| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 5162826 | Organic Geochemistry | 2011 | 7 Pages |
Abstract
⺠Foxtail and common millet are ideal materials for palaeoclimate carbon isotope studies. ⺠δ13C trends of modern millets carbonized at varying temperatures were defined and explained. ⺠The observed 13C carbonization fractionation of only 0.2Ⱐin millets is much lighter than in wood. ⺠δ13C in carbonized millets can serve as an effective indicator for paleoclimatic reconstruction.
Related Topics
Physical Sciences and Engineering
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Organic Chemistry
Authors
Qing Yang, Xiaoqiang Li, Weiguo Liu, Xinying Zhou, Keliang Zhao, Nan Sun,