TY - JOUR

T1 - Multiproxy record of late Holocene climatic changes and natural hazards from paleolake deposits of Urup Island (Kuril Islands, North-Western Pacific)

AU - Razjigaeva, Nadezhda G.

AU - Ganzey, Larisa A.

AU - Grebennikova, Tatiana A.

AU - Belyanina, Nina I.

AU - Ganzei, Kirill S.

AU - Kaistrenko, Victor M.

AU - Arslanov, Khikmatulla A.

AU - Maksimov, Fedor E.

AU - Rybin, Alexsander V.

N1 - Publisher Copyright: © 2019

PY - 2019/9/1

Y1 - 2019/9/1

N2 - The evolution of the late Holocene environments has been reconstructed on the basis of multiproxy studies of peat sequences. The vegetation response to short-period climate fluctuations has been traced. Early in the late Holocene there were birch forests with oak and other broadleaf trees; vast areas were occupied by forb meadows. Under cooling (3250 yr BP) the shrub pine (Pinus pumila) became the landscape-forming species, and since 2490 yr BP Selaginella selaginoides appeared in abundance. The Little Ice Age was marked by the disappearance of broadleaf trees and widely spread heath land communities. The higher stands of the lake level were related to warmings (3660–3590; 3450–3180; 2960–2840; 2410–2260 cal yr BP). Shallowing coincided with short-term coolings (3590–3450; 3180–2960; 2840–2410; 2260–2150 cal yr BP) marked by reduced precipitations. The dune ridge formation began during the longest cooling accompanied by a minor regression. The dunes were stabilized and a paleosol developed ~2340–2260 yr BP. A younger generation of eolian sands developed during the Little Ice Age. An ecological effect of volcanic ashfalls has been estimated. The local biotic components seem to have been most afflicted by the eruption in the north of Iturup in ~2100–2300 cal yr BP, when CKr tephra up to 30 cm thick was deposited. The ages of 4 strongest tsunamis that occurred over the last 3660 years were determined. They appeared to be related to the earthquakes with focuses close to Urup Island or south of it. The lake microflora shows ecological effect of the marine water invasions.

AB - The evolution of the late Holocene environments has been reconstructed on the basis of multiproxy studies of peat sequences. The vegetation response to short-period climate fluctuations has been traced. Early in the late Holocene there were birch forests with oak and other broadleaf trees; vast areas were occupied by forb meadows. Under cooling (3250 yr BP) the shrub pine (Pinus pumila) became the landscape-forming species, and since 2490 yr BP Selaginella selaginoides appeared in abundance. The Little Ice Age was marked by the disappearance of broadleaf trees and widely spread heath land communities. The higher stands of the lake level were related to warmings (3660–3590; 3450–3180; 2960–2840; 2410–2260 cal yr BP). Shallowing coincided with short-term coolings (3590–3450; 3180–2960; 2840–2410; 2260–2150 cal yr BP) marked by reduced precipitations. The dune ridge formation began during the longest cooling accompanied by a minor regression. The dunes were stabilized and a paleosol developed ~2340–2260 yr BP. A younger generation of eolian sands developed during the Little Ice Age. An ecological effect of volcanic ashfalls has been estimated. The local biotic components seem to have been most afflicted by the eruption in the north of Iturup in ~2100–2300 cal yr BP, when CKr tephra up to 30 cm thick was deposited. The ages of 4 strongest tsunamis that occurred over the last 3660 years were determined. They appeared to be related to the earthquakes with focuses close to Urup Island or south of it. The lake microflora shows ecological effect of the marine water invasions.

KW - Chronology

KW - Climate changes

KW - Environments

KW - Late Holocene

KW - Natural hazards

KW - Paleo-lake

KW - The Kuril Islands

KW - Vegetation response

UR - http://www.scopus.com/inward/record.url?scp=85068463260&partnerID=8YFLogxK

U2 - 10.1016/j.jseaes.2019.103916

DO - 10.1016/j.jseaes.2019.103916

M3 - Article

AN - SCOPUS:85068463260

VL - 181

JO - Journal of Asian Earth Sciences

JF - Journal of Asian Earth Sciences

SN - 1367-9120

M1 - 103916

ER -