Genetic and isotope analysis of a triple burial from medieval St. Peter's cemetery in Cölln/Berlin.

The German capital Berlin originates from the two medieval settlements Berlin and Cölln on either side of the river Spree. Whereas Berlin is world famous, there is very little awareness of former Cölln. From 2007-2009, during excavations of the earliest cemetery of this forgotten medieval town; 3,126 graves were discovered containing the remains of 3,717 individuals.

Linking Microbial Community Structure to Trait Distributions and Functions Using Salinity as an Environmental Filter.

The structure and function of microbial communities vary along environmental gradients; however, interlinking the two has been challenging. In this study, salinity was used as an environmental filter to study how it could shape trait distributions, community structures, and the resulting functions of soil microbes. The environmental filter was applied by salinizing nonsaline soil (0 to 22 mg NaCl g).

Linking bacterial community composition to soil salinity along environmental gradients.

Salinization is recognized as a threat to soil fertility worldwide. A challenge in understanding the effects of salinity on soil microbial communities is the fact that it can be difficult to disentangle the effects of salinity from those of other variables that may co-vary with salinity. Here we use a trait-based approach to identify direct effects of salinity on soil bacterial communities across two salinity gradients.

Comparative Toxicities of Salts on Microbial Processes in Soil.

Soil salinization is a growing threat to global agriculture and carbon sequestration, but to date it remains unclear how microbial processes will respond. We studied the acute response to salt exposure of a range of anabolic and catabolic microbial processes, including bacterial (leucine incorporation) and fungal (acetate incorporation into ergosterol) growth rates, respiration, and gross N mineralization and nitrification rates. To distinguish effects of specific ions from those of overall ionic strength, we compared the addition of four salts frequently associated with soil salinization (NaCl, KCl, Na2SO4, and K2SO4) to a nonsaline soil.