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Autotrophic growth of bacterial and archaeal ammonia oxidizers in freshwater sediment microcosms incubated at different temperatures

Autotrophic growth of bacterial and archaeal ammonia oxidizers in freshwater sediment microcosms incubated at different temperatures
Autotrophic growth of bacterial and archaeal ammonia oxidizers in freshwater sediment microcosms incubated at different temperatures
Both bacteria and archaea potentially contribute to ammonia oxidation, but their roles in freshwater sediments are still poorly understood. Seasonal differences in the relative activities of these groups might exist, since cultivated archaeal ammonia oxidizers have higher temperature optima than their bacterial counterparts. In this study, sediment collected from eutrophic freshwater Lake Taihu (China) was incubated at different temperatures (4°C, 15°C, 25°C, and 37°C) for up to 8 weeks. We examined the active bacterial and archaeal ammonia oxidizers in these sediment microcosms by using combined stable isotope probing (SIP) and molecular community analysis. The results showed that accumulation of nitrate in microcosms correlated negatively with temperature, although ammonium depletion was the same, which might have been related to enhanced activity of other nitrogen transformation processes. Incubation at different temperatures significantly changed the microbial community composition, as revealed by 454 pyrosequencing targeting bacterial 16S rRNA genes. After 8 weeks of incubation, [(13)C]bicarbonate labeling of bacterial amoA genes, which encode the ammonia monooxygenase subunit A, and an observed increase in copy numbers indicated the activity of ammonia-oxidizing bacteria in all microcosms. Nitrosomonas sp. strain Is79A3 and Nitrosomonas communis lineages dominated the heavy fraction of CsCl gradients at low and high temperatures, respectively, indicating a niche differentiation of active bacterial ammonia oxidizers along the temperature gradient. The (13)C labeling of ammonia-oxidizing archaea in microcosms incubated at 4 to 25°C was minor. In contrast, significant (13)C labeling of Nitrososphaera-like archaea and changes in the abundance and composition of archaeal amoA genes were observed at 37°C, implicating autotrophic growth of ammonia-oxidizing archaea under warmer conditions
0099-2240
3076-3084
Wu, Y.
84854e37-ada6-4cc8-995f-6ce5ebc77423
Ke, X.
7ce19883-4155-4457-b239-efe78e8087ff
Hernandez Garcia, Marcela
e73477e7-cf3e-4f50-97c8-4494c5b05cd0
Wang, B.
501f63aa-3bb3-4b8b-ab2b-655467454ebe
Dumont, Marc
afd9f08f-bdbb-4cee-b792-1a7f000ee511
Jia, Z.
91d75600-2f55-4d88-9577-a59bd4d43c55
Conrad, R.
4a1d4987-a975-4184-930f-9a638f534434
Wu, Y.
84854e37-ada6-4cc8-995f-6ce5ebc77423
Ke, X.
7ce19883-4155-4457-b239-efe78e8087ff
Hernandez Garcia, Marcela
e73477e7-cf3e-4f50-97c8-4494c5b05cd0
Wang, B.
501f63aa-3bb3-4b8b-ab2b-655467454ebe
Dumont, Marc
afd9f08f-bdbb-4cee-b792-1a7f000ee511
Jia, Z.
91d75600-2f55-4d88-9577-a59bd4d43c55
Conrad, R.
4a1d4987-a975-4184-930f-9a638f534434

Wu, Y., Ke, X., Hernandez Garcia, Marcela, Wang, B., Dumont, Marc, Jia, Z. and Conrad, R. (2013) Autotrophic growth of bacterial and archaeal ammonia oxidizers in freshwater sediment microcosms incubated at different temperatures. Applied and Environmental Microbiology, 79 (9), 3076-3084. (doi:10.1128/AEM.00061-13). (PMID:23455342)

Record type: Article

Abstract

Both bacteria and archaea potentially contribute to ammonia oxidation, but their roles in freshwater sediments are still poorly understood. Seasonal differences in the relative activities of these groups might exist, since cultivated archaeal ammonia oxidizers have higher temperature optima than their bacterial counterparts. In this study, sediment collected from eutrophic freshwater Lake Taihu (China) was incubated at different temperatures (4°C, 15°C, 25°C, and 37°C) for up to 8 weeks. We examined the active bacterial and archaeal ammonia oxidizers in these sediment microcosms by using combined stable isotope probing (SIP) and molecular community analysis. The results showed that accumulation of nitrate in microcosms correlated negatively with temperature, although ammonium depletion was the same, which might have been related to enhanced activity of other nitrogen transformation processes. Incubation at different temperatures significantly changed the microbial community composition, as revealed by 454 pyrosequencing targeting bacterial 16S rRNA genes. After 8 weeks of incubation, [(13)C]bicarbonate labeling of bacterial amoA genes, which encode the ammonia monooxygenase subunit A, and an observed increase in copy numbers indicated the activity of ammonia-oxidizing bacteria in all microcosms. Nitrosomonas sp. strain Is79A3 and Nitrosomonas communis lineages dominated the heavy fraction of CsCl gradients at low and high temperatures, respectively, indicating a niche differentiation of active bacterial ammonia oxidizers along the temperature gradient. The (13)C labeling of ammonia-oxidizing archaea in microcosms incubated at 4 to 25°C was minor. In contrast, significant (13)C labeling of Nitrososphaera-like archaea and changes in the abundance and composition of archaeal amoA genes were observed at 37°C, implicating autotrophic growth of ammonia-oxidizing archaea under warmer conditions

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Accepted/In Press date: 23 February 2013
Published date: 1 March 2013
Organisations: Centre for Biological Sciences

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Local EPrints ID: 387934
URI: http://eprints.soton.ac.uk/id/eprint/387934
ISSN: 0099-2240
PURE UUID: 891c09c9-20e5-40fc-a784-dd0e4a223162
ORCID for Marc Dumont: ORCID iD orcid.org/0000-0002-7347-8668

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Date deposited: 08 Jul 2016 14:09
Last modified: 15 Mar 2024 03:53

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Contributors

Author: Y. Wu
Author: X. Ke
Author: Marcela Hernandez Garcia
Author: B. Wang
Author: Marc Dumont ORCID iD
Author: Z. Jia
Author: R. Conrad

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