C-Biomass of Bacteria, Fungi, and Protozoan Communities in Arctic Tundra Soil, Including Some Trophic Relationships

The ecology of tundra terrestrial environments has gained increasing attention due to potential major changes resulting from global warming and climate change. However, the composition of terrestrial microbial communities and their role in the biogeochemical carbon cycle are less well studied. This...

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Main Authors: Anderson, O. Roger, McGuire, Krista
Format: Article in Journal/Newspaper
Language:Polish
Published: Acta Protozoologica 2015
Subjects:
Online Access:http://www.ejournals.eu/sj/index.php/AProto/article/view/4079
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spelling ftejournalsojs:oai:ojs.www.ejournals.eu:article/4079 2023-05-15T15:18:50+02:00 C-Biomass of Bacteria, Fungi, and Protozoan Communities in Arctic Tundra Soil, Including Some Trophic Relationships Anderson, O. Roger McGuire, Krista 2015-09-08 application/pdf http://www.ejournals.eu/sj/index.php/AProto/article/view/4079 pol pol Acta Protozoologica http://www.ejournals.eu/sj/index.php/AProto/article/view/4079/4015 http://www.ejournals.eu/sj/index.php/AProto/article/view/4079 ##submission.copyrightStatement## Acta Protozoologica; Vol 52, No 4 (2013); 217–227 1689-0027 0065-1583 Bacterial biomass carbon biogeochemistry climate change fungal biomass protozoan biomass soil carbon enrichment info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Recenzowany artykuł 2015 ftejournalsojs 2020-03-01T09:10:56Z The ecology of tundra terrestrial environments has gained increasing attention due to potential major changes resulting from global warming and climate change. However, the composition of terrestrial microbial communities and their role in the biogeochemical carbon cycle are less well studied. This is the first report of the C-biomass of bacteria, fungi, and representative protozoa (heterotrophic nanoflagellates, naked amoebae, and testate amoebae) in Alaskan tundra soil samples, and the effects of glucose solution enrichment in laboratory studies simulating release of soluble organic compounds as may occur during permafrost melt and increased plant root exudates due to global warming. The data for three moss-rich surface samples, two in spring and one in summer (2011), are reported for C-supplemented (8,000 μg glucose-C) and non-supplemented treatments in laboratory culture. Seven days after supplementation, fungal C-biomass in the glucose-treated and untreated samples were similar in the range of 5 to 11 mg g–1 soil dry weight, the highest values in the summer samples. The bacterial C-biomass was the next highest in the range of 20 to 120 μg g–1 soil dry weight, followed by heterotrophic nanoflagellates (2 to 14 μg g–1 soil dry weight). The naked amoebae (0.13 to 0.94 μg C g–1 soil dry weight) and testate amoebae (2 to 20 ng C g–1 soil dry weight) contributed the least C-biomass. All of the bacterial and protozoan treatments showed increased biomass with glucose supplementation. Based on size, and C-biomass estimates, the phagotrophic protozoa appear to be organized in a classical bacterial-based trophic hierarchy (i.e. bacteria – nanoflagellates – naked amoebae – testate amoebae, in ascending order). Correlations of the C-biomass of bacteria to each of the protozoa, provided further evidence of a trophic pyramid; bacteria vs. nanoflagellates (r = –0.986), indicating top-down control by predatory flagellates, bacteria vs. naked amoebae (r = –0.361) and bacteria vs. testate amoebae (r = –0.131), each of decreasing magnitude as would be predicted for higher level consumers. Estimates of bacterial predation indicated strong predatory pressures on bacteria by the protozoa, greater with C-supplementation compared to the non-supplemented treatments. Article in Journal/Newspaper Arctic Climate change Global warming permafrost Tundra Portal Czasopism Naukowych (E-Journals) Arctic Pyramid ENVELOPE(157.300,157.300,-81.333,-81.333)
institution Open Polar
collection Portal Czasopism Naukowych (E-Journals)
op_collection_id ftejournalsojs
language Polish
topic Bacterial biomass
carbon biogeochemistry
climate change
fungal biomass
protozoan biomass
soil carbon enrichment
spellingShingle Bacterial biomass
carbon biogeochemistry
climate change
fungal biomass
protozoan biomass
soil carbon enrichment
Anderson, O. Roger
McGuire, Krista
C-Biomass of Bacteria, Fungi, and Protozoan Communities in Arctic Tundra Soil, Including Some Trophic Relationships
topic_facet Bacterial biomass
carbon biogeochemistry
climate change
fungal biomass
protozoan biomass
soil carbon enrichment
description The ecology of tundra terrestrial environments has gained increasing attention due to potential major changes resulting from global warming and climate change. However, the composition of terrestrial microbial communities and their role in the biogeochemical carbon cycle are less well studied. This is the first report of the C-biomass of bacteria, fungi, and representative protozoa (heterotrophic nanoflagellates, naked amoebae, and testate amoebae) in Alaskan tundra soil samples, and the effects of glucose solution enrichment in laboratory studies simulating release of soluble organic compounds as may occur during permafrost melt and increased plant root exudates due to global warming. The data for three moss-rich surface samples, two in spring and one in summer (2011), are reported for C-supplemented (8,000 μg glucose-C) and non-supplemented treatments in laboratory culture. Seven days after supplementation, fungal C-biomass in the glucose-treated and untreated samples were similar in the range of 5 to 11 mg g–1 soil dry weight, the highest values in the summer samples. The bacterial C-biomass was the next highest in the range of 20 to 120 μg g–1 soil dry weight, followed by heterotrophic nanoflagellates (2 to 14 μg g–1 soil dry weight). The naked amoebae (0.13 to 0.94 μg C g–1 soil dry weight) and testate amoebae (2 to 20 ng C g–1 soil dry weight) contributed the least C-biomass. All of the bacterial and protozoan treatments showed increased biomass with glucose supplementation. Based on size, and C-biomass estimates, the phagotrophic protozoa appear to be organized in a classical bacterial-based trophic hierarchy (i.e. bacteria – nanoflagellates – naked amoebae – testate amoebae, in ascending order). Correlations of the C-biomass of bacteria to each of the protozoa, provided further evidence of a trophic pyramid; bacteria vs. nanoflagellates (r = –0.986), indicating top-down control by predatory flagellates, bacteria vs. naked amoebae (r = –0.361) and bacteria vs. testate amoebae (r = –0.131), each of decreasing magnitude as would be predicted for higher level consumers. Estimates of bacterial predation indicated strong predatory pressures on bacteria by the protozoa, greater with C-supplementation compared to the non-supplemented treatments.
format Article in Journal/Newspaper
author Anderson, O. Roger
McGuire, Krista
author_facet Anderson, O. Roger
McGuire, Krista
author_sort Anderson, O. Roger
title C-Biomass of Bacteria, Fungi, and Protozoan Communities in Arctic Tundra Soil, Including Some Trophic Relationships
title_short C-Biomass of Bacteria, Fungi, and Protozoan Communities in Arctic Tundra Soil, Including Some Trophic Relationships
title_full C-Biomass of Bacteria, Fungi, and Protozoan Communities in Arctic Tundra Soil, Including Some Trophic Relationships
title_fullStr C-Biomass of Bacteria, Fungi, and Protozoan Communities in Arctic Tundra Soil, Including Some Trophic Relationships
title_full_unstemmed C-Biomass of Bacteria, Fungi, and Protozoan Communities in Arctic Tundra Soil, Including Some Trophic Relationships
title_sort c-biomass of bacteria, fungi, and protozoan communities in arctic tundra soil, including some trophic relationships
publisher Acta Protozoologica
publishDate 2015
url http://www.ejournals.eu/sj/index.php/AProto/article/view/4079
long_lat ENVELOPE(157.300,157.300,-81.333,-81.333)
geographic Arctic
Pyramid
geographic_facet Arctic
Pyramid
genre Arctic
Climate change
Global warming
permafrost
Tundra
genre_facet Arctic
Climate change
Global warming
permafrost
Tundra
op_source Acta Protozoologica; Vol 52, No 4 (2013); 217–227
1689-0027
0065-1583
op_relation http://www.ejournals.eu/sj/index.php/AProto/article/view/4079/4015
http://www.ejournals.eu/sj/index.php/AProto/article/view/4079
op_rights ##submission.copyrightStatement##
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