Question

Difficulty: MediumMulti-Sentence Synthesis Inferences

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?

  1. 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
  2. B
    They rely primarily on sulfate-reducing bacteria to oxidize methane because heterotrophic bacteria deplete the available pool of ferric oxides.
  3. C
    They experience a complete cessation of all heterotrophic bacterial respiration due to the total absence of organic carbon input.
  4. D
    They act as less effective methane sinks than oligotrophic sediments that lack reactive iron oxides entirely.
  5. E
    They release elevated levels of methane directly caused by the increased metabolic respiration of iron-reducing methanotrophs.

Answer

Benthic sediments rich in reactive iron oxides exhibit lower net methane emissions during periods of low surface primary productivity because decreased heterotrophic activity preserves the ferric oxides needed by methanotrophs to oxidize methane.
The passage establishes in Paragraph 2 that heterotrophic bacteria compete for ferric oxides during high organic deposition, depriving iron-reducing methanotrophs of electron acceptors and causing methane emissions to rise. Paragraph 3 adds that during periods of low organic input (low surface productivity), heterotrophic competition subsides, allowing methanotrophs to utilize ferric oxides efficiently and suppress methane emissions. Combining these statements leads directly to the conclusion that lower surface primary productivity results in lower net methane emissions due to preserved ferric oxide availability.

Step-by-Step Solution

1
Locate relevant premises regarding low surface primary productivity across the passage.
Identified that low surface primary productivity corresponds to oligotrophic conditions with low organic input (Paragraph 3).
The question asks specifically about conditions during periods of low surface primary productivity.
2
Synthesize the interaction between heterotrophic bacteria and iron-reducing methanotrophs from Paragraphs 2 and 3.
Paragraph 2 explains that heterotrophic bacteria consume ferric oxides when organic carbon flux is high, leaving fewer electron acceptors for methanotrophs and causing methane emissions to surge. Paragraph 3 states that when organic input is low, heterotrophic competition subsides, enabling methanotrophs to use ferric oxides efficiently and suppress methane emissions.
Combining these non-contiguous premises reveals the direct inverse relationship between surface productivity and the effectiveness of iron-rich sediments as a methane sink.
3
Evaluate the choices against the synthesized conclusion.
The option stating that net methane emissions are lower because reduced heterotrophic competition leaves more ferric oxides available accurately reflects this multi-sentence synthesis.
This is the only choice strictly derived from combining the two structural halves of the argument.

Key Concept

Multi-Sentence Synthesis Inference
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