Abstract
The level of the North Sea has risen about 110 m during the last 15000 years, i.e. during the Weichselian Late Glacial and the Holocene periods. Only the last 46 m of this rise, covering the time interval since 8900 B.P., can be reconstructed on the basis of reliable radiocarbon dates from the southern North Sea and the German Bight.
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.
