Viral lysis and microzooplankton grazing of phytoplankton throughout the Southern Ocean

We investigated microzooplankton grazing and viral lysis of the pico‐ and nanophytoplankton community in the Southern Ocean during the “Sensitivity of Sub‐Antarctic Zone Waters to Global Change” cruise to the Australian sector (January–February 2007) and the Antarctic–XXIV/3 (February–March 2008) ex...

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Published in:Limnology and Oceanography
Main Authors: Evans, Claire, Brussaard, Corina P. D.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2012
Subjects:
Online Access:http://dx.doi.org/10.4319/lo.2012.57.6.1826
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.2012.57.6.1826
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spelling crwiley:10.4319/lo.2012.57.6.1826 2024-09-15T17:48:06+00:00 Viral lysis and microzooplankton grazing of phytoplankton throughout the Southern Ocean Evans, Claire Brussaard, Corina P. D. 2012 http://dx.doi.org/10.4319/lo.2012.57.6.1826 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.2012.57.6.1826 https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lo.2012.57.6.1826 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Limnology and Oceanography volume 57, issue 6, page 1826-1837 ISSN 0024-3590 1939-5590 journal-article 2012 crwiley https://doi.org/10.4319/lo.2012.57.6.1826 2024-08-09T04:26:59Z We investigated microzooplankton grazing and viral lysis of the pico‐ and nanophytoplankton community in the Southern Ocean during the “Sensitivity of Sub‐Antarctic Zone Waters to Global Change” cruise to the Australian sector (January–February 2007) and the Antarctic–XXIV/3 (February–March 2008) expedition to the Greenwich Meridian and the Drake Passage. A dilution assay was employed in concert with flow cytometry at stations that spanned the sub‐Antarctic, Polar Frontal, and Antarctic Zones and in the Weddell Gyre. Both viral lysis and microzooplankton grazing played a significant role in controlling cyanobacterial populations, except in the sub‐Antarctic west of Tasmania, where their growth was regulated by grazing alone. Three main groups of eukaryotic algae were detected, and these were calculated to have average cell diameters of 0.8, 2.1, and 3.7 µm. Grazing was significant in the control of their growth at all locations, whereas viral lysis of eukaryotic algae was comparatively minor, as it was detected in only 40% of the experiments. Throughout the surveyed sites no pattern between geographical location and growth rates and/or mortality rates could be established for any of the phytoplankton groups. Estimates of iron regeneration indicated that as a result of its widespread occurrence, microzooplankton grazing is a more consistent source of regenerated iron to the Southern Ocean but that viral lysis can be responsible for significant pulses of iron into the dissolved pool. Article in Journal/Newspaper Antarc* Antarctic Drake Passage Southern Ocean Wiley Online Library Limnology and Oceanography 57 6 1826 1837
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description We investigated microzooplankton grazing and viral lysis of the pico‐ and nanophytoplankton community in the Southern Ocean during the “Sensitivity of Sub‐Antarctic Zone Waters to Global Change” cruise to the Australian sector (January–February 2007) and the Antarctic–XXIV/3 (February–March 2008) expedition to the Greenwich Meridian and the Drake Passage. A dilution assay was employed in concert with flow cytometry at stations that spanned the sub‐Antarctic, Polar Frontal, and Antarctic Zones and in the Weddell Gyre. Both viral lysis and microzooplankton grazing played a significant role in controlling cyanobacterial populations, except in the sub‐Antarctic west of Tasmania, where their growth was regulated by grazing alone. Three main groups of eukaryotic algae were detected, and these were calculated to have average cell diameters of 0.8, 2.1, and 3.7 µm. Grazing was significant in the control of their growth at all locations, whereas viral lysis of eukaryotic algae was comparatively minor, as it was detected in only 40% of the experiments. Throughout the surveyed sites no pattern between geographical location and growth rates and/or mortality rates could be established for any of the phytoplankton groups. Estimates of iron regeneration indicated that as a result of its widespread occurrence, microzooplankton grazing is a more consistent source of regenerated iron to the Southern Ocean but that viral lysis can be responsible for significant pulses of iron into the dissolved pool.
format Article in Journal/Newspaper
author Evans, Claire
Brussaard, Corina P. D.
spellingShingle Evans, Claire
Brussaard, Corina P. D.
Viral lysis and microzooplankton grazing of phytoplankton throughout the Southern Ocean
author_facet Evans, Claire
Brussaard, Corina P. D.
author_sort Evans, Claire
title Viral lysis and microzooplankton grazing of phytoplankton throughout the Southern Ocean
title_short Viral lysis and microzooplankton grazing of phytoplankton throughout the Southern Ocean
title_full Viral lysis and microzooplankton grazing of phytoplankton throughout the Southern Ocean
title_fullStr Viral lysis and microzooplankton grazing of phytoplankton throughout the Southern Ocean
title_full_unstemmed Viral lysis and microzooplankton grazing of phytoplankton throughout the Southern Ocean
title_sort viral lysis and microzooplankton grazing of phytoplankton throughout the southern ocean
publisher Wiley
publishDate 2012
url http://dx.doi.org/10.4319/lo.2012.57.6.1826
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.4319%2Flo.2012.57.6.1826
https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.4319/lo.2012.57.6.1826
genre Antarc*
Antarctic
Drake Passage
Southern Ocean
genre_facet Antarc*
Antarctic
Drake Passage
Southern Ocean
op_source Limnology and Oceanography
volume 57, issue 6, page 1826-1837
ISSN 0024-3590 1939-5590
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.4319/lo.2012.57.6.1826
container_title Limnology and Oceanography
container_volume 57
container_issue 6
container_start_page 1826
op_container_end_page 1837
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