Yield responses of wild C₃ and C₄ crop progenitors to subambient CO₂: a test for the role of CO₂ limitation in the origin of agriculture

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• 作者：Jennifer Cunniff ; Glynis Jones ; Michael Charles and Colin P. Osborne
• 刊名：Global Change Biology
• 出版年：2017
• 出版时间：January 2017
• 年：2017
• 卷：23
• 期：1
• 页码：380-393
• 全文大小：478K
• ISSN：1365-2486

文摘

Limitation of plant productivity by the low partial pressure of atmospheric CO₂ (C_a) experienced during the last glacial period is hypothesized to have been an important constraint on the origins of agriculture. In support of this hypothesis, previous work has shown that glacial C_a limits vegetative growth in the wild progenitors of both C₃ and C₄ founder crops. Here, we present data showing that glacial C_a also reduces grain yield in both crop types. We grew four wild progenitors of C₃ (einkorn wheat and barley) and C₄ crops (foxtail and broomcorn millets) at glacial and postglacial C_a, measuring grain yield and the morphological and physiological components contributing to these yield changes. The C₃ species showed a significant increase in unthreshed grain yield of ~50% with the glacial to postglacial increase in C_a, which matched the stimulation of photosynthesis, suggesting that increases in photosynthesis are directly translated into yield at subambient levels of C_a. Increased yield was controlled by a higher rate of tillering, leading to a larger number of tillers bearing fertile spikes, and increases in seed number and size. The C₄ species showed smaller, but significant, increases in grain yield of 10–15%, arising from larger seed numbers and sizes. Photosynthesis was enhanced by C_a in only one C₄ species and the effect diminished during development, suggesting that an indirect mechanism mediated by plant water relations could also be playing a role in the yield increase. Interestingly, the C₄ species at glacial C_a showed some evidence that photosynthetic capacity was upregulated to enhance carbon capture. Development under glacial C_a also impacted negatively on the subsequent germination and viability of seeds. These results suggest that the grain production of both C₃ and C₄ crop progenitors was limited by the atmospheric conditions of the last glacial period, with important implications for the origins of agriculture.