Holocene hydrographical change in the eastern Laptev Sea (Siberian Arctic) recorded in delta 18 O profiles of bivalve shells
Oxygen isotope profiles along the growth axis of fossil bivalve shells of Macoma calcarea were established to reconstruct hydrographical changes in the eastern Laptev Sea since 8400 cal yr B.P. The variability of the oxygen isotopes (δ18O) in the individual records is mainly attributed to variations...
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Elsevier
2004
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ftoceanrep:oai:oceanrep.geomar.de:5442 2023-05-15T14:26:28+02:00 Holocene hydrographical change in the eastern Laptev Sea (Siberian Arctic) recorded in delta 18 O profiles of bivalve shells Müller-Lupp, Thomas Bauch, Henning Erlenkeuser, Helmut 2004 text https://oceanrep.geomar.de/id/eprint/5442/ https://oceanrep.geomar.de/id/eprint/5442/3/2004_Mueller-Lupp-etal_Holocene_QuaSci-61.pdf http://dx.doi.org/0.1016/j.yqres.2003.09.003 https://doi.org/10.1016/j.yqres.2003.09.003 en eng Elsevier https://oceanrep.geomar.de/id/eprint/5442/3/2004_Mueller-Lupp-etal_Holocene_QuaSci-61.pdf Müller-Lupp, T., Bauch, H. and Erlenkeuser, H. (2004) Holocene hydrographical change in the eastern Laptev Sea (Siberian Arctic) recorded in delta18O profiles of bivalve shells. Quaternary Research, 61 (1). pp. 32-41. DOI 10.1016/j.yqres.2003.09.003 <https://doi.org/10.1016/j.yqres.2003.09.003>. doi:10.1016/j.yqres.2003.09.003 info:eu-repo/semantics/restrictedAccess Article PeerReviewed 2004 ftoceanrep https://doi.org/10.1016/j.yqres.2003.09.003 2023-04-07T14:51:03Z Oxygen isotope profiles along the growth axis of fossil bivalve shells of Macoma calcarea were established to reconstruct hydrographical changes in the eastern Laptev Sea since 8400 cal yr B.P. The variability of the oxygen isotopes (δ18O) in the individual records is mainly attributed to variations in the salinity of bottom waters in the Laptev Sea with a modern ratio of 0.50‰/salinity. The high-resolution δ18O profiles exhibit distinct and annual cycles from which the seasonal and annual salinity variations at the investigated site can be reconstructed. Based on the modern analogue approach oxygen isotope profiles of radiocarbon-dated bivalve shells from a sediment core located northeast of the Lena Delta provide seasonal and subdecadal insights into past hydrological conditions and their relation to the Holocene transgressional history of the Laptev Sea shelf. Under the assumption that the modern relationship between δ18Ow and salinity has been constant throughout the time, the δ18O of an 8400-cal-yr-old bivalves would suggest that bottom-water salinity was reduced and the temperature was slightly warmer, both suggesting a stronger mixture of riverine water to the bottom water. Reconstruction of the inundation history of the Laptev Sea shelf indicates local sea level ∼27 m below present at this time and a closer proximity of the site to the coastline and the Lena River mouth. Due to continuing sea level rise and a southward retreat of the river mouth, bottom-water salinity increased at 7200 cal yr B.P. along with an increase in seasonal variability. Conditions comparable to the modern hydrography were achieved by 3800 cal yr B.P. Article in Journal/Newspaper Arctic Arctic laptev Laptev Sea lena delta lena river OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Arctic Laptev Sea Quaternary Research 61 1 32 41 |
institution |
Open Polar |
collection |
OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
op_collection_id |
ftoceanrep |
language |
English |
description |
Oxygen isotope profiles along the growth axis of fossil bivalve shells of Macoma calcarea were established to reconstruct hydrographical changes in the eastern Laptev Sea since 8400 cal yr B.P. The variability of the oxygen isotopes (δ18O) in the individual records is mainly attributed to variations in the salinity of bottom waters in the Laptev Sea with a modern ratio of 0.50‰/salinity. The high-resolution δ18O profiles exhibit distinct and annual cycles from which the seasonal and annual salinity variations at the investigated site can be reconstructed. Based on the modern analogue approach oxygen isotope profiles of radiocarbon-dated bivalve shells from a sediment core located northeast of the Lena Delta provide seasonal and subdecadal insights into past hydrological conditions and their relation to the Holocene transgressional history of the Laptev Sea shelf. Under the assumption that the modern relationship between δ18Ow and salinity has been constant throughout the time, the δ18O of an 8400-cal-yr-old bivalves would suggest that bottom-water salinity was reduced and the temperature was slightly warmer, both suggesting a stronger mixture of riverine water to the bottom water. Reconstruction of the inundation history of the Laptev Sea shelf indicates local sea level ∼27 m below present at this time and a closer proximity of the site to the coastline and the Lena River mouth. Due to continuing sea level rise and a southward retreat of the river mouth, bottom-water salinity increased at 7200 cal yr B.P. along with an increase in seasonal variability. Conditions comparable to the modern hydrography were achieved by 3800 cal yr B.P. |
format |
Article in Journal/Newspaper |
author |
Müller-Lupp, Thomas Bauch, Henning Erlenkeuser, Helmut |
spellingShingle |
Müller-Lupp, Thomas Bauch, Henning Erlenkeuser, Helmut Holocene hydrographical change in the eastern Laptev Sea (Siberian Arctic) recorded in delta 18 O profiles of bivalve shells |
author_facet |
Müller-Lupp, Thomas Bauch, Henning Erlenkeuser, Helmut |
author_sort |
Müller-Lupp, Thomas |
title |
Holocene hydrographical change in the eastern Laptev Sea (Siberian Arctic) recorded in delta 18 O profiles of bivalve shells |
title_short |
Holocene hydrographical change in the eastern Laptev Sea (Siberian Arctic) recorded in delta 18 O profiles of bivalve shells |
title_full |
Holocene hydrographical change in the eastern Laptev Sea (Siberian Arctic) recorded in delta 18 O profiles of bivalve shells |
title_fullStr |
Holocene hydrographical change in the eastern Laptev Sea (Siberian Arctic) recorded in delta 18 O profiles of bivalve shells |
title_full_unstemmed |
Holocene hydrographical change in the eastern Laptev Sea (Siberian Arctic) recorded in delta 18 O profiles of bivalve shells |
title_sort |
holocene hydrographical change in the eastern laptev sea (siberian arctic) recorded in delta 18 o profiles of bivalve shells |
publisher |
Elsevier |
publishDate |
2004 |
url |
https://oceanrep.geomar.de/id/eprint/5442/ https://oceanrep.geomar.de/id/eprint/5442/3/2004_Mueller-Lupp-etal_Holocene_QuaSci-61.pdf http://dx.doi.org/0.1016/j.yqres.2003.09.003 https://doi.org/10.1016/j.yqres.2003.09.003 |
geographic |
Arctic Laptev Sea |
geographic_facet |
Arctic Laptev Sea |
genre |
Arctic Arctic laptev Laptev Sea lena delta lena river |
genre_facet |
Arctic Arctic laptev Laptev Sea lena delta lena river |
op_relation |
https://oceanrep.geomar.de/id/eprint/5442/3/2004_Mueller-Lupp-etal_Holocene_QuaSci-61.pdf Müller-Lupp, T., Bauch, H. and Erlenkeuser, H. (2004) Holocene hydrographical change in the eastern Laptev Sea (Siberian Arctic) recorded in delta18O profiles of bivalve shells. Quaternary Research, 61 (1). pp. 32-41. DOI 10.1016/j.yqres.2003.09.003 <https://doi.org/10.1016/j.yqres.2003.09.003>. doi:10.1016/j.yqres.2003.09.003 |
op_rights |
info:eu-repo/semantics/restrictedAccess |
op_doi |
https://doi.org/10.1016/j.yqres.2003.09.003 |
container_title |
Quaternary Research |
container_volume |
61 |
container_issue |
1 |
container_start_page |
32 |
op_container_end_page |
41 |
_version_ |
1766299050084139008 |