Organic carbon contents of sediments from Lake Schalkenmehrener Maar: A paleoclimate indicator
Identifieur interne : 000887 ( Istex/Curation ); précédent : 000886; suivant : 000888Organic carbon contents of sediments from Lake Schalkenmehrener Maar: A paleoclimate indicator
Auteurs : B. Rein ; J. F. W. NegendankSource :
- Lecture Notes in Earth Sciences [ 0930-0317 ] ; 1993.
Abstract
Abstract: Investigations on orgnaic carbon in sediments of Maar lakes reveal a relationship to paleotemperatures as reconstructed from Camp Century ice cores. Of great influence are also anthropogenic activities in the catchment area. Clearing of forest, agriculture and related settlement are related to increased soil erosion. These periods are characterised by high amounts of minerogenic deposition and increased absolute orgnaic carbon accumulation but lower organic carbon weight percentages. A microscopic examination of sediment thin sections provides data of mineral- and diatom assemblages, varve counts and enables to estimate sedimentation- and accumulation rates. Based on this information it seems to be possible to separate climatic and anthropogenic reasons for orgnaic carbon contents in Lake Schalkenmehrener Maar.
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DOI: 10.1007/BFb0117595
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B. Rein<affiliation><mods:affiliation>Dept. of Geology, University of Trier, D-5500, Trier</mods:affiliation><wicri:noCountry code="subField">Trier</wicri:noCountry></affiliation><affiliation><mods:affiliation>Dept. of Geology, University of Trier, D-5500, Trier</mods:affiliation><wicri:noCountry code="subField">Trier</wicri:noCountry></affiliation>Le document en format XML
<record><TEI wicri:istexFullTextTei="biblStruct"><teiHeader><fileDesc><titleStmt><title xml:lang="en">Organic carbon contents of sediments from Lake Schalkenmehrener Maar: A paleoclimate indicator</title><author><name sortKey="Rein, B" sort="Rein, B" uniqKey="Rein B" first="B." last="Rein">B. Rein</name><affiliation><mods:affiliation>Dept. of Geology, University of Trier, D-5500, Trier</mods:affiliation><wicri:noCountry code="subField">Trier</wicri:noCountry></affiliation></author><author><name sortKey="Negendank, J F W" sort="Negendank, J F W" uniqKey="Negendank J" first="J. F. W." last="Negendank">J. F. W. Negendank</name><affiliation><mods:affiliation>Dept. of Geology, University of Trier, D-5500, Trier</mods:affiliation><wicri:noCountry code="subField">Trier</wicri:noCountry></affiliation></author></titleStmt><publicationStmt><idno type="wicri:source">ISTEX</idno><idno type="RBID">ISTEX:8A35E4C65C925D6FEC54620DC764D2AF0357302C</idno><date when="1993" year="1993">1993</date><idno type="doi">10.1007/BFb0117595</idno><idno type="url">https://api.istex.fr/document/8A35E4C65C925D6FEC54620DC764D2AF0357302C/fulltext/pdf</idno><idno type="wicri:Area/Istex/Corpus">000939</idno><idno type="wicri:explorRef" wicri:stream="Istex" wicri:step="Corpus" wicri:corpus="ISTEX">000939</idno><idno type="wicri:Area/Istex/Curation">000887</idno></publicationStmt><sourceDesc><biblStruct><analytic><title level="a" type="main" xml:lang="en">Organic carbon contents of sediments from Lake Schalkenmehrener Maar: A paleoclimate indicator</title><author><name sortKey="Rein, B" sort="Rein, B" uniqKey="Rein B" first="B." last="Rein">B. Rein</name><affiliation><mods:affiliation>Dept. of Geology, University of Trier, D-5500, Trier</mods:affiliation><wicri:noCountry code="subField">Trier</wicri:noCountry></affiliation></author><author><name sortKey="Negendank, J F W" sort="Negendank, J F W" uniqKey="Negendank J" first="J. F. W." last="Negendank">J. F. W. Negendank</name><affiliation><mods:affiliation>Dept. of Geology, University of Trier, D-5500, Trier</mods:affiliation><wicri:noCountry code="subField">Trier</wicri:noCountry></affiliation></author></analytic><monogr></monogr><series><title level="s">Lecture Notes in Earth Sciences</title><imprint><date>1993</date></imprint><idno type="ISSN">0930-0317</idno><idno type="eISSN">1613-2580</idno><idno type="ISSN">0930-0317</idno></series><idno type="istex">8A35E4C65C925D6FEC54620DC764D2AF0357302C</idno><idno type="DOI">10.1007/BFb0117595</idno><idno type="ChapterID">11</idno><idno type="ChapterID">Chap11</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0930-0317</idno></seriesStmt></fileDesc><profileDesc><textClass></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Abstract: Investigations on orgnaic carbon in sediments of Maar lakes reveal a relationship to paleotemperatures as reconstructed from Camp Century ice cores. Of great influence are also anthropogenic activities in the catchment area. Clearing of forest, agriculture and related settlement are related to increased soil erosion. These periods are characterised by high amounts of minerogenic deposition and increased absolute orgnaic carbon accumulation but lower organic carbon weight percentages. A microscopic examination of sediment thin sections provides data of mineral- and diatom assemblages, varve counts and enables to estimate sedimentation- and accumulation rates. Based on this information it seems to be possible to separate climatic and anthropogenic reasons for orgnaic carbon contents in Lake Schalkenmehrener Maar.</div></front></TEI></record>Pour manipuler ce document sous Unix (Dilib)
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