georefid:2012-050561SEDIS Publication Catalogue

ana.macario@awi.de

http://sedis.iodp.org/pub-catalogue/informationpointOfContact2013-07-08T00:00:00Zhttp://sedis.iodp.org/pub-catalogue/index.php?id=10.1016/j.quascirev.2009.11.0262010-01-01publicationgeorefid:2012-050561doi:10.1016/j.quascirev.2009.11.026Takahara, HikaruKyoto Prefectural University, Graduate School of Life and Environmental Sciences, Kyoto, JapanauthorIgarashi, YaekoUniversity of Bristol, United KingdomauthorHayashi, RyomaInstitute for Paleoenvironment of Northern Regions, JapanauthorKumon, FujioShinshu University, JapanauthorLiew, Ping-MeiNational Taiwan University, TaiwanauthorYamamoto, MasanobuHokkaido University, JapanauthorKawai, SayuriauthorOba, TadamichiauthorIrino, TomohisaauthorElsevier, InternationalpublisherdocumentHardcopyIn: Goni, Maria Fernanda Sanchez (editor), Harrison, Sandy P. (editor), Vegetation response to millennial-scale variability during the last glacial29 (21-22)2900-2917High-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. Abstract Copyright (2010) Elsevier, B.V.completedQuaternary geologyGeochronologyabsolute ageAsiaassemblagesC-14carbonCenozoicclimate forcingCommonwealth of Independent StatesDansgaard-Oeschger cyclesFar EastglaciationisotopesJapanLeg 184microfossilsmillennial variationsmiosporesNorth PacificNorthwest PacificOcean Drilling ProgramODP Site 1144orbital forcingPacific OceanpaleoclimatologypaleoenvironmentpalynomorphsPleistocenepollenquantitative analysisQuaternaryradioactive isotopesRussian FederationSakhalinSakhalin Russian FederationSouth China SeaTaiwanterrestrial environmentupper PleistocenevegetationWest Pacificurn:org.iodp:exp:184urnlargerWorkCitationcampaignurn:org.iodp:exp:184:site:1144urnlargerWorkCitationstudyurn:org.iodp:exp:184urnlargerWorkCitationcampaignEnglishgeoscientificInformation117.2508117.250820.031120.0311