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A D/H ratio consistent with Earth’s water in Halley-type comet 12P from ALMA HDO mapping

Abstract

Isotopic measurements of Solar System bodies provide a primary paradigm within which to understand the origins and histories of planetary materials. The deuterium-to-hydrogen (D/H) ratio, in particular, helps reveal the relationship between (and heritage of) different H2O reservoirs within the Solar System. Here we present interferometric maps of water (H2O) and semiheavy water (HDO) in the gas-phase coma of a comet (Halley-type comet 12P/Pons–Brooks), obtained using the Atacama Large Millimeter/submillimeter Array. The maps are consistent with outgassing of both H2O and HDO directly from the nucleus, and they imply a coma D/H ratio (for water) of (1.71 ± 0.44) × 10−4. This is at the lower end of the range of previously observed values in comets and is consistent with D/H in Earth’s ocean water. Our results indicate a possible common heritage between a component of the water ice reservoir in the Oort cloud and the water that was delivered to the young Earth during the early history of the Solar System.

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Fig. 1: ALMA emission (integrated flux) maps of H2O and HDO in comet 12P/Pons–Brooks.
Fig. 2: Interferometric data for H2O and HDO in comet 12P.
Fig. 3: Comparison of D/H ratios in different bodies.

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Data availability

This work makes use of ALMA dataset ADS/JAO.ALMA#2023.1.01143.L, which is available for download from the ALMA Science Archive (https://almascience.nrao.edu/aq/). The IRTF iSHELL data, including all necessary science and calibration files, can be accessed from the IRTF Data Archive (https://irtfweb.ifa.hawaii.edu/research/irtf_data_archive.php).

Code availability

The SUBLIME radiative transfer model required to reproduce the results of this study is available for download from https://bitbucket.org/mcordiner/sublimed/src/master. The IRTF data reduction codes are available from https://github.com/nasapsg. The infrared telluric and cometary emission models are available through the PSG (https://psg.gsfc.nasa.gov).

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Acknowledgements

This work was supported by NASA’s Planetary Science Division Internal Scientist Funding Program through the Fundamental Laboratory Research (FLaRe) work package. E.L.G. was supported by the NSF (Grant No. AST-2009910). B.P.B. was supported by the NSF (Grant No. AST-2009398) and NASA (SSO Grant No. 80NSSC22K1401). K.F. was supported by the JSPS (KAKENHI Grant No. 20H05847). Part of this research was carried out at the Jet Propulsion Laboratory, California Institute of Technology, under a contract with NASA (Contract No. 80NM0018D0004). D.C.L. acknowledges financial support from the NASA Astrophysics Data Analysis Program. ALMA is a partnership of ESO, NSF (USA), NINS (Japan), NRC (Canada), NSC and ASIAA (Taiwan), and KASI (Republic of Korea), in cooperation with the Republic of Chile. The Joint ALMA Observatory is operated by ESO, AUI/NRAO and NAOJ. The NRAO is a facility of the NSF operated under cooperative agreement by Associated Universities, Inc. We thank M. R. Combi for sharing 12P water production rates derived from SOHO/SWAN observations, and for helpful discussions on the radial dependence of coma outflow velocities. E.L.G., B.P.B. and N.X.R. are visiting astronomers at the IRTF, which is operated by the University of Hawaii under contract NNH14CK55B with the National Aeronautics and Space Administration. The authors wish to recognize and acknowledge the very significant cultural role and reverence that the summit of Maunakea has always had within the indigenous Hawaiian community. We are most fortunate and grateful to have the opportunity to conduct IRTF observations from this mountain.

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All authors helped write the telescope observing proposals, checked and validated the data analysis methods, and edited the paper. M.A.C. performed the data reduction and radiative transfer modelling, generated the figures and wrote the text of the paper. E.L.G. performed the IRTF observations, data reduction and analysis. B.P.B. investigated the IRTF H2O OPR. Z.K. performed the HDO laboratory spectroscopy.

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Correspondence to M. A. Cordiner.

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Extended data

Extended Data Fig. 1 Observed ALMA spectrum of comet 12P.

These data were observed using ALMA on 2024 April 18-25, and show the comet’s spectrum in the vicinity of the HDO 21,1 − 21,2 and CH3OH JK = 5K − 4K lines (labeled). The (continuum-subtracted) spectrum was extracted at the position of the continuum emission peak (the assumed location of the nucleus), and molecular lines were assigned using data from the Splatalogue (https://splatalogue.online/)39. Inset panel shows a zoom of the detected HDO line.

Extended Data Fig. 2 ALMA emission maps of CH3OH in comet 12P.

The data, observed in Band 6 (between 2024 April 18-25; left) and Band 5 (2024 May 4; right), have been spectrally integrated, continuum-subtracted, and are centered on the thermal continuum peak. The Band 6 image is integrated over 14 transitions, with a contour separation of 10σ, while the Band 5 image is integrated over 8 transitions, with 5σ contours (see Supplementary Table 2 for details). Inset panels (upper right) show the spectral line profiles of selected transitions as a function of cometocentric velocity (v), extracted at the origin (8 lines in the Band 5 CH3OH spectrum have been averaged in velocity space, to improve the signal-to-noise rato). The spatial resolution (beam FWHM) is shown lower left, and the directions of the (sky-projected) comet-Sun and orbital trail vectors are shown lower right.

Extended Data Fig. 3 Coma kinetic temperature radial profiles.

Temperatures were retrieved independently on the HDO and H2O observation dates dates using multi-line ALMA CH3OH observations. 1σ error envelopes are shown.

Extended Data Fig. 4 ALMA interferometric spectra of H2O and HDO.

The real part of the observed visibility data is shown as a function of frequency for H2O (left) and HDO (right), averaged across the antenna baseline range uv=12-100 m (corresponding to angular scales on the sky <24” for H2O and <21” for HDO). Best-fit SUBLIME radiative transfer models (see Table 1 and Figure 2 for details), are overlaid in red.

Extended Data Fig. 5 ALMA interferometric spectra of CH3OH (average of observations in the date range 18–25 April 2024).

The real parts of the observed visibility spectra are shown as a function of baseline interval, averaged within the uv range specified in each panel (corresponding to angular sizes θ in the plane of the sky). The best-fit SUBLIME radiative transfer model is overlaid in red.

Extended Data Fig. 6 ALMA interferometric spectra of CH3OH (observed 4 May 2024).

The real parts of the observed visibility spectra are shown as a function of baseline interval, averaged within the uv range specified in each panel (corresponding to angular sizes θ in the plane of the sky). The best-fit SUBLIME radiative transfer model is overlaid in red.

Extended Data Table 1 IRTF Measurements

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Supplementary Information

Supplementary Tables 1–3 and Fig. 1.

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Cordiner, M.A., Gibb, E.L., Kisiel, Z. et al. A D/H ratio consistent with Earth’s water in Halley-type comet 12P from ALMA HDO mapping. Nat Astron (2025). https://doi.org/10.1038/s41550-025-02614-7

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