An abiotic formation of meso- and DL-tartrates in 80% yield via the cyanide-catalyzed dimerization of glyoxylate under alkaline conditions is demonstrated. A detailed mechanism for this conversion is proposed, supported by NMR evidence and (13)C-labeled reactions. Simple dehydration of tartrates to oxaloacetate and an ensuing decarboxylation to form pyruvate are known processes that provide a ready feedstock for entry into the citric acid cycle. While glyoxylate and high hydroxide concentration are atypical in the prebiotic literature, there is evidence for natural, abiotic availability of each. It is proposed that this availability, coupled with the remarkable efficiency of tartrate production from glyoxylate, merits consideration of an alternative prebiotic pathway for providing constituents of the citric acid cycle.
An abiotic formation of meso- and DL-tartrates in 80% yield via the cyanide-catalyzed dimerization of glyoxylate under alkaline conditions is demonstrated. A detailed mechanism for this conversion is proposed, supported by NMR evidence and (13)C-labeled reactions. Simple dehydration of tartrates to oxaloacetate and an ensuing decarboxylation to form pyruvate are known processes that provide a ready feedstock for entry into the citric acid cycle. While glyoxylate and high hydroxide concentration are atypical in the prebiotic literature, there is evidence for natural, abiotic availability of each. It is proposed that this availability, coupled with the remarkable efficiency of tartrate production from glyoxylate, merits consideration of an alternative prebiotic pathway for providing constituents of the citric acid cycle.
The emergence of primordial metabolism
has been postulated to play
a central role in the origins of life.[1] Many of the investigations so far have centered on the reductive
citric acid cycle.[2,3] However, in his “glyoxylate
scenario”,[4] Eschenmoser theorized
that glyoxylate 1 may have played an important role in
the development of a primordial metabolism, acting as a primal source
for biogenic molecules such as sugars, amino acids, and nucleobases.
Crucial to the scenario was the hypothetical formation of dihydroxyfumarate
(DHF) 5, by dimerization of glyoxylic acid under the
influence of an umpolung catalyst such as cyanide.[5] DHF was proposed to undergo reaction with glyoxylate and
aldoses, ultimately yielding biologically relevant α-keto acids
and sugars, respectively.[4] Subsequently
it was shown by Sagi et al.[6] that the reaction
of DHF with glyoxylate, glycolaldehyde, and glyceraldehyde led, via
α-keto acid intermediates, to the formation of triose, tetrulose,
and pentuloses, with remarkable efficiency. This success emphasized
the need to demonstrate the formation of DHF from glyoxylate. To this
end, we set out to investigate the cyanide-mediated dimerization of
glyoxylate (“glyoxoin reaction”) with the expectation
of chemistry similar to the benzoin reaction.[7] Herein we report the results of this investigation: the unanticipated
formation of meso- and dl-tartrates
(the formal reduction products of DHF) rapidly and in high yield (Scheme 1). We also present evidence that the glyoxoin reaction
proceeds via DHF as a putative intermediate, thus strengthening the
proposals made in the “glyoxylate scenario”.[4] This facile production of tartrate combined with
the known dehydration of tartrate to give oxaloacetate,[8] and its decarboxylation to give pyruvate,[9] potentially, provides an alternate entry into
the citric acid cycle based on the “glyoxylate scenario”.[4]
Scheme 1
Cyanide-Mediated Dimerization of Glyoxylate
Leads Predominantly to
Tartrates and Oxalate
Cyanide-Mediated Dimerization of Glyoxylate
The (homogeneous)
glyoxoin reaction of glyoxylate (1.0 M) with
a catalytic amount of NaCN (0.1 M) in aqueous medium at room temperature
in 2.0 M NaOH (pH ≈ 14) showed complete consumption of glyoxylate
(by 13C NMR after 28 h); no signals corresponding to the
expected DHF were observed. (High pH was required to ensure cyanide
was present only as its anion; however pH 14 was obtained when 2.0
M NaOH was prepared rather than 0.5 M.) Rather, the 13C
NMR spectrum of the crude reaction mixture (Figure 1) suggested the formation of meso- and dl-tartrates 8 in high yields (in some cases exceeding
80%, see Table S1 for example calculations)
along with carbonate, oxalate 9, formate 11, tartronate 12, and glycolate 13. The
identities of products were confirmed by comparison to and by spiking
with authentic materials (Figure S1). In
addition, the tartrates were isolated from the reaction mixture as
calcium salts according to literature procedure[10] and confirmed by 13C NMR spectroscopy and mass
spectrometry (Figure S2). The meso-tartrate is produced in equal or greater quantity than the combined dl-tartrates (Table S1).
No interconversion of meso-tartrate to and from dl-tartrates (nor conversion to any other reaction
product) was observed under reaction conditions (Figure S3).
Figure 1
Typical 13C NMR of the glyoxoin reaction. Reaction
of
1.0 M sodium glyoxylate (182/94 ppm, completely consumed) with 0.1
M cyanide (167 ppm) in aqueous 2.0 M NaOH (room temperature, 1 h)
produces meso-tartrate 8 (178.9/76.1
ppm) and dl-tartrates 8 (179.8/75.0
ppm). Signals for carbonate (169.1 ppm), oxalate 9 (173.6
ppm), formate 11 (172 ppm), tartronate 12 (179.7/76.2 ppm), and glycolate 13 (trace, 181.4/62.4
ppm) were observed. CD3OD was used as external standard
(49.15 ppm).
Typical 13C NMR of the glyoxoin reaction. Reaction
of
1.0 M sodium glyoxylate (182/94 ppm, completely consumed) with 0.1
M cyanide (167 ppm) in aqueous 2.0 M NaOH (room temperature, 1 h)
produces meso-tartrate 8 (178.9/76.1
ppm) and dl-tartrates 8 (179.8/75.0
ppm). Signals for carbonate (169.1 ppm), oxalate 9 (173.6
ppm), formate 11 (172 ppm), tartronate 12 (179.7/76.2 ppm), and glycolate 13 (trace, 181.4/62.4
ppm) were observed. CD3OD was used as external standard
(49.15 ppm).The glyoxoin reaction
also produced tartrates at lower concentrations
(0.01 M of 1 and 0.002 M CN–) and at
lower temperatures (4 °C). The reaction is, in fact, so resilient
that even under heterogeneous conditions (when insoluble lithium glyoxylate
was substituted in place of sodium glyoxylate), tartrates were still
produced (Figure S4). However, when the
pH was lowered (pH ≈ 9), tartrates were not observed, indicating
that high pH was crucial. When a control reaction (at pH ≈
14) was conducted by omitting the cyanide ion, no tartrates were formed;
only the disproportionation of glyoxylate to glycolate 13 and oxalate 9 was observed, proceeding through the
well-known Cannizzaro reaction (Figure S5C).[11,12]
Reaction of DHF with Glyxoylate
The production of tartrates (as opposed to DHF) from the glyoxoin
reaction in basic media was unanticipated but did implicate DHF as
an intermediate, since tartrate is formally the reduction product
of DHF. Therefore, a reaction of DHF 5 (5 mmol, insoluble),
NaCN (1 mmol/0.1 M), and glyoxylic acid (5 mmol/0.5 M) in aqueous
NaOH (2.0 M/10 mL) at room temperature was investigated. A vigorous
bubbling was observed in this heterogeneous reaction mixture for ∼2
h, at which point a 13C NMR spectrum of the supernatant
showed the production of tartrates 8 along with carbonate,
oxalate 9, formate 11, tartronate 12, and glycolate 13. More revealingly, when
the DHF/glyoxylate reaction was repeated, omitting the cyanide, tartrates 8 were still formed. When the reaction of 0.25 M of DHF 5 with 0.25 M glyoxylic acid (in the absence of cyanide) was
repeated in a mixture of 1.0 M NaOH and 1.0 M LiOH, the reaction mixture
became homogeneous (similar to the glyoxoin reaction). 13C NMR spectrum, after 1 h, showed production of tartrates 8, (in 69% yield by quantitative 13C NMR) with complete
glyoxylate conversion and little carbonate formation (Figure 2); the ratios of the accompanying product peaks
were similar to the glyoxoin reaction (Figure
S5A,B) with higher proportion of meso-tartrate
(Table S1). Interestingly, in the heterogeneous
case, the 13C NMR spectrum of the reaction was also nearly
identical to the glyoxoin reaction with the exception of a much more
intense carbonate peak (Figure S6B). In
both heterogeneous and homogeneous cases, these results demonstrated
that DHF could, by itself, mediate the transformation of glyoxylate
to tartrates (Figure S6).
Figure 2
Typical 13C NMR of the homogeneous DHF/glyoxylate (without
cyanide) reaction. Reaction of 0.25 M glyoxylate with 0.25 M DHF in
aqueous 1.0 M NaOH and 1M LiOH (room temperature, 1 h). For NMR details
see caption of Figure 1.
Typical 13C NMR of the homogeneous DHF/glyoxylate (without
cyanide) reaction. Reaction of 0.25 M glyoxylate with 0.25 M DHF in
aqueous 1.0 M NaOH and 1M LiOH (room temperature, 1 h). For NMR details
see caption of Figure 1.
Mechanistic Investigations
While these reactions showed
that DHF might be an intermediate,
it may not be the only path in the cyanide-mediated glyoxoin reaction.
Tartrates could have been additionally produced from the base catalyzed
condensation reaction of glycolate 13 (a product of the
Cannizzaro reaction) with glyoxylate 1. This pathway
was ruled out, since tartrates were observed neither in the glyoxylate
control reaction discussed above nor when glyoxylate and glycolate
were combined under identical reaction conditions. This leaves DHF
formation and its reaction with glyoxylate as the most likely route
to tartrates. Two possible mechanisms were considered for this formal
reduction of DHF 5 (Scheme 2).
The first is a simple cross-Cannizzaro reaction[13] in which the hydroxide adduct of glyoxylate transfers a
hydride to the carbonyl of the keto form of DHF leading directly to
tartrates 8 and oxalate 9. The second pathway
involves an aldol reaction between DHF and glyoxylate resulting in
a six-carbon tricarboxylate 6. This six-carbon compound 6 can undergo a hydroxide promoted fragmentation to form tartrates 8 and oxalate 9 (Scheme 2).
Scheme 2
Two Possible Routes to Tartrate from Glyoxylate
Cross-Cannizzaro reaction involving
a hydride transfer (top) versus an aldol-reaction followed by hydroxide-mediated
fragmentation (bottom).
Two Possible Routes to Tartrate from Glyoxylate
Cross-Cannizzaro reaction involving
a hydride transfer (top) versus an aldol-reaction followed by hydroxide-mediated
fragmentation (bottom).To differentiate between
these two possible pathways, a reaction
of DHF and glyoxylate was conducted using 13C-dilabeled
glyoxylate. If the cross-Cannizzaro hydride transfer was the sole
pathway, only the formation of 13C labeled oxalate 9* would be expected. If the fragmentation of the six-carbontricarboxylate 6* was the only pathway, only signals
corresponding to labeled tartrates 8* would be observed.
However, when 13C-dilabeled glyoxylic acid (0.1 M) was
reacted with DHF (0.1 M) in 1.0 M NaOH and 1.0 M LiOH (homogeneous
reaction), the13C NMR spectrum showed that both labeled
tartrates 8* and oxalate 9* were formed.While the presence of labeled tartrates 8* indicates
that an aldol reaction–fragmentation reaction must have occurred,
formation of labeled oxalate 9* could be explained via
the competing self-Cannizzaro (as opposed to the cross-Cannizzaro)
reaction of glyoxylate. However, integration of the 13C
signals corresponding to the carboxylate peaks of oxalate 9* and glycolate 13* revealed that there is ∼50%
less labeled oxalate than labeled glycolate in the reaction mixture
(Figure S7C). This excess of glycolate
indicated that (a) there is likely some side reaction that results
in the production of labeled glycolate 13*; and (b) if
the cross-Cannizzaro hydride transfer reaction is taking place, it
is doing so to a lesser extent than this glycolate producing side
reaction. Therefore, although the cross-Cannizzaro reaction cannot
be ruled out entirely, this experiment supports the aldol reaction–fragmentation
sequence as the primary pathway. A separate reaction using unlabeled
glyoxylate (1.0 M) and 13C-labeled NaCN (0.01 M), clearly
revealed the glyoxylate cyanohydrin 2 at ≈125
ppm an otherwise empty spectral region; as the reaction progressed,
a second peak appeared at ≈126 ppm (attributed to the DHF cyanohydrin 4) persisting for ∼4 h before disappearing (Figure S8).In the heterogeneous reaction
(in 2.0 M aqNaOH) of labeled glyoxylate
with DHF, a second pathway was suggested by the formation of significant
amount (∼10%) of singly labeled tartrates 8 (Figure S7B), along with singly labeled tartronate 12. Interestingly, the (single) labeling occurs
only at the carboxylate moiety of tartrates 8 and tartronate 12 as evidenced by a lack of splitting of the carboxylate signal.
Some of this could be explained by incomplete labeling of the starting
material; however, the starting material contains <1% of singly
labeled material (by 13C NMR, Figure
S7A). This suggested that the carbon–carbon bond in
glyoxylate is being broken during the course of the reaction.Based on the above observations, we propose an overall mechanism
(Scheme 3), which accounts for the bulk of
the tartrates 8 and oxalate 9. In this mechanism,
cyanide adds to glyoxylate 1 to form the glyoxylate cyanohydrin 2. The deprotonated glyoxylate cyanohydrin 3 then
reacts with an additional molecule of glyoxylate to form the cyanohydrin
adduct of DHF 4, which is then converted to the keto
form of DHF 5 (which tautomerizes to the typical enol
form). DHF, thus formed, can react via an aldol reaction with an additional
molecule of glyoxylate (13C labeling shown in red) to yield
a six-carbon tricarboxylate intermediate 6*, which can
(under high pH) rearrange to 7* via a cyanide-mediated
retro-aldol pathway.
Scheme 3
Major Pathway Leading to Tartrates and Oxalate
from Glyoxylate
The catalytic role of cyanide
is shown in blue. Results of labeled experiments are shown by the
position of red carbons. This mechanism accounts for the primary pathway
to tartrates, in which oxalate and tartrates are formed in a 1:1 ratio.
Major Pathway Leading to Tartrates and Oxalate
from Glyoxylate
The catalytic role of cyanide
is shown in blue. Results of labeled experiments are shown by the
position of red carbons. This mechanism accounts for the primary pathway
to tartrates, in which oxalate and tartrates are formed in a 1:1 ratio.These intermediates 6*/7* can be attacked
at the carbonyl by a free hydroxide anion (under high pH) and undergo
fragmentation to yield tartrates 8/8* and
oxalate 9/9*. This mechanism accounts for the primary
pathway to tartrates, in which oxalate and tartrates are formed in
a 1:1 ratio. Additional side products are formed by pathways (Scheme 4) that include a series of benzoin-type rearrangements,[4] which are possible under these high alkaline
conditions[14,15] and which also account for the
formation of singly labeled products. In these pathways the tricarboxylate
intermediate 6(6*)/7(7*) can undergo benzoin-type rearrangements to a six-carbon
aldehyde intermediate which fragments to yield singly labeled tartrates
and formate.
Scheme 4
Potential
Pathways Leading to Side Products
The
three pathways shown above
account for all observed side products, including isotopically labeled
side products.
Alternatively 6(6*)/7(7*) can undergo a retro-aldol reaction generating
DHF 5/5*, which under these high-alkaline
conditions
undergoes a benzoin-type rearrangement to an aldehyde intermediate 10/10*. This intermediate can then react with
hydroxide and fragment to form bicarbonate, formate 11/11*, tartronate 12/12*, and
glycolate 13/13*. This second reaction pathway
was identified from the experiments dealing with the heterogeneous
decomposition of DHF alone to give formate and tartronate in 2.0 M
NaOH. This also accounts for the presence of formate in these samples;
glycolate and oxalate are also produced by the hydroxide promoted
fragmentation reaction of the keto form of DHF.In addition,
there is a side reaction that occurs when glyoxylate 1 is in a far higher concentration than DHF 5, where
tartrates 8 and tartronate 12 are
formed in a 1:1 ratio. This side reaction (Scheme 4, bottom) begins at intermediate 6/7, which decarboxylates to intermediate 14, which then
undergoes an aldol reaction with an additional molecule of glyoxylate 1 to form a seven carbon tricarboxylate 15. Further
benzoin-type rearrangements followed by fragmentation gives rise to
tartrates 8 and tartronate 12.
Potential
Pathways Leading to Side Products
The
three pathways shown above
account for all observed side products, including isotopically labeled
side products.
Discussion
The
results of the DHF–glyoxylate reaction presented here
are in sharp contrast to the work of Sagi et al.;[6] there, DHF was reacted with glyoxylate in lithium hydroxide
at pH 7–8 to produce dihydroxyacetone and pentulosonic acid
by way of six- and seven-carbon tricarboxylate intermediates (6 and 15) via several decarboxylations. However,
in our work, 6 and 15 undergo attack by
free hydroxide at the carbonyl, yielding oxalate 9, tartronate 12, and tartrates 8. While the carbonate produced
in the glyoxoin reaction is indicative of decarboxylations occurring,
no evidence was seen for any of the intermediates or products observed
in the work of Sagi et al. (6) This contrasting
result demonstrates how even in consistently basic environments, pH
may be used to alter the product suite of this reaction, from selective
production of pentulosonic acid to selective production of tartrate.
This dependence on pH underscores the need to investigate a wide range
of conditions for potentially prebiotic reactions to fully explore
the possibilities for producing these biologically relevant molecules.The products of this simple and robust glyoxoin reaction are stable
in the high-pH environment, illustrating their potential as feedstock
for further reactions. However two questions must be raised to determine
the relevance to prebiotic chemistry; specifically, what are the abiotic
availabilities of glyoxylate and of a high-hydroxide concentration?
For the former there are many possibilities: (a) Glyoxylate has been
shown to be readily produced by photo-oxidation of acetylene under
anoxic conditions;[16] (b) reductive conversion
of carbon dioxide and carbon monoxide to glyoxylate has been experimentally
demonstrated;[17−21] some of these could be reasonably extrapolated to early earth scenarios;
and (c) glyoxylate was shown by Weber to form reliably in the reaction
of glycolaldehyde and formaldehyde, catalyzed by various primary amines,[22] though it was not the primary product. Overall
these observations provide an array of options for production of glyoxylate.
The results of this investigation underscore the need and the opportunity
to further explore these options and fully investigate formation of
glyoxylate under prebiotic conditions.High-hydroxide concentrations
are considered to be extreme (and
unusual) in the conventional prebiotic line of thought. This usually
renders any high-pH reaction problematic in this context. However,
there are at least three plausible prebiotic scenarios one can consider.
The first possible scenario is the widely investigated alkaline hydrothermal
vent system;[23−25] however, this system is not without drawbacks.[26] Related reservoirs of natural hydroxide are
lakes fed by alkali springs,[27] which could
act as a natural reactor for this type of chemistry. While these lakes
may have the advantage of sidestepping the magnitude of both dilution
and thermolysis faced by oceanic vents, they too have their limitations.
Another possible high-alkaline environment can be found in the interlayer
framework of double-layered hydroxides (e.g., hydrotalcites), which
are especially conducive for uptake and concentration of anions, such
as glyoxylate and cyanide, from dilute solutions.[28,200] While each of these possibilities appear to be highly localized
with their attendant weaknesses in a prebiotic context, they do offer
potential for highly alkaline environments on early earth, that need
to be validated from a prebiotic perspective, for the chemistry described
here.Notwithstanding the arguments presented above, it remains
that
the cyanide-mediated dimerization of glyoxylate at high pH to produce
tartrates proceeds with remarkable consistency and speed, even at
low temperature, low concentration, and low solubility. The fact that
these reactions occur reliably and that the products are stable at
high hydroxide concentrations demonstrates that a high pH environment
need not be antithetical to production of such organics in a primordial
setting. Moreover, the use of cyanide as a catalyst is to be contrasted
with many other conventional prebiotic scenarios that start with cyanide
as a source molecule.[30,31]In the context of primordial
metabolism, the robust production
of tartrates from glyoxylate opens up new venues for the origins of
biologically relevant small molecules. The simple and known dehydration
of tartrates[8] results in oxaloacetate which
is known to decarboxylate to give pyruvate,[9] thus providing an entry into a prebiotic citric acid cycle. In extant
biology, oxaloacetate is the entry point to the citric acid cycle,
reacting with pyruvate to form citrate.[29] There are examples in extant biology where tartrate is utilized
and metabolized for production of oxaloacetate to be used in the citric
acid cycle.[32−34] Thus, it is reasonable to posit that tartrates could
have acted as a source of small molecules, which could become part
of an emerging proto-metabolic process (e.g., reductive citric acid
cycle).[2,3] Thus, the glyoxoin reaction (and the “glyoxylate
scenario”) could serve as a plausible alternative start for
rudimentary chemical evolution (Scheme 5).[4]
Scheme 5
A Potential Abiotic Pathway to the Citric
Acid Cycle
Experimental
Section
Reaction of Glyoxylate with Cyanide
Glyoxylic acid
monohydrate (0.1–10 mmol, 10–100 equiv) and sodium cyanide
(0.01–1 mmol, 1 equiv) were each weighed in individual 6 dram
vials. Ten mL of 2.0 M NaOH or 2.0 M LiOH was then added to the vial
containing the sodium cyanide. This vial was mixed until no solid
remained. The solution was then transferred by syringe to the vial
containing the glyoxylic acid. The cyanide solution was added down
the side of the vial to the glyoxylic acid over the course of ∼20
s and then closed, and the vial was cooled (by running cool water
over the vial) as necessary to avoid with excess heating. The pH measurements
of the resulting solutions were ≈14.
Heterogeneous Reaction
of DHF with Glyoxylate and Cyanide
Dihydroxyfumaric
acid dihydrate (0.1–5 mmol, 5 equiv),
glyoxylic acid monohydrate (0.1–5 mmol, 5 equiv), and sodium
cyanide (0.01–1 mmol, 1 equiv) were each weighed in individual
6 dram vials. Five mL of 2.0 M NaOH was then added to the vial containing
the sodium cyanide. This vial was mixed until no solid remained. In
a separate vial an additional 5 mL of 2.0 M aqNaOH was then added
to the vial containing the glyoxylic acid. The glyoxylate and sodium
cyanide solutions were then added to the dihydroxyfumaric acid. The
glyoxylate solution was added down the side of the vial to the dihydroxyfumaric
acid over the course of ∼20 s and then closed, and the vial
was cooled (by running cool water over the vial) as necessary to avoid
with excess heating. The pH of the resulting solution was ≈14.
Homogeneous Reaction of DHF with Glyoxylate
Dihydroxyfumaric
acid dihydrate (0.1–5 mmol, 1 equiv) and glyoxylic acid monohydrate
(0.1–5 mmol, 1 equiv) were each weighed in individual 6 dram
vials. Five mL of 2.0 M NaOH as then added to the vial containing
the glyoxylic acid monohydrate. This vial was mixed until no solid
remained. In a separate vial, 5 mL of 2.0 M aqLiOH was then added
to the vial containing the dihydroxyfumaric acid. This vial was mixed
until no solid remained. The glyoxylate solution was then transferred
into the vial containing the DHF solution, and the vial was closed
and shaken. Alternately, adding DHF to glyoxylate resulted in no noticeable
differences. The pH of the resulting solutions was ≈14 by pH
paper.
Authors: J W Boclair; P S Braterman; B D Brister; J Jiang; S Lou; Z Wang; F Yarberry Journal: Orig Life Evol Biosph Date: 2001 Feb-Apr Impact factor: 1.950
Authors: Jason R Nielson; Anjali K Nath; Kim P Doane; Xu Shi; Jangwoen Lee; Emily G Tippetts; Kusumika Saha; Jordan Morningstar; Kevin G Hicks; Adriano Chan; Yanbin Zhao; Amy Kelly; Tara B Hendry-Hofer; Alyssa Witeof; Patrick Y Sips; Sari Mahon; Vikhyat S Bebarta; Vincent Jo Davisson; Gerry R Boss; Jared Rutter; Calum A MacRae; Matthew Brenner; Robert E Gerszten; Randall T Peterson Journal: Sci Rep Date: 2022-03-23 Impact factor: 4.996