The Tibetan Plateau,the world's "Third Pole",has an average elevation above 4,000 masl (meters above sea level)and an area of over 500×10^4km^2,It is the highest and largest plateau on earth and is ...The Tibetan Plateau,the world's "Third Pole",has an average elevation above 4,000 masl (meters above sea level)and an area of over 500×10^4km^2,It is the highest and largest plateau on earth and is very sensitive to global climate change [1,2].The cold,dry and hypoxic high-altitude environment of the plateau presents a major challenge to human survival.Therefore,the history and mechanisms of prehistoric human history on the Tibetan Plateau-from brief hunting expeditions to seasonal hunting-gathering and finally to permanent settlements-has attracted both general interest and substantial scientific debates [3-6].Archaeological studies indicate that humans probably first explored the plateau at the end of the late Pleistocene.They practiced intensive seasonal hunting-gathering from 15 ka BP [6],and permanently settled regions above 3,000 masl after 3.6 ka BP,which was facilitated by the development of an agropastoral economy [3].However, the early part of the human history of the Tibetan Plateau is still poorly documented,due to the lack of well-preserved archaeological sites and reliable dating results (Fig.la).展开更多
Changes in the East Asian summer monsoon (EASM)are closely related to human wellbeing,and thus improving our knowledge of the evolution of the EASM is of major socioeconomic importance, as well as being of scientific ...Changes in the East Asian summer monsoon (EASM)are closely related to human wellbeing,and thus improving our knowledge of the evolution of the EASM is of major socioeconomic importance, as well as being of scientific interest.Previous studies have shown that during the Holocene (the present interglacial)a "North-South" dipolar mode of precipitation change occurred over eastern China (i.e.the so-called "northern drought-southern flood"scenario, or vice versa)on decadal [1,2],centennial [3]and millennial timescales ([4]and references therein).A recent high-resolution speleothem trace element-based precipitation record from Haozhu Cave in the Yangtze River Valley (YRV)[5],together with a pollenbased quantitative precipitation reconstruction from Lake Gonghai in North China [6],further suggests that this dipolar mode extended to the Last Deglaciation [5].This inference is based on the recorded anti-phased variation of precipitation between North China and the YRV during the Younger Dryas (YD),Bolling-Allerod (B-A),and part of Heinrich Event 1(H1)(Fig.1a,b).展开更多
基金supported by the National Natural Science Foundation of China (41771225 and 41620104007)the Fundamental Research Funds for the Central Universities (lzujbky-2018-146)
文摘The Tibetan Plateau,the world's "Third Pole",has an average elevation above 4,000 masl (meters above sea level)and an area of over 500×10^4km^2,It is the highest and largest plateau on earth and is very sensitive to global climate change [1,2].The cold,dry and hypoxic high-altitude environment of the plateau presents a major challenge to human survival.Therefore,the history and mechanisms of prehistoric human history on the Tibetan Plateau-from brief hunting expeditions to seasonal hunting-gathering and finally to permanent settlements-has attracted both general interest and substantial scientific debates [3-6].Archaeological studies indicate that humans probably first explored the plateau at the end of the late Pleistocene.They practiced intensive seasonal hunting-gathering from 15 ka BP [6],and permanently settled regions above 3,000 masl after 3.6 ka BP,which was facilitated by the development of an agropastoral economy [3].However, the early part of the human history of the Tibetan Plateau is still poorly documented,due to the lack of well-preserved archaeological sites and reliable dating results (Fig.la).
基金supported by the National Natural Science Foundation of China(41790421 and 41722105)
文摘Changes in the East Asian summer monsoon (EASM)are closely related to human wellbeing,and thus improving our knowledge of the evolution of the EASM is of major socioeconomic importance, as well as being of scientific interest.Previous studies have shown that during the Holocene (the present interglacial)a "North-South" dipolar mode of precipitation change occurred over eastern China (i.e.the so-called "northern drought-southern flood"scenario, or vice versa)on decadal [1,2],centennial [3]and millennial timescales ([4]and references therein).A recent high-resolution speleothem trace element-based precipitation record from Haozhu Cave in the Yangtze River Valley (YRV)[5],together with a pollenbased quantitative precipitation reconstruction from Lake Gonghai in North China [6],further suggests that this dipolar mode extended to the Last Deglaciation [5].This inference is based on the recorded anti-phased variation of precipitation between North China and the YRV during the Younger Dryas (YD),Bolling-Allerod (B-A),and part of Heinrich Event 1(H1)(Fig.1a,b).
