Vegetation and climate during the Weichselian Early Glacial and Pleniglacial in the Niederlausitz, eastern Germany — macrofossil and pollen evidence
Identifieur interne : 000D84 ( Istex/Corpus ); précédent : 000D83; suivant : 000D85Vegetation and climate during the Weichselian Early Glacial and Pleniglacial in the Niederlausitz, eastern Germany — macrofossil and pollen evidence
Auteurs : Johanna A. A. Bos ; Sjoerd J. P. Bohncke ; Cornelis Kasse ; Jef VandenbergheSource :
- Journal of Quaternary Science [ 0267-8179 ] ; 2001-03.
English descriptors
Abstract
Cryoturbated organic beds and channel fills, intercalated with sandy and gravelly fluvial units, have been studied in an opencast brown‐coal mine near Nochten (Niederlausitz), eastern Germany. The fluvial–aeolian sequence covers parts of the Early, Pleni‐ and Late‐glacial. The detailed chronology is based on 11 radiocarbon and 12 OSL dates, covering the period between ca. 100 kyr and 11 kyr BP. Basal peat deposits are correlated with an Early Weichselian interstadial. During this period boreal forests were present and minimum mean summer temperatures were > 13°C. Early Pleniglacial deposits are absent. The Middle and Late Pleniglacial environments were treeless and different types of tundra vegetation can be recognised. Minimum mean summer temperatures varied between 10 and 15°C. Vegetation and climate is reconstructed in detail for the periods around 34–38 kyr BP and 24–25 kyr BP. Around 34–38 ka, a mixture between a low shrub tundra and a cottongrass tussock–subshrub tundra was present. The botanical and sedimentological data suggest that from the Middle to the Late Pleniglacial, the climate became more continental, aridity and wind strength increased, and the role of a protecting winter snow cover decreased. A sedge–grass–moss tundra dominated around 24 and 25 kyr BP. Copyright © 2001 John Wiley & Sons, Ltd.
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DOI: 10.1002/jqs.606
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ISTEX:70DDDC6A036A62AB9CC78E63209894B06DEDD5DBLe document en format XML
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A." last="Bos">Johanna A. A. Bos</name><affiliation><mods:affiliation>Interuniversitair Centrum voor Geo‐ecologisch onderzoek (ICG), Department of Quaternary Geology and Geomorphology, Faculty of Earth Sciences, Vrije Universiteit, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands</mods:affiliation></affiliation><affiliation><mods:affiliation>Interuniversitair Centrum voor Geo‐ecologisch onderzoek (ICG), Department of Quaternary Geology and Geomorphology, Faculty of Earth Sciences, Vrije Universiteit, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands.</mods:affiliation></affiliation></author><author><name sortKey="Bohncke, Sjoerd J P" sort="Bohncke, Sjoerd J P" uniqKey="Bohncke S" first="Sjoerd J. P." last="Bohncke">Sjoerd J. P. Bohncke</name><affiliation><mods:affiliation>Interuniversitair Centrum voor Geo‐ecologisch onderzoek (ICG), Department of Quaternary Geology and Geomorphology, Faculty of Earth Sciences, Vrije Universiteit, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands</mods:affiliation></affiliation></author><author><name sortKey="Kasse, Cornelis" sort="Kasse, Cornelis" uniqKey="Kasse C" first="Cornelis" last="Kasse">Cornelis Kasse</name><affiliation><mods:affiliation>Interuniversitair Centrum voor Geo‐ecologisch onderzoek (ICG), Department of Quaternary Geology and Geomorphology, Faculty of Earth Sciences, Vrije Universiteit, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands</mods:affiliation></affiliation></author><author><name sortKey="Vandenberghe, Jef" sort="Vandenberghe, Jef" uniqKey="Vandenberghe J" first="Jef" last="Vandenberghe">Jef Vandenberghe</name><affiliation><mods:affiliation>Interuniversitair Centrum voor Geo‐ecologisch onderzoek (ICG), Department of Quaternary Geology and Geomorphology, Faculty of Earth Sciences, Vrije Universiteit, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands</mods:affiliation></affiliation></author></analytic><monogr></monogr><series><title level="j">Journal of Quaternary Science</title><title level="j" type="sub">Published for the Quaternary Research Association</title><title level="j" type="abbrev">J. Quaternary Sci.</title><idno type="ISSN">0267-8179</idno><idno type="eISSN">1099-1417</idno><imprint><publisher>John Wiley & Sons, Ltd.</publisher><pubPlace>Chichester, UK</pubPlace><date type="published" when="2001-03">2001-03</date><biblScope unit="volume">16</biblScope><biblScope unit="issue">3</biblScope><biblScope unit="page" from="269">269</biblScope><biblScope unit="page" to="289">289</biblScope></imprint><idno type="ISSN">0267-8179</idno></series><idno type="istex">70DDDC6A036A62AB9CC78E63209894B06DEDD5DB</idno><idno type="DOI">10.1002/jqs.606</idno><idno type="ArticleID">JQS606</idno></biblStruct></sourceDesc><seriesStmt><idno type="ISSN">0267-8179</idno></seriesStmt></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Germany</term><term>Weichselian</term><term>climate reconstruction</term><term>pollen‐ and macrofossils</term><term>tundra</term></keywords></textClass><langUsage><language ident="en">en</language></langUsage></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">Cryoturbated organic beds and channel fills, intercalated with sandy and gravelly fluvial units, have been studied in an opencast brown‐coal mine near Nochten (Niederlausitz), eastern Germany. The fluvial–aeolian sequence covers parts of the Early, Pleni‐ and Late‐glacial. The detailed chronology is based on 11 radiocarbon and 12 OSL dates, covering the period between ca. 100 kyr and 11 kyr BP. Basal peat deposits are correlated with an Early Weichselian interstadial. During this period boreal forests were present and minimum mean summer temperatures were > 13°C. Early Pleniglacial deposits are absent. The Middle and Late Pleniglacial environments were treeless and different types of tundra vegetation can be recognised. Minimum mean summer temperatures varied between 10 and 15°C. Vegetation and climate is reconstructed in detail for the periods around 34–38 kyr BP and 24–25 kyr BP. Around 34–38 ka, a mixture between a low shrub tundra and a cottongrass tussock–subshrub tundra was present. The botanical and sedimentological data suggest that from the Middle to the Late Pleniglacial, the climate became more continental, aridity and wind strength increased, and the role of a protecting winter snow cover decreased. A sedge–grass–moss tundra dominated around 24 and 25 kyr BP. Copyright © 2001 John Wiley & Sons, Ltd.</div></front></TEI><istex><corpusName>wiley</corpusName><author><json:item><name>Johanna A. A. Bos</name><affiliations><json:string>Interuniversitair Centrum voor Geo‐ecologisch onderzoek (ICG), Department of Quaternary Geology and Geomorphology, Faculty of Earth Sciences, Vrije Universiteit, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands</json:string><json:string>Interuniversitair Centrum voor Geo‐ecologisch onderzoek (ICG), Department of Quaternary Geology and Geomorphology, Faculty of Earth Sciences, Vrije Universiteit, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands.</json:string></affiliations></json:item><json:item><name>Sjoerd J. P. Bohncke</name><affiliations><json:string>Interuniversitair Centrum voor Geo‐ecologisch onderzoek (ICG), Department of Quaternary Geology and Geomorphology, Faculty of Earth Sciences, Vrije Universiteit, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands</json:string></affiliations></json:item><json:item><name>Cornelis Kasse</name><affiliations><json:string>Interuniversitair Centrum voor Geo‐ecologisch onderzoek (ICG), Department of Quaternary Geology and Geomorphology, Faculty of Earth Sciences, Vrije Universiteit, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands</json:string></affiliations></json:item><json:item><name>Jef Vandenberghe</name><affiliations><json:string>Interuniversitair Centrum voor Geo‐ecologisch onderzoek (ICG), Department of Quaternary Geology and Geomorphology, Faculty of Earth Sciences, Vrije Universiteit, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands</json:string></affiliations></json:item></author><subject><json:item><lang><json:string>eng</json:string></lang><value>Weichselian</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>pollen‐ and macrofossils</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>tundra</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>climate reconstruction</value></json:item><json:item><lang><json:string>eng</json:string></lang><value>Germany</value></json:item></subject><articleId><json:string>JQS606</json:string></articleId><language><json:string>eng</json:string></language><originalGenre><json:string>article</json:string></originalGenre><abstract>Cryoturbated organic beds and channel fills, intercalated with sandy and gravelly fluvial units, have been studied in an opencast brown‐coal mine near Nochten (Niederlausitz), eastern Germany. The fluvial–aeolian sequence covers parts of the Early, Pleni‐ and Late‐glacial. The detailed chronology is based on 11 radiocarbon and 12 OSL dates, covering the period between ca. 100 kyr and 11 kyr BP. Basal peat deposits are correlated with an Early Weichselian interstadial. During this period boreal forests were present and minimum mean summer temperatures were > 13°C. Early Pleniglacial deposits are absent. The Middle and Late Pleniglacial environments were treeless and different types of tundra vegetation can be recognised. Minimum mean summer temperatures varied between 10 and 15°C. Vegetation and climate is reconstructed in detail for the periods around 34–38 kyr BP and 24–25 kyr BP. Around 34–38 ka, a mixture between a low shrub tundra and a cottongrass tussock–subshrub tundra was present. The botanical and sedimentological data suggest that from the Middle to the Late Pleniglacial, the climate became more continental, aridity and wind strength increased, and the role of a protecting winter snow cover decreased. A sedge–grass–moss tundra dominated around 24 and 25 kyr BP. Copyright © 2001 John Wiley & Sons, Ltd.</abstract><qualityIndicators><score>7.436</score><pdfVersion>1.2</pdfVersion><pdfPageSize>598 x 846 pts</pdfPageSize><refBibsNative>true</refBibsNative><abstractCharCount>1332</abstractCharCount><pdfWordCount>12069</pdfWordCount><pdfCharCount>79828</pdfCharCount><pdfPageCount>21</pdfPageCount><abstractWordCount>203</abstractWordCount></qualityIndicators><title>Vegetation and climate during the Weichselian Early Glacial and Pleniglacial in the Niederlausitz, eastern Germany — macrofossil and pollen evidence</title><refBibs><json:item><author><json:item><name>G Aalbersberg</name></json:item><json:item><name>T Litt</name></json:item></author><host><volume>13</volume><pages><last>390</last><first>367</first></pages><author></author><title>Journal of Quaternary Science</title></host><title>Multiproxy climate reconstructions for the Eemian and Early Weichselian</title></json:item><json:item><author><json:item><name>P Adam</name></json:item></author><host><volume>78</volume><pages><last>244</last><first>237</first></pages><author></author><title>New Phytologist</title></host><title>The ecological significance of ‘Halophytes’ in the Devensian flora</title></json:item><json:item><host><author></author><title>Anderberg AL. 1994. 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A.</forename><surname>Bos</surname></persName><affiliation>Interuniversitair Centrum voor Geo‐ecologisch onderzoek (ICG), Department of Quaternary Geology and Geomorphology, Faculty of Earth Sciences, Vrije Universiteit, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands</affiliation><affiliation>Interuniversitair Centrum voor Geo‐ecologisch onderzoek (ICG), Department of Quaternary Geology and Geomorphology, Faculty of Earth Sciences, Vrije Universiteit, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands.</affiliation></author><author xml:id="author-2"><persName><forename type="first">Sjoerd J. P.</forename><surname>Bohncke</surname></persName><affiliation>Interuniversitair Centrum voor Geo‐ecologisch onderzoek (ICG), Department of Quaternary Geology and Geomorphology, Faculty of Earth Sciences, Vrije Universiteit, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands</affiliation></author><author xml:id="author-3"><persName><forename type="first">Cornelis</forename><surname>Kasse</surname></persName><affiliation>Interuniversitair Centrum voor Geo‐ecologisch onderzoek (ICG), Department of Quaternary Geology and Geomorphology, Faculty of Earth Sciences, Vrije Universiteit, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands</affiliation></author><author xml:id="author-4"><persName><forename type="first">Jef</forename><surname>Vandenberghe</surname></persName><affiliation>Interuniversitair Centrum voor Geo‐ecologisch onderzoek (ICG), Department of Quaternary Geology and Geomorphology, Faculty of Earth Sciences, Vrije Universiteit, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands</affiliation></author></analytic><monogr><title level="j">Journal of Quaternary Science</title><title level="j" type="sub">Published for the Quaternary Research Association</title><title level="j" type="abbrev">J. 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The fluvial–aeolian sequence covers parts of the Early, Pleni‐ and Late‐glacial. The detailed chronology is based on 11 radiocarbon and 12 OSL dates, covering the period between ca. 100 kyr and 11 kyr BP. Basal peat deposits are correlated with an Early Weichselian interstadial. During this period boreal forests were present and minimum mean summer temperatures were > 13°C. Early Pleniglacial deposits are absent. The Middle and Late Pleniglacial environments were treeless and different types of tundra vegetation can be recognised. Minimum mean summer temperatures varied between 10 and 15°C. Vegetation and climate is reconstructed in detail for the periods around 34–38 kyr BP and 24–25 kyr BP. Around 34–38 ka, a mixture between a low shrub tundra and a cottongrass tussock–subshrub tundra was present. The botanical and sedimentological data suggest that from the Middle to the Late Pleniglacial, the climate became more continental, aridity and wind strength increased, and the role of a protecting winter snow cover decreased. A sedge–grass–moss tundra dominated around 24 and 25 kyr BP. 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The fluvial–aeolian sequence covers parts of the Early, Pleni‐ and Late‐glacial. The detailed chronology is based on 11 radiocarbon and 12 OSL dates, covering the period between ca. 100 kyr and 11 kyr BP. Basal peat deposits are correlated with an Early Weichselian interstadial. During this period boreal forests were present and minimum mean summer temperatures were > 13°C. Early Pleniglacial deposits are absent. The Middle and Late Pleniglacial environments were treeless and different types of tundra vegetation can be recognised. Minimum mean summer temperatures varied between 10 and 15°C. Vegetation and climate is reconstructed in detail for the periods around 34–38 kyr BP and 24–25 kyr BP. Around 34–38 ka, a mixture between a low shrub tundra and a cottongrass tussock–subshrub tundra was present. The botanical and sedimentological data suggest that from the Middle to the Late Pleniglacial, the climate became more continental, aridity and wind strength increased, and the role of a protecting winter snow cover decreased. A sedge–grass–moss tundra dominated around 24 and 25 kyr BP. Copyright © 2001 John Wiley & Sons, Ltd.</p></abstract></abstractGroup></contentMeta></header></component></istex:document></istex:metadataXml><mods version="3.6"><titleInfo lang="en"><title>Vegetation and climate during the Weichselian Early Glacial and Pleniglacial in the Niederlausitz, eastern Germany — macrofossil and pollen evidence</title></titleInfo><titleInfo type="abbreviated" lang="en"><title>WEICHSELIAN VEGETATION AND CLIMATE IN EASTERN GERMANY</title></titleInfo><titleInfo type="alternative" contentType="CDATA" lang="en"><title>Vegetation and climate during the Weichselian Early Glacial and Pleniglacial in the Niederlausitz, eastern Germany — macrofossil and pollen evidence</title></titleInfo><name type="personal"><namePart type="given">Johanna A. A.</namePart><namePart type="family">Bos</namePart><affiliation>Interuniversitair Centrum voor Geo‐ecologisch onderzoek (ICG), Department of Quaternary Geology and Geomorphology, Faculty of Earth Sciences, Vrije Universiteit, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands</affiliation><affiliation>Interuniversitair Centrum voor Geo‐ecologisch onderzoek (ICG), Department of Quaternary Geology and Geomorphology, Faculty of Earth Sciences, Vrije Universiteit, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands.</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Sjoerd J. P.</namePart><namePart type="family">Bohncke</namePart><affiliation>Interuniversitair Centrum voor Geo‐ecologisch onderzoek (ICG), Department of Quaternary Geology and Geomorphology, Faculty of Earth Sciences, Vrije Universiteit, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Cornelis</namePart><namePart type="family">Kasse</namePart><affiliation>Interuniversitair Centrum voor Geo‐ecologisch onderzoek (ICG), Department of Quaternary Geology and Geomorphology, Faculty of Earth Sciences, Vrije Universiteit, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands</affiliation><role><roleTerm type="text">author</roleTerm></role></name><name type="personal"><namePart type="given">Jef</namePart><namePart type="family">Vandenberghe</namePart><affiliation>Interuniversitair Centrum voor Geo‐ecologisch onderzoek (ICG), Department of Quaternary Geology and Geomorphology, Faculty of Earth Sciences, Vrije Universiteit, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands</affiliation><role><roleTerm type="text">author</roleTerm></role></name><typeOfResource>text</typeOfResource><genre type="article" displayLabel="article"></genre><originInfo><publisher>John Wiley & Sons, Ltd.</publisher><place><placeTerm type="text">Chichester, UK</placeTerm></place><dateIssued encoding="w3cdtf">2001-03</dateIssued><copyrightDate encoding="w3cdtf">2001</copyrightDate></originInfo><language><languageTerm type="code" authority="rfc3066">en</languageTerm><languageTerm type="code" authority="iso639-2b">eng</languageTerm></language><physicalDescription><internetMediaType>text/html</internetMediaType><extent unit="figures">6</extent><extent unit="tables">3</extent><extent unit="references">94</extent></physicalDescription><abstract lang="en">Cryoturbated organic beds and channel fills, intercalated with sandy and gravelly fluvial units, have been studied in an opencast brown‐coal mine near Nochten (Niederlausitz), eastern Germany. The fluvial–aeolian sequence covers parts of the Early, Pleni‐ and Late‐glacial. The detailed chronology is based on 11 radiocarbon and 12 OSL dates, covering the period between ca. 100 kyr and 11 kyr BP. Basal peat deposits are correlated with an Early Weichselian interstadial. During this period boreal forests were present and minimum mean summer temperatures were > 13°C. Early Pleniglacial deposits are absent. The Middle and Late Pleniglacial environments were treeless and different types of tundra vegetation can be recognised. Minimum mean summer temperatures varied between 10 and 15°C. Vegetation and climate is reconstructed in detail for the periods around 34–38 kyr BP and 24–25 kyr BP. Around 34–38 ka, a mixture between a low shrub tundra and a cottongrass tussock–subshrub tundra was present. The botanical and sedimentological data suggest that from the Middle to the Late Pleniglacial, the climate became more continental, aridity and wind strength increased, and the role of a protecting winter snow cover decreased. A sedge–grass–moss tundra dominated around 24 and 25 kyr BP. Copyright © 2001 John Wiley & Sons, Ltd.</abstract><subject lang="en"><genre>keywords</genre><topic>Weichselian</topic><topic>pollen‐ and macrofossils</topic><topic>tundra</topic><topic>climate reconstruction</topic><topic>Germany</topic></subject><relatedItem type="host"><titleInfo><title>Journal of Quaternary Science</title><subTitle>Published for the Quaternary Research Association</subTitle></titleInfo><titleInfo type="abbreviated"><title>J. 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