss Zone (Bavaria). Greenschists and amphibolites from the Domazlice metamorphic complex show an alkaline-basaltic tendency conforming to modern within-plate basalts or basalts from anomalaus midocean ridge segments. In their chemical character, these metabasites compare weil with the flaseramphibolites of the Erbendorf-Vohenstrauss Zone. Fine-grained amphibolites in the Warzenrieth area and (gabbro-) amphibolites in the Blätterberg-Hoher Bogen area show normal MORB character. The metamorphosed gabbroic rocks in the southern part of the Neukirchen-Kdyne (meta-) igneous complex are subalkaline - tholeiitic and exhibit a magmatic differentiation trend. They differ from the neighbouring amphibolites by generally lower contents of incompatible elements.
No abstract available
No abstract available