High-molecular-weight organic matter in the particles of comet 67P/Churyumov–Gerasimenko
Nicolas Fray
(1)
,
Anaïs Bardyn
(2)
,
Hervé Cottin
(1)
,
Kathrin Altwegg
(3, 4)
,
Donia Baklouti
(5)
,
Christelle Briois
(2)
,
Luigi Colangeli
(6)
,
Cécile Engrand
(7)
,
Henning Fischer
(8)
,
Albrecht Glasmachers
,
Eberhard Grün
(9)
,
Gerhard Haerendel
,
Hartmut Henkel
,
Herwig Höfner
,
Klaus Hornung
(10)
,
Elmar K. Jessberger
,
Andreas Koch
,
Harald Krüger
(11)
,
Yves Langevin
(5)
,
Harry Lehto
(12)
,
Kirsi Lehto
,
Léna Le Roy
(3)
,
Sihane Merouane
(13)
,
Paola Modica
(2)
,
François-Régis Orthous-Daunay
(14)
,
John Paquette
(13)
,
François Raulin
(1)
,
Jouni Rynö
(15)
,
Rita Schulz
(6)
,
Johan Silén
(15)
,
Sandra Siljeström
(16)
,
Wolfgang Steiger
,
Oliver Stenzel
,
Thomas Stephan
(17)
,
Laurent Thirkell
(2)
,
Roger Thomas
(2)
,
Klaus Torkar
,
Kurt Varmuza
,
Karl-Peter Wanczek
,
Boris Zaprudin
,
Jochen Kissel
,
Martin Hilchenbach
(13)
1
LISA (UMR_7583) -
Laboratoire Interuniversitaire des Systèmes Atmosphériques
2 LPC2E - Laboratoire de Physique et Chimie de l'Environnement et de l'Espace
3 CSH - Center for Space and Habitability
4 Physikalisches Institut [Bern]
5 IAS - Institut d'astrophysique spatiale
6 ESTEC - European Space Research and Technology Centre
7 CSNSM AS - Centre de Sciences Nucléaires et de Sciences de la Matière
8 CEP - Climate and Environmental Physics [Bern]
9 MPIK - Max-Planck-Institut für Kernphysik
10 LRT-7 - Institut für Strömungsmechanik und Aerodynamik
11 MPS - Max Planck Institute for Solar System Research
12 Tuorla Observatory
13 MPS - Max-Planck-Institut für Sonnensystemforschung
14 IPAG - Institut de Planétologie et d'Astrophysique de Grenoble
15 Finnish Meteorological Institute Observation Services
16 Department of Chemistry, Materials and Surfaces [Boras]
17 Department of Geophysical Sciences [Chicago]
2 LPC2E - Laboratoire de Physique et Chimie de l'Environnement et de l'Espace
3 CSH - Center for Space and Habitability
4 Physikalisches Institut [Bern]
5 IAS - Institut d'astrophysique spatiale
6 ESTEC - European Space Research and Technology Centre
7 CSNSM AS - Centre de Sciences Nucléaires et de Sciences de la Matière
8 CEP - Climate and Environmental Physics [Bern]
9 MPIK - Max-Planck-Institut für Kernphysik
10 LRT-7 - Institut für Strömungsmechanik und Aerodynamik
11 MPS - Max Planck Institute for Solar System Research
12 Tuorla Observatory
13 MPS - Max-Planck-Institut für Sonnensystemforschung
14 IPAG - Institut de Planétologie et d'Astrophysique de Grenoble
15 Finnish Meteorological Institute Observation Services
16 Department of Chemistry, Materials and Surfaces [Boras]
17 Department of Geophysical Sciences [Chicago]
Nicolas Fray
- Function : Author
- PersonId : 755928
- ORCID : 0000-0002-9140-5462
Christelle Briois
- Function : Author
- PersonId : 974700
Albrecht Glasmachers
- Function : Author
Gerhard Haerendel
- Function : Author
Hartmut Henkel
- Function : Author
Herwig Höfner
- Function : Author
Elmar K. Jessberger
- Function : Author
Andreas Koch
- Function : Author
Kirsi Lehto
- Function : Author
Léna Le Roy
- Function : Author
- PersonId : 18376
- IdHAL : lena-le-roy
- ORCID : 0000-0002-5984-6153
Jouni Rynö
- Function : Author
- PersonId : 774614
- ORCID : 0000-0002-5677-1651
Wolfgang Steiger
- Function : Author
Oliver Stenzel
- Function : Author
Laurent Thirkell
- Function : Author
- PersonId : 774612
- ORCID : 0000-0001-8659-3879
Klaus Torkar
- Function : Author
Kurt Varmuza
- Function : Author
Karl-Peter Wanczek
- Function : Author
Boris Zaprudin
- Function : Author
Jochen Kissel
- Function : Author
Abstract
The presence of solid carbonaceous matter in cometary dust was established by the detection of elements such as carbon, hydrogen, oxygen and nitrogen in particles from comet 1P/Halley1, 2. Such matter is generally thought to have originated in the interstellar medium3, but it might have formed in the solar nebula—the cloud of gas and dust that was left over after the Sun formed4. This solid carbonaceous material cannot be observed from Earth, so it has eluded unambiguous characterization5. Many gaseous organic molecules, however, have been observed6, 7, 8, 9; they come mostly from the sublimation of ices at the surface or in the subsurface of cometary nuclei8. These ices could have been formed from material inherited from the interstellar medium that suffered little processing in the solar nebula10. Here we report the in situ detection of solid organic matter in the dust particles emitted by comet 67P/Churyumov–Gerasimenko; the carbon in this organic material is bound in very large macromolecular compounds, analogous to the insoluble organic matter found in the carbonaceous chondrite meteorites11, 12. The organic matter in meteorites might have formed in the interstellar medium and/or the solar nebula, but was almost certainly modified in the meteorites’ parent bodies11. We conclude that the observed cometary carbonaceous solid matter could have the same origin as the meteoritic insoluble organic matter, but suffered less modification before and/or after being incorporated into the comet.