OceanRep
The Eyjafiallajökull 2010 eruption and the preservation of medium-sized eruptions in marine surface sediment, offshore southern Iceland.
Bonanati, Christina, Wehrmann, Heidi, Portnyagin, Maxim and Hoernle, Kaj (2017) The Eyjafiallajökull 2010 eruption and the preservation of medium-sized eruptions in marine surface sediment, offshore southern Iceland. Quaternary Research, 87 (3). pp. 386-406. DOI 10.1017/qua.2017.15.
Text
Bonanati.pdf - Published Version Restricted to Registered users only Download (3MB) | Contact |
|
Text (Suppl. 1)
urn_cambridge.org_id_binary_20170525095607504-0788_S0033589417000151_S0033589417000151sup005.docx - Supplemental Material Restricted to Registered users only Download (37kB) | Contact |
|
Text (Suppl. 2)
urn_cambridge.org_id_binary_20170525095607504-0788_S0033589417000151_S0033589417000151sup006.docx - Supplemental Material Restricted to Registered users only Download (17kB) | Contact |
|
Text (Suppl. Figure)
urn_cambridge.org_id_binary_20170525095607504-0788_S0033589417000151_S0033589417000151sup001.pdf - Supplemental Material Restricted to Registered users only Download (58MB) | Contact |
Abstract
The recent volcanic eruptions of Eyjafjallajökull 2010 and Grímsvötn 2011 demonstrated the risks that mediumsized explosive Icelandic eruptions pose to the North Atlantic region. Using the Eyjafjallajökull 2010 eruption as a case study, we assess how traceable such eruptions are in the marine sedimentary record at medial distances from the source and investigate which factors have affected the particle transport to the marine sedimentary archive. During R/V Poseidon cruise 457, we recovered 13 box cores at 100–1600 m water depths and distances of 18–180 km southwest, south, and east of Iceland. Volcanic glass shards from the uppermost surface sediment were analyzed for their major element composition by electron microprobe and assigned to their eruptive source by geochemical fingerprinting. The predominantly basaltic particles are mostly derived from the Katla, Grímsvötn-Lakagígar, and Bárðarbunga-Veiðivötn volcanic systems. We also identified rhyolitic particles from the Askja 1875 and Öræfajökull 1362 eruptions. Only three out of almost 900 analyzed glass shards are derived from the recent Eyjafjallajökull 2010 eruption, suggesting that medium-sized eruptions are only poorly preserved in marine sediments located at medial distances southwest to east of Iceland. We conclude that the frequency of past medium-sized eruptions is likely higher than detectable in this archive.
Document Type: | Article |
---|---|
Keywords: | Iceland; Marine tephra preservation; Eyjafjallajökull 2010; Öræfajökull 1362; Askja 1875; Icelandic volcanism; Geochemical fingerprinting; Particle sedimentation; Tephra reworking; Marine sediment |
Research affiliation: | OceanRep > GEOMAR > FB4 Dynamics of the Ocean Floor > FB4-MUHS Kiel University |
Refereed: | Yes |
Open Access Journal?: | No |
Publisher: | Elsevier |
Expeditions/Models/Experiments: | |
Date Deposited: | 23 Dec 2016 08:09 |
Last Modified: | 06 Feb 2020 09:12 |
URI: | https://oceanrep.geomar.de/id/eprint/35411 |
Actions (login required)
View Item |
Copyright 2023 | GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel | All rights reserved
Questions, comments and suggestions regarding the GEOMAR repository are welcomed
at bibliotheksleitung@geomar.de !