Pollen-based seasonal temperature reconstruction in Northeast China over the past 10,000 years, and its implications for understanding the Holocene Temperature Conundrum
文献类型:期刊论文
作者 | Geng, Rongwei1,6; Zhao, Yan1,10; Herzschuh, Ulrike7,8,9; Cui, Qiaoyu1; Zheng, Zhuo2; Xiao, Xiayun3; Ma, Chunmei4; Liang, Chen5 |
刊名 | PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
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出版日期 | 2024-10-01 |
卷号 | 651页码:112391 |
关键词 | Holocene Paleoclimatology Pollen Quantitative reconstruction Northeast China |
DOI | 10.1016/j.palaeo.2024.112391 |
产权排序 | 2 |
文献子类 | Article |
英文摘要 | The Holocene Temperature Conundrum refers to the mismatch between proxy-based temperature records and those based on climate model simulations. A possible reason for this mismatch is a putative proxy-based bias in reconstructed summer temperatures, and therefore, regional reconstructions of seasonal temperature are crucial for resolving the conundrum. In this paper, we reconstruct vegetation and climate changes over the last similar to 10,000 years BP based on a high-resolution pollen record from Gushantun peatland, Changbai Mountains, Northeast China. Multiple quantitative reconstruction approaches were used and weighted averaging partial least squares regression (WAPLS) was found to be the most appropriate method for reconstructing Holocene temperature and precipitation. The reconstructed climate record shows that the Holocene Climate Optimum occurred between 8 ka and 6 ka and exhibited a cold month mean temperature that was 3 degrees C warmer than modern temperatures. Climate gradually cooled during late Holocene with a minimum cold month temperature of -19.6 degrees C. Four prominent cold events occurred around 8.7 ka BP, 7.8 ka BP, 5.7 ka BP, and 2.5 ka BP with an amplitude variation up to 3 degrees C. The synthesized seasonal temperature time series and a comparison with other proxies show that the decreasing trend in mean annual temperature is not a seasonal bias caused by summer temperature change. This study provides evidence of a Holocene seasonal temperature change at a regional scale and insights for further understanding of the Holocene Temperature Conundrum. |
WOS关键词 | EAST-ASIAN MONSOON ; QUANTITATIVE RECONSTRUCTION ; ARCTIC OSCILLATION ; GLOBAL TEMPERATURE ; CLIMATE DYNAMICS ; NE CHINA ; VEGETATION ; EVOLUTION ; RECORD ; SEDIMENTS |
WOS研究方向 | Physical Geography ; Geology ; Paleontology |
WOS记录号 | WOS:001286838600001 |
出版者 | ELSEVIER |
源URL | [http://ir.igsnrr.ac.cn/handle/311030/206882] ![]() |
专题 | 陆地表层格局与模拟院重点实验室_外文论文 |
通讯作者 | Zhao, Yan |
作者单位 | 1.Chinese Acad Sci, Key Lab Land Surface Pattern & Simulat, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China 2.Sun Yat Sen Univ, Sch Earth Sci & Engn, Zhuhai 51900, Peoples R China 3.Chinese Acad Sci, Nanjing Inst Geog & Limnol, Nanjing 210008, Peoples R China 4.Nanjing Univ, Sch Geog & Ocean Sci, Nanjing 210023, Peoples R China 5.Hebei GEO Univ, Sch Land Sci & Space Planning, Shijiazhuang 050031, Peoples R China 6.Univ Kiel, Cluster Excellence ROOTS, D-24118 Kiel, Germany 7.Univ Potsdam, Inst Biochem & Biol, D-14476 Potsdam, Germany 8.Univ Potsdam, Inst Environm Sci & Geog, D-14476 Potsdam, Germany 9.Alfred Wegener Inst, Helmholtz Ctr Polar & Marine Res, Polar Terr Environm Syst, D-14473 Potsdam, Germany 10.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100049, Peoples R China |
推荐引用方式 GB/T 7714 | Geng, Rongwei,Zhao, Yan,Herzschuh, Ulrike,et al. Pollen-based seasonal temperature reconstruction in Northeast China over the past 10,000 years, and its implications for understanding the Holocene Temperature Conundrum[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2024,651:112391. |
APA | Geng, Rongwei.,Zhao, Yan.,Herzschuh, Ulrike.,Cui, Qiaoyu.,Zheng, Zhuo.,...&Liang, Chen.(2024).Pollen-based seasonal temperature reconstruction in Northeast China over the past 10,000 years, and its implications for understanding the Holocene Temperature Conundrum.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,651,112391. |
MLA | Geng, Rongwei,et al."Pollen-based seasonal temperature reconstruction in Northeast China over the past 10,000 years, and its implications for understanding the Holocene Temperature Conundrum".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 651(2024):112391. |
入库方式: OAI收割
来源:地理科学与资源研究所
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