Die hebräischen Traditionen in den Werken des Hieronymus

Moritz Rahmer

Die hebräischen Traditionen in den Werken des Hieronymus

Moritz Rahmer

Die hebräischen Traditionen in den Commentarien des Hieronymus

Moritz Rahmer

Die hebräischen Traditionen in den Werken des Hieronymus

Moritz Rahmer

Welcher biblische Ortsname ist "Cedson" im Onomastikon des Hieronymus

Moritz Rahmer

Sh. Niger. - Wégn jide͏̈she͏̈ chráber. Krite͏̈she artikle͏̈n. 2 bd. Farlag Z. Sh. Sreberk, Wilne 673 [Rezension]

Nathan Birnbaum

A travers l'Afrique centrale du Congo au Niger : 1892 - 1893

par C. Maistre

Briefe aus Afrika : vom Niger-Benue

von Eduard Flegel ...

Bilsenkraut - Hyoscyamus niger

AR

Blattformen : Zahlbrucknera paradoxa - Cortusa matthioli - Helleborus viridis - Helleborus niger - Anemone nemorosa - Zahlbrucknera paradoxa - Anemone narcissiflora - Betonica officinalis

AR

Die deutsche Niger-Benue-Tsadsee-Expedition 1902-1903

von Fritz Bauer, Führer der Expedition

Ausst. 204 - Beschreibu[n]g des heyligen Bischoffs Eusebij: der ain junger vn[d] discipel deß heyligen Sancti Hieronymi gewest ist zu dem Bischoff Damaso vn[d] dem Römer Theodosio von dem leben vn[d] sterben desselben heyligsten Hieronymi. Welche beschreybung sonnst Sannt Hieronymus geschefft oder Testament genannt wirdet mit vil gezierten götliche[n] vn[d] Cristenlichen leern vermenget durch ainen sondern liebhaber Sancti Hieronymi auß dem Latein in das tewtsch gezogen

Vorbesitzer: Heinrich Anton Cornill-d'Orville (Exlibris im Vorderdeckel)

Bulk rock magnetic measurements and thermomagnetic analyses of sediment core GeoB4901-8 from the southeastern flank of the Niger deep-sea fan

Diagenesis has extensively affected the magnetic mineral inventory of organic-rich late Quaternary sediments in the Niger deep-sea fan. Changes in concentration, grain size, and coercivity document modifications of the primary magnetic mineral assemblages at two horizons. The first front, the modern iron redox boundary, is characterized by a drastic decline in magnetic mineral content, coarsening of the grain size spectrum, and reduction in coercivity. Beneath a second front, the transition from the suboxic to the sulfidic anoxic domain, a further but less pronounced decrease in concentration and bulk grain size occurs. Finer grains and higher coercive magnetic constituents substantially increase in the anoxic environment. Low- and high-temperature experiments were performed on bulk sediments and on extracts which have also been examined by X-ray diffraction. Thermomagnetic analyses proved ferrimagnetic titanomagnetites of terrigenous provenance as the principal primary magnetic mineral components. Their broad range of titanium contents reflects the volcanogenic traits of the Niger River drainage areas. Diagenetic alteration is not only a grain size selective process but also critically depends on titanomagnetite composition. Low-titanium compounds are less resistant to diagenetic dissolution. Intermediate titanium content titanomagnetite thus persists as the predominant magnetic mineral fraction in the sulfidic anoxic sediments. At the Fe redox boundary, precipitation of authigenic, possibly bacterial, magnetite is documented. The presence of hydrogen sulfide in the pore water suggests a formation of secondary magnetic iron sulfides in the anoxic domain. Grain size-specific data argue for a gradual development of a superparamagnetic and single-domain iron sulfide phase in this milieu, most likely greigite.