Abstract

Diel oscillations in primary and secondary production, growth, metabolic activity, and gene expression commonly occur in marine microbial communities in ocean surface waters. Diel periodicity of gene transcription has been demonstrated in photoautotrophic and heterotrophic microbes in both coastal and open ocean environments. To better define the spatiotemporal distribution and patterns of these daily oscillations, we investigated how diel periodicity in gene transcripts changed with depth from the surface waters to the upper mesopelagic. We postulated that diel oscillation of transcript abundances would diminish at greater depths across the collective microbial community due to decreasing light availability. The results showed that the number and total proportion of gene transcripts and taxa exhibiting diel periodicity were greatest in the shallow sunlit mixed layer, diminished rapidly with increasing depth to the base of the euphotic zone, and could not be detected in the mesopelagic. The results confirmed an overall decrease in microbial diel transcript oscillation with depth through the euphotic zone and suggested a relationship between abundance of diel oscillating transcripts and the daily integrated light exposure experienced by planktonic microbes in the water column. Local dissolved macronutrient concentration also appeared to influence the diel transcriptional patterns of specific microbial genes. The diminishing diel transcript oscillations found at increasing depths suggest that diel patterns of other microbial processes and interactions may likewise be attenuated at depth.

Highlights

  • Marine microbes dominate biomass, biodiversity, and metabolism in the oceans and form the foundation of marine food webs and major biogeochemical cycles on Earth (Azam and Malfatti, 2007; Falkowski et al, 2008)

  • Most microbial taxa detected in euphotic zone, including all taxa having their transcript maxima there, demonstrated statistically significant levels of diel oscillation, underscoring the significance of the diel cycling for microbial communities in the sunlit open ocean

  • Functional annotations of periodic transcripts confirmed the diversity of diel functions across this community especially in phytoplankton

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Summary

Introduction

Biodiversity, and metabolism in the oceans and form the foundation of marine food webs and major biogeochemical cycles on Earth (Azam and Malfatti, 2007; Falkowski et al, 2008). Marine phytoplankton are responsible for approximately one-half of global primary production, about 75% of which takes place in the vast oligotrophic gyres (Karl and Church, 2014). The largest gyre, the North Pacific Subtropical Gyre (NPSG), spans 2×107 km from 15°N to 35°N and from 135°E to 135°W (Sverdrup et al, 1946). Wind-driven mixing and seasonally stable temperatures in the NPSG produce a uniform, warm (>24°C), low-density surface mixed layer ranging from 20 to 100 m, which is separated year-round from the rest of the density-stratified water column (Karl and Church, 2017). The microbial community throughout the upper mixed layer experiences uniform low-nutrient conditions and the delivery of equal amounts of time-integrated solar irradiation, when overturning within the mixed layer.

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