Pleistocene land—sea correlations I. Europe
Identifieur interne : 001A88 ( Istex/Corpus ); précédent : 001A87; suivant : 001A89Pleistocene land—sea correlations I. Europe
Auteurs : G. J. KuklaSource :
- Earth-Science Reviews [ 0012-8252 ] ; 1977.
Abstract
Abstract: At least seventeen glacials and seventeen interglacials occurred in Europe over the last 1.7 million years. Eight glacials and eight interglacials are of Brunhes age. Only four glacials and three interglacials are recognized by classical Alpine and north European subdivisions of the Pleistocene. The classical units are correlated with continuous oxygen isotope records from the oceans using loess sections and terraces as a link (cf. Fig. 21). It is found that: (1) the terraces representing the four Alpine “glacial” stages fully cover the last 0.8 million years but correspond to both glacial and interglacial climates; (2) the Alpine “interglacial” stages do not represent episodes of interglacial climate but probably intervals of accelerated crustal movements; (3) the physical evidence on which the north European classical subdivision is based accounts for only about 15% of the time represented. This has led to serious miscorrelations.It is urgently recommended to abandon the classical terminology in all interregional correlations and to base the chronostratigraphic subdivision of Pleistocene on the18O record of deep-sea sediments.
Url:
DOI: 10.1016/0012-8252(77)90125-8
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<front><div type="abstract" xml:lang="en">Abstract: At least seventeen glacials and seventeen interglacials occurred in Europe over the last 1.7 million years. Eight glacials and eight interglacials are of Brunhes age. Only four glacials and three interglacials are recognized by classical Alpine and north European subdivisions of the Pleistocene. The classical units are correlated with continuous oxygen isotope records from the oceans using loess sections and terraces as a link (cf. Fig. 21). It is found that: (1) the terraces representing the four Alpine “glacial” stages fully cover the last 0.8 million years but correspond to both glacial and interglacial climates; (2) the Alpine “interglacial” stages do not represent episodes of interglacial climate but probably intervals of accelerated crustal movements; (3) the physical evidence on which the north European classical subdivision is based accounts for only about 15% of the time represented. This has led to serious miscorrelations.It is urgently recommended to abandon the classical terminology in all interregional correlations and to base the chronostratigraphic subdivision of Pleistocene on the18O record of deep-sea sediments.</div>
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<abstract>Abstract: At least seventeen glacials and seventeen interglacials occurred in Europe over the last 1.7 million years. Eight glacials and eight interglacials are of Brunhes age. Only four glacials and three interglacials are recognized by classical Alpine and north European subdivisions of the Pleistocene. The classical units are correlated with continuous oxygen isotope records from the oceans using loess sections and terraces as a link (cf. Fig. 21). It is found that: (1) the terraces representing the four Alpine “glacial” stages fully cover the last 0.8 million years but correspond to both glacial and interglacial climates; (2) the Alpine “interglacial” stages do not represent episodes of interglacial climate but probably intervals of accelerated crustal movements; (3) the physical evidence on which the north European classical subdivision is based accounts for only about 15% of the time represented. This has led to serious miscorrelations.It is urgently recommended to abandon the classical terminology in all interregional correlations and to base the chronostratigraphic subdivision of Pleistocene on the18O record of deep-sea sediments.</abstract>
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<abstract xml:lang="en"><p>Abstract: At least seventeen glacials and seventeen interglacials occurred in Europe over the last 1.7 million years. Eight glacials and eight interglacials are of Brunhes age. Only four glacials and three interglacials are recognized by classical Alpine and north European subdivisions of the Pleistocene. The classical units are correlated with continuous oxygen isotope records from the oceans using loess sections and terraces as a link (cf. Fig. 21). It is found that: (1) the terraces representing the four Alpine “glacial” stages fully cover the last 0.8 million years but correspond to both glacial and interglacial climates; (2) the Alpine “interglacial” stages do not represent episodes of interglacial climate but probably intervals of accelerated crustal movements; (3) the physical evidence on which the north European classical subdivision is based accounts for only about 15% of the time represented. This has led to serious miscorrelations.It is urgently recommended to abandon the classical terminology in all interregional correlations and to base the chronostratigraphic subdivision of Pleistocene on the18O record of deep-sea sediments.</p>
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<head><ce:title>Pleistocene land—sea correlations I. Europe</ce:title>
<ce:author-group><ce:author><ce:given-name>G.J.</ce:given-name>
<ce:surname>Kukla</ce:surname>
</ce:author>
</ce:author-group>
<ce:date-received day="3" month="8" year="1977"></ce:date-received>
<ce:abstract id="ab1" class="author" xml:lang="en"><ce:section-title>Abstract</ce:section-title>
<ce:abstract-sec><ce:simple-para>At least seventeen glacials and seventeen interglacials occurred in Europe over the last 1.7 million years. Eight glacials and eight interglacials are of Brunhes age. Only four glacials and three interglacials are recognized by classical Alpine and north European subdivisions of the Pleistocene. The classical units are correlated with continuous oxygen isotope records from the oceans using loess sections and terraces as a link (cf. Fig. 21). It is found that: (1) the terraces representing the four Alpine “glacial” stages fully cover the last 0.8 million years but correspond to both glacial and interglacial climates; (2) the Alpine “interglacial” stages do not represent episodes of interglacial climate but probably intervals of accelerated crustal movements; (3) the physical evidence on which the north European classical subdivision is based accounts for only about 15% of the time represented. This has led to serious miscorrelations.</ce:simple-para>
<ce:simple-para>It is urgently recommended to abandon the classical terminology in all interregional correlations and to base the chronostratigraphic subdivision of Pleistocene on the<ce:sup loc="pre">18</ce:sup>
O record of deep-sea sediments.</ce:simple-para>
</ce:abstract-sec>
</ce:abstract>
</head>
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</article>
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<mods version="3.6"><titleInfo lang="en"><title>Pleistocene land—sea correlations I. Europe</title>
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<titleInfo type="alternative" lang="en" contentType="CDATA"><title>Pleistocene land—sea correlations I. Europe</title>
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<name type="personal"><namePart type="given">G.J.</namePart>
<namePart type="family">Kukla</namePart>
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<copyrightDate encoding="w3cdtf">1977</copyrightDate>
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<abstract lang="en">Abstract: At least seventeen glacials and seventeen interglacials occurred in Europe over the last 1.7 million years. Eight glacials and eight interglacials are of Brunhes age. Only four glacials and three interglacials are recognized by classical Alpine and north European subdivisions of the Pleistocene. The classical units are correlated with continuous oxygen isotope records from the oceans using loess sections and terraces as a link (cf. Fig. 21). It is found that: (1) the terraces representing the four Alpine “glacial” stages fully cover the last 0.8 million years but correspond to both glacial and interglacial climates; (2) the Alpine “interglacial” stages do not represent episodes of interglacial climate but probably intervals of accelerated crustal movements; (3) the physical evidence on which the north European classical subdivision is based accounts for only about 15% of the time represented. This has led to serious miscorrelations.It is urgently recommended to abandon the classical terminology in all interregional correlations and to base the chronostratigraphic subdivision of Pleistocene on the18O record of deep-sea sediments.</abstract>
<relatedItem type="host"><titleInfo><title>Earth-Science Reviews</title>
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<titleInfo type="abbreviated"><title>EARTH</title>
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<genre type="journal">journal</genre>
<originInfo><dateIssued encoding="w3cdtf">197712</dateIssued>
</originInfo>
<identifier type="ISSN">0012-8252</identifier>
<identifier type="PII">S0012-8252(00)X0121-3</identifier>
<part><date>197712</date>
<detail type="volume"><number>13</number>
<caption>vol.</caption>
</detail>
<detail type="issue"><number>4</number>
<caption>no.</caption>
</detail>
<extent unit="issue pages"><start>307</start>
<end>409</end>
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<extent unit="pages"><start>307</start>
<end>374</end>
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<identifier type="istex">2FC40EF60227BA2F5EB7712A068D77B69E952E91</identifier>
<identifier type="DOI">10.1016/0012-8252(77)90125-8</identifier>
<identifier type="PII">0012-8252(77)90125-8</identifier>
<identifier type="ArticleID">77901258</identifier>
<accessCondition type="use and reproduction" contentType="copyright">©1977 Elsevier Scientific Publishing Company</accessCondition>
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