Palaeoecological implications from the sedimentary record of a subtropical maar lake (Eocene Eckfelder Maar; Germany)
Identifieur interne : 002C17 ( Main/Exploration ); précédent : 002C16; suivant : 002C18Palaeoecological implications from the sedimentary record of a subtropical maar lake (Eocene Eckfelder Maar; Germany)
Auteurs : Bernd ZolitschkaSource :
- Lecture Notes in Earth Sciences [ 0930-0317 ] ; 1993.
Descripteurs français
- Pascal (Inist)
- Wicri :
- geographic : Allemagne.
English descriptors
- KwdEn :
Abstract
Abstract: The sediments from Eocene Eckfelder Maar display a cycle from an initial clastic stage via organic oil shale deposition to a final clastic stage. Increasing aridity is related with the onset of oil shale formation, increasing freshwater input with the gradual change from organic back to final clastic deposition. Eutrophic conditions occurred only during a short period of the early oil shale stage related to maximum organic carbon and oxygen isotope values and to the formation of pyrite and vivianite.
Url:
DOI: 10.1007/BFb0117615
Affiliations:
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Le document en format XML
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<term>Eocene</term>
<term>Germany</term>
<term>clastic rocks</term>
<term>lake sediments</term>
<term>maars</term>
<term>oil shale</term>
<term>organic carbon</term>
<term>paleoecology</term>
<term>pyrite</term>
<term>vivianite</term>
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<keywords scheme="Pascal" xml:lang="fr"><term>Allemagne</term>
<term>Carbone organique</term>
<term>Eocène</term>
<term>Europe Centrale</term>
<term>Maar</term>
<term>Paléoécologie</term>
<term>Pyrite</term>
<term>Roche clastique</term>
<term>Schiste bitumineux</term>
<term>Sédiment lacustre</term>
<term>Vivianite</term>
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<front><div type="abstract" xml:lang="en">Abstract: The sediments from Eocene Eckfelder Maar display a cycle from an initial clastic stage via organic oil shale deposition to a final clastic stage. Increasing aridity is related with the onset of oil shale formation, increasing freshwater input with the gradual change from organic back to final clastic deposition. Eutrophic conditions occurred only during a short period of the early oil shale stage related to maximum organic carbon and oxygen isotope values and to the formation of pyrite and vivianite.</div>
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