Stable and radiogenic isotopic records have been successfully used for investigating continental settings, such as palaeosols, lacustrine, caves, peatlands, bogs and evaporative environments. The session invites contributions presenting an applied as well as a theoretical approach. We are looking for contributions that use isotopes along with mineralogical, biological, paleontological and chemical records in order to unravel past and present climate and environmental changes. We welcome papers related to both reconstructions (at various timescales) as well as on fractionation factors, measurement methods, proxy calibration and verification.