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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Online Access: | https://orca.cardiff.ac.uk/id/eprint/144691/ https://doi.org/10.3390/geosciences11090390 https://orca.cardiff.ac.uk/id/eprint/144691/1/geosciences-11-00390.pdf |
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ftunivcardiff:oai:https://orca.cardiff.ac.uk:144691 2023-05-15T16:51:41+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 2021-09-15 application/pdf https://orca.cardiff.ac.uk/id/eprint/144691/ https://doi.org/10.3390/geosciences11090390 https://orca.cardiff.ac.uk/id/eprint/144691/1/geosciences-11-00390.pdf en eng MDPI https://orca.cardiff.ac.uk/id/eprint/144691/1/geosciences-11-00390.pdf Anjar, Johanna, Akҫar, Naki, Larsen, Eiliv A., Lyså, Astrid, Marrero, Shasta https://orca.cardiff.ac.uk/view/cardiffauthors/A2529897K.html orcid:0000-0003-2917-0292 orcid:0000-0003-2917-0292, Mozafari, Nasim and Vockenhuber, Christof 2021. Cosmogenic exposure dating (36Cl) of landforms on Jan Mayen, North Atlantic, and the effects of bedrock formation age assumptions on 36Cl ages. Geosciences 11 (9) , 390. 10.3390/geosciences11090390 https://doi.org/10.3390/geosciences11090390 file https://orca.cardiff.ac.uk/144691/1/geosciences-11-00390.pdf doi:10.3390/geosciences11090390 cc_by CC-BY Article PeerReviewed 2021 ftunivcardiff https://doi.org/10.3390/geosciences11090390 2022-11-10T23:41:49Z 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. Article in Journal/Newspaper Iceland Jan Mayen North Atlantic Cardiff University: ORCA (Online Research @ Cardiff) Beerenberg ENVELOPE(-8.167,-8.167,71.083,71.083) Jan Mayen Geosciences 11 9 390 |
institution |
Open Polar |
collection |
Cardiff University: ORCA (Online Research @ Cardiff) |
op_collection_id |
ftunivcardiff |
language |
English |
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 |
Article in Journal/Newspaper |
author |
Anjar, Johanna Akҫar, Naki Larsen, Eiliv A. Lyså, Astrid Marrero, Shasta Mozafari, Nasim Vockenhuber, Christof |
spellingShingle |
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 |
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://orca.cardiff.ac.uk/id/eprint/144691/ https://doi.org/10.3390/geosciences11090390 https://orca.cardiff.ac.uk/id/eprint/144691/1/geosciences-11-00390.pdf |
long_lat |
ENVELOPE(-8.167,-8.167,71.083,71.083) |
geographic |
Beerenberg Jan Mayen |
geographic_facet |
Beerenberg Jan Mayen |
genre |
Iceland Jan Mayen North Atlantic |
genre_facet |
Iceland Jan Mayen North Atlantic |
op_relation |
https://orca.cardiff.ac.uk/id/eprint/144691/1/geosciences-11-00390.pdf Anjar, Johanna, Akҫar, Naki, Larsen, Eiliv A., Lyså, Astrid, Marrero, Shasta https://orca.cardiff.ac.uk/view/cardiffauthors/A2529897K.html orcid:0000-0003-2917-0292 orcid:0000-0003-2917-0292, Mozafari, Nasim and Vockenhuber, Christof 2021. Cosmogenic exposure dating (36Cl) of landforms on Jan Mayen, North Atlantic, and the effects of bedrock formation age assumptions on 36Cl ages. Geosciences 11 (9) , 390. 10.3390/geosciences11090390 https://doi.org/10.3390/geosciences11090390 file https://orca.cardiff.ac.uk/144691/1/geosciences-11-00390.pdf doi:10.3390/geosciences11090390 |
op_rights |
cc_by |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.3390/geosciences11090390 |
container_title |
Geosciences |
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11 |
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9 |
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390 |
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