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dc.contributor.authorMcClure, M. K.
dc.contributor.authorRocha, W. R. M.
dc.contributor.authorPontoppidan, K. M.
dc.contributor.authorCrouzet, N.
dc.contributor.authorChu, L. E. U.
dc.contributor.authorDartois, E.
dc.contributor.authorLamberts, T.
dc.contributor.authorNoble, J. A.
dc.contributor.authorPendleton, Y. J.
dc.contributor.authorPerotti, G.
dc.contributor.authorQasim, D.
dc.contributor.authorRachid, M. G.
dc.contributor.authorSmith, Z. L.
dc.contributor.authorSun, Fengwu
dc.contributor.authorBeck, Tracy L.
dc.contributor.authorBoogert, A. C. A.
dc.contributor.authorBrown, W. A.
dc.contributor.authorCaselli, P.
dc.contributor.authorCharnley, S. B.
dc.contributor.authorCuppen, Herma M.
dc.contributor.authorDickinson, H.
dc.contributor.authorDrozdovskaya, M. N.
dc.contributor.authorEgami, E.
dc.contributor.authorErkal, J.
dc.contributor.authorFraser, H.
dc.contributor.authorGarrod, R. T.
dc.contributor.authorHarsono, D.
dc.contributor.authorIoppolo, S.
dc.contributor.authorJiménez-Serra, I.
dc.contributor.authorJin, M.
dc.contributor.authorJørgensen, J. K.
dc.contributor.authorKristensen, L. E.
dc.contributor.authorLis, D. C.
dc.contributor.authorMcCoustra, M. R. S.
dc.contributor.authorMcGuire, Brett A.
dc.contributor.authorMelnick, G. J.
dc.contributor.authorÖberg, Karin I.
dc.contributor.authorPalumbo, M. E.
dc.contributor.authorShimonishi, T.
dc.contributor.authorSturm, J. A.
dc.contributor.authorvan Dishoeck, E. F.
dc.contributor.authorLinnartz, H.
dc.date.accessioned2024-05-16T18:50:45Z
dc.date.available2024-05-16T18:50:45Z
dc.date.issued2023-01-23
dc.identifier.citationMcClure, M.K., Rocha, W.R.M., Pontoppidan, K.M. et al. An Ice Age JWST inventory of dense molecular cloud ices. Nat Astron 7, 431–443 (2023). https://doi.org/10.1038/s41550-022-01875-wen_US
dc.identifier.doi10.1038/s41550-022-01875-w
dc.identifier.urihttp://hdl.handle.net/10150/672369
dc.description.abstractIcy grain mantles are the main reservoir of the volatile elements that link chemical processes in dark, interstellar clouds with the formation of planets and the composition of their atmospheres. The initial ice composition is set in the cold, dense parts of molecular clouds, before the onset of star formation. With the exquisite sensitivity of the James Webb Space Telescope, this critical stage of ice evolution is now accessible for detailed study. Here we show initial results of the Early Release Science programme Ice Age that reveal the rich composition of these dense cloud ices. Weak ice features, including 13CO2, OCN−, 13CO, OCS and complex organic molecule functional groups, are now detected along two pre-stellar lines of sight. The 12CO2 ice profile indicates modest growth of the icy grains. Column densities of the major and minor ice species indicate that ices contribute between 2% and 19% of the bulk budgets of the key C, O, N and S elements. Our results suggest that the formation of simple and complex molecules could begin early in a water-ice-rich environment.en_US
dc.description.sponsorshipNederlandse Organisatie voor Wetenschappelijk Onderzoeken_US
dc.language.isoenen_US
dc.publisherSpringer Science and Business Media LLCen_US
dc.rights© The Author(s), under exclusive licence to Springer Nature Limited 2023.en_US
dc.rights.urihttp://rightsstatements.org/vocab/InC/1.0/en_US
dc.titleAn Ice Age JWST inventory of dense molecular cloud icesen_US
dc.typeArticleen_US
dc.identifier.eissn2397-3366
dc.contributor.departmentSteward Observatory, University of Arizonaen_US
dc.identifier.journalNature Astronomyen_US
dc.description.note6 month embargo; first published 23 January 2023en_US
dc.description.collectioninformationThis item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.en_US
dc.eprint.versionFinal accepted manuscripten_US
dc.identifier.pii1875
dc.source.journaltitleNature Astronomy
dc.source.volume7
dc.source.issue4
dc.source.beginpage431
dc.source.endpage443
refterms.dateFOA2023-07-23T00:00:00Z


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