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  • port of this carbon through sinking of organic particles out of the surface layer (&lsquo;organic carbon pump&rsquo;) &ndash; this process is limited to first order by availability of light and nutrients (phosphate, nitrate, silicic acid and micronutrients such as iron); and (3) changes in the release of CO<sub>2</sub> in surface waters during formation of CaCO<sub>3</sub> shell material by plankt
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