In contrast, R P displays an increasing trend in Paleozoic followed by a high-value interval in Mesozoic, and declines in Cenozoic (Fig. 1C,D ).
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The coupling of Phanerozoic continental weathering and marine phosphorus cycle.
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In contrast, R P displays an increasing trend in Paleozoic followed by a high-value interval in Mesozoic, and declines in Cenozoic (Fig. 1C,D ).