Life in Solid Ice on Earth and Other Planetary Bodies

Theory and direct observation indicate that micro-organisms exist in liquid veins in ice and permafrost, provided the temperature is above the eutectic for H 2 O and soluble impurities present. Microbes can exist and metabolize in glacial ice and permafrost on Earth, Mars, and Europa. One can search...

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Bibliographic Details
Published in:Symposium - International Astronomical Union
Main Author: Price, P. Buford
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2004
Subjects:
Ice
Online Access:http://dx.doi.org/10.1017/s0074180900193556
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0074180900193556
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spelling crcambridgeupr:10.1017/s0074180900193556 2024-03-03T08:45:16+00:00 Life in Solid Ice on Earth and Other Planetary Bodies Price, P. Buford 2004 http://dx.doi.org/10.1017/s0074180900193556 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0074180900193556 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Symposium - International Astronomical Union volume 213, page 363-366 ISSN 0074-1809 journal-article 2004 crcambridgeupr https://doi.org/10.1017/s0074180900193556 2024-02-08T08:46:30Z Theory and direct observation indicate that micro-organisms exist in liquid veins in ice and permafrost, provided the temperature is above the eutectic for H 2 O and soluble impurities present. Microbes can exist and metabolize in glacial ice and permafrost on Earth, Mars, and Europa. One can search directly (with fluorescence microscopy at liquid veins in Vostok ice core samples) or with a biologging instrument (for microbial fluorescence in a borehole in terrestrial or martian permafrost or ice). The viability lifetime against DNA destruction of bacterial spores can be measured with analytical techniques that identify calcium dipicolinate, which is unique to spores. Article in Journal/Newspaper Ice ice core permafrost Cambridge University Press Symposium - International Astronomical Union 213 363 366
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Theory and direct observation indicate that micro-organisms exist in liquid veins in ice and permafrost, provided the temperature is above the eutectic for H 2 O and soluble impurities present. Microbes can exist and metabolize in glacial ice and permafrost on Earth, Mars, and Europa. One can search directly (with fluorescence microscopy at liquid veins in Vostok ice core samples) or with a biologging instrument (for microbial fluorescence in a borehole in terrestrial or martian permafrost or ice). The viability lifetime against DNA destruction of bacterial spores can be measured with analytical techniques that identify calcium dipicolinate, which is unique to spores.
format Article in Journal/Newspaper
author Price, P. Buford
spellingShingle Price, P. Buford
Life in Solid Ice on Earth and Other Planetary Bodies
author_facet Price, P. Buford
author_sort Price, P. Buford
title Life in Solid Ice on Earth and Other Planetary Bodies
title_short Life in Solid Ice on Earth and Other Planetary Bodies
title_full Life in Solid Ice on Earth and Other Planetary Bodies
title_fullStr Life in Solid Ice on Earth and Other Planetary Bodies
title_full_unstemmed Life in Solid Ice on Earth and Other Planetary Bodies
title_sort life in solid ice on earth and other planetary bodies
publisher Cambridge University Press (CUP)
publishDate 2004
url http://dx.doi.org/10.1017/s0074180900193556
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0074180900193556
genre Ice
ice core
permafrost
genre_facet Ice
ice core
permafrost
op_source Symposium - International Astronomical Union
volume 213, page 363-366
ISSN 0074-1809
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0074180900193556
container_title Symposium - International Astronomical Union
container_volume 213
container_start_page 363
op_container_end_page 366
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