Postglacial relative sea level change and glacier activity in the early and late Holocene: Wahlenbergfjorden, Nordaustlandet, Svalbard

Sediment cores from Kløverbladvatna, a threshold lake in Wahlenbergfjorden, Nordaustlandet, Svalbard were used to reconstruct Holocene glacier fluctuations. Meltwater from Etonbreen spills over a threshold to the lake, only when the glacier is significantly larger than at present. Lithological logg...

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Published in:Scientific Reports
Main Authors: Schomacker, Anders, Farnsworth, Wesley R., Ingólfsson, Ólafur, Allaart, Lis, Håkansson, Lena, Retelle, Michael, Siggaard-Andersen, Marie-Louise, Korsgaard, Niels Jákup, Rouillard, Alexandra, Kjellman, Sofia E.
Format: Article in Journal/Newspaper
Language:English
Published: Department of Geosciences, UiT The Arctic University of Norway, Langnes, Tromsø, Norway 2019
Subjects:
Online Access:http://urn.kb.se/resolve?urn=urn:nbn:se:umu:diva-225435
https://doi.org/10.1038/s41598-019-43342-z
id ftumeauniv:oai:DiVA.org:umu-225435
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spelling ftumeauniv:oai:DiVA.org:umu-225435 2024-09-09T19:41:37+00:00 Postglacial relative sea level change and glacier activity in the early and late Holocene: Wahlenbergfjorden, Nordaustlandet, Svalbard Schomacker, Anders Farnsworth, Wesley R. Ingólfsson, Ólafur Allaart, Lis HÃ¥kansson, Lena Retelle, Michael Siggaard-Andersen, Marie-Louise Korsgaard, Niels Jákup Rouillard, Alexandra Kjellman, Sofia E. 2019 application/pdf http://urn.kb.se/resolve?urn=urn:nbn:se:umu:diva-225435 https://doi.org/10.1038/s41598-019-43342-z eng eng Department of Geosciences, UiT The Arctic University of Norway, Langnes, Tromsø, Norway Department of Arctic Geology, The University Centre in Svalbard (UNIS), Longyearbyen, Norway Department of Arctic Geology, The University Centre in Svalbard (UNIS), Longyearbyen, Norway; Faculty of Earth Sciences, University of Iceland, Askja, Reykjavík, Iceland Department of Geosciences, UiT The Arctic University of Norway, Tromsø, Norway Department of Arctic Geology, The University Centre in Svalbard (UNIS), Longyearbyen, Norway; Bates College, Carnegie Science Center, Lewiston, Maine, USA Center for GeoGenetics, Natural History Museum of Denmark, University of Copenhagen, Copenhagen, Denmark Geological Survey of Denmark and Greenland (GEUS), Copenhagen, Denmark Department of Geosciences, UiT The Arctic University of Norway, Tromsø, Norway; Center for GeoGenetics, Natural History Museum of Denmark, University of Copenhagen, Copenhagen, Denmark Scientific Reports, 2019, 9:1, orcid:0000-0002-8031-9008 orcid:0000-0002-8700-7023 http://urn.kb.se/resolve?urn=urn:nbn:se:umu:diva-225435 doi:10.1038/s41598-019-43342-z PMID 31043668 ISI:000466359700012 Scopus 2-s2.0-85065159841 info:eu-repo/semantics/openAccess Earth and Related Environmental Sciences Geovetenskap och miljövetenskap Article in journal info:eu-repo/semantics/article text 2019 ftumeauniv https://doi.org/10.1038/s41598-019-43342-z 2024-06-18T23:59:04Z Sediment cores from Kløverbladvatna, a threshold lake in Wahlenbergfjorden, Nordaustlandet, Svalbard were used to reconstruct Holocene glacier fluctuations. Meltwater from Etonbreen spills over a threshold to the lake, only when the glacier is significantly larger than at present. Lithological logging, loss-on-ignition, ITRAX scanning and radiocarbon dating of the cores show that Kløverbladvatna became isolated from Wahlenbergfjorden c. 5.4 cal. kyr BP due to glacioisostatic rebound. During the Late Holocene, laminated clayey gyttja from lacustrine organic production and surface runoff from the catchment accumulated in the lake. The lacustrine sedimentary record suggests that meltwater only spilled over the threshold at the peak of the surge of Etonbreen in AD 1938. Hence, we suggest that this was the largest extent of Etonbreen in the (mid-late) Holocene. In Palanderbukta, a tributary fjord to Wahlenbergfjorden, raised beaches were surveyed and organic material collected to determine the age of the beaches and reconstruct postglacial relative sea level change. The age of the postglacial raised beaches ranges from 10.7 cal. kyr BP at 50 m a.s.l. to 3.13 cal. kyr BP at 2 m a.s.l. The reconstructed postglacial relative sea level curve adds valuable spatial and chronological data to the relative sea level record of Nordaustlandet. Article in Journal/Newspaper glacier Nordaustlandet Svalbard Umeå University: Publications (DiVA) Svalbard Nordaustlandet ENVELOPE(22.400,22.400,79.800,79.800) The Beaches ENVELOPE(-56.832,-56.832,49.583,49.583) Wahlenbergfjorden ENVELOPE(20.593,20.593,79.721,79.721) Etonbreen ENVELOPE(21.892,21.892,79.716,79.716) Palanderbukta ENVELOPE(20.642,20.642,79.590,79.590) Scientific Reports 9 1
institution Open Polar
collection Umeå University: Publications (DiVA)
op_collection_id ftumeauniv
language English
topic Earth and Related Environmental Sciences
Geovetenskap och miljövetenskap
spellingShingle Earth and Related Environmental Sciences
Geovetenskap och miljövetenskap
Schomacker, Anders
Farnsworth, Wesley R.
Ingólfsson, Ólafur
Allaart, Lis
HÃ¥kansson, Lena
Retelle, Michael
Siggaard-Andersen, Marie-Louise
Korsgaard, Niels Jákup
Rouillard, Alexandra
Kjellman, Sofia E.
Postglacial relative sea level change and glacier activity in the early and late Holocene: Wahlenbergfjorden, Nordaustlandet, Svalbard
topic_facet Earth and Related Environmental Sciences
Geovetenskap och miljövetenskap
description Sediment cores from Kløverbladvatna, a threshold lake in Wahlenbergfjorden, Nordaustlandet, Svalbard were used to reconstruct Holocene glacier fluctuations. Meltwater from Etonbreen spills over a threshold to the lake, only when the glacier is significantly larger than at present. Lithological logging, loss-on-ignition, ITRAX scanning and radiocarbon dating of the cores show that Kløverbladvatna became isolated from Wahlenbergfjorden c. 5.4 cal. kyr BP due to glacioisostatic rebound. During the Late Holocene, laminated clayey gyttja from lacustrine organic production and surface runoff from the catchment accumulated in the lake. The lacustrine sedimentary record suggests that meltwater only spilled over the threshold at the peak of the surge of Etonbreen in AD 1938. Hence, we suggest that this was the largest extent of Etonbreen in the (mid-late) Holocene. In Palanderbukta, a tributary fjord to Wahlenbergfjorden, raised beaches were surveyed and organic material collected to determine the age of the beaches and reconstruct postglacial relative sea level change. The age of the postglacial raised beaches ranges from 10.7 cal. kyr BP at 50 m a.s.l. to 3.13 cal. kyr BP at 2 m a.s.l. The reconstructed postglacial relative sea level curve adds valuable spatial and chronological data to the relative sea level record of Nordaustlandet.
format Article in Journal/Newspaper
author Schomacker, Anders
Farnsworth, Wesley R.
Ingólfsson, Ólafur
Allaart, Lis
HÃ¥kansson, Lena
Retelle, Michael
Siggaard-Andersen, Marie-Louise
Korsgaard, Niels Jákup
Rouillard, Alexandra
Kjellman, Sofia E.
author_facet Schomacker, Anders
Farnsworth, Wesley R.
Ingólfsson, Ólafur
Allaart, Lis
HÃ¥kansson, Lena
Retelle, Michael
Siggaard-Andersen, Marie-Louise
Korsgaard, Niels Jákup
Rouillard, Alexandra
Kjellman, Sofia E.
author_sort Schomacker, Anders
title Postglacial relative sea level change and glacier activity in the early and late Holocene: Wahlenbergfjorden, Nordaustlandet, Svalbard
title_short Postglacial relative sea level change and glacier activity in the early and late Holocene: Wahlenbergfjorden, Nordaustlandet, Svalbard
title_full Postglacial relative sea level change and glacier activity in the early and late Holocene: Wahlenbergfjorden, Nordaustlandet, Svalbard
title_fullStr Postglacial relative sea level change and glacier activity in the early and late Holocene: Wahlenbergfjorden, Nordaustlandet, Svalbard
title_full_unstemmed Postglacial relative sea level change and glacier activity in the early and late Holocene: Wahlenbergfjorden, Nordaustlandet, Svalbard
title_sort postglacial relative sea level change and glacier activity in the early and late holocene: wahlenbergfjorden, nordaustlandet, svalbard
publisher Department of Geosciences, UiT The Arctic University of Norway, Langnes, Tromsø, Norway
publishDate 2019
url http://urn.kb.se/resolve?urn=urn:nbn:se:umu:diva-225435
https://doi.org/10.1038/s41598-019-43342-z
long_lat ENVELOPE(22.400,22.400,79.800,79.800)
ENVELOPE(-56.832,-56.832,49.583,49.583)
ENVELOPE(20.593,20.593,79.721,79.721)
ENVELOPE(21.892,21.892,79.716,79.716)
ENVELOPE(20.642,20.642,79.590,79.590)
geographic Svalbard
Nordaustlandet
The Beaches
Wahlenbergfjorden
Etonbreen
Palanderbukta
geographic_facet Svalbard
Nordaustlandet
The Beaches
Wahlenbergfjorden
Etonbreen
Palanderbukta
genre glacier
Nordaustlandet
Svalbard
genre_facet glacier
Nordaustlandet
Svalbard
op_relation Scientific Reports, 2019, 9:1,
orcid:0000-0002-8031-9008
orcid:0000-0002-8700-7023
http://urn.kb.se/resolve?urn=urn:nbn:se:umu:diva-225435
doi:10.1038/s41598-019-43342-z
PMID 31043668
ISI:000466359700012
Scopus 2-s2.0-85065159841
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1038/s41598-019-43342-z
container_title Scientific Reports
container_volume 9
container_issue 1
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