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Journal Article

Viruses as mortality agents of picophytoplankton in the deep chlorophyll maximum layer during IRONAGES III

Anne-Claire Baudoux; Marcel J. W. Veldhuis; Harry J. Witte; Corina P. D. Brussaard
Limnology and Oceanography · Vol. 52, Issue 6 · pp. 2519-2529 · 2007

Abstract

We report viral‐induced mortality rates of the picoeukaryotic (two size classes) and prokaryotic (cyanobacteria Prochlorococcus and Synechococcus ) phytoplankton during a cruise in the oligotrophic subtropical northeastern Atlantic (October 2002). A dilution assay, simultaneously estimating viral lysis and microzooplankton grazing, was applied around the deep chlorophyll maximum (DCM) at six stations. For the smallest picoeukaryotes (group I), viral lysis was responsible for 50‐100% of the total cell losses, with rates ranging from 0.1 to 0.8 d −1 . Viral lysis rates were positively linked to the abundance and contribution of large genome‐sized (180–225 kb) putative algal viruses. In contrast, the prokaryotic picophytoplankton did not seem to be controlled by viral lysis. For Synechococcus , microzooplankton grazing dominated, with rates between 0.1 and 0.25 d −1 (comparable to those for the eukaryotic algae). For Prochlorococcus , both viral lysis and microzooplankton grazing rates were very low (0–0.1 d −1 ). Overall, the total carbon production by the picophytoplankton community was balanced by the combined losses due to viral lysis and microzooplankton grazing. Viral lysis released 0.1‐0.3 µg of picophytoplanktonic C L −1 d −1 , which comprised 21% of the total carbon production by picophytoplankton.

Bibliographic Information

JournalLimnology and Oceanography
PublisherWiley
Publication Date2007-11-01
Publication Year2007
Volume52
Issue6
Pages2519-2529
Document TypeJournal Article
Print ISSN0024-3590
eISSN1939-5590
DOI10.4319/lo.2007.52.6.2519
SubjectAquatic Science

Access Information

NARA Access Coverage1997-01-01~Current
Journal Homepagehttps://aslopubs.onlinelibrary.wiley.com/loi/19395590
Publisher PageOpen Publisher Page
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