Abstract

In oligotrophic ocean regions such as the North Pacific Subtropical Gyre (NPSG), N2 fixation (i.e. diazotrophy) by a diverse consortium of microorganisms has been shown to contribute significantly to new production and particle export. In 2015 and 2016, we measured near-monthly abundances of the large cell-sized (> 10 m) diazotrophic genera Trichodesmium and diatom-associated Richelia and Calothrix spp. in the NPSG via microscopy and quantitative PCR of nifH genes. Of these genera, we find Trichodesmium to be the more abundant over our study period, with cell concentrations in the upper water column (0-45 m) ranging from 1-5988 cells L-1, while the sum of Richelia and Calothrix spp. abundances ranged from 4-157 heterocysts L-1. Significant discrepancies between absolute abundances were noted between cell and gene-based approaches to biomass determination (nifH copies L-1 were up to 102-103 higher than cell concentrations). Potential explanations for these striking discrepancies are discussed. Using the maximum N2 fixation rates per cell found in the existing literature for these genera, we estimate potential N2 fixation rates via these large diazotroph communities to be between 0.01-1.5 nmol N L-1 d-1. When comparing these rates to available 15N2 tracer measurements, we conclude that large diazotrophs were generally minor (50% of measured N2 fixation rates. While these large cell-sized and heterogeneously distributed organisms may still disproportionately contribute to export, cell-abundance based rate estimates suggests that other diazotrophs are largely responsible for N2 fixation rates measured in bottle-based incubations.

Highlights

  • The biological reduction of dinitrogen gas (N2) into ammonia by certain genera of oceanic microorganisms represents the largest incoming flux of nitrogen to the global ocean (Galloway et al, 2004)

  • In the oligotrophic North Pacific Subtropical Gyre (NPSG), isotopic models indicate that N2 fixation is directly or indirectly responsible for 26–47% of the particulate N that is exported from the euphotic zone (Böttjer et al, 2017)

  • Diazotrophic organisms in this ecosystem range from unicellular cyanobacterial symbionts to small and generally free-living cyanobacteria such as Crocosphaera spp. and heterotrophic diazotrophs (Church et al, 2005; Gradoville et al, 2017b), to more conspicuous and large cell-sized diazotrophs such as Trichodesmium and symbioses of Richelia and Calothrix with various diatoms

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Summary

Introduction

The biological reduction of dinitrogen gas (N2) into ammonia (termed N2 fixation or diazotrophy) by certain genera of oceanic microorganisms represents the largest incoming flux of nitrogen to the global ocean (Galloway et al, 2004). In the oligotrophic North Pacific Subtropical Gyre (NPSG), isotopic models indicate that N2 fixation is directly or indirectly responsible for 26–47% of the particulate N that is exported from the euphotic zone (Böttjer et al, 2017) Diazotrophic organisms in this ecosystem range from unicellular cyanobacterial symbionts (termed Group A, Zehr et al, 1998, 2001) to small and generally free-living cyanobacteria such as Crocosphaera spp. and heterotrophic diazotrophs (Church et al, 2005; Gradoville et al, 2017b), to more conspicuous and large cell-sized diazotrophs such as Trichodesmium and symbioses of Richelia and Calothrix with various diatoms (termed DDAs, diatom-diazotroph assemblages). These latter, larger organisms have been recognized as important contributors to upper ocean productivity and the annual flux of organic matter to the mesopelagic of the NPSG (Scharek et al, 1999; Dore et al, 2002; Karl et al, 2012)

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