The fraction of CO32 − in DIC (CO32 − fraction, for short) under all the experimental conditions was calculated from pH and DIC by using CO2SYS (Pierrot et al., 2006). The results of CO2SYS are not reliable for the calculation of the CO2 system at high salinities because

the functional expressions for the equilibrium constants are based on measurements over a limited range of salinities and temperatures. Here, we chose two sets of carbonate equilibrium constants, one from Mehrbach et al. (1973) as refitted by Dickson and Millero (1987) (referred to as constants_a), and the other one from Millero (2010) (referred to as constants_b), to evaluate the sensitivity of the calculated CO32 − fraction to uncertainties in the magnitude of the equilibrium constants. Depsipeptide The remaining parameters were the same: KHSO4− was from Dickson (1990); [B]T HSP inhibition value was from Uppström (1974) and the pHNBS scale was applied. The input parameters for the CO2 system calculation were consistent with the experimental conditions except that the DIC was fixed at 2000 μmol kg− 1 for each run, since the change in DIC concentration does not affect the CO32 − fraction calculation. According to the vibration ν1 and ν4 of CO32 −, two types of Raman spectra were distinguished in this study. After a comparison with the available references (Behrens

et al., 1995 and Tlili et al., 2001), ikaite was identified by the vibrational modes ν1 (1071 cm− 1) and ν4 (718 cm− 1), Morin Hydrate and vaterite was identified by the two doublets of the vibration modes ν1 (1075 cm− 1, 1090 cm− 1) and ν4 (742 cm− 1, 752 cm− 1). In ASW, according to the Raman measurements (Fig. 3a), ikaite is the only calcium carbonate polymorph precipitated at pH ranging from 8.5 to 10.0, salinities from 0 to 105, temperatures from 0 to − 4 °C and PO4 concentrations from 0 to 50 μmol kg− 1. The morphology of ikaite crystals

precipitated from ASW is similar under all the conditions, with an average crystal size of approximately 20 μm (Fig. 3b). The morphology resembles that of natural ikaite crystals found in sea ice (Rysgaard et al., 2013), however, crystals in our study are generally smaller. In the NaCl medium, and the presence of 10 μmol kg− 1 PO4, according to the Raman measurements (Fig. 3c), ikaite is the only precipitate in the salinity range from 0 to 105. The crystal size is similar to the one observed for the crystals precipitated from ASW. However, the morphology of ikaite crystals differs (Fig. 3d). In the absence of PO4 and the same salinity range, vaterite (see Raman spectrum given in Fig. 3e) is the dominant calcium carbonate polymorph precipitated and only few ikaite crystals were observed. The small spherical crystals shown in Fig.