Bacterial activity at –2 to –20◦C in arctic wintertime sea ice

Arctic wintertime sea-ice cores, characterized by a temperature gradient of 2 to 20°C, were investigated to better understand constraints on bacterial abundance, activity, and diversity at subzero temperatures. With the fluorescent stains 4,6-diamidino-2-phenylindole 2HCl (DAPI) (for DNA) and 5-cyan...

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Main Authors: Karen Junge, Hajo Eicken, Jody W. Deming
Other Authors: The Pennsylvania State University CiteSeerX Archives
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Language:English
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.499.3191
http://www2.gi.alaska.edu/~eicken/he_publ/04JED.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.499.3191 2023-05-15T14:59:24+02:00 Bacterial activity at –2 to –20◦C in arctic wintertime sea ice Karen Junge Hajo Eicken Jody W. Deming The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.499.3191 http://www2.gi.alaska.edu/~eicken/he_publ/04JED.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.499.3191 http://www2.gi.alaska.edu/~eicken/he_publ/04JED.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www2.gi.alaska.edu/~eicken/he_publ/04JED.pdf text ftciteseerx 2016-01-08T08:57:24Z Arctic wintertime sea-ice cores, characterized by a temperature gradient of 2 to 20°C, were investigated to better understand constraints on bacterial abundance, activity, and diversity at subzero temperatures. With the fluorescent stains 4,6-diamidino-2-phenylindole 2HCl (DAPI) (for DNA) and 5-cyano-2,3-ditoyl tetrazo-lium chloride (CTC) (for O2-based respiration), the abundances of total, particle-associated (>3-m), free-living, and actively respiring bacteria were determined for ice-core samples melted at their in situ temperatures (2 to20°C) and at the corresponding salinities of their brine inclusions (38 to 209 ppt). Fluorescence in situ hybridization was applied to determine the proportions of Bacteria, Cytophaga-Flavobacteria-Bacteroides (CFB), and Archaea. Microtome-prepared ice sections also were examined microscopically under in situ conditions to evaluate bacterial abundance (by DAPI staining) and particle associations within the brine-inclusion network of the ice. For both melted and intact ice sections, more than 50 % of cells were found to be associated with particles or surfaces (sediment grains, detritus, and ice-crystal boundaries). CTC-active bacteria (0.5 to 4 % of the total) and cells detectable by rRNA probes (18 to 86 % of the total) were found in all ice samples, including the coldest (20°C), where virtually all active cells were particle associated. The percentage of active bacteria associated with particles increased with decreasing temperature, as did the percentages of CFB (16 to 82 % of Bacteria) and Archaea (0.0 to 3.4 % of total cells). These results, combined with correlation analyses between Text Arctic ice core Sea ice Unknown Arctic Lium ENVELOPE(18.897,18.897,68.991,68.991)
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description Arctic wintertime sea-ice cores, characterized by a temperature gradient of 2 to 20°C, were investigated to better understand constraints on bacterial abundance, activity, and diversity at subzero temperatures. With the fluorescent stains 4,6-diamidino-2-phenylindole 2HCl (DAPI) (for DNA) and 5-cyano-2,3-ditoyl tetrazo-lium chloride (CTC) (for O2-based respiration), the abundances of total, particle-associated (>3-m), free-living, and actively respiring bacteria were determined for ice-core samples melted at their in situ temperatures (2 to20°C) and at the corresponding salinities of their brine inclusions (38 to 209 ppt). Fluorescence in situ hybridization was applied to determine the proportions of Bacteria, Cytophaga-Flavobacteria-Bacteroides (CFB), and Archaea. Microtome-prepared ice sections also were examined microscopically under in situ conditions to evaluate bacterial abundance (by DAPI staining) and particle associations within the brine-inclusion network of the ice. For both melted and intact ice sections, more than 50 % of cells were found to be associated with particles or surfaces (sediment grains, detritus, and ice-crystal boundaries). CTC-active bacteria (0.5 to 4 % of the total) and cells detectable by rRNA probes (18 to 86 % of the total) were found in all ice samples, including the coldest (20°C), where virtually all active cells were particle associated. The percentage of active bacteria associated with particles increased with decreasing temperature, as did the percentages of CFB (16 to 82 % of Bacteria) and Archaea (0.0 to 3.4 % of total cells). These results, combined with correlation analyses between
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Karen Junge
Hajo Eicken
Jody W. Deming
spellingShingle Karen Junge
Hajo Eicken
Jody W. Deming
Bacterial activity at –2 to –20◦C in arctic wintertime sea ice
author_facet Karen Junge
Hajo Eicken
Jody W. Deming
author_sort Karen Junge
title Bacterial activity at –2 to –20◦C in arctic wintertime sea ice
title_short Bacterial activity at –2 to –20◦C in arctic wintertime sea ice
title_full Bacterial activity at –2 to –20◦C in arctic wintertime sea ice
title_fullStr Bacterial activity at –2 to –20◦C in arctic wintertime sea ice
title_full_unstemmed Bacterial activity at –2 to –20◦C in arctic wintertime sea ice
title_sort bacterial activity at –2 to –20◦c in arctic wintertime sea ice
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.499.3191
http://www2.gi.alaska.edu/~eicken/he_publ/04JED.pdf
long_lat ENVELOPE(18.897,18.897,68.991,68.991)
geographic Arctic
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genre_facet Arctic
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op_source http://www2.gi.alaska.edu/~eicken/he_publ/04JED.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.499.3191
http://www2.gi.alaska.edu/~eicken/he_publ/04JED.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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