Potential climate change impacts on microbial distribution and carbon cycling in the Australian Southern Ocean
Potential climate change impacts on microbial distribution and carbon cycling in the Australian Southern Ocean
Changes in oceanic circulation and physiochemical parameters due to climate change may alter the distribution, structure and function of marine microbial communities, thereby altering the action of the biological carbon pump. One area of current and predicted future change is the sub-Antarctic zone (SAZ) to the southeast of Tasmania, Australia, where a southward shift in westerly winds appears to be forcing warmer and macronutrient-poor subtropical waters into the sub-Antarctic zone (SAZ). We investigated the impact of these subtropical waters on the microbial community of the SAZ on the SAZ-Sense cruise during the austral summer of 2007. The abundance of pico- and nanoeukaryotic algae, cyanobacteria, heterotrophic nanoflagellates, bacteria and viruses was determined by flow cytometry at stations in the Polar Frontal Zone (PFZ), the SAZ and in Subtropical Zone (STZ). Using cluster and similarity profile analyses on integrated microbial abundances over the top 200 m, we found that microbial communities located in the potential future SAZ to the southeast of Tasmania formed two distinct groups from those of the remainder of the SAZ and the PFZ. In the waters of the potential future SAZ, shallow mixed layers and increased iron concentrations elevated cyanobacterial, bacterial and viral abundances and increased percentage high DNA bacteria, resulting in communities similar to those of subtropical waters. Conversely, waters of the PFZ exhibited relatively low concentrations of autotrophic and heterotrophic microbes and viruses, indicative of the iron limitation in this region. A Distance Based Linear Model determined that salinity and nitrogen availability (nitrate, nitrite and ammonia concentrations) were the most influential environmental parameters over the survey, explaining 72% of the variation in microbial community structure. The microbial community of the potential future SAZ showed a shift away from particulate carbon export from the photic zone towards increased production by smaller cells, increased significance of the microbial loop and viral lysis. These changes would promote carbon recycling within the photic zone, thereby potentially decreasing the capacity of the future SAZ to absorb CO2.
2150-2161
Evans, Claire
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Thomson, Paul G.
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Davidson, Andrew T.
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Bowie, Andrew R.
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Van Den Enden, Rick
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Witte, Harry
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Brussaard, Corina P.d.
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1 November 2011
Evans, Claire
93350709-cad3-4adf-8483-9bee595412f4
Thomson, Paul G.
9aa28598-116a-4153-b212-8f05ee16496a
Davidson, Andrew T.
8f6e91c4-e8fb-40a4-b98f-a7865be83ef5
Bowie, Andrew R.
b693c3a6-8975-4095-ad4b-81a5a3bb1f29
Van Den Enden, Rick
ee221ed3-87a2-4b40-a01b-14f0a79dabef
Witte, Harry
7fc6e4f9-3864-46fe-b6d1-4020bd7a36c5
Brussaard, Corina P.d.
433a0c4f-d666-4c89-a1f8-ddbd3aeafc63
Evans, Claire, Thomson, Paul G., Davidson, Andrew T., Bowie, Andrew R., Van Den Enden, Rick, Witte, Harry and Brussaard, Corina P.d.
(2011)
Potential climate change impacts on microbial distribution and carbon cycling in the Australian Southern Ocean.
Deep Sea Research Part II: Topical Studies in Oceanography, 58 (21-22), .
(doi:10.1016/j.dsr2.2011.05.019).
Abstract
Changes in oceanic circulation and physiochemical parameters due to climate change may alter the distribution, structure and function of marine microbial communities, thereby altering the action of the biological carbon pump. One area of current and predicted future change is the sub-Antarctic zone (SAZ) to the southeast of Tasmania, Australia, where a southward shift in westerly winds appears to be forcing warmer and macronutrient-poor subtropical waters into the sub-Antarctic zone (SAZ). We investigated the impact of these subtropical waters on the microbial community of the SAZ on the SAZ-Sense cruise during the austral summer of 2007. The abundance of pico- and nanoeukaryotic algae, cyanobacteria, heterotrophic nanoflagellates, bacteria and viruses was determined by flow cytometry at stations in the Polar Frontal Zone (PFZ), the SAZ and in Subtropical Zone (STZ). Using cluster and similarity profile analyses on integrated microbial abundances over the top 200 m, we found that microbial communities located in the potential future SAZ to the southeast of Tasmania formed two distinct groups from those of the remainder of the SAZ and the PFZ. In the waters of the potential future SAZ, shallow mixed layers and increased iron concentrations elevated cyanobacterial, bacterial and viral abundances and increased percentage high DNA bacteria, resulting in communities similar to those of subtropical waters. Conversely, waters of the PFZ exhibited relatively low concentrations of autotrophic and heterotrophic microbes and viruses, indicative of the iron limitation in this region. A Distance Based Linear Model determined that salinity and nitrogen availability (nitrate, nitrite and ammonia concentrations) were the most influential environmental parameters over the survey, explaining 72% of the variation in microbial community structure. The microbial community of the potential future SAZ showed a shift away from particulate carbon export from the photic zone towards increased production by smaller cells, increased significance of the microbial loop and viral lysis. These changes would promote carbon recycling within the photic zone, thereby potentially decreasing the capacity of the future SAZ to absorb CO2.
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Published date: 1 November 2011
Organisations:
Ocean Biochemistry & Ecosystems, National Oceanography Centre
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Local EPrints ID: 406865
URI: http://eprints.soton.ac.uk/id/eprint/406865
ISSN: 0967-0645
PURE UUID: b3500951-2531-411c-bf76-a7d912a6d6c5
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Date deposited: 25 Mar 2017 02:02
Last modified: 15 Mar 2024 12:55
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Author:
Claire Evans
Author:
Paul G. Thomson
Author:
Andrew T. Davidson
Author:
Andrew R. Bowie
Author:
Rick Van Den Enden
Author:
Harry Witte
Author:
Corina P.d. Brussaard
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