KFU. Card publication. Sediments of Lake Malye Chany as a Late Holocene paleoecological archive in the south of West Siberia (Russia)

KAZAN
FEDERAL UNIVERSITY

- RUS
- 中文
- ES

SEDIMENTS OF LAKE MALYE CHANY AS A LATE HOLOCENE PALEOECOLOGICAL ARCHIVE IN THE SOUTH OF WEST SIBERIA (RUSSIA)

Form of presentation

Articles in Russian journals and collections

Year of publication

2022

��

��

Authors, employees of KFU

Nazarova Larisa Borisovna, author

Palagushkina Olga Viktorovna, author

Bibliographic description in the original language

Zhilich S. Krivonogov S., Nazarova L., Palagushkina O., Cao X., Rudaya N.Sediments of Lake Malye Chany as a Late Holocene paleoecological archive in the south of West Siberia (Russia),Limnology and Freshwater Biology 2022 (4): 1628-1629 DOI:10.31951/2658-3518-2022-A-4-1628

Annotation

LIMNOLOGY AND FRESHWATER BIOLOGY

Keywords

Lake Malye Chany, south of West Siberia, multiproxy study, reconstructions

The name of the journal

LIMNOLOGY AND FRESHWATER BIOLOGY

Please use this ID to quote from or refer to the card

https://repository.kpfu.ru/eng/?p_id=270079&p_lang=2

Full metadata record

Field DC	Value	Language
dc.contributor.author	Nazarova Larisa Borisovna	ru_RU
dc.contributor.author	Palagushkina Olga Viktorovna	ru_RU
dc.date.accessioned	2022-01-01T00:00:00Z	ru_RU
dc.date.available	2022-01-01T00:00:00Z	ru_RU
dc.date.issued	2022	ru_RU
dc.identifier.citation	Zhilich S. Krivonogov S., Nazarova L., Palagushkina O., Cao X., Rudaya N.Sediments of Lake Malye Chany as a Late Holocene paleoecological archive in the south of West Siberia (Russia),Limnology and Freshwater Biology 2022 (4): 1628-1629 DOI:10.31951/2658-3518-2022-A-4-1628	ru_RU
dc.identifier.uri	https://repository.kpfu.ru/eng/?p_id=270079&p_lang=2	ru_RU
dc.description.abstract	LIMNOLOGY AND FRESHWATER BIOLOGY	ru_RU
dc.description.abstract	The paper presents the first results of multiproxy study of the sediment core from Lake Malye Chany. This lake is a part of the biggest drainless lake in Russian Lake Chany. The Kargat and Chulym Rivers flow into Malye Chany. The lake locates in the forest-steppe near the southern border of taiga zone which makes it a promising object for reconstructions of the vegetation shifts and other ecological changes of the past periods. The sediment core was investigated by sedimentological, pollen, chironomid, diatom, ostracod analyses. Based on pollen and chironomid data were maid quantitative reconstructins of climate, vegetation cover and biodiversity. According to radiocarbon dates the upper 200 cm of the core covers the last ca. 3900 years. It was established that reconstructed time boundaries of climate, vegetation and ecological changes coincide according to various reconstruction approaches. At the beginning of its existence, Lake Malye Chany was a shallow saline lake with warm water; only after 2.4 thousand years BP the water level rose and the lake became fresh and the water colder. Then the water level and salinity changed, and only 1 thousand years BP the lake became deep again. The last 200 years recorded a slight warming of the water. Landscapes developed from very dry steppe to modern forest-steppe, about 2 thousand years ago there was a short-term cooling and spread of taiga elements. Last 200-300 years, there has been a steppification.	ru_RU
dc.language.iso	ru	ru_RU
dc.subject	Lake Malye Chany	ru_RU
dc.subject	south of West Siberia	ru_RU
dc.subject	multiproxy study	ru_RU
dc.subject	reconstructions	ru_RU
dc.title	Sediments of Lake Malye Chany as a Late Holocene paleoecological archive in the south of West Siberia (Russia)	ru_RU
dc.type	Articles in Russian journals and collections	ru_RU