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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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).
References
Lyons, J. R. & Young, E. D. CO self-shielding as the origin of oxygen isotope anomalies in the early solar nebula. Nature 435, 317–320 (2005).
Furuya, K. et al. Water delivery from cores to disks: deuteration as a probe of the prestellar inheritance of H2O. Astron. Astrophys. 599, A40 (2017).
Visser, R. et al. Nitrogen isotope fractionation in protoplanetary disks. Astron. Astrophys. 615, A75 (2018).
Nomura, H. et al. The isotopic links from planet forming regions to the Solar System. In Proc. Astronomical Society of the Pacific Conference Series, Vol. 534 (eds Inutsuka, S. et al.) 1075–1099 (ASP, 2023).
Cleeves, L. I. et al. The ancient heritage of water ice in the Solar System. Science 345, 1590–1593 (2014).
Meech, K. & Raymond, S. N. in Planetary Astrobiology (eds Meadows, V. S. et al.) 325–356 (Univ. Arizona Press, 2020).
Marty, B. The origins and concentrations of water, carbon, nitrogen and noble gases on Earth. Earth Planet. Sci. Lett. 313, 56–66 (2012).
Alexander, C. M. O., McKeegan, K. D. & Altwegg, K. Water reservoirs in small planetary bodies: meteorites, asteroids, and comets. Space Sci. Rev. 214, 36 (2018).
Eberhardt, P., Reber, M., Krankowsky, D. & Hodges, R. R. The D/H and 18O/16O ratios in water from comet P/Halley. Astron. Astrophys. 302, 301–316 (1995).
Brown, R. H., Lauretta, D. S., Schmidt, B. & Moores, J. Experimental and theoretical simulations of ice sublimation with implications for the chemical, isotopic, and physical evolution of icy objects. Planet. Space Sci. 60, 166–180 (2012).
Villanueva, G. L. et al. A sensitive search for deuterated water in comet 8P/Tuttle. Astrophys. J. Lett. 690, L5–L9 (2009).
Meier, R. et al. A determination of the HDO/H2O ratio in comet C/1995 O1 (Hale-Bopp). Science 279, 842–844 (1998).
Bockelée-Morvan, D. et al. Deuterated water in comet C/1996 B2 (Hyakutake) and its implications for the origin of comets. Icarus 133, 147–162 (1998).
Lis, D. C. et al. Terrestrial deuterium-to-hydrogen ratio in water in hyperactive comets. Astron. Astrophys. 625, L5 (2019).
Biver, N. et al. Isotopic ratios of H, C, N, O, and S in comets C/2012 F6 (Lemmon) and C/2014 Q2 (Lovejoy). Astron. Astrophys. 589, A78 (2016).
Levison, H. F. in Completing the Inventory of the Solar System (eds Rettig, T. & Hahn, J. M.) 173–191 (ASP, 1996).
Nesvorný, D. et al. Origin and evolution of short-period comets. Astrophys. J. 845, 27 (2017).
Cordiner, M. A. et al. Gas sources from the coma and nucleus of comet 46P/Wirtanen observed using ALMA. Astrophys. J. 953, 59 (2023).
Hama, T., Kouchi, A. & Watanabe, N. Statistical ortho-to-para ratio of water desorbed from ice at 10 kelvin. Science 351, 65–67 (2016).
Cordiner, M. A. et al. Mapping the release of volatiles in the inner comae of comets C/2012 F6 (Lemmon) and C/2012 S1 (ISON) using the Atacama Large Millimeter/Submillimeter Array. Astrophys. J. Lett. 792, L2 (2014).
Roth, N. X. et al. Leveraging the ALMA Atacama Compact Array for cometary science: an interferometric survey of comet C/2015 ER61 (PanSTARRS) and evidence for a distributed source of carbon monosulfide. Astrophys. J. 921, 14 (2021).
Mandt, K. E. et al. A nearly terrestrial D/H for comet 67P/Churyumov-Gerasimenko. Sci. Adv. 10, eadp2191 (2024).
Rodgers, S. D. & Charnley, S. B. A model of the chemistry in cometary comae: deuterated molecules. Mon. Not. R. Astron. Soc. 330, 660–674 (2002).
Hartogh, P. et al. Ocean-like water in the Jupiter-family comet 103P/Hartley 2. Nature 478, 218–220 (2011).
Massey, F. J. The Kolmogorov-Smirnov test for goodness of fit. J. Am. Stat. Assoc. 46, 68–78 (1951).
Willacy, K. The chemistry of multiply deuterated molecules in protoplanetary disks. I. The outer disk. Astrophys. J. 660, 441–460 (2007).
Albertsson, T., Semenov, D. & Henning, T. Chemodynamical deuterium fractionation in the early solar nebula: the origin of water on Earth and in asteroids and comets. Astrophys. J. 784, 39 (2014).
Ceccarelli, C. et al. in Protostars and Planets VI (eds Beuther, H. et al.) 859–882 (Univ. Arizona Press, 2014).
Taquet, V., Charnley, S. B. & Sipilä, O. Multilayer formation and evaporation of deuterated ices in prestellar and protostellar cores. Astrophys. J. 791, 1 (2014).
Eistrup, C., Walsh, C. & van Dishoeck, E. F. Molecular abundances and C/O ratios in chemically evolving planet-forming disk midplanes. Astron. Astrophys. 613, A14 (2018).
Tsiganis, K., Gomes, R., Morbidelli, A. & Levison, H. F. Origin of the orbital architecture of the giant planets of the Solar System. Nature 435, 459–461 (2005).
Millar, T. J., Bennett, A. & Herbst, E. Deuterium fractionation in dense interstellar clouds. Astrophys. J. 340, 906–920 (1989).
Meier, R. et al. Deuterium in comet C/1995 O1 (Hale-Bopp): detection of DCN. Science 279, 1707–1710 (1998).
Müller, D. R. et al. High D/H ratios in water and alkanes in comet 67P/Churyumov-Gerasimenko measured with Rosetta/ROSINA DFMS. Astron. Astrophys. 662, A69 (2022).
Garrod, R. T., Widicus Weaver, S. L. & Herbst, E. Complex chemistry in star-forming regions: an expanded gas-grain warm-up chemical model. Astrophys. J. 682, 283–302 (2008).
Biver, N. et al. Ethyl alcohol and sugar in comet C/2014 Q2 (Lovejoy). Sci. Adv. 1, 1500863 (2015).
CASA Team. et al. CASA, the Common Astronomy Software Applications for radio astronomy. Publ. Astron. Soc. Pac. 134, 114501 (2022).
Remijan, A., Seifert, N. A. & McGuire, B. A. The Database for Astronomical Spectroscopy – updates, additions and plans for Splatalogue for ALMA full science operations. In Proc. 71st International Symposium on Molecular Spectroscopy (eds McCall, B., McCall, B. & Polfer, N.) FB11 (University of Illinois, 2016).
Cordiner, M. A. et al. A SUBLIME 3D model for cometary coma emission: the hypervolatile-rich comet C/2016 R2 (PanSTARRS). Astrophys. J. 929, 38 (2022).
Ferellec, L. et al. Coma composition and profiles of comet 12P/Pons-Brooks using long-slit spectroscopy. Mon. Not. R. Astron. Soc. 534, 1816–1826 (2024).
van der Tak, F. F. S., Lique, F., Faure, A., Black, J. H. & van Dishoeck, E. F. The Leiden Atomic and Molecular Database (LAMDA): current status, recent updates, and future plans. Atoms 8, 15 (2020).
Mandal, B., Zoltowski, M., Cordiner, M., Lique, F. & Babikov, D. Rotational state-to-state transition rate coefficients for H2O + H2O collisions at nonequilibrium conditions. Astron. Astrophys. 688, A208 (2024).
Crovisier, J. Rotational and vibrational synthetic spectra of linear parent molecules in comets. Astron. Astrophys. Suppl. Ser. 68, 223–258 (1987).
Bockelée-Morvan, D. et al. Herschel measurements of the D/H and 16O/18O ratios in water in the Oort-cloud comet C/2009 P1 (Garradd). Astron. Astrophys. 544, L15 (2012).
Biver, N. et al. Spectroscopic monitoring of comet C/1996 B2 (Hyakutake) with the JCMT and IRAM Radio Telescopes. Astron. J. 118, 1850–1872 (1999).
Itikawa, Y. Rotational transition in an asymmetric-top molecule by electron collision: applications to H2O and H2CO. J. Phys. Soc. Jpn 32, 217–226 (1972).
Hartogh, P. et al. HIFI observations of water in the atmosphere of comet C/2008 Q3 (Garradd). Astron. Astrophys. 518, L150 (2010).
Biver, N. et al. Long-term monitoring of the outgassing and composition of comet 67P/Churyumov-Gerasimenko with the Rosetta/MIRO instrument. Astron. Astrophys. 630, A19 (2019).
Villanueva, G. L., Smith, M. D., Protopapa, S., Faggi, S. & Mandell, A. M. Planetary Spectrum Generator: an accurate online radiative transfer suite for atmospheres, comets, small bodies and exoplanets. J. Quant. Spectrosc. Radiat. Transf. 217, 86–104 (2018).
Huebner, W. F. & Mukherjee, J. Photoionization and photodissociation rates in solar and blackbody radiation fields. Planet. Space Sci. 106, 11–45 (2015).
Newville, M. et al. LMFIT: Non-linear least-square minimization and curve-fitting for Python. Astrophysics Source Code Library ascl:1606.014 (2016).
Lammerzahl, P. et al. Expansion velocity and temperatures of gas and ions measured in the coma of comet p/ Halley. Astron. Astrophys. 187, 169 (1987).
Tseng, W. L., Bockelée-Morvan, D., Crovisier, J., Colom, P. & Ip, W. H. Cometary water expansion velocity from OH line shapes. Astron. Astrophys. 467, 729–735 (2007).
Tenishev, V., Combi, M. & Davidsson, B. A global kinetic model for cometary comae: the evolution of the coma of the Rosetta target comet Churyumov-Gerasimenko throughout the mission. Astrophys. J. 685, 659–677 (2008).
Shou, Y. et al. A new 3D multi-fluid model: a study of kinetic effects and variations of physical conditions in the cometary coma. Astrophys. J. 833, 160 (2016).
Cordiner, M. A. & Charnley, S. B. Neutral-neutral synthesis of organic molecules in cometary comae. Mon. Not. R. Astron. Soc. 504, 5401–5408 (2021).
Haser, L. Distribution d’intensité dans la tête d’une comète. Bull. Classe Sci. Acad. R. Belg. 43, 740–750 (1957).
DiSanti, M. A. et al. Hypervolatiles in a Jupiter-family comet: observations of 45P/Honda-Mrkos-Pajdušáková using iSHELL at the NASA-IRTF. Astron. J. 154, 246 (2017).
Villanueva, G. L. et al. Water in planetary and cometary atmospheres: H2O/HDO transmittance and fluorescence models. J. Quant. Spectrosc. Radiat. Transf. 113, 202–220 (2012).
Villanueva, G. L., DiSanti, M. A., Mumma, M. J. & Xu, L.-H. A quantum band model of the ν3 fundamental of methanol (CH3OH) and its application to fluorescence spectra of comets. Astrophys. J. 747, 37 (2012).
DiSanti, M. A., Bonev, B. P., Villanueva, G. L. & Mumma, M. J. Highly depleted ethane and mildly depleted methanol in comet 21P/Giacobini-Zinner: application of a new empirical ν2-band model for CH3OH near 50 K. Astrophys. J. 763, 1 (2013).
Bonev, B. P. Towards a Chemical Taxonomy of Comets: Infrared Spectroscopic Methods for Quantitative Measurements of Cometary Water. PhD thesis, Univ. Toledo (2005).
Xie, X. & Mumma, M. J. Monte Carlo simulation of cometary atmospheres: application to comet P/Halley at the time of the Giotto spacecraft encounter. I. Isotropic model. Astrophys. J. 464, 442 (1996).
Cheng, Y. C. et al. Water ortho-to-para ratio in the coma of comet 67P/Churyumov-Gerasimenko. Astron. Astrophys. 663, A43 (2022).
Bonev, B. P. et al. A search for variation in the H2O ortho-para ratio and rotational temperature in the inner coma of comet C/2004 Q2 (Machholz). Astrophys. J. Lett. 661, L97–L100 (2007).
Bonev, B. P. et al. Evidence for two modes of water release in comet 103P/Hartley. 2. Distributions of column density, rotational temperature, and ortho-para ratio. Icarus 222, 740–751 (2013).
Villanueva, G. L. et al. The molecular composition of Comet C/2007 W1 (Boattini): evidence of a peculiar outgassing and a rich chemistry. Icarus 216, 227–240 (2011).
Faure, A. et al. The ortho-to-para ratio of water in interstellar clouds. Mon. Not. R. Astron. Soc. 487, 3392–3403 (2019).
De Lucia, F. C., Cook, R. L., Helminger, P. & Gordy, W. Millimeter and submillimeter wave rotational spectrum and centrifugal distortion effects of HDO. J. Chem. Phys. 55, 5334–5339 (1971).
Kisiel, Z. & Kraśnicki, A. The millimetre-wave rotational spectrum of phenylacetylene. J. Mol. Spectrosc. 262, 82–88 (2010).
Nixon, C. A. et al. Isotopic ratios in Titan’s methane: measurements and modeling. Astrophys. J. 749, 159 (2012).
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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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.
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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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DOI: https://doi.org/10.1038/s41550-025-02614-7