Tab. 1: Pollen concentration and flux of sediment core Fiekers Busch

The yearly pollen influx of four samples was calculated from different, estimated shortest length of deposition times (row 2) and pollen concentrations (row 4), using Lycopodium spores as markers for the pollen counts. The resulting very low influx values (row 5) prove that most of the original pollen was decomposed since its deposition. Therefore the pollen diagram must not be interpreted in too much detail.

Identifier
DOI https://doi.org/10.1594/PANGAEA.729846
PID https://hdl.handle.net/10013/epic.33818.d001
Related Identifier https://doi.org/10.1594/PANGAEA.729724
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.729846
Provenance
Creator Grüger, Eberhard
Publisher PANGAEA
Publication Year 1980
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Language English
Resource Type Dataset
Format text/tab-separated-values
Size 48 data points
Discipline Earth System Research
Spatial Coverage (9.043 LON, 52.208 LAT); Lower Saxony, Northern Germany