GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
  • 1
    facet.materialart.
    Unknown
    EUCC
    In:  In: Geographie der Meere und Küsten : Ergebnisse der 22. Jahrestagung des Arbeitskreises “Geographie der Meere und Küsten” in Warnemünde = Geography of Seas and Coasts : proceedings of the 22nd annual conference in Warnemünde, Germany / EUCC – Die Küsten Union Deutschland e.V. , ed. by Schernewski, G. and Dolch, T. Coastline Reports, 2004 (1). EUCC, Warnemünde, pp. 9-21.
    Publication Date: 2014-03-18
    Description: The lowland of the Oldenburger Graben was investigated in an interdisciplinary cooperation between Geologists, Archaeologists and Palaeobotanists. The postglacial sea level rise was reconstructed by combining and evaluating different methods and results. A new preliminary shoreline displacement curve for the south-western Baltic was created on the basis of reliable sea level data from adjacent regions. The shoreline displacement curve for the Oldenburger Graben mainly covering the time interval from 5100 to 3000 BC cal suggests an oscillating sea level rise. Two periods of intensive sea level rise can be distinguished from two periods of modest rise. The duration between two periods of intensive rise mounts up to 900 years. These oscillations correspond with climatic variations in the North Atlantic. The new preliminary shoreline displacement curve for the south-western Baltic reveals at least eleven oscillations during the last 9000 years.
    Type: Book chapter , NonPeerReviewed
    Format: text
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...