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The Saksunarvatn Ash and the G10ka series tephra. Review and current state of knowledge

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dc.contributor Háskóli Íslands
dc.contributor University of Iceland
dc.contributor.author Óladóttir, Bergrún Arna
dc.contributor.author Thordarson, Thorvaldur
dc.contributor.author Geirsdóttir, Áslaug
dc.contributor.author Jóhannsdóttir, Guðrún Eva
dc.contributor.author Mangerud, Jan
dc.date.accessioned 2020-08-24T14:41:19Z
dc.date.available 2020-08-24T14:41:19Z
dc.date.issued 2020-03
dc.identifier.citation Óladóttir, B. A., Thordarson, T., Geirsdóttir, Á., Jóhannsdóttir, G. E., & Mangerud, J. (2020). The saksunarvatn ash and the G10ka series tephra. review and current state of knowledge. Quaternary Geochronology, 56 doi:10.1016/j.quageo.2019.101041
dc.identifier.issn 1871-1014
dc.identifier.uri https://hdl.handle.net/20.500.11815/2010
dc.description Post-print (lokagerð höfundar)
dc.description.abstract The Saksunarvatn Ash, first found in the Faroe Islands, is a tephra produced by the Grímsvötn volcanic system in Iceland. Since its discovery in the Faroe Islands, dark tephra with a similar stratigraphic position has been described at numerous locations around the North-Atlantic region; including 46 sites in Iceland (soil and lake sediments), 37 marine sediment cores from the North-Atlantic, 23 terrestrial locations in northern Europe (Faroe Islands, Scotland, Orkney, Shetland, Norway and Germany), and 4 sites from the Greenland Ice Sheet. The chemical composition of the tephra found around the North-Atlantic is, in most cases, within the published chemical range of the Saksunarvatn Ash originally found in the Faroe Islands, i.e. tholeiitic basalt with MgO and K2O wt% that places it in the more evolved part of the Grímsvötn chemical field. Published ages of the inferred Saksunarvatn Ash range significantly, dating from 10,625 ± 53 to 9586 ± 315 cal yr BP, although the widespread usage of the ice-core age of ~10,300 yr BP has given the tephra high chronological importance. Based on the reported sites, the tephra covers an area of about 2 million km2. However, in the last decade new studies have shown that the Grímsvötn volcanic system produced several widely distributed tephra layers of very similar chemical composition in the time period from 10,400–9900 yr BP. Hence, the Saksunarvatn Ash appears to be one of multiple early Holocene Grímsvötn tephra layers distributed around the North-Atlantic area. Where such tephras are identified, they therefore reflect a time interval rather than a precise marker as previously anticipated. Although still chemically indistinguishable, these Grímsvötn tephra layers represent a marker horizon around the North-Atlantic region spanning approximately 500 years, and are referred to as the G10ka series tephra. The exact number of eruptions that form the tephra marker horizon remains unknown, but up to seven have been proposed.
dc.description.sponsorship This project was financed by project grant no. 141363 from the Icelandic Research Fund (RANNÍS), and grants NÝR01-2015, NÝR01-2016 from Orkurannsóknarsjóður Landsvirkjunar. Ásta Rut Hjartardóttir is sincerely thanked for help with figures and Jessica Lynn Till for language improvements. Co-workers at the Earth Science Institute, University of Iceland are genuinely thanked for fruitful discussion during writing of the manuscript. Simon Blockley and an anonymous reviewer are acknowledged for their detailed and constructive reviews. Efficient editorial handling by the editors was appreciated.
dc.format.extent 101041
dc.language.iso en
dc.publisher Elsevier BV
dc.relation.ispartofseries Quaternary Geochronology;56
dc.rights info:eu-repo/semantics/embargoedAccess
dc.subject Saksunarvatn ash
dc.subject G10ka series tephra
dc.subject Grímsvötn volcano
dc.subject Tephra marker
dc.subject Basalt
dc.subject Aska
dc.subject Gjóska
dc.subject Eldfjöll
dc.subject Grímsvötn
dc.title The Saksunarvatn Ash and the G10ka series tephra. Review and current state of knowledge
dc.type info:eu-repo/semantics/article
dcterms.license © 2019 Elsevier B.V. CC BY-NC-ND License
dc.description.version Peer reviewed
dc.identifier.journal Quaternary Geochronology
dc.identifier.doi 10.1016/j.quageo.2019.101041
dc.contributor.department Norræna eldfjallasetrið (HÍ)
dc.contributor.department Nordic Volcanological Centre (UI)
dc.contributor.department Jarðvísindadeild (HÍ)
dc.contributor.department Faculty of Earth Sciences (UI)
dc.contributor.school Verkfræði- og náttúruvísindasvið (HÍ)
dc.contributor.school School of Engineering and Natural Sciences (UI)


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