The Erlangen AMS facility and its applications in (super 14) C sediment and bone dating.
Abstract
We report here on the radiocarbon dating of sediment samples from Bavaria using the Erlangen accelerator mass spectrometry facility. The absolute time calibration of different sediment profiles, together with pollen analyses, should establish a better chronology of climate and vegetation during Holocene in Bavaria. For an enhanced reliability of sediment dating, we measured different fractions such as bulk sediments, pollen grains, macrofossils and humic acids. For these fraction, we describe the separation methods and conversion to sputter targets. Furthermore, we discuss the sample preparation for the dating of bones and present some results.
Keywords
Bavaria Germany;cores;Germany;organic acids;humic acids;vegetation;Holocene;microfossils;miospores;palynomorphs;pollen;Central Europe;accelerator mass spectroscopy;mass spectroscopy;spectroscopy;paleoclimatology;Pleistocene;organic compounds;Europe;peat;sample preparation;bones;sediments;Cenozoic;Quaternary;C 14;carbon;dates;isotopes;radioactive isotopes;absolute age