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The Stability of Some Selected Amino Acids Under Attempted Redox Constrained Hydrothermal Conditions
Open accessAbstract
In order to evaluate the stability of aspartic acid, serine, leucine, and alanine under redox buffered hydrothermal conditions, a series of experiments have been performed. The pyrite-pyrrhotite-magnetite (PPM) mineral assemblage was used in the experimental systems in order to constrain the oxygen fugacity. Likewise, the K-feldspar-muscovite-quartz (KMQ) assemblage was added to control the hydrogen ion activity during the experiments. The purpose was to compare the relative stabilities in buffered and unbuffered experiments. The experiments were conducted at 200 degrees C and 50 bar in Teflon coated autoclaves. Glycine, which was not present initially, started to appear at an early stage in the experimental systems and is believed to be the result of decomposition of serine. Similarly, the increase in relative abundance of alanine is likely to be the result of decomposition of serine. Decomposition rates of leucine, alanine and aspartic acid were found to be lower in experiments containing the redox buffer assemblage pyrite-pyrrhotite-magnetite than in non-redox buffered experiments. The decomposition rate of serine was higher in buffered experiments, which indicates that a transformation pathway via dehydration of serine to dehydroalanine followed by reduction to alanine is promoted by reducing conditions.
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Amino acid synthesis is very likely to occur under the circumstances of tectonic fault zones.
“An example for such a process is the synthesis of amino acids which is very likely to occur under the given circumstances [12,13,14].”
From Selection of Prebiotic Molecules in Amphiphilic Environments (2017) · cites this paper as [13]
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Metadata
- Authors
- Andersson, E., & Holm, N. G.
- Affiliations
- Stockholm University (SE)
- Venue
- Origins of life and evolution of the biosphere
- Published
- 2000-01
- Volume
- 30
- Issue
- 1
- Pages
- 9-23
- ISSN
- 0169-6149 (ISSN-L)
- 1573-0875
- OpenAlex
- W1674984745
- Cited by
- 72
- References
- 41
- Citations by year
- 2026: 1 · 2025: 3 · 2024: 1 · 2023: 2 · 2021: 3 · 2020: 2 · 2019: 2 · 2018: 2 · 2017: 4 · 2015: 8 · 2014: 3 · 2013: 5 · 2012: 5
- FWCI
- 1.98
- Type
- journal article
- Language
- en
- Open access
- bronze
- doi.org
- Licence
- Locations
- Origins of Life and Evolution of Biospheres (publishedVersion)
- PubMed (publishedVersion)
- Funders
- Royal Swedish Academy of Sciences
- Topics
- Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Origins and Evolution of Life
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
- Keywords
- amino acid stability, aspartic acid, leucine, alanine, glycine formation, redox buffering, oxygen fugacity, hydrogen ion activity, hydrothermal conditions, dehydroalanine, prebiotic chemistry, origin of life
- MeSH terms
- Amino Acids, Hot Temperature, Models, Chemical, Oxidation-Reduction
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
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