“…During the dissolution of calcite, the precipitation of several secondary minerals has been observed in the presence of aqueous cations (Pb 2+ , Cu 2+ , and ) 125 – 128 , oxyanions ( , , and ) 129 , 130 , and F − 131 due to the formation of less soluble phases. Sometimes, calcite might be entirely replaced by the secondary minerals, such as cerussite (PbCO 3 ) 132 , dolomite (CaMg(CO 3 ) 2 ) 133 – 135 , magnesite (MgCO 3 ) 134 , siderite (FeCO 3 ) 133 , gypsum (CaSO 4 ) 136 , 137 , whewellite (CaC 2 O 4 ·H 2 O) 138 and fluorite (CaF 2 ) 139 , 140 , via a coupled dissolution–precipitation mechanism. Interestingly, the capture of aqueous Mg on the calcite surface was recognized when calcite dissolved in seawater, resulting in an enriched Mg surface 141 .…”