Research output: Contribution to journal › Article › peer-review
Record of Late Glacial–Holocene Paleogeographical Events in Ogranogenic Deposits of Matua Island (Central Kurils). / Razjigaeva, N. G.; Ganzey, L. A.; Arslanov, Kh A.; Mokhova, L. M.; Degterev, A. V.; Ganzei, K. S.; Pshenichnikova, N. F.; Maksimov, F. E.; Starikova, A. A.; Petrov, A. Yu.
In: Russian Journal of Pacific Geology, Vol. 12, No. 5, 05.10.2018, p. 384-399.Research output: Contribution to journal › Article › peer-review
}
TY - JOUR
T1 - Record of Late Glacial–Holocene Paleogeographical Events in Ogranogenic Deposits of Matua Island (Central Kurils)
AU - Razjigaeva, N. G.
AU - Ganzey, L. A.
AU - Arslanov, Kh A.
AU - Mokhova, L. M.
AU - Degterev, A. V.
AU - Ganzei, K. S.
AU - Pshenichnikova, N. F.
AU - Maksimov, F. E.
AU - Starikova, A. A.
AU - Petrov, A. Yu
PY - 2018/10/5
Y1 - 2018/10/5
N2 - The manifestation of paleoclimatic events since the latest Pleistocene recorded in paleosoils from the soil–pyroclastic covers of Matua Island in the Central Kurils is analyzed for the first time. Throughout this period, the landscape development occurred in conditions of volcanic activity. The studied sections are located under different types of vegetation. Spore and pollen analysis of buried and modern soils is performed. Age binding of the events is carried out on the basis of radiocarbon dating and tephrastratigraphy. Stages of landscape development, including pre- and post-caldera-forming eruptions of the Matua volcano and eruptive activity in the post-caldera period before and after the formation of the Sarychev Peak volcano are established. The interaction of volcanic and climatic factors in the development of the biotic components is determined.
AB - The manifestation of paleoclimatic events since the latest Pleistocene recorded in paleosoils from the soil–pyroclastic covers of Matua Island in the Central Kurils is analyzed for the first time. Throughout this period, the landscape development occurred in conditions of volcanic activity. The studied sections are located under different types of vegetation. Spore and pollen analysis of buried and modern soils is performed. Age binding of the events is carried out on the basis of radiocarbon dating and tephrastratigraphy. Stages of landscape development, including pre- and post-caldera-forming eruptions of the Matua volcano and eruptive activity in the post-caldera period before and after the formation of the Sarychev Peak volcano are established. The interaction of volcanic and climatic factors in the development of the biotic components is determined.
KW - CLIMATE
KW - Central Kurils
KW - Holocene
KW - Late Glacial
KW - Matua Island
KW - climatic changes
KW - paleolandscapes
KW - paleosoils
KW - radiocarbon dating
KW - volcanic eruptions
UR - http://www.scopus.com/inward/record.url?scp=85054534473&partnerID=8YFLogxK
U2 - 10.1134/S181971401805010X
DO - 10.1134/S181971401805010X
M3 - Article
AN - SCOPUS:85054534473
VL - 12
SP - 384
EP - 399
JO - Russian Journal of Pacific Geology
JF - Russian Journal of Pacific Geology
SN - 1819-7140
IS - 5
ER -
ID: 35940175