Mineral-facilitated aqueous synthesis of hydrogen cyanide from prebiotically abundant amino acids for chemical evolution

Z Zening Yang (Earth-Life Science Institute, Institute of Future Science, Institute of Science Tokyo) Y Yamei Li N Norio Kitadai (Institute for Extra-Cutting-Edge Science and Technology Avant-Garde Research, Japan Agency for Marine-Earth Science and Technology) M Masahiro Yamamoto (Department of Immunoparasitology, Research Institute for Microbial Diseases, Osaka University) Y Yuichiro Ueno (Earth-Life Science Institute, Institute of Future Science, Institute of Science Tokyo) Y Yanjing Lu (Earth-Life Science Institute, Institute of Future Science, Institute of Science Tokyo) A Ailong Li (State Key Laboratory of Precision and Intelligent Chemistry) K Kiyohiro Adachi (RIKEN Center for Emergent Matter Science (CEMS)) A Akira Yamaguchi D Daisuke Hashizume (RIKEN Center for Emergent Matter Science (CEMS), 2-1 Hirosawa, Wako-shi, Saitama 351-0198, Japan) R Ryuhei Nakamura (Earth-Life Science Institute, Institute of Future Science, Institute of Science Tokyo)

Abstract

Recent advances in prebiotic chemistry suggest that hydrogen cyanide (HCN) serves as a fundamental precursor for nearly all essential biomolecules and protometabolic processes for life’s emergence. Although prevailing models of endogenous cyanide production rely on atmospheric methane, the availability of methane remains uncertain. Unlike methane, amino acids were likely prebiotically abundant, forming through multiple synthetic pathways under a methane-free, nonreducing atmosphere. Here, we demonstrate that HCN can form from proteinogenic amino acids in anaerobic aqueous solutions facilitated by geochemically available minerals, offering a route to overcome HCN scarcity under a nonreducing atmosphere. On manganese dioxide, the glycine-to-cyanide conversion proceeded across a broad range of pHs (2.0 to 12.6) and substrate concentrations (1 μM to 100 mM), achieving a maximum selectivity of 57%. The reaction involves α-proton abstraction in amino acids, which is distinct from conventional chemical decarboxylation processes of amino acids, highlighting the unique role of MnO 2 in activating the α-C-H bond to form HCN. HCN generation was observed for nearly all proteinogenic amino acids and short peptides. Because amino acids can be synthesized from HCN-independent pathways from abundant carbon sources such as CO 2 and CO, amino acid-derived HCN alleviates the requirement on atmospheric methane and can sustain continued chemical evolution in ambient aqueous environments.

Article Details

Volume / Issue Vol. 123, Issue 13
Published March 31, 2026
ISSN 0027-8424
Publisher National Academy of Sciences

Authors (11)

Z

Zening Yang

Earth-Life Science Institute, Institute of Future Science, Institute of Science Tokyo

Y

Yamei Li

N

Norio Kitadai

Institute for Extra-Cutting-Edge Science and Technology Avant-Garde Research, Japan Agency for Marine-Earth Science and Technology

M

Masahiro Yamamoto

Department of Immunoparasitology, Research Institute for Microbial Diseases, Osaka University

Y

Yuichiro Ueno

Earth-Life Science Institute, Institute of Future Science, Institute of Science Tokyo

Y

Yanjing Lu

Earth-Life Science Institute, Institute of Future Science, Institute of Science Tokyo

A

Ailong Li

State Key Laboratory of Precision and Intelligent Chemistry

K

Kiyohiro Adachi

RIKEN Center for Emergent Matter Science (CEMS)

A

Akira Yamaguchi

D

Daisuke Hashizume

RIKEN Center for Emergent Matter Science (CEMS), 2-1 Hirosawa, Wako-shi, Saitama 351-0198, Japan

R

Ryuhei Nakamura

Earth-Life Science Institute, Institute of Future Science, Institute of Science Tokyo