Oxfordian microbial laminites from La Manga Formation, Neuquén Basin, Argentina: Remarkable nanobacteria preservation

Exceptionally preserved stromatolites have been found in the shallow marine carbonate facies of the Callovian-Oxfordian La Manga Formation, in the Neuquén Basin (Argentina). The stromatolites exhibit planar and crinkle lamination, often disrupted by sheet-cracks, mudcracks, and fenestral structures,...

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Autores principales: Palma, R.M., Kietzmann, D.A., Comerio, M., Martín-Chivelet, J., López-Gómez, J., Bressan, G.S.
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_16986180_v41_n3_p351_Palma
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spelling todo:paper_16986180_v41_n3_p351_Palma2023-10-03T16:30:10Z Oxfordian microbial laminites from La Manga Formation, Neuquén Basin, Argentina: Remarkable nanobacteria preservation Palma, R.M. Kietzmann, D.A. Comerio, M. Martín-Chivelet, J. López-Gómez, J. Bressan, G.S. Argentina Jurassic Nanobacteria Neuquén basin Stromatolite bacterium biofacies body size depositional environment fossil record Jurassic lamination metabolism nanofossil preservation pyrite stromatolite Argentina Neuquen Basin Exceptionally preserved stromatolites have been found in the shallow marine carbonate facies of the Callovian-Oxfordian La Manga Formation, in the Neuquén Basin (Argentina). The stromatolites exhibit planar and crinkle lamination, often disrupted by sheet-cracks, mudcracks, and fenestral structures, which indicate periodic subaerial exposure. These and other evidences suggest that these stromatolites grew in low energy upper intertidal to lower supratidal environments. They consist of fine micrite/microsparite crystal fabrics (with a remarkable lack of allochems) that define submillimiter alternations of dense laminae. Extensive SEM examinations of polished samples of the stromatolites reveal exceptional preservation of rod-shaped bacteria, coccoid like microorganisms, and abundant aggregates of framboidal pyrite. The rod-like bacteria consists of a network of irregular distributed filaments, which range from 150 nm to an uncommon 640 nm in length; diameters range from 54 nm to 90 nm. Subspherical bodies range in size between 70 and 89 nm. The presence of abundant framboidal pyrites is interpreted as the result of the metabolic activity of sulfate–reducing bacteria and decay of organic matter. © 2015, Universidad Complutense de Madrid. All Rights Reserved. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_16986180_v41_n3_p351_Palma
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Argentina
Jurassic
Nanobacteria
Neuquén basin
Stromatolite
bacterium
biofacies
body size
depositional environment
fossil record
Jurassic
lamination
metabolism
nanofossil
preservation
pyrite
stromatolite
Argentina
Neuquen Basin
spellingShingle Argentina
Jurassic
Nanobacteria
Neuquén basin
Stromatolite
bacterium
biofacies
body size
depositional environment
fossil record
Jurassic
lamination
metabolism
nanofossil
preservation
pyrite
stromatolite
Argentina
Neuquen Basin
Palma, R.M.
Kietzmann, D.A.
Comerio, M.
Martín-Chivelet, J.
López-Gómez, J.
Bressan, G.S.
Oxfordian microbial laminites from La Manga Formation, Neuquén Basin, Argentina: Remarkable nanobacteria preservation
topic_facet Argentina
Jurassic
Nanobacteria
Neuquén basin
Stromatolite
bacterium
biofacies
body size
depositional environment
fossil record
Jurassic
lamination
metabolism
nanofossil
preservation
pyrite
stromatolite
Argentina
Neuquen Basin
description Exceptionally preserved stromatolites have been found in the shallow marine carbonate facies of the Callovian-Oxfordian La Manga Formation, in the Neuquén Basin (Argentina). The stromatolites exhibit planar and crinkle lamination, often disrupted by sheet-cracks, mudcracks, and fenestral structures, which indicate periodic subaerial exposure. These and other evidences suggest that these stromatolites grew in low energy upper intertidal to lower supratidal environments. They consist of fine micrite/microsparite crystal fabrics (with a remarkable lack of allochems) that define submillimiter alternations of dense laminae. Extensive SEM examinations of polished samples of the stromatolites reveal exceptional preservation of rod-shaped bacteria, coccoid like microorganisms, and abundant aggregates of framboidal pyrite. The rod-like bacteria consists of a network of irregular distributed filaments, which range from 150 nm to an uncommon 640 nm in length; diameters range from 54 nm to 90 nm. Subspherical bodies range in size between 70 and 89 nm. The presence of abundant framboidal pyrites is interpreted as the result of the metabolic activity of sulfate–reducing bacteria and decay of organic matter. © 2015, Universidad Complutense de Madrid. All Rights Reserved.
format JOUR
author Palma, R.M.
Kietzmann, D.A.
Comerio, M.
Martín-Chivelet, J.
López-Gómez, J.
Bressan, G.S.
author_facet Palma, R.M.
Kietzmann, D.A.
Comerio, M.
Martín-Chivelet, J.
López-Gómez, J.
Bressan, G.S.
author_sort Palma, R.M.
title Oxfordian microbial laminites from La Manga Formation, Neuquén Basin, Argentina: Remarkable nanobacteria preservation
title_short Oxfordian microbial laminites from La Manga Formation, Neuquén Basin, Argentina: Remarkable nanobacteria preservation
title_full Oxfordian microbial laminites from La Manga Formation, Neuquén Basin, Argentina: Remarkable nanobacteria preservation
title_fullStr Oxfordian microbial laminites from La Manga Formation, Neuquén Basin, Argentina: Remarkable nanobacteria preservation
title_full_unstemmed Oxfordian microbial laminites from La Manga Formation, Neuquén Basin, Argentina: Remarkable nanobacteria preservation
title_sort oxfordian microbial laminites from la manga formation, neuquén basin, argentina: remarkable nanobacteria preservation
url http://hdl.handle.net/20.500.12110/paper_16986180_v41_n3_p351_Palma
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