Die alteren Musikalien der Stadt Freiberg in Sachsen.

Catalog of the printed works and manuscripts of the 16th and 17th centuries in the libraries of the Freiberg Gymnasium and Freiberger Altertumsverein.

Geschichte der Goldenen horde in Kiptschak, das ist: der Mongolen in Russland.

"Preisaufgabe der Politisch-historisch-philogischen Classe der Kaiserl. Akademie der wissenschaften zu St. Petersburg ... 1832."

Commentatio de Hermagora rhetora.

Pages extracted from "Jahresbericht ueber das Kurfuerstliche Gymnasium zu Hersfeld" 1839.

Quintus Horatius Flaccus Brief an die Pisonen /

Mills College checklist,

Mit Gerhart Hauptmann : erinnerungen und bekenntnisse aus seinem freundeskreis /

W. Heynen: Zum geleit.--M. Fleischer: Der Breslauer kunstschüler.--Meo: Der nothelfer.--H. Bahr: In erwartung Hauptmanns.--H. Lux: Der Breslauer sozialistenprozess.--B. Wille: Erinnerungen an Gerhart Hauptmann und seine dichtergeneration.--G. Hirschfeld: Von Brahm zu Hauptmann.--H. Church: "Atlantis" in dichtung und wahrheit.--H. Stehr: Ein erinnerungsblatt.--M. Heinmann: Gerhart Hauptmann, züge zu seinem porträt.

Sagen der alten Griechen : der reiferen Jugend beiderlei Geschlechts erzählt

von R. Schneider, Professor am Gymnasium zu Meiningen

3D Reconstruction of Cultural Values at the Regional History Museum-Veliko Tarnovo

The project paper presents the work done by the Regional History Museum – Veliko Tarnovo (RHM) on 3D reconstruction of cultural values and objects from the Veliko Tarnovo region – the St Peter and St Paul church in Veliko Tarnovo, the chorus of the metropolitan Nativity church in Arbanassi and the St. Dimitar church in Arbanassi.

Global compilation of benthic data sets I

Approaches to quantify the organic carbon accumulation on a global scale generally do not consider the small-scale variability of sedimentary and oceanographic boundary conditions along continental margins. In this study, we present a new approach to regionalize the total organic carbon (TOC) content in surface sediments (<5 cm sediment depth). It is based on a compilation of more than 5500 single measurements from various sources. Global TOC distribution was determined by the application of a combined qualitative and quantitative-geostatistical method. Overall, 33 benthic TOC-based provinces were defined and used to process the global distribution pattern of the TOC content in surface sediments in a 1°x1° grid resolution. Regional dependencies of data points within each single province are expressed by modeled semi-variograms. Measured and estimated TOC values show good correlation, emphasizing the reasonable applicability of the method. The accumulation of organic carbon in marine surface sediments is a key parameter in the control of mineralization processes and the material exchange between the sediment and the ocean water. Our approach will help to improve global budgets of nutrient and carbon cycles.

Swath sonar bathymetry during POLARSTERN cruise ARK-VII/3a (PS17) with links to multibeam raw data files

In multibeam echosounder and subbottom profiler data acquired during R/V Polarstern cruise ARK-VII/3a from the Hovgaard Ridge (Fram Strait), we found evidence for very deep (>1200 m) iceberg scouring. Five elongated seafloor features have been detected that are interpreted to be iceberg scours. The scours are oriented in north-south/south-north direction and are about 15 m deep, 300 m wide, and 4 km long crossing the entire width of the ridge. They are attributed to multiple giant paleo-icebergs that most probably left the Arctic Ocean southward through Fram Strait. The huge keel depths are indicative of ice sheets extending into the Arctic Ocean being at least 1200 m thick at the calving front during glacial maxima. The deep St. Anna Trough or grounded ice observed at the East Siberian Continental Margin are likely source regions of these icebergs that delivered freshwater to the Nordic Seas.

Global data compilation of benthic data sets II

In this study we present a global distribution pattern and budget of the minimum flux of particulate organic carbon to the sea floor (J POC alpha). The estimations are based on regionally specific correlations between the diffusive oxygen flux across the sediment-water interface, the total organic carbon content in surface sediments, and the oxygen concentration in bottom waters. For this, we modified the principal equation of Cai and Reimers [1995] as a basic monod reaction rate, applied within 11 regions where in situ measurements of diffusive oxygen uptake exist. By application of the resulting transfer functions to other regions with similar sedimentary conditions and areal interpolation, we calculated a minimum global budget of particulate organic carbon that actually reaches the sea floor of ~0.5 GtC yr**-1 (>1000 m water depth (wd)), whereas approximately 0.002-0.12 GtC yr**-1 is buried in the sediments (0.01-0.4% of surface primary production). Despite the fact that our global budget is in good agreement with previous studies, we found conspicuous differences among the distribution patterns of primary production, calculations based on particle trap collections of the POC flux, and J POC alpha of this study. These deviations, especially located at the southeastern and southwestern Atlantic Ocean, the Greenland and Norwegian Sea and the entire equatorial Pacific Ocean, strongly indicate a considerable influence of lateral particle transport on the vertical link between surface waters and underlying sediments. This observation is supported by sediment trap data. Furthermore, local differences in the availability and quality of the organic matter as well as different transport mechanisms through the water column are discussed.

Accumulation of organic carbon in the Laptev Sea

Composition and accumulation rates of organic carbon in Holocene sediments provided data to calculate an organic carbon budget for the Laptev Sea continental margin. Mean Holocene accumulation rates in the inner Laptev Sea vary between 0.14 and 2.7 g C cm**2/ky; maximum values occur close to the Lena River delta. Seawards, the mean accumulation rates decrease from 0.43 to 0.02 g C cm**2/ky. The organic matter is predominantly of terrigenous origin. About 0.9*10**6 t/year of organic carbon are buried in the Laptev Sea, and 0.25*10**6 t/year on the continental slope. Between about 8.5 and 9 ka, major changes in supply of terrigenous and marine organic carbon occur, related to changes in coastal erosion, Siberian river discharge, and/or Atlantic water inflow along the Eurasian continental margin.

Predigt, bei der dreihundertjährigen Jubelfeier der Uebergabe des evangelischen Glaubens-Bekenntnisses zu Augsburg, in der Haupt-Pfarr-Kirche St. Maria Magdalena zu Breslau : am 25sten Junius 1830

gehalten von Johann Wilhelm Fischer, Königlichem Consistorial-Rath und Pastor der genannten Kirche

Geschichte des im Jahre 1530 zu Augsburg gehaltenen Reichstages und der Augsburgischen Confession : zur Vorbereitung auf die bevorstehende dritte Jubel-Feier der evangelischen Kirche /

"Nebst einem Abdrucke der unveränderten Augsburgischen Confession."

Beurtheilung einer Schrift, welche unter dem Titel : Einleitung zu näherer und deutlicher Aufklärung der Offenbarung Jeus Christi oder St Johannis, nach Chronologie und Geschichte, als Beytrag zum Beweis, dass Bengels apokalyptisches System das wahre sei : in diesem Jahr zu Carlsruhe in Macklots Verlag im Druck erschienen ist.

Anhang has special t.p.: Anhang: Versuch eines allein aus den Worten des Textes ohne schwehre mathematische Berechnung, hergeleiteten, fasslichen, und ein-leuchtenden Ausschlusses der geheimen Zeiten der Offenbarung JesuChristi oder St. Johannis.

Die drei St.Johannisgrade der grossen National-Mutter-Loge zu den drei Weltkugeln.

Mode of access: Internet.