Geochemists studying paleoclimate records in subterranean cave formations have established the following premises:
• Every stalagmite specimen from the Hanlin formation that preserves intact lipid biomarkers exhibits depleted isotopic ratios.
• Any stalagmite specimen from this formation that has undergone calcite recrystallization fails to preserve intact lipid biomarkers.
• A stalagmite specimen exhibits depleted isotopic ratios only if it formed during an era of elevated precipitation.
• Analysis of Hanlin specimen H-4 confirms that it preserves intact lipid biomarkers.
If the statements above are true, which one of the following must be true on the basis of them?
- AAny stalagmite specimen from the Hanlin formation that formed during an era of elevated precipitation preserves intact lipid biomarkers.
- BAny stalagmite specimen from the Hanlin formation that has not undergone calcite recrystallization exhibits depleted isotopic ratios.
- Hanlin specimen H-4 formed during an era of elevated precipitation.Cevap
- DNo stalagmite specimen from the Hanlin formation that lacks intact lipid biomarkers formed during an era of elevated precipitation.
- ECalcite recrystallization is the only process that prevents the preservation of intact lipid biomarkers in the Hanlin formation.
Cevap
Hanlin specimen H-4 formed during an era of elevated precipitation.
The stimulus provides a direct deductive chain. We are told that Hanlin specimen H-4 possesses intact lipid biomarkers. According to the first premise, any specimen with intact lipid biomarkers exhibits depleted isotopic ratios. According to the third premise, exhibiting depleted isotopic ratios occurs 'only if' the specimen formed during an era of elevated precipitation, meaning that elevated precipitation is a necessary condition for depleted ratios. Chaining these validly () proves conclusively that specimen H-4 must have formed during an era of elevated precipitation.
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Conditional Logic Chaining and Valid Deductive Inferences
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