Articles | Volume 18, issue 10
https://doi.org/10.5194/cp-18-2381-2022
https://doi.org/10.5194/cp-18-2381-2022
Research article
 | 
25 Oct 2022
Research article |  | 25 Oct 2022

Palynological evidence reveals an arid early Holocene for the northeast Tibetan Plateau

Nannan Wang, Lina Liu, Xiaohuan Hou, Yanrong Zhang, Haicheng Wei, and Xianyong Cao

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2022-366', Anonymous Referee #1, 13 Jul 2022
  • RC2: 'Comment on egusphere-2022-366', Anonymous Referee #2, 16 Jul 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to minor revisions (review by editor) (01 Sep 2022) by Claudio Latorre
AR by Xianyong Cao on behalf of the Authors (01 Sep 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (13 Sep 2022) by Claudio Latorre
AR by Xianyong Cao on behalf of the Authors (14 Sep 2022)  Manuscript 

Post-review adjustments

AA: Author's adjustment | EA: Editor approval
AA by Xianyong Cao on behalf of the Authors (19 Oct 2022)   Author's adjustment   Manuscript
EA: Adjustments approved (19 Oct 2022) by Claudio Latorre
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Short summary
We reconstructed the vegetation and climate change since the last 14.2 ka BP from a fossil pollen record together with multiple proxies (grain size, contents of total organic carbon and total nitrogen) on the northeast Tibetan Plateau. The results reveal that an arid climate occurs in the early Holocene and the vegetation could be disturbed by human activities to some extent after ca. 0.24 ka BP (1710 CE).