A revised age for the Kawakawa/Oruanui tephra, a key marker for the Last Glacial Maximum in New Zealand
The Kawakawa/Oruanui tephra (KOT) is a key chronostratigraphic marker in terrestrial and marine deposits of the New Zealand (NZ) sector of the southwest Pacific. Erupted early during the Last Glacial Maximum (LGM), the wide distribution of the KOT enables inter-regional alignment of proxy records an...
Gespeichert in:
| Veröffentlicht in: | Quaternary science reviews 2013-08, Vol.74, p.195-201 |
|---|---|
| Hauptverfasser: | , , , , , , , , , , , , , , |
| Format: | Artikel |
| Sprache: | eng |
| Schlagworte: | |
| Online-Zugang: | Volltext |
| Tags: |
Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
|
| container_end_page | 201 |
|---|---|
| container_issue | |
| container_start_page | 195 |
| container_title | Quaternary science reviews |
| container_volume | 74 |
| creator | Vandergoes, Marcus J. Hogg, Alan G. Lowe, David J. Newnham, Rewi M. Denton, George H. Southon, John Barrell, David J.A. Wilson, Colin J.N. McGlone, Matt S. Allan, Aidan S.R. Almond, Peter C. Petchey, Fiona Dabell, Kathleen Dieffenbacher-Krall, Ann C. Blaauw, Maarten |
| description | The Kawakawa/Oruanui tephra (KOT) is a key chronostratigraphic marker in terrestrial and marine deposits of the New Zealand (NZ) sector of the southwest Pacific. Erupted early during the Last Glacial Maximum (LGM), the wide distribution of the KOT enables inter-regional alignment of proxy records and facilitates comparison between NZ climatic variations and those from well-dated records elsewhere. We present 22 new radiocarbon ages for the KOT from sites and materials considered optimal for dating, and apply Bayesian statistical methods via OxCal4.1.7 that incorporate stratigraphic information to develop a new age probability model for KOT. The revised calibrated age, ±2 standard deviations, for the eruption of the KOT is 25,360 ± 160 cal yr BP. The age revision provides a basis for refining marine reservoir ages for the LGM in the southwest Pacific.
► Presents a new age of 25.4 cal ka for Kawakawa/Oruanui tephra. ► Applies Bayesian statistical modelling to quantify and reduce uncertainties. ► Refines age of critical datum for LGM climate comparisons in the Southwest Pacific. |
| doi_str_mv | 10.1016/j.quascirev.2012.11.006 |
| format | Article |
| fullrecord | <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_1805503741</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><els_id>S0277379112004775</els_id><sourcerecordid>1805503741</sourcerecordid><originalsourceid>FETCH-LOGICAL-a486t-cc3d54c1d4c632e79b6fc589b3f1f492053f19337365d0b41bf7eb1fa6e0d1f03</originalsourceid><addsrcrecordid>eNqFkEtPwzAQhC0EEuXxG_CRAwneOImTY4V4iQIXkBAXa-OswW3aFDvh8e8xKuLKYbV7-Ga0M4wdgUhBQHk6T99GDMZ5ek8zAVkKkApRbrEJVEomeaGettlEZEolUtWwy_ZCmAshiqzKJuxlyqPQBWo5vhC3vefDK_Eb_MBFnNN7P-JqdHyg9avHE458QV98iX5B_o-eYRj4ZYfGYcdv8dMtxyV3K35HH_yZsMNVe8B2LHaBDn_3Pnu8OH84u0pm95fXZ9NZgnlVDokxsi1yA21uSpmRqpvSmqKqG2nB5nUminjUUipZFq1ocmisogYsliRasELus-ON79r3byOFQS9dMNTFH6gfg4ZKFIWQKoeIqg1qfB-CJ6vX3sVkXxqE_qlWz_VftfqnWg2gY7VROd0oKSZ5d-R1hGhlqI2oGXTbu389vgGFZ4aV</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1805503741</pqid></control><display><type>article</type><title>A revised age for the Kawakawa/Oruanui tephra, a key marker for the Last Glacial Maximum in New Zealand</title><source>Elsevier ScienceDirect Journals</source><creator>Vandergoes, Marcus J. ; Hogg, Alan G. ; Lowe, David J. ; Newnham, Rewi M. ; Denton, George H. ; Southon, John ; Barrell, David J.A. ; Wilson, Colin J.N. ; McGlone, Matt S. ; Allan, Aidan S.R. ; Almond, Peter C. ; Petchey, Fiona ; Dabell, Kathleen ; Dieffenbacher-Krall, Ann C. ; Blaauw, Maarten</creator><creatorcontrib>Vandergoes, Marcus J. ; Hogg, Alan G. ; Lowe, David J. ; Newnham, Rewi M. ; Denton, George H. ; Southon, John ; Barrell, David J.A. ; Wilson, Colin J.N. ; McGlone, Matt S. ; Allan, Aidan S.R. ; Almond, Peter C. ; Petchey, Fiona ; Dabell, Kathleen ; Dieffenbacher-Krall, Ann C. ; Blaauw, Maarten</creatorcontrib><description>The Kawakawa/Oruanui tephra (KOT) is a key chronostratigraphic marker in terrestrial and marine deposits of the New Zealand (NZ) sector of the southwest Pacific. Erupted early during the Last Glacial Maximum (LGM), the wide distribution of the KOT enables inter-regional alignment of proxy records and facilitates comparison between NZ climatic variations and those from well-dated records elsewhere. We present 22 new radiocarbon ages for the KOT from sites and materials considered optimal for dating, and apply Bayesian statistical methods via OxCal4.1.7 that incorporate stratigraphic information to develop a new age probability model for KOT. The revised calibrated age, ±2 standard deviations, for the eruption of the KOT is 25,360 ± 160 cal yr BP. The age revision provides a basis for refining marine reservoir ages for the LGM in the southwest Pacific.
► Presents a new age of 25.4 cal ka for Kawakawa/Oruanui tephra. ► Applies Bayesian statistical modelling to quantify and reduce uncertainties. ► Refines age of critical datum for LGM climate comparisons in the Southwest Pacific.</description><identifier>ISSN: 0277-3791</identifier><identifier>EISSN: 1873-457X</identifier><identifier>DOI: 10.1016/j.quascirev.2012.11.006</identifier><language>eng</language><publisher>Elsevier Ltd</publisher><subject>14C dating ; Chronostratigraphy ; Isochron ; Kawakawa/Oruanui tephra ; Last Glacial Maximum (LGM) ; Marine ; Marine reservoir ages ; New Zealand ; NZ climate event stratigraphy ; Oruanui eruption ; Paleoclimate ; Southwest Pacific ; Tephrochronology</subject><ispartof>Quaternary science reviews, 2013-08, Vol.74, p.195-201</ispartof><rights>2012</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a486t-cc3d54c1d4c632e79b6fc589b3f1f492053f19337365d0b41bf7eb1fa6e0d1f03</citedby><cites>FETCH-LOGICAL-a486t-cc3d54c1d4c632e79b6fc589b3f1f492053f19337365d0b41bf7eb1fa6e0d1f03</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/S0277379112004775$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,776,780,3537,27901,27902,65306</link.rule.ids></links><search><creatorcontrib>Vandergoes, Marcus J.</creatorcontrib><creatorcontrib>Hogg, Alan G.</creatorcontrib><creatorcontrib>Lowe, David J.</creatorcontrib><creatorcontrib>Newnham, Rewi M.</creatorcontrib><creatorcontrib>Denton, George H.</creatorcontrib><creatorcontrib>Southon, John</creatorcontrib><creatorcontrib>Barrell, David J.A.</creatorcontrib><creatorcontrib>Wilson, Colin J.N.</creatorcontrib><creatorcontrib>McGlone, Matt S.</creatorcontrib><creatorcontrib>Allan, Aidan S.R.</creatorcontrib><creatorcontrib>Almond, Peter C.</creatorcontrib><creatorcontrib>Petchey, Fiona</creatorcontrib><creatorcontrib>Dabell, Kathleen</creatorcontrib><creatorcontrib>Dieffenbacher-Krall, Ann C.</creatorcontrib><creatorcontrib>Blaauw, Maarten</creatorcontrib><title>A revised age for the Kawakawa/Oruanui tephra, a key marker for the Last Glacial Maximum in New Zealand</title><title>Quaternary science reviews</title><description>The Kawakawa/Oruanui tephra (KOT) is a key chronostratigraphic marker in terrestrial and marine deposits of the New Zealand (NZ) sector of the southwest Pacific. Erupted early during the Last Glacial Maximum (LGM), the wide distribution of the KOT enables inter-regional alignment of proxy records and facilitates comparison between NZ climatic variations and those from well-dated records elsewhere. We present 22 new radiocarbon ages for the KOT from sites and materials considered optimal for dating, and apply Bayesian statistical methods via OxCal4.1.7 that incorporate stratigraphic information to develop a new age probability model for KOT. The revised calibrated age, ±2 standard deviations, for the eruption of the KOT is 25,360 ± 160 cal yr BP. The age revision provides a basis for refining marine reservoir ages for the LGM in the southwest Pacific.
► Presents a new age of 25.4 cal ka for Kawakawa/Oruanui tephra. ► Applies Bayesian statistical modelling to quantify and reduce uncertainties. ► Refines age of critical datum for LGM climate comparisons in the Southwest Pacific.</description><subject>14C dating</subject><subject>Chronostratigraphy</subject><subject>Isochron</subject><subject>Kawakawa/Oruanui tephra</subject><subject>Last Glacial Maximum (LGM)</subject><subject>Marine</subject><subject>Marine reservoir ages</subject><subject>New Zealand</subject><subject>NZ climate event stratigraphy</subject><subject>Oruanui eruption</subject><subject>Paleoclimate</subject><subject>Southwest Pacific</subject><subject>Tephrochronology</subject><issn>0277-3791</issn><issn>1873-457X</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2013</creationdate><recordtype>article</recordtype><recordid>eNqFkEtPwzAQhC0EEuXxG_CRAwneOImTY4V4iQIXkBAXa-OswW3aFDvh8e8xKuLKYbV7-Ga0M4wdgUhBQHk6T99GDMZ5ek8zAVkKkApRbrEJVEomeaGettlEZEolUtWwy_ZCmAshiqzKJuxlyqPQBWo5vhC3vefDK_Eb_MBFnNN7P-JqdHyg9avHE458QV98iX5B_o-eYRj4ZYfGYcdv8dMtxyV3K35HH_yZsMNVe8B2LHaBDn_3Pnu8OH84u0pm95fXZ9NZgnlVDokxsi1yA21uSpmRqpvSmqKqG2nB5nUminjUUipZFq1ocmisogYsliRasELus-ON79r3byOFQS9dMNTFH6gfg4ZKFIWQKoeIqg1qfB-CJ6vX3sVkXxqE_qlWz_VftfqnWg2gY7VROd0oKSZ5d-R1hGhlqI2oGXTbu389vgGFZ4aV</recordid><startdate>20130815</startdate><enddate>20130815</enddate><creator>Vandergoes, Marcus J.</creator><creator>Hogg, Alan G.</creator><creator>Lowe, David J.</creator><creator>Newnham, Rewi M.</creator><creator>Denton, George H.</creator><creator>Southon, John</creator><creator>Barrell, David J.A.</creator><creator>Wilson, Colin J.N.</creator><creator>McGlone, Matt S.</creator><creator>Allan, Aidan S.R.</creator><creator>Almond, Peter C.</creator><creator>Petchey, Fiona</creator><creator>Dabell, Kathleen</creator><creator>Dieffenbacher-Krall, Ann C.</creator><creator>Blaauw, Maarten</creator><general>Elsevier Ltd</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7UA</scope><scope>C1K</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>20130815</creationdate><title>A revised age for the Kawakawa/Oruanui tephra, a key marker for the Last Glacial Maximum in New Zealand</title><author>Vandergoes, Marcus J. ; Hogg, Alan G. ; Lowe, David J. ; Newnham, Rewi M. ; Denton, George H. ; Southon, John ; Barrell, David J.A. ; Wilson, Colin J.N. ; McGlone, Matt S. ; Allan, Aidan S.R. ; Almond, Peter C. ; Petchey, Fiona ; Dabell, Kathleen ; Dieffenbacher-Krall, Ann C. ; Blaauw, Maarten</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a486t-cc3d54c1d4c632e79b6fc589b3f1f492053f19337365d0b41bf7eb1fa6e0d1f03</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2013</creationdate><topic>14C dating</topic><topic>Chronostratigraphy</topic><topic>Isochron</topic><topic>Kawakawa/Oruanui tephra</topic><topic>Last Glacial Maximum (LGM)</topic><topic>Marine</topic><topic>Marine reservoir ages</topic><topic>New Zealand</topic><topic>NZ climate event stratigraphy</topic><topic>Oruanui eruption</topic><topic>Paleoclimate</topic><topic>Southwest Pacific</topic><topic>Tephrochronology</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Vandergoes, Marcus J.</creatorcontrib><creatorcontrib>Hogg, Alan G.</creatorcontrib><creatorcontrib>Lowe, David J.</creatorcontrib><creatorcontrib>Newnham, Rewi M.</creatorcontrib><creatorcontrib>Denton, George H.</creatorcontrib><creatorcontrib>Southon, John</creatorcontrib><creatorcontrib>Barrell, David J.A.</creatorcontrib><creatorcontrib>Wilson, Colin J.N.</creatorcontrib><creatorcontrib>McGlone, Matt S.</creatorcontrib><creatorcontrib>Allan, Aidan S.R.</creatorcontrib><creatorcontrib>Almond, Peter C.</creatorcontrib><creatorcontrib>Petchey, Fiona</creatorcontrib><creatorcontrib>Dabell, Kathleen</creatorcontrib><creatorcontrib>Dieffenbacher-Krall, Ann C.</creatorcontrib><creatorcontrib>Blaauw, Maarten</creatorcontrib><collection>CrossRef</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Quaternary science reviews</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Vandergoes, Marcus J.</au><au>Hogg, Alan G.</au><au>Lowe, David J.</au><au>Newnham, Rewi M.</au><au>Denton, George H.</au><au>Southon, John</au><au>Barrell, David J.A.</au><au>Wilson, Colin J.N.</au><au>McGlone, Matt S.</au><au>Allan, Aidan S.R.</au><au>Almond, Peter C.</au><au>Petchey, Fiona</au><au>Dabell, Kathleen</au><au>Dieffenbacher-Krall, Ann C.</au><au>Blaauw, Maarten</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>A revised age for the Kawakawa/Oruanui tephra, a key marker for the Last Glacial Maximum in New Zealand</atitle><jtitle>Quaternary science reviews</jtitle><date>2013-08-15</date><risdate>2013</risdate><volume>74</volume><spage>195</spage><epage>201</epage><pages>195-201</pages><issn>0277-3791</issn><eissn>1873-457X</eissn><abstract>The Kawakawa/Oruanui tephra (KOT) is a key chronostratigraphic marker in terrestrial and marine deposits of the New Zealand (NZ) sector of the southwest Pacific. Erupted early during the Last Glacial Maximum (LGM), the wide distribution of the KOT enables inter-regional alignment of proxy records and facilitates comparison between NZ climatic variations and those from well-dated records elsewhere. We present 22 new radiocarbon ages for the KOT from sites and materials considered optimal for dating, and apply Bayesian statistical methods via OxCal4.1.7 that incorporate stratigraphic information to develop a new age probability model for KOT. The revised calibrated age, ±2 standard deviations, for the eruption of the KOT is 25,360 ± 160 cal yr BP. The age revision provides a basis for refining marine reservoir ages for the LGM in the southwest Pacific.
► Presents a new age of 25.4 cal ka for Kawakawa/Oruanui tephra. ► Applies Bayesian statistical modelling to quantify and reduce uncertainties. ► Refines age of critical datum for LGM climate comparisons in the Southwest Pacific.</abstract><pub>Elsevier Ltd</pub><doi>10.1016/j.quascirev.2012.11.006</doi><tpages>7</tpages><oa>free_for_read</oa></addata></record> |
| fulltext | fulltext |
| identifier | ISSN: 0277-3791 |
| ispartof | Quaternary science reviews, 2013-08, Vol.74, p.195-201 |
| issn | 0277-3791 1873-457X |
| language | eng |
| recordid | cdi_proquest_miscellaneous_1805503741 |
| source | Elsevier ScienceDirect Journals |
| subjects | 14C dating Chronostratigraphy Isochron Kawakawa/Oruanui tephra Last Glacial Maximum (LGM) Marine Marine reservoir ages New Zealand NZ climate event stratigraphy Oruanui eruption Paleoclimate Southwest Pacific Tephrochronology |
| title | A revised age for the Kawakawa/Oruanui tephra, a key marker for the Last Glacial Maximum in New Zealand |
| url | https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-08T10%3A14%3A36IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=A%20revised%20age%20for%20the%20Kawakawa/Oruanui%20tephra,%20a%20key%20marker%20for%20the%20Last%20Glacial%20Maximum%20in%20New%20Zealand&rft.jtitle=Quaternary%20science%20reviews&rft.au=Vandergoes,%20Marcus%20J.&rft.date=2013-08-15&rft.volume=74&rft.spage=195&rft.epage=201&rft.pages=195-201&rft.issn=0277-3791&rft.eissn=1873-457X&rft_id=info:doi/10.1016/j.quascirev.2012.11.006&rft_dat=%3Cproquest_cross%3E1805503741%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=1805503741&rft_id=info:pmid/&rft_els_id=S0277379112004775&rfr_iscdi=true |