Journal
NATURE GEOSCIENCE
Volume 1, Issue 8, Pages 497-498Publisher
NATURE PUBLISHING GROUP
DOI: 10.1038/ngeo273
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The ratio of magnesium to calcium in sea water is thought to have influenced the skeletal mineralogy of certain marine calcifiers throughout the Phanerozoic eon. A fresh look at old data suggests that mass extinctions may have also played a role.
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