Articles | Volume 14, issue 3
https://doi.org/10.5194/cp-14-383-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-14-383-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
20 Mar 2018
Research article |
| 20 Mar 2018
| 20 Mar 2018
A chironomid-based record of temperature variability during the past 4000 years in northern China and its possible societal implications
Haipeng Wang
State Key Laboratory of Cryospheric Science, Northwest Institute of
Eco-Environment and Resources, Chinese Academy of Sciences,
Lanzhou 730000, China
MOE Key Laboratory of Western China's
Environmental Systems, College of Earth Environmental Sciences, Lanzhou
University, Lanzhou 730000, China
Jianhui Chen
CORRESPONDING AUTHOR
MOE Key Laboratory of Western China's
Environmental Systems, College of Earth Environmental Sciences, Lanzhou
University, Lanzhou 730000, China
Shengda Zhang
Department of Geography, The
University of Hong Kong, Hong Kong SAR, China
David D. Zhang
School of Geographical
Sciences, Guangzhou University, Guangzhou 510000, China
Department of Geography, The
University of Hong Kong, Hong Kong SAR, China
Zongli Wang
MOE Key Laboratory of Western China's
Environmental Systems, College of Earth Environmental Sciences, Lanzhou
University, Lanzhou 730000, China
Qinghai Xu
Institute
of Nihewan Archaeology Research, Hebei Normal University, Shijiazhuang
050024, China
Shengqian Chen
MOE Key Laboratory of Western China's
Environmental Systems, College of Earth Environmental Sciences, Lanzhou
University, Lanzhou 730000, China
Shijin Wang
State Key Laboratory of Cryospheric Science, Northwest Institute of
Eco-Environment and Resources, Chinese Academy of Sciences,
Lanzhou 730000, China
Shichang Kang
State Key Laboratory of Cryospheric Science, Northwest Institute of
Eco-Environment and Resources, Chinese Academy of Sciences,
Lanzhou 730000, China
Fahu Chen
MOE Key Laboratory of Western China's
Environmental Systems, College of Earth Environmental Sciences, Lanzhou
University, Lanzhou 730000, China
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Cited
20 citations as recorded by crossref.
- Aeolian Soils on the Eastern Side of the Horqin Sandy Land, China: A Provenance and Sedimentary Environment Reconstruction Perspective J. Wang et al. 10.2139/ssrn.3940881
- Anthropogenic mountain forest degradation and soil erosion recorded in the sediments of Mayinghai Lake in northern China X. Huang et al. 10.1016/j.catena.2021.105597
- Quantification of temperature and precipitation changes in northern China during the “5000-year” Chinese History C. Zhang et al. 10.1016/j.quascirev.2021.106819
- Diverse effects of climate changes and anthropogenic activities on sedimentary nitrogen isotope (δ15Nsed.) in lakes across different regions of China since the late Holocene K. Zhou et al. 10.1016/j.scitotenv.2024.176550
- Anthropogenic forest degradation and its impact on soil erosion in the mountainous region of northern China X. Ren et al. 10.1016/j.catena.2024.108217
- A rapid late Holocene lake ecosystem shift driven by climate change: evidence from the first cladoceran record from an alpine lake in northern China F. Li et al. 10.1016/j.scib.2019.12.010
- The impact of early trans-Eurasian exchange on animal utilization in northern China during 5000–2500 BP G. Dong et al. 10.1177/0959683620941169
- Effects of climate warming and nitrogen deposition on subtropical montane ponds (central China) over the last two centuries: Evidence from subfossil chironomids T. Zheng et al. 10.1016/j.envpol.2020.114256
- Cycles of grazing and agricultural activity during the historical period and its relationship with climatic and societal changes in northern China J. Zhang et al. 10.1002/ldr.4007
- A major hydrobiological change in Dasht-e Arjan Wetland (southwestern Iran) during the late glacial – early Holocene transition revealed by subfossil chironomids C. Aubert et al. 10.1139/cjes-2018-0256
- Climate-driven desertification and its implications for the ancient Silk Road trade G. Dong et al. 10.5194/cp-17-1395-2021
- Aeolian soils on the eastern side of the Horqin Sandy Land, China: A provenance and sedimentary environment reconstruction perspective J. Wang et al. 10.1016/j.catena.2021.105945
- Variations in the East Asian winter monsoon from 3500 to 1300 cal. yr BP in northern China and their possible societal impacts J. Chen et al. 10.1016/j.jseaes.2019.103912
- Asynchronous transformation of human livelihoods in key regions of the trans-Eurasia exchange in China during 4000-2200 BP M. Ma et al. 10.1016/j.quascirev.2022.107665
- Dietary shift and social hierarchy from the Proto-Shang to Zhou Dynasty in the Central Plains of China X. Li et al. 10.1088/1748-9326/ab6783
- How did the late 1920s drought affect northern Chinese society? X. Chen et al. 10.1016/j.wace.2022.100451
- Spatiotemporal variation in human settlements and their interaction with living environments in Neolithic and Bronze Age China G. Dong et al. 10.1177/03091333221087992
- Concurrent mid-Holocene East Asian temperature and summer monsoon maxima forced by high- and low-latitude interplay X. Zhang et al. 10.1016/j.gloplacha.2022.104008
- Body size of fossil Pediastrum in lake sediments as an indicator of temperature variation X. Huang et al. 10.1016/j.palaeo.2023.111687
- Vertical sediment migrations of dominant midge species in subtropical lakes with implications for bioassessment W. Zou et al. 10.1016/j.ecolind.2018.08.020
19 citations as recorded by crossref.
- Aeolian Soils on the Eastern Side of the Horqin Sandy Land, China: A Provenance and Sedimentary Environment Reconstruction Perspective J. Wang et al. 10.2139/ssrn.3940881
- Anthropogenic mountain forest degradation and soil erosion recorded in the sediments of Mayinghai Lake in northern China X. Huang et al. 10.1016/j.catena.2021.105597
- Quantification of temperature and precipitation changes in northern China during the “5000-year” Chinese History C. Zhang et al. 10.1016/j.quascirev.2021.106819
- Diverse effects of climate changes and anthropogenic activities on sedimentary nitrogen isotope (δ15Nsed.) in lakes across different regions of China since the late Holocene K. Zhou et al. 10.1016/j.scitotenv.2024.176550
- Anthropogenic forest degradation and its impact on soil erosion in the mountainous region of northern China X. Ren et al. 10.1016/j.catena.2024.108217
- A rapid late Holocene lake ecosystem shift driven by climate change: evidence from the first cladoceran record from an alpine lake in northern China F. Li et al. 10.1016/j.scib.2019.12.010
- The impact of early trans-Eurasian exchange on animal utilization in northern China during 5000–2500 BP G. Dong et al. 10.1177/0959683620941169
- Effects of climate warming and nitrogen deposition on subtropical montane ponds (central China) over the last two centuries: Evidence from subfossil chironomids T. Zheng et al. 10.1016/j.envpol.2020.114256
- Cycles of grazing and agricultural activity during the historical period and its relationship with climatic and societal changes in northern China J. Zhang et al. 10.1002/ldr.4007
- A major hydrobiological change in Dasht-e Arjan Wetland (southwestern Iran) during the late glacial – early Holocene transition revealed by subfossil chironomids C. Aubert et al. 10.1139/cjes-2018-0256
- Climate-driven desertification and its implications for the ancient Silk Road trade G. Dong et al. 10.5194/cp-17-1395-2021
- Aeolian soils on the eastern side of the Horqin Sandy Land, China: A provenance and sedimentary environment reconstruction perspective J. Wang et al. 10.1016/j.catena.2021.105945
- Variations in the East Asian winter monsoon from 3500 to 1300 cal. yr BP in northern China and their possible societal impacts J. Chen et al. 10.1016/j.jseaes.2019.103912
- Asynchronous transformation of human livelihoods in key regions of the trans-Eurasia exchange in China during 4000-2200 BP M. Ma et al. 10.1016/j.quascirev.2022.107665
- Dietary shift and social hierarchy from the Proto-Shang to Zhou Dynasty in the Central Plains of China X. Li et al. 10.1088/1748-9326/ab6783
- How did the late 1920s drought affect northern Chinese society? X. Chen et al. 10.1016/j.wace.2022.100451
- Spatiotemporal variation in human settlements and their interaction with living environments in Neolithic and Bronze Age China G. Dong et al. 10.1177/03091333221087992
- Concurrent mid-Holocene East Asian temperature and summer monsoon maxima forced by high- and low-latitude interplay X. Zhang et al. 10.1016/j.gloplacha.2022.104008
- Body size of fossil Pediastrum in lake sediments as an indicator of temperature variation X. Huang et al. 10.1016/j.palaeo.2023.111687
Discussed (final revised paper)
Latest update: 14 Dec 2024
Short summary
The chironomid-inferred temperature record from Gonghai Lake exhibits a stepwise decreasing trend since 4 ka. A cold event in the Era of Disunity, the Sui-Tang Warm Period, the Medieval Warm Period and the Little Ice Age can all be recognized in our record, as well as in many other temperature reconstructions in China. Local wars in Shanxi Province, documented in the historical literature during the past 2700 years, are statistically significantly correlated with changes in temperature.
The chironomid-inferred temperature record from Gonghai Lake exhibits a stepwise decreasing...
