Bubble trail and folia in cenote Zapote, Mexico: petrographic evidence for abiotic precipitation driven by CO2 degassing below the water table

• Published in: International journal of speleology Vol. 49; no. 3; pp. 173 - 186
• Main Authors: López-Martínez, Rafael, Gázquez, Fernando, Calaforra, José, Audra, Philippe, Bigot, Jean, Pi Puig, Teresa, Alcántara-Hernández, Rocío, Navarro, Ángel, Crochet, Philippe, Corona Martínez, Liliana, Daza Brunet, Raquel
• Format: Journal Article
• Language: English
• Published: Bologna University of South Florida Board of Trustees, a public body corporate, having locations in Tampa, St. Petersburg, and Sarasota 01.09.2020; University of South Florida Libraries
• Subjects: Abiotic factors; Bells; bubble trails; Bubbles; Calcite; Calcium carbonate; Carbon dioxide; Carbonates; Caves; cenote; Chemical precipitation; Cold water; Cupolas; Degassing; Fabrics; folia; Fungi; Geochemistry; Groundwater table; Halocline; hells bells; Hydrogen sulfide; karst; Laboratories; Mineralogy; Sinkholes; speleothems; Underwater; underwater caves; Water masses; Water table; Water temperature; Frisia; Mexico
• ISSN: 0392-6672; 1827-806X
• DOI: 10.5038/1827-806X.49.3.2344

Folia are speleothems that resemble bells, inverted cups, or bracket fungi, and whose origins are still controversial. Cenote Zapote (an underwater cave) in the Yucatán Peninsula (México), is home to some of the largest folia reported to date. These speleothems are currently growing in an active underwater system, meaning this site offers an excellent opportunity to constrain the different formation models proposed for folia, which have traditionally relied on inactive examples. In Cenote Zapote, folia are closely related to bubble trails and cupolas, suggesting an underwater CO2-degassing process. In thin section, they display a succession of columnar-open and columnar-elongated endings in micrite-dendritic fabrics. Our petrographic and geochemical results demonstrate the abiotic origin of these folia and indicate carbonate precipitation from cold water by CO2 degassing below the water table that started at least 5,210 yrs BP. We conclude that these folia formed as a result of subaqueous calcite precipitation around CO2 bubbles trapped below overhanging walls of the cave. The sequential alternation of columnar and micritic fabrics can be explained by changes in the position of the halocline and H2S-rich water mass while the exceptional size is the result of carbonate precipitation from waters saturated in CaCO3 during thousans of years. Then we propose the classification of these speleothems as a subtype of folia. This subtype could be named Hells Bells, respecting its original description.