Cloned (Comment) | Organism |
---|---|
gene dacZ, DNA and amino acid sequence determination and analysis, phylogenetic tree, the Haloferax volcanii genome encodes one diadenylate cyclase (DAC). The dacZ gene is constantly expressed at different growth phases in rich and selective media. Recombinant overexpression of gene dacZ in HAloferax volcanii strain H26, A double auxotrophic background strain H98 (DELTApyrE2 DELTAhdrB) is also transformed with the dacZ-complementing plasmid [p-dacZ+ hdrB+] and subsequently subjected to identical unselective growth conditions. In these control experiments, several colonies auxotrophic for thymidine and hypoxanthine can be detected. Recombinant expression of His10-tagged DacZ in Escherichia coli strain Rosetta | Haloferax volcanii |
Protein Variants | Comment | Organism |
---|---|---|
additional information | transformation and construction of deletion mutants in Haloferax volcanii strain H26 based on selection with uracil, gene dacZ knockout and overexpression. Because neither gene deletion nor overexpression of dacZ had been possible, a promotor exchange approach is used to examine the effects of altered intracellular c-di-AMP levels. Two mutant strains are created where the native promotor of dacZ is replaced with the tryptophan-inducible promotor (p.tnaA) of the tryptophanase gene tnaA (HVO_0789) or, respectively, with a genetically engineered version of p.tnaA with about 50% reduced activity (with regard to p.tnaA) (p.tnaM3). In comparison to the wild type, the p.tnaA-dacZ strain exhibits in general slightly elevated OD600 values in this condition The p.tnaM3-induced mutant has a different phenotype as it exhibits a prolonged lag phase followed by an extended exponential phase that peaked at an increased maximal OD. Changed intracellular c-di-AMP levels causes increased cell volume in medium with low sodium chloride concentration, phenotypes, overview. When the expression of DacZ is reduced, it leads in turn to decreased c-di-AMP concentrations within the two mutant strains which leads to ta hypo-salt phenotype | Haloferax volcanii |
Metals/Ions | Comment | Organism | Structure |
---|---|---|---|
Mn2+ | required, specific for | Haloferax volcanii |
Natural Substrates | Organism | Comment (Nat. Sub.) | Natural Products | Comment (Nat. Pro.) | Rev. | Reac. |
---|---|---|---|---|---|---|
2 ATP | Haloferax volcanii | - |
2 diphosphate + cyclic di-3',5'-adenylate | - |
? | |
2 ATP | Haloferax volcanii NCIMB 2012 | - |
2 diphosphate + cyclic di-3',5'-adenylate | - |
? | |
2 ATP | Haloferax volcanii JCM 8879 | - |
2 diphosphate + cyclic di-3',5'-adenylate | - |
? | |
2 ATP | Haloferax volcanii DS2 | - |
2 diphosphate + cyclic di-3',5'-adenylate | - |
? | |
2 ATP | Haloferax volcanii DSM 3757 | - |
2 diphosphate + cyclic di-3',5'-adenylate | - |
? | |
2 ATP | Haloferax volcanii ATCC 29605 | - |
2 diphosphate + cyclic di-3',5'-adenylate | - |
? | |
2 ATP | Haloferax volcanii NBRC 14742 | - |
2 diphosphate + cyclic di-3',5'-adenylate | - |
? | |
2 ATP | Haloferax volcanii VKM B-1768 | - |
2 diphosphate + cyclic di-3',5'-adenylate | - |
? |
Organism | UniProt | Comment | Textmining |
---|---|---|---|
Haloferax volcanii | D4GZM5 | Halobacterium volcanii | - |
Haloferax volcanii ATCC 29605 | D4GZM5 | Halobacterium volcanii | - |
Haloferax volcanii DS2 | D4GZM5 | Halobacterium volcanii | - |
Haloferax volcanii DSM 3757 | D4GZM5 | Halobacterium volcanii | - |
Haloferax volcanii JCM 8879 | D4GZM5 | Halobacterium volcanii | - |
Haloferax volcanii NBRC 14742 | D4GZM5 | Halobacterium volcanii | - |
Haloferax volcanii NCIMB 2012 | D4GZM5 | Halobacterium volcanii | - |
Haloferax volcanii VKM B-1768 | D4GZM5 | Halobacterium volcanii | - |
Purification (Comment) | Organism |
---|---|
recombinant His10-tagged DacZ from Escherichia coli strain Rosetta by nickel affinity chromatography and dialysis | Haloferax volcanii |
Source Tissue | Comment | Organism | Textmining |
---|---|---|---|
additional information | gene dacZ is constantly expressed at different growth phases in rich and selective media | Haloferax volcanii | - |
Substrates | Comment Substrates | Organism | Products | Comment (Products) | Rev. | Reac. |
---|---|---|---|---|---|---|
2 ATP | - |
Haloferax volcanii | 2 diphosphate + cyclic di-3',5'-adenylate | - |
? | |
2 ATP | - |
Haloferax volcanii NCIMB 2012 | 2 diphosphate + cyclic di-3',5'-adenylate | - |
? | |
2 ATP | - |
Haloferax volcanii JCM 8879 | 2 diphosphate + cyclic di-3',5'-adenylate | - |
? | |
2 ATP | - |
Haloferax volcanii DS2 | 2 diphosphate + cyclic di-3',5'-adenylate | - |
? | |
2 ATP | - |
Haloferax volcanii DSM 3757 | 2 diphosphate + cyclic di-3',5'-adenylate | - |
? | |
2 ATP | - |
Haloferax volcanii ATCC 29605 | 2 diphosphate + cyclic di-3',5'-adenylate | - |
? | |
2 ATP | - |
Haloferax volcanii NBRC 14742 | 2 diphosphate + cyclic di-3',5'-adenylate | - |
? | |
2 ATP | - |
Haloferax volcanii VKM B-1768 | 2 diphosphate + cyclic di-3',5'-adenylate | - |
? | |
additional information | thin layer chromatography product determination. The DAC activity is specific for ATP as substrate and manganese (II) ions as cofactor | Haloferax volcanii | ? | - |
- |
|
additional information | thin layer chromatography product determination. The DAC activity is specific for ATP as substrate and manganese (II) ions as cofactor | Haloferax volcanii NCIMB 2012 | ? | - |
- |
|
additional information | thin layer chromatography product determination. The DAC activity is specific for ATP as substrate and manganese (II) ions as cofactor | Haloferax volcanii JCM 8879 | ? | - |
- |
|
additional information | thin layer chromatography product determination. The DAC activity is specific for ATP as substrate and manganese (II) ions as cofactor | Haloferax volcanii DS2 | ? | - |
- |
|
additional information | thin layer chromatography product determination. The DAC activity is specific for ATP as substrate and manganese (II) ions as cofactor | Haloferax volcanii DSM 3757 | ? | - |
- |
|
additional information | thin layer chromatography product determination. The DAC activity is specific for ATP as substrate and manganese (II) ions as cofactor | Haloferax volcanii ATCC 29605 | ? | - |
- |
|
additional information | thin layer chromatography product determination. The DAC activity is specific for ATP as substrate and manganese (II) ions as cofactor | Haloferax volcanii NBRC 14742 | ? | - |
- |
|
additional information | thin layer chromatography product determination. The DAC activity is specific for ATP as substrate and manganese (II) ions as cofactor | Haloferax volcanii VKM B-1768 | ? | - |
- |
Synonyms | Comment | Organism |
---|---|---|
Dac | - |
Haloferax volcanii |
dacZ | - |
Haloferax volcanii |
Temperature Optimum [°C] | Temperature Optimum Maximum [°C] | Comment | Organism |
---|---|---|---|
37 | - |
assay at | Haloferax volcanii |
pH Optimum Minimum | pH Optimum Maximum | Comment | Organism |
---|---|---|---|
7.5 | - |
assay at | Haloferax volcanii |
General Information | Comment | Organism |
---|---|---|
evolution | enzyme DacZ belongs to the proposed DacZ subfamily, sequence and structure comparisons with other DACs. The adenylate cyclase domains of proteins of the DacZ and DacY/CdaZ classes are found in a similar branch of the tree, which is distinct from other bacterial and archaeal classes, and this branch also contains several bacterial proteins. Homologues are identified in most euryarchaeal species, but no DACs are identified in crenarchaeota | Haloferax volcanii |
malfunction | a strain with decreased c-di-AMP levels exhibits an increased cell area in hypo-salt medium, implying impaired osmoregulation. Homologous overexpression of DacZ leads to cell death. Changed intracellular c-di-AMP levels causes increased cell volume in medium with low sodium chloride concentration | Haloferax volcanii |
physiological function | the DAC encoding gene (dacZ) is essential, but homologous overexpression of DacZ leads to cell death, suggesting the need for tight regulation of c-di-AMP levels. A central target of c-di-AMP signaling in bacteria is cellular osmohomeostasis and a comparable function in euryarchaeon Haloferax volcanii is suggested. Osmoregulation is likely to be a common function of c-di-AMP in bacteria and archaea | Haloferax volcanii |