Table 1 DOC and isotope characteristics throughout the fluvial network.

From: Utilization of ancient permafrost carbon in headwaters of Arctic fluvial networks

 

n

Initial DOC (μM)

SUVA254 (l mgC−1m−1)

DOCloss (%)

Init. Δ 14 C (‰)

OC loss Δ 14 C (‰)

Mean OC loss age ( 14 C years)

Permafrost (%)

Contemporary (%)

In situ (%)

Yedoma thaw

5

10,939±1,278

1.63±0.19

47.2±7.6

−884±41

−873±48

16,576

97.2±0.8

1.7±0.5

1.1±0.5

Erosion streams

3

2,503±518

3.25±0.44

17.5±4.9

−214±145

−405±185

4,171

42.8±20.7

56.4±20.7

0.8±0.4

Streams

25

1,691±87.6

3.44±0.11

13.3±2.0

51±6

−21±50

170

13.0±4.0

85.9±4.0

1.1±0.2

Minor tributaries

7

766±110

3.56±0.19

21.0±5.5

25±13

26±88

Modern

5.7±3.5

93.7±3.6

0.6±0.2

Major tributaries

8

511±68

4.03±0.08

12.2±1.8

40±3

68±32

Modern

0.6±0.1

73.1±8.4

26.3±9.9

Main stem

6

425±46

3.67±0.10

14.6±1.8

22±9

74±42

Modern

0.7±0.1

88.6±2.8

10.7±4.4

  1. DOC, dissolved organic carbon; OC, organic carbon.
  2. Mean initial DOC concentration, specific ultraviolet absorbance at 254 nm (SUVA254), percent DOC loss over 28 days (DOCloss), calculated Δ14C value and mean radiocarbon age of DOCloss (using equation (1) in Methods). The sample size at each site type is provided (n) and individual data are detailed in Supplementary Table 2. Mean percentage (±s.e.m.) contribution of permafrost, contemporary and in situ-derived DOC to DOCloss determined using the dual-carbon isotope mixing model.