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- W2387031208 abstract "The use of stable carbon isotope as climate proxies is widely accepted for climate reconstruction, but how the stable carbon isotope composition of C 4 plants responds to the climate is still unclear in the trace studies of the carbon isotope. In this research, we observe the carbon isotope discrimination of the typical C 4 plant, corn, during the growing period, and we find the obvious variation of the carbon isotope composition. The carbon isotope compositions of the top leaves vary more apparently than those of the lower leaves. This variation is related to several climate factors, such as temperature, moisture, the intensity of sunlight and the CO 2 level. Furthermore, to the same corn, the δ 13 C values of the top leaves are positive to those of the lower leaves, and this phenomenon is more obvious with the growing of the corn. We attribute it to the variation of the temperature and the intensity of the sunlight. The isotope fractionation during the growing process of corn indicates that the δ 13 C value increases when the climate is warm and dry. This will offer us the evidence for reconstructing the paleoclimate by using the carbon isotope of plants." @default.
- W2387031208 created "2016-06-24" @default.
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- W2387031208 date "2002-01-01" @default.
- W2387031208 modified "2023-09-25" @default.
- W2387031208 title "HOW DOES THE CARBON ISOTOPE COMPOSITION RESPONSE TO THE CLIMATE DURING THE PLANT GROWING" @default.
- W2387031208 hasPublicationYear "2002" @default.
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