Abstract

The occurrence and activity of aerobic methanotrophs are influenced by environmental conditions, including pH, temperature, salinity, methane and oxygen concentrations, and nutrient availability. Aerobic methanotrophs synthesize a variety of lipids important for cell functions. However, culture-based experiments studying the influence of environmental parameters on lipid production by aerobic methanotrophs are scarce. Such information is crucial to interpret lipid patterns of methanotrophic bacteria in the environment. In this study, the alkaliphilic strain Methylotuvimicrobium alcaliphilum was cultivated under different salinities and different nitrate concentrations to assess the effect of changing conditions on the inventory of pentacyclic triterpenoids. The results indicate that hopanoid abundance is enhanced at lower salinity and higher nitrate concentration. The production of most pentacyclic triterpenoids was favored at low salinity, especially for aminotriol. Interestingly, 3-methyl-aminotetrol and tetrahymanol were favored at higher salinity. Bacteriohopanepolyols (BHPs), particularly aminotriol and 3-methyl-aminotriol, increased considerably at higher nitrate concentrations. Four novel N-containing BHPs—aminodiol, 3-methyl-aminodiol, and isomers of aminotriol and 3-methyl-aminotriol—were identified. This study highlights the significance of environmental factors for bacterial lipid production and documents the need for cultivation studies under variable conditions to utilize the full potential of the biomarker concept.

Highlights

  • Aerobic methanotrophic bacteria are an important methane sink due to their ability to utilize methane as the sole carbon and energy source, using the key enzyme monooxygenase (Hanson and Hanson 1996; Semrau et al 2010)

  • Bacterial aerobic methane oxidation (MOx) contributes significantly to the withdrawal of methane released from anoxic sediments and soils, which otherwise could accumulate in the atmosphere as a severe greenhouse gas

  • In addition to the amino-BHPs previously reported for M. alcaliphilum (IIIb, IVb, V, and VI; Figs. 2, 3), the highperformance liquid chromatography–mass spectrometry (HPLC–MS) analysis revealed the presence of four novel components with base peaks at m/z 656, m/z 670, m/z 714 (IIIa) and m/z 728 (IVa), respectively ([M + ­H]+; Figs. 2, 3)

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Summary

Introduction

Aerobic methanotrophic bacteria are an important methane sink due to their ability to utilize methane as the sole carbon and energy source, using the key enzyme monooxygenase (Hanson and Hanson 1996; Semrau et al 2010). Bacterial aerobic methane oxidation (MOx) contributes significantly to the withdrawal of methane released from anoxic sediments and soils, which otherwise could accumulate in the atmosphere as a severe greenhouse gas. Geomikrobiologie, Zentrum für Angewandte Geowissenschaften, Universität Tübingen, Tübingen, Germany essential for methane consumption (Hanson and Hanson 1996; Sherry et al 2016). Aerobic methanotrophs occur in terrestrial, freshwater, and marine ecosystems, preferably at oxic-anoxic interfaces. Aerobic methanotrophic bacteria are microaerophilic, using oxygen as electron acceptor and methane as carbon and energy source (Boetius and Wenzhöfer 2013; Bessette et al 2017). Aerobic methanotrophs are divided into two major groups, belonging to the Gammaproteobacteria (Type I and Type X methanotrophs) and Alphaproteobacteria (Type II methanotrophs), which differ in physiology, chemotaxonomy, internal ultrastructure, carbon assimilation pathways, and other biochemical aspects (Bowman 2006)

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