Open AccessLarge and interacting effects of temperature and nutrient addition on stratified microbial ecosystems in a small, replicated, and liquid‐dominated Winogradsky column approach
Author(s) -
Suleiman Marcel,
Choffat Yves,
Daugaard Uriah,
Petchey Owen L.
Publication year - 2021
Publication title -
microbiologyopen
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.881
H-Index - 36
ISSN - 2045-8827
DOI - 10.1002/mbo3.1189
Subject(s) - anoxic waters , phototroph , water column , ecosystem , abiotic component , microbial ecology , ecology , microbial population biology , environmental science , aquatic ecosystem , nutrient , environmental change , stratification (seeds) , eutrophication , nutrient cycle , environmental chemistry , biology , chemistry , climate change , photosynthesis , bacteria , botany , seed dormancy , genetics , germination , dormancy
Aquatic ecosystems are often stratified, with cyanobacteria in oxic layers and phototrophic sulfur bacteria in anoxic zones. Changes in stratification caused by the global environmental change are an ongoing concern. Increasing understanding of how such aerobic and anaerobic microbial communities, and associated abiotic conditions, respond to multifarious environmental changes is an important endeavor in microbial ecology. Insights can come from observational and experimental studies of naturally occurring stratified aquatic ecosystems, theoretical models of ecological processes, and experimental studies of replicated microbial communities in the laboratory. Here, we demonstrate a laboratory‐based approach with small, replicated, and liquid‐dominated Winogradsky columns, with distinct oxic/anoxic strata in a highly replicable manner. Our objective was to apply simultaneous global change scenarios (temperature, nutrient addition) on this micro‐ecosystem to report how the microbial communities (full‐length 16S rRNA gene seq.) and the abiotic conditions (O 2 , H 2 S, TOC) of the oxic/anoxic layer responded to these environmental changes. The composition of the strongly stratified microbial communities was greatly affected by temperature and by the interaction of temperature and nutrient addition, demonstrating the need of investigating global change treatments simultaneously. Especially phototrophic sulfur bacteria dominated the water column at higher temperatures and may indicate the presence of alternative stable states. We show that the establishment of such a micro‐ecosystem has the potential to test global change scenarios in stratified eutrophic limnic systems.