该文综述了北京地区全新世以来植被演替和气候变化的相关研究资料,这些资料反映了当前阶段对该地区该时段植被与气候环境格局特征的认识。北京地区全新世早期(约12 000–8 000 cal a B.P.)植被为森林草地和/或针叶树占主导的针阔混交林...该文综述了北京地区全新世以来植被演替和气候变化的相关研究资料,这些资料反映了当前阶段对该地区该时段植被与气候环境格局特征的认识。北京地区全新世早期(约12 000–8 000 cal a B.P.)植被为森林草地和/或针叶树占主导的针阔混交林,森林中阔叶树类群逐渐增多,指示了气候由寒冷干燥转为温暖湿润;全新世中期(约8 000–2 000 cal a B.P.前后)植被为暖温带针阔混交林,指示暖湿气候;全新世晚期(约2 000 cal a B.P.以来)转为森林草地和/或针叶树占主导的针阔混交林,气候转向凉干。植被演替反映的湿润度变化与季风区其它地区变化趋势一致。值得注意的是,前人研究揭示北京地区山区与平原中植被类型和类群组成已经出现空间分异。今后如能深入开展定量古气候重建研究,有可能精确描述其气候变化的过程,增进中国不同地理单元同时期气候变化的对比。展开更多
The uplift of different parts of the Tibetan Plateau caused by the collision,subduction and thickening of the Indian-Eurasian continent is considered to be the most significant landform change of Asia in the last 50 M...The uplift of different parts of the Tibetan Plateau caused by the collision,subduction and thickening of the Indian-Eurasian continent is considered to be the most significant landform change of Asia in the last 50 Ma.The plateau uplift led to elevation and topographical changes in neighboring areas and created diversified niches for the distribution and migration of plants and animals.The resultant high mountains controlled the South Asian monsoon,preventing the monsoon from crossing the plateau and reaching the hinterland of Asia.展开更多
文摘该文综述了北京地区全新世以来植被演替和气候变化的相关研究资料,这些资料反映了当前阶段对该地区该时段植被与气候环境格局特征的认识。北京地区全新世早期(约12 000–8 000 cal a B.P.)植被为森林草地和/或针叶树占主导的针阔混交林,森林中阔叶树类群逐渐增多,指示了气候由寒冷干燥转为温暖湿润;全新世中期(约8 000–2 000 cal a B.P.前后)植被为暖温带针阔混交林,指示暖湿气候;全新世晚期(约2 000 cal a B.P.以来)转为森林草地和/或针叶树占主导的针阔混交林,气候转向凉干。植被演替反映的湿润度变化与季风区其它地区变化趋势一致。值得注意的是,前人研究揭示北京地区山区与平原中植被类型和类群组成已经出现空间分异。今后如能深入开展定量古气候重建研究,有可能精确描述其气候变化的过程,增进中国不同地理单元同时期气候变化的对比。
基金supported by the Strategic Priority Research Program of the Chinese Academy of Sciences(XDB26000000)the China National Key Basic Research Program(2014CB954201)+2 种基金the National Natural Science Foundation of China(31570223,32000174)the State Key Laboratory of Systematic and Evolutionary Botany(LSEB2019-1,LSEB2019-4)the Chinese Academy of Sciences President’s International Fellowship Initiative(2018VBA0016)。
文摘The uplift of different parts of the Tibetan Plateau caused by the collision,subduction and thickening of the Indian-Eurasian continent is considered to be the most significant landform change of Asia in the last 50 Ma.The plateau uplift led to elevation and topographical changes in neighboring areas and created diversified niches for the distribution and migration of plants and animals.The resultant high mountains controlled the South Asian monsoon,preventing the monsoon from crossing the plateau and reaching the hinterland of Asia.
