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Rates of seafloor and continental weathering govern Phanerozoic marine phosphate levels - Nature Geoscience
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Phosphate is an essential macronutrient for all organisms with a key role in setting levels of marine primary productivity. Despite its importance for marine biogeochemical cycles and its role in shaping the evolution of marine organisms, the factors controlling phosphate bioavailability on geologic timescales remain poorly understood.
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