Stoichiometry of natural bacterial assemblages from lakes located across an elevational gradient

Abstract Heterotrophic bacteria are thought to be phosphorus-rich organisms with relatively homeostatic stoichiometry, but the elemental composition of natural bacterial communities has rarely been assessed. Here we tested whether bacterial stoichiometry changes with the trophic status of lakes by a...

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Main Authors: Birgit Stenzel, Carina Rofner, Maria Teresa Pérez, Ruben Sommaruga
Format: Article
Language:English
Published: Nature Publishing Group 2017-07-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-017-06282-0
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spelling doaj-e4f7b6c1e878407ba6e2912a8295331c2020-12-08T01:36:52ZengNature Publishing GroupScientific Reports2045-23222017-07-017111010.1038/s41598-017-06282-0Stoichiometry of natural bacterial assemblages from lakes located across an elevational gradientBirgit Stenzel0Carina Rofner1Maria Teresa Pérez2Ruben Sommaruga3University of Innsbruck, Institute of EcologyUniversity of Innsbruck, Institute of EcologyUniversity of Innsbruck, Institute of EcologyUniversity of Innsbruck, Institute of EcologyAbstract Heterotrophic bacteria are thought to be phosphorus-rich organisms with relatively homeostatic stoichiometry, but the elemental composition of natural bacterial communities has rarely been assessed. Here we tested whether bacterial stoichiometry changes with the trophic status of lakes by assessing the elemental composition of the bacterial-dominated (hereafter microbial) fraction together with that of the dissolved and seston fractions in 11 lakes situated along an elevational gradient. The stoichiometry of these three size-fractions was analyzed during the thermal stratification and mixing periods in composite water samples and in the water layer of the deep chlorophyll-a maximum. In addition, we analyzed the relative abundance of the most common bacterial groups in the lakes. Our results show that the microbial fraction was always enriched in phosphorus compared to the dissolved fraction, irrespectively of the lake trophic status. Further, they indicate that the elemental composition of bacteria in mountain lakes is at least seasonally very dynamic, resulting not only from changes in the nutrient ratios of the resource itself, but probably from changes in the composition of the dominant bacterial taxa too, though at the taxonomic level analyzed, we did not find evidence for this.https://doi.org/10.1038/s41598-017-06282-0
collection DOAJ
language English
format Article
sources DOAJ
author Birgit Stenzel
Carina Rofner
Maria Teresa Pérez
Ruben Sommaruga
spellingShingle Birgit Stenzel
Carina Rofner
Maria Teresa Pérez
Ruben Sommaruga
Stoichiometry of natural bacterial assemblages from lakes located across an elevational gradient
Scientific Reports
author_facet Birgit Stenzel
Carina Rofner
Maria Teresa Pérez
Ruben Sommaruga
author_sort Birgit Stenzel
title Stoichiometry of natural bacterial assemblages from lakes located across an elevational gradient
title_short Stoichiometry of natural bacterial assemblages from lakes located across an elevational gradient
title_full Stoichiometry of natural bacterial assemblages from lakes located across an elevational gradient
title_fullStr Stoichiometry of natural bacterial assemblages from lakes located across an elevational gradient
title_full_unstemmed Stoichiometry of natural bacterial assemblages from lakes located across an elevational gradient
title_sort stoichiometry of natural bacterial assemblages from lakes located across an elevational gradient
publisher Nature Publishing Group
series Scientific Reports
issn 2045-2322
publishDate 2017-07-01
description Abstract Heterotrophic bacteria are thought to be phosphorus-rich organisms with relatively homeostatic stoichiometry, but the elemental composition of natural bacterial communities has rarely been assessed. Here we tested whether bacterial stoichiometry changes with the trophic status of lakes by assessing the elemental composition of the bacterial-dominated (hereafter microbial) fraction together with that of the dissolved and seston fractions in 11 lakes situated along an elevational gradient. The stoichiometry of these three size-fractions was analyzed during the thermal stratification and mixing periods in composite water samples and in the water layer of the deep chlorophyll-a maximum. In addition, we analyzed the relative abundance of the most common bacterial groups in the lakes. Our results show that the microbial fraction was always enriched in phosphorus compared to the dissolved fraction, irrespectively of the lake trophic status. Further, they indicate that the elemental composition of bacteria in mountain lakes is at least seasonally very dynamic, resulting not only from changes in the nutrient ratios of the resource itself, but probably from changes in the composition of the dominant bacterial taxa too, though at the taxonomic level analyzed, we did not find evidence for this.
url https://doi.org/10.1038/s41598-017-06282-0
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