Abstract

CL500-11 (phylum Chloroflexi) is one of the most ubiquitous and abundant bacterioplankton lineages in deep freshwater lakes inhabiting the oxygenated hypolimnion. While metagenomics predicted possible eco-physiological characteristics of this uncultured lineage, no consensus on their ecology has so far been reached, partly because their niche is not clearly understood due to a limited number of quantitative field observations. This study investigated the abundance and distribution of CL500-11 in seven deep perialpine lakes using catalyzed reporter deposition-fluorescence in situ hybridization (CARD-FISH). Samples were taken vertically (5–12 depths in each lake) and temporally (in two lakes) at the deepest point of the lakes located in Switzerland, Italy, and Austria with varying depth, trophic state, mixing regime, and water retention time. The results showed a dominance of CL500-11 in all the lakes; their proportion to total prokaryotes ranged from 4.3% (Mondsee) to 24.3% (Lake Garda) and their abundance ranged from 0.65 × 105 (Mondsee) to 1.77 × 105 (Lake Garda) cells mL-1. By summarizing available information on CL500-11 occurrence to date, we demonstrated their broad habitat spectrum, ranging from ultra-oligotrophic to meso-eutrophic lakes, while low abundances or complete absence was observed in lakes with shallow depth, low pH, and/or short water retention time (<1 year). Together with available metagenomic and geochemical evidences from literatures, here we reviewed potential substrates supporting growth of CL500-11. Overall, the present study further endorsed ubiquity and quantitative significance of CL500-11 in deep freshwater systems and narrowed the focus on their physiological characteristics and ecological importance.

Highlights

  • In thermally stratified lakes, the water layer below the thermocline is defined as hypolimnion

  • The present study aims to measure the abundances of CL500-11 in seven deep perialpine lakes by means of CARD-FISH

  • The CL500-11 cells detected by CARDFISH were of the same size and shape as previously described (Okazaki et al, 2013, 2017; Denef et al, 2016; Mehrshad et al, 2018), indicating universality of their cell morphology

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Summary

Introduction

The water layer below the thermocline is defined as hypolimnion. Catalyzed reporter deposition-fluorescence in situ hybridization (CARD-FISH) revealed a dominance of CL500-11 in the hypolimnia of Lake Biwa (Japan, 16.5% of the total bacterioplankton in maximum) (Okazaki et al, 2013), Lake Michigan (United States, 18.1%) (Denef et al, 2016), six deep Japanese lakes (3.9–25.9% in each lake) (Okazaki et al, 2017), and Lake Zurich (Switzerland, 11%) (Mehrshad et al, 2018) Despite their high abundances in deep water layers, CL500-11 were barely detected in the epilimnia during the stratification period, indicating their specificity to the hypolimnion (Okazaki et al, 2013, 2017; Okazaki and Nakano, 2016). This dynamic population succession suggests ecological and biogeochemical significance of CL500-11 in deep lakes’ ecosystems

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