Late glacial and holocene 10 Be production rates for western Norway
We present a new regional calibration of the 10 Be production rate from two well‐dated surfaces in southern Norway: a rock avalanche with 14 C‐dated wood and a precisely dated Younger Dryas moraine. Calculated 10 Be production rates are 4.26 ± 0.13 and 4.65 ± 0.14 at g −1 a −1 for the Lal/Stone and...
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| Veröffentlicht in: | Journal of quaternary science 2012-01, Vol.27 (1), p.89-96 |
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| container_title | Journal of quaternary science |
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| creator | Goehring, Brent M. Lohne, Øystein Strand Mangerud, Jan Svendsen, John Inge Gyllencreutz, Richard Schaefer, Joerg Finkel, Robert |
| description | We present a new regional calibration of the
10
Be production rate from two well‐dated surfaces in southern Norway: a rock avalanche with
14
C‐dated wood and a precisely dated Younger Dryas moraine. Calculated
10
Be production rates are 4.26 ± 0.13 and 4.65 ± 0.14 at g
−1
a
−1
for the Lal/Stone and Lifton scaling models, respectively. Our regional production rate for southern Norway is 5% lower than the canonical global
10
Be production rate with lower uncertainties. Our
10
Be production rate agrees with regional
10
Be production rates from north‐eastern North America and New Zealand. The
10
Be production rate estimate presented here can be used to improve the precision and accuracy of exposure‐dated ice‐marginal features, as well as other surfaces, in northern Europe. Copyright © 2011 John Wiley & Sons, Ltd. |
| doi_str_mv | 10.1002/jqs.1517 |
| format | Article |
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10
Be production rate from two well‐dated surfaces in southern Norway: a rock avalanche with
14
C‐dated wood and a precisely dated Younger Dryas moraine. Calculated
10
Be production rates are 4.26 ± 0.13 and 4.65 ± 0.14 at g
−1
a
−1
for the Lal/Stone and Lifton scaling models, respectively. Our regional production rate for southern Norway is 5% lower than the canonical global
10
Be production rate with lower uncertainties. Our
10
Be production rate agrees with regional
10
Be production rates from north‐eastern North America and New Zealand. The
10
Be production rate estimate presented here can be used to improve the precision and accuracy of exposure‐dated ice‐marginal features, as well as other surfaces, in northern Europe. Copyright © 2011 John Wiley & Sons, Ltd.</description><identifier>ISSN: 0267-8179</identifier><identifier>EISSN: 1099-1417</identifier><identifier>DOI: 10.1002/jqs.1517</identifier><language>eng</language><ispartof>Journal of quaternary science, 2012-01, Vol.27 (1), p.89-96</ispartof><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c727-d348fcf013184ac6a48c4705998a24b98303182e3e95300ad9a2efe64dc68b103</citedby><cites>FETCH-LOGICAL-c727-d348fcf013184ac6a48c4705998a24b98303182e3e95300ad9a2efe64dc68b103</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Goehring, Brent M.</creatorcontrib><creatorcontrib>Lohne, Øystein Strand</creatorcontrib><creatorcontrib>Mangerud, Jan</creatorcontrib><creatorcontrib>Svendsen, John Inge</creatorcontrib><creatorcontrib>Gyllencreutz, Richard</creatorcontrib><creatorcontrib>Schaefer, Joerg</creatorcontrib><creatorcontrib>Finkel, Robert</creatorcontrib><title>Late glacial and holocene 10 Be production rates for western Norway</title><title>Journal of quaternary science</title><description>We present a new regional calibration of the
10
Be production rate from two well‐dated surfaces in southern Norway: a rock avalanche with
14
C‐dated wood and a precisely dated Younger Dryas moraine. Calculated
10
Be production rates are 4.26 ± 0.13 and 4.65 ± 0.14 at g
−1
a
−1
for the Lal/Stone and Lifton scaling models, respectively. Our regional production rate for southern Norway is 5% lower than the canonical global
10
Be production rate with lower uncertainties. Our
10
Be production rate agrees with regional
10
Be production rates from north‐eastern North America and New Zealand. The
10
Be production rate estimate presented here can be used to improve the precision and accuracy of exposure‐dated ice‐marginal features, as well as other surfaces, in northern Europe. Copyright © 2011 John Wiley & Sons, Ltd.</description><issn>0267-8179</issn><issn>1099-1417</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2012</creationdate><recordtype>article</recordtype><recordid>eNotj0FLwzAYhoMoWKfgT8jRS-f3JWmTHHXoFIpedi_f0kQ7ajOTyti_t0NP7-F5eeBh7BZhiQDifvedl1ihPmMFgrUlKtTnrABR69KgtpfsKucdwMxqKNiqocnzj4FcTwOnseOfcYjOj54j8EfP9yl2P27q48jTfM08xMQPPk8-jfwtpgMdr9lFoCH7m_9dsM3z02b1Ujbv69fVQ1M6LXTZSWWCC4ASjSJXkzJOaaisNSTU1hoJMxFeeltJAOosCR98rTpXmy2CXLC7P61LMefkQ7tP_RelY4vQntrbub09tctfFzZLLA</recordid><startdate>201201</startdate><enddate>201201</enddate><creator>Goehring, Brent M.</creator><creator>Lohne, Øystein Strand</creator><creator>Mangerud, Jan</creator><creator>Svendsen, John Inge</creator><creator>Gyllencreutz, Richard</creator><creator>Schaefer, Joerg</creator><creator>Finkel, Robert</creator><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>201201</creationdate><title>Late glacial and holocene 10 Be production rates for western Norway</title><author>Goehring, Brent M. ; Lohne, Øystein Strand ; Mangerud, Jan ; Svendsen, John Inge ; Gyllencreutz, Richard ; Schaefer, Joerg ; Finkel, Robert</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c727-d348fcf013184ac6a48c4705998a24b98303182e3e95300ad9a2efe64dc68b103</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2012</creationdate><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Goehring, Brent M.</creatorcontrib><creatorcontrib>Lohne, Øystein Strand</creatorcontrib><creatorcontrib>Mangerud, Jan</creatorcontrib><creatorcontrib>Svendsen, John Inge</creatorcontrib><creatorcontrib>Gyllencreutz, Richard</creatorcontrib><creatorcontrib>Schaefer, Joerg</creatorcontrib><creatorcontrib>Finkel, Robert</creatorcontrib><collection>CrossRef</collection><jtitle>Journal of quaternary science</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Goehring, Brent M.</au><au>Lohne, Øystein Strand</au><au>Mangerud, Jan</au><au>Svendsen, John Inge</au><au>Gyllencreutz, Richard</au><au>Schaefer, Joerg</au><au>Finkel, Robert</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Late glacial and holocene 10 Be production rates for western Norway</atitle><jtitle>Journal of quaternary science</jtitle><date>2012-01</date><risdate>2012</risdate><volume>27</volume><issue>1</issue><spage>89</spage><epage>96</epage><pages>89-96</pages><issn>0267-8179</issn><eissn>1099-1417</eissn><abstract>We present a new regional calibration of the
10
Be production rate from two well‐dated surfaces in southern Norway: a rock avalanche with
14
C‐dated wood and a precisely dated Younger Dryas moraine. Calculated
10
Be production rates are 4.26 ± 0.13 and 4.65 ± 0.14 at g
−1
a
−1
for the Lal/Stone and Lifton scaling models, respectively. Our regional production rate for southern Norway is 5% lower than the canonical global
10
Be production rate with lower uncertainties. Our
10
Be production rate agrees with regional
10
Be production rates from north‐eastern North America and New Zealand. The
10
Be production rate estimate presented here can be used to improve the precision and accuracy of exposure‐dated ice‐marginal features, as well as other surfaces, in northern Europe. Copyright © 2011 John Wiley & Sons, Ltd.</abstract><doi>10.1002/jqs.1517</doi><tpages>8</tpages></addata></record> |
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| ispartof | Journal of quaternary science, 2012-01, Vol.27 (1), p.89-96 |
| issn | 0267-8179 1099-1417 |
| language | eng |
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| source | Access via Wiley Online Library |
| title | Late glacial and holocene 10 Be production rates for western Norway |
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