Articles | Volume 15, issue 2
https://doi.org/10.5194/cp-15-405-2019
https://doi.org/10.5194/cp-15-405-2019
Research article
 | Highlight paper
 | 
11 Mar 2019
Research article | Highlight paper |  | 11 Mar 2019

Late Miocene–Pliocene climate evolution recorded by the red clay cover on the Xiaoshuizi planation surface, NE Tibetan Plateau

Xiaomiao Li, Tingjiang Peng, Zhenhua Ma, Meng Li, Zhantao Feng, Benhong Guo, Hao Yu, Xiyan Ye, Zhengchuang Hui, Chunhui Song, and Jijun Li

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (03 Oct 2018) by Ran Feng
AR by Xiaomiao Li on behalf of the Authors (20 Oct 2018)
ED: Referee Nomination & Report Request started (27 Oct 2018) by Ran Feng
RR by Anonymous Referee #3 (17 Nov 2018)
RR by Anonymous Referee #4 (04 Dec 2018)
ED: Reconsider after major revisions (19 Dec 2018) by Ran Feng
AR by Xiaomiao Li on behalf of the Authors (16 Jan 2019)  Author's response   Manuscript 
ED: Publish subject to minor revisions (review by editor) (22 Jan 2019) by Ran Feng
AR by Xiaomiao Li on behalf of the Authors (26 Jan 2019)  Author's response   Manuscript 
ED: Publish as is (17 Feb 2019) by Ran Feng
AR by Xiaomiao Li on behalf of the Authors (22 Feb 2019)  Manuscript 
Download
Short summary
Multiple proxies for the XSZ planation surface reveal that the climate was dry and stable during the late Miocene but became intermittently humid with more seasonality at 4.7–3.9 Ma. Regional climatic differences between the central and western CLP reveal that expansion of the paleo-EASM occurred during the early Pliocene. The warming of the high northern latitudes in response to the closure of the Panama Seaway may have been responsible for the thermodynamical enhancement of the paleo–EASM.