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Microzooplankton grazing impact in the Bering Sea during spring sea ice conditions

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Title Microzooplankton grazing impact in the Bering Sea during spring sea ice conditions
Names Sherr, Evelyn B. (creator)
Sherr, Barry F. (creator)
Ross, Celia (creator)
Date Issued 2013-10-01 (iso8601)
Note This is an author's peer-reviewed final manuscript, as accepted by the publisher. The published article is copyrighted by Elsevier and can be found at: http://www.journals.elsevier.com/deep-sea-research-part-ii-topical-studies-in-oceanography/.
Abstract Microzooplankton grazing impact on phytoplankton in the Bering Sea during spring was
assessed in 2008, 2009 and 2010 using two-point dilution assays. Forty-nine experiments were
completed in a region encompassing shelf to slope waters, including the 70 m line along the edge
of the shelf. A variety of conditions were encountered, with a concomitant range of trophic
states, from pre-bloom low chlorophyll-a (Chl-a) < 3 μg l⁻¹ during heavy ice cover to late spring
open water diatom blooms with Chl-a up to 40 μg l⁻¹. Microzooplankton biomass was dominated
by large heterotrophic dinoflagellates and ciliates. Both athecate and thecate dinoflagellates, as
well as some species of ciliates, fed on diatom cells and chains. Other types of protists, notably
thecate amoebae and parasitoid flagellates, were also observed preying on diatoms. Total
microzooplankton biomass ranged from 0.1 to 109 μg C l⁻¹ and was positively related to Chl-a
concentration. Significant rates of microzooplankton herbivory were found in 55% of dilution
experiments. Maximum grazing rate was 0.49 d⁻¹, and average grazing rate, including
experiments with no significant grazing, was 0.09 ± 0.10 d⁻¹. Phytoplankton intrinsic growth
rates varied from slightly negative growth to > 0.4 d⁻¹. Microzooplankton grazing was significant
in both non-bloom and bloom conditions, averaging 46 ± 75% of phytoplankton daily growth.
Based on the amount of phytoplankton carbon consumed, we estimated potential
microzooplankton community growth rates of up to 1.3 d⁻¹. Our results confirm the importance
of protist grazers in planktonic food webs of high latitude ecosystems. We also conclude that our
finding of significant grazing by microzooplankton on spring blooms in the Bering Sea does not
support theories about phytoplankton bloom formation based on escape from grazing, due either
to predation resistance or to slow growth of herbivorous protists at cold temperature.
Genre Article
Topic microzooplankton
Identifier Sherr, E. B., Sherr, B. F., & Ross, C. (2013). Microzooplankton grazing impact in the Bering Sea during spring sea ice conditions. Deep-Sea Research Part II-Topical Studies in Oceanography, 94, 57-67. doi:10.1016/j.dsr2.2013.03.019

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