Clay mineral and Nd, Pb, and Sr isotope provenance of a MIS 4-3 sediment record from the Lomonosov Ridge, central Arctic Ocean
Modern techniques for detrital mineral provenance were applied to sediment core 96/12-1pc from the Lomonosov Ridge in the central Arctic Ocean. The techniques include quantitative clay mineralogy analysis combined with determination of Nd, Pb, and Sr isotopes from clay fraction. The clay mineral ass...
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Geological Society of Finland
2023
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ftdoajarticles:oai:doaj.org/article:7d33ffeac795429d808e0bd80be1cc9a 2023-07-30T04:01:08+02:00 Clay mineral and Nd, Pb, and Sr isotope provenance of a MIS 4-3 sediment record from the Lomonosov Ridge, central Arctic Ocean Raisa Alatarvas Ninna Immonen Kari Strand 2023-04-01T00:00:00Z https://doi.org/10.17741/bgsf/95.1.003 https://doaj.org/article/7d33ffeac795429d808e0bd80be1cc9a EN eng Geological Society of Finland https://www.geologinenseura.fi/sites/geologinenseura.fi/files/alatarvas_et_al_95_1_2023.pdf https://doaj.org/toc/0367-5211 https://doaj.org/toc/1799-4632 doi:10.17741/bgsf/95.1.003 0367-5211 1799-4632 https://doaj.org/article/7d33ffeac795429d808e0bd80be1cc9a Bulletin of the Geological Society of Finland, Vol 95, Iss 1, Pp 35-46 (2023) lomonosov ridge arctic ocean marine sediments middle weichselian glaciation clay mineralogy nd-sr-pb isotopes Geology QE1-996.5 article 2023 ftdoajarticles https://doi.org/10.17741/bgsf/95.1.003 2023-07-16T00:37:33Z Modern techniques for detrital mineral provenance were applied to sediment core 96/12-1pc from the Lomonosov Ridge in the central Arctic Ocean. The techniques include quantitative clay mineralogy analysis combined with determination of Nd, Pb, and Sr isotopes from clay fraction. The clay mineral assemblage and the isotope signatures depict distinct changes during the Marine Isotope Stage (MIS) 4-3 transition corresponding to the Middle Weichselian deglaciation. This transition is characterised by a homogenous, 48 cm thick, dark grey, silty clay layer with a distinctive IRD concentration, forming a prominent marker bed for the central Arctic Ocean sediments. The elevated smectite and kaolinite contents in the transitional interval are possible weathering products of the Siberian basaltic rocks, such as the Putorana Plateau, feeding the shelves of the Kara Sea and the western Laptev Sea. The Nd and Sr isotope values are compatible with input from the basaltic rocks and fall within the isotopic range of sediments from these shelves. The abrupt changes in the Nd, Pb and Sr isotopic data from the distinct grey layer attributed to the MIS 4-3 transition likely mark a pronounced deglaciation event. An increase in coarse debris in the grey layer indicates a change in the sedimentation regime with a strong iceberg rafting component. This change may also be related to a sudden release of meltwater from a large ice-dammed lake in the northern Siberia. Article in Journal/Newspaper Arctic Arctic Ocean Iceberg* Kara Sea laptev Laptev Sea Lomonosov Ridge Siberia Directory of Open Access Journals: DOAJ Articles Arctic Arctic Ocean Dammed Lake ENVELOPE(-68.258,-68.258,68.496,68.496) Kara Sea Laptev Sea Bulletin of the Geological Society of Finland 95 1 35 46 |
institution |
Open Polar |
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Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
lomonosov ridge arctic ocean marine sediments middle weichselian glaciation clay mineralogy nd-sr-pb isotopes Geology QE1-996.5 |
spellingShingle |
lomonosov ridge arctic ocean marine sediments middle weichselian glaciation clay mineralogy nd-sr-pb isotopes Geology QE1-996.5 Raisa Alatarvas Ninna Immonen Kari Strand Clay mineral and Nd, Pb, and Sr isotope provenance of a MIS 4-3 sediment record from the Lomonosov Ridge, central Arctic Ocean |
topic_facet |
lomonosov ridge arctic ocean marine sediments middle weichselian glaciation clay mineralogy nd-sr-pb isotopes Geology QE1-996.5 |
description |
Modern techniques for detrital mineral provenance were applied to sediment core 96/12-1pc from the Lomonosov Ridge in the central Arctic Ocean. The techniques include quantitative clay mineralogy analysis combined with determination of Nd, Pb, and Sr isotopes from clay fraction. The clay mineral assemblage and the isotope signatures depict distinct changes during the Marine Isotope Stage (MIS) 4-3 transition corresponding to the Middle Weichselian deglaciation. This transition is characterised by a homogenous, 48 cm thick, dark grey, silty clay layer with a distinctive IRD concentration, forming a prominent marker bed for the central Arctic Ocean sediments. The elevated smectite and kaolinite contents in the transitional interval are possible weathering products of the Siberian basaltic rocks, such as the Putorana Plateau, feeding the shelves of the Kara Sea and the western Laptev Sea. The Nd and Sr isotope values are compatible with input from the basaltic rocks and fall within the isotopic range of sediments from these shelves. The abrupt changes in the Nd, Pb and Sr isotopic data from the distinct grey layer attributed to the MIS 4-3 transition likely mark a pronounced deglaciation event. An increase in coarse debris in the grey layer indicates a change in the sedimentation regime with a strong iceberg rafting component. This change may also be related to a sudden release of meltwater from a large ice-dammed lake in the northern Siberia. |
format |
Article in Journal/Newspaper |
author |
Raisa Alatarvas Ninna Immonen Kari Strand |
author_facet |
Raisa Alatarvas Ninna Immonen Kari Strand |
author_sort |
Raisa Alatarvas |
title |
Clay mineral and Nd, Pb, and Sr isotope provenance of a MIS 4-3 sediment record from the Lomonosov Ridge, central Arctic Ocean |
title_short |
Clay mineral and Nd, Pb, and Sr isotope provenance of a MIS 4-3 sediment record from the Lomonosov Ridge, central Arctic Ocean |
title_full |
Clay mineral and Nd, Pb, and Sr isotope provenance of a MIS 4-3 sediment record from the Lomonosov Ridge, central Arctic Ocean |
title_fullStr |
Clay mineral and Nd, Pb, and Sr isotope provenance of a MIS 4-3 sediment record from the Lomonosov Ridge, central Arctic Ocean |
title_full_unstemmed |
Clay mineral and Nd, Pb, and Sr isotope provenance of a MIS 4-3 sediment record from the Lomonosov Ridge, central Arctic Ocean |
title_sort |
clay mineral and nd, pb, and sr isotope provenance of a mis 4-3 sediment record from the lomonosov ridge, central arctic ocean |
publisher |
Geological Society of Finland |
publishDate |
2023 |
url |
https://doi.org/10.17741/bgsf/95.1.003 https://doaj.org/article/7d33ffeac795429d808e0bd80be1cc9a |
long_lat |
ENVELOPE(-68.258,-68.258,68.496,68.496) |
geographic |
Arctic Arctic Ocean Dammed Lake Kara Sea Laptev Sea |
geographic_facet |
Arctic Arctic Ocean Dammed Lake Kara Sea Laptev Sea |
genre |
Arctic Arctic Ocean Iceberg* Kara Sea laptev Laptev Sea Lomonosov Ridge Siberia |
genre_facet |
Arctic Arctic Ocean Iceberg* Kara Sea laptev Laptev Sea Lomonosov Ridge Siberia |
op_source |
Bulletin of the Geological Society of Finland, Vol 95, Iss 1, Pp 35-46 (2023) |
op_relation |
https://www.geologinenseura.fi/sites/geologinenseura.fi/files/alatarvas_et_al_95_1_2023.pdf https://doaj.org/toc/0367-5211 https://doaj.org/toc/1799-4632 doi:10.17741/bgsf/95.1.003 0367-5211 1799-4632 https://doaj.org/article/7d33ffeac795429d808e0bd80be1cc9a |
op_doi |
https://doi.org/10.17741/bgsf/95.1.003 |
container_title |
Bulletin of the Geological Society of Finland |
container_volume |
95 |
container_issue |
1 |
container_start_page |
35 |
op_container_end_page |
46 |
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1772811880750907392 |