Researchers investigated the effects of ocean warming and acidification on the calcification rates of the coccolithophore *Emiliania huxleyi*. They grew cultures of the marine microalgae under various combinations of temperature, partial pressure of carbon dioxide (), and salinity for 14 days. All other growth parameters, including light-dark cycles and nutrient concentrations, were held constant. The conditions for Trials 1–5 are shown in the table below:
| Trial | Temperature (°C) | (µatm) | Salinity (psu) |
|---|---|---|---|
| 1 | 15 | 400 | 35 |
| 2 | 15 | 800 | 35 |
| 3 | 19 | 400 | 35 |
| 4 | 19 | 800 | 35 |
| 5 | 19 | 800 | 30 |
In Trial 5, salinity was lowered to 30 psu to simulate the influx of fresh water from glacier melting, which is associated with warming oceans. To isolate and determine the specific effect of this reduced salinity on the calcification rate under projected future conditions of ocean warming and acidification, which of the other trials should be used as the control?
- ATrial 1, because it represents the ambient baseline conditions for temperature, , and salinity.
- BTrial 3, because it maintains the same elevated temperature of 19°C but keeps and salinity at their baseline levels.
- Trial 4, because it maintains the same elevated temperature and elevated levels as Trial 5, with salinity being the only differing variable.Answer
- DTrial 2, because it isolates the effect of elevated at the baseline temperature of 15°C and standard salinity of 35 psu.