Show simple item record

Files in this item

Thumbnail

Item metadata

dc.contributor.authorWatson, E. J.
dc.contributor.authorSwindles, G. T.
dc.contributor.authorLawson, I. T.
dc.contributor.authorSavov, I. P.
dc.contributor.authorWastegård, S.
dc.date.accessioned2017-04-21T11:30:12Z
dc.date.available2017-04-21T11:30:12Z
dc.date.issued2017-05-12
dc.identifier249748208
dc.identifier8134301d-99b1-4181-b964-4ab71f72252a
dc.identifier85018645908
dc.identifier000401172500004
dc.identifier.citationWatson , E J , Swindles , G T , Lawson , I T , Savov , I P & Wastegård , S 2017 , ' The presence of Holocene cryptotephra in Wales and southern England ' , Journal of Quaternary Science , vol. 32 , no. 4 , pp. 493-500 . https://doi.org/10.1002/jqs.2942en
dc.identifier.issn1099-1417
dc.identifier.otherBibtex: urn:cc223bc12feb17b651def1d1dffd0272
dc.identifier.otherORCID: /0000-0002-3547-2425/work/75996907
dc.identifier.urihttps://hdl.handle.net/10023/10639
dc.descriptionThis research was undertaken while E.W. held a NERC-funded Doctoral Training grant (NE/K500847/1). This research was also supported by a Young Research Workers award to E.W. from the Quaternary Research Association.en
dc.description.abstractThere have been few detailed studies into the tephrostratigraphy of southern Britain. We report the tephrostratigraphy of two sites, one in southern England (Rough Tor, Cornwall) and one in Wales (Cors Fochno, west Wales). Our study extends the known southernmost reach of Icelandic cryptotephra in northern Europe. Given the large distance between sites in southern England and eruptive sources (e.g. Iceland 1500–1700 km distant), most of the cryptotephra layers consist of sparse numbers of shards, even by the standards of distal tephrostratigraphy (as low as 3 shards cm−1), each layer spanning only 1 or 2 cm in depth. We identify multiple cryptotephra layers in both sites, extending the known distribution of several tephra layers including the MOR-T4 tephra (∼AD 1000) most probably of Icelandic origin, and the AD 860 B tephra correlated to an eruption of Mount Churchill, Alaska. The two sites record contrasting tephrostratigraphies, illustrating the need for the inclusion of multiple sites in the construction of a regional tephrostratigraphic framework. The tephra layers we describe may provide important isochrons for the dating and correlation of palaeoenvironmental sequences in the south of Britain.
dc.format.extent8
dc.format.extent1390475
dc.language.isoeng
dc.relation.ispartofJournal of Quaternary Scienceen
dc.subjectChronologyen
dc.subjectPeatlandsen
dc.subjectTephraen
dc.subjectVolcanic ashen
dc.subjectGE Environmental Sciencesen
dc.subjectDASen
dc.subject.lccGEen
dc.titleThe presence of Holocene cryptotephra in Wales and southern Englanden
dc.typeJournal articleen
dc.contributor.institutionUniversity of St Andrews. Geography & Sustainable Developmenten
dc.contributor.institutionUniversity of St Andrews. Bell-Edwards Geographic Data Instituteen
dc.identifier.doi10.1002/jqs.2942
dc.description.statusPeer revieweden
dc.identifier.urlhttp://onlinelibrary.wiley.com/doi/10.1002/jqs.2942/full#footer-support-infoen


This item appears in the following Collection(s)

Show simple item record