Biology subjects

Kurth, J. M.

Publications and source records attributed to Kurth, J. M..

3 recordsLinked to original sources

bioRxiv2023

Differences in the regulation mechanisms of the glutamine synthetase from methanogenic archaea unveiled by structural investigations

Glutamine synthetases catalyze the ATP-dependent ammonium assimilation, the initial step of nitrogen acquisition that must be tightly regulated to fit cellular needs. While their catalytic mechanisms and regulation are well-characterized in bacteria and eukaryotes, only limited knowledge exists about the archaeal representatives. Here, we natively purified the glutamine synthetases type I- from Methanothermococcus thermolithotrophicus and Methermicoccus shengliensis, two thermophilic methanogens belonging to different orders. Biochemical investigations combined with X-ray crystallography unveiled the first structures of archaeal glutamine synthetases and highlighted differences in their regulation. The enzyme from M. thermolithotrophicus is inactive in its resting state and employs 2-oxoglutarate as an on-switch. The 2-oxoglutarate acts as a sensor of cellular nitrogen deficiency, and its reported cellular concentration remarkably overlays with that required for the enzyme activation. Its binding to an allosteric pocket leads to the reconfiguration of the active site and promotes a catalytically competent state. The homolog from M. shengliensis does not harbor the 2-oxoglutarate binding motif and, consequently, is 2-oxoglutarate insensitive. Instead, it is directly feedback-inhibited by glutamine, as shown for bacterial homologs. The glutamine inhibition depends on a key arginine residue from the Asp50-loop. The arginine is substituted by a glycine in M. thermolithotrophicus, abolishing the inhibitory effect. While the effectors are surprisingly different, the molecular switch controlling the glutamine synthetase activity is fundamentally the same and depends on the correct positioning of the Asp50-loop and a catalytic arginine. Residue conservation suggests that both regulation mechanisms are widespread and not mutually exclusive across archaea.

biochemistry↗

bioRxiv2021

Unraveling nitrogen, sulfur and carbon metabolic pathways and microbial community transcriptional responses to substrate deprivation and toxicity stresses in a bioreactor mimicking anoxic brackish coastal sediment conditions

Microbial communities are key drivers of carbon, sulfur and nitrogen cycling in coastal ecosystems, where they are subjected to dynamic shifts in substrate availability and exposure to toxic compounds. However, how these shifts affect microbial interactions and function is poorly understood. Unraveling such microbial community responses is key to understand their environmental distribution and resilience under current and future disturbances. Here, we used metagenomics and metatranscriptomics to investigate microbial community structure and transcriptional responses to prolonged ammonium deprivation and sulfide and nitric oxide toxicity stresses in a controlled bioreactor system mimicking coastal sediment conditions. Candidatus Nitrobium versatile, identified in this study as a sulfide-oxidizing denitrifier, became a rare community member upon ammonium removal. The methanotroph Ca. Methanoperedens nitroreducens showed remarkable resilience to both experimental conditions, dominating transcriptional activity of dissimilatory nitrate reduction to ammonium (DNRA). After the ammonium removal experiment, a novel methanotroph species that we have named Ca. Methylomirabilis tolerans outcompeted Ca. Methylomirabilis lanthanidiphila and the anaerobic ammonium oxidizer (anammox) Ca. Kuenenia stuttgartiensis outcompeted Ca. Scalindua rubra. At the end of the sulfide and nitric oxide experiment, a gammaproteobacterium affiliated to the family Thiohalobacteraceae was enriched and dominated transcriptional activity of sulfide:quinone oxidoreductase. Our results indicate that some community members could be more resilient to stresses than others in coastal ecosystems, leading to dynamic microbial community shifts and novel functional states. Methane and sulfide oxidation could be ecosystem functions preserved across the investigated disturbances, while differing nitrogen cycling pathways might be favored in response to stresses. ImportanceCoastal ecosystems are primary zones of biogeochemical cycling, processing inputs of nutrients both generated in situ and derived from land runoff. Microbial communities that inhabit costal sediments perform these biogeochemical reactions, but microbial responses to dynamic, periodic substrate deprivation and exposure to toxic compounds remain elusive. In this study, we sought to address this knowledge gap in a controlled bioreactor system, unraveling microbial metabolic pathways and monitoring microbial responses to stresses that might occur in costal sediments. We identified key microbial players and shifts in their abundance and transcriptional activity. Our results indicated that methanotrophs were particularly resilient to stresses, sulfide oxidizers differed in resiliency but the community maintained sulfide oxidation function across stresses, and that anaerobic ammonium oxidizing (anammox) bacteria were sensitive to substrate deprivation but could restore activity once favorable conditions were reestablished. These insights will help to understand and predict coastal ecosystem responses to future disturbances.

microbiology↗

bioRxiv2019

ANME-2d anaerobic methanotrophic archaea differ from other ANME archaea in lipid composition and carbon source

The anaerobic oxidation of methane (AOM) is a microbial process present in marine and freshwater environments. AOM is important for reducing the emission of the second most important greenhouse gas methane. In marine environments anaerobic methanotrophic archaea (ANME) are involved in sulfate-reducing AOM. In contrast, Ca. Methanoperedens of the ANME-2d cluster carries out nitrate AOM in freshwater ecosystems. Despite the importance of those organisms for AOM in non-marine environments not much is known about their lipid composition or carbon sources. To close this gap, we analyzed the lipid composition of ANME-2d archaea and found that they mainly synthesize archaeol and hydroxyarchaeol as well as different (hydroxy-) glycerol dialkyl glycerol tetraethers, albeit in much lower amounts. Abundant lipid headgroups were dihexose, monomethyl-phosphatidyl ethanolamine and phosphatidyl hexose. Moreover, a monopentose was detected as a lipid headgroup which is rare among microorganisms. Batch incubations with 13C labelled bicarbonate and methane showed that methane is the main carbon source of ANME-2d archaea varying from ANME-1 archaea which primarily assimilate dissolved inorganic carbon (DIC). ANME-2d archaea also assimilate DIC, but to a lower extent than methane. The lipid characterization and analysis of the carbon source of Ca. Methanoperedens facilitates distinction between ANME-2d and other ANMEs.

microbiology↗