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How Oxygen-16 Becomes More Concentrated in Glacial Ice

How Oxygen-16 Becomes More Concentrated in Glacial Ice
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Description: b) During times of glaciation, water vapor enriched in O-16 becomes trapped in ice accumulations and doesn’t return to the oceans. As a result, the relative concentration of  O-18 in seawater increases
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Source: https://biology-forums.com/index.php?action=gallery;sa=view;id=22523
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