Abstract
Sulfur-rich karst springs that drain middle to Late Cretaceous carbonates in southern Tabasco, Mexico, contain elevated total dissolved solids with high chloride and either high sulfide or sulfate. The mostly meteoric waters circulate along intermediate-depth flow paths, interacting with Jurassic evaporites and then mixing with shallow-circulating rainwater to produce brackish, sulfur- and NaCl-rich spring waters. Several caves, notably Cueva de Villa Luz and Cueva de Luna Azufre near Tapijulapa, are developing from these waters. Both are fed by small, warm subterranean springs that release hydrogen sulfide and carbon dioxide at the water–air interface. These gases combine with water vapor in the air and moisture on cave walls to form acidic solutions, which enlarge the cave passages. Speleogenesis is aided by abundant chemoautotrophic microbes that facilitate oxidation and the production of acid solutions. Cave walls and ceilings display several distinctive colonies of these microbes, notably filamentous bundles (snottites) and biovermiculations. The organisms also reside in unusual mineral deposits, including sulfur folia, sulfur crusts, and gypsum paste. Pore fluids in these deposits and growths have very low pH despite their proximity to limestone walls. Speleogenesis appears to follow a three-step process: (1) an early sulfide-rich phreatic phase; (2) a sulfide-rich, vadose–phreatic phase of chemical alteration and mechanical stoping; and (3) a tertiary sulfide-depleted phase of epigenic speleogenesis. The second phase of development dominates speleogenesis in Cuevas de Villa Luz and Luna Azufre.
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Acknowledgements
The authors wish to thank the people and officials of the Tapijulapa community, the authorities from the Municipio de Tacotalpa, Teapa, and Ixtapangajovya for their generous support and kindness. LDH’s research was financially supported by grants from the National Speleological Foundation, Richmond Area Speleological Society, and National Geographic Society grants 6541-99, and 6634-9. LR-L’s research was supported by Consejo Nacional de Ciencia y TecnologÃa, the National Cave and Karst Research Institute, the Matuszeski Grant, the Anita and Anton Budding Research Grant, and the Graduate Student Association Travel Grant from New Mexico Institute of Mining and Technology. The authors benefitted from assistance from members of the National Speleological Society’s Caves of Tabasco Project, especially from Jim Pisarowicz and Vickie Siegel. The personnel from PEMEX Exploración y Producción Zona Sur, especially Dr. Javier Meneses-Rocha, granted access to geologic information and oil wells. Consejo Nacional del Agua Villahermosa, Instituto Nacional de EstadÃstica y GeografÃa, and the SecretarÃa de Agua Potable y Alcantarillado del Estado de Tabasco also provided useful information.
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Hose, L.D., Rosales-Lagarde, L. (2017). Sulfur-Rich Caves of Southern Tabasco, Mexico. In: Klimchouk, A., N. Palmer, A., De Waele, J., S. Auler, A., Audra, P. (eds) Hypogene Karst Regions and Caves of the World. Cave and Karst Systems of the World. Springer, Cham. https://doi.org/10.1007/978-3-319-53348-3_54
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