Late Pleistocene Eifel eruptions: insights from clinopyroxene and glass geochemistry of tephra layers from Eifel Laminated Sediment Archive sediment cores
ABSTRACT The Eifel Laminated Sediment Archive (ELSA), which comprises several cores from maar lakes, includes numerous tephra layers spanning the last 140 000 years. The sediment cores are dated by 14C and thermoluminescence as well as tuned to Greenland stadial–interstadial successions. Within the...
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Veröffentlicht in: | Journal of quaternary science 2020-01, Vol.35 (1-2), p.186-198 |
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creator | Förster, Michael W. Zemlitskaya, Anastasia Otter, Laura M. Buhre, Stephan Sirocko, Frank |
description | ABSTRACT
The Eifel Laminated Sediment Archive (ELSA), which comprises several cores from maar lakes, includes numerous tephra layers spanning the last 140 000 years. The sediment cores are dated by 14C and thermoluminescence as well as tuned to Greenland stadial–interstadial successions. Within the last glacial cycle, the Eifel Volcanic Fields are source to several widespread tephra layers, namely the Laacher See, Eltville, Rambach and Rocourt Tephra. However, a corresponding source volcano was so far only identified for the Laacher See Tephra. In this study we use glass and clinopyroxene geochemistry to link the remaining tephra layers to possible eruption centers within the West and East Eifel Volcanic Fields: while we demonstrate that the Eltville Tephra originated from an earlier eruption of the Laacher See Volcano at 24 300 a bp from within the East Eifel Volcanic Field, the Rambach and Rocourt Tephras are sourced from the West Eifel Volcanic Field and erupted from Wartgesberg at 27 900 a bp and Pulvermaar at 75 000 a bp, respectively. Phases of volcanic activity peaked at 10 000–30 000 and 60 000–80 000 a bp and were thus erupted around the temperature minima of the last glacial cycle. The longest phase of dormancy between individual vents was around 30 000 years long, within the last interglacial. |
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The Eifel Laminated Sediment Archive (ELSA), which comprises several cores from maar lakes, includes numerous tephra layers spanning the last 140 000 years. The sediment cores are dated by 14C and thermoluminescence as well as tuned to Greenland stadial–interstadial successions. Within the last glacial cycle, the Eifel Volcanic Fields are source to several widespread tephra layers, namely the Laacher See, Eltville, Rambach and Rocourt Tephra. However, a corresponding source volcano was so far only identified for the Laacher See Tephra. In this study we use glass and clinopyroxene geochemistry to link the remaining tephra layers to possible eruption centers within the West and East Eifel Volcanic Fields: while we demonstrate that the Eltville Tephra originated from an earlier eruption of the Laacher See Volcano at 24 300 a bp from within the East Eifel Volcanic Field, the Rambach and Rocourt Tephras are sourced from the West Eifel Volcanic Field and erupted from Wartgesberg at 27 900 a bp and Pulvermaar at 75 000 a bp, respectively. Phases of volcanic activity peaked at 10 000–30 000 and 60 000–80 000 a bp and were thus erupted around the temperature minima of the last glacial cycle. The longest phase of dormancy between individual vents was around 30 000 years long, within the last interglacial.</description><identifier>ISSN: 0267-8179</identifier><identifier>EISSN: 1099-1417</identifier><identifier>DOI: 10.1002/jqs.3134</identifier><language>eng</language><publisher>Chichester: Wiley Subscription Services, Inc</publisher><subject>Archives & records ; ash layers ; Cores ; Dormancy ; Eifel Volcanic Fields ; Eltville Tephra ; EPMA ; Eruptions ; Geochemistry ; Glass ; Lakes ; Laminates ; Pleistocene ; Rocourt Tephra ; sediment archive ; Sediments ; Thermoluminescence ; Vents ; Volcanic activity ; Volcanic eruptions ; Volcanic fields ; Volcanoes</subject><ispartof>Journal of quaternary science, 2020-01, Vol.35 (1-2), p.186-198</ispartof><rights>2019 John Wiley & Sons, Ltd.</rights><rights>2020 John Wiley & Sons, Ltd.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c3274-9d1e447c18cb19ab934f85bfbd3ed9773b31456ef19cd372a3e13faeb94e0e013</citedby><cites>FETCH-LOGICAL-c3274-9d1e447c18cb19ab934f85bfbd3ed9773b31456ef19cd372a3e13faeb94e0e013</cites><orcidid>0000-0002-0778-5811 ; 0000-0003-0737-4497</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1002%2Fjqs.3134$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1002%2Fjqs.3134$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,780,784,1417,27924,27925,45574,45575</link.rule.ids></links><search><creatorcontrib>Förster, Michael W.</creatorcontrib><creatorcontrib>Zemlitskaya, Anastasia</creatorcontrib><creatorcontrib>Otter, Laura M.</creatorcontrib><creatorcontrib>Buhre, Stephan</creatorcontrib><creatorcontrib>Sirocko, Frank</creatorcontrib><title>Late Pleistocene Eifel eruptions: insights from clinopyroxene and glass geochemistry of tephra layers from Eifel Laminated Sediment Archive sediment cores</title><title>Journal of quaternary science</title><description>ABSTRACT
The Eifel Laminated Sediment Archive (ELSA), which comprises several cores from maar lakes, includes numerous tephra layers spanning the last 140 000 years. The sediment cores are dated by 14C and thermoluminescence as well as tuned to Greenland stadial–interstadial successions. Within the last glacial cycle, the Eifel Volcanic Fields are source to several widespread tephra layers, namely the Laacher See, Eltville, Rambach and Rocourt Tephra. However, a corresponding source volcano was so far only identified for the Laacher See Tephra. In this study we use glass and clinopyroxene geochemistry to link the remaining tephra layers to possible eruption centers within the West and East Eifel Volcanic Fields: while we demonstrate that the Eltville Tephra originated from an earlier eruption of the Laacher See Volcano at 24 300 a bp from within the East Eifel Volcanic Field, the Rambach and Rocourt Tephras are sourced from the West Eifel Volcanic Field and erupted from Wartgesberg at 27 900 a bp and Pulvermaar at 75 000 a bp, respectively. Phases of volcanic activity peaked at 10 000–30 000 and 60 000–80 000 a bp and were thus erupted around the temperature minima of the last glacial cycle. The longest phase of dormancy between individual vents was around 30 000 years long, within the last interglacial.</description><subject>Archives & records</subject><subject>ash layers</subject><subject>Cores</subject><subject>Dormancy</subject><subject>Eifel Volcanic Fields</subject><subject>Eltville Tephra</subject><subject>EPMA</subject><subject>Eruptions</subject><subject>Geochemistry</subject><subject>Glass</subject><subject>Lakes</subject><subject>Laminates</subject><subject>Pleistocene</subject><subject>Rocourt Tephra</subject><subject>sediment archive</subject><subject>Sediments</subject><subject>Thermoluminescence</subject><subject>Vents</subject><subject>Volcanic activity</subject><subject>Volcanic eruptions</subject><subject>Volcanic fields</subject><subject>Volcanoes</subject><issn>0267-8179</issn><issn>1099-1417</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><recordid>eNp1kF1LwzAUhoMoOKfgTwh4401n0mTL4t0Y84uByvS6pOnJmtE2XdKp_Sv-Wjs7L706cM5z3hcehC4pGVFC4pvNNowYZfwIDSiRMqKcimM0IPFERFMq5Ck6C2FDSHebkAH6XqoG8EsBNjROQwV4YQ0UGPyubqyrwi22VbDrvAnYeFdiXdjK1a13X3tYVRleFyoEvAancyi7GN9iZ3ADde4VLlQL_vDaJy9VaauuNMMryGwJVYNnXuf2A3D4W2jnIZyjE6OKABeHOUTvd4u3-UO0fL5_nM-WkWax4JHMKHAuNJ3qlEqVSsbNdJyaNGOQSSFYyigfT8BQqTMmYsWAMqMglRwIEMqG6KrPrb3b7iA0ycbtfNVVJjHjgo3jzltHXfeU9i4EDyapvS2VbxNKkr35pDOf7M13aNSjn7aA9l8ueXpd_fI_CriIiQ</recordid><startdate>202001</startdate><enddate>202001</enddate><creator>Förster, Michael W.</creator><creator>Zemlitskaya, Anastasia</creator><creator>Otter, Laura M.</creator><creator>Buhre, Stephan</creator><creator>Sirocko, Frank</creator><general>Wiley Subscription Services, Inc</general><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/0000-0002-0778-5811</orcidid><orcidid>https://orcid.org/0000-0003-0737-4497</orcidid></search><sort><creationdate>202001</creationdate><title>Late Pleistocene Eifel eruptions: insights from clinopyroxene and glass geochemistry of tephra layers from Eifel Laminated Sediment Archive sediment cores</title><author>Förster, Michael W. ; Zemlitskaya, Anastasia ; Otter, Laura M. ; Buhre, Stephan ; Sirocko, Frank</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c3274-9d1e447c18cb19ab934f85bfbd3ed9773b31456ef19cd372a3e13faeb94e0e013</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>Archives & records</topic><topic>ash layers</topic><topic>Cores</topic><topic>Dormancy</topic><topic>Eifel Volcanic Fields</topic><topic>Eltville Tephra</topic><topic>EPMA</topic><topic>Eruptions</topic><topic>Geochemistry</topic><topic>Glass</topic><topic>Lakes</topic><topic>Laminates</topic><topic>Pleistocene</topic><topic>Rocourt Tephra</topic><topic>sediment archive</topic><topic>Sediments</topic><topic>Thermoluminescence</topic><topic>Vents</topic><topic>Volcanic activity</topic><topic>Volcanic eruptions</topic><topic>Volcanic fields</topic><topic>Volcanoes</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Förster, Michael W.</creatorcontrib><creatorcontrib>Zemlitskaya, Anastasia</creatorcontrib><creatorcontrib>Otter, Laura M.</creatorcontrib><creatorcontrib>Buhre, Stephan</creatorcontrib><creatorcontrib>Sirocko, Frank</creatorcontrib><collection>CrossRef</collection><collection>Environment Abstracts</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>Engineering Research Database</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Environment Abstracts</collection><jtitle>Journal of quaternary science</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Förster, Michael W.</au><au>Zemlitskaya, Anastasia</au><au>Otter, Laura M.</au><au>Buhre, Stephan</au><au>Sirocko, Frank</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Late Pleistocene Eifel eruptions: insights from clinopyroxene and glass geochemistry of tephra layers from Eifel Laminated Sediment Archive sediment cores</atitle><jtitle>Journal of quaternary science</jtitle><date>2020-01</date><risdate>2020</risdate><volume>35</volume><issue>1-2</issue><spage>186</spage><epage>198</epage><pages>186-198</pages><issn>0267-8179</issn><eissn>1099-1417</eissn><abstract>ABSTRACT
The Eifel Laminated Sediment Archive (ELSA), which comprises several cores from maar lakes, includes numerous tephra layers spanning the last 140 000 years. The sediment cores are dated by 14C and thermoluminescence as well as tuned to Greenland stadial–interstadial successions. Within the last glacial cycle, the Eifel Volcanic Fields are source to several widespread tephra layers, namely the Laacher See, Eltville, Rambach and Rocourt Tephra. However, a corresponding source volcano was so far only identified for the Laacher See Tephra. In this study we use glass and clinopyroxene geochemistry to link the remaining tephra layers to possible eruption centers within the West and East Eifel Volcanic Fields: while we demonstrate that the Eltville Tephra originated from an earlier eruption of the Laacher See Volcano at 24 300 a bp from within the East Eifel Volcanic Field, the Rambach and Rocourt Tephras are sourced from the West Eifel Volcanic Field and erupted from Wartgesberg at 27 900 a bp and Pulvermaar at 75 000 a bp, respectively. Phases of volcanic activity peaked at 10 000–30 000 and 60 000–80 000 a bp and were thus erupted around the temperature minima of the last glacial cycle. The longest phase of dormancy between individual vents was around 30 000 years long, within the last interglacial.</abstract><cop>Chichester</cop><pub>Wiley Subscription Services, Inc</pub><doi>10.1002/jqs.3134</doi><tpages>13</tpages><orcidid>https://orcid.org/0000-0002-0778-5811</orcidid><orcidid>https://orcid.org/0000-0003-0737-4497</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Archives & records ash layers Cores Dormancy Eifel Volcanic Fields Eltville Tephra EPMA Eruptions Geochemistry Glass Lakes Laminates Pleistocene Rocourt Tephra sediment archive Sediments Thermoluminescence Vents Volcanic activity Volcanic eruptions Volcanic fields Volcanoes |
title | Late Pleistocene Eifel eruptions: insights from clinopyroxene and glass geochemistry of tephra layers from Eifel Laminated Sediment Archive sediment cores |
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