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Microbial role in N2O-NO2 production and CH4 oxidation under active hypogenic settings

Authors :
Martín-Pozas, Tamara
Cuezva, Soledad
Jurado, Valme
Pérez López, Raúl
Sáiz-Jiménez, Cesáreo
Calaforra, José María
Sánchez-Moral, Sergio
Fernández-Cortés, Ángel
Martín-Pozas, Tamara
Cuezva, Soledad
Jurado, Valme
Pérez López, Raúl
Sáiz-Jiménez, Cesáreo
Calaforra, José María
Sánchez-Moral, Sergio
Fernández-Cortés, Ángel
Publication Year :
2020

Abstract

The hydrothermal caves linked to active faulting have subterranean atmospheres with a distinctive gaseous composition containing deep endogenous gases, such as carbon dioxide, methane and nitrogen oxides (NOx). Ascending fluids through associated near-surface hydrothermal processes can mobilize endogenous gases into the Critical Zone and, ultimately, to the lower troposphere. Nitrogen oxides are polluting gases and can have adverse effects on human health, especially inhaled NO2. They also catalyse ozone (O3) production in the lower layers of the atmosphere and the greenhouse effect, when they react with volatile organic compounds. The largest source of NOx emissions is anthropogenic. The rest is produced naturally by microbial processes in soil and water, by lightning, volcanic activity, storms, etc. Production of N2O and NO2 is associated with soil and other active-geothermal ecosystems, far less is known about the sources and sinks of these gases within subterranean locations. Here, we report high N2O and NO2 concentrations detected along a hypogenic system associated with an active faulting (Vapour Cave, southern Spain), which enables direct gas exchange with the low-atmosphere. These anomalous concentrations of N2O and, NO2 are about ten and five times higher than the typical atmospheric background, respectively. Gaseous composition analyses of subterranean atmosphere were conducted by high precision field-deployable CRDS and FTIR spectrometers for measuring in situ the target tracer gases (NO2, N2O, CH4, CO2) and ¿13C of both carbon-GHGs. DNA extraction, sequencing and phylogenetic analyses were conducted to characterize the microbial community of cave sediments. The results showed that N2O and NO2 emission depends on the activity of nitrification by ammonia oxidizing microorganisms (such as members of the family Nitrosomonadaceae and phylum Thaumarchaeota) and/or as a result of incomplete denitrification by heterotrophic denitrifying bacteria (such as Bacillu

Details

Database :
OAIster
Publication Type :
Electronic Resource
Accession number :
edsoai.on1286566995
Document Type :
Electronic Resource