Transformation of organic matter in the Holocene sediments of Lake Ochki (south Baikal region): Evidence from pyrolysis data View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

2015-10

AUTHORS

V. N. Melenevskii, G. A. Leonova, V. A. Bobrov, V. A. Kashirtsev, S. K. Krivonogov

ABSTRACT

Transformation of organic matter (OM) in Holocene sediments of Lake Ochki (southern coast of Lake Baikal) at the early stages of diagenesis has been studied using pyrolytic methods of Rock Eval (RE-pyrolysis) and pyrolysis-gas chromatography-mass spectrometry (Pyr-GC-MS). OM has been analyzed in lacustrine sediments and their main producers, phytoplankton and zooplankton. Data on the distribution of hydrocarbon–biomarkers in sediments indicate an uninterrupted influx of terrigenous OM and transformation of OM precipitated by microorganisms. The analysis of molecular composition of pyrolysates makes it possible to assume a sharp change of sedimentation conditions in the upper part of sedimentary sequence (0–60 cm). It is shown that the macromolecular aliphatic kerogen structure begins to form in incoherent sediment at the very early stages of diagenesis. More... »

PAGES

903-921

References to SciGraph publications

Identifiers

URI

http://scigraph.springernature.com/pub.10.1134/s0016702915080054

DOI

http://dx.doi.org/10.1134/s0016702915080054

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1045375158


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