Abstract

Ciliates in shallow alpine lakes are exposed to high levels of incident solar ultraviolet radiation (UVR). We observed the presence of specific sunscreen compounds, the mycosporine-like amino acids (MAAs), in several populations of Bursaridium, a relatively large ciliate species found in such lakes. The populations from 3 highly UV transparent lakes revealed the presence of 7 MAAs (MG, SH, PR, PI, AS, US, and PE) in total concentrations of 3.6–52.4 10−5 μg μg−1 dry weight (DW) per individual, whereas in one glacially turbid and less UV transparent lake, no MAAs were detected in the Bursaridium population. The MAAs in the ciliates generally reflected the composition and relative amounts of the lakes’ seston MAAs, assuming that the ciliates fed on MAA-rich plankton. We experimentally found that naturally acquired MAAs prevented ciliate mortality under simulated UVR and photosynthetically active radiation (PAR) conditions. We further tested the dietary regulation of the MAAs-content in the ciliates under artificial UVR and PAR exposure and found an increase in MAAs concentrations in all treatments. Our assumption was that several stress factors other than irradiation were involved in the synthesis or up-regulation of MAAs.

Highlights

  • In clear alpine lakes, the impact of solar ultraviolet radiation (UVR; 280–400 nm) is an essential factor influencing the life of planktonic communities

  • Differences in the optical appearance among the lakes are reflected by the Kd of UVR and photosynthetically active radiation (PAR) (Tables 1 and 3)

  • In HAI, we identified the same 2 mycosporine-like amino acids (MAAs) in Bursaridium over all sampling years: 89 ± 4% SH and 11 ± 4% AS in concentrations of 33.9 ± 21.0 10−5 μg μg−1 dry weight (DW); seston MAAs were detected in concentrations of 20.0 ± 4.5 μg [μg chlorophyll a (Chl-a)]−1, and proportions of MAAs were 86 ± 0% SH, 13 ± 0% AS, 1 ± 0% PI,

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Summary

Introduction

The impact of solar ultraviolet radiation (UVR; 280–400 nm) is an essential factor influencing the life of planktonic communities. One factor responsible for high UVR transparency in lake water is the low amount of allochthonous chromophoric dissolved organic material (CDOM; Morris et al 1995, Laurion et al 2000). Glacier-fed lake water is highly turbid and absorbs UVR at the surface level, and, plankton is almost never exposed to high incident UVR (Rose et al 2014, Kammerlander et al 2016). Depending on the turbidity conditions, including more or less exposure to UVR, planktonic organisms are well adapted to varying levels of the incident solar radiation (Sommaruga 2001)

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