Y. Inoue et al.
aldehyde and CO (Scheme 1, bottom row). Experimentally,
the detection of propene, a photodecomposition product
from isovaleraldehyde, in the photolyzed solution (Table 2)
may support this mechanism (Scheme 1, middle right).
On the other hand, we are less certain about the potential
roles of different ice phases in controlling the photobehavior
as we cooled the sample solutions at a constant rate to the
designated temperatures and no literature information is
available on the phases of ice matrices containing 7–30 mm
rac-Leu (and HCl). However, the experimental results ob-
tained in this study (i.e., no clear jump is observed in con-
version or product yield at the phase transition tempera-
tures) suggest that the photobehavior is not significantly af-
fected by the phase transitions from metastable phase I
cubic (Ic) to phase I hexagonal (Ih) and then to phase XI ob-
served upon cooling pure ice,[22] or more likely the ice matri-
ces containing Leu and/or HCl are amorphous in nature and
hence experience no clear phase transition.
From the point of view of the chemical evolution, it is cru-
cial that not only the CPL photoreaction of rac-amino acids
in ice has been experimentally proven to proceed under in-
terstellar conditions, but also that the major photoreaction
mechanisms and products have been elucidated. These re-
sults substantiate the cosmic scenario in which interstellar
ice analogues containing simple starting materials irradiated
by VUV light produce a mixture of racemic amino acids[10]
that subsequently photodecompose enantioselectively by
CPL radiated from the star-formation region en route to
primitive Earth.
Conclusion
In this study, we have identified the major volatile and non-
volatile products obtained upon direct irradiation of Leu in
aqueous solutions and also in ice matrices. Based on the re-
sults of the product study, we have discussed the photo-
chemical behavior of Leu (as a representative aliphatic
amino acid) in acidic and neutral media at temperatures
ranging from 298 to 21 K to reveal that the photoreaction
mechanism and the major products derived therefrom are
critical functions of the phase, temperature, and pH of the
media.
In acidic media, the overall photoreaction is greatly decel-
erated by lowering the irradiation temperature, particularly
below the freezing point, and the main photoreaction mech-
anism switches from the Norrish-type II g-hydrogen abstrac-
tion, which affords Gly and isobutene, to SNi deamination to
give isobutyl-a-lactone, which is trapped in situ and subse-
quently photodecarbonylated to isovaleraldehyde in ice ma-
trices.
However, the enantiomeric excesses obtained in the CPL
photolysis of aliphatic amino acids are generally low (0.1–
2.6% ee),[12,16a,b,17] including the present case. It has been
shown that the enantioselectivity obtained by CPL photode-
composition of a racemic mixture is highly conversion-de-
pendent and can be enhanced to 90% ee and even to 99%
ee at 88 and 96% conversion, respectively, if the g factor is
1.0.[11] In reality, the g factors of aliphatic amino acids, in-
cluding Leu (Figure 1), are typically 0.02 or slightly higher
at the irradiation wavelength (215 nm).[23] This means that
an ee of 4.6% will be achieved at 99% conversion and fur-
thermore that the last single molecule will have statistically
48% ee on average even when one mole of an amino acid
with g=0.02 is subjected to CPL photolysis.[11] Hence, the
unexpectedly high ee values of up to 50–60% reported re-
cently by Pizzarello and co-workers[3] for nonterrestrial iso-
leucine and allo-isoleucine extracted from the Murchison
and other meteorites, and also by Glavin et al.[3m] for nonter-
restrial proteinogenic aspartic acid and glutamic acid from
two out of the three examined fragments of the Tagish Lake
meteorite, are evidently unexplainable by the CPL photode-
composition mechanism alone and indicate the operation of
other mechanisms such as preferential crystallization to con-
glomerates[24] during the aqueous alteration in a meteorite
parent body.[3m] Nevertheless, it is also worth noting that es-
sentially all of the proteinogenic amino acids found in the
Tagish Lake meteorite are l-enriched,[3m] which suggests a
certain seeding or biasing mechanism to trigger the enantio-
meric imbalance in which the CPL photodecomposition
would have played some role.
In neutral media, the photoreaction proceeds consistently
by the SNi deamination mechanism to give the a-lactone,
which is followed by the nucleophilic attack of water leading
to a-hydroxyisocaproic acid in aqueous solutions at ambient
temperatures or alternatively by photodecarbonylation to
isovaleraldehyde in ice matrices at cryogenic temperatures.
The overall efficiency of the photoreaction is surprisingly in-
sensitive to the irradiation temperature (and medium),
maintaining the same level of conversion throughout the
temperature range examined (21–298 K). This suggests that
the SNi deamination survives as the major photoreaction
process under interstellar conditions (10–20 K).
Intriguingly, the photoreaction mechanism converges to
the deamination process in both acidic and neutral media at
temperatures below 77 K. This indicates that the amino acid
exists in its zwitterionic form in ice matrices at lower tem-
peratures, irrespective of the original pH at 298 K, because
the deamination occurs only upon excitation of the carboxy-
late moiety of a zwitterionic amino acid.[12,19a,20a] In this con-
nection, it is crucial to point out that the dissociation of HCl
adsorbed on an ice surface is discouraged at low temperatur-
es[21a,b] and HCl on amorphous ice at 70 K is totally molecu-
lar[21a.c] whereas around 85% of HCl is molecular in ice
nanocrystals at 60 K.[21d] This means that HCl becomes more
molecular, or less acidic, at lower temperatures and that it is
difficult to protonate zwitterionic amino acid in ice matrices.
This shift in equilibrium rationalizes the switching of the
major photoreaction mechanism from the g-hydrogen ab-
straction by an excited carboxylic acid to the SNi deamina-
tion by an excited carboxylate (Scheme 1).
13934
ꢀ 2013 Wiley-VCH Verlag GmbH & Co. KGaA, Weinheim
Chem. Eur. J. 2013, 19, 13929 – 13936