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Stratigraphy and dating of Middle Pleistocene sediments from Rodderberg, Germany
ABSTRACT The stratigraphy and dating of lacustrine sediments and loess derivatives from Rodderberg, a crater of the East Eifel Volcanic Field in Germany, is based on luminescence dating and incorporates radiocarbon ages, fingerprinting of key tephra layers of the East Eifel Volcanic Field (Rieden Te...
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Published in: | Journal of quaternary science 2024-10, Vol.39 (7), p.1011-1030 |
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creator | Zolitschka, Bernd Preusser, Frank Zhang, Junjie Hogrefe, Ines Froitzheim, Nikolaus Böning, Philipp Schläfli, Patrick Bittmann, Felix Binot, Franz Frechen, Manfred |
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The stratigraphy and dating of lacustrine sediments and loess derivatives from Rodderberg, a crater of the East Eifel Volcanic Field in Germany, is based on luminescence dating and incorporates radiocarbon ages, fingerprinting of key tephra layers of the East Eifel Volcanic Field (Rieden Tephra, Hüttenberg Tephra, Laacher See Tephra), pollen stratigraphy, varve counting data, and a correlative age–depth model. These methods yield a robust age–depth model for the last 258 ka. Beyond this, luminescence ages differ from tephra‐derived ages. In light of the apparent presence of the Rieden Tephra, the lowermost interglacial is assigned to Marine Isotope Stage (MIS) 11 or 420 ka. This provides a high‐resolution record of environmental conditions representing an analogue for the Holocene, characterized by a warming planet. However, new luminescence ages may indicate a younger age for basal sediments, with the lowermost interglacial representing MIS 9. Both age–depth models constrain regional environmental changes during the Middle Pleistocene controlled by global climate variations. For the hydrologically closed nature of the Rodderberg crater, with limited pathways for sediment inflow and erosional export, these results shed new light on the continuity of long Middle Pleistocene records. |
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The stratigraphy and dating of lacustrine sediments and loess derivatives from Rodderberg, a crater of the East Eifel Volcanic Field in Germany, is based on luminescence dating and incorporates radiocarbon ages, fingerprinting of key tephra layers of the East Eifel Volcanic Field (Rieden Tephra, Hüttenberg Tephra, Laacher See Tephra), pollen stratigraphy, varve counting data, and a correlative age–depth model. These methods yield a robust age–depth model for the last 258 ka. Beyond this, luminescence ages differ from tephra‐derived ages. In light of the apparent presence of the Rieden Tephra, the lowermost interglacial is assigned to Marine Isotope Stage (MIS) 11 or 420 ka. This provides a high‐resolution record of environmental conditions representing an analogue for the Holocene, characterized by a warming planet. However, new luminescence ages may indicate a younger age for basal sediments, with the lowermost interglacial representing MIS 9. Both age–depth models constrain regional environmental changes during the Middle Pleistocene controlled by global climate variations. For the hydrologically closed nature of the Rodderberg crater, with limited pathways for sediment inflow and erosional export, these results shed new light on the continuity of long Middle Pleistocene records.</description><identifier>ISSN: 0267-8179</identifier><identifier>EISSN: 1099-1417</identifier><identifier>DOI: 10.1002/jqs.3654</identifier><language>eng</language><publisher>Chichester: Wiley Subscription Services, Inc</publisher><subject>Age ; Carbon 14 ; Climate models ; Climate variations ; Dating ; East Eifel Volcanic Field ; Environmental changes ; Environmental conditions ; Fingerprinting ; Global climate ; Holocene ; Lacustrine sediments ; Loess ; loess derivates ; Luminescence ; luminescence dating ; Middle Pleistocene ; Pleistocene ; Pollen ; Radiocarbon dating ; Radiometric dating ; Sediments ; Stratigraphy ; Volcanic fields</subject><ispartof>Journal of quaternary science, 2024-10, Vol.39 (7), p.1011-1030</ispartof><rights>2024 The Authors Published by John Wiley & Sons Ltd</rights><rights>2024. This article is published under http://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><cites>FETCH-LOGICAL-c2184-db0c58075aeacc457da4d426f9692787b8bd1dcdb16d62604fa7713c7095548e3</cites><orcidid>0000-0001-8256-0420</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,27903,27904</link.rule.ids></links><search><creatorcontrib>Zolitschka, Bernd</creatorcontrib><creatorcontrib>Preusser, Frank</creatorcontrib><creatorcontrib>Zhang, Junjie</creatorcontrib><creatorcontrib>Hogrefe, Ines</creatorcontrib><creatorcontrib>Froitzheim, Nikolaus</creatorcontrib><creatorcontrib>Böning, Philipp</creatorcontrib><creatorcontrib>Schläfli, Patrick</creatorcontrib><creatorcontrib>Bittmann, Felix</creatorcontrib><creatorcontrib>Binot, Franz</creatorcontrib><creatorcontrib>Frechen, Manfred</creatorcontrib><title>Stratigraphy and dating of Middle Pleistocene sediments from Rodderberg, Germany</title><title>Journal of quaternary science</title><description>ABSTRACT
The stratigraphy and dating of lacustrine sediments and loess derivatives from Rodderberg, a crater of the East Eifel Volcanic Field in Germany, is based on luminescence dating and incorporates radiocarbon ages, fingerprinting of key tephra layers of the East Eifel Volcanic Field (Rieden Tephra, Hüttenberg Tephra, Laacher See Tephra), pollen stratigraphy, varve counting data, and a correlative age–depth model. These methods yield a robust age–depth model for the last 258 ka. Beyond this, luminescence ages differ from tephra‐derived ages. In light of the apparent presence of the Rieden Tephra, the lowermost interglacial is assigned to Marine Isotope Stage (MIS) 11 or 420 ka. This provides a high‐resolution record of environmental conditions representing an analogue for the Holocene, characterized by a warming planet. However, new luminescence ages may indicate a younger age for basal sediments, with the lowermost interglacial representing MIS 9. Both age–depth models constrain regional environmental changes during the Middle Pleistocene controlled by global climate variations. For the hydrologically closed nature of the Rodderberg crater, with limited pathways for sediment inflow and erosional export, these results shed new light on the continuity of long Middle Pleistocene records.</description><subject>Age</subject><subject>Carbon 14</subject><subject>Climate models</subject><subject>Climate variations</subject><subject>Dating</subject><subject>East Eifel Volcanic Field</subject><subject>Environmental changes</subject><subject>Environmental conditions</subject><subject>Fingerprinting</subject><subject>Global climate</subject><subject>Holocene</subject><subject>Lacustrine sediments</subject><subject>Loess</subject><subject>loess derivates</subject><subject>Luminescence</subject><subject>luminescence dating</subject><subject>Middle Pleistocene</subject><subject>Pleistocene</subject><subject>Pollen</subject><subject>Radiocarbon dating</subject><subject>Radiometric dating</subject><subject>Sediments</subject><subject>Stratigraphy</subject><subject>Volcanic fields</subject><issn>0267-8179</issn><issn>1099-1417</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2024</creationdate><recordtype>article</recordtype><sourceid>24P</sourceid><recordid>eNp10E1LAzEQBuAgCtYq-BMCXjy4NbObTbJHKVqVitXqOWST2bplP9pki-y_d2u9ehqGeXgHXkIugU2Asfh2vQ2TRKT8iIyAZVkEHOQxGbFYyEiBzE7JWQhrxoabYCOyWHbedOXKm81XT03jqBvWZkXbgr6UzlVIFxWWoWstNkgDurLGpgu08G1N31vn0OfoVzd0hr42TX9OTgpTBbz4m2Py-XD_MX2M5q-zp-ndPLIxKB65nNlUMZkaNNbyVDrDHY9FkYkslkrmKnfgrMtBOBELxgsjJSRWsixNucJkTK4OuRvfbncYOr1ud74ZXuoEABIFMeeDuj4o69sQPBZ648va-F4D0_u-9NCX3vc10OhAv8sK-3-dfn5b_vof6HJruQ</recordid><startdate>202410</startdate><enddate>202410</enddate><creator>Zolitschka, Bernd</creator><creator>Preusser, Frank</creator><creator>Zhang, Junjie</creator><creator>Hogrefe, Ines</creator><creator>Froitzheim, Nikolaus</creator><creator>Böning, Philipp</creator><creator>Schläfli, Patrick</creator><creator>Bittmann, Felix</creator><creator>Binot, Franz</creator><creator>Frechen, Manfred</creator><general>Wiley Subscription Services, Inc</general><scope>24P</scope><scope>WIN</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7ST</scope><scope>7TG</scope><scope>8FD</scope><scope>C1K</scope><scope>FR3</scope><scope>KL.</scope><scope>KR7</scope><scope>SOI</scope><orcidid>https://orcid.org/0000-0001-8256-0420</orcidid></search><sort><creationdate>202410</creationdate><title>Stratigraphy and dating of Middle Pleistocene sediments from Rodderberg, Germany</title><author>Zolitschka, Bernd ; 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The stratigraphy and dating of lacustrine sediments and loess derivatives from Rodderberg, a crater of the East Eifel Volcanic Field in Germany, is based on luminescence dating and incorporates radiocarbon ages, fingerprinting of key tephra layers of the East Eifel Volcanic Field (Rieden Tephra, Hüttenberg Tephra, Laacher See Tephra), pollen stratigraphy, varve counting data, and a correlative age–depth model. These methods yield a robust age–depth model for the last 258 ka. Beyond this, luminescence ages differ from tephra‐derived ages. In light of the apparent presence of the Rieden Tephra, the lowermost interglacial is assigned to Marine Isotope Stage (MIS) 11 or 420 ka. This provides a high‐resolution record of environmental conditions representing an analogue for the Holocene, characterized by a warming planet. However, new luminescence ages may indicate a younger age for basal sediments, with the lowermost interglacial representing MIS 9. Both age–depth models constrain regional environmental changes during the Middle Pleistocene controlled by global climate variations. For the hydrologically closed nature of the Rodderberg crater, with limited pathways for sediment inflow and erosional export, these results shed new light on the continuity of long Middle Pleistocene records.</abstract><cop>Chichester</cop><pub>Wiley Subscription Services, Inc</pub><doi>10.1002/jqs.3654</doi><tpages>20</tpages><orcidid>https://orcid.org/0000-0001-8256-0420</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Age Carbon 14 Climate models Climate variations Dating East Eifel Volcanic Field Environmental changes Environmental conditions Fingerprinting Global climate Holocene Lacustrine sediments Loess loess derivates Luminescence luminescence dating Middle Pleistocene Pleistocene Pollen Radiocarbon dating Radiometric dating Sediments Stratigraphy Volcanic fields |
title | Stratigraphy and dating of Middle Pleistocene sediments from Rodderberg, Germany |
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