“…These include, but are not limited to, calcite, aragonite, vaterite, dolomite, CaCO 3 monohydrate, CaCO 3 hexahydrate and amorphous CaCO 3 ( Rodriguez-Navarro et al, 2012 ; Murugan et al, 2021 ). The shape and size of CaCO 3 crystal changes during the precipitation process under different physico-chemical conditions and in association with different microbial communities ( Wilby et al, 1996 ; O'Brien et al, 2002 ; Raff et al, 2008 ; Dhami et al, 2012 ; Raff and Raff, 2014 ; Plet et al, 2016 ; Zhu and Dittrich, 2016 ; Iniesto et al, 2018 ; Grice et al, 2019 ; Dubey et al, 2022 ; Murugan et al, 2022 ). The major factors responsible for microbially induced concretion precipitation include the concentration of calcium, concentration of DIC, pH, and the availability of nucleation sites ( Hammes and Verstraete, 2002 ; Dhami et al, 2013b ; Murugan et al, 2021 ).…”