Abstract

Mesozooplankton play a key role in marine ecosystems as they modulate the transfer of energy from phytoplankton to large marine organisms. In addition, they directly influence the oceanic cycles of carbon and nutrients through vertical migrations, fecal pellet production, respiration, and excretion. Mesozooplankton are mainly made up of metazoans, which undergo important size changes during their life cycle, resulting in significant variations in metabolic rates. However, most marine biogeochemical models represent mesozooplankton as protists-like organisms. Here, we study the potential caveats of this simplistic representation by using a chemostat-like zero-dimensional model with four different Nutrient-Phytoplankton-Zooplankton configurations in which the description of mesozooplankton ranges from protist-type organisms to using a size-based formulation including explicit reproduction and ontogenetic growth. We show that the size-based formulation strongly impacts mesozooplankton. First, it generates a delay of a few months in the response to an increase in food availability. Second, the increase in mesozooplankton biomass displays much larger temporal variations, in the form of successive cohorts, because of the dependency of the ingestion rate to body size. However, the size-based formulation does not affect smaller plankton or nutrient concentrations. A proper assessment of these top-down effects would require implementing our size-resolved approach in a 3-dimensional biogeochemical model. Furthermore, the bottom-up effects on higher trophic levels resulting from the significant changes in the temporal dynamics of mesozooplankton could be estimated in an end-to-end model coupling low and high trophic levels.

Highlights

  • Zooplankton plays a pivotal role in the marine ecosystems because they are at the interface between primary producers and higher trophic levels

  • We focus our analysis on the response to the High-Nutrient mode (HNM) and present the results of the standard model first, and a comparison to the alternative models

  • The explicit representation of metazoan life-cycle in our simple biogeochemical model does not affect the temporal dynamics of non-mesozooplankton compartments

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Summary

Introduction

Zooplankton plays a pivotal role in the marine ecosystems because they are at the interface between primary producers and higher trophic levels. They are as such responsible for a large fraction of the energy transfer to fish (Beaugrand et al 2010; Carlotti and Poggiale 2010; Mitra et al 2014). They are key players in marine biogeochemical cycles as they convert a large fraction of the organic matter they consume to dissolved inorganic carbon and nutrient pools. Mesozooplankton respiration has been estimated as 10% to about 30% of global PP, both phytoplankton and microzooplankton contributing importantly to the diet of mesozooplankton (Calbet 2001; Hernandez-Len and Ikeda 2005)

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