Establish destruction and interconversion kinetics in candidate Oxia mineral mixtures
Establish compound-specific destruction and true L↔D interconversion rates for amino acids in candidate Oxia Planum mineral–oxychlorine mixtures under relevant irradiation conditions, in order to determine which laboratory preservation regime applies at Oxia.
References
Which case applies at Oxia Planum is not established.
The baseline $C_{0,\min}$ values derive from a single kinetic compilation, so the ranking of amino acids by radiation resistance is uncertain. For example, the converted DSC values of \citet{IglesiasGroth2011} give $D_{37}{\mathrm{Asp}=69.5$~MGy and $D_{37}{\mathrm{Ala}=8.55$~MGy, whereas fits to the multi-dose HPLC concentrations of \citet{KminekBada2006} give 6.25 and 8.87~MGy, respectively. The ordering of aspartic acid and alanine therefore reverses between published datasets. Differences in irradiation protocol, observable, fitting, and sample form may explain part of the discrepancy, and the available data do not show which set applies to Oxia Planum.
The excited-state estimate suggests that the high laboratory dose rate may have little effect on degradation, although dose-rate dependence in solid amino acids has not, to our knowledge, been tested experimentally.