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- W2498385671 abstract "14 C activities of decadal samples from beech trees growing under extreme calcareous conditions were compared to 14 C activities of decadal samples of the same age from a beech tree growing in a normal mold soil in order to see whether part of the carbon assimilated during photosynthesis might originate from 14 C-deficient carbonates in the soil. The calcareous soils contained from 18 to 52% calcium carbonate, and this carbonate had a mean 14 C age of 10,200 to 17,600 years BP. A comparison was also made with the 14 C activity of contemporaneous samples from Douglas Fir from the US North Pacific (Stuiver, 1982). No significant depletion in 14 C activity in beech trees growing in the highly calcareous soils was detected. The measured mean difference in 14 C activity in beech trees from calcareous and non-calcareous sites corresponds to an uptake of 0.12 ± 0.3% carbon from soil carbonates in the calcareous sites." @default.
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- W2498385671 date "1983-01-01" @default.
- W2498385671 modified "2023-09-23" @default.
- W2498385671 title "Possible Depletion in 14C in Trees Growing in Calcareous Soils" @default.
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- W2498385671 doi "https://doi.org/10.1017/s0033822200005701" @default.
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