In the laboratories for stable isotopes in sediments and water, the isotope ratios of the light elements nitrogen (N), carbon (C) and oxygen (O) in continental geoarchives such as lake sediments and speleothems as well as oxygen (O) and hydrogen (H) in precipitation and surface water are determined. This allows us to decipher changing environmental conditions and climate fluctuations in continental climate archives. For a better understanding of the archives, we use monitoring systems that …