Сибирский федеральный университет

Тип публикации: статья из журнала

Год издания: 2012

Идентификатор DOI: 10.1134/S199542551204018X

Ключевые слова: okenone, meromixis, holomixis, anaerobiosis, bottom sediments, bacterium, bioindicator, biomarker, carotenoid, Holocene, lacustrine deposit, molecular analysis, paleoclimate, photoautotrophy, reconstruction, Khakassia, Lake Shira, Russian Federation

Аннотация: The concentrations of carotenoids buried in the bottom sediments of Lake Shira (Siberia, Khakassiya) have analyzed for the period of the last 2300 years. The bottom sediments were found to contain carotenoids, which are molecular markers of the corresponding groups of Phototrophic organisms. The bottom sediments of Lake Shira were shown to be a promising object for climate reconstructions of the Late Holocene in southern Siberia.

Журнал: CONTEMPORARY PROBLEMS OF ECOLOGY

Выпуск журнала: Vol. 5, Is. 4

Номера страниц: 434-442

ISSN журнала: 19954255

Место издания: NEW YORK

Издатель: SPRINGER

• Zykov V.V. (Institute of Biophysics, Siberian Branch,Russian Academy of Sciences)
• Rogozin D.Y. (Siberian Federal University)
• Degermendzhi A.G. (Institute of Biophysics, Siberian Branch,Russian Academy of Sciences)
• Kalugin I.A. (Sobolev Institute of Geology and Mineralogy, Siberian Branch,Russian Academy of Sciences)
• Dar'in A.V. (Sobolev Institute of Geology and Mineralogy, Siberian Branch,Russian Academy of Sciences)

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