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Climate of the Past An interactive open-access journal of the European Geosciences Union
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Volume 12, issue 12
Clim. Past, 12, 2229–2240, 2016
https://doi.org/10.5194/cp-12-2229-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
Clim. Past, 12, 2229–2240, 2016
https://doi.org/10.5194/cp-12-2229-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

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.

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Subject: Proxy Use-Development-Validation | Archive: Terrestrial Archives | Timescale: Holocene
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Cited articles

An, Z. M.: Prehistoric agriculture in China, Acta. Archaeol. Sin., 4, 369–381, in Chinese, 1988.
Araus, J. L. and Buxo, R.: Changes in carbon isotope discrimination in grain cereals from the north-western Mediterranean Basin during the past seven millennia, Aust. J. Plant. Physiol., 20, 117–128, 1993.
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Chai, Y.: Broomcorn millet, Chinese Agriculture Press, Beijing, China, 47–70, 1999.
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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.
The fossilized seeds of common millet are suited to the production of quantitative Holocene...
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