Pollen analysis of sediment profile KOE0 from Königseggsee

A core from the deepest part of lake Königsegg. near Ostrach (Oberschwaben), has been studied palynologically and lithologically. The core is only 4.6 m long; lacustrine sedimentation began in the Oldest Dryas. The Alleroedian pumice tuff from Laacher See (Eifel) is present. The origin of the lake as a dead ice lake and its limnogeological development are briefly discussed.

Supplement to: Homann, Marion; Merkt, Josef; Müller, Helmut (1990): Über Alter und Entwicklung des Königseggsees bei Hoßkirch (Oberschwaben). Jahreshefte des Geologischen Landesamts Baden-Württemberg, Freiburg, 32, 247-254

DOI https://doi.org/10.1594/PANGAEA.54300
PID https://hdl.handle.net/10013/epic.35165.d001
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.54300
Creator Homann, Marion; Merkt, Josef; Müller, Helmut
Publisher PANGAEA
Contributor Müller, H H
Publication Year 1990
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Language English
Resource Type Supplementary Dataset; Dataset
Format text/tab-separated-values
Size 949 data points
Discipline Earth System Research
Spatial Coverage (9.450 LON, 47.932 LAT); Königseggsee