Microbial trace-fossil formation, biogenous, and abiotic weathering in the Antarctic cold desert
In the Antarctic cold desert (Ross Desert), the survival of the cryptoendolithic microorganisms that colonize the near-surface layer of porous sandstone rocks depends on a precarious equilibrium of biological and geological factors. An unfavorable shift of this equilibrium results in death, and this...
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ftnasantrs:oai:casi.ntrs.nasa.gov:19870054166 2023-05-15T14:01:08+02:00 Microbial trace-fossil formation, biogenous, and abiotic weathering in the Antarctic cold desert Friedmann, E. Imre Weed, Rebecca Unclassified, Unlimited, Publicly available May 8, 1987 http://ntrs.nasa.gov/search.jsp?R=19870054166 unknown http://ntrs.nasa.gov/search.jsp?R=19870054166 Accession ID: 87A41440 Copyright Other Sources 55 Science; 236; 703-705 1987 ftnasantrs 2012-02-15T17:14:58Z In the Antarctic cold desert (Ross Desert), the survival of the cryptoendolithic microorganisms that colonize the near-surface layer of porous sandstone rocks depends on a precarious equilibrium of biological and geological factors. An unfavorable shift of this equilibrium results in death, and this may be followed by formation of trace fossils that preserve the characteristic iron-leaching pattern caused by microbial activity. Similar microbial trace fossils may exist in the geological record. If life ever arose on early Mars, similar processes may have occurred there and left recognizable traces. Other/Unknown Material Antarc* Antarctic NASA Technical Reports Server (NTRS) Antarctic The Antarctic |
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NASA Technical Reports Server (NTRS) |
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ftnasantrs |
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55 |
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55 Friedmann, E. Imre Weed, Rebecca Microbial trace-fossil formation, biogenous, and abiotic weathering in the Antarctic cold desert |
topic_facet |
55 |
description |
In the Antarctic cold desert (Ross Desert), the survival of the cryptoendolithic microorganisms that colonize the near-surface layer of porous sandstone rocks depends on a precarious equilibrium of biological and geological factors. An unfavorable shift of this equilibrium results in death, and this may be followed by formation of trace fossils that preserve the characteristic iron-leaching pattern caused by microbial activity. Similar microbial trace fossils may exist in the geological record. If life ever arose on early Mars, similar processes may have occurred there and left recognizable traces. |
format |
Other/Unknown Material |
author |
Friedmann, E. Imre Weed, Rebecca |
author_facet |
Friedmann, E. Imre Weed, Rebecca |
author_sort |
Friedmann, E. Imre |
title |
Microbial trace-fossil formation, biogenous, and abiotic weathering in the Antarctic cold desert |
title_short |
Microbial trace-fossil formation, biogenous, and abiotic weathering in the Antarctic cold desert |
title_full |
Microbial trace-fossil formation, biogenous, and abiotic weathering in the Antarctic cold desert |
title_fullStr |
Microbial trace-fossil formation, biogenous, and abiotic weathering in the Antarctic cold desert |
title_full_unstemmed |
Microbial trace-fossil formation, biogenous, and abiotic weathering in the Antarctic cold desert |
title_sort |
microbial trace-fossil formation, biogenous, and abiotic weathering in the antarctic cold desert |
publishDate |
1987 |
url |
http://ntrs.nasa.gov/search.jsp?R=19870054166 |
op_coverage |
Unclassified, Unlimited, Publicly available |
geographic |
Antarctic The Antarctic |
geographic_facet |
Antarctic The Antarctic |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_source |
Other Sources |
op_relation |
http://ntrs.nasa.gov/search.jsp?R=19870054166 Accession ID: 87A41440 |
op_rights |
Copyright |
_version_ |
1766270736847077376 |