In paleoclimatology, the ratio of oxygen isotopes () in stalagmites is used to reconstruct historical rainfall, as wetter periods typically result in lower values in the precipitated calcium carbonate. However, researchers analyzing a stalagmite from Spain’s system of caves noticed that during a documented multi-decade drought in the thirteenth century, the stalagmite’s values remained persistently low. They hypothesized that the cave's drip water during this dry spell was fed by a massive, deep aquifer that takes decades to filter water downward, rather than by immediate precipitation. If this hypothesis is correct, it suggests that the Spanish stalagmite ______
Which choice most logically completes the text?
- was formed from groundwater that had fallen as precipitation decades prior to the thirteenth-century drought.Answer
- Bwill exhibit a dramatic increase in values if the drought continues for another fifty years.
- Cproves that subterranean aquifers worldwide consistently delay climatic signals recorded in geological formations.
- Drecorded rapid, year-to-year shifts in Spain's rainfall patterns throughout the thirteenth century.
Answer
the option stating that the stalagmite was formed from groundwater that had fallen as precipitation decades prior to the thirteenth-century drought
The correct option logically completes the argument by identifying the source of the low oxygen isotope values. Since the aquifer requires decades to transport water, the mineral deposits laid down during the dry spell reflect the wetter climate of decades past.
Step-by-Step Solution
Key Concept
Logical Inferences
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