In the Organic Surface Geochemistry Lab we conduct research on regional differences of the causes and effects of past climate change and variations in biogeochemical cycles.
In the Physical Laboratory, we perform experiments to study mainly the interactions of sediment and water, but also measure rheological properties of sediment and prepare samples for further analysis in the other labs.
The world in a grain of sand: The physical composition of sediments allows conclusions to be drawn about earth surface processes. We therefore analyse the size, shape, weight and size distribution of grains in order to better understand weathering processes.
In the laboratory for tephrochronology, visible and invisible (crypto-) tephras are extracted from sediment records and prepared for geochemical fingerprinting of the volcanic source as a chronological tool for palaeoclimate archives.
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.
The laboratory for XRF Element Scanning provides qualitative and non-destructive analyses of sediment compositions based on X-ray Fluoresces. These analyses provide detailed element records and maps that can be used to characterise past depositional, environmental and climatic conditions.
The laboratory for microscopy focuses on the specific requirements of microfacies analysis of lake sediments, but also offers a wide range of possibilities for other applications.
The thin section preparation is used to make or produce sections of soft sediments (lacustrine and marin), hard rock, minerals, frozen kernels, organic materials, soils, ores and hygroscopic samples such as salts and clays.
The Dendroclimatology Laboratory serves for the reconstruction of temporal and spatial variability of the climate of the past utilizing multi-parameter tree ring analysis.
Taiwan is one of Earth's most interesting locations, because high uplift rates meet with powerful taifuns. Therefore we set up an observation network of high precision meteorological, hydrological and seismic stations.
Central Asia, extending between the Caucasus and the eastern Tibetan Plateau, with a semiarid/arid belt with water shortage to the west and a glaciered mountainous area with very unstable surface conditions to the east, holds a key position for understanding geodynamic and climate processes.
With the monitoring in the framework of the TERENO-project we aim at better understand the formation processes of lake sediments for an advanced reconstruction of past climate and environment.
We have a collection of field equipment for the acquisition of high resolution topographic data which enables us to investigate magnitudes and patterns of surface processes such as fluvial erosion and deposition, rockfalls, landslides, and debris flows.
Seismic Stations for Autonomous Acquisition and Transmission of Data
Broadband seismometers, geophones, and data loggers enable us in combination with custom software libraries for the preparation, analysis and visualisation of data to investigate Earth surface dynamics at the catchment scale.
