Table 3.
Sources | Sinks | Annual O2 Deficit | Time until anoxia | Time since source | |||||||
---|---|---|---|---|---|---|---|---|---|---|---|
Ice Melt | Inflow | Total Source | Water Auto | Water Hetero | Sediment Hetero | Sediment Methano | Total Sink | ||||
Moles O2 y−1 | 1.0 × 106 | 5.0 × 105 | 1.5 × 106 | 2.6 × 106 | 1.2 × 105 | 4.9 × 105 | 6.1 × 105 | 3.9 × 106 | 1.2 × 106 | 4 | 39 |
% of total sink or source | 67 | 33 | – | 68 | 3 | 13 | 16 | – | – | – | – |
“Auto” refers to chemoautotrophy, “Hetero” refers to heterotrophy, “Methano” refers to methanotrophy. Sediment data are from the top 2 cm (Christner et al., 2014; Michaud, 2016). All “times” are in years. Annual oxygen deficit was computed by subtracting the total sinks from the sources. Time until anoxia was computed by dividing the measured oxygen concentration by the annual deficit. Time since source is the amount of time required to achieve the measured concentration of oxygen, starting at atmospheric equilibrium at standard temperature and pressure.