Research output: Contribution to journal › Article › peer-review
Environmental changes recorded in deposits of the Izyubrinye Salontsi Lake, Sikhote-Alin. / Razzhigaeva, N. G.; Ganzey, L. A.; Grebennikova, T. A.; Kopoteva, T. A.; Mokhova, L. M.; Panichev, A. M.; Kudryavtseva, E. P.; Arslanov, Kh A.; Maksimov, F. E.; Petrov, A. Yu; Klimin, M. A.
In: Contemporary Problems of Ecology, Vol. 10, No. 4, 01.07.2017, p. 441-453.Research output: Contribution to journal › Article › peer-review
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TY - JOUR
T1 - Environmental changes recorded in deposits of the Izyubrinye Salontsi Lake, Sikhote-Alin
AU - Razzhigaeva, N. G.
AU - Ganzey, L. A.
AU - Grebennikova, T. A.
AU - Kopoteva, T. A.
AU - Mokhova, L. M.
AU - Panichev, A. M.
AU - Kudryavtseva, E. P.
AU - Arslanov, Kh A.
AU - Maksimov, F. E.
AU - Petrov, A. Yu
AU - Klimin, M. A.
PY - 2017/7/1
Y1 - 2017/7/1
N2 - Paleoecological changes during the development of Lake Izyubrinye Solontsi from the Solontsovskie (Shanduyskie) Lakes located in the midlands of the Eastern Sikhote-Alin have been reconstructed. Lake formation is related to landslides on the paleovolcano slopes. A complex study of the peat-bog section (botanical, diatom, spore-pollen, and radiocarbon analysis) allows reconstructing paleoenvironmental changes with high resolution. A considerable variability of lake and swamp environments highly responsive to climate changes in the late Holocene has been revealed. Peat accumulation began about 400014С BP. The main peat-forming plants were Sphagnum mosses and herbs, except for the period 2330‒1530 14C BP (2360‒1480 cal. BP), when a swamp overgrown by larch forests and predominantly woody peat accumulated. Forest ecosystems on the lake coasts were quite stable. The role of fir and broadleaved species increased in the composition of dark coniferous forests with Korean pine during the warm phases and the role of birch, in the cold phases; secondary forests occupied the low slopes during the last 1000 years. The age of paleofires has been determined.
AB - Paleoecological changes during the development of Lake Izyubrinye Solontsi from the Solontsovskie (Shanduyskie) Lakes located in the midlands of the Eastern Sikhote-Alin have been reconstructed. Lake formation is related to landslides on the paleovolcano slopes. A complex study of the peat-bog section (botanical, diatom, spore-pollen, and radiocarbon analysis) allows reconstructing paleoenvironmental changes with high resolution. A considerable variability of lake and swamp environments highly responsive to climate changes in the late Holocene has been revealed. Peat accumulation began about 400014С BP. The main peat-forming plants were Sphagnum mosses and herbs, except for the period 2330‒1530 14C BP (2360‒1480 cal. BP), when a swamp overgrown by larch forests and predominantly woody peat accumulated. Forest ecosystems on the lake coasts were quite stable. The role of fir and broadleaved species increased in the composition of dark coniferous forests with Korean pine during the warm phases and the role of birch, in the cold phases; secondary forests occupied the low slopes during the last 1000 years. The age of paleofires has been determined.
KW - climatic changes
KW - fires
KW - lacustrine–swamp environments
KW - Late Holocene
KW - paleolandscapes
KW - Sikhote-Alin
UR - http://www.scopus.com/inward/record.url?scp=85028040779&partnerID=8YFLogxK
U2 - 10.1134/S1995425517040096
DO - 10.1134/S1995425517040096
M3 - Article
AN - SCOPUS:85028040779
VL - 10
SP - 441
EP - 453
JO - Contemporary Problems of Ecology
JF - Contemporary Problems of Ecology
SN - 1995-4255
IS - 4
ER -
ID: 35955298