A hot origin of dissimilatory sulfite reduction catalyzed by DsrAB in the Paleoarchean EraOA
Dissimilatory sulfite reduction(DSR)has been essential to microbial energy metabolism in the biogeochemical sulfur cycle since the Paleoarchean Era.However,due to the lack of an integrated assessment of geological record and genomic data,the evolutionary origin of DSR remains elusive in terms of time,habitat,and genetic basis.In this study,we reconstructed the evolutionary pathways and the ancestral sequences of Dsr proteins by mining metagenomes ranging from mesothermal to hyperthermal environments.A phylogenetic analysis of the key catalytic enzyme,DsrAB,and other Dsr proteins indicates that the earliest and most basic functional cascade,DsrABCNM,emerged prior to the latest common ancestor of several basal branching DsrAB clusters encoded by bacteria and archaea.Using a molecular dating strategy that calibrates the protein tree with a species tree,we predicted that the DSR originated 3.508 billion years ago(Ga).This finding strongly confirms the earliest geological evidence of DSR(~3.47 Ga).Further predictions from ancestral sequence reconstruction indicate that the optimal catalytic temperature of DsrA at the time of DSR origin was approximately 73℃,which is consistent with the petrographic and geochemical evidence in early Archean hydrothermal deposits.After its hot origin,DsrA diversified into subclades that adapted to various temperature levels following the Great Oxidation Event.This is exemplified by the evolution of the reductive archaeal-type DsrA.Our results synchronize the molecular ages with the geological record,which advances our understanding of the earliest DSR systems and highlights the enzymatic adaptations of microbial life in the Archean biosphere.
Lingyun Tang;Zhenhao Luo;Shaoming Gao;Zhiliang Lin;Mengqi Sun;Runsheng Li;Shu-Hong Gao;Geng Wu;Yiliang Li;Linan Huang;Lu Fan
Department of Ocean Science and Engineering,Southern University of Science and Technology(SUSTech),Shenzhen,ChinaState Key Laboratory of Biocontrol,Guangdong Provincial Key Laboratory of Plant Resources and Southern Marine Science and Engineering Guangdong Laboratory(Zhuhai),School of Life Sciences,Sun Yat-Sen University,Guangzhou,ChinaSchool of Life Sciences,Sun Yat-Sen University,Guangzhou,ChinaSchool of Life Sciences,Sun Yat-Sen University,Guangzhou,ChinaDepartment of Ocean Science and Engineering,Southern University of Science and Technology(SUSTech),Shenzhen,ChinaDepartment of Infectious Diseases and Public Health,Jockey Club College of Veterinary Medicine and Life Sciences,City University of Hong Kong,Hong Kong,ChinaState Key Laboratory of Urban Water Resource and Environment,School of Civil&Environmental Engineering,Harbin Institute of Technology,Shenzhen,ChinaState Key Laboratory of Geomicrobiology and Environmental Changes,China University of Geosciences,Wuhan,ChinaDepartment of Earth Sciences,The University of Hong Kong,Hong Kong,ChinaSchool of Life Sciences,Sun Yat-Sen University,Guangzhou,ChinaDepartment of Ocean Science and Engineering,Southern University of Science and Technology(SUSTech),Shenzhen,China
生物科学
archaeal evolutiondsrABmetagenomicssulfite reductionsulfur cycling
《mLife》 2026 (1)
P.108-121,14
supported by the National Key R&D Program of China(No.2024YFA0919700 to L.F.)the National Natural Science Foundation of China(Nos.32300001 to Z.Luo and 42206122 to M.S.)the Natural Science Foundation of Guangdong Province(No.2025A1515010753 to L.H.)the Guangdong Basic and Applied Basic Research Foundation(No.2021B1515120080 to L.F.)the Shenzhen Key Laboratory of Marine Archaea Geo-Omics,Southern University of Science and Technology(No.ZDSYS201802081843490 to L.F.).
评论