In the Isotope Laboratory, stable isotopes of carbon, nitrogen, oxygen, and hydrogen are investigated by determining the ratio of individual isotopes (atoms of one element whose nuclei contain different numbers of neutrons) in the sample material. The isotopic composition of the sample allows conclusions about, for instance, the prevailing temperature and precipitation regime when the material was formed. In addition to paleoclimatology, stable isotopes are also utilized in geological, …

The Dendroclimatology Laboratory serves for the reconstruction of temporal and spatial variability of the climate of the past utilizing multi-parameter tree ring analysis.

Aims:

• to reconstruct the temporal and spatial variability of the climate of the past utilizing multi-parameter tree ring analysis
• to assess and verify the causes of climate change and its impact on woody plants
  
  

Tasks:

• quantitative analysis of the climate-signal transfer from atmosphere through soil …