通过对鄂尔多斯高原中部的巴汗淖湖泊沉积物的环境代用指标综合分析，以AMS^14C测年为基础，重建了鄂尔多斯高原全新世的气候变化历史．分析结果显示：鄂尔多斯高原约7．65 ^14C kaBP前气候寒冷干燥；7．65—5．40^14C ka BP气候温暖湿润，其中7．65—6．70^14C ka BP气候相对暖湿，以湿度条件改善更明显，随后6．70—6．20^14C ka BP气候偏暖干，6．20—5．40^14C ka BP研究区温湿组合状况最佳；5．40^14C ka BP后鄂尔多斯高原总体向干凉方向发展，但在4．70-4．60^14C ka BP和4．20～3．70^14C ka BP出现两个明显的相对湿润时期；约3．70^14C ka BP后巴汗淖湖泊完全干涸．
A 5.3 m lake core was drilled in Baahar Nuur Lake in the Ordos Plateau, and measurements of meangrain size, organic δ 13C (δ 13Corg), organic carbon content (TOC), C/N, carbonate content, carbonate δ 13C(δ 13Ccar) and δ 18O (δ 18Ocar) were conducted for retrieving the Holocene chronosequence of climaticchanges based on 15 AMS 14C dates. The record documented four major stages of climate change inthe Ordos Plateau: (IV) a cold and dry condition before ～7.65 14C ka BP; (III) a warm and humid stagebetween ～7.65 and ～5.40 ka BP; (II) a generally drier and cooler climate since ～5.40 ka BP with twohumid events occurring from ～4.70 to ～4.60 ka BP and from ～4.20 to ～3.70 ka BP, and (I) a dry climatecharacterized by complete desiccation of the lake after 3.70 ka BP. Stage III can be further divided intothree sub-stages: (IIIa) a warm and humid episode from ～7.65 to ～6.70 ka BP, (IIIb) a warm and relativelydry episode from ～6.70 to ～6.20 ka BP, and (IIIc) the magthermal and maghumid episode of the Holo-cene from ～6.20 to ～5.40 ka BP.
