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Which outcome occurs when carbon dioxide concentrations increase within karst cave systems?

A)Increased dissolution of carbonate bedrock
B)Decreased formation of speleothems
C)Enhanced precipitation of calcium carbonate
D)Reduced chemical weathering of silicates

💡 Explanation

Increased CO₂ elevates carbonic acid levels, accelerating bedrock dissolution via the dissolution-precipitation equilibrium mechanism; because carbonic acid reacts with limestone, bedrock erosion increases. Therefore, dissolution accelerates, rather than slowing speleothem formation or affecting silicate weathering.

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