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Rivers carry the dissolved and solid products of silicate mineral weathering, a process that removes [Formula see text] through the atmosphere and offers a vital negative weather feedback over geological timescales. Right here we reveal that, in some river systems, a reactive trade pool on river suspended particulate matter, bonded weakly to mineral areas, advances the cellular cation flux by 50%. The chemistry of both river seas while the change pool demonstrates trade equilibrium, verifie
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