Table 2 τsoil and soil mean carbon ages for the Ganga–Brahmaputra river catchment during the past 17 kyrs

From: Dominant control of temperature on (sub-)tropical soil carbon turnover

Deposition age [kyrs BP]

n-Alkanoic acid homologues

Mass weighted mean R [14C yrs]

τsoil [yrs]

Soil mean carbon ages [yrs]

0.003

n-C24:0, n-C26:0, n-C28:0, n-C30:0, n-C32:0

1446 ± 80a

36 ± 4

2333 ± 293

0.004

n-C24:0, n-C26:0, n-C28:0, n-C30:0, n-C32:0

927 ± 87a

23 ± 3

1495 ± 220

3.54 ± 0.39

n-C24:0, n-C26:0, n-C28:0, n-C30:0, n-C34:0

7119 ± 1149

178 ± 33

11483 ± 2261

6.57 ± 0.42

n-C24:0, n-C28:0, n-C30:0, n-C32:0

1489 ± 618

37 ± 16

2401 ± 1033

10272 ± 504

n-C24:0, n-C26:0, n-C28:0, n-C30:0, n-C32:0

3009 ± 749

75 ± 20

4853 ± 1327

10.92 ± 0.48

n-C24:0, n-C28:0, n-C30:0, n-C32:0, n-C34:0

2070 ± 1116

52 ± 28

3339 ± 1839

12.74 ± 0.42

n-C24:0, n-C26:0, n-C28:0, n-C30:0, n-C34:0

3234 ± 1166

80 ± 30

5216 ± 1971

13.61 ± 0.23

n-C24:0, n-C26:0, n-C28:0, n-C30:0, n-C32, n-C34:0

1375 ± 830

34 ± 21

2217 ± 1363

15.62 ± 0.37

n-C24:0, n-C26:0, n-C28:0

8709 ± 4166

217 ± 106

14047 ± 6903

16.77 ± 0.39

n-C24:0, n-C26:0, n-C28:0, n-C30:0, n-C34:0

6453 ± 2177

116 ± 55

7506 ± 3612

16.90 ± 0.10

n-C24:0, n-C26:0 n-C28:0, n-C30:0, n-C32:0

4004 ± 3507

100 ± 88

6458 ± 5703

  1. τsoil and soil mean carbon ages (this study) are calculated from compound-specific radiocarbon analysis (CSRA) of n-alkanoic acids in marine sediments from the Bengal Fan (data from ref. 16). CSRA-data of n-alkanoic acids are presented as the reservoir age offset (R) between the n-alkanoic acids and the atmosphere at the time of deposition in the Bengal Fan. R is based upon the mass-weighted results of the listed n-alkanoic acid homologues16. The deposition age is adopted from ref. 16. The standard deviations (±) are reported along with the results.
  2. aData of pre-1950 Bengal Fan sediments are adopted from ref. 27.