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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2004
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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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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 |
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Open Polar |
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Cambridge University Press |
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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 |
_version_ |
1792500795646672896 |