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Autores principales: Negendank, Jörg F W, Büchel, Georg, Hansen, R B, Hofmann, W, Irion, G, Haverkamp, B, Lorenz, V, Scharf, B, Sonne, V, Usinger, H, Weiler, H
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 1985
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Acceso en línea:https://doi.org/10.1594/PANGAEA.826297
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author Negendank, Jörg F W
Büchel, Georg
Hansen, R B
Hofmann, W
Irion, G
Haverkamp, B
Lorenz, V
Scharf, B
Sonne, V
Usinger, H
Weiler, H
author_facet Negendank, Jörg F W
Büchel, Georg
Hansen, R B
Hofmann, W
Irion, G
Haverkamp, B
Lorenz, V
Scharf, B
Sonne, V
Usinger, H
Weiler, H
collection Datos científicos de ciencias marinas y ambientales
contents A core from Meerfelder Maar, with a basal age of 29,000 years, provides a continuous sedimentary sequence from Late-Glacial times to the present. It includes the stratigraphical marker of the Laach Pumice Tuff. Sedimentological, geochemical, palynological, palaeobiological, palaeomagnetic and palaeontological analyses permit reconstructions of the history of the lake and its catchment area, and hence of the climate of the region, to be made. The discovery of Middle Oligocene marine, detrital fossils in the maar sediments provides insights into the palaeogeography of the Eifel region during Tertiary times.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_826297
institution PANGAEA
language en
publishDate 1985
publisher PANGAEA
record_format pangaea
spellingShingle Tab. 1: Meerfelder Maar Drilling B4, stratigraphy and sequence of the lake sediments (pdf 215 kB)
Negendank, Jörg F W
Büchel, Georg
Hansen, R B
Hofmann, W
Irion, G
Haverkamp, B
Lorenz, V
Scharf, B
Sonne, V
Usinger, H
Weiler, H
B4; DRILL; Drilling/drill rig; Meerfelder Maar, Germany
A core from Meerfelder Maar, with a basal age of 29,000 years, provides a continuous sedimentary sequence from Late-Glacial times to the present. It includes the stratigraphical marker of the Laach Pumice Tuff. Sedimentological, geochemical, palynological, palaeobiological, palaeomagnetic and palaeontological analyses permit reconstructions of the history of the lake and its catchment area, and hence of the climate of the region, to be made. The discovery of Middle Oligocene marine, detrital fossils in the maar sediments provides insights into the palaeogeography of the Eifel region during Tertiary times.
title Tab. 1: Meerfelder Maar Drilling B4, stratigraphy and sequence of the lake sediments (pdf 215 kB)
topic B4; DRILL; Drilling/drill rig; Meerfelder Maar, Germany
url https://doi.org/10.1594/PANGAEA.826297