Water vapor evaporated from the ocean contains a greater proportion of oxygen-16 and a smaller proportion of the heavier oxygen-18 than does seawater. Normally, this phenomenon has no effect on the overall composition of the ocean, because evaporated seawater returns to the ocean through precipitation. During an falls on ice caps, where it is trapped as ice.
What this question is testing
Premise
Think about it this way. The water that evaporates off the ocean is lighter in composition — more O-16 (light), less O-18 (heavy). In normal times, that's a wash because the vapor falls back as rain into the ocean.
Evaluate
But during an ice age, that vapor doesn't come back. It piles up on ice caps and stays there. So the ocean is steadily losing the lighter oxygen-16 with no replacement. What's left behind in the ocean? More of the heavier stuff: oxygen-18.
Imagine pouring a salt-water solution through a coffee filter that catches one of the components. The water that drips through is missing one ingredient, and what stays in the filter has a higher concentration of the other. Same idea here — the ocean is the "filter," and what remains is enriched in O-18.
Goal
Find the answer that says O-18 in seawater is more concentrated during ice ages.
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