干旱区研究2024，Vol.41Issue(8)：1309-1322,14.DOI:10.13866/j.azr.2024.08.05
中中新世气候适宜期全球变暖背景下亚洲内陆干旱区古气候演化特征及驱动机制
Paleoclimatic evolution and driving mechanisms in arid areas of inland Asia during the Middle Miocene Climatic Optimum in the context of global climate warming
摘要
Abstract
The Mid-Miocene Climatic Optimum,a notable global warming event that occurred during cooling in the Cenozoic period,is being considered as a potential analog for future climate conditions.Arid areas of inland Asia are representative of mid-latitude arid zones throughout the globe,and their desertification exerts the stron-gest and most direct impacts on human habitation environments.Against the backdrop of global warming,which is compounded by human activities,these arid zones become increasingly fragile,with their expansion or altera-tion directly impacting human survival and sustainable development.The exploration of the climatic evolutionary history of the arid areas of inland Asia during the Middle Miocene under a global warming scenario can provide crucial insights for the projection of climate changes in arid regions under future warming patterns.This study re-viewed the existing research on the paleoclimatic evolution during the Middle Miocene in typical basins of arid areas of inland Asia.Through a comprehensive analysis of various climatic proxies,including environmental mag-netic parameters,pollen,and isotopes,the findings indicate the prevailing trend is toward increased humidity in most regions during this period,although there were variations in the timing of humidification and some areas re-mained arid.However,significant controversy remains regarding the primary regulator of the formation of the Mid-Miocene Climatic Optimum:some scholars argue that eruptions of Columbia basalt are the primary factor;others propose that tectonic activity is the main driver.To address the aforementioned controversies,obtaining higher-resolution records with precise age control is essential to determine the onset response time of the Mid-Miocene warming event.Through the accurate interpretation of climatic proxies,especially pollen,which directly and sensitively responds to paleoclimatic changes,as well as environmental magnetic parameters and geochemi-cal ratios encapsulating paleoenvironmental information,the various factors influencing climate change can be clarified to reveal the driving mechanisms behind the climatic evolution during the Mid-Miocene Climatic Opti-mum in arid areas of inland Asia.关键词
中中新世气候适宜期/全球气候变化/气候代用指标/驱动机制/环境磁学/亚洲内陆干旱区Key words
the Mid-Miocene Climatic Optimum/global climate change/climate proxy indicators/driving mechanisms/study of environmental magnetism/arid areas of inland Asia引用本文复制引用
吕壮壮,乔庆庆,董孙艺,汪冬..中中新世气候适宜期全球变暖背景下亚洲内陆干旱区古气候演化特征及驱动机制[J].干旱区研究,2024,41(8):1309-1322,14.基金项目
国家自然科学基金优秀青年科学基金项目(42122028) （42122028）
国家自然科学基金面上项目(41774077) （41774077）
中国科学院西部之光人才培养引进计划西部青年学者(2022-XBQNXZ-005) （2022-XBQNXZ-005）
