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摘要:
One of the Holocene abrupt events around 4200 years ago,lasting for ~ 200 years,is thought to have caused cultural disruptions,yet terrestrial climatic status right after the cold/dry event remains poorly defined and is often presumed that a generally cool condition prevailed during the Bronze Age (~4000-2200 years ago).Here we report an alkenone-based summer temperature record over the past ~ 12,000 years,in addition to two updated alkenone records,from Northwest China,providing new insights into the climatic status right after the event.Our results indicate that exceptional terrestrial warmth,up to ~ 6 ℃,occurred around 4200-2800 years ago during the Bronze Age,superimposed on the long-term Holocene cooling trend.The exceptional warmth in Northwest China,together with other cli-mate anomalies elsewhere,suggests an unusual large-scale climatic reorganization at 4200-2800 years ago when solar activity remained high,with important implications to the climate background for cul-tural developments during the Bronze Age.
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篇名 Exceptional terrestrial warmth around 4200-2800 years ago in Northwest China
来源期刊 科学通报(英文版) 学科
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年,卷(期) 2022,(4) 所属期刊栏目 ARTICLES
研究方向 页码范围 427-436
页数 10页 分类号
字数 语种 英文
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科学通报(英文版)
半月刊
1001-6538
11-1785/N
大16开
北京东黄城根北街16号
2-177
1950
eng
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9507
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1
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