Endostromatolites: Life in extreme environments and lessons for the detection of life on Mars

Finely laminated carbonate columns---endostromatolites, grow in carbonate rock fissures in permafrost regions. Their formation is thought to be microbially mediated but the processes of accretion are thought to be very slow and possibly intertwined with abiotic mineralization processes. The samples...

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Main Author: Pellerin, Andre
Format: Thesis
Language:English
Published: Université d'Ottawa / University of Ottawa 2008
Subjects:
Online Access:https://dx.doi.org/10.20381/ruor-18794
http://www.ruor.uottawa.ca/handle/10393/27603
id ftdatacite:10.20381/ruor-18794
record_format openpolar
spelling ftdatacite:10.20381/ruor-18794 2023-05-15T15:08:47+02:00 Endostromatolites: Life in extreme environments and lessons for the detection of life on Mars Pellerin, Andre 2008 https://dx.doi.org/10.20381/ruor-18794 http://www.ruor.uottawa.ca/handle/10393/27603 en eng Université d'Ottawa / University of Ottawa Geology. Paleontology. Text Thesis article-journal ScholarlyArticle 2008 ftdatacite https://doi.org/10.20381/ruor-18794 2021-11-05T12:55:41Z Finely laminated carbonate columns---endostromatolites, grow in carbonate rock fissures in permafrost regions. Their formation is thought to be microbially mediated but the processes of accretion are thought to be very slow and possibly intertwined with abiotic mineralization processes. The samples analyzed in this study are from the Haughton impact structure, located on Devon Island, Nunavut in the Canadian high Arctic. The carbon and nitrogen isotopic composition of the endostromatolites, along will the microbial community diversity were determined. The delta13C and delta 15N of the organic matter contained within the endostromatolites averaged around -30‰ and 0‰, respectively. Scanning electron microscopy observations revealed the presence of spheroidal calcite and filamentous structures reminiscent of biological activity. Molecular phylogenetic analysis of the endostromatolites and soil samples found in Haughton crater showed that the endostromatolite microbial community is mostly aerobic and chemoheterotrophic, belonging in large part to the Phylum Actinobacteria and the subphylum Alphaproteobacteria. Rubrobacter radiotolerans was the dominant species in the endostromatolites. Soil bacterial communities were more diverse, harboring all the phyla found in the endostromatolites as well as many others which were not encountered in endostromatolites. Understanding the variability of microbial life between specific environments might shed some light on the mechanisms responsible for endostromatolite formation and provide useful data for contrasting abiotic and biotic systems on earth and other planetary bodies, such as Mars. Thesis Arctic Devon Island Nunavut permafrost DataCite Metadata Store (German National Library of Science and Technology) Arctic Devon Island ENVELOPE(-88.000,-88.000,75.252,75.252) Nunavut
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Geology.
Paleontology.
spellingShingle Geology.
Paleontology.
Pellerin, Andre
Endostromatolites: Life in extreme environments and lessons for the detection of life on Mars
topic_facet Geology.
Paleontology.
description Finely laminated carbonate columns---endostromatolites, grow in carbonate rock fissures in permafrost regions. Their formation is thought to be microbially mediated but the processes of accretion are thought to be very slow and possibly intertwined with abiotic mineralization processes. The samples analyzed in this study are from the Haughton impact structure, located on Devon Island, Nunavut in the Canadian high Arctic. The carbon and nitrogen isotopic composition of the endostromatolites, along will the microbial community diversity were determined. The delta13C and delta 15N of the organic matter contained within the endostromatolites averaged around -30‰ and 0‰, respectively. Scanning electron microscopy observations revealed the presence of spheroidal calcite and filamentous structures reminiscent of biological activity. Molecular phylogenetic analysis of the endostromatolites and soil samples found in Haughton crater showed that the endostromatolite microbial community is mostly aerobic and chemoheterotrophic, belonging in large part to the Phylum Actinobacteria and the subphylum Alphaproteobacteria. Rubrobacter radiotolerans was the dominant species in the endostromatolites. Soil bacterial communities were more diverse, harboring all the phyla found in the endostromatolites as well as many others which were not encountered in endostromatolites. Understanding the variability of microbial life between specific environments might shed some light on the mechanisms responsible for endostromatolite formation and provide useful data for contrasting abiotic and biotic systems on earth and other planetary bodies, such as Mars.
format Thesis
author Pellerin, Andre
author_facet Pellerin, Andre
author_sort Pellerin, Andre
title Endostromatolites: Life in extreme environments and lessons for the detection of life on Mars
title_short Endostromatolites: Life in extreme environments and lessons for the detection of life on Mars
title_full Endostromatolites: Life in extreme environments and lessons for the detection of life on Mars
title_fullStr Endostromatolites: Life in extreme environments and lessons for the detection of life on Mars
title_full_unstemmed Endostromatolites: Life in extreme environments and lessons for the detection of life on Mars
title_sort endostromatolites: life in extreme environments and lessons for the detection of life on mars
publisher Université d'Ottawa / University of Ottawa
publishDate 2008
url https://dx.doi.org/10.20381/ruor-18794
http://www.ruor.uottawa.ca/handle/10393/27603
long_lat ENVELOPE(-88.000,-88.000,75.252,75.252)
geographic Arctic
Devon Island
Nunavut
geographic_facet Arctic
Devon Island
Nunavut
genre Arctic
Devon Island
Nunavut
permafrost
genre_facet Arctic
Devon Island
Nunavut
permafrost
op_doi https://doi.org/10.20381/ruor-18794
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