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  4. Millennial-scale variability in vegetation records from the East Asian Islands: Taiwan, Japan and Sakhalin
 
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Millennial-scale variability in vegetation records from the East Asian Islands: Taiwan, Japan and Sakhalin

Resource
Quaternary Science Reviews, 29(21-22), 2900-2917
Journal
Quaternary Science Reviews
Pages
2900-2917
Date Issued
2010
Date
2010
Author(s)
Takahara, Hikaru
Igarashi, Yaeko
Hayashi, Ryoma
Kumon, Fujio
Liew, Ping-Mei
Yamamoto, Masanobu
Kawai, Sayuri
Oba, Tadamichi
Irino, Tomohisa
DOI
10.1016/j.quascirev.2009.11.026
URI
http://ntur.lib.ntu.edu.tw//handle/246246/240572
Abstract
High-resolution pollen records from Taiwan, Japan and Sakhalin document regional vegetation changes during Dansgaard-Oeschger (D-O) cycles during the last glacial. During the period from the cold phase (GS 18/19) to warm phase (D-O 19), the biome shift from temperate conifer forest to cold/cool conifer forest in Japan and from subtropical forest to temperate deciduous/conifer forest in Taiwan. The vegetation in D-O 17, cool mixed forest in central Japan, temperate deciduous broadleaf forest in western Japan and subtropical forest in Taiwan, indicates warm condition but not wet in all area. These vegetation changes lead to biome shift from MIS (Marine Isotope Stage) 4 to MIS 3. The abundance of Cryptomeria japonica and Fagus crenata in D-O 12 and D-O 8 indicates wet conditions brought by the strong summer monsoon through the Islands and high snowfall brought by the inflow of the Tsushima Warm Current into the Sea of Japan. The registration of other D-O warming events in MIS 3, although reflected by shifts in the abundance of key species, is not sufficient to produce changes in biomes. Development of cold deciduous forest in HS (Heinrich events) 1 in Sakhalin, Hokkaido and central Japan was conspicuous and was much larger than that in YD. Vegetation response in YD was small scale and within the same biome in the East Asian Islands. In D-O 1 at the termination of the last glacial, the same taxa that developed in the early Holocene, cold evergreen needleleaf trees in northern region, temperate deciduous broadleaf trees in central and western Japan, and warm-temperate evergreen trees in Taiwan, increased. © 2009 Elsevier Ltd.
SDGs

[SDGs]SDG13

Other Subjects
Broadleaf forest; Broadleaf trees; Conifer forests; Cryptomeria japonica; Deciduous forest; Evergreen trees; Fagus crenata; Heinrich Events; High resolution; Hokkaido; Holocenes; Last glacial; Marine isotope stages; Mixed forests; Northern regions; Sea of Japan; Small scale; Subtropical forests; Summer monsoon; Vegetation change; Vegetation response; Warm conditions; Western Japan; Wet conditions; Glacial geology; Isotopes; Security of data; Vegetation; Forestry; biome; broad-leaved forest; climate variation; coniferous forest; Dansgaard-Oeschger cycle; deciduous forest; evergreen forest; historical record; inflow; Last Glacial; marine isotope stage; paleoclimate; palynology; pollen; vegetation dynamics; vegetation history; Data Processing; Forestry; Isotopes; Phases; Plants; Snow; Japan; Pacific Ocean; Russian Federation; Sakhalin; Sea of Japan; Taiwan; Coniferophyta; Cryptomeria japonica; Fagus; Fagus crenata
Type
journal article
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