No Cover Image

ResearchReportExternalBody 551 views

Merchant Adventurers Hall, Fossgate, York, North Yorkshire. Oxygen Isotope Dendrochronology of Oak Timbers

Neil Loader Orcid Logo, Darren Davies, Danny McCarroll, Daniel Miles, Robert Howard, Cathy Tyers, Giles Young

Research Report Series 9-2021

Swansea University Authors: Neil Loader Orcid Logo, Darren Davies, Danny McCarroll, Giles Young

Full text not available from this repository: check for access using links below.

Abstract

As part of an initiative to investigate the practical extent of the south-central England chronology for isotopic dating, two timbers that had been securely dated by ring-width dendrochronology from the Merchant Adventurers Hall, York were sampled for oxygen isotope analysis. Seventy-eight measureme...

Full description

Published in: Research Report Series 9-2021
ISSN: 2059-4453
Published: Swindon, UK. Historic England 2022
Online Access: Check full text

URI: https://cronfa.swan.ac.uk/Record/cronfa60792
Tags: Add Tag
No Tags, Be the first to tag this record!
first_indexed 2022-08-11T05:54:55Z
last_indexed 2023-01-13T19:21:11Z
id cronfa60792
recordtype SURis
fullrecord <?xml version="1.0"?><rfc1807><datestamp>2022-08-31T10:16:41.3281436</datestamp><bib-version>v2</bib-version><id>60792</id><entry>2022-08-11</entry><title>Merchant Adventurers Hall, Fossgate, York, North Yorkshire. Oxygen Isotope Dendrochronology of Oak Timbers</title><swanseaauthors><author><sid>8267a62100791965d08df6a7842676e6</sid><ORCID>0000-0002-6841-1813</ORCID><firstname>Neil</firstname><surname>Loader</surname><name>Neil Loader</name><active>true</active><ethesisStudent>false</ethesisStudent></author><author><sid>9fa284670cd135b40307d8550bfbb306</sid><firstname>Darren</firstname><surname>Davies</surname><name>Darren Davies</name><active>true</active><ethesisStudent>false</ethesisStudent></author><author><sid>6d181d926aaac8932c2bfa8d0e7f6960</sid><firstname>Danny</firstname><surname>McCarroll</surname><name>Danny McCarroll</name><active>true</active><ethesisStudent>false</ethesisStudent></author><author><sid>e0c807e6b9b663f1c297feecd2f54c3a</sid><firstname>Giles</firstname><surname>Young</surname><name>Giles Young</name><active>true</active><ethesisStudent>false</ethesisStudent></author></swanseaauthors><date>2022-08-11</date><deptcode>SGE</deptcode><abstract>As part of an initiative to investigate the practical extent of the south-central England chronology for isotopic dating, two timbers that had been securely dated by ring-width dendrochronology from the Merchant Adventurers Hall, York were sampled for oxygen isotope analysis. Seventy-eight measurements were obtained on latewood from single growth-rings of core YOR-A05 from a king post, truss 13, (rings 1&#x2013;78 of the measured ring-width series spanning AD 1265&#x2013;1346) and 68 measurements were obtained on latewood from single growth-rings of core YORA08 a tie-beam, truss 14 (rings 2&#x2013;69 of the measured ring-width series spanning AD 1272&#x2013;1355). The two isotopic series cross-match when offset by two years. This is consistent with the ring-width cross-matching. The 78-year isotopic mean cross-dates (t =7.07, 1/p&gt;1 million, IF&gt;1000) with the south-central England oxygen isotope master chronology, at a position that is compatible with that provided by ring-width dendrochronology. Independently, YOR-A08 cross-dates at a position consistent with the ring-width dendrochronology, (t =7.52, 1/p&gt;1 million, IF&gt;1000). YORA05 returns a tentative result consistent with the ring-width dating (t =5.22, 1/p=1415, IF=63). The location of the Merchant Adventurers Hall in York, well to the north-east of the south-central England master chronology is currently challenging for oxygen isotope dendrochronology. Isotopic analysis has returned dates consistent with ring-width dendrochronology, but this study suggests that whilst secure dating is possible, it may not routinely be obtained from isotopic measurements on single timbers in this region. This demonstrates that an oxygen isotope master chronology for northern England is required to enhance the potential for applying oxygen isotope dendrochronology in this region.</abstract><type>ResearchReportExternalBody</type><journal>Research Report Series 9-2021</journal><volume/><journalNumber/><paginationStart/><paginationEnd/><publisher>Historic England</publisher><placeOfPublication>Swindon, UK.</placeOfPublication><isbnPrint/><isbnElectronic/><issnPrint/><issnElectronic>2059-4453</issnElectronic><keywords/><publishedDay>9</publishedDay><publishedMonth>8</publishedMonth><publishedYear>2022</publishedYear><publishedDate>2022-08-09</publishedDate><doi/><url>https://historicengland.org.uk/research/results/reports/9-2021?searchType=research+report&amp;amp;search=*&amp;amp;searchResultsPerPage=100&amp;amp;sort=publicationDate+desc</url><notes>https://historicengland.org.uk/research/results/reports/9-2021?searchType=research+report&amp;search=*&amp;searchResultsPerPage=100&amp;sort=publicationDate+desc</notes><college>COLLEGE NANME</college><department>Geography</department><CollegeCode>COLLEGE CODE</CollegeCode><DepartmentCode>SGE</DepartmentCode><institution>Swansea University</institution><apcterm/><funders>Historic England</funders><projectreference/><lastEdited>2022-08-31T10:16:41.3281436</lastEdited><Created>2022-08-11T06:49:03.4981857</Created><path><level id="1">Faculty of Science and Engineering</level><level id="2">School of Biosciences, Geography and Physics - Geography</level></path><authors><author><firstname>Neil</firstname><surname>Loader</surname><orcid>0000-0002-6841-1813</orcid><order>1</order></author><author><firstname>Darren</firstname><surname>Davies</surname><order>2</order></author><author><firstname>Danny</firstname><surname>McCarroll</surname><order>3</order></author><author><firstname>Daniel</firstname><surname>Miles</surname><order>4</order></author><author><firstname>Robert</firstname><surname>Howard</surname><order>5</order></author><author><firstname>Cathy</firstname><surname>Tyers</surname><order>6</order></author><author><firstname>Giles</firstname><surname>Young</surname><order>7</order></author></authors><documents/><OutputDurs/></rfc1807>
spelling 2022-08-31T10:16:41.3281436 v2 60792 2022-08-11 Merchant Adventurers Hall, Fossgate, York, North Yorkshire. Oxygen Isotope Dendrochronology of Oak Timbers 8267a62100791965d08df6a7842676e6 0000-0002-6841-1813 Neil Loader Neil Loader true false 9fa284670cd135b40307d8550bfbb306 Darren Davies Darren Davies true false 6d181d926aaac8932c2bfa8d0e7f6960 Danny McCarroll Danny McCarroll true false e0c807e6b9b663f1c297feecd2f54c3a Giles Young Giles Young true false 2022-08-11 SGE As part of an initiative to investigate the practical extent of the south-central England chronology for isotopic dating, two timbers that had been securely dated by ring-width dendrochronology from the Merchant Adventurers Hall, York were sampled for oxygen isotope analysis. Seventy-eight measurements were obtained on latewood from single growth-rings of core YOR-A05 from a king post, truss 13, (rings 1–78 of the measured ring-width series spanning AD 1265–1346) and 68 measurements were obtained on latewood from single growth-rings of core YORA08 a tie-beam, truss 14 (rings 2–69 of the measured ring-width series spanning AD 1272–1355). The two isotopic series cross-match when offset by two years. This is consistent with the ring-width cross-matching. The 78-year isotopic mean cross-dates (t =7.07, 1/p>1 million, IF>1000) with the south-central England oxygen isotope master chronology, at a position that is compatible with that provided by ring-width dendrochronology. Independently, YOR-A08 cross-dates at a position consistent with the ring-width dendrochronology, (t =7.52, 1/p>1 million, IF>1000). YORA05 returns a tentative result consistent with the ring-width dating (t =5.22, 1/p=1415, IF=63). The location of the Merchant Adventurers Hall in York, well to the north-east of the south-central England master chronology is currently challenging for oxygen isotope dendrochronology. Isotopic analysis has returned dates consistent with ring-width dendrochronology, but this study suggests that whilst secure dating is possible, it may not routinely be obtained from isotopic measurements on single timbers in this region. This demonstrates that an oxygen isotope master chronology for northern England is required to enhance the potential for applying oxygen isotope dendrochronology in this region. ResearchReportExternalBody Research Report Series 9-2021 Historic England Swindon, UK. 2059-4453 9 8 2022 2022-08-09 https://historicengland.org.uk/research/results/reports/9-2021?searchType=research+report&amp;search=*&amp;searchResultsPerPage=100&amp;sort=publicationDate+desc https://historicengland.org.uk/research/results/reports/9-2021?searchType=research+report&search=*&searchResultsPerPage=100&sort=publicationDate+desc COLLEGE NANME Geography COLLEGE CODE SGE Swansea University Historic England 2022-08-31T10:16:41.3281436 2022-08-11T06:49:03.4981857 Faculty of Science and Engineering School of Biosciences, Geography and Physics - Geography Neil Loader 0000-0002-6841-1813 1 Darren Davies 2 Danny McCarroll 3 Daniel Miles 4 Robert Howard 5 Cathy Tyers 6 Giles Young 7
title Merchant Adventurers Hall, Fossgate, York, North Yorkshire. Oxygen Isotope Dendrochronology of Oak Timbers
spellingShingle Merchant Adventurers Hall, Fossgate, York, North Yorkshire. Oxygen Isotope Dendrochronology of Oak Timbers
Neil Loader
Darren Davies
Danny McCarroll
Giles Young
title_short Merchant Adventurers Hall, Fossgate, York, North Yorkshire. Oxygen Isotope Dendrochronology of Oak Timbers
title_full Merchant Adventurers Hall, Fossgate, York, North Yorkshire. Oxygen Isotope Dendrochronology of Oak Timbers
title_fullStr Merchant Adventurers Hall, Fossgate, York, North Yorkshire. Oxygen Isotope Dendrochronology of Oak Timbers
title_full_unstemmed Merchant Adventurers Hall, Fossgate, York, North Yorkshire. Oxygen Isotope Dendrochronology of Oak Timbers
title_sort Merchant Adventurers Hall, Fossgate, York, North Yorkshire. Oxygen Isotope Dendrochronology of Oak Timbers
author_id_str_mv 8267a62100791965d08df6a7842676e6
9fa284670cd135b40307d8550bfbb306
6d181d926aaac8932c2bfa8d0e7f6960
e0c807e6b9b663f1c297feecd2f54c3a
author_id_fullname_str_mv 8267a62100791965d08df6a7842676e6_***_Neil Loader
9fa284670cd135b40307d8550bfbb306_***_Darren Davies
6d181d926aaac8932c2bfa8d0e7f6960_***_Danny McCarroll
e0c807e6b9b663f1c297feecd2f54c3a_***_Giles Young
author Neil Loader
Darren Davies
Danny McCarroll
Giles Young
author2 Neil Loader
Darren Davies
Danny McCarroll
Daniel Miles
Robert Howard
Cathy Tyers
Giles Young
format ResearchReportExternalBody
container_title Research Report Series 9-2021
publishDate 2022
institution Swansea University
issn 2059-4453
publisher Historic England
college_str Faculty of Science and Engineering
hierarchytype
hierarchy_top_id facultyofscienceandengineering
hierarchy_top_title Faculty of Science and Engineering
hierarchy_parent_id facultyofscienceandengineering
hierarchy_parent_title Faculty of Science and Engineering
department_str School of Biosciences, Geography and Physics - Geography{{{_:::_}}}Faculty of Science and Engineering{{{_:::_}}}School of Biosciences, Geography and Physics - Geography
url https://historicengland.org.uk/research/results/reports/9-2021?searchType=research+report&amp;search=*&amp;searchResultsPerPage=100&amp;sort=publicationDate+desc
document_store_str 0
active_str 0
description As part of an initiative to investigate the practical extent of the south-central England chronology for isotopic dating, two timbers that had been securely dated by ring-width dendrochronology from the Merchant Adventurers Hall, York were sampled for oxygen isotope analysis. Seventy-eight measurements were obtained on latewood from single growth-rings of core YOR-A05 from a king post, truss 13, (rings 1–78 of the measured ring-width series spanning AD 1265–1346) and 68 measurements were obtained on latewood from single growth-rings of core YORA08 a tie-beam, truss 14 (rings 2–69 of the measured ring-width series spanning AD 1272–1355). The two isotopic series cross-match when offset by two years. This is consistent with the ring-width cross-matching. The 78-year isotopic mean cross-dates (t =7.07, 1/p>1 million, IF>1000) with the south-central England oxygen isotope master chronology, at a position that is compatible with that provided by ring-width dendrochronology. Independently, YOR-A08 cross-dates at a position consistent with the ring-width dendrochronology, (t =7.52, 1/p>1 million, IF>1000). YORA05 returns a tentative result consistent with the ring-width dating (t =5.22, 1/p=1415, IF=63). The location of the Merchant Adventurers Hall in York, well to the north-east of the south-central England master chronology is currently challenging for oxygen isotope dendrochronology. Isotopic analysis has returned dates consistent with ring-width dendrochronology, but this study suggests that whilst secure dating is possible, it may not routinely be obtained from isotopic measurements on single timbers in this region. This demonstrates that an oxygen isotope master chronology for northern England is required to enhance the potential for applying oxygen isotope dendrochronology in this region.
published_date 2022-08-09T04:19:11Z
_version_ 1763754274436677632
score 11.013552