Mobile mud layer underneath the desiccated maar lake of Rincon de Parangueo and insights into its microbial fingerprints


Por: Sanchez-Sanchez, Janet, Cerca, Mariano, Alcantara-Hernandez, Rocio J., Aranda-Gomez, Jose Jorge, Carreon-Freyre, Dora, Lozano-Flores, Carlos, Munoz-Velasco, Israel, Levresse, Gilles, Varela-Echavarria, Alfredo

Publicada: 1 dic 2021
Categoría: Geology

Resumen:
We surveyed a subsurface layer of saturated mobile mud and its microbial fingerprints below the desiccated bottom of a maar lake at Rincon de Parangueo (RP), Mexico. A multi-scale approach was followed using geological fieldwork, coring of the sediments, ground penetrating radar survey, physico-chemical characterization including X-ray diffraction and scanning electron microscope, and high-throughput DNA sequencing methods. The mobile mud is an organic-rich silty clay, with high values of alkalinity, volumetric water content and conductivity. Mud mobility has been attributed to overpressure caused by disequilibrium compaction of sediments related to active subsidence and pore overpressure produced by an input of groundwater and gas content in the sediments and resulted in a diverse set of structures related to mud tectonics such as injection domes and fluid seeps through fractures. Extraction and sequencing of sedimentary environmental DNA in the mud layer were performed for Bacteria and Archaea. Despite the small number of samples ob-tained, the microbial fingerprint from the sedimentary environmental DNA at subsurface shares similarities with the microbial communi-ties identified on the crater surface. Additionally, we identify the DNA of specific methanogenic microorganisms in the mud, such as Bathyarchaeia, Methanomassiliicoccales, and Methanobacteriales, and we speculate on their probable role in gas production and pore overpressure in the mud layer. The underground mud at Rincon de Parangueo represents a geologically dynamic environment with conditions that are favorable for the thriving of microbial communities.

Filiaciones:
Sanchez-Sanchez, Janet:
 Univ Nacl Autonoma Mexico, Ctr Geociencias, Posgrad Ciencias Tierra, Blvd Juriquilla 3001, Juriquilla 76230, Queretaro, Mexico

Cerca, Mariano:
 Univ Nacl Autonoma Mexico, Ctr Geociencias, Blvd Juriquilla 3001, Juriquilla 76230, Queretaro, Mexico

Alcantara-Hernandez, Rocio J.:
 Univ Nacl Autonoma Mexico, Inst Geol, Ciudad Univ,Av Univ 3000, Mexico City 04510, DF, Mexico

Aranda-Gomez, Jose Jorge:
 Univ Nacl Autonoma Mexico, Ctr Geociencias, Blvd Juriquilla 3001, Juriquilla 76230, Queretaro, Mexico

Carreon-Freyre, Dora:
 Univ Nacl Autonoma Mexico, Ctr Geociencias, Blvd Juriquilla 3001, Juriquilla 76230, Queretaro, Mexico

Lozano-Flores, Carlos:
 Univ Nacl Autonoma Mexico, Inst Neurobiol, Dept Biol Desarrollo & Neurofisiol, Queretaro, Mexico

Munoz-Velasco, Israel:
 Univ Nacl Autonoma Mexico, Fac Ciencias, Apdo Postal 70-407,Cd Univ, Mexico City 04510, DF, Mexico

Levresse, Gilles:
 Univ Nacl Autonoma Mexico, Ctr Geociencias, Blvd Juriquilla 3001, Juriquilla 76230, Queretaro, Mexico

Varela-Echavarria, Alfredo:
 Univ Nacl Autonoma Mexico, Inst Neurobiol, Dept Biol Desarrollo & Neurofisiol, Queretaro, Mexico
ISSN: 10268774
Editorial
CENTRO GEOCIENCIAS UNAM, CENTRO GEOCIENCIAS, UNAM, CAMPUS JURIQUILLA, QUERETARO, QRO 76230, MEXICO, México
Tipo de documento: Article
Volumen: 38 Número: 3
Páginas: 178-192
WOS Id: 000734090800003
imagen All Open Access; Gold

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