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Molecular basis of hyper-thermostability in the thermophilic archaeal aldolase MfnB.


ABSTRACT: Methanogenic archaea are chemolithotrophic prokaryotes that can reduce carbon dioxide with hydrogen gas to form methane. These microorganisms make a significant contribution to the global carbon cycle, with methanogenic archaea from anoxic environments estimated to contribute > 500 million tons of global methane annually. Archaeal methanogenesis is dependent on the methanofurans; aminomethylfuran containing coenzymes that act as the primary C1 acceptor molecule during carbon dioxide fixation. Although the biosynthetic pathway to the methanofurans has been elucidated, structural adaptations which confer thermotolerance to Mfn enzymes from extremophilic archaea are yet to be investigated. Here we focus on the methanofuran biosynthetic enzyme MfnB, which catalyses the condensation of two molecules of glyceralde-3-phosphate to form 4‑(hydroxymethyl)-2-furancarboxaldehyde-phosphate. In this study, MfnB enzymes from the hyperthermophile Methanocaldococcus jannaschii and the mesophile Methanococcus maripaludis have been recombinantly overexpressed and purified to homogeneity. Thermal unfolding studies, together with steady-state kinetic assays, demonstrate thermoadaptation in the M. jannaschii enzyme. Molecular dynamics simulations have been used to provide a structural explanation for the observed properties. These reveal a greater number of side chain interactions in the M. jannaschii enzyme, which may confer protection from heating effects by enforcing spatial residue constraints.

SUBMITTER: Maddock RMA 

PROVIDER: S-EPMC11365854 | biostudies-literature | 2024 Aug

REPOSITORIES: biostudies-literature

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Molecular basis of hyper-thermostability in the thermophilic archaeal aldolase MfnB.

Maddock Rosie M A RMA   Marsh Carl O CO   Johns Samuel T ST   Rooms Lynden D LD   Duke Phillip W PW   van der Kamp Marc W MW   Stach James E M JEM   Race Paul R PR  

Extremophiles : life under extreme conditions 20240831 3


Methanogenic archaea are chemolithotrophic prokaryotes that can reduce carbon dioxide with hydrogen gas to form methane. These microorganisms make a significant contribution to the global carbon cycle, with methanogenic archaea from anoxic environments estimated to contribute > 500 million tons of global methane annually. Archaeal methanogenesis is dependent on the methanofurans; aminomethylfuran containing coenzymes that act as the primary C<sub>1</sub> acceptor molecule during carbon dioxide f  ...[more]

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