How to identify cell material in a single ice grain emitted from Enceladus or Europa

Author:

Klenner Fabian12ORCID,Bönigk Janine2,Napoleoni Maryse2ORCID,Hillier Jon2,Khawaja Nozair2ORCID,Olsson-Francis Karen3,Cable Morgan L.4ORCID,Malaska Michael J.4ORCID,Kempf Sascha5ORCID,Abel Bernd67ORCID,Postberg Frank2ORCID

Affiliation:

1. Department of Earth and Space Sciences, University of Washington, Seattle, WA, USA.

2. Institute of Geological Sciences, Freie Universität Berlin, Berlin, Germany.

3. Faculty of Science, Technology, Engineering and Mathematics, The Open University, Milton Keynes, UK.

4. Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA.

5. Laboratory for Atmospheric and Space Physics, University of Colorado, Boulder, CO, USA.

6. Institute of Chemical Technology, University of Leipzig, Leipzig, Germany.

7. Leibniz-Institute of Surface Engineering (IOM), Leipzig, Germany.

Abstract

Icy moons like Enceladus, and perhaps Europa, emit material sourced from their subsurface oceans into space via plumes of ice grains and gas. Both moons are prime targets for astrobiology investigations. Cassini measurements revealed a large compositional diversity of emitted ice grains with only 1 to 4% of Enceladus’s plume ice grains containing organic material in high concentrations. Here, we report experiments simulating mass spectra of ice grains containing one bacterial cell, or fractions thereof, as encountered by advanced instruments on board future space missions to Enceladus or Europa, such as the SUrface Dust Analyzer onboard NASA’s upcoming Europa Clipper mission at flyby speeds of 4 to 6 kilometers per second. Mass spectral signals characteristic of the bacteria are shown to be clearly identifiable by future missions, even if an ice grain contains much less than one cell. Our results demonstrate the advantage of analyses of individual ice grains compared to a diluted bulk sample in a heterogeneous plume.

Publisher

American Association for the Advancement of Science (AAAS)

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