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Detection of HCN and diverse redox chemistry in the plume of Enceladus

Abstract

The Cassini spacecraft observed that Saturn’s moon Enceladus has a series of jets erupting from its South Polar Terrain. Previous studies of in situ data collected by Cassini’s Ion and Neutral Mass Spectrometer (INMS) have identified H2O, CO2, CH4, NH3 and H2 within the plume of ejected material. Identification of minor species in the plume remains an ongoing challenge, owing to the large number of possible combinations that can be used to fit the INMS data. Here we present the detection of several additional compounds of strong importance to the habitability of Enceladus, including HCN, C2H2, C3H6 and C2H6. Our analyses of the low-velocity INMS data, coupled with our detailed statistical framework, enable discrimination between previously ambiguous species in the plume by alleviating the effects of high-dimensional model fitting. Together with plausible mineralogical catalysts and redox gradients derived from surface radiolysis, these compounds could potentially support extant microbial communities or drive complex organic synthesis leading to the origin of life.

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Fig. 1: Previously unidentified compounds in the Enceladus plume indicate a potentially habitable environment.
Fig. 2: Model performance as a function of model complexity.
Fig. 3: Average low-velocity INMS spectrum and reconstructed model fit.
Fig. 4: Contributions of individual species to the model fit.

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Data availability

All INMS REU spectra are publicly available from the Planetary Data System at https://doi.org/10.17189/1519605. All NIST spectra are publicly available from the NIST Chemistry WebBook at https://doi.org/10.18434/T4D303.

Code availability

The code for this work was implemented using open-source Python libraries available at https://pypi.org/ and is available upon request.

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Acknowledgements

We thank J. H. Waite and B. A. Magee for their help on interpreting INMS instrument effects. J.S.P. thanks M. Sako and K. L. Wagstaff for useful discussions and statistical insight, and D. D. Sasselov for helpful discussions on prebiotic chemistry. All authors acknowledge the support of the Cassini Data Analysis Program (NNN13D466T) and the Jet Propulsion Laboratory, California Institute of Technology, under a contract with the National Aeronautics and Space Administration (80NM0018D0004). T.A.N. was also supported by an appointment to the NASA Postdoctoral Fellowship Program at the Jet Propulsion Laboratory administered by Oak Ridge Associated Universities and Universities Space Research Association through a contract with NASA. K.P.H. also acknowledges support from the NASA Astrobiology Program (80NSSC19K1427) and the Europa Lander Pre-Project, managed by the Jet Propulsion Laboratory, California Institute of Technology, under a contract with NASA.

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J.S.P., T.A.N. and K.P.H. contributed to the conceptual development of the study, to the interpretation of results and to the final version of the paper. J.S.P. developed the methodology, performed the mathematical analysis and wrote the first version of the paper.

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Correspondence to Jonah S. Peter.

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Nature Astronomy thanks Christelle Briois and Brian Magee for their contribution to the peer review of this work.

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Extended data

Extended Data Fig. 1 Full mass range INMS spectrum and analysis of residuals.

(a) The black silhouette shows the full mass range of the INMS spectrum used in this work. Shaded gray bars indicate count values at 1 and 2 u that were omitted from this work (see Methods). The spectrum was adapted from ref. 12. Error bars show 1σ Gaussian uncertainty in the observed count rates. The minimum count uncertainty was estimated as ~ 2 counts from the count rates of noisy mass channels at masses >46 u. Red circles show the reconstructed model fit based on the mixing ratios of Extended Data Table 2. (b) Scatterplot of the standardized residuals produced by fitting the model. Only mass channels with counts above the minimum uncertainty are shown. There is no discernable pattern amongst the residuals or evidence of heteroscedasticity. (c) Histogram of the standardized residuals (red bars) compared to a reference Gaussian distribution with zero mean (black curve). The residuals show good agreement with the Gaussian distribution, indicating a robust model fit. The black arrow indicates a potential outlier at mass 16, which likely results from the standardization of the slow flyby count rates at neighboring mass channels.

Extended Data Fig. 2 Comparison of model performance without HCN.

Blue circles show the maximum relative likelihoods across all models for each value of d species (as in Fig. 2a). Red diamonds indicate the highest likelihood models without HCN. All models without HCN exhibit exceptionally poor performance, with a maximum relative likelihood peaking at λ = 6.1 × 10−4 for d = 12.

Extended Data Table 1 Complete list of compounds included in the analysis
Extended Data Table 2 Modeling results for the complete spectral library

Supplementary information

Supplementary Information

Supplementary Figs. 1–4, Tables 1 and 2, Results and Discussion.

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Peter, J.S., Nordheim, T.A. & Hand, K.P. Detection of HCN and diverse redox chemistry in the plume of Enceladus. Nat Astron 8, 164–173 (2024). https://doi.org/10.1038/s41550-023-02160-0

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