ArticleOrigins of life and evolution of the biosphere : the journal of the International Society for the Study of the Origin of Life2017
The Influence of Mineral Matrices on the Thermal Behavior of Glycine.
Article in Origins of life and evolution of the biosphere : the journal of the International Society for the Study of the Origin of Life, 2017. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 4 papers.
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4 citing papers in PubMed, 18 citations in OpenAlex.
- Redox chemistry of early Earth and the origin of life.Communications chemistry · 2026Review
- A Fusion-Growth Protocell Model Based on Vesicle Interactions with Pyrite Particles.Molecules (Basel, Switzerland) · 2024Article
- Chemical, Thermal, and Radiation Resistance of an Iron Porphyrin: A Model Study of Biosignature Stability.Astrobiology · 2022Article
- Article
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4 authors at 1 institution in 1 country.
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Abstract
On the Hadean-Early Archean Earth, the first islands must have provided hot and dry environments for abiotically formed organic molecules. The heat sources, mainly volcanism and meteorite impacts, were also available on Mars during the Noachian period. In recent work simulating this scenario, we have shown that neat glycine forms a black, sparingly water-soluble polymer ("thermomelanoid") when dry-heated at 200 °C under pure nitrogen. The present study explores whether relevant minerals and mineral mixtures can change this thermal behavior. Most experiments were conducted at 200 or 250 °C for 2 or 7 days. The mineral matrices used were phyllosilicates (Ca-montmorillonites SAz-1 and STx-1, Na-montmorillonite SAz-1-Na, nontronite NAu-1, kaolinite KGa-1), salts (NaCl, NaCl-KCl, CaCl
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