1School of Geography Science, Nanjing Normal University, Nanjing , 210023, China
2Key Laboratory of Vertebrate Evolution and Human Origin of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing, 100044, China
3The School of Earth Science and Resources, Chang’an University, Xi’an, Sha’anxi, 710054, China
Received: 10 Aug 2016 – Accepted: 23 Aug 2016 – Published: 29 Aug 2016
Abstract: In order to produce quantitative Holocene precipitation reconstructions for particular geographical areas, explicit proxies and accurate dating controls are required. The fossilized seeds of common millet (Panicum miliaceum) are found throughout the sedimentary strata of northern China, and are highly suited to the production of accurate quantitative Holocene precipitation reconstructions: their isotopic carbon composition (δ13C) gives a measure of the precipitation required during the growing season, and allows these seeds to be dated.
We therefore used a robust regression function, as part of a systematic study of the δ13C of common millet, to produce a quantitative reconstruction of Mid Holocene summer precipitation in the Guanzhong Basin. Our results showed that summer precipitation from 7.7–3.4 ka BP was 240–477 mm, with a mean of 354 mm, i.e. ~ 50 mm or 17 % higher than present levels. Maximal mean summer precipitation peaked at 414 mm, ~ 109 mm (or 36 %) higher than today, occurring during 6.4–5.5 ka BP; this is when the East Asian Summer Monsoon (EASM) was at its peak. As the δ13C-based precipitation record can reliably indicate EASM intensity during the Holocene, this work can provide a reliable proxy for further research into the detailed processes, and precise mechanisms, of the EASM.
Citation: Yang, Q., Li, X., Zhou, X., Zhao, K., and Sun, N.: Summer precipitation reconstructed quantitatively using a Mid Holocene δ13C common millet record from Guanzhong Basin, China, Clim. Past Discuss., doi:10.5194/cp-2016-87, in review, 2016.