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balance the entry and exit of rTCA cycle metabolites (Scheme 2).
The equilibrium point is controlled by the concentration of the
hole scavenger. This scenario envisages a primary role of
mineral-driven catalysis for the archaic redox homeostasis.
Taken together with the results in previous studies,5,6 the
minerals in the submarine hydrothermal systems make the
whole homeostasis possible by modulating a series of cascading
reactions (Scheme 2). Later on in the evolutionary context, the
enzyme-like chemistry of the minerals was replaced by extant
enzymatic networks.1
Given its activity in both reductive amination and oxidative
deamination, the ZnS-based model presented in this study implies
that it may also perform a similar function to that of transaminase.
Work along this line is in progress in this laboratory.
This work is financially supported by NSFC (40902014),
CPSF (20080430918), and HIT.NSRIF (200811).
Notes and references
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Fig. 1 Main reaction products from the reductive amination of 1a–1d
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demonstrates that the reversible amination of several a-keto
acid intermediates pertinent to the rTCA cycle can occur on
the photo-irradiated surface of mineral sphalerite. The yields
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closely as are presently known, the results can be related to how an
extant metabolic mechanism might have evolved on early Earth.
Not only do they provide a new pathway for the prebiotic synthesis
of amino acids, but also an abiotic archetype for the primeval
redox metabolism. The ZnS-photo-assisted redox chemistry could
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2148 Chem. Commun., 2012, 48, 2146–2148
This journal is The Royal Society of Chemistry 2012