Biomineralization of endolithic microbes in rocks from the McMurdo Dry Valleys of Antarctica: implications for microbial fossil formation and their detection

10 páges, and photos. In some zones of Antarctica’s cold and dry desert, the extinction of cryptoendolithic microorganisms leaves behind inorganic traces of microbial life. In this paper, we examine the transition from live microorganisms, through their decay, to microbial fossils using in situ micr...

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Main Authors: Wierzchos, Jacek, García Sancho, Leopoldo, Ascaso, Carmen
Format: Article in Journal/Newspaper
Language:English
Published: Blackwell Publishing 2005
Subjects:
Online Access:http://hdl.handle.net/10261/17080
https://doi.org/10.1111/j.1462-2920.2004.00725.x
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author Wierzchos, Jacek
García Sancho, Leopoldo
Ascaso, Carmen
author_facet Wierzchos, Jacek
García Sancho, Leopoldo
Ascaso, Carmen
author_sort Wierzchos, Jacek
collection Digital.CSIC (Spanish National Research Council)
description 10 páges, and photos. In some zones of Antarctica’s cold and dry desert, the extinction of cryptoendolithic microorganisms leaves behind inorganic traces of microbial life. In this paper, we examine the transition from live microorganisms, through their decay, to microbial fossils using in situ microscopy (transmission electron microscopy, scanning electron microscopy in back-scattered electron mode) and microanalytical (energy dispersive X-ray spectroscopy) techniques. Our results demonstrate that, after their death, endolithic microorganisms inhabiting Commonwealth Glacier sandstone from the Antarctica McMurdo Dry Valleys become mineralized. In some cases, epicellular deposition of minerals and/ or simply filling up of empty moulds by minerals leads to the formation of cell-shaped structures that may be considered biomarkers. The continuous deposition of allochthonous clay minerals and sulfate-rich salts fills the sandstone pores. This process can give rise to microbial fossils with distinguishable cell wall structures. Often, fossilized cell interiors were of a different chemical composition to the mineralized cell walls. We propose that the microbial fossil formation observed was induced by mineral precipitation resulting from inorganic processes occurring after the death of cryptoendolithic microorganisms. Nevertheless, it must have been the organic template that provoked the diffusion of mineral elements and gave rise to their characteristic distribution pattern inside the fossilized cells. Peer reviewed
format Article in Journal/Newspaper
genre Antarc*
Antarctica
Commonwealth Glacier
McMurdo Dry Valleys
genre_facet Antarc*
Antarctica
Commonwealth Glacier
McMurdo Dry Valleys
geographic Commonwealth Glacier
McMurdo Dry Valleys
geographic_facet Commonwealth Glacier
McMurdo Dry Valleys
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language English
long_lat ENVELOPE(163.317,163.317,-77.583,-77.583)
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op_doi https://doi.org/10.1111/j.1462-2920.2004.00725.x10.1111/j.1462-2920.2005.00725.x
op_relation http://dx.doi.org/10.1111/j.1462-2920.2005.00725.x
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op_rights none
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publisher Blackwell Publishing
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spelling ftcsic:oai:digital.csic.es:10261/17080 2025-03-16T15:16:38+00:00 Biomineralization of endolithic microbes in rocks from the McMurdo Dry Valleys of Antarctica: implications for microbial fossil formation and their detection Wierzchos, Jacek García Sancho, Leopoldo Ascaso, Carmen 2005 725417 bytes application/pdf http://hdl.handle.net/10261/17080 https://doi.org/10.1111/j.1462-2920.2004.00725.x en eng Blackwell Publishing http://dx.doi.org/10.1111/j.1462-2920.2005.00725.x http://hdl.handle.net/10261/17080 none Biomineralization Endolithic microbes in rocks Microbial fossil artículo http://purl.org/coar/resource_type/c_6501 2005 ftcsic https://doi.org/10.1111/j.1462-2920.2004.00725.x10.1111/j.1462-2920.2005.00725.x 2025-02-18T02:04:31Z 10 páges, and photos. In some zones of Antarctica’s cold and dry desert, the extinction of cryptoendolithic microorganisms leaves behind inorganic traces of microbial life. In this paper, we examine the transition from live microorganisms, through their decay, to microbial fossils using in situ microscopy (transmission electron microscopy, scanning electron microscopy in back-scattered electron mode) and microanalytical (energy dispersive X-ray spectroscopy) techniques. Our results demonstrate that, after their death, endolithic microorganisms inhabiting Commonwealth Glacier sandstone from the Antarctica McMurdo Dry Valleys become mineralized. In some cases, epicellular deposition of minerals and/ or simply filling up of empty moulds by minerals leads to the formation of cell-shaped structures that may be considered biomarkers. The continuous deposition of allochthonous clay minerals and sulfate-rich salts fills the sandstone pores. This process can give rise to microbial fossils with distinguishable cell wall structures. Often, fossilized cell interiors were of a different chemical composition to the mineralized cell walls. We propose that the microbial fossil formation observed was induced by mineral precipitation resulting from inorganic processes occurring after the death of cryptoendolithic microorganisms. Nevertheless, it must have been the organic template that provoked the diffusion of mineral elements and gave rise to their characteristic distribution pattern inside the fossilized cells. Peer reviewed Article in Journal/Newspaper Antarc* Antarctica Commonwealth Glacier McMurdo Dry Valleys Digital.CSIC (Spanish National Research Council) Commonwealth Glacier ENVELOPE(163.317,163.317,-77.583,-77.583) McMurdo Dry Valleys
spellingShingle Biomineralization
Endolithic microbes in rocks
Microbial fossil
Wierzchos, Jacek
García Sancho, Leopoldo
Ascaso, Carmen
Biomineralization of endolithic microbes in rocks from the McMurdo Dry Valleys of Antarctica: implications for microbial fossil formation and their detection
title Biomineralization of endolithic microbes in rocks from the McMurdo Dry Valleys of Antarctica: implications for microbial fossil formation and their detection
title_full Biomineralization of endolithic microbes in rocks from the McMurdo Dry Valleys of Antarctica: implications for microbial fossil formation and their detection
title_fullStr Biomineralization of endolithic microbes in rocks from the McMurdo Dry Valleys of Antarctica: implications for microbial fossil formation and their detection
title_full_unstemmed Biomineralization of endolithic microbes in rocks from the McMurdo Dry Valleys of Antarctica: implications for microbial fossil formation and their detection
title_short Biomineralization of endolithic microbes in rocks from the McMurdo Dry Valleys of Antarctica: implications for microbial fossil formation and their detection
title_sort biomineralization of endolithic microbes in rocks from the mcmurdo dry valleys of antarctica: implications for microbial fossil formation and their detection
topic Biomineralization
Endolithic microbes in rocks
Microbial fossil
topic_facet Biomineralization
Endolithic microbes in rocks
Microbial fossil
url http://hdl.handle.net/10261/17080
https://doi.org/10.1111/j.1462-2920.2004.00725.x