CUEVA DE VILLA LUZ, TABASCO, MEXICO: RECONNAISSANCE STUDY OF AN ACTIVE SULFUR SPRING CAVE AND ECOSYSTEM
Cueva de Villa Luz (a.k.a. Cueva de las Sardinas) in Tabasco, Mexico, is a stream cave with over a dozen H2S-rich springs rising from the floor. Oxidation of the H2S in the stream results in abundant, suspended elemental sulfur in the stream, which is white and nearly opaque. Hydrogen sulfide concen...
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ftusouthflorida:oai:digitalcommons.usf.edu:kip_articles-2258 2023-08-15T12:40:55+02:00 CUEVA DE VILLA LUZ, TABASCO, MEXICO: RECONNAISSANCE STUDY OF AN ACTIVE SULFUR SPRING CAVE AND ECOSYSTEM Hose, Louise D. Pisarowicz, James A. 1999-04-01T08:00:00Z application/pdf https://digitalcommons.usf.edu/kip_articles/1259 https://digitalcommons.usf.edu/context/kip_articles/article/2258/viewcontent/K26_00076_cave_61_01_fullr.pdf unknown Digital Commons @ University of South Florida https://digitalcommons.usf.edu/kip_articles/1259 https://digitalcommons.usf.edu/context/kip_articles/article/2258/viewcontent/K26_00076_cave_61_01_fullr.pdf KIP Articles text 1999 ftusouthflorida 2023-07-23T16:33:30Z Cueva de Villa Luz (a.k.a. Cueva de las Sardinas) in Tabasco, Mexico, is a stream cave with over a dozen H2S-rich springs rising from the floor. Oxidation of the H2S in the stream results in abundant, suspended elemental sulfur in the stream, which is white and nearly opaque. Hydrogen sulfide concentrations in the cave atmosphere fluctuate rapidly and often exceed U.S. government tolerance levels. Pulses of elevated carbon monoxide and depleted oxygen levels also occasionally enter the cave. Active speleogenesis occurs in this cave, which is forming in a small block of Lower Cretaceous limestone adjacent to a fault. Atmospheric hydrogen sulfide combines with oxygen and water to form sulfuric acid, probably through both biotic and abiotic reactions. The sulfuric acid dissolves the limestone bedrock and forms gypsum, which is readily removed by active stream flow. In addition, carbon dioxide from the reaction as well as the spring water and cave atmosphere combines with water. The resultant carbonic acid also dissolves the limestone bedrock. A robust and diverse ecosystem thrives within the cave. Abundant, chemoautotrophic microbial colonies are ubiquitous and apparently act as the primary producers to the cave’s ecosystem. Microbial veils resembling soda straw stalactites, draperies, and “u-loops” suspended from the ceiling and walls of the cave produce drops of sulfuric acid with pH values of <0.5-3.0 ±0.1. Copious macroscopic invertebrates, particularly midges and spiders, eat the microbes or the organisms that graze on the microbes. A remarkably dense population of fish, Poecilia mexicana, fill most of the stream. The fish mostly eat bacteria and midges. Participants in an ancient, indigenous Zoque ceremony annually harvest the fish in the spring to provide food during the dry season. Text Carbonic acid University of South Florida St. Petersburg: Digital USFSP Cueva ENVELOPE(-62.600,-62.600,-64.150,-64.150) |
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University of South Florida St. Petersburg: Digital USFSP |
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ftusouthflorida |
language |
unknown |
description |
Cueva de Villa Luz (a.k.a. Cueva de las Sardinas) in Tabasco, Mexico, is a stream cave with over a dozen H2S-rich springs rising from the floor. Oxidation of the H2S in the stream results in abundant, suspended elemental sulfur in the stream, which is white and nearly opaque. Hydrogen sulfide concentrations in the cave atmosphere fluctuate rapidly and often exceed U.S. government tolerance levels. Pulses of elevated carbon monoxide and depleted oxygen levels also occasionally enter the cave. Active speleogenesis occurs in this cave, which is forming in a small block of Lower Cretaceous limestone adjacent to a fault. Atmospheric hydrogen sulfide combines with oxygen and water to form sulfuric acid, probably through both biotic and abiotic reactions. The sulfuric acid dissolves the limestone bedrock and forms gypsum, which is readily removed by active stream flow. In addition, carbon dioxide from the reaction as well as the spring water and cave atmosphere combines with water. The resultant carbonic acid also dissolves the limestone bedrock. A robust and diverse ecosystem thrives within the cave. Abundant, chemoautotrophic microbial colonies are ubiquitous and apparently act as the primary producers to the cave’s ecosystem. Microbial veils resembling soda straw stalactites, draperies, and “u-loops” suspended from the ceiling and walls of the cave produce drops of sulfuric acid with pH values of <0.5-3.0 ±0.1. Copious macroscopic invertebrates, particularly midges and spiders, eat the microbes or the organisms that graze on the microbes. A remarkably dense population of fish, Poecilia mexicana, fill most of the stream. The fish mostly eat bacteria and midges. Participants in an ancient, indigenous Zoque ceremony annually harvest the fish in the spring to provide food during the dry season. |
format |
Text |
author |
Hose, Louise D. Pisarowicz, James A. |
spellingShingle |
Hose, Louise D. Pisarowicz, James A. CUEVA DE VILLA LUZ, TABASCO, MEXICO: RECONNAISSANCE STUDY OF AN ACTIVE SULFUR SPRING CAVE AND ECOSYSTEM |
author_facet |
Hose, Louise D. Pisarowicz, James A. |
author_sort |
Hose, Louise D. |
title |
CUEVA DE VILLA LUZ, TABASCO, MEXICO: RECONNAISSANCE STUDY OF AN ACTIVE SULFUR SPRING CAVE AND ECOSYSTEM |
title_short |
CUEVA DE VILLA LUZ, TABASCO, MEXICO: RECONNAISSANCE STUDY OF AN ACTIVE SULFUR SPRING CAVE AND ECOSYSTEM |
title_full |
CUEVA DE VILLA LUZ, TABASCO, MEXICO: RECONNAISSANCE STUDY OF AN ACTIVE SULFUR SPRING CAVE AND ECOSYSTEM |
title_fullStr |
CUEVA DE VILLA LUZ, TABASCO, MEXICO: RECONNAISSANCE STUDY OF AN ACTIVE SULFUR SPRING CAVE AND ECOSYSTEM |
title_full_unstemmed |
CUEVA DE VILLA LUZ, TABASCO, MEXICO: RECONNAISSANCE STUDY OF AN ACTIVE SULFUR SPRING CAVE AND ECOSYSTEM |
title_sort |
cueva de villa luz, tabasco, mexico: reconnaissance study of an active sulfur spring cave and ecosystem |
publisher |
Digital Commons @ University of South Florida |
publishDate |
1999 |
url |
https://digitalcommons.usf.edu/kip_articles/1259 https://digitalcommons.usf.edu/context/kip_articles/article/2258/viewcontent/K26_00076_cave_61_01_fullr.pdf |
long_lat |
ENVELOPE(-62.600,-62.600,-64.150,-64.150) |
geographic |
Cueva |
geographic_facet |
Cueva |
genre |
Carbonic acid |
genre_facet |
Carbonic acid |
op_source |
KIP Articles |
op_relation |
https://digitalcommons.usf.edu/kip_articles/1259 https://digitalcommons.usf.edu/context/kip_articles/article/2258/viewcontent/K26_00076_cave_61_01_fullr.pdf |
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1774293951500517376 |