Abstract
This paper reviews major results of the recent German research priority program “Changes of the geo-biosphere during the last 15,000 years”, a contribution to PAGES focussing on changes of the geo-biosphere during the Weichselian Lateglacial. Different continental archives such as annually laminated lacustrine sediments, floodplain sediments, and speleothems were used to reconstruct environmental response to climatic changes and the Laacher See eruption event at ca 12,900cal BP. Special emphasis is paid to establish a reliable time control using varve counting, high-precision radiocarbon dating of tree-ring series, and AMS radiocarbon dating of terrestrial plant macrofossils recovered from lacustrine sediments to correlate and synchronize large-scale environmental changes and events in central Europe.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
