[Diversity and community characteristics of organic phosphate-mineralizing bacteria in the sea area between Minjiang Estuary to Pingtan.] / 闽江口-å¹³æ½­æµ·åŸŸæœ‰æœºè§£ç£·èŒå¤šæ ·æ€§åŠç¾¤è½ç‰¹å¾.

Microbial mineralization of organic phosphorus is an important component of marine phosphorus cycle. The research on organic phosphate-mineralizing bacteria (OPB) is helpful to reveal microbial driving mechanism of organic phosphorus mineralization in eutrophic sea area. The diversity and community characteristics of OPB were examined by Illumina high-throughput sequencing using the primer sets phoX in the sea area between Minjiang Estuary to Pingtan in April (spring) and July (summer) 2019. The results showed that the Shannon index of OPB in the surface seawater samples ranged from 3.21 to 7.91, and that the diversity at each station was greater in spring than that in summer. Shannon index of OPB in the sediment samples ranged from 2.04 to 8.70, which was greater in summer than that in spring. Shannon index of OPB in surface seawater of each station was higher than that of sediment in spring, while it was in adverse in summer. Nine phyla of OPB were detected in surface seawater, with Proteobacteria and Cyanobacteria being the most abundant. Tweleve phyla of OPB were detected in the sediments, with Proteobacteria and Bacteroidetes being the most dominant. OPB community composition at the genus level showed obvious spatio-temporal variation. Leisingera, Phaeobacter, Thalassococcus, and Pseudomonas were the major genera in the seawater in spring, while Synechococcus, Halioglobus, Roseovarius, Phaeo-bacter, Sulfitobacter, and Hyphomonas were the major genera detected in summer. Leisingera, Phaeobacter, Vibrio, and Sulfitobacter were major genera in the sediment in spring, while Azospirillum, Aminobacter, Sulfurifustis, Burkholderia, and Thiohalobacter were the major genera in summer. A large number of unclassified OPB were detected in both surface seawater and sediment. The redundancy analysis results showed that dissolved oxygen, water temperature, pH, dissolved inorganic nitrogen, NO2--N, and NO3--N had great influences on community distribution of OPB in the surface seawater. The abundant OPB in the surface seawater and sediment might play an important role in phosphorus cycle in this sea area.

[Community characteristics of polyphosphate accummulating organisms in the heart sediment of three reservoirs in Fujian Province, China.] / 福建省3座水库库心沉积物聚磷菌的群落特征.

Polyphosphate accummulating organisms (PAOs) play an important role in the phosphorus metabolic cycling in the sediment of reservoir. We assessed the diversity and community structure of PAOs in the sediments by T-RFLP and clone sequencing which targeted ppk1 gene at the hearts of three reservoirs (Jiulongjiangxipi reservoir, Sanshiliujiao lake reservoir and Dongyaxi reservoir) in Fujian Province. The results showed that the diversity of PAOs varied among different reservoirs, though not statistically significant. The diversity of PAOs in the Sanshiliujiao lake reservoir was highest (Shannon index H=2.89±0.03, Simpson index D=0.06±0.01). The community structure of the PAOs in the Sanshiliujiao lake reservoir was most complicated, consistent with the results of the T-RFLP. The differences of dominant PAOs genera in three reservoirs were distinct, mainly concentrated in the Proteobacteria, Actinobacteria and Acidobacteria. The percentage of those three phylum accounted for 74.5%, 85.0% and 75.0%, respectively, of the total PAOs. The dominant groups in each reservoir sediment were Anaeromyxobacter and Solibacter. Various forms of phosphorus had certain influence on the diversity of PAOs. There were significantly correlation between Fe/Al-P and PAOs diversity and community structure. The dominant genus in the three reservoirs, Anaeromyxobacter, was positively correlated with all forms of phosphorus and significantly correlated with insoluble phosphorus such as OP and Ca-P, while Solibacter was negatively correlated with all forms of phosphorus. The results suggested that PAOs had important impacts on the phosphorus cycle of sediment in eutrophicatied reservoirs.

The theoretical study of excited-state intramolecular proton transfer of 2,5-bis(benzoxazol-2-yl)thiophene-3,4-diol.

The symmetrical structures 2,5-bis(benzoxazol-2-yl)thiophene-3,4-diol (BBTD) can take shape two intramolecular hydrogen bonds in chloroform. In order to research the molecular dynamic behavior of BBTD upon photo-induced process, we utilize density functional theory (DFT) and time-dependent density functional theory (TDDFT) to complete theoretical calculation. Through the comparison of bond length, bond angle, IR spectra, and frontier molecular orbitals between ground state (S0) and first excited state (S1), it clearly indicates that photoexcitation have slightly influence for intensity of hydrogen bond. For the sake of understanding the mechanism of excited state intramolecular proton transfer (ESIPT) of BBTD in chloroform, potential energy surfaces have been scanned along with the orientation of O1-H2 and O4-H5 in S0 and S1 state, respectively. A intrigued hydrogen bond dynamic phenomenon has been found that ESIPT of BBTD is not a synergetic double proton transfer process, but a stepwise single proton transfer process BBTD→BBTD-S→BBTD-D. Moreover, the proton transfer process of BBTD-S→BBTD-D is easier to occur than that of BBTD→BBTD-S in S1 state.