New unspiked K-Ar ages of quaternary sub-glacial and sub-aerial volcanic activity in Iceland
Application of volcanic proxies to paleoenvironmental studies in Iceland has generally lagged behind the improvements of undisputable geochronologies. This is particularly frustrating because a link between volcanism and deglaciation in Iceland is an appealing hypothesis and questions about the exte...
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Language: | English |
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HAL CCSD
2010
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Online Access: | https://hal.univ-brest.fr/hal-00482046 https://hal.univ-brest.fr/hal-00482046/document https://hal.univ-brest.fr/hal-00482046/file/Guillou_resume1.pdf |
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ftccsdartic:oai:HAL:hal-00482046v1 |
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Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) |
op_collection_id |
ftccsdartic |
language |
English |
topic |
[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanology [SDE.MCG]Environmental Sciences/Global Changes |
spellingShingle |
[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanology [SDE.MCG]Environmental Sciences/Global Changes Guillou, Hervé Van Vliet-Lanoë, Brigitte Gudmundsson, Agust Nomade, Sébastien New unspiked K-Ar ages of quaternary sub-glacial and sub-aerial volcanic activity in Iceland |
topic_facet |
[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanology [SDE.MCG]Environmental Sciences/Global Changes |
description |
Application of volcanic proxies to paleoenvironmental studies in Iceland has generally lagged behind the improvements of undisputable geochronologies. This is particularly frustrating because a link between volcanism and deglaciation in Iceland is an appealing hypothesis and questions about the extent of the ice cap during Icelandic glaciations remain pending (Einarsson et al., 1988; Geirsdttir et al., 1997; Ingolfsson et al., 1997; Hoppe, 1982). The postglacial eruptive history of Iceland after the last deglaciation is now well documented (Licciardi et al., 2007; Sinton et al., 2005, Saemundsson, 1991). One of its main characteristics is an increase in the volcanic eruption rate, which coincides with the end of the last ice age (11 ka BP; Slater et al., 1998; Maclennan et al., 2002; Sigvaldason et al., 1992; Hardarson et al., 1991; Jull et al., 1996). However, the pattern of volcanism for more evolved rocks, such as rhyolites, comprising 10-12% of outcrop on Iceland, is less well established. In fact, the opposite trend may be apparent, or at least sub-glacial rhyolite eruptions are frequent during interglacial periods (Flude et al., 2008). This relationship between deglaciation and volcanism has been convincingly demonstrated in Iceland only for the last deglaciation (Maclennan et al., 2004; Sinton et al., 2005; Licciardi et al., 2007, McGarvie et al., 2006, McGarvie et al., 2007). Therefore, we consider that it is important to explore this relationship through older periods. The purpose of this study is then to evaluate the potential of the unspiked K-Ar dating method in dating Quaternary Icelandic volcanics to contribute to this debate. The unspiked K-Ar technique applied here is perfectly adapted to these purposes because it is an accurate and precise dating tool which has proven to be efficient and suitable to date young Quaternary lavas. To test the relevance of our approach, we collected and dated sub-aerial lavas contemporaneous with warm periods; hyaloclastites and lavas formed in sub-glacial ... |
author2 |
Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ) Paléocéanographie (PALEOCEAN) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ) Domaines Océaniques (LDO) Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Observatoire des Sciences de l'Univers-Institut d'écologie et environnement-Centre National de la Recherche Scientifique (CNRS) Université européenne de Bretagne - European University of Brittany (UEB) JFS Geological Services JFS |
format |
Conference Object |
author |
Guillou, Hervé Van Vliet-Lanoë, Brigitte Gudmundsson, Agust Nomade, Sébastien |
author_facet |
Guillou, Hervé Van Vliet-Lanoë, Brigitte Gudmundsson, Agust Nomade, Sébastien |
author_sort |
Guillou, Hervé |
title |
New unspiked K-Ar ages of quaternary sub-glacial and sub-aerial volcanic activity in Iceland |
title_short |
New unspiked K-Ar ages of quaternary sub-glacial and sub-aerial volcanic activity in Iceland |
title_full |
New unspiked K-Ar ages of quaternary sub-glacial and sub-aerial volcanic activity in Iceland |
title_fullStr |
New unspiked K-Ar ages of quaternary sub-glacial and sub-aerial volcanic activity in Iceland |
title_full_unstemmed |
New unspiked K-Ar ages of quaternary sub-glacial and sub-aerial volcanic activity in Iceland |
title_sort |
new unspiked k-ar ages of quaternary sub-glacial and sub-aerial volcanic activity in iceland |
publisher |
HAL CCSD |
publishDate |
2010 |
url |
https://hal.univ-brest.fr/hal-00482046 https://hal.univ-brest.fr/hal-00482046/document https://hal.univ-brest.fr/hal-00482046/file/Guillou_resume1.pdf |
op_coverage |
Plouzané, France |
genre |
Ice cap Iceland |
genre_facet |
Ice cap Iceland |
op_source |
Iceland in the central Northern Atlantic : hotspot, sea currents and climate change https://hal.univ-brest.fr/hal-00482046 Iceland in the central Northern Atlantic : hotspot, sea currents and climate change, May 2010, Plouzané, France |
op_relation |
hal-00482046 https://hal.univ-brest.fr/hal-00482046 https://hal.univ-brest.fr/hal-00482046/document https://hal.univ-brest.fr/hal-00482046/file/Guillou_resume1.pdf |
op_rights |
info:eu-repo/semantics/OpenAccess |
_version_ |
1766028659180699648 |
spelling |
ftccsdartic:oai:HAL:hal-00482046v1 2023-05-15T16:38:23+02:00 New unspiked K-Ar ages of quaternary sub-glacial and sub-aerial volcanic activity in Iceland Guillou, Hervé Van Vliet-Lanoë, Brigitte Gudmundsson, Agust Nomade, Sébastien Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ) Paléocéanographie (PALEOCEAN) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ) Domaines Océaniques (LDO) Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Observatoire des Sciences de l'Univers-Institut d'écologie et environnement-Centre National de la Recherche Scientifique (CNRS) Université européenne de Bretagne - European University of Brittany (UEB) JFS Geological Services JFS Plouzané, France 2010-05-11 https://hal.univ-brest.fr/hal-00482046 https://hal.univ-brest.fr/hal-00482046/document https://hal.univ-brest.fr/hal-00482046/file/Guillou_resume1.pdf en eng HAL CCSD hal-00482046 https://hal.univ-brest.fr/hal-00482046 https://hal.univ-brest.fr/hal-00482046/document https://hal.univ-brest.fr/hal-00482046/file/Guillou_resume1.pdf info:eu-repo/semantics/OpenAccess Iceland in the central Northern Atlantic : hotspot, sea currents and climate change https://hal.univ-brest.fr/hal-00482046 Iceland in the central Northern Atlantic : hotspot, sea currents and climate change, May 2010, Plouzané, France [SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanology [SDE.MCG]Environmental Sciences/Global Changes info:eu-repo/semantics/conferenceObject Conference papers 2010 ftccsdartic 2021-12-19T03:51:46Z Application of volcanic proxies to paleoenvironmental studies in Iceland has generally lagged behind the improvements of undisputable geochronologies. This is particularly frustrating because a link between volcanism and deglaciation in Iceland is an appealing hypothesis and questions about the extent of the ice cap during Icelandic glaciations remain pending (Einarsson et al., 1988; Geirsdttir et al., 1997; Ingolfsson et al., 1997; Hoppe, 1982). The postglacial eruptive history of Iceland after the last deglaciation is now well documented (Licciardi et al., 2007; Sinton et al., 2005, Saemundsson, 1991). One of its main characteristics is an increase in the volcanic eruption rate, which coincides with the end of the last ice age (11 ka BP; Slater et al., 1998; Maclennan et al., 2002; Sigvaldason et al., 1992; Hardarson et al., 1991; Jull et al., 1996). However, the pattern of volcanism for more evolved rocks, such as rhyolites, comprising 10-12% of outcrop on Iceland, is less well established. In fact, the opposite trend may be apparent, or at least sub-glacial rhyolite eruptions are frequent during interglacial periods (Flude et al., 2008). This relationship between deglaciation and volcanism has been convincingly demonstrated in Iceland only for the last deglaciation (Maclennan et al., 2004; Sinton et al., 2005; Licciardi et al., 2007, McGarvie et al., 2006, McGarvie et al., 2007). Therefore, we consider that it is important to explore this relationship through older periods. The purpose of this study is then to evaluate the potential of the unspiked K-Ar dating method in dating Quaternary Icelandic volcanics to contribute to this debate. The unspiked K-Ar technique applied here is perfectly adapted to these purposes because it is an accurate and precise dating tool which has proven to be efficient and suitable to date young Quaternary lavas. To test the relevance of our approach, we collected and dated sub-aerial lavas contemporaneous with warm periods; hyaloclastites and lavas formed in sub-glacial ... Conference Object Ice cap Iceland Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) |