Das Judentum in christlicher Darstellung : (Fortsetzung)

Rosalie Perles

Das Judentum in christlicher Darstellung : (Fortsetzung)

Rosalie Perles

Der Wilnaer Gaon R. Elija : (zur Zweihundertjahrfeier seines Geburtstages)

Rosalie Perles

Das moderne Hep! Hep! : zum 100. Geburtstage der Verfasserin

Rosalie Perles

Unsere Großmütter

Rosalie Perles

Jüdische Kriegsgedanken

Rosalie Perles

Unsere Großväter

Rosalie Perles

Gezeugnis der Waarheit, gegeben durch grosse Anzahl glaubwürdiger Leute in unterschiedlichen Briefen und Testimonien über daß Leben, Sitten, Tugenden und Schrifften Jungf. Anthoinette Bourignons, von dero Kindheit an biß auf jetzige Zeit, zu Vernichtung der Lügen und falschen Beschuldigungen, die unter den Nahmen Johan Berckendals, wieder bemelte Jungfrau und dero Schrifften außgesprenget worden, durch zwo Schmäh-Schrifften ...

Vorr.: Johann Conrad Hase

Familien-Kochbuch : Vollständiges Kochbuch für Hausfrauen und angehende Köchinnen, die sich selbst belehren und vervollkommnen wollen

hrsg. von drei erfahrenen Hausfrauen Louise Apel, Bertha Schneider und Rosalie Gruber

Stable oxygen isotope record and relative abundances of planktonic foraminifera of ODP Hole 117-728A

High resolution stratigraphy based on oxygen isotope ratios of the planktonic foraminifers Neogloboquadrina dutertrei (d'Orbigny), Globigeriniodes ruber (d'Orbigny), and Globigerina bulloides (d'Orbigny), magnetic susceptibility, and calcium carbonate content covers the sedimentary record of ODP Hole 728A drilled on the Oman Margin from approximately 10 k.y. to 525 k.y., comprising isotopic stages 1-13. Below stage 13 isotopic stage boundaries cannot be defined with certainty in our data. Sediment accumulation rates were calculated from the isotopic record of N. dutertrei by matching it with the age model SPECMAP curve. During the glacial periods sediment accumulation rates were higher than during the interglacial periods, reflecting increased input from the shelf during low-stands of sea level and increased eolian input. Periodograms for the past 524 k.y. on oxygen isotope records of N. dutertrei, G. ruber, and G. bulloides, on calcium carbonate content, magnetic susceptibility, and on a foraminiferal fragmentation record show powers matching the Milankovitch periodicities. High powers are concentrated around 103 k.y. In the spectra of oxygen isotope ratios of N. dutertrei, magnetic susceptibility, and foraminiferal fragmentation these are significant at the 80% confidence level with respect to a first order autoregressive model. Power concentrations near 43 k.y., matching obliquity, are present but subdued in all spectra. Power concentrations near 23 k.y., matching precession, are significant in the spectra of the oxygen isotope record of N. dutertrei, magnetic susceptibility, and calcium carbonate content record. Fragmentation of planktonic foraminifers increased during the interglacial periods. This is attributed to dissolution of the tests in an expanded oxygen minimum zone (OMZ), where undersaturation of calcium carbonate is caused by enhanced production in the euphotic zone, which would suggest stronger monsoonal induced upwelling during interglacial periods. Extension of the OMZ could also be increased by outflow of low oxygen marginal basin bottom water.

Distribution of biological, anthropogenic, and volcanic constituents in the San Francisco Bay Coastal System

Although conventional sediment parameters (mean grain size, sorting, and skewness) and provenance have typically been used to infer sediment transport pathways, most freshwater, brackish, and marine environments are also characterized by abundant sediment constituents of biological, and possibly anthropogenic and volcanic, origin that can provide additional insight into local sedimentary processes. The biota will be spatially distributed according to its response to environmental parameters such as water temperature, salinity, dissolved oxygen, organic carbon content, grain size, and intensity of currents and tidal flow, whereas the presence of anthropogenic and volcanic constituents will reflect proximity to source areas and whether they are fluvially- or aerially-transported. Because each of these constituents have a unique environmental signature, they are a more precise proxy for that source area than the conventional sedimentary process indicators. This San Francisco Bay Coastal System study demonstrates that by applying a multi-proxy approach, the primary sites of sediment transport can be identified. Many of these sites are far from where the constituents originated, showing that sediment transport is widespread in the region. Although not often used, identifying and interpreting the distribution of naturally-occurring and allochthonous biologic, anthropogenic, and volcanic sediment constituents is a powerful tool to aid in the investigation of sediment transport pathways in other coastal systems.