Abstract

Kongsfjorden is a small Arctic fjord but with great hydrographic complexity and has changed greatly due to the climate change. Arctic warming has increased melts of sea ice and glaciers that results in higher freshwater content. Microbial community variability and increasing terrestrial input were detected continuously in recent years ITag eukaryotic 18S rRNA V4 metabarcoding, photosynthetic pigments analysis and epifluorescence microscopy were used to reveal the dominant species of small eukaryotic community (<20 μm). Both Spearman correlation and redundant analysis were used to study the correlation between the small eukaryotes and the environmental conditions. In the present study, the surface water with salinity lower than 34 was thicker than in summers of previous years. The freshwater mixotrophic chrysophyte Poterioochromonas malhamensis was found for the first time as the dominant species. No general trends were found for the contributions of P. malhamensis to the total reads of small eukaryotes in water depths; and no obvious differences were found at different stations and water masses. Phagotrophy, which is more common than phototrophy at all times in P. malhamensis, is thought to be the main reason for the prevalence of P. malhamensis in Kongsfjorden. The occurrence of P. malhamensis induced a disorder in the small eukaryotic community, which biodiversity and composition showed weak correlation with the water masses. The dominance of the freshwater-originating phytoplankton may indicate an ecosystem change in the Kongsjforden, which probably might become more remarkable in the future as the climate continues to change.

Highlights

  • Microbes with a diameter of less than 20 μm are fundamental components of marine food webs [1]

  • The occurrence of P. malhamensis induced a disorder in the small eukaryotic community, which biodiversity and composition showed weak correlation with the water masses

  • The abundance of bacteria and diatom were determined by epifluorescence microscopy of filters stained with 40,6-diamidino-2-phenylindole (DAPI) [24]

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Summary

Introduction

Microbes with a diameter of less than 20 μm are fundamental components of marine food webs [1]. Global warming is responsible for glacier retreat, increased inflow of meltwater and inorganic suspended sediments, and salinity and temperature fluctuations in the fjord [3,9,12]. This study is different from all the previous ones because it presents the first time that a small mixotrophic phytoflagellate outcompeted the marine phytoplankton in the coastal water of Kongsfjorden. It represents a new phenomenon, that consisted in a small freshwater mixotrophic phytoflagellate outcompeting the marine phytoplankton in Arctic coastal marine water It is very interesting, and we confirmed the prevalence of this phytoflagellate with DNA boarding, characteristic pigment, and microscopic observation. Both biotic and abiotic aspects were analyzed to find the cause of the prevalence of a freshwater phytoflagellate in a marine environment

Sampling and Environmental Factors Analyses
Sampling sites in Kongsfjorden ofK1
Phytoplankton Identification by HPLC Pigment Analysis
Microbial Community Biomass Obtained by Epifluorescence Microscopy
Statistical Analysis of Microbial and Environmental Factors
Water Masses and Physicochemical Factors in the Study Area
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