TABLE 10.
Calculation of carbon flow via acetate to sulfate reduction, to methanogenesis, and in uncoupled processes in pond sediments of the McMurdo Ice Shelf incubated at temperatures below freezing
Pond | Temp (°C) | % Carbon flow via acetate:
|
||
---|---|---|---|---|
To CH4a | Coupled to sulfate reductionb | To CO2 (electron acceptor undefined)c | ||
Orange | −10 | 8.0 | 2.6 | 89.4 |
Brack | −10 | 3.9 | 44.4 | 51.7 |
Determined from the percentage of CH4 accounted for by acetate × CH4 production/rate of acetate dissimilation (data from Table 5).
Determined from the percentage of sulfate reduction accounted for by acetate × sulfate reduction/rate of acetate dissimilation (data from Table 5).
Calculated as 100 − (% CH4 [ac] + % SO42−[ac]).