Results from ikaite investigations in the Kara Sea ...

The authigenic carbonate mineral ikaite is specific of low-temperature high latitude environments. The depletion of ikaite carbon in 13C isotopes in most cases implies a causal relation of ikaite generation with methane geochemistry. In this paper we present new data on ikaite minerals in Holocene s...

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Main Authors: Kodina, Ludmilla A, Tokarev, V G, Vlasova, Ludmilla N, Korobeinik, G S
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2003
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.804557
https://doi.pangaea.de/10.1594/PANGAEA.804557
id ftdatacite:10.1594/pangaea.804557
record_format openpolar
spelling ftdatacite:10.1594/pangaea.804557 2024-09-15T18:16:09+00:00 Results from ikaite investigations in the Kara Sea ... Kodina, Ludmilla A Tokarev, V G Vlasova, Ludmilla N Korobeinik, G S 2003 application/zip https://dx.doi.org/10.1594/pangaea.804557 https://doi.pangaea.de/10.1594/PANGAEA.804557 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Siberian River Run-Off SIRRO article Collection Supplementary Publication Series of Datasets 2003 ftdatacite https://doi.org/10.1594/pangaea.804557 2024-08-01T10:59:23Z The authigenic carbonate mineral ikaite is specific of low-temperature high latitude environments. The depletion of ikaite carbon in 13C isotopes in most cases implies a causal relation of ikaite generation with methane geochemistry. In this paper we present new data on ikaite minerals in Holocene sediments sampled along the Yenisei channel at the southern (74°N) and northern (77°N) ends. Stable carbon isotopes of the ikaite crystals were studied in conjunction with the hydrochemistry and isotope geochemistry of the sediments. Pore water and natural gas samples were separated from sediments to describe the methane carbon isotope distribution pattern throughout two sedimentary sequences embedding the ikaite crystals of different isotope composition (-24 per mil and -42 per mil). The biogenic nature of the methane is indicated by 51 C values being as low as -104.4 per mil. In the case of the moderately depleted sample (-24 per mil) from the southern location the small-scale ikaite formation fits best into the ... : Supplement to: Kodina, Ludmilla A; Tokarev, V G; Vlasova, Ludmilla N; Korobeinik, G S (2003): Contribution of biogenic methane to ikaite formation in the Kara Sea: evidence from the stable carbon isotope geochemistry. In: Stein, R; Fahl, K; Fütterer, D K; Galimov, E M & Stepanets, O V (eds.), Siberian River Run-off in the Kara Sea: Characterisation, Quantification, Variability, and Environmental Significance, 488 pp. Proceedings in Marine Sciences, Elsevier, Amsterdam, 6, 349-374 ... Article in Journal/Newspaper Kara Sea DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Siberian River Run-Off SIRRO
spellingShingle Siberian River Run-Off SIRRO
Kodina, Ludmilla A
Tokarev, V G
Vlasova, Ludmilla N
Korobeinik, G S
Results from ikaite investigations in the Kara Sea ...
topic_facet Siberian River Run-Off SIRRO
description The authigenic carbonate mineral ikaite is specific of low-temperature high latitude environments. The depletion of ikaite carbon in 13C isotopes in most cases implies a causal relation of ikaite generation with methane geochemistry. In this paper we present new data on ikaite minerals in Holocene sediments sampled along the Yenisei channel at the southern (74°N) and northern (77°N) ends. Stable carbon isotopes of the ikaite crystals were studied in conjunction with the hydrochemistry and isotope geochemistry of the sediments. Pore water and natural gas samples were separated from sediments to describe the methane carbon isotope distribution pattern throughout two sedimentary sequences embedding the ikaite crystals of different isotope composition (-24 per mil and -42 per mil). The biogenic nature of the methane is indicated by 51 C values being as low as -104.4 per mil. In the case of the moderately depleted sample (-24 per mil) from the southern location the small-scale ikaite formation fits best into the ... : Supplement to: Kodina, Ludmilla A; Tokarev, V G; Vlasova, Ludmilla N; Korobeinik, G S (2003): Contribution of biogenic methane to ikaite formation in the Kara Sea: evidence from the stable carbon isotope geochemistry. In: Stein, R; Fahl, K; Fütterer, D K; Galimov, E M & Stepanets, O V (eds.), Siberian River Run-off in the Kara Sea: Characterisation, Quantification, Variability, and Environmental Significance, 488 pp. Proceedings in Marine Sciences, Elsevier, Amsterdam, 6, 349-374 ...
format Article in Journal/Newspaper
author Kodina, Ludmilla A
Tokarev, V G
Vlasova, Ludmilla N
Korobeinik, G S
author_facet Kodina, Ludmilla A
Tokarev, V G
Vlasova, Ludmilla N
Korobeinik, G S
author_sort Kodina, Ludmilla A
title Results from ikaite investigations in the Kara Sea ...
title_short Results from ikaite investigations in the Kara Sea ...
title_full Results from ikaite investigations in the Kara Sea ...
title_fullStr Results from ikaite investigations in the Kara Sea ...
title_full_unstemmed Results from ikaite investigations in the Kara Sea ...
title_sort results from ikaite investigations in the kara sea ...
publisher PANGAEA
publishDate 2003
url https://dx.doi.org/10.1594/pangaea.804557
https://doi.pangaea.de/10.1594/PANGAEA.804557
genre Kara Sea
genre_facet Kara Sea
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.804557
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