Early Holocene M~6 explosive eruption from Plosky volcanic massif (Kamchatka) and its tephra as a link between terrestrial and marine paleoenvironmental records
We report tephrochronological and geochemical data on early Holocene activity from Plosky volcanic massif in the Kliuchevskoi volcanic group, Kamchatka Peninsula. Explosive activity of this volcano lasted for ~1.5 kyr, produced a series of widely dispersed tephra layers, and was followed by profuse...
Published in: | International Journal of Earth Sciences |
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Language: | English |
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2013
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Online Access: | http://repo.kscnet.ru/1047/ http://repo.kscnet.ru/1047/1/Ponomareva%202013.pdf https://doi.org/10.1007/s00531-013-0898-0 |
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Institute of Volcanology and Seismology, Petropavlovsk-Kamchatsky: IVS FEB RAS Repository |
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English |
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38.37.25 Вулканология Крестовский Безымянный Острый Толбачик Плоский Толбачик Средний Ушковский Ключевской |
spellingShingle |
38.37.25 Вулканология Крестовский Безымянный Острый Толбачик Плоский Толбачик Средний Ушковский Ключевской Ponomareva Vera Portnyagin Maxim Derkachev Alexander Pendea I. Florin Bourgeois Joanne Reimer Paula J. Garbe-Schönberg Dieter Krasheninnikov Stepan Nürnberg Dirk Early Holocene M~6 explosive eruption from Plosky volcanic massif (Kamchatka) and its tephra as a link between terrestrial and marine paleoenvironmental records |
topic_facet |
38.37.25 Вулканология Крестовский Безымянный Острый Толбачик Плоский Толбачик Средний Ушковский Ключевской |
description |
We report tephrochronological and geochemical data on early Holocene activity from Plosky volcanic massif in the Kliuchevskoi volcanic group, Kamchatka Peninsula. Explosive activity of this volcano lasted for ~1.5 kyr, produced a series of widely dispersed tephra layers, and was followed by profuse low-viscosity lava flows. This eruptive episode started a major reorganization of the volcanic structures in the western part of the Kliuchevskoi volcanic group. An explosive eruption from Plosky (M~6), previously unstudied, produced tephra (coded PL2) of a volume of 10–12 km3 (11–13 Gt), being one of the largest Holocene explosive eruptions in Kamchatka. Characteristic diagnostic features of the PL2 tephra are predominantly vitric sponge-shaped fragments with rare phenocrysts and microlites of plagioclase, olivine and pyroxenes, medium- to high-K basaltic andesitic bulk composition, high-K, high-Al and high-P trachyandesitic glass composition with SiO2 = 57.5–59.5 wt%, K2O = 2.3–2.7 wt%, Al2O3 = 15.8–16.5 wt%, and P2O5 = 0.5–0.7 wt%. Other diagnostic features include a typical subduction-related pattern of incompatible elements, high concentrations of all REE (>10× mantle values), moderate enrichment in LREE (La/Yb ~ 5.3), and non-fractionated mantle-like pattern of LILE. Geochemical fingerprinting of the PL2 tephra with the help of EMP and LA-ICP-MS analyses allowed us to map its occurrence in terrestrial sections across Kamchatka and to identify this layer in Bering Sea sediment cores at a distance of >600 km from the source. New high-precision 14C dates suggest that the PL2 eruption occurred ~10,200 cal BP, which makes it a valuable isochrone for early Holocene climate fluctuations and permits direct links between terrestrial and marine paleoenvironmental records. The terrestrial and marine 14C dates related to the PL2 tephra have allowed us to estimate an early Holocene reservoir age for the western Bering Sea at 1,410 ± 64 14C years. Another important tephra from the early Holocene eruptive episode of ... |
format |
Text |
author |
Ponomareva Vera Portnyagin Maxim Derkachev Alexander Pendea I. Florin Bourgeois Joanne Reimer Paula J. Garbe-Schönberg Dieter Krasheninnikov Stepan Nürnberg Dirk |
author_facet |
Ponomareva Vera Portnyagin Maxim Derkachev Alexander Pendea I. Florin Bourgeois Joanne Reimer Paula J. Garbe-Schönberg Dieter Krasheninnikov Stepan Nürnberg Dirk |
author_sort |
Ponomareva Vera |
title |
Early Holocene M~6 explosive eruption from Plosky volcanic massif (Kamchatka) and its tephra as a link between terrestrial and marine paleoenvironmental records |
title_short |
Early Holocene M~6 explosive eruption from Plosky volcanic massif (Kamchatka) and its tephra as a link between terrestrial and marine paleoenvironmental records |
title_full |
Early Holocene M~6 explosive eruption from Plosky volcanic massif (Kamchatka) and its tephra as a link between terrestrial and marine paleoenvironmental records |
title_fullStr |
Early Holocene M~6 explosive eruption from Plosky volcanic massif (Kamchatka) and its tephra as a link between terrestrial and marine paleoenvironmental records |
title_full_unstemmed |
Early Holocene M~6 explosive eruption from Plosky volcanic massif (Kamchatka) and its tephra as a link between terrestrial and marine paleoenvironmental records |
title_sort |
early holocene m~6 explosive eruption from plosky volcanic massif (kamchatka) and its tephra as a link between terrestrial and marine paleoenvironmental records |
publishDate |
2013 |
url |
http://repo.kscnet.ru/1047/ http://repo.kscnet.ru/1047/1/Ponomareva%202013.pdf https://doi.org/10.1007/s00531-013-0898-0 |
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ENVELOPE(160.000,160.000,56.000,56.000) |
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Bering Sea Kamchatka Peninsula |
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Bering Sea Kamchatka Peninsula |
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Bering Sea Kamchatka Kamchatka Peninsula |
genre_facet |
Bering Sea Kamchatka Kamchatka Peninsula |
op_relation |
http://repo.kscnet.ru/1047/1/Ponomareva%202013.pdf Ponomareva Vera <http://repo.kscnet.ru/view/creators/Ponomareva=3AVera=3A=3A.html>, Portnyagin Maxim <http://repo.kscnet.ru/view/creators/Portnyagin=3AMaxim=3A=3A.html>, Derkachev Alexander <http://repo.kscnet.ru/view/creators/Derkachev=3AAlexander=3A=3A.html>, Pendea I. Florin <http://repo.kscnet.ru/view/creators/Pendea=3AI=2E_Florin=3A=3A.html>, Bourgeois Joanne <http://repo.kscnet.ru/view/creators/Bourgeois=3AJoanne=3A=3A.html>, Reimer Paula J. <http://repo.kscnet.ru/view/creators/Reimer=3APaula_J=2E=3A=3A.html>, Garbe-Schönberg Dieter <http://repo.kscnet.ru/view/creators/Garbe-Sch=F6nberg=3ADieter=3A=3A.html>, Krasheninnikov Stepan <http://repo.kscnet.ru/view/creators/Krasheninnikov=3AStepan=3A=3A.html>, Nürnberg Dirk <http://repo.kscnet.ru/view/creators/N=FCrnberg=3ADirk=3A=3A.html> (2013) Early Holocene M~6 explosive eruption from Plosky volcanic massif (Kamchatka) and its tephra as a link between terrestrial and marine paleoenvironmental records // International Journal of Earth Sciences. Vol. 102, No. 6. pp. 1673-1699. doi:10.1007/s00531-013-0898-0 <http://doi.org/10.1007/s00531-013-0898-0>. |
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International Journal of Earth Sciences |
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1673 |
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ftinstvs:oai:repo.kscnet.ru:1047 2023-05-15T15:43:44+02:00 Early Holocene M~6 explosive eruption from Plosky volcanic massif (Kamchatka) and its tephra as a link between terrestrial and marine paleoenvironmental records Ponomareva Vera Portnyagin Maxim Derkachev Alexander Pendea I. Florin Bourgeois Joanne Reimer Paula J. Garbe-Schönberg Dieter Krasheninnikov Stepan Nürnberg Dirk 2013 text http://repo.kscnet.ru/1047/ http://repo.kscnet.ru/1047/1/Ponomareva%202013.pdf https://doi.org/10.1007/s00531-013-0898-0 en eng http://repo.kscnet.ru/1047/1/Ponomareva%202013.pdf Ponomareva Vera <http://repo.kscnet.ru/view/creators/Ponomareva=3AVera=3A=3A.html>, Portnyagin Maxim <http://repo.kscnet.ru/view/creators/Portnyagin=3AMaxim=3A=3A.html>, Derkachev Alexander <http://repo.kscnet.ru/view/creators/Derkachev=3AAlexander=3A=3A.html>, Pendea I. Florin <http://repo.kscnet.ru/view/creators/Pendea=3AI=2E_Florin=3A=3A.html>, Bourgeois Joanne <http://repo.kscnet.ru/view/creators/Bourgeois=3AJoanne=3A=3A.html>, Reimer Paula J. <http://repo.kscnet.ru/view/creators/Reimer=3APaula_J=2E=3A=3A.html>, Garbe-Schönberg Dieter <http://repo.kscnet.ru/view/creators/Garbe-Sch=F6nberg=3ADieter=3A=3A.html>, Krasheninnikov Stepan <http://repo.kscnet.ru/view/creators/Krasheninnikov=3AStepan=3A=3A.html>, Nürnberg Dirk <http://repo.kscnet.ru/view/creators/N=FCrnberg=3ADirk=3A=3A.html> (2013) Early Holocene M~6 explosive eruption from Plosky volcanic massif (Kamchatka) and its tephra as a link between terrestrial and marine paleoenvironmental records // International Journal of Earth Sciences. Vol. 102, No. 6. pp. 1673-1699. doi:10.1007/s00531-013-0898-0 <http://doi.org/10.1007/s00531-013-0898-0>. 38.37.25 Вулканология Крестовский Безымянный Острый Толбачик Плоский Толбачик Средний Ушковский Ключевской Статья PeerReviewed 2013 ftinstvs https://doi.org/10.1007/s00531-013-0898-0 2022-08-09T17:04:22Z We report tephrochronological and geochemical data on early Holocene activity from Plosky volcanic massif in the Kliuchevskoi volcanic group, Kamchatka Peninsula. Explosive activity of this volcano lasted for ~1.5 kyr, produced a series of widely dispersed tephra layers, and was followed by profuse low-viscosity lava flows. This eruptive episode started a major reorganization of the volcanic structures in the western part of the Kliuchevskoi volcanic group. An explosive eruption from Plosky (M~6), previously unstudied, produced tephra (coded PL2) of a volume of 10–12 km3 (11–13 Gt), being one of the largest Holocene explosive eruptions in Kamchatka. Characteristic diagnostic features of the PL2 tephra are predominantly vitric sponge-shaped fragments with rare phenocrysts and microlites of plagioclase, olivine and pyroxenes, medium- to high-K basaltic andesitic bulk composition, high-K, high-Al and high-P trachyandesitic glass composition with SiO2 = 57.5–59.5 wt%, K2O = 2.3–2.7 wt%, Al2O3 = 15.8–16.5 wt%, and P2O5 = 0.5–0.7 wt%. Other diagnostic features include a typical subduction-related pattern of incompatible elements, high concentrations of all REE (>10× mantle values), moderate enrichment in LREE (La/Yb ~ 5.3), and non-fractionated mantle-like pattern of LILE. Geochemical fingerprinting of the PL2 tephra with the help of EMP and LA-ICP-MS analyses allowed us to map its occurrence in terrestrial sections across Kamchatka and to identify this layer in Bering Sea sediment cores at a distance of >600 km from the source. New high-precision 14C dates suggest that the PL2 eruption occurred ~10,200 cal BP, which makes it a valuable isochrone for early Holocene climate fluctuations and permits direct links between terrestrial and marine paleoenvironmental records. The terrestrial and marine 14C dates related to the PL2 tephra have allowed us to estimate an early Holocene reservoir age for the western Bering Sea at 1,410 ± 64 14C years. Another important tephra from the early Holocene eruptive episode of ... Text Bering Sea Kamchatka Kamchatka Peninsula Institute of Volcanology and Seismology, Petropavlovsk-Kamchatsky: IVS FEB RAS Repository Bering Sea Kamchatka Peninsula ENVELOPE(160.000,160.000,56.000,56.000) International Journal of Earth Sciences 102 6 1673 1699 |