Passage:
In benthic marine ecosystems, methane-oxidizing archaea typically form syntrophic consortia with sulfate-reducing bacteria to metabolize dissolved methane, a process known as anaerobic oxidation of methane (AOM). Early oceanographic models assumed that AOM rates were strictly limited by sulfate availability in subsurface sediments. However, recent biogeochemical surveys in the Santa Barbara Basin revealed that in areas rich in reactive iron oxides, certain methanotrophs can bypass sulfate-reducing partners entirely by coupling methane oxidation directly to ferric iron reduction.
Intriguingly, while these iron-reducing archaea operate independently of sulfate reducers, their metabolic activity remains tightly regulated by local organic carbon flux. High organic deposition stimulates heterotrophic bacterial communities, which consume available ferric oxides for their own anaerobic respiration, thereby depleting the electron acceptors required by the iron-reducing methanotrophs. Consequently, even in iron-rich benthic zones, methane flux into the overlying water column surges during periods of elevated surface primary productivity, despite the abundance of iron oxides.
Conversely, under oligotrophic conditions with low organic input, heterotrophic competition subsides, allowing iron-reducing methanotrophs to utilize the iron oxides efficiently and suppress methane emissions. Thus, the capacity of iron-rich sediments to act as a methane sink is paradoxically compromised, rather than enhanced, by high surface biological activity.
Based on the passage, which of the following can be inferred about benthic sediments rich in reactive iron oxides during periods of low surface primary productivity?
- They exhibit lower net methane emissions into the water column than during periods of high surface productivity because reduced heterotrophic competition leaves more ferric oxides available for methanotrophs.Answer
- BThey rely primarily on sulfate-reducing bacteria to oxidize methane because heterotrophic bacteria deplete the available pool of ferric oxides.
- CThey experience a complete cessation of all heterotrophic bacterial respiration due to the total absence of organic carbon input.
- DThey act as less effective methane sinks than oligotrophic sediments that lack reactive iron oxides entirely.
- EThey release elevated levels of methane directly caused by the increased metabolic respiration of iron-reducing methanotrophs.