Abstract

The impacts of grazing by meso- and microzooplankton on phytoplankton primary production (PP) was investigated in the surface layer of the western North Atlantic during spring. Shipboard experiments were performed on a latitudinal transect at three stations that differed in mixed layer depth, temperature, and mesozooplankton taxonomic composition. The mesozooplankton community was numerically dominated by Calanus finmarchicus at the northern and central station, with Calanus hyperboreus also present at the northern station. The southern station was >10 °C warmer than the other stations and had the most diverse mesozooplankton assemblage, dominated by small copepods including Paracalanus spp. Microzooplankton grazing was detected only at the northern station, where it removed 97% of PP. Estimated clearance rates by C. hyperboreus and C. finmarchicus suggested that at in-situ abundance these mesozooplankton were not likely to have a major impact on phytoplankton abundance, unless locally aggregated. Although mesozooplankton grazing impact on total phytoplankton was minimal, these grazers completely removed the numerically scarce > 10 µm particles, altering the particle-size spectrum. At the southern station, grazing by the whole mesozooplankton assemblage resulted in a removal of 14% of PP, and its effect on net phytoplankton growth rate was similar irrespective of ambient light. In contrast, reduction in light availability had an approximately 3-fold greater impact on net phytoplankton growth rate than mesozooplankton grazing pressure. The low mesozooplankton grazing impact across stations suggests limited mesozooplankton-mediated vertical export of phytoplankton production. The constraints provided here on trophic transfer, as well as quantitative estimates of the relative contribution of light and grazer controls of PP and of grazer-induced shifts in particle size spectra, illuminate food web dynamics and aid in parameterizing modeling-frameworks assessing global elemental fluxes and carbon export.

Highlights

  • Zooplankton occupy a pivotal position in pelagic food webs

  • Grazing by zooplankton represents the major fate of marine phytoplankton production (Banse, 2013; Steinberg & Landry, 2017), influencing energy transfer to higher trophic levels, nutrient cycling, and carbon flow

  • Our findings suggest that feeding by large herbivorous copepods only had a minimal impact on primary production (PP) but did alter the particle size spectrum, and that the effect of light availability on phytoplankton growth controlled

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Summary

Introduction

Grazing by zooplankton represents the major fate of marine phytoplankton production (Banse, 2013; Steinberg & Landry, 2017), influencing energy transfer to higher trophic levels, nutrient cycling, and carbon flow. Mesozooplankton have generation times on the order of weeks and months and are numerically less abundant (Schmoker, Hernández-León & Calbet, 2013). Due to their capacity to reproduce asexually, microzooplankton are thought to increase in biomass faster than mesozooplankton in response to the increase in phytoplankton biomass such as occurs during the formation of a bloom (Sherr et al, 2003; Sherr & Sherr, 2009). While mesozooplankton grazing on oceanic primary production (PP) can occasionally be high (Calbet, 2001), microzooplankton generally tend to exert a higher grazing pressure on PP than mesozooplankton (Calbet, 2008; Calbet et al, 2009; Campbell et al, 2009)

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