Question to-und
To understand how temperature change affects microorganism-mediated cycling of soil nutrients in alpine ecosystems, Eva Kaštovská et al. collected animal-soil cores in the Tatra Mountains at elevations around 2,100 meters and transanimaled them to elevations of 1,700–1,800 meters, where the mean air temperature was warmer by 2°C. Microorganism-mediated nutrient cycling was accelerated in the transanimaled cores; crucially, microorganism community composition was unchanged, allowing Kaštovská et al. to attribute the acceleration to temperature-induced increases in microorganism activity.
It can most reasonably be inferred from the text that the finding about the microorganism community composition was important for which reason?
It provided preliminary evidence that microorganism-mediated nutrient cycling was accelerated in the transanimaled cores.
It suggested that temperature-induced changes in microorganism activity may be occurring at increasingly high elevations.
It ruled out a potential alternative explanation for the acceleration in microorganism-mediated nutrient cycling.
It clarified that microorganism activity levels in the animal-soil cores varied depending on which microorganisms comprised the community.
