Magnetic susceptibility measurements of a Holocene sediment core from Limni Volvi, Greece

In 2020 and 2021, we retrieved six parallel sediment cores from Limni Volvi, northern Greece (coring location: 40°39′51.40″N, 23°32′30.70″E), at a water depth of 19.3 m using a UWITEC piston corer (6 cm diameter). Here, we present X-ray fluorescence (XRF), hyperspectral imaging (HSI) and magnetic susceptibility (MS) measurements made on the 19.65 m long composite core. The investigated time interval covers the entire Holocene. The core sequence was analysed to reconstruct the environmental history and palaeoclimatic changes in the area during the Holocene.