Grainsize composition of composite sediment core ROD11 from the crater basin of Rodderberg, Germany

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Autores principales: Zolitschka, Bernd, Frechen, Manfred
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 2025
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author Zolitschka, Bernd
Frechen, Manfred
author_facet Zolitschka, Bernd
Frechen, Manfred
collection Datos científicos de ciencias marinas y ambientales
contents Grainsize data supports palaeoclimatic reconstruction of glacial/interglacial cycles for the Middle Pleistocene sediment record from the crater basin of Rodderberg, Germany. A sediment record measuring 72.8 m in length was retrieved by employing wire-line drilling techniques, utilising 3 m-long liners, from the silted-up crater basin of Rodderberg (East Eifel Volcanic Field) in the vicinity of the city of Bonn, Germany. For the purpose of grainsize analysis, the composite record ROD11 was systematically subsampled at a spatial resolution of 2 cm and examined through a laser diffraction particle size analyser (Beckman Coulter LS 13320). The resulting sedimentological data characterise glacials as silt-dominated (aeolian sediments: loess), interglacials as sand-dominated (runoff-related deposits from the step crater walls) and clay dominance for the Holocene soil. The terrestrial sediment record has been evaluated through multiple dating techniques and it provides a comprehensive environmental reconstruction since the Middle Pleistocene, thus providing valuable insights into the region's climate history.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_975229
institution PANGAEA
language en
publishDate 2025
publisher PANGAEA
record_format pangaea
spellingShingle Grainsize composition of composite sediment core ROD11 from the crater basin of Rodderberg, Germany
Zolitschka, Bernd
Frechen, Manfred
AGE; biogenic silica; carbonates; Clay; cluster analysis; Comment; COMPCORE; Composite Core; Composite records; crater lake; DEPTH, sediment/rock; diatoms; East Eifel Volcanic Field; Germany; grain size; Grain size, mean; Interglacials; lake sediment proxies; Laser diffraction particle size analyser, Beckman Coulter, LS13 320; Magnetic susceptibility; minerogenic matter; organic matter; Palaeoclimate reconstructions; Pleistocene; ROD11; Rodderberg, North Rhine-Westphalia, Germany; Sand; Silt; XRF-core scanning
Grainsize data supports palaeoclimatic reconstruction of glacial/interglacial cycles for the Middle Pleistocene sediment record from the crater basin of Rodderberg, Germany. A sediment record measuring 72.8 m in length was retrieved by employing wire-line drilling techniques, utilising 3 m-long liners, from the silted-up crater basin of Rodderberg (East Eifel Volcanic Field) in the vicinity of the city of Bonn, Germany. For the purpose of grainsize analysis, the composite record ROD11 was systematically subsampled at a spatial resolution of 2 cm and examined through a laser diffraction particle size analyser (Beckman Coulter LS 13320). The resulting sedimentological data characterise glacials as silt-dominated (aeolian sediments: loess), interglacials as sand-dominated (runoff-related deposits from the step crater walls) and clay dominance for the Holocene soil. The terrestrial sediment record has been evaluated through multiple dating techniques and it provides a comprehensive environmental reconstruction since the Middle Pleistocene, thus providing valuable insights into the region's climate history.
title Grainsize composition of composite sediment core ROD11 from the crater basin of Rodderberg, Germany
topic AGE; biogenic silica; carbonates; Clay; cluster analysis; Comment; COMPCORE; Composite Core; Composite records; crater lake; DEPTH, sediment/rock; diatoms; East Eifel Volcanic Field; Germany; grain size; Grain size, mean; Interglacials; lake sediment proxies; Laser diffraction particle size analyser, Beckman Coulter, LS13 320; Magnetic susceptibility; minerogenic matter; organic matter; Palaeoclimate reconstructions; Pleistocene; ROD11; Rodderberg, North Rhine-Westphalia, Germany; Sand; Silt; XRF-core scanning
url https://doi.org/10.1594/PANGAEA.975229