Soda Lakes. Table 3 List of modern soda lakes with CaCO3 precipitation in comparison with modern oceanic conditions
From: Soda Lakes
Site | Minerals dominating | Saturation index | Kind of CaCO3 precipitate | Source |
---|---|---|---|---|
North Sea 1986 | Calcite | 0.375–0.904 Cc mean of 122 samples: 0.567 | Biomineralization of coccolithophorids | Pegler and Kempe, 1988 |
Bahamas banks | Aragonite | 0.47–0.6 Ara | Extremely low rates (if any) of aragonite (not the reason of whitings) | Morse et al., 2002 |
Satonda crater lake | Aragonite, Calcite | 0.98Â Cc, 0.84Â Ara | Biomineralization by red algae and cyanobacterial sheaths permineralization | |
Lake Van | Aragonite, Calcite | 1.14 at 0 m to 1.06 at 440 m Cc, 0.99–0.91 Ara 4.09–3.81 Dol | Permineralization of cyanobacterial sheaths, inorganic chemical gardens, river plume whiting, summer whitings | Kempe et al., 1991; Reimer, 1995; Kazmierczak et al., 2004; Reimer et al., 2008 |
Lake Tanganyika | High-Mg Calcite | 0.96Â Cc | Five zones of massive thrombolites down to 50 m | Kempe and Kazmierczak, 1990 and citations therein |
Andros Island | Low-Mg Calcite | Upon degassing and evaporation 1.14Â Cc | Inland lakes with weakly calcified cyanobacterial and algal mats | Same as above |
Walker Lake | Low-Mg Calcite | 1.11Â Cc, 0.95Â Ara, 3.90Â Dol | Small cabbage-like stromatolites up to 4Â cm high, built by filamentous green alga and oscillatorian and coccoidal cyanobacteria. | Same as above; Kempe and Kazmierczak, 1997 |
Mono Lake Figure 2 top | Aragonite (Ikaite) | 1.24Â Cc, 1.09Â Ara, 3.74Â Dol | Large tufa columns at former groundwater outlets | |
Pyramid Lake Figure 2 bottom | Calcite | 1.36Â Cc, 1.21Â Ara, 3.89Â Dol | Huge towers and mounds at former groundwater outlets | |
Niuafo‘ou, crater lake | Aragonite | 0.65 Cc, 0.50 Ara, 2.65 Dol | Head-like stromatolites built by coccoid and filamentous cyanobacteria | Kazmierczak and Kempe, 2006 |
Kauhako crater lake | Calcite | 0.97Â Cc, 0.82Â Ara | Calcified sheaths of filamentous cyanobacteria | Kempe, unpublished |