Search bioRxiv⌕ Search

Biology subjects

Hach, P.

Publications and source records attributed to Hach, P..

2 recordsLinked to original sources

Seagrass excretes sugars to their rhizosphere making them the sweet spots in the sea

Seagrasses are one of the most efficient sinks of carbon dioxide on Earth1: They bury carbon 35 times faster than tropical rainforests on a per unit area basis2. While we know that carbon sequestration in terrestrial plants is intimately linked to the microorganisms living in their soils3-6, the interactions of seagrasses with their rhizospheres are poorly understood. We show that three seagrass species from two oceans excrete simple sugars, mainly sucrose, into their rhizosphere that accumulate to over 200 {micro}M. Such high concentrations are at least 80 times higher than previously observed in the ocean, and surprising, as sugars are quickly consumed by microorganisms. In situ analyses and incubation experiments indicated that phenolic compounds from the seagrass inhibited microbial consumption of sucrose. Metagenomic and metatranscriptomic analyses of the microbial communities in the seagrass rhizosphere revealed that many members had the genes for degrading sucrose, but these were only expressed by a few specialists that also expressed genes for degrading phenolics. Our results explain why sucrose accumulates under seagrass meadows, where it comprises as much as 40% of the dissolved organic carbon. Destruction of extant seagrass canopies would allow sediment microorganisms to consume the tremendous deposits of sucrose buried underneath their meadows, thereby releasing large amounts of CO2 into the oceans and atmosphere.

microbiology↗

Dark aerobic sulfide oxidation by anoxygenic phototrophs in the anoxic waters of Lake Cadagno

SUMMARYAnoxygenic phototrophic sulfide oxidation by green and purple sulfur bacteria (PSB) plays a key role in sulfide removal from anoxic shallow sediments and stratified waters. Although some PSB can also oxidize sulfide with nitrate and oxygen, little is known about the prevalence of this chemolithotrophic lifestyle in the environment. In this study, we investigated the role of these phototrophs in light-independent sulfide removal in the chemocline of Lake Cadagno. Our temporally resolved, high-resolution chemical profiles indicated that dark sulfide oxidation was coupled to high oxygen consumption rates of ~9 M O2{middle dot}h-1. Single-cell analyses of lake water incubated with 13CO2 in the dark revealed that Chr. okenii was to a large extent responsible for aerobic sulfide oxidation and it accounted for up to 40 % of total dark carbon fixation. The genome of Chr. okenii reconstructed from the Lake Cadagno metagenome confirms its capacity for microaerophilic growth and provides further insights into its metabolic capabilities. Moreover, our genomic and single-cell data indicated that other PSB grow microaerobically in these apparently anoxic waters. Altogether, our observations suggest that aerobic respiration may not only play an underappreciated role in anoxic environments, but also that organisms typically considered strict anaerobes may be involved.\n\nORIGINALITY-SIGNIFICANCE STATEMENTThis study reveals that dark aerobic sulfide oxidation within an anoxic layer dominated by anoxygenic phototrophic bacteria in the stratified water column of Lake Cadagno is to a large extent carried out by the anoxygenic phototrophic bacterium Chromatium okenii. Our findings imply that aerobic metabolisms may be more prevalent in anoxic zones than previously thought. We also present an environmental metagenome-assembled genome of Chr. okenii which is the first genome sequence for the genus Chromatium and reveals new interesting physiological features of this environmentally relevant organism, including its capacity for aerobic respiration.

microbiology↗