Articles | Volume 14, issue 3
Research article
20 Mar 2018
Research article |  | 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, Jianhui Chen, Shengda Zhang, David D. Zhang, Zongli Wang, Qinghai Xu, Shengqian Chen, Shijin Wang, Shichang Kang, and Fahu Chen


Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (15 Dec 2017) by Denis-Didier Rousseau
AR by Haipeng Wang on behalf of the Authors (16 Dec 2017)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (20 Dec 2017) by Denis-Didier Rousseau
RR by Anonymous Referee #2 (22 Dec 2017)
ED: Publish subject to technical corrections (12 Feb 2018) by Denis-Didier Rousseau
AR by Haipeng Wang on behalf of the Authors (13 Feb 2018)  Author's response    Manuscript
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.