Handbüchlein für die Sonntags-Schulen in Deutschland

von Johann Peter Gerlach, königl. baierischem Distrikts-Schulen-Inspektor und Pfarrer zu Burk im Rezatkreise des Königreichs Baiern.

Deutschland und die Schuldfrage

in Verb. mit dem Arbeitsausschuß deutscher Verbände bearb. von Wilhelm Ziegler. [Beitr.: Bernh. Dernburg, Wilhelm v. Schoen...]

Deutschland und seine Kolonieen : Wanderungen durch das Reich und seine überseeischen Besitzungen

unter Mitwirkung von Arthur Achleitner [und 17 weiteren] herausgegeben von Joseph Kürschner

Unpartheyische Gedancken über zwey schändliche Pasquille, betitelt 1. Die Charlatanerie der Buchhandlung; 2. Schreiben eines Buchhändlers aus Europa, an einem Buchhändler in Deutschland, von der Charlatanerie der Buchhandlung : aus grossen Mitleiden gegen diese hirnlose Autores und Pasquillanten mitgetheilet

In Fraktur

Der Krieg und die polnischen Juden in ihrem Verhältnis zu Deutschland

von Felix Perles

Luthers Stellung zu den Juden : ein Beitrag zur Geschichte der Juden in Deutschland während des Reformationszeitalters

von Reinhold Lewin

Von dem Dreissig Jährigen Deutschen Kriege/ Welcher sich Anno 1618 angefangen/ vnd durch Gottes Gnade Anno 1648 geendiget hat : Eben als wann Gott durch den 1618 erschrecklich leuchtenden Cometen/ welcher Dreissig Tage Vber Europen gesehen worden ... ; Ein Auszug/ Wie viel Schlachten diese Jahren über in Deutschland vnd dessen Nachbarschafft geschehen ...

Original am Oberrand knapp beschnitten, teil Textverlust

(Table 3) Lanthanum and scandium contents in phosphorites from seamounts and submarine rises

Scandium and lanthanum were analyzed using neutron activation and ICP-MS methods in 60 samples of oceanic phosphorites of various composition and age recovered from continental margins and seamounts in the Atlantic and Pacific Oceans. In the samples studied scandium content ranges from 0.1 to 60 ppm, lanthanum content ranges from 0.4 to 513 ppm, and La/Sc ratio varies from 1.1 to 114. The lowest scandium content occurs in recent phosphorite nodules, intermediate - in Pleistocene phosphatic sand, and the highest - in ancient seamount phosphorites. Process of scandium accumulation in the phosphorites is mainly controlled by their specific surface area and duration of their contact with ocean water. Lanthanum concentrates in the phosphorites much more intensely than scandium. Correlation between scandium and lanthanum distribution is weak, and it appears only when average concentrations of these elements in various groups of samples are compared.

Food composition of beryx-alfonsino over submarine rises near Azores

Qualitative and quantitative food composition, as well as intensity of feeding of beryx-alfonsino Beryx splendens was examined on banks near the Azores. Data are presented with respect to size groups and taking into account type of feeding of males and females. Crustaceans and fishes were constituents of their feeding ration. A tendency toward increase in the number of consumed fishes in the course of ontogenetic development of beryx-alfonsino was noted. Beryx-alfonsino was shown to occupy the trophic level of consumers of the third order performing function of a deep-water predator.

Borehole temperature, submarine permafrost methane concentrations and pore water chemistry measured on borehole BK2, central Laptev Sea shelf

Submarine permafrost degradation has been invoked as a cause for recent observations of methane emissions from the seabed to the water column and atmosphere of the East Siberian shelf. Sediment drilled 52 m down from the sea ice in Buor Khaya Bay, central Laptev Sea revealed unfrozen sediment overlying ice-bonded permafrost. Methane concentrations in the overlying unfrozen sediment were low (mean 20 µM) but higher in the underlying ice-bonded submarine permafrost (mean 380 µM). In contrast, sulfate concentrations were substantially higher in the unfrozen sediment (mean 2.5 mM) than in the underlying submarine permafrost (mean 0.1 mM). Using deduced permafrost degradation rates, we calculate potential mean methane efflux from degrading permafrost of 120 mg/m**2 per year at this site. However, a drop of methane concentrations from 190 µM to 19 µM and a concomitant increase of methane d13C from -63 per mil to -35 per mil directly above the ice-bonded permafrost suggest that methane is effectively oxidized within the overlying unfrozen sediment before it reaches the water column. High rates of methane ebullition into the water column observed elsewhere are thus unlikely to have ice-bonded permafrost as their source.