- Gypsum appears in caves on the Nullarbor Plain
- δ34S of gypsum shows relatively high positive δ34S values
- Cave sulphate minerals are evaporates
Large deep caves with little relation to surface topography are distinctive karst features on the Nullarbor Plain of Australia. The presence of gypsum deposits and chemoautotrophic bacteria within the caves have been suggested as evidence for cave formation and (or) enlargement via sulfuric acid speleogenesis. To test this hypothesis, the stable sulfur isotope compositions (δ34S) of both cave gypsum and surface gypsum were measured. Analyses yielded relatively high, positive δ34S values from both cave gypsum and surface gypsum, arguing against gypsum genesis via microbial chemoautotrophy, and more broadly, sulfuric acid speleogenesis. Instead, the gypsum is interpreted as forming via evaporation of seawater during the Quaternary.
Creative Commons License
This work is licensed under a Creative Commons Attribution-Noncommercial 4.0 License
Lipar, Matej; Mateja Ferk; Sonja Lojen; and Milo Barham.
Sulfur (34S/32S) isotope composition of gypsum and implications for deep cave formation on the Nullarbor Plain, Australia.
International Journal of Speleology,
Available at: https://scholarcommons.usf.edu/ijs/vol48/iss1/1