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Earlandite (TL)  | | Ca | | [CH | | (COO)-CHOH(COO)-CH | | (COO)] | | · 4H | | O |
| | | Type Locality: | 71°22'S; 16°34'W, Weddell Sea, Western Antarctica, Antarctica | | Description: | Occurs in ocean bottom sediments. | | Reference: | [Palache, C., Berman, H., & Frondel, C. (1951), The System of Mineralogy of James Dwight Dana and Edward Salisbury Dana, Yale University 1837-1892, Volume II: 1106.] |
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Gypsum  | | | | Reference: | [Bannister, F. A., Hey, M. H.: Report on some crystalline compounds of the Weddell Sea deposits. Discovery reports, 1936, Vol. 13, s. 60 - 69.] |
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Ikaite  | | | | Description: | In sea ice. | | Reference: | [Dieckmann, G. S., Nehrke, G., Papadimitriou, S., Göttlicher, J., Steininger, R., Kennedy, H., Wolf-Gladrow, D., and Thomas, D. N. (2008): Calcium carbonate as ikaite crystals in Antarctic sea ice. Geophys. Res. Lett., 35, L08501.] |
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Weddellite (TL)  | | | | Type Locality: | Weddell Sea, Western Antarctica, Antarctica | | Description: | Occurs as isolated crystakls in bottom muds. | | Reference: | [Palache, C., Berman, H., & Frondel, C. (1951), The System of Mineralogy of James Dwight Dana and Edward Salisbury Dana, Yale University 1837-1892, Volume II: 1102.] |
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