Workshop on Stable Isotope Analysis in Biogeochemistry with focus on the Baltic Sea and its catchment

Figure 4: Oxygen/hydrogen sulphide in the bottom near layer for selected stations Figure 5: Cross section from Kiel Bight to eastern Gotland Basin showing the.. hydrographic

In the Bornholm and Eastern Gotland Basin are 4 samples (TF213, TF271, TF272, TF285) of sea bed sediments taken to analyse the resettlement of foraminifera due to

The second part of this EMB 100 cruise was used gathering hydrographic, chemical, biological and geological data in the Bornholm Basin and Eastern Gotland Basin to follow

Human activities in the Baltic Sea and its surround- ings are responsible for pressures on the environ- ment. The size of the catchment area of the Baltic Sea is four times

The oxygen concentrations in the bottom water are still relatively high in the central Kiel and Mecklenburg Bay, but they decrease already in the Arkona Basin and are

The situation changed further to the north (stat. TF0259, TF0255, TF0253, TF0250); here a water body containing higher oxygen concentrations in comparison with the overlaying

Up to these stations, the oxygen minimum was found above the ground, but at the following, more northern stations (TF0255 toTF0253), a water body of almost 10 m thickness was

Based on the interpretation of sediment data of samples acquired from Laizhou Bay surface sediments in 2012 and the geological development of the area, the coast of