Cosmogenic Exposure Dating (36Cl) of Landforms on Jan Mayen, North Atlantic, and the Effects of Bedrock Formation Age Assumptions on 36Cl Ages

Jan Mayen is a small volcanic island situated 550 km north of Iceland. Glacial sediments and landforms are relatively common on the island but, so far, only a few of them have been dated. In this study, we present and discuss 89 36Cl dates of primarily glacial and volcanic events on Jan Mayen. Calcu...

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Main Authors: Anjar, Johanna, Akҫar, Naki, Larsen, Eiliv A., Lyså, Astrid, Marrero, Shasta, Mozafari, Nasim, Vockenhuber, Christof
Format: Text
Language:unknown
Published: MDPI 2021
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Online Access:https://dx.doi.org/10.48350/166685
https://boris.unibe.ch/166685/
id ftdatacite:10.48350/166685
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spelling ftdatacite:10.48350/166685 2023-05-15T16:52:28+02:00 Cosmogenic Exposure Dating (36Cl) of Landforms on Jan Mayen, North Atlantic, and the Effects of Bedrock Formation Age Assumptions on 36Cl Ages Anjar, Johanna Akҫar, Naki Larsen, Eiliv A. Lyså, Astrid Marrero, Shasta Mozafari, Nasim Vockenhuber, Christof 2021 https://dx.doi.org/10.48350/166685 https://boris.unibe.ch/166685/ unknown MDPI https://dx.doi.org/10.3390/geosciences11090390 open access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 http://purl.org/coar/access_right/c_abf2 CC-BY 550 Earth sciences & geology article-journal ScholarlyArticle journal article Text 2021 ftdatacite https://doi.org/10.48350/166685 https://doi.org/10.3390/geosciences11090390 2022-04-01T13:05:45Z Jan Mayen is a small volcanic island situated 550 km north of Iceland. Glacial sediments and landforms are relatively common on the island but, so far, only a few of them have been dated. In this study, we present and discuss 89 36Cl dates of primarily glacial and volcanic events on Jan Mayen. Calculations of sample exposure ages were complicated by young exposure ages, young rock formation age, and high native Cl contents, leading to updates in CRONUScalc to enable accurate exposure age calculations. The samples provide good evidence against an equilibrium assumption when subtracting background production (e.g., 36Cl produced by neutron capture from fission of U or Th) for samples on young bedrock, with younger exposure ages most significantly affected. Exposure ages were calculated with a range of assumptions of bedrock formation ages appropriate for Jan Mayen, including the assumption that the rock formation age equaled the exposure age (i.e., the youngest age it could possibly have), and we found that although the effect on most of the ages was small, the calculated ages of 25 of the samples increased by more than 1 standard deviation from the age calculated assuming equilibrium background production, with a maximum deviation of 6.1 ka. Due to the very young bedrock on Jan Mayen, we consider the nonequilibrium ages to be the most reliable ages from the island and conclude that large-scale deglaciation on the south and central, lower-lying, parts of the island, started around 20 ka and lasted until ~7 ka. On northern Jan Mayen, the slopes of the 2277 m high stratovolcano Beerenberg are currently partly glaciated; however, outside of the Little Ice Age moraines, all but two samples give ages between 14 and 5.7 ka. Text Iceland Jan Mayen North Atlantic DataCite Metadata Store (German National Library of Science and Technology) Jan Mayen Beerenberg ENVELOPE(-8.167,-8.167,71.083,71.083)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic 550 Earth sciences & geology
spellingShingle 550 Earth sciences & geology
Anjar, Johanna
Akҫar, Naki
Larsen, Eiliv A.
Lyså, Astrid
Marrero, Shasta
Mozafari, Nasim
Vockenhuber, Christof
Cosmogenic Exposure Dating (36Cl) of Landforms on Jan Mayen, North Atlantic, and the Effects of Bedrock Formation Age Assumptions on 36Cl Ages
topic_facet 550 Earth sciences & geology
description Jan Mayen is a small volcanic island situated 550 km north of Iceland. Glacial sediments and landforms are relatively common on the island but, so far, only a few of them have been dated. In this study, we present and discuss 89 36Cl dates of primarily glacial and volcanic events on Jan Mayen. Calculations of sample exposure ages were complicated by young exposure ages, young rock formation age, and high native Cl contents, leading to updates in CRONUScalc to enable accurate exposure age calculations. The samples provide good evidence against an equilibrium assumption when subtracting background production (e.g., 36Cl produced by neutron capture from fission of U or Th) for samples on young bedrock, with younger exposure ages most significantly affected. Exposure ages were calculated with a range of assumptions of bedrock formation ages appropriate for Jan Mayen, including the assumption that the rock formation age equaled the exposure age (i.e., the youngest age it could possibly have), and we found that although the effect on most of the ages was small, the calculated ages of 25 of the samples increased by more than 1 standard deviation from the age calculated assuming equilibrium background production, with a maximum deviation of 6.1 ka. Due to the very young bedrock on Jan Mayen, we consider the nonequilibrium ages to be the most reliable ages from the island and conclude that large-scale deglaciation on the south and central, lower-lying, parts of the island, started around 20 ka and lasted until ~7 ka. On northern Jan Mayen, the slopes of the 2277 m high stratovolcano Beerenberg are currently partly glaciated; however, outside of the Little Ice Age moraines, all but two samples give ages between 14 and 5.7 ka.
format Text
author Anjar, Johanna
Akҫar, Naki
Larsen, Eiliv A.
Lyså, Astrid
Marrero, Shasta
Mozafari, Nasim
Vockenhuber, Christof
author_facet Anjar, Johanna
Akҫar, Naki
Larsen, Eiliv A.
Lyså, Astrid
Marrero, Shasta
Mozafari, Nasim
Vockenhuber, Christof
author_sort Anjar, Johanna
title Cosmogenic Exposure Dating (36Cl) of Landforms on Jan Mayen, North Atlantic, and the Effects of Bedrock Formation Age Assumptions on 36Cl Ages
title_short Cosmogenic Exposure Dating (36Cl) of Landforms on Jan Mayen, North Atlantic, and the Effects of Bedrock Formation Age Assumptions on 36Cl Ages
title_full Cosmogenic Exposure Dating (36Cl) of Landforms on Jan Mayen, North Atlantic, and the Effects of Bedrock Formation Age Assumptions on 36Cl Ages
title_fullStr Cosmogenic Exposure Dating (36Cl) of Landforms on Jan Mayen, North Atlantic, and the Effects of Bedrock Formation Age Assumptions on 36Cl Ages
title_full_unstemmed Cosmogenic Exposure Dating (36Cl) of Landforms on Jan Mayen, North Atlantic, and the Effects of Bedrock Formation Age Assumptions on 36Cl Ages
title_sort cosmogenic exposure dating (36cl) of landforms on jan mayen, north atlantic, and the effects of bedrock formation age assumptions on 36cl ages
publisher MDPI
publishDate 2021
url https://dx.doi.org/10.48350/166685
https://boris.unibe.ch/166685/
long_lat ENVELOPE(-8.167,-8.167,71.083,71.083)
geographic Jan Mayen
Beerenberg
geographic_facet Jan Mayen
Beerenberg
genre Iceland
Jan Mayen
North Atlantic
genre_facet Iceland
Jan Mayen
North Atlantic
op_relation https://dx.doi.org/10.3390/geosciences11090390
op_rights open access
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
http://purl.org/coar/access_right/c_abf2
op_rightsnorm CC-BY
op_doi https://doi.org/10.48350/166685
https://doi.org/10.3390/geosciences11090390
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