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Table 1 Measurements of ozone concentrations by bioluminescence,
iodometric titration and UV spectroscopy methods (mean Æ s.d., n = 3)
Ozone
concentration (mM)
Sample
solution (nM)
Bioluminescence method 10.0 Æ 0.69 20.0 Æ 1.1 53.5 Æ 0.62
Iodometric titration
UV spectroscopy
9.73 Æ 0.50 19.6 Æ 1.3 N/A
10.4 Æ 0.66 21.2 Æ 1.7 N/A
N/A: not applicable. A sample solution was obtained at the main gate of
Yonsei University.
higher in areas with heavy automobile traffic. Moreover, ozone in
each of the samples could not be detected by using iodometric
titration and UV spectroscopy methods, which are typically
Fig. 2 Responses of (A) 1 and (B) 2 to various ROS. A solution of each probe
(
2 mM) in potassium phosphate buffer (5 mM, pH 7.0) was treated with 20 mM
1
ꢀ
À À
ꢀ
3
O , 1 mM
O
2
, 1 mM H
2
O
2
, 1 mM OH, 1 mM O
2
, 1 mM ClO or
myeloperoxidase (40 nM)–H
2
O
2
(200 mM)–NaCl (150 mM). After incubation employed to measure micromolar concentrations of this ROS.
for 1 h, luciferase in assay buffer was added to the mixture, and then bio- This observation demonstrates that the newly developed probe is
luminescence intensity was measured by using a bioluminescence microplate
reader (error bar: mean Æ s.d., n = 3). ‘Un’ in each graph means ‘untreated’.
highly sensitive to ozone.
In conclusion, in this investigation we designed and synthe-
sized the first bioluminescent probe that selectively and sensi-
ozone but not to other ROS, indicating their high levels of tively responds to ozone. We demonstrated the application of one
selectivity (Fig. 2).
of the probes for measuring ozone concentrations in environ-
The sensitivities of 1 and 2 for O
3
detection were determined mental samples. It is anticipated that the bioluminescence-based
next. Bioluminescence intensities of 1 and 2 linearly correlate probes may show great potential in detecting ozone in environ-
with ozone concentrations in the 0–400 nM (0–15 ppb) range mental and biological samples.
and the detection limits of 1 and 2 were determined to be 1.0 Â
This work was supported financially by a grant from the National
M, respectively (Fig. S8, ESI†). Because 1 Creative Research Initiative (2010-0018272) Program in Korea.
À11
À10
10
and 1.1 Â 10
exhibits a greater luminescence increase induced by ozone than
does 2, the former probe was used in further studies.
Recently, it was reported that amino acids, including tryptophan
Notes and references
1
(a) B. C. Dickinson and C. J. Chang, Nat. Chem. Biol., 2011, 7, 504;
(b) X. Chen, X. Tian, I. Shin and J. Yoon, Chem. Soc. Rev., 2011, 40, 4783.
M. K. Pulfer and R. C. Murphy, J. Biol. Chem., 2004, 279, 26331.
(a) P. Wentworth Jr, J. E. McDunn, A. D. Wentworth, C. Takeuchi,
J. Nieva, T. Jones, C. Bautista, J. M. Ruedi, A. Gutierrez, K. D. Janda,
B. M. Babior, A. Eschenmoser and R. A. Lerner, Science, 2002,
(Trp), methionine (Met), cysteine (Cys) and histidine (His), in
2
3
aqueous solutions generate ozone-like species upon UV irradiation
11
in the presence of 6-formylpterin (6-FP). To ascertain whether
ozone is generated in these processes, solutions of 1 (20 mM), 6-FP
2
98, 2195; (b) B. M. Babior, C. Takeuchi, J. Ruedi, A. Gutierrez and
P. Wentworth, Jr., Proc. Natl. Acad. Sci. U. S. A., 2003, 100, 3031;
c) P. Jr. Wentworth, J. Nieva, C. Takeuchi, R. Galve, A. D.
(100 mM) and the individual amino acids were irradiated for 5 min
by using a UVA irradiation apparatus according to the previously
(
11
reported procedure. As in the previous study, Indigo carmine was
used as the chemical probe. As the data given in Fig. S9A (ESI†)
show, the UV absorbance of indigo carmine at 610 nm is attenu-
ated in a concentration-dependent manner in irradiated solutions
containing Trp, Met, Cys and His, but not in those containing other
amino acids. This finding indicates that indigo carmine is con-
verted to isatin sulfonic acid, a phenomenon which is fully
Wentworth, R. B. Dilley, G. A. DeLaria, A. Saven, B. M. Babior,
K. D. Janda, A. Eschenmoser and R. A. Lerner, Science, 2003,
3
02, 1053; (d) K. Yamashita, T. Miyoshi, T. Arai, N. Endo, H. Itoh,
K. Makino, K. Mizugishi, T. Uchiyama and M. Sasada, Proc. Natl.
Acad. Sci. U. S. A., 2008, 105, 16912.
4
5
J. Brinkhorst, S. J. Nara and D. A. Pratt, J. Am. Chem. Soc., 2008,
1
30, 12224.
(a) L. Garner, C. M. St Croix, B. R. Pitt, G. D. Leikauf, S. Ando and
K. Koide, Nat. Chem., 2009, 1, 316; (b) Y. Zhang, W. Shi, X. Li and
H. Ma, Sci. Rep., 2013, 3, 2830, DOI: 10.1038/srep02830; (c) K. Xu,
S. Sun, J. Li, L. Li, M. Qiang and B. Tang, Chem. Commun., 2012,
11
consistent with the previous results. Notably, the results show
that the bioluminescence intensity of 1 is not altered by its addition
to irradiated solutions containing 6-FP and each of Trp, Met, Cys
and His followed by incubation with luciferase and pyrrolidine
4
8, 684; (d) C. C. Beltr ´a n, E. A. Palmer, B. R. Buckley and F. Iza,
Chem. Commun., 2015, 51, 1579; (e) X. Li, X. Gao, W. Shi and H. Ma,
Chem. Rev., 2014, 114, 590.
(a) X. Chen, T. Pradhan, F. Wang, J. S. Kim and J. Yoon, Chem. Rev.,
6
(
Fig. S9B, ESI†). Because indigo carmine can react with ozone as
2011, 40, 4783; (b) Y. Yang, Q. Zhao, W. Feng and F. Li, Chem. Rev.,
12
well as other ROS, our findings suggest that ROS other than
ozone are likely produced in this system.
2013, 113, 192; (c) Z. Guo, S. Park, J. Yoon and I. Shin, Chem. Soc.
Rev., 2014, 43, 16.
J. Li, L. Chen, L. Du and M. Li, Chem. Soc. Rev., 2013, 42, 662.
Y. Ando, K. Niwa, N. Yamada, T. Enomoto, T. Irie, H. Kubota,
Y. Ohmiya and H. Akiyama, Nat. Photonics, 2008, 2, 44.
9 A. K. Leslie, D. Li and K. Koide, J. Org. Chem., 2011, 76, 6860.
0 S. L. Hazen, F. F. Hsu, D. M. Mueller, J. R. Crowley and
J. W. Heinecke, J. Clin. Invest., 1996, 98, 1283.
7
8
In the final phase of this effort, we demonstrated that probe 1
can be employed to detect O
convenient manner.
3
in environmental samples in a
For this purpose, open, wide mouth glass
bottles containing buffer solutions were placed at four different
5a,b
1
locations for 8 h. The ozone concentration of each sample was 11 K. Yamashita, T. Miyoshi, T. Arai, N. Endo, H. Itoh, K. Makino,
K. Mizugishi, T. Uchiyama and M. Sasada, Proc. Natl. Acad. Sci. U. S. A.,
determined by using probe 1. It was found that ozone concentra-
tions depend on the collection location (Table 1 and Fig. S10,
2008, 105, 16912.
1
2 A. J. Kettle, B. M. Clark and C. C. Winterbourn, J. Biol. Chem., 2004,
ESI†). Specifically, the ozone concentration was found to be much
279, 18521.
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