Articles | Volume 12, issue 12
Clim. Past, 12, 2229–2240, 2016
https://doi.org/10.5194/cp-12-2229-2016
Clim. Past, 12, 2229–2240, 2016
https://doi.org/10.5194/cp-12-2229-2016

Research article 19 Dec 2016

Research article | 19 Dec 2016

Quantitative reconstruction of summer precipitation using a mid-Holocene δ13C common millet record from Guanzhong Basin, northern China

Qing Yang et al.

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: Publish subject to minor revisions (review by Editor) (13 Nov 2016) by Zhengtang Guo
AR by X. Q. Li on behalf of the Authors (22 Nov 2016)  Author's response    Manuscript
ED: Publish as is (27 Nov 2016) by Zhengtang Guo
AR by X. Q. Li on behalf of the Authors (30 Nov 2016)  Author's response    Manuscript
Download
Short summary
The fossilized seeds of common millet are suited to the production of quantitative Holocene precipitation reconstructions. Our reconstructed results showed that summer precipitation from 7.7–3.4 ka BP was ~ 50 mm, or 17 % higher than present levels. Maximal mean summer precipitation peaked at 414 mm during 6.1–5.5 ka BP, ~ 109 mm, or 36 % higher than today, indicating the EASM peaked at this time. This work can provide a new proxy for further research into continuous paleoprecipitation sequences.