Petroleum-related hydrocarbons in deep and subsurface sediments from South-Western Barents Sea

International audience Subsurface sediments from a pockmark area in South-Western Barents Sea have been earlier found to contain elevated levels of petroleum-related polycyclic aromatic hydrocarbons. This work describes a comprehensive analysis of various biomarkers, including the highly source-spec...

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Bibliographic Details
Published in:Marine Environmental Research
Main Authors: Boitsov, Stepan, Petrova, Vera, Jensen, Henning K.B., Kursheva, Anna, Litvinenko, Ivan, Chen, Yifeng, Klungsøyr, Jarle
Other Authors: Institute of Marine Research Bergen (IMR), University of Bergen (UiB), Academician I.S. Gramberg All-Russia Research Institute for Geology and Mineral Resources of the World Ocean (VNIIO)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2011
Subjects:
Biomarkers
hopanes
sediments
pockmarks
PAH
alkanes
Barents Sea
[SDV]Life Sciences [q-bio]
Online Access:https://hal.archives-ouvertes.fr/hal-00703485
https://hal.archives-ouvertes.fr/hal-00703485/document
https://hal.archives-ouvertes.fr/hal-00703485/file/PEER_stage2_10.1016%252Fj.marenvres.2011.04.003.pdf
https://doi.org/10.1016/j.marenvres.2011.04.003
Description
Summary:International audience Subsurface sediments from a pockmark area in South-Western Barents Sea have been earlier found to contain elevated levels of petroleum-related polycyclic aromatic hydrocarbons. This work describes a comprehensive analysis of various biomarkers, including the highly source-specific hopanes, in a 4.5 m long gravity core from the same area, together with subsurface sediment samples from other areas in the region without pockmarks present ("background samples"). A clear difference between the pockmark gravity core and the background sediment cores was found, both with regard to genesis and the level of transformation of organic matter. A number of indicator parameters, such as methylphenanthrene index (MPI-1), point towards a significantly higher maturity of hydrocarbons in the pockmark core throughout its length as compared to the other sampled locations. Higher contents of microbial hopanoids (hopenes) may indicate the former presence of petroleum. These findings confirm the hypothesis of a natural hydrocarbon source in the deeper strata present in the studied location with pockmarks.

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