Abstract

Diel vertical migration of zooplankton profoundly impacts the transport of nutrients and carbon through the water column. Despite the acknowledged importance of this active flux to ocean biogeochemistry, these contributions remain poorly constrained, in part because daily variations in metabolic rates are not considered or are modeled as simple functions of temperature. To address this uncertainty, we sampled the subtropical copepod Pleuromamma xiphias at 4- to 7-h intervals throughout the daily migration and measured rates of oxygen consumption, ammonium excretion, fecal pellet production and metabolic enzyme activity. No significant patterns were detected in rates of oxygen consumption or ammonium excretion for freshly caught animals over the diel cycle. Fecal pellet production was highest during mid-night, consistent with several hours of feeding near the surface. Surface feeding resulted in fecal pellet production at depth in the morning, providing direct evidence that active flux of particulate organic carbon occurs in this region. Electron transport system activity was highest during the afternoon, contrary to our prediction of reduced daytime metabolism. Activity of both glutamate dehydrogenase and citrate synthase increased during early night, reflecting higher capacity for excretion and aerobic respiration, respectively. Overall, these results show that activities of metabolic enzymes vary during diel vertical migration. The surprising observation of elevated afternoon enzyme activity coupled with daytime fecal pellet and ammonium production suggests that additional characterization of the daytime activity of migratory zooplankton is warranted.

Highlights

  • Diel vertical migration (DVM) of zooplankton is typified by the presence of migrators in the photic epipelagic during the night followed by their movement into deeper water during the day

  • This study demonstrates that the copepod P. xiphias exhibits varia­ tion in fecal pellet production and activity of metabolic enzymes as it undergoes DVM, supporting our hypothesis that circadian rhythms and other environmental factors beyond temperature create emergent pat­ terns in zooplankton physiology

  • Observed production of fecal pellets in deep water during morning indicates that surface feeding by migratory copepods contributes to active flux of particulate organic matter

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Summary

Introduction

Diel vertical migration (DVM) of zooplankton is typified by the presence of migrators in the photic epipelagic during the night followed by their movement into deeper water during the day These daily mi­ grations, during which individuals of a few millimeters in length or less travel hundreds of meters in a few hours, are thought to be energetically expensive. Through the excretion of nitroge­ nous compounds at depth, DVM reduces the availability of this limiting nutrient to phytoplankton in surface waters, influencing the potential for new production (Longhurst and Harrison, 1988) In many cases, this daily shuttling of material meets or exceeds the vertical transport associated with passively sinking particles (Hernandez-Leon et al, 2019a; Kobari et al, 2013; Steinberg et al, 2008). The magnitude and relative importance of active transport varies regionally and seasonally, but the factors driving this variation are poorly understood (Burd et al, 2010; Steinberg and Landry, 2017) and have been identified as a priority for future research on the biological pump (Burd et al, 2016)

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