Alkanes in Quaternary deposits of the Laptev Sea

E. A. Romankevich; A. A. Vetrov; N. A. Belyaev; V. I. Sergienko; I. P. Semiletov; S. V. Sukhoverkhov; S. Yu. Bratskaya; N. A. Prokuda; A. S. Ulyantsev

doi:10.1134/S1028334X17010093

Alkanes in Quaternary deposits of the Laptev Sea

作者: Romankevich E.A.¹^,2, Vetrov A.A.¹, Belyaev N.A.¹^,2, Sergienko V.I.³, Semiletov I.P.⁴^,2, Sukhoverkhov S.V.³, Bratskaya S.Y.³, Prokuda N.A.³, Ulyantsev A.S.¹
隶属关系:
1. Shirshov Institute of Oceanology
2. Tomsk National Research Polytechnic University
3. Institute of Chemistry, Far East Branch
4. Il’ichev Pacific Institute of Oceanology, Far East Branch
期: 卷 472, 编号 1 (2017)
页面: 36-39
栏目: Geochemistry
URL: https://journal-vniispk.ru/1028-334X/article/view/189374
DOI: https://doi.org/10.1134/S1028334X17010093
ID: 189374

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The distribution and genesis of n-alkanes in sediments from the 38-m sequence obtained during core boring in the Ivashkina lagoon were studied. Sediments were formed in the Holocene as a result of thermokarst and penetration of seawater. The sequence mostly includes permafrost rocks partially molten in the upper horizons and covered by Quaternary deposits, which are mostly the products of thermoabrasion.