Abstract

Oligotrophic ocean gyre ecosystems may be expanding due to rising global temperatures [1–5]. Models predicting carbon flow through these changing ecosystems require accurate descriptions of phytoplankton communities and their metabolic activities [6]. We therefore measured distributions and activities of cyanobacteria and small photosynthetic eukaryotes throughout the euphotic zone on a zonal transect through the South Pacific Ocean, focusing on the ultraoligotrophic waters of the South Pacific Gyre (SPG). Bulk rates of CO2 fixation were low (0.1 µmol C l−1 d−1) but pervasive throughout both the surface mixed-layer (upper 150 m), as well as the deep chlorophyll a maximum of the core SPG. Chloroplast 16S rRNA metabarcoding, and single-cell 13CO2 uptake experiments demonstrated niche differentiation among the small eukaryotes and picocyanobacteria. Prochlorococcus abundances, activity, and growth were more closely associated with the rims of the gyre. Small, fast-growing, photosynthetic eukaryotes, likely related to the Pelagophyceae, characterized the deep chlorophyll a maximum. In contrast, a slower growing population of photosynthetic eukaryotes, likely comprised of Dictyochophyceae and Chrysophyceae, dominated the mixed layer that contributed 65–88% of the areal CO2 fixation within the core SPG. Small photosynthetic eukaryotes may thus play an underappreciated role in CO2 fixation in the surface mixed-layer waters of ultraoligotrophic ecosystems.

Highlights

  • Ocean gyre ecosystems are characterized by high-light intensities, extremely low nutrient concentrations and deep chlorophyll a maxima that are registered as very low chl a regions in satellite data

  • Global ocean circulation model results suggest that net dissolved organic carbon (DOC) export is responsible for ~50% of the fixed C export out of oligotrophic gyre ecosytems, and that this DOC export is strongly correlated with ecosystem structure in the form of picoplankton community composition [13]

  • Our study shows that the niche-partitioning among small photosynthetic eukaryotes and picocyanobacteria drives low, but similar rates of CO2 fixation within the deep chl a maximum and throughout the overlying 150 m deep, clear, ultraoligotrophic water column of the core South Pacific Gyre (SPG)

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Summary

INTRODUCTION

Ocean gyre ecosystems are characterized by high-light intensities, extremely low nutrient concentrations and deep chlorophyll a maxima (chl a max) that are registered as very low chl a regions in satellite data. To biomass and CO2 fixation rates in oligotrophic and mesotrophic marine ecosystems due to their relatively large size [20,21,22] How these key groups of CO2 fixing organisms respond to changing temperature and nutrient regimes is a topic of intense. We measured rates of photosynthetic CO2 fixation and the abundance of picophytoplankton, including Prochlorococcus and small eukaryotes (1–5 μm), through the upper mixed layer into the deep chl a max. Our study shows that the niche-partitioning among small photosynthetic eukaryotes and picocyanobacteria drives low, but similar rates of CO2 fixation within the deep chl a maximum and throughout the overlying 150 m deep, clear, ultraoligotrophic water column of the core SPG. Due to potential inaccuracies in counting using an Accuri C6 (BD Biosciences) flow cytometer in oligotrophic environments Prochlorococcus [39], cell numbers

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