Analysis of carbon isotope in phytoliths from C3 and C4 plants and modern soils |
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Authors: | Houyuan Lü Yongji Wang Guo’an Wang Hui Yang Zhen Li |
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Institution: | (1) First Institute of Oceanography, State Oceanic Administration, 266003 Qingdao, China;(2) Institute of Geology and Geophysics, Chinese Academy of Sciences, 100029 Beijing, China;(3) Lanzhou Institute of Geology, Chinese Academy of Sciences, 730000 Lanzhou, China |
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Abstract: | The analysis of carbon isotope in phytoliths from modern plants and surface soils in China shows that the values of carbon
isotope are consistent with those from C3 and C4 plants, and the processes of photosynthesis of the original plants can be
clearly identified by carbon isotope in phytoliths. The value of carbon isotope varied from −23.8‰ to −28‰, with the maximum
distributed in the latitude zone from 34°N to 40°N in North China and East China areas, and the minimum in the Northeast China
and South China regions. The values of carbon of phytoliths tend to increase from low to high and then reduce to low value
again as the latitude increases. In the same latitude zone, the carbon isotope in phytoliths from grassland soil under the
trees is obviously lower than that from grassland soil without any trees with the difference of 1%–2‰ |
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Keywords: | C3 and C4 plants phytoliths carbon isotope |
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