The formation of pyrazines from l-serine and l-threonine has been studied. l-Serine and l-threonine,
either alone or combined, were heated at 120 °C as low temperature for 4 h or at 300 °C as high
temperature for 7 min. The pyrazines formed from each reaction were identified by GC/MS, and
the yields (to the amino acid used, as parts per million) were determined by GC/FID. It was found
that pyrazine, methylpyrazine, ethylpyrazine, 2-ethyl-6-methylpyrazine, and 2,6-diethylpyrazine
were formed from serine, whereas 2,5-dimethylpyrazine, 2,6-dimethylpyrazine, trimethylpyrazine,
2-ethyl-3,6-dimethylpyrazine, and 2-ethyl-3,5-dimethylpyrazine were formed from threonine.
Mechanistically, it is proposed that the thermal degradation of serine or threonine is composed of
various complex reactions. Among these reactions, decarbonylation followed by dehydration is the
main pathway to generate the α-aminocarbonyl intermediates leading to the formation of the main
product, such as pyrazine from serine or 2,5-dimethylpyrazine from threonine. Also, deamination
after decarbonylation generates more reactive intermediates, α-hydroxycarbonyls. Furthermore, aldol
condensation of these reactive intermediates provides α-dicarbonyls. Subsequently, these α-dicarbonyls react with the remaining serine or threonine by Strecker degradation to form additional
α-aminocarbonyl intermediates, which then form additional pyrazines. In addition, decarboxylation
and retroaldol reaction may also involve the generation of the intermediates.
Keywords: Serine; threonine; pyrazine formation; decarbonylation; decarboxylation; deamination;
α-aminocarbonyls; Strecker degradation; aldol condensation