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Synechococcus sp. PCC7002 Uses Peroxiredoxin to Cope with Reactive Sulfur Species Stress

Cyanobacteria are a widely distributed group of microorganisms in the ocean, and they often need to cope with the stress of reactive sulfur species, such as sulfide and sulfane sulfur. Sulfane sulfur refers to the various forms of zero-valent sulfur, including persulfide, polysulfide, and element su...

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Detalles Bibliográficos
Autores principales: Liu, Daixi, Chen, Jinyu, Wang, Yafei, Meng, Yue, Li, Yuanning, Huang, Ranran, Xia, Yongzhen, Liu, Huaiwei, Jiao, Nianzhi, Xun, Luying, Liu, Jihua
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Society for Microbiology 2022
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9426444/
https://www.ncbi.nlm.nih.gov/pubmed/35861504
http://dx.doi.org/10.1128/mbio.01039-22
Descripción
Sumario:Cyanobacteria are a widely distributed group of microorganisms in the ocean, and they often need to cope with the stress of reactive sulfur species, such as sulfide and sulfane sulfur. Sulfane sulfur refers to the various forms of zero-valent sulfur, including persulfide, polysulfide, and element sulfur (S(8)). Although sulfane sulfur participates in signaling transduction and resistance to reactive oxygen species in cyanobacteria, it is toxic at high concentrations and induces sulfur stress, which has similar effects to oxidative stress. In this study, we report that Synechococcus sp. PCC7002 uses peroxiredoxin to cope with the stress of cellular sulfane sulfur. Synechococcus sp. PCC7002 contains six peroxiredoxins, and all were induced by S(8). Peroxiredoxin I (PrxI) reduced S(8) to H(2)S by forming a disulfide bond between residues Cys(53) and Cys(153) of the enzyme. A partial deletion strain of Synechococcus sp. PCC7002 with decreased copy numbers of the prxI gene was more sensitive to S(8) than was the wild type. Thus, peroxiredoxin is involved in maintaining the homeostasis of cellular sulfane sulfur in cyanobacteria. Given that peroxiredoxin evolved before the occurrence of O(2) on Earth, its original function could have been to cope with reactive sulfur species stress, and that function has been preserved.