0000000000282782

AUTHOR

Cristina Carbone

showing 4 related works from this author

New insights on secondary minerals from Italian sulfuric acid caves

2018

Sulfuric acid minerals are important clues to identify the speleogenetic phases of hypogene caves. Italy hosts ~25% of the known worldwide sulfuric acid speleogenetic (SAS) systems, including the famous well-studied Frasassi, Monte Cucco, and Acquasanta Terme caves. Nevertheless, other underground environments have been analyzed, and interesting mineralogical assemblages were found associated with peculiar geomorphological features such as cupolas, replacement pockets, feeders, sulfuric notches, and sub-horizontal levels. In this paper, we focused on 15 cave systems located along the Apennine Chain, in Apulia, in Sicily, and in Sardinia, where copious SAS minerals were observed. Some of the…

010504 meteorology & atmospheric sciencesHypogeneQH301-705.5cave minerals speleothem sulfuric acid cave secondary mineralsSettore GEO/04 - Geografia Fisica E GeomorfologiahypogeneGeochemistrySpeleothem010502 geochemistry & geophysics01 natural scienceschemistry.chemical_compoundCavesulfuric acid caverising watersBiology (General)speleothem0105 earth and related environmental sciencesEarth-Surface Processescave mineralsgeographyCave sulfateSettore GEO/06 - MineralogiaQE1-996.5geography.geographical_feature_categorycave sulfatesSulfuric acidRising waterGeologyhypogene rising waters Apennine Chain mineralogy cave sulfateschemistryApennine Chainmineralogysecondary mineralsGeologyInternational Journal of Speleology
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Secondary minerals from salt caves in the Atacama Desert (Chile): a hyperarid and hypersaline environment with potential analogies to the Martian sub…

2017

Over the past 15 years several expeditions by French, American and especially Italian cavers have unveiled over 50 caves in the Cordillera de la Sal (Atacama Desert, Northern Chile). Many of these caves contain a variety of speleothems and minerals, some of which have rarely been observed within karst systems. Most of the secondary deposits in these caves are composed of halite, but also other halide, carbonate, sulphate, nitrate, phosphate, and silicate minerals have been found. Among the sixteen cave mineral species recognized, atacamite, darapskite, blödite, leonite, anhydrite, and especially antarcticite are worth mentioning. In one of the samples an unknown Ca-Sr-bearing chloride miner…

010504 meteorology & atmospheric sciencesQH301-705.5Settore GEO/04 - Geografia Fisica E GeomorfologiaEarth scienceSalt (chemistry)martian010502 geochemistry & geophysics01 natural sciencesAstrobiologyatacamaCaveminerogenesisMinerogenesiBiology (General)Hyperaridity0105 earth and related environmental sciencesEarth-Surface Processescave mineralschemistry.chemical_classificationMartianQE1-996.5Settore GEO/06 - Mineralogiageographygeography.geographical_feature_categoryDesert (philosophy)Mars analoguesMars analogueCave mineralGeologysalt cavescave minerals atacama martianchemistrySalt cavecave minerals salt caves hyperaridity minerogenesis Mars analoguesGeologyInternational Journal of Speleology
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Guano-related phosphate-rich minerals in European caves

2019

International audience; Guano is a typical deposit found in caves derived from the excretions of bats and in minor cases of birds. These organic deposits decompose and form a series of acid fluids and gases that can interact with the minerals, sediments, and rocks present in the cave. Over sixty phosphates are known and described from caves, but guano decay also often leads to the formation of nitrates and sulfates. In this study twenty-two European caves were investigated for their guano-related secondary minerals. Using various analytical techniques, seventeen phosphates, along with one sulfate (gypsum), were recognized as secondary products of guano decay. Among those minerals, some are …

phosphatesGypsum010504 meteorology & atmospheric sciencesQH301-705.5Settore GEO/04 - Geografia Fisica E GeomorfologiaGeochemistrybat guanocave minerals phosphate bat guanoengineering.material010502 geochemistry & geophysics01 natural sciencessecondary cave mineralsApatitechemistry.chemical_compoundCavesecondary cave minerals phosphates minerogenesis limestone caves bat guanominerogenesisBiology (General)Sulfatelimestone cavephosphate0105 earth and related environmental sciencesEarth-Surface Processescave mineralsQE1-996.5geographygeography.geographical_feature_categoryMineralSettore GEO/07 - Petrologia E PetrografiaGeology15. Life on landPhosphatehumanitiessecondary cave mineralchemistryminerogenesivisual_artlimestone cavesGuanoengineeringvisual_art.visual_art_mediumPyrite[SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/Mineralogy
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Secondary minerals from halite caves in the Atacama Desert (Chile)

2017

In the past 15 years several expeditions by French, American and especially Italian cavers have surveyed over 15 km of salt cave passages in the Cordillera de la Sal, close to San Pedro de Atacama village (Atacama Desert, Northern Chile). Over 50 caves have been explored up to now at an elevation around 2,500 m asl. These karst systems are characterized by in-cave temperature of around 17 °C and a relative humidity always very low, with a maximum of 15%. This extreme aridity is due to the severe conditions of the area with only a couple millimeters annual rainfall and several years without rain. Currently the rare precipitation events are enough to allow the dissolution of the salt rock and…

Settore GEO/06 - MineralogiaSettore GEO/04 - Geografia Fisica E GeomorfologiaKarstsalt karst sulphates halides speleothems minerogenesis
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