1. Secondary products and molecular mechanism of calcium oxalate degradation by the strain Azospirillum sp. OX-1.
- Author
-
Xia D, Nie W, Li X, Finlay RD, and Lian B
- Subjects
- Proteomics methods, Calcium Carbonate metabolism, Biodegradation, Environmental, Methane metabolism, Bacterial Proteins metabolism, Bacterial Proteins genetics, Carboxy-Lyases metabolism, Carboxy-Lyases genetics, Calcium Oxalate metabolism, Soil Microbiology
- Abstract
The oxalate-carbonate pathway (OCP) involves degradation of soil oxalate to carbonate. To exploit and manage this natural mineralization of assimilated atmospheric CO
2 into stable carbonates, improved understanding of this complex biotransformation process is needed. A strain of oxalate-degrading bacteria, Azospirillum sp. OX-1, was isolated from soil, and its secondary products of calcium oxalate degradation were analyzed and characterized using SEM, XRD, TG/DTG-DTA and FTIR-spectroscopy. The molecular mechanism of calcium oxalate degradation was also analyzed using proteomics. The results showed, for the first time, that OX-1 could not only degrade calcium oxalate to calcium carbonate, but also that the process was accompanied by synthesis of methane. Proteomic analysis demonstrated that OX-1 has a dual enzyme system for calcium oxalate degradation, using formyl-CoA transferase (FRC) and thiamine pyrophosphate (ThDP)-dependent oxalyl-CoA decarboxylase (OXC) to form calcium carbonate. Up-regulated expression of enzymes related to methane synthesis was also detected during calcium oxalate degradation. Since methane is also a potent greenhouse gas, these new results suggest that the utility of exploiting the OCP to reduce atmospheric CO2 must be re-evaluated and that further studies should be conducted to reveal how widespread the methane producing capacity of strain OX-1 is in other bacteria and soil environments., (© 2024. The Author(s).)- Published
- 2024
- Full Text
- View/download PDF