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AMS radiocarbon dating of annually laminated sediments from lake Holzmaar, Germany

Identifieur interne : 001043 ( Istex/Corpus ); précédent : 001042; suivant : 001044

AMS radiocarbon dating of annually laminated sediments from lake Holzmaar, Germany

Auteurs : Irena Hajdas ; Bernd Zolitschka ; Susan D. Ivy-Ochs ; Jürg Beer ; Georges Bonani ; Suzanne A. G. Leroy ; Jörg W. Negendank ; Matthias Ramrath ; Martin Suter

Source :

RBID : ISTEX:407779F2CAB4DA1ACB2103027936B0576DDA089E

Abstract

AMS radiocarbon ages have been determined on terrestrial macrofossils selected from the annually laminated sediments of lake Holzmaar (Germany). The radiocarbon chronology of this lake covers the last 12.6 ka. Comparison of the radiocarbon dated varve chronology with tree ring data shows that an additional 878 years have to be added to the varve chronology. The corrected 14C varve chronology of Holzmaar reaches back to ca. 13.8 ka cal. BP and compares favourably with the results from Soppensee (Switzerland) (Hajdas et al., 1993). The corrected ages for the onset and the end of the Younger Dryas biozone are 11,940 cal. BP and 11,490 cal. BP, respectively. The ash layer of the Laacher See volcanic eruption is dated at 12,201 ± 224 cal. BP and the Ulmener Tephra layer is dated at 10,904 cal. BP.

Url:
DOI: 10.1016/0277-3791(94)00123-S

Links to Exploration step

ISTEX:407779F2CAB4DA1ACB2103027936B0576DDA089E

Le document en format XML

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<div type="abstract" xml:lang="en">AMS radiocarbon ages have been determined on terrestrial macrofossils selected from the annually laminated sediments of lake Holzmaar (Germany). The radiocarbon chronology of this lake covers the last 12.6 ka. Comparison of the radiocarbon dated varve chronology with tree ring data shows that an additional 878 years have to be added to the varve chronology. The corrected 14C varve chronology of Holzmaar reaches back to ca. 13.8 ka cal. BP and compares favourably with the results from Soppensee (Switzerland) (Hajdas et al., 1993). The corrected ages for the onset and the end of the Younger Dryas biozone are 11,940 cal. BP and 11,490 cal. BP, respectively. The ash layer of the Laacher See volcanic eruption is dated at 12,201 ± 224 cal. BP and the Ulmener Tephra layer is dated at 10,904 cal. BP.</div>
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<ce:simple-para>AMS radiocarbon ages have been determined on terrestrial macrofossils selected from the annually laminated sediments of lake Holzmaar (Germany). The radiocarbon chronology of this lake covers the last 12.6 ka. Comparison of the radiocarbon dated varve chronology with tree ring data shows that an additional 878 years have to be added to the varve chronology. The corrected
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<role>
<roleTerm type="text">author</roleTerm>
</role>
</name>
<name type="personal">
<namePart type="given">Martin</namePart>
<namePart type="family">Suter</namePart>
<affiliation>Institut fur Teilchenphysik, ETH Hönggerberg, CH-8093 Zürich, Switzerland</affiliation>
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<roleTerm type="text">author</roleTerm>
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<publisher>ELSEVIER</publisher>
<dateIssued encoding="w3cdtf">1995</dateIssued>
<copyrightDate encoding="w3cdtf">1995</copyrightDate>
</originInfo>
<language>
<languageTerm type="code" authority="iso639-2b">eng</languageTerm>
<languageTerm type="code" authority="rfc3066">en</languageTerm>
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<abstract lang="en">AMS radiocarbon ages have been determined on terrestrial macrofossils selected from the annually laminated sediments of lake Holzmaar (Germany). The radiocarbon chronology of this lake covers the last 12.6 ka. Comparison of the radiocarbon dated varve chronology with tree ring data shows that an additional 878 years have to be added to the varve chronology. The corrected 14C varve chronology of Holzmaar reaches back to ca. 13.8 ka cal. BP and compares favourably with the results from Soppensee (Switzerland) (Hajdas et al., 1993). The corrected ages for the onset and the end of the Younger Dryas biozone are 11,940 cal. BP and 11,490 cal. BP, respectively. The ash layer of the Laacher See volcanic eruption is dated at 12,201 ± 224 cal. BP and the Ulmener Tephra layer is dated at 10,904 cal. BP.</abstract>
<relatedItem type="host">
<titleInfo>
<title>Quaternary Science Reviews</title>
</titleInfo>
<titleInfo type="abbreviated">
<title>JQSR</title>
</titleInfo>
<genre type="journal">journal</genre>
<originInfo>
<dateIssued encoding="w3cdtf">1995</dateIssued>
</originInfo>
<identifier type="ISSN">0277-3791</identifier>
<identifier type="PII">S0277-3791(00)X0009-1</identifier>
<part>
<date>1995</date>
<detail type="volume">
<number>14</number>
<caption>vol.</caption>
</detail>
<detail type="issue">
<number>2</number>
<caption>no.</caption>
</detail>
<extent unit="issue pages">
<start>101</start>
<end>207</end>
</extent>
<extent unit="pages">
<start>137</start>
<end>143</end>
</extent>
</part>
</relatedItem>
<identifier type="istex">407779F2CAB4DA1ACB2103027936B0576DDA089E</identifier>
<identifier type="DOI">10.1016/0277-3791(94)00123-S</identifier>
<identifier type="PII">0277-3791(94)00123-S</identifier>
<recordInfo>
<recordContentSource>ELSEVIER</recordContentSource>
</recordInfo>
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