Abstract
Earth's deep carbon cycle affects atmospheric CO(2), climate, and habitability. Owing to the extreme solubility of CaCO(3), aqueous fluids released from the subducting slab could extract all carbon from the slab. However, recycling efficiency is estimated at only around 40%. Data from carbonate inclusions, petrology, and Mg isotope systematics indicate Ca(2+) in carbonates is replaced by Mg(2+) and other cations during subduction. Here we determined the solubility of dolomite [CaMg(CO(3))(2)] and rhodochrosite (MnCO(3)), and put an upper limit on that of magnesite (MgCO(3)) under subduction zone conditions. Solubility decreases at least two orders of magnitude as carbonates become Mg-rich. This decreased solubility, coupled with heterogeneity of carbon and water subduction, may explain discrepancies in carbon recycling estimates. Over a range of slab settings, we find aqueous dissolution responsible for mobilizing 10 to 92% of slab carbon. Globally, aqueous fluids mobilise [Formula: see text]% ([Formula: see text] Mt/yr) of subducted carbon from subducting slabs.