Augsburg during the Reformation Era: An Anthology of Sources

Edited and Translated, with an Introduction, by B. Ann Tlusty

Latin Sources of Inspiration for 15th and 16th Century Orthodox Prints

The project studied the history of Orthodox graphic art in the context of artistic links between the Eastern and Western worlds, tracing the routes by which iconographic models from western Europe penetrated into eastern Europe and underscoring the role of central European countries in the shaping of the culture of the modern Orthodox church. One important element was the identification of graphic prototypes and export routes for woodcutting blocks which travelled from Germany via Prague, Cracow and Vilnius to Moscow and Kiev, revealing the artistic ties between followers of different religions. Another major element was a study of the appearance of copper engraving in the second half of the 17th century.

Sensitivity of Nd isotopic composition in seawater to changes in Nd sources and paleoceanographic implications

It has been argued that past changes in the sources of Nd could hamper the use of the Nd isotopic composition (ϵNd) as a proxy for past changes in the overturning of deep water masses. Here we reconsider uncertainties associated with ϵNd in seawater due to potential regional to global scale changes in the sources of Nd by applying a modeling approach. For illustrative purposes we describe rather extreme changes in the magnitude of source fluxes, their isotopic composition or both. We find that the largest effects on ϵNd result from changes in the boundary source. Considerable changes also result from variations in the magnitude or ϵNd of dust and rivers but are largely constrained to depths shallower than 1 km, except if they occur in or upstream of regions where deep water masses are formed. From these results we conclude that changes in Nd sources have the potential to affect ϵNd. However, substantial changes are required to generate large-scale changes inϵNd in deep water that are similar in magnitude to those that have been reconstructed from sediment cores or result from changes in meridional overturning circulation in model experiments. Hence, it appears that a shift in ϵNdcomparable to glacial-interglacial variations is difficult to obtain by changes in Nd sources alone, but that more subtle variations can be caused by such changes and must be interpreted with caution.