Intcal04 Terrestrial Radiocarbon Age Calibration, 0–26 Cal Kyr BP
A new calibration curve for the conversion of radiocarbon ages to calibrated (cal) ages has been constructed and internationally ratified to replace IntCal98, which extended from 0–24 cal kyr BP (Before Present, 0 cal BP = AD 1950). The new calibration data set for terrestrial samples extends from 0...
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| Veröffentlicht in: | Radiocarbon 2004, Vol.46 (3), p.1029-1058 |
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| creator | REIMER, Paula J BAILLIE, Mike G. L DAMON, Paul E EDWARDS, R. Lawrence FAIRBANKS, Richard G FRIEDRICH, Michael GUILDERSON, Thomas P HOGG, Alan G HUGHEN, Konrad A KROMER, Bernd MCCORMAC, Gerry MANNING, Sturt BARD, Edouard RAMSEY, Christopher Bronk REIMER, Ron W REMMELE, Sabine SOUTHON, John R STUIVER, Minze TALAMO, Sahra TAYLOR, F. W VAN DER PLICHT, Johannes WEYHENMEYER, Constanze E BAYLISS, Alex BECK, J. Warren BERTRAND, Chanda J. H BLACKWELL, Paul G BUCK, Caitlin E BURR, George S CUTLER, Kirsten B |
| description | A new calibration curve for the conversion of radiocarbon ages to calibrated (cal) ages has been constructed and internationally ratified to replace IntCal98, which extended from 0–24 cal kyr BP (Before Present, 0 cal BP = AD 1950). The new calibration data set for terrestrial samples extends from 0–26 cal kyr BP, but with much higher resolution beyond 11.4 cal kyr BP than IntCal98. Dendrochronologically-dated tree-ring samples cover the period from 0–12.4 cal kyr BP. Beyond the end of the tree rings, data from marine records (corals and foraminifera) are converted to the atmospheric equivalent with a site-specific marine reservoir correction to provide terrestrial calibration from 12.4–26.0 cal kyr B P. A substantial enhancement relative to IntCal98 is the introduction of a coherent statistical approach based on a random walk model, which takes into account the uncertainty in both the calendar age and the 14C age to calculate the underlying calibration curve (Buck and Blackwell, this issue). The tree-ring data sets, sources of uncertainty, and regional offsets are discussed here. The marine data sets and calibration curve for marine samples from the surface mixed layer (Marine04) are discussed in brief, but details are presented in Hughen et al. (this issue a). We do not make a recommendation for calibration beyond 26 cal kyr BP at this time; however, potential calibration data sets are compared in another paper (van der Plicht et al., this issue). |
| doi_str_mv | 10.1017/S0033822200032999 |
| format | Article |
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L ; DAMON, Paul E ; EDWARDS, R. Lawrence ; FAIRBANKS, Richard G ; FRIEDRICH, Michael ; GUILDERSON, Thomas P ; HOGG, Alan G ; HUGHEN, Konrad A ; KROMER, Bernd ; MCCORMAC, Gerry ; MANNING, Sturt ; BARD, Edouard ; RAMSEY, Christopher Bronk ; REIMER, Ron W ; REMMELE, Sabine ; SOUTHON, John R ; STUIVER, Minze ; TALAMO, Sahra ; TAYLOR, F. W ; VAN DER PLICHT, Johannes ; WEYHENMEYER, Constanze E ; BAYLISS, Alex ; BECK, J. Warren ; BERTRAND, Chanda J. H ; BLACKWELL, Paul G ; BUCK, Caitlin E ; BURR, George S ; CUTLER, Kirsten B</creator><creatorcontrib>REIMER, Paula J ; BAILLIE, Mike G. L ; DAMON, Paul E ; EDWARDS, R. Lawrence ; FAIRBANKS, Richard G ; FRIEDRICH, Michael ; GUILDERSON, Thomas P ; HOGG, Alan G ; HUGHEN, Konrad A ; KROMER, Bernd ; MCCORMAC, Gerry ; MANNING, Sturt ; BARD, Edouard ; RAMSEY, Christopher Bronk ; REIMER, Ron W ; REMMELE, Sabine ; SOUTHON, John R ; STUIVER, Minze ; TALAMO, Sahra ; TAYLOR, F. W ; VAN DER PLICHT, Johannes ; WEYHENMEYER, Constanze E ; BAYLISS, Alex ; BECK, J. Warren ; BERTRAND, Chanda J. H ; BLACKWELL, Paul G ; BUCK, Caitlin E ; BURR, George S ; CUTLER, Kirsten B</creatorcontrib><description>A new calibration curve for the conversion of radiocarbon ages to calibrated (cal) ages has been constructed and internationally ratified to replace IntCal98, which extended from 0–24 cal kyr BP (Before Present, 0 cal BP = AD 1950). The new calibration data set for terrestrial samples extends from 0–26 cal kyr BP, but with much higher resolution beyond 11.4 cal kyr BP than IntCal98. Dendrochronologically-dated tree-ring samples cover the period from 0–12.4 cal kyr BP. Beyond the end of the tree rings, data from marine records (corals and foraminifera) are converted to the atmospheric equivalent with a site-specific marine reservoir correction to provide terrestrial calibration from 12.4–26.0 cal kyr B P. A substantial enhancement relative to IntCal98 is the introduction of a coherent statistical approach based on a random walk model, which takes into account the uncertainty in both the calendar age and the 14C age to calculate the underlying calibration curve (Buck and Blackwell, this issue). The tree-ring data sets, sources of uncertainty, and regional offsets are discussed here. The marine data sets and calibration curve for marine samples from the surface mixed layer (Marine04) are discussed in brief, but details are presented in Hughen et al. (this issue a). We do not make a recommendation for calibration beyond 26 cal kyr BP at this time; however, potential calibration data sets are compared in another paper (van der Plicht et al., this issue).</description><identifier>ISSN: 0033-8222</identifier><identifier>EISSN: 1945-5755</identifier><identifier>DOI: 10.1017/S0033822200032999</identifier><language>eng</language><publisher>New York, US: Cambridge University Press</publisher><subject>Bioclimatology ; Dating ; Ecology, environment ; Environmental studies ; Excavation and methods ; Flora ; Laboratory methods ; Life Sciences ; Metal industry ; Methodology and general studies ; Prehistory and protohistory ; Radiocarbon Calibration from 0–26 cal kyr BP ; Typology, technology and attribute analysis</subject><ispartof>Radiocarbon, 2004, Vol.46 (3), p.1029-1058</ispartof><rights>Copyright © The Arizona Board of Regents on behalf of the University of Arizona</rights><rights>2008 INIST-CNRS</rights><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a533t-9d20560c2b716a79796d103c8c282d4a6342997191c740560c2f612510ebb0523</citedby><cites>FETCH-LOGICAL-a533t-9d20560c2b716a79796d103c8c282d4a6342997191c740560c2f612510ebb0523</cites><orcidid>0000-0002-7237-8622</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.cambridge.org/core/product/identifier/S0033822200032999/type/journal_article$$EHTML$$P50$$Gcambridge$$H</linktohtml><link.rule.ids>164,314,776,780,881,4010,27900,27901,27902,55603</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=16599074$$DView record in Pascal Francis$$Hfree_for_read</backlink><backlink>$$Uhttps://hal.science/hal-03772463$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>REIMER, Paula J</creatorcontrib><creatorcontrib>BAILLIE, Mike G. L</creatorcontrib><creatorcontrib>DAMON, Paul E</creatorcontrib><creatorcontrib>EDWARDS, R. Lawrence</creatorcontrib><creatorcontrib>FAIRBANKS, Richard G</creatorcontrib><creatorcontrib>FRIEDRICH, Michael</creatorcontrib><creatorcontrib>GUILDERSON, Thomas P</creatorcontrib><creatorcontrib>HOGG, Alan G</creatorcontrib><creatorcontrib>HUGHEN, Konrad A</creatorcontrib><creatorcontrib>KROMER, Bernd</creatorcontrib><creatorcontrib>MCCORMAC, Gerry</creatorcontrib><creatorcontrib>MANNING, Sturt</creatorcontrib><creatorcontrib>BARD, Edouard</creatorcontrib><creatorcontrib>RAMSEY, Christopher Bronk</creatorcontrib><creatorcontrib>REIMER, Ron W</creatorcontrib><creatorcontrib>REMMELE, Sabine</creatorcontrib><creatorcontrib>SOUTHON, John R</creatorcontrib><creatorcontrib>STUIVER, Minze</creatorcontrib><creatorcontrib>TALAMO, Sahra</creatorcontrib><creatorcontrib>TAYLOR, F. W</creatorcontrib><creatorcontrib>VAN DER PLICHT, Johannes</creatorcontrib><creatorcontrib>WEYHENMEYER, Constanze E</creatorcontrib><creatorcontrib>BAYLISS, Alex</creatorcontrib><creatorcontrib>BECK, J. Warren</creatorcontrib><creatorcontrib>BERTRAND, Chanda J. H</creatorcontrib><creatorcontrib>BLACKWELL, Paul G</creatorcontrib><creatorcontrib>BUCK, Caitlin E</creatorcontrib><creatorcontrib>BURR, George S</creatorcontrib><creatorcontrib>CUTLER, Kirsten B</creatorcontrib><title>Intcal04 Terrestrial Radiocarbon Age Calibration, 0–26 Cal Kyr BP</title><title>Radiocarbon</title><addtitle>Radiocarbon</addtitle><description>A new calibration curve for the conversion of radiocarbon ages to calibrated (cal) ages has been constructed and internationally ratified to replace IntCal98, which extended from 0–24 cal kyr BP (Before Present, 0 cal BP = AD 1950). The new calibration data set for terrestrial samples extends from 0–26 cal kyr BP, but with much higher resolution beyond 11.4 cal kyr BP than IntCal98. Dendrochronologically-dated tree-ring samples cover the period from 0–12.4 cal kyr BP. Beyond the end of the tree rings, data from marine records (corals and foraminifera) are converted to the atmospheric equivalent with a site-specific marine reservoir correction to provide terrestrial calibration from 12.4–26.0 cal kyr B P. A substantial enhancement relative to IntCal98 is the introduction of a coherent statistical approach based on a random walk model, which takes into account the uncertainty in both the calendar age and the 14C age to calculate the underlying calibration curve (Buck and Blackwell, this issue). The tree-ring data sets, sources of uncertainty, and regional offsets are discussed here. The marine data sets and calibration curve for marine samples from the surface mixed layer (Marine04) are discussed in brief, but details are presented in Hughen et al. (this issue a). We do not make a recommendation for calibration beyond 26 cal kyr BP at this time; however, potential calibration data sets are compared in another paper (van der Plicht et al., this issue).</description><subject>Bioclimatology</subject><subject>Dating</subject><subject>Ecology, environment</subject><subject>Environmental studies</subject><subject>Excavation and methods</subject><subject>Flora</subject><subject>Laboratory methods</subject><subject>Life Sciences</subject><subject>Metal industry</subject><subject>Methodology and general studies</subject><subject>Prehistory and protohistory</subject><subject>Radiocarbon Calibration from 0–26 cal kyr BP</subject><subject>Typology, technology and attribute analysis</subject><issn>0033-8222</issn><issn>1945-5755</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2004</creationdate><recordtype>article</recordtype><recordid>eNp9UM1Kw0AQXkTBWn0Ab7l4EIzO7mZ3s8ca1BYLitZzmGySuiVNym4UevMdfEOfxIQUPQieZvj-mPkIOaVwSYGqq2cAzmPGGHQL01rvkRHVkQiFEmKfjHo67PlDcuT9CoBRGasRSWZ1a7CCKFgUzhW-dRar4Alz2xh0WVMHk2URJFjZzGFrm_oigK-PTyZ7LLjfuuD68ZgclFj54mQ3x-Tl9maRTMP5w90smcxDFJy3oc4ZCAmGZYpKVFppmVPgJjYsZnmEkkfd4YpqalQ0KEtJmaBQZBkIxsfkfMh9xSrdOLtGt00btOl0Mk97DLhSLJL8nXZaOmiNa7x3RfljoJD2jaV_Gus8Z4Nng77rpHRYG-t_jVJoDSrqdHyXjevM2XxZpKvmzdXd7_-kfwPdP3XQ</recordid><startdate>2004</startdate><enddate>2004</enddate><creator>REIMER, Paula J</creator><creator>BAILLIE, Mike G. 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Lawrence</au><au>FAIRBANKS, Richard G</au><au>FRIEDRICH, Michael</au><au>GUILDERSON, Thomas P</au><au>HOGG, Alan G</au><au>HUGHEN, Konrad A</au><au>KROMER, Bernd</au><au>MCCORMAC, Gerry</au><au>MANNING, Sturt</au><au>BARD, Edouard</au><au>RAMSEY, Christopher Bronk</au><au>REIMER, Ron W</au><au>REMMELE, Sabine</au><au>SOUTHON, John R</au><au>STUIVER, Minze</au><au>TALAMO, Sahra</au><au>TAYLOR, F. W</au><au>VAN DER PLICHT, Johannes</au><au>WEYHENMEYER, Constanze E</au><au>BAYLISS, Alex</au><au>BECK, J. Warren</au><au>BERTRAND, Chanda J. H</au><au>BLACKWELL, Paul G</au><au>BUCK, Caitlin E</au><au>BURR, George S</au><au>CUTLER, Kirsten B</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Intcal04 Terrestrial Radiocarbon Age Calibration, 0–26 Cal Kyr BP</atitle><jtitle>Radiocarbon</jtitle><addtitle>Radiocarbon</addtitle><date>2004</date><risdate>2004</risdate><volume>46</volume><issue>3</issue><spage>1029</spage><epage>1058</epage><pages>1029-1058</pages><issn>0033-8222</issn><eissn>1945-5755</eissn><abstract>A new calibration curve for the conversion of radiocarbon ages to calibrated (cal) ages has been constructed and internationally ratified to replace IntCal98, which extended from 0–24 cal kyr BP (Before Present, 0 cal BP = AD 1950). The new calibration data set for terrestrial samples extends from 0–26 cal kyr BP, but with much higher resolution beyond 11.4 cal kyr BP than IntCal98. Dendrochronologically-dated tree-ring samples cover the period from 0–12.4 cal kyr BP. Beyond the end of the tree rings, data from marine records (corals and foraminifera) are converted to the atmospheric equivalent with a site-specific marine reservoir correction to provide terrestrial calibration from 12.4–26.0 cal kyr B P. A substantial enhancement relative to IntCal98 is the introduction of a coherent statistical approach based on a random walk model, which takes into account the uncertainty in both the calendar age and the 14C age to calculate the underlying calibration curve (Buck and Blackwell, this issue). The tree-ring data sets, sources of uncertainty, and regional offsets are discussed here. The marine data sets and calibration curve for marine samples from the surface mixed layer (Marine04) are discussed in brief, but details are presented in Hughen et al. (this issue a). We do not make a recommendation for calibration beyond 26 cal kyr BP at this time; however, potential calibration data sets are compared in another paper (van der Plicht et al., this issue).</abstract><cop>New York, US</cop><pub>Cambridge University Press</pub><doi>10.1017/S0033822200032999</doi><tpages>30</tpages><orcidid>https://orcid.org/0000-0002-7237-8622</orcidid><oa>free_for_read</oa></addata></record> |
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| ispartof | Radiocarbon, 2004, Vol.46 (3), p.1029-1058 |
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| source | Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals; Cambridge Journals; Free Full-Text Journals in Chemistry |
| subjects | Bioclimatology Dating Ecology, environment Environmental studies Excavation and methods Flora Laboratory methods Life Sciences Metal industry Methodology and general studies Prehistory and protohistory Radiocarbon Calibration from 0–26 cal kyr BP Typology, technology and attribute analysis |
| title | Intcal04 Terrestrial Radiocarbon Age Calibration, 0–26 Cal Kyr BP |
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