Lago Grande di Monticchio (southern Italy) a high resolution sedimentary record of the last 70,000 years
Identifieur interne : 000831 ( Istex/Corpus ); précédent : 000830; suivant : 000832Lago Grande di Monticchio (southern Italy) a high resolution sedimentary record of the last 70,000 years
Auteurs : Bernd Zolitschka ; Jörg F. W. NegendankSource :
- Lecture Notes in Earth Sciences [ 0930-0317 ] ; 1993.
Abstract
Abstract: Lithology, measurements of dry density, total organic carbon and first microstratigraphic investigations were used to calculate a tentative time scale for the lacustrine sediments from Lago Grande di Monticchio. A comparison of these records with dated Italian lake sediments of Valle di Castiglione, Lago di Vico and Lagaccione Maar and with the eolian dust record from Vostok ice core (Antarctica) demonstrates the time scale to be reasonable. According to this tentative time scale the 51.8 m of sediment cover the last 70,000 years.
Url:
DOI: 10.1007/BFb0117601
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<front><div type="abstract" xml:lang="en">Abstract: Lithology, measurements of dry density, total organic carbon and first microstratigraphic investigations were used to calculate a tentative time scale for the lacustrine sediments from Lago Grande di Monticchio. A comparison of these records with dated Italian lake sediments of Valle di Castiglione, Lago di Vico and Lagaccione Maar and with the eolian dust record from Vostok ice core (Antarctica) demonstrates the time scale to be reasonable. According to this tentative time scale the 51.8 m of sediment cover the last 70,000 years.</div>
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<Abstract ID="Abs1" Language="En"><Heading>Abstract</Heading>
<Para>Lithology, measurements of dry density, total organic carbon and first microstratigraphic investigations were used to calculate a tentative time scale for the lacustrine sediments from Lago Grande di Monticchio. A comparison of these records with dated Italian lake sediments of Valle di Castiglione, Lago di Vico and Lagaccione Maar and with the eolian dust record from Vostok ice core (Antarctica) demonstrates the time scale to be reasonable. According to this tentative time scale the 51.8 m of sediment cover the last 70,000 years.</Para>
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<name type="personal"><namePart type="given">Bernd</namePart>
<namePart type="family">Zolitschka</namePart>
<affiliation>Geologie, Universität Trier, D-5500, Trier</affiliation>
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<name type="personal"><namePart type="given">Jörg</namePart>
<namePart type="given">F.</namePart>
<namePart type="given">W.</namePart>
<namePart type="family">Negendank</namePart>
<affiliation>Geo Forschungs Zentrum, Telegrafenberg A26, O-1561, Potsdam</affiliation>
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<abstract lang="en">Abstract: Lithology, measurements of dry density, total organic carbon and first microstratigraphic investigations were used to calculate a tentative time scale for the lacustrine sediments from Lago Grande di Monticchio. A comparison of these records with dated Italian lake sediments of Valle di Castiglione, Lago di Vico and Lagaccione Maar and with the eolian dust record from Vostok ice core (Antarctica) demonstrates the time scale to be reasonable. According to this tentative time scale the 51.8 m of sediment cover the last 70,000 years.</abstract>
<relatedItem type="host"><titleInfo><title>Paleolimnology of European Maar Lakes</title>
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<name type="personal"><namePart type="given">Jorg</namePart>
<namePart type="given">F.</namePart>
<namePart type="given">W.</namePart>
<namePart type="family">Negendank</namePart>
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<topic authority="SpringerSubjectCodes" authorityURI="G">Geosciences</topic>
<topic authority="SpringerSubjectCodes" authorityURI="G27008">Sedimentology</topic>
<topic authority="SpringerSubjectCodes" authorityURI="G24009">Mineralogy</topic>
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<identifier type="DOI">10.1007/BFb0117584</identifier>
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<part><date>1993</date>
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<relatedItem type="series"><titleInfo><title>Lecture Notes in Earth Sciences</title>
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