Abstract
There is overwhelming evidence that meteorites bring α-methylated amino acids to earth with some l(S) enantiomeric excess. How does that get transferred into normal biological molecules? In this brief account, we show that an α-methylated amino acid, d(R)-α-methylvaline, can react with pyruvate and phenylpyruvate salts in dry mixtures to form alanine and phenylalanine with l enantiomeric excesses, under sensible prebiotic conditions. Thus the meteoritic l(S) excesses of this compound would produce excess d-alanine and d-phenylalanine, which are found in some organisms.
Original language | English |
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Pages (from-to) | 1809-1812 |
Number of pages | 4 |
Journal | Tetrahedron Letters |
Volume | 47 |
Issue number | 11 |
DOIs | |
State | Published - 13 Mar 2006 |
Externally published | Yes |
Keywords
- Amino acids
- Chirality
- Murchison carbonaceous chondritic meteorites
- Origin of optical activity
- Transaminations