Abstract

The temporal variability of planktonic ciliates was studied in an extreme oligotrophic environment with special focus on trophic modes and size classes. Abundance, biomass, size classes, mixotrophy vs. heterotrophy, and species composition of planktonic ciliates were investigated focusing on temporal (samples collected on a monthly basis during 2019) and vertical (7 depth layers in the euphotic zone, from surface to 120 m) distribution at a coastal station in the oligotrophic Eastern Mediterranean. Abundance was in general very low (20 to 1150 cells L–1), except for September, which presented the highest abundance and biomass. Aloricate species dominated the ciliate community in all months and depths (% contribution from 77% in September to 99% in April). In general, oligotrichs presented maximum abundance at 2–10 m (except for June, July, and November: 100–120 m) whereas choreotrichs were more homogeneously distributed [and showed maxima at deep chlorophyll maximum (DCM)]. Small heterotrophs dominated the ciliate community at all depths and months, on average by 76% (they were 3 times more abundant than mixotrophs in terms of abundance and 2.5 times in terms of biomass). They were equally distributed both vertically and seasonally (and also in terms of size classes). In contrast, mixotrophs were found mainly at the surface layer to 20 m throughout the year, except for June and July (max at 100, 50 m). On average, 63% of integrated aloricate abundance was species <30 μm, of which 25% were mixotrophs. During the stratification period of May to November, the very small (<18 μm) and small (18–30 μm) mixotrophic species were distributed throughout the water column whereas the >50 μm mixotrophic species were found only above the DCM. In contrast, during the mixing period of December to May, mixotrophic ciliates were very few and were dominated by small and medium-sized species. It seems that mixotrophic and heterotrophic ciliates, on one hand, and the four size classes, on the other, are very distinct groups characterized by different distributions both vertically and seasonally. This may have important consequences for the structure and function of the microbial food web of which they are part, as well as for the carbon flow to the higher trophic levels of this oligotrophic environment in which ciliates are the main grazers.

Highlights

  • Ciliated protozoa are an important part of the microbial food web (Lynn and Montagnes, 1991; Pierce and Turner, 1992)

  • According to the group division by Flynn et al (2019), mixotrophic ciliates are part of non-constitutive mixotrophs (NCMs), a group represented by grazers capable of keeping the chloroplasts of their prey and using them to perform photosynthesis

  • Constitutive mixotrophs (CMs) are represented by organisms that perform photosynthesis but are able to take up carbon from their ingested prey

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Summary

Introduction

Ciliated protozoa are an important part of the microbial food web (Lynn and Montagnes, 1991; Pierce and Turner, 1992). They are traditionally considered to be microzooplanktonic, i.e., 20– 200 μm heterotrophic organisms; they are known to comprise mixotrophic forms (Blackbourn et al, 1973; LavalPeuto, 1986; McManus and Fuhrman, 1986; Stoecker and Silver, 1987; Stoecker et al, 1987; Laval-Peuto and Rassoulzadegan, 1988). Constitutive mixotrophs (CMs) are represented by organisms that perform photosynthesis but are able to take up carbon from their ingested prey. Studies conducted in oligotrophic marine environments report that in the neritic zone, about 40% of the microplanktonic ciliate fauna contains chloroplasts (Stoecker et al, 1987)

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