Coexistence of Microaerophilic, Nitrate-Reducing, and Phototrophic Fe(II) Oxidizers and Fe(III) Reducers in Coastal Marine Sediment

Author:

Laufer Katja1,Nordhoff Mark1,Røy Hans2,Schmidt Caroline1,Behrens Sebastian13,Jørgensen Bo Barker2,Kappler Andreas12

Affiliation:

1. Geomicrobiology, Center for Applied Geosciences, University of Tübingen, Tübingen, Germany

2. Center for Geomicrobiology, Department of Bioscience, Aarhus University, Aarhus, Denmark

3. Department of Civil, Environmental, and Geo-Engineering, University of Minnesota, Minneapolis, Minnesota, USA

Abstract

ABSTRACT Iron is abundant in sediments, where it can be biogeochemically cycled between its divalent and trivalent redox states. The neutrophilic microbiological Fe cycle involves Fe(III)-reducing and three different physiological groups of Fe(II)-oxidizing microorganisms, i.e., microaerophilic, anoxygenic phototrophic, and nitrate-reducing Fe(II) oxidizers. However, it is unknown whether all three groups coexist in one habitat and how they are spatially distributed in relation to gradients of O 2 , light, nitrate, and Fe(II). We examined two coastal marine sediments in Aarhus Bay, Denmark, by cultivation and most probable number (MPN) studies for Fe(II) oxidizers and Fe(III) reducers and by quantitative-PCR (qPCR) assays for microaerophilic Fe(II) oxidizers. Our results demonstrate the coexistence of all three metabolic types of Fe(II) oxidizers and Fe(III) reducers. In qPCR, microaerophilic Fe(II) oxidizers ( Zetaproteobacteria ) were present with up to 3.2 × 10 6 cells g dry sediment −1 . In MPNs, nitrate-reducing Fe(II) oxidizers, anoxygenic phototrophic Fe(II) oxidizers, and Fe(III) reducers reached cell numbers of up to 3.5 × 10 4 , 3.1 × 10 2 , and 4.4 × 10 4 g dry sediment −1 , respectively. O 2 and light penetrated only a few millimeters, but the depth distribution of the different iron metabolizers did not correlate with the profile of O 2 , Fe(II), or light. Instead, abundances were homogeneous within the upper 3 cm of the sediment, probably due to wave-induced sediment reworking and bioturbation. In microaerophilic Fe(II)-oxidizing enrichment cultures, strains belonging to the Zetaproteobacteria were identified. Photoferrotrophic enrichments contained strains related to Chlorobium and Rhodobacter ; the nitrate-reducing Fe(II) enrichments contained strains related to Hoeflea and Denitromonas . This study shows the coexistence of all three types of Fe(II) oxidizers in two near-shore marine environments and the potential for competition and interrelationships between them.

Funder

EC | European Research Council

Publisher

American Society for Microbiology

Subject

Ecology,Applied Microbiology and Biotechnology,Food Science,Biotechnology

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