Table 1. Methanogenic slurry potentials in which the methane concentration was measured daily.
Seafloor depth (m) | Mean sediment depth (cm) | Methanogenesis (nmol g−1 day−1) | s.e. | Number of replicates |
---|---|---|---|---|
150 | Water | 0 | 0.003 | 4 |
1 | 0.67 | 0.229 | 6 | |
3 | 0.44 | 0.402 | 6 | |
350 | Water | 0 | 0.001 | 2 |
1 | 17.87 | 7.82 | 4 | |
3 | 2.19 | 1.85 | 4 | |
550 | Water | 0.01 | 0.002 | 4 |
2.5 | 4.66 | 2.288 | 2 | |
7.5 | 0.08 | 0.008 | 2 | |
12.5 | 0.06 | 0.012 | 2 | |
17.5 | 0.06 | 0.022 | 2 | |
22.5 | 0.05 | 0.003 | 2 | |
550 | Water | 0.01 | 0.012 | 4 |
1 | 13.09 | 5.213 | 6 | |
3 | 0.27 | 0.028 | 6 | |
650 | Water | 0.004 | 0.0008 | 8 |
2.5 | 9.73 | 1.162 | 4 | |
7.5 | 0.03 | 0.007 | 4 | |
12.5 | 0.03 | 0.008 | 4 | |
17.5 | 0.02 | 0.001 | 2 | |
22.5 | 0 | - | 1 | |
750 | Water | 0.002 | 0.0025 | 2 |
1 | 87.84 | 15.32 | 4 | |
3 | 0.32 | 0.040 | 4 |
Mean rates of methane production (± s.e.) are presented for discrete sediment depth intervals and for the water immediately overlying the sediment. The rate of methanogenesis was calculated over 3–5 days depending on the linearity of production with time. Cores were collected from six locations with varying seabed depths. Two separate locations, where the seabed depth was 550 m, were targeted.