Laser Ablation Ionization Mass Spectrometry: A Space Prototype System for In Situ Sulphur Isotope Fractionation Analysis on Planetary Surfaces

The signatures of element isotope fractionation can be used for the indirect identification of extant or extinct life on planetary surfaces or their moons. Element isotope fractionation signatures are very robust against the harsh environmental conditions, such as temperature or irradiation, which t...

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Autores principales: Andreas Riedo, Valentine Grimaudo, Joost W. Aerts, Rustam Lukmanov, Marek Tulej, Peter Broekmann, Robert Lindner, Peter Wurz, Pascale Ehrenfreund
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Publicado: Frontiers Media S.A. 2021
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spelling oai:doaj.org-article:ae5789e345ca49b6ab7e3a323ec103b52021-11-05T14:46:32ZLaser Ablation Ionization Mass Spectrometry: A Space Prototype System for In Situ Sulphur Isotope Fractionation Analysis on Planetary Surfaces2296-987X10.3389/fspas.2021.726373https://doaj.org/article/ae5789e345ca49b6ab7e3a323ec103b52021-11-01T00:00:00Zhttps://www.frontiersin.org/articles/10.3389/fspas.2021.726373/fullhttps://doaj.org/toc/2296-987XThe signatures of element isotope fractionation can be used for the indirect identification of extant or extinct life on planetary surfaces or their moons. Element isotope fractionation signatures are very robust against the harsh environmental conditions, such as temperature or irradiation, which typically prevail on solar system bodies. Sulphur is a key element for life as we know it and bacteria exist, such as sulphur reducing bacteria, that can metabolize sulphur resulting in isotope fractionations of up to −70‰ δ34S. Geochemical processes are observed to fractionate up to values of −20‰ δ34S hence, fractionation exceeding that value might be highly indicative for the presence of life. However, the detection of sulphur element isotope fractionation in situ, under the assumption that life has existed or still does exist, is extremely challenging. To date, no instrument developed for space application showed the necessary detection sensitivity or measurement methodology for such an identification. In this contribution, we report a simple measurement protocol for the accurate detection of sulphur fractionation δ34S using our prototype laser ablation ionization mass spectrometer system designed for in situ space exploration missions. The protocol was elaborated based on measurements of five sulphur containing species that were sampled at different Mars analogue field sites, including two cave systems in Romania and the Río Tinto river environment in Spain. Optimising the laser pulse energy of our laser ablation ionization mass spectrometer (LIMS) allowed the identification of a peak-like trend of the 34S/32S ratio, where the maximum, compared to internal standards, allowed to derive isotope fractionation with an estimated δ34S accuracy of ∼2‰. This accuracy is sufficiently precise to differentiate between abiotic and biotic signatures, of which the latter, induced by, e.g., sulphate-reducing microorganism, may fractionate sulphur isotopes by more than −70‰ δ34S. Our miniature LIMS system, including the discussed measurement protocol, is simple and can be applied for life detection on extra-terrestrial surfaces, e.g., Mars or the icy moons like Europa.Andreas RiedoValentine GrimaudoJoost W. AertsRustam LukmanovMarek TulejPeter BroekmannRobert LindnerPeter WurzPascale EhrenfreundPascale EhrenfreundFrontiers Media S.A.articleLIMSsulphur isotope fractionationbiosignaturemass spectrometryspace instrumentlifeAstronomyQB1-991Geophysics. Cosmic physicsQC801-809ENFrontiers in Astronomy and Space Sciences, Vol 8 (2021)
institution DOAJ
collection DOAJ
language EN
topic LIMS
sulphur isotope fractionation
biosignature
mass spectrometry
space instrument
life
Astronomy
QB1-991
Geophysics. Cosmic physics
QC801-809
spellingShingle LIMS
sulphur isotope fractionation
biosignature
mass spectrometry
space instrument
life
Astronomy
QB1-991
Geophysics. Cosmic physics
QC801-809
Andreas Riedo
Valentine Grimaudo
Joost W. Aerts
Rustam Lukmanov
Marek Tulej
Peter Broekmann
Robert Lindner
Peter Wurz
Pascale Ehrenfreund
Pascale Ehrenfreund
Laser Ablation Ionization Mass Spectrometry: A Space Prototype System for In Situ Sulphur Isotope Fractionation Analysis on Planetary Surfaces
description The signatures of element isotope fractionation can be used for the indirect identification of extant or extinct life on planetary surfaces or their moons. Element isotope fractionation signatures are very robust against the harsh environmental conditions, such as temperature or irradiation, which typically prevail on solar system bodies. Sulphur is a key element for life as we know it and bacteria exist, such as sulphur reducing bacteria, that can metabolize sulphur resulting in isotope fractionations of up to −70‰ δ34S. Geochemical processes are observed to fractionate up to values of −20‰ δ34S hence, fractionation exceeding that value might be highly indicative for the presence of life. However, the detection of sulphur element isotope fractionation in situ, under the assumption that life has existed or still does exist, is extremely challenging. To date, no instrument developed for space application showed the necessary detection sensitivity or measurement methodology for such an identification. In this contribution, we report a simple measurement protocol for the accurate detection of sulphur fractionation δ34S using our prototype laser ablation ionization mass spectrometer system designed for in situ space exploration missions. The protocol was elaborated based on measurements of five sulphur containing species that were sampled at different Mars analogue field sites, including two cave systems in Romania and the Río Tinto river environment in Spain. Optimising the laser pulse energy of our laser ablation ionization mass spectrometer (LIMS) allowed the identification of a peak-like trend of the 34S/32S ratio, where the maximum, compared to internal standards, allowed to derive isotope fractionation with an estimated δ34S accuracy of ∼2‰. This accuracy is sufficiently precise to differentiate between abiotic and biotic signatures, of which the latter, induced by, e.g., sulphate-reducing microorganism, may fractionate sulphur isotopes by more than −70‰ δ34S. Our miniature LIMS system, including the discussed measurement protocol, is simple and can be applied for life detection on extra-terrestrial surfaces, e.g., Mars or the icy moons like Europa.
format article
author Andreas Riedo
Valentine Grimaudo
Joost W. Aerts
Rustam Lukmanov
Marek Tulej
Peter Broekmann
Robert Lindner
Peter Wurz
Pascale Ehrenfreund
Pascale Ehrenfreund
author_facet Andreas Riedo
Valentine Grimaudo
Joost W. Aerts
Rustam Lukmanov
Marek Tulej
Peter Broekmann
Robert Lindner
Peter Wurz
Pascale Ehrenfreund
Pascale Ehrenfreund
author_sort Andreas Riedo
title Laser Ablation Ionization Mass Spectrometry: A Space Prototype System for In Situ Sulphur Isotope Fractionation Analysis on Planetary Surfaces
title_short Laser Ablation Ionization Mass Spectrometry: A Space Prototype System for In Situ Sulphur Isotope Fractionation Analysis on Planetary Surfaces
title_full Laser Ablation Ionization Mass Spectrometry: A Space Prototype System for In Situ Sulphur Isotope Fractionation Analysis on Planetary Surfaces
title_fullStr Laser Ablation Ionization Mass Spectrometry: A Space Prototype System for In Situ Sulphur Isotope Fractionation Analysis on Planetary Surfaces
title_full_unstemmed Laser Ablation Ionization Mass Spectrometry: A Space Prototype System for In Situ Sulphur Isotope Fractionation Analysis on Planetary Surfaces
title_sort laser ablation ionization mass spectrometry: a space prototype system for in situ sulphur isotope fractionation analysis on planetary surfaces
publisher Frontiers Media S.A.
publishDate 2021
url https://doaj.org/article/ae5789e345ca49b6ab7e3a323ec103b5
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