Table 2 Application of a two-endmember mixing model to the measured Δ 14C values in ten paleosol samples.
From: Accumulation of radiocarbon in ancient landscapes: A small but significant input of unknown origin
Paleosol | Depth (cm) | TOC (wt%) | 1/TOC | FM | Modern C (%) | Error ± (%) |
|---|---|---|---|---|---|---|
Lakim | 0 | 0.26 | 3.80 | 0.057 | 1.70 | 0.19 |
Lakim | 25 | 0.09 | 11.21 | 0.136 | 1.56 | 0.19 |
Lakim | 50 | 0.14 | 7.07 | 0.080 | 1.00 | 0.19 |
Lakim | 75 | 0.24 | 4.23 | 0.055 | 1.36 | 0.19 |
Lakim | 100 | 0.03 | 30.86 | 0.181 | 2.36 | 0.19 |
Luca | 22 | 0.01 | 71.43 | 0.232 | 0.32 | 1.84 |
TC | 0 | 0.17 | 5.87 | 0.028 | 0.47 | 0.19 |
TC | 25 | 0.15 | 6.80 | 0.028 | 0.55 | 0.19 |
TC | 50 | 0.23 | 4.35 | 0.024 | 0.61 | 0.19 |
TC | 100 | 0.08 | 11.82 | 0.062 | 0.71 | 0.33 |