S. R. Ali et al.
Bull. Chem. Soc. Jpn., 77, No. 9 (2004) 1685
Table 6. Percent Binding of Ribonucleotides on Metal Hexacyanochromates(III)
aÞ
0
0
0
0
Metal hexacyanochromates(III)
5 -AMP
5 -GMP
5 -CMP
5 -UMP
Cobalt(II) hexacyanochromates(III)
Cadmium(II) hexacyanochromates(III)
34.25
24.66
41.56
30.52
32.17
24.25
28.62
23.42
a) % binding ¼ fðO.D. before adsorption ꢃ O.D. after adsorptionÞ=O.D. before adsorptiong ꢄ 100.
Table 7. Langmuir Constants for Ribonucleotides Adsorption on Metal Hexacyanochromates(III)
Cobalt(II) chromicynide
Cadmium(II) chromicynide
Ribose
nucleotides
Xm
KL
3
Xm
KL
3
ꢃ1
ꢃ1
ꢃ1
ꢃ1
/
mg g
/dm mol
/mg g
/dm mol
0
5
5
5
5
-AMP
-GMP
-CMP
-UMP
16.55
18.82
13.71
12.72
6.57
8.28
7.06
6.51
13.36
14.20
10.85
10.07
4.04
8.27
6.67
4.76
0
0
0
cleotides was observed, which indicates an interaction between
the ribonucleotides and metal hexacyanochromates(III). The
characteristic infrared spectral frequencies are summarized in
Tables 4 and 5. In the infrared spectra of ribonucleotides, typi-
Earth,’’ Prentice Hall, Inc., Englewood Cliffs, N.J. (1974),
pp. 83–117.
2
1979).
3
S. C. Bondy and M. E. Harrington, Science, 203, 1243
(
ꢃ1
C. Ponnamperuma, A. Shimoyama, and E. Frieble, Origins
cal strong bands in the region 950–1150 cm are due to the
Life, 12, 9 (1982).
4 D. J. Greenland, R. H. Laby, and J. P. Quirk, Trans.
Faraday Soc., 58, 829 (1962).
presence of the ribose residue, and change negligibly after ad-
sorption. This suggests that the ribose residue does not interact
with metal hexacyanochromates(III). A remarkable shift was
observed in the characteristic frequencies of the purine nucleus
and phosphate group of ribonucleotides, which suggested a
probable involvement of N-7 and the phosphate groups in
5
D. J. Greenland, R. H. Laby, and J. P. Quirk, Trans.
Faraday Soc., 61, 2013 (1965).
D. J. Greenland, R. H. Laby, and J. P. Quirk, Trans.
Faraday Soc., 61, 2024 (1965).
6
0
the interaction of the 5 -ribonucleotides with the metal hexa-
7
8
M. M. Mortland, Adv. Agron., 22, 75 (1970).
B. K. G. Theng, ‘‘Chemistry of Clay of Organic Reaction,’’
cyanochromates(III). Typical infrared frequencies of metal
hexacyanochromates(III) were found to be almost unchanged,
suggesting that the ribonucleotide molecules do not enter into
the coordination sphere of metal hexacyanochromates(III) by
replacing the cyanide ion. Further, insertion of ribonucleotide
in the coordination sphere of a metal hexacyanochromate(III)
Wiley, New York (1974).
9
A. Weiss, ‘‘Organic Geochemistry,’’ ed by G. Eglinton and
M. T. J. Murphy, Springer-Verlag, New York (1969), p. 737.
1
1
0
1
N. Lahav and S. Chang, J. Mol. Evol., 8, 357 (1976).
P. Liebmann, G. Loew, S. Burt, J. Lawless, and R. D.
ꢃ
is quite improbable, because CN can be substituted by other
Maceroy, Inorg. Chem., 21, 1586 (1982).
12 J. P. Ferris and W. J. Hagan, Origins Life Evol. Biosphere,
17, 69 (1986).
13 J. P. Ferris, C. H. Huang, and W. J. Hagan, Origins Life
Evol. Biosphere, 18, 121 (1988).
ligands only under UV light.31 Thus, it seems that the interac-
tion of ribonucleotides with metal hexacyanochromates(III)
takes place through certain chemical forces. Ribonucleotides
interact through their purine or pyrimidine residue and phos-
phate group with metal cations present in the lattice of metal
hexacyanochromates(III).
14 J. P. Ferris, G. Ertem, and V. K. Agarwal, Origins Life
Evol. Biosphere, 19, 153 (1989).
1
5
J. P. Ferris and Kamaluddin, Origins Life Evol. Biosphere,
9, 609 (1989).
K. Kobayashi and C. Ponnamperuma, Origins Life Evol.
Biosphere, 16, 41 (1985).
The results of the present study support the postulate that
metal cyanogen complexes could have provided a surface onto
which biomonomers could have concentrated from their dilute
aqueous solutions through adsorption processes during the
course of chemical evolution. The biomonomers so concentrat-
ed would have been protected from degradation and might
have undergone a reaction such as condensation, oligomerisa-
tion and/or polymerization to produce biopolymers. Thus,
metal cyanogen complexes played an important role during
the course of chemical evolution.
1
1
6
1
1
7
8
F. Egami, J. Biochem., 77, 1165 (1975).
M. T. Beck, ‘‘Metal Ion in Biological System,’’ ed by
H. Sigel, Marcel Dekker, New York (1978), Vol. 7, p. 1.
G. Arrhenius, ‘‘Fourth Symposium on Chemical Evolution
1
9
and Origin and Evolution of Life,’’ NASA Am. Research Centre,
Moffet Field, July 24–27 (1990).
2
0
Kamaluddin, M. Nath, S. W. Deopujari, and A. Sharma,
Origins Life Evol. Biosphere, 20, 259 (1990).
Kamaluddin, M. Nath, and A. Sharma, Origins Life Evol.
Biosphere, 24, 469 (1994).
S. Viladkar, A. Rachana, and Kamaluddin, Bull. Chem.
Soc. Jpn., 69, 95 (1996).
T. Alam and Kamaluddin, Bull. Chem. Soc. Jpn., 72, 1697
(1999).
This research work was sponsored by the Indian Space
Research Organisation, Bangalore (India).
2
1
2
2
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