PLEISTOCENE–HOLOCENE TRANSITION IN BENELUX
Identifieur interne : 000D86 ( Main/Corpus ); précédent : 000D85; suivant : 000D87PLEISTOCENE–HOLOCENE TRANSITION IN BENELUX
Auteurs : Marc De Bie ; Pierre M. VermeerschSource :
- Quaternary International [ 1040-6182 ] ; 1998.
Abstract
In Benelux (Belgium, The Netherlands, and Luxembourg), considerable progress in Late Glacial and Early Postglacial archaeological and environmental research has been made during the last decade. A substantial part of this paper discusses new evidence on the chronology of the industries which occupied the southern part of Benelux. Dating the occupations from the sandy North is still problematic. Long after the glacial maximum, during which the area remained uninhabited, the south of Benelux was visited by Magdalenian hunter-gatherers, while Hamburgian settlements were present in the North. The significance of the continental ‘Creswellian’ is debated. During the Allerød Interstadial, Federmesser groups occupied most of the area, abandoning it with the onset of the Younger Dryas. The presence of the Ahrensburgian during that stadial may have been punctuated. New elements were introduced, and were maintained during the development of the Preboreal Early Mesolithic, which eventually colonised the entire region. Throughout this sequence, changes in material culture and related subsistence activities are evident. In view of the major problems concerning the quality of the chrono-ecological data, this paper can only suggest provisional explanations in terms of human reactions to changing environmental conditions.
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DOI: 10.1016/S1040-6182(97)00052-9
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A substantial part of this paper discusses new evidence on the chronology of the industries which occupied the southern part of Benelux. Dating the occupations from the sandy North is still problematic. Long after the glacial maximum, during which the area remained uninhabited, the south of Benelux was visited by Magdalenian hunter-gatherers, while Hamburgian settlements were present in the North. The significance of the continental ‘Creswellian’ is debated. During the Allerød Interstadial, Federmesser groups occupied most of the area, abandoning it with the onset of the Younger Dryas. The presence of the Ahrensburgian during that stadial may have been punctuated. New elements were introduced, and were maintained during the development of the Preboreal Early Mesolithic, which eventually colonised the entire region. Throughout this sequence, changes in material culture and related subsistence activities are evident. In view of the major problems concerning the quality of the chrono-ecological data, this paper can only suggest provisional explanations in terms of human reactions to changing environmental conditions.</div></front></TEI><istex><corpusName>elsevier</corpusName><author><json:item><name>Marc De Bie</name><affiliations><json:string>Instituut voor het Archeologisch Patrimonium, Vlaamse Gemeenschap, Doornveld 1-b30, B-1731 Asse-Zellik & Laboratorium voor Prehistorie, Redingenstraat 16, B-3000 Leuven, Belgium</json:string></affiliations></json:item><json:item><name>Pierre M. 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During the Allerød Interstadial, Federmesser groups occupied most of the area, abandoning it with the onset of the Younger Dryas. The presence of the Ahrensburgian during that stadial may have been punctuated. New elements were introduced, and were maintained during the development of the Preboreal Early Mesolithic, which eventually colonised the entire region. Throughout this sequence, changes in material culture and related subsistence activities are evident. 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A substantial part of this paper discusses new evidence on the chronology of the industries which occupied the southern part of Benelux. Dating the occupations from the sandy North is still problematic. Long after the glacial maximum, during which the area remained uninhabited, the south of Benelux was visited by Magdalenian hunter-gatherers, while Hamburgian settlements were present in the North. The significance of the continental ‘Creswellian’ is debated. During the Allerød Interstadial, Federmesser groups occupied most of the area, abandoning it with the onset of the Younger Dryas. The presence of the Ahrensburgian during that stadial may have been punctuated. New elements were introduced, and were maintained during the development of the Preboreal Early Mesolithic, which eventually colonised the entire region. Throughout this sequence, changes in material culture and related subsistence activities are evident. In view of the major problems concerning the quality of the chrono-ecological data, this paper can only suggest provisional explanations in terms of human reactions to changing environmental conditions.</p></abstract></profileDesc><revisionDesc><change when="1998">Published</change><change xml:id="refBibs-istex" who="#ISTEX-API" when="2016-3-4">References added</change></revisionDesc></teiHeader></istex:fulltextTEI><json:item><original>false</original><mimetype>text/plain</mimetype><extension>txt</extension><uri>https://api.istex.fr/document/5D7FFF727B0F59DF202A652B75071ED3F6FFC4AE/fulltext/txt</uri></json:item></fulltext><metadata><istex:metadataXml wicri:clean="Elsevier converted-article found"><istex:xmlDeclaration>version="1.0" encoding="utf-8"</istex:xmlDeclaration><istex:docType PUBLIC="-//ES//DTD journal article DTD version 4.5.2//EN//XML" URI="art452.dtd" name="istex:docType"></istex:docType><istex:document><converted-article version="4.5.2" docsubtype="fla"><item-info><jid>JQI</jid><aid>301</aid><ce:pii>S1040-6182(97)00052-9</ce:pii><ce:doi>10.1016/S1040-6182(97)00052-9</ce:doi><ce:copyright type="joint" year="1998">INQUA/Elsevier Science Ltd</ce:copyright></item-info><head><ce:title>PLEISTOCENE–HOLOCENE TRANSITION IN BENELUX</ce:title><ce:author-group><ce:author><ce:given-name>Marc</ce:given-name><ce:surname>De Bie</ce:surname><ce:cross-ref refid="ORFA"><ce:sup>∗</ce:sup></ce:cross-ref></ce:author><ce:author><ce:given-name>Pierre M.</ce:given-name><ce:surname>Vermeersch</ce:surname><ce:cross-ref refid="ORFB"><ce:sup>b</ce:sup></ce:cross-ref></ce:author><ce:affiliation id="ORFA"><ce:label>∗</ce:label><ce:textfn>Instituut voor het Archeologisch Patrimonium, Vlaamse Gemeenschap, Doornveld 1-b30, B-1731 Asse-Zellik & Laboratorium voor Prehistorie, Redingenstraat 16, B-3000 Leuven, Belgium</ce:textfn></ce:affiliation><ce:affiliation id="ORFB"><ce:label>b</ce:label><ce:textfn>Laboratorium voor Prehistorie, Katholieke Universiteit te Leuven, Redingenstraat 16, B-3000 Leuven, Belgium</ce:textfn></ce:affiliation></ce:author-group><ce:abstract><ce:section-title>Abstract</ce:section-title><ce:abstract-sec><ce:simple-para>In Benelux (Belgium, The Netherlands, and Luxembourg), considerable progress in Late Glacial and Early Postglacial archaeological and environmental research has been made during the last decade. A substantial part of this paper discusses new evidence on the chronology of the industries which occupied the southern part of Benelux. Dating the occupations from the sandy North is still problematic.</ce:simple-para><ce:simple-para>Long after the glacial maximum, during which the area remained uninhabited, the south of Benelux was visited by Magdalenian hunter-gatherers, while Hamburgian settlements were present in the North. The significance of the continental ‘Creswellian’ is debated. During the Allerød Interstadial, <ce:italic>Federmesser</ce:italic> groups occupied most of the area, abandoning it with the onset of the Younger Dryas. The presence of the Ahrensburgian during that stadial may have been punctuated. New elements were introduced, and were maintained during the development of the Preboreal Early Mesolithic, which eventually colonised the entire region. Throughout this sequence, changes in material culture and related subsistence activities are evident. In view of the major problems concerning the quality of the chrono-ecological data, this paper can only suggest provisional explanations in terms of human reactions to changing environmental conditions.</ce:simple-para></ce:abstract-sec></ce:abstract></head></converted-article></istex:document></istex:metadataXml><mods version="3.6"><titleInfo><title>PLEISTOCENE–HOLOCENE TRANSITION IN BENELUX</title></titleInfo><titleInfo type="alternative" contentType="CDATA"><title>PLEISTOCENE–HOLOCENE TRANSITION IN BENELUX</title></titleInfo><name type="personal"><namePart type="given">Marc</namePart><namePart type="family">De Bie</namePart><affiliation>Instituut voor het Archeologisch Patrimonium, Vlaamse Gemeenschap, Doornveld 1-b30, B-1731 Asse-Zellik & Laboratorium voor Prehistorie, Redingenstraat 16, B-3000 Leuven, Belgium</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Pierre M.</namePart><namePart type="family">Vermeersch</namePart><affiliation>Laboratorium voor Prehistorie, Katholieke Universiteit te Leuven, Redingenstraat 16, B-3000 Leuven, Belgium</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="research-article" displayLabel="Full-length article"></genre><originInfo><publisher>ELSEVIER</publisher><dateIssued encoding="w3cdtf">1998</dateIssued><copyrightDate encoding="w3cdtf">1998</copyrightDate></originInfo><language><languageTerm type="code" authority="iso639-2b">eng</languageTerm><languageTerm type="code" authority="rfc3066">en</languageTerm></language><physicalDescription><internetMediaType>text/html</internetMediaType></physicalDescription><abstract lang="en">In Benelux (Belgium, The Netherlands, and Luxembourg), considerable progress in Late Glacial and Early Postglacial archaeological and environmental research has been made during the last decade. A substantial part of this paper discusses new evidence on the chronology of the industries which occupied the southern part of Benelux. Dating the occupations from the sandy North is still problematic. Long after the glacial maximum, during which the area remained uninhabited, the south of Benelux was visited by Magdalenian hunter-gatherers, while Hamburgian settlements were present in the North. The significance of the continental ‘Creswellian’ is debated. During the Allerød Interstadial, Federmesser groups occupied most of the area, abandoning it with the onset of the Younger Dryas. The presence of the Ahrensburgian during that stadial may have been punctuated. New elements were introduced, and were maintained during the development of the Preboreal Early Mesolithic, which eventually colonised the entire region. Throughout this sequence, changes in material culture and related subsistence activities are evident. 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