A team of biogeochemists investigated anaerobic oxidation of methane by marine sediment microbes under simulated deep-sea temperature conditions (). Four distinct reactor setups were prepared containing equal masses of marine sediment and methane gas, but with varying additions of electron acceptors, heat sterilization, and hydrostatic pressures.
Match each experimental setup to its corresponding role or baseline function in the experiment.
- Setup 1: Untreated sediment + sulphate () at hydrostatic pressurePrimary experimental group testing microbial methane oxidation under simulated in situ conditions
- Setup 2: Untreated sediment without added electron acceptors at hydrostatic pressureBaseline control group to measure background methane consumption without external electron acceptors
- Setup 3: Autoclaved (heat-sterilized) sediment + sulphate () at hydrostatic pressureAbiotic negative control to quantify non-biological methane loss or chemical leakage
- Setup 4: Untreated sediment + sulphate () at (atmospheric) hydrostatic pressureVariable comparison group to evaluate the specific influence of hydrostatic pressure on metabolic rates
Answer
Setup 1 matches the primary experimental group under simulated in situ conditions; Setup 2 matches the baseline control measuring activity without added electron acceptors; Setup 3 matches the abiotic negative control using heat sterilization; Setup 4 matches the variable comparison group evaluating the effect of hydrostatic pressure.
In experimental design, control groups isolate variables and establish baseline measurements. Heat-sterilized setups serve as abiotic controls to confirm biological necessity. Setups lacking specific reactants (such as sulphate) provide a baseline for background activity without that variable. Setups altering a single physical condition (such as hydrostatic pressure) allow direct comparison of that specific variable against the primary experimental group.
Step-by-Step Solution
Key Concept
Determining Control Groups and Baseline Conditions