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100 _aYang, Yunpeng
_952197
245 _aPollen-based reconstructions of vegetation and climate changes during the late Holocene in the southern Altai Mountains/
260 _bSage,
_c2019.
300 _aVol 29, issue 9, 2019 : (1450-1458 p.).
520 _aWe here preset a result of high-resolution pollen data of a lacustrine-peat sediment core from Yushenkule (YSKL) Peat, southern Altai Mountains, northwestern China. We aim to reconstruct the palaeovegetation and palaeoclimate variations in the southern Altai Mountains and further evaluate the role of autogenic process of the raised bog itself in driving the local vegetation dynamics. The pollen data of YSKL core-2 show two major vegetation stages in YSKL Peat area and the surrounding areas during the data-covering period. During the stage lasting from ~4870 to ~2550 cal. yr BP, regional vegetation was dominated by desert steppe and local vegetation in YSKL Peat was characterized by Artemisia-dominated mountain steppe. During the stage lasting from ~2550 to ~700 cal. yr BP, regional vegetation was characterized by Artemisia-dominated steppe and local vegetation in YSKL Peat was characterized by Cyperaceae-dominated wetland herbs. The Ar/Am (Artemisia/Amaranthaceae) ratio-indicated moisture increasing trend of southern Altai Mountains can attribute to the combined effects of decreased temperature and increased precipitation. The lithologic transition from lake to peat of YSKL core-2 can be explained by invoking the variations in the areal extent of ice covers in the Altai Mountains
650 _aAltai Mountains,
_952198
650 _a climate change,
_949417
650 _alate Holocene,
_951310
650 _amoisture change,
_952199
650 _apollen analysis
_951054
700 _aZhang, Dongliang
_952200
700 _aSun, Aizhi
_952201
700 _aWang, Wei
_952202
700 _aLan, Bo
_952203
700 _a Feng, Zhaodong
_952204
773 0 _012756
_916504
_dLondon: Sage Publication Ltd, 2019.
_tHolocene/
_x09596836
856 _uhttps://doi.org/10.1177/0959683619854515
942 _2ddc
_cART
999 _c12858
_d12858