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Source regions and timescales for the delivery of water to the Earth
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Abstract—In the primordial solar system, the most plausible sources of the water accreted by the Earth were in the outer asteroid belt, in the giant planet regions, and in the Kuiper Belt. We investigate the implications on the origin of Earth's water of dynamical models of primordial evolution of solar system bodies and check them with respect to chemical constraints. We find that it is plausible that the Earth accreted water all along its formation, from the early phases when the solar nebula was still present to the late stages of gas‐free sweepup of scattered planetesimals. Asteroids and the comets from the Jupiter‐Saturn region were the first water deliverers, when the Earth was less than half its present mass. The bulk of the water presently on Earth was carried by a few planetary embryos, originally formed in the outer asteroid belt and accreted by the Earth at the final stage of its formation. Finally, a late veneer, accounting for at most 10% of the present water mass, occurred due to comets from the Uranus‐Neptune region and from the Kuiper Belt. The net result of accretion from these several reservoirs is that the water on Earth had essentially the D/H ratio typical of the water condensed in the outer asteroid belt. This is in agreement with the observation that the D/H ratio in the oceans is very close to the mean value of the D/H ratio of the water inclusions in carbonaceous chondrites.
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“Impacts from comets and asteroids delivered a variety of organics to early Earth, even though they provided only a very small fraction of Earth's water budget (Morbidelli et al., 2000).”
From The Astrobiology Primer v2.0 (2016) · cites this paper as Morbidelli et al., 2000
In the citing paper
“This idea has since been largely discredited due to the low probability of cometary collisions with Earth (Morbidelli et al., 2000) and the high D/H ratio of many, though not all, comets (e.g., Marty and Yokochi, 2006).”
From The Astrobiology Primer v2.0 (2016) · cites this paper as Morbidelli et al., 2000
In the citing paper
“No more than 10% of Earth's water was delivered by comets originating from the trans-uranian region, based on the differences in observed D/H ratio between comets and Earth's current water supply (Morbidelli et al., 2000).”
From The Astrobiology Primer v2.0 (2016) · cites this paper as Morbidelli et al., 2000
In the citing paper
“However, it is widely agreed that the primary source of water on Earth was delivery by material similar to C-type asteroids (Morbidelli et al., 2000) via the Grand Tack model, as discussed above.”
From The Astrobiology Primer v2.0 (2016) · cites this paper as Morbidelli et al., 2000
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A Decreased Probability of Habitable Planet Formation around Low‐Mass Stars
Raymond, S. N., Scalo, J., & Meadows, V. S. (2007) · The Astrophysical Journal · doi:10.1086/521587 · Cited by 210
“…HZs of lower-mass stars – is inefficient dynamical stirring in the low-mass disks found around low-mass stars, because more massive embryos are needed to increase eccentricities enough for significant radial mixing and therefore water delivery (Morbidelli et al. 2000; Raymond et al. 2004, 2007).”
BackgroundChemistry in Protoplanetary Disks
Henning, T. K., & Semenov, D. A. (2013) · Chemical Reviews · doi:10.1021/cr400128p · Cited by 278
Origin and evolution of the atmospheres of early Venus, Earth and Mars
Lammer, H., Zerkle, A. L., Gebauer, S., Tosi, N., Noack, L., Scherf, M., Pilat-Lohinger, E., Güdel, M., Grenfell, J. L., Godolt, M., et al. (2018) · The Astronomy and Astrophysics Review · doi:10.1007/s00159-018-0108-y · Cited by 202
“…materials are delivered via volatile-rich planetesimals - of chondritic composition (e.g., Drake and Righter 2002; Alexander et al. 2012; Marty 2012; Bouvier and Boyet 2016) - from the outer Solar System to accreting protoplanets (e.g. Morbidelli et al. 2000; Raymond et al. 2009; Marty 2012).”
BackgroundHeterogeneous Accretion and the Moderately Volatile Element Budget of Earth
Schönbächler, M., Carlson, R. W., Horan, M. F., Mock, T. D., & Hauri, E. H. (2010) · Science · doi:10.1126/science.1186239 · Cited by 205
The Compositional Structure of the Asteroid Belt
DeMeo, F. E., Alexander, C. M. O., Walsh, K. J., Chapman, C. R., & Binzel, R. P. (2015) · University of Arizona Press eBooks · doi:10.2458/azu_uapress_9780816532131-ch002 · Cited by 390
“…using the Asteroid Belt as a constraint for their model outcomes, both for delivering water-rich asteroid material to the growing planets (Morbidelli et al., 2000), and also for using their orbits to rule out other modes of planet migration (Minton and Malhotra 2009, Walsh and Morbidelli…”
Growth, destruction, and preservation of Earth’s continental crust
Spencer, C. J., Roberts, N. M. W., & Santosh, M. (2017) · Earth-Science Reviews · doi:10.1016/j.earscirev.2017.07.013 · Cited by 199
The global distribution of pyroclastic deposits on Mercury: the view from MESSENGER flybys 1-3.
Kerber, L., Head, J., Blewett, D., Solomon, S., Wilson, L., Murchie, S., Robinson, M., Denevi, B., & Domingue, D. (2011) · doi:10.1016/j.pss.2011.03.020 · Cited by 195
“However, the presence of pyroclastic volcanism on Mercury suggests that the devolatilization of the planet was not complete, or that the initial volatile budget of the planet was greater than previously hypothesized, perhaps due to the incorporation during accretion of planetesimals formed over a large range of solar…”
The habitability of Proxima Centauri b
Ribas, I., Bolmont, É., Selsis, F., Reiners, A., Leconte, J., Raymond, S. N., Engle, S. G., Guinan, E. F., Morin, J., Turbet, M., et al. (2016) · Astronomy and Astrophysics · doi:10.1051/0004-6361/201629576 · Cited by 252
“In the classical model of accretion, water-rich planetesimals originated in the outer asteroid belt (Morbidelli et al. 2000; Raymond et al. 2007a, 2009; Izidoro et al. 2015).”
BackgroundHirschmann, M. M., & Dasgupta, R. (2009) · Chemical Geology · doi:10.1016/j.chemgeo.2009.02.008 · Cited by 199
“%) cometary contribution to terrestrial volatiles may be likely (Morbidelli et al., 2000).”
BackgroundThe cosmic molybdenum–ruthenium isotope correlation
Dauphas, N., Davis, A., Marty, B., & Reisberg, L. (2004) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2004.07.026 · Cited by 187
“Recent dynamical [41] and geochemical [43] evidence support the idea that the Earth accreted wet, thus removing any requirement for a drastic change in the nature of the material accreted by our planet.”
BackgroundOn the Location of the Snow Line in a Protoplanetary Disk
Lecar, M., Podolak, M., Sasselov, D., & Chiang, E. (2006) · The Astrophysical Journal · doi:10.1086/500287 · Cited by 184
“The evidence points to about 2.7 AU, in the outer asteroid belt where icy C-class asteroids abound (Abe et al. 2000; Morbidelli et al. 2000; Rivkin et al. 2002).”
BackgroundInfluentialCould the Lunar “Late Heavy Bombardment” Have Been Triggered by the Formation of Uranus and Neptune?
Levison, H., Dones, L., Chapman, C., Stern, S., Duncan, M., & Zahnle, K. (2001) · Icarus · doi:10.1006/icar.2001.6608 · Cited by 181
Outgassing History and Escape of the Martian Atmosphere and Water Inventory
Lammer, H., Chassefière, E., Karatekin, Ö., Morschhauser, A., Niles, P. B., Mousis, O., Odert, P., Möstl, U. V., Breuer, D., Dehant, V., et al. (2013) · Space Science Reviews · doi:10.1007/s11214-012-9943-8 · Cited by 180
“According to Morbidelli et al. (2000), Lunine et al. (2003) the equivalent of ∼0.1 terrestrial ocean of H2O, that is a ∼300 m deep EGL of water, could have been provided to Earth by comets during the few 100 Myr following main accretion.”
BackgroundInfluentialMarty, B. M., Avice, G., Sano, Y., Altwegg, K., Balsiger, H., Hässig, M., Morbidelli, A., Mousis, O. J., & Rubin, M. (2016) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2016.02.031 · Cited by 207
Self-citationFossilized condensation lines in the Solar System protoplanetary disk
Morbidelli, A., Bitsch, B., Crida, A., Gounelle, M., Guillot, T., Jacobson, S. A., Johansen, A., Lambrechts, M., & Lega, E. (2015) · Icarus · doi:10.1016/j.icarus.2015.11.027 · Cited by 225
Self-citationEarly accretion of water in the inner solar system from a carbonaceous chondrite–like source
Sarafian, A., Nielsen, S., Marschall, H., McCubbin, F., & Monteleone, B. (2014) · Science · doi:10.1126/science.1256717 · Cited by 179
Origin of water in the terrestrial planets
Drake, M. (2005) · Meteoritics and Planetary Science · doi:10.1111/j.1945-5100.2005.tb00960.x · Cited by 179
“Morbidelli et al. (2000) have shown that up to 15% of the mass of the Earth could be accreted late in Earth’s growth by collision of one or a few asteroids originating in the Main Belt.”
BackgroundRanges of Atmospheric Mass and Composition of Super‐Earth Exoplanets
Elkins-Tanton, L. T., & Seager, S. (2008) · The Astrophysical Journal · doi:10.1086/591433 · Cited by 209
“…Venus, and Mars, present-day atmospheres indicate that water and carbon dioxide have remained since accretion, though perhaps the bulk of volatiles were delivered toward the end of accretion (e.g., Morbidelli et al. 2000; Chambers 2006; Raymond et al. 2006; O’Brien, Morbidelli, & Levison 2006).”
BackgroundLunine, J., Chambers, J., Morbidelli, A., & Leshin, L. (2002) · Icarus · doi:10.1016/s0019-1035(03)00172-6 · Cited by 170
“…integra (Levison and Duncan, 1994) until it was ejected on hyp bolic orbit or entered into collision with a giant planet. total collision probability with Mars (assumed to be on present orbit) is computed over the test particle’s lifeti with the method discussed in Morbidelli et al. (2000).”
BackgroundMethodInfluentialSelf-citationThe solid Earth’s influence on sea level
Conrad, C. (2013) · Geological Society of America Bulletin · doi:10.1130/b30764.1 · Cited by 168
“Earth’s water originally accumulated during planetary accretion (Wood et al., 2010) and/or soon afterward (Albarede, 2009) by delivery from asteroids (Morbidelli et al., 2000) and comets (Hartogh et al., 2011).”
BackgroundThe Geologic History of Seawater
Lowenstein, T. K., Kendall, B., & Anbar, A. D. (2013) · Elsevier eBooks · doi:10.1016/b978-0-08-095975-7.00621-5 · Cited by 117
Tracing the ingredients for a habitable earth from interstellar space through planet formation
Bergin, E., Blake, G., Ciesla, F., Hirschmann, M., & Li, J. (2015) · Proceedings of the National Academy of Sciences of the United States of America · doi:10.1073/pnas.1500954112 · Cited by 164
“Also, the effects of core segregation depend on the fraction of metal equilibrated with volatile-bearing silicate [43], as much of the core may have segregated prior to bulk volatile delivery [44].”
BackgroundMETAL-SILICATE PARTITIONING OF SIDEROPHILE ELEMENTS AND CORE FORMATION IN THE EARLY EARTH*
Righter, K. (2003) · Annual Review of Earth and Planetary Sciences · doi:10.1146/annurev.earth.31.100901.145451 · Cited by 164
Magma ocean influence on early atmosphere mass and composition
Hirschmann, M. M. (2012) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2012.06.015 · Cited by 172
“(C) Much of the BSE inventory of C was delivered as part of a late veneer that post-dated core formation (Morbidelli et al., 2000; Dauphas and Marty, 2002; Javoy, 2005).”
BackgroundHigh-energy chemistry of formamide: A unified mechanism of nucleobase formation
Ferus, M., Nesvorný, D., Šponer, J., Kubelík, P., Michalčíková, R. B., Shestivská, V., Šponer, J. E., & Civiš, S. (2014) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.1412072111 · Cited by 184
“1B) (9): The atmosphere was partly eroded and transformed (10, 11), and the hydrosphere was enriched by water (12, 13).”
BackgroundChondritic Mg isotope composition of the Earth
Bourdon, B., Tipper, E., Fitoussi, C., & Stracke, A. (2009) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2010.06.008 · Cited by 160
Experimental evidence for water formation on interstellar dust grains by hydrogen and oxygen atoms
Dulieu, F., Amiaud, L., Congiu, E., Fillion, J., Matar, E., Momeni, A., Pirronello, V., & Lemaire, J. (2009) · doi:10.1051/0004-6361/200912079 · Cited by 151
“While the means of delivery of water to Earth remain a subject of debate (Morbidelli et al. 2000), the synthesis of water in the Universe is a fundamental link in establishing our origins.”
BackgroundHalliday, A. N. (2008) · Philosophical Transactions of the Royal Society A Mathematical Physical and Engineering Sciences · doi:10.1098/rsta.2008.0209 · Cited by 149
Chambers, J., & Wetherill, G. (2001) · Meteoritics and Planetary Science · doi:10.1111/j.1945-5100.2001.tb01881.x · Cited by 148
Self-citationA hydrogen-based oxidation mechanism relevant to planetary formation
Sharp, Z. D., McCubbin, F. M., & Shearer, C. K. (2013) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2013.08.015 · Cited by 147
“In a homogeneous accretion model, volatiles are incorporated throughout the accretion of a growing body, from the early stages when the solar nebula was still present until the final stages of growth of planetary embryos (Bottke et al., 2010; Morbidelli et al., 2000).”
BackgroundRobert, F. (2001) · Science · doi:10.1126/science.1064051 · Cited by 147
Self-citationAtmospheric and water loss from early Venus
Kulikov, Y. N., Lammer, H., Lichtenegger, H. I. M., Terada, N., Ribas, I., Kolb, C., Langmayr, D., Lundin, R., Guinan, E. F., Barabash, S., et al. (2006) · Planetary and Space Science · doi:10.1016/j.pss.2006.04.021 · Cited by 146
A SPITZER SURVEY OF MID-INFRARED MOLECULAR EMISSION FROM PROTOPLANETARY DISKS. I. DETECTION RATES
Pontoppidan, K., Salyk, C., Blake, G., Meijerink, R., Carr, J., & Najita, J. (2010) · The Astrophysical Journal · doi:10.1088/0004-637x/720/1/887 · Cited by 145
“The mechanism for delivering a veneer of water to an otherwise dry Earth is controversial, although primitive carbonaceous chondrites provide the best match to the D/H ratio of the Earth’s oceans (for an overview, see Morbidelli et al. 2000).”
BackgroundRaymond, S. N., Quinn, T., & Lunine, J. I. (2007) · Astrobiology · doi:10.1089/ast.2006.06-0126 · Cited by 193
“We propose a bimodal model for water delivery to Earth-like planets, which is a direct out-growth of our simulations that included a larger number of particles than the pioneering simulations of Morbidelli et al. (2000).”
InfluentialSelf-citationThe naked planet Earth: Most essential pre-requisite for the origin and evolution of life
Maruyama, S., Ikoma, M., Genda, H., Hirose, K., Yokoyama, T., & Santosh, M. (2013) · Geoscience Frontiers · doi:10.1016/j.gsf.2012.11.001 · Cited by 140
“Additionally, accretion event of asteroids seems to be stochastic event (e.g., Morbidelli et al., 2000; Petit et al., 2001).”
BackgroundKulikov, Y. N., Lammer, H., Lichtenegger, H. I. M., Penz, T., Breuer, D., Spohn, T., Lundin, R., & Biernat, H. K. (2007) · Space Science Reviews · doi:10.1007/s11214-007-9192-4 · Cited by 139
Felsic highland crust on Venus suggested by Galileo Near‐Infrared Mapping Spectrometer data
Hashimoto, G. L., Roos‐Serote, M., Sugita, S., Gilmore, M. S., Kamp, L. W., Carlson, R. W., & Baines, K. H. (2008) · Journal of Geophysical Research: Planets · doi:10.1029/2008je003134 · Cited by 139
Abe, Y., Ohtani, E., Okuchi, T., Righter, K., & Drake, M. (2007) · Journal of Geography (Chigaku Zasshi) · doi:10.5026/jgeography.116.188 · Cited by 138
Sanctis, M. C. D., Combe, J., Ammannito, E., Palomba, E., Longobardo, A., McCord, T. B., Marchi, S., Capaccioni, F., Capria, M. T., Mittlefehldt, D. W., et al. (2012) · The Astrophysical Journal Letters · doi:10.1088/2041-8205/758/2/l36 · Cited by 147
“Notably, the link between distant Vestoids and HEDs is provided by several V-types observed among nearEarth objects (e.g., Marchi et al. 2005).”
BackgroundDomagal-Goldman, S. D., Wright, K. E., Domagal-Goldman, S. D., Wright, K. E., Adamala, K., Arina de la Rubia, L., Bond, J., Dartnell, L. R., Goldman, A. D., Lynch, K., et al. (2016) · Astrobiology · doi:10.1089/ast.2015.1460 · Cited by 136
“Impacts from comets and asteroids delivered a variety of organics to early Earth, even though they provided only a very small fraction of Earth’s water budget (Morbidelli et al., 2000).”
InfluentialMars’ growth stunted by an early giant planet instability
Clement, M. S., Kaib, N. A., Raymond, S. N., & Walsh, K. J. (2018) · Icarus · doi:10.1016/j.icarus.2018.04.008 · Cited by 170
Origin of the ocean on the Earth : Early evolution of water D/H in a hydrogen-rich atmosphere
Genda, H., & Ikoma, M. (2007) · Icarus · doi:10.1016/j.icarus.2007.09.007 · Cited by 133
“e planetesimals forms a massive steam atmosphere that ends up the ocean after its cooling (Lange and Ahrens 1982; Matsui and Abe 1986; Zahnle et al. 1988). Water-containing rocky planetesimals (e.g., Morbidelli et al. 2000; Raymond et al. 2004, 2005) and/or icy planetesimals (e.g., Gomes et al. 2005) can be delivered…”
BackgroundWay, M. J., Anthony, & Genio, D. D. (2019) · Journal of Geophysical Research - Planets · doi:10.1002/essoar.10501118.3 · Cited by 130
“At the same time, work by Gillmann et al. (2009), Morbidelli et al. (2000), and Raymond et al. (2006) shows that Venus’ initial water inventory at formation could be as much as two terrestrial ocean’s worth while large planetary embryos could deliver much more within 200 Myr of formation.”
BackgroundObservable consequences of planet formation models in systems with close-in terrestrial planets
Raymond, S. N., Barnes, R., & Mandell, A. M. (2008) · Monthly Notices of the Royal Astronomical Society · doi:10.1111/j.1365-2966.2007.12712.x · Cited by 167
“…then their growth would be similar to that of Solar System’s terrestrial planets (Wetherill 1990, 1996; Chambers & Wetherill 1998; Agnor et al. 1999; Morbidelli et al. 2000; Chambers 2001; Kenyon & Bromley 2006), but minus the dynamical effects of Jupiter and Saturn (although giant planets may…”
BackgroundKlein, B., Jura, M., Koester, D., Zuckerman, B., & Melis, C. (2009) · The Astrophysical Journal · doi:10.1088/0004-637x/709/2/950 · Cited by 126
“(2.5–4 AU) are up to 10% water by mass, while those originating from the inner asteroid belt (∼ 2 AU) range from 0.05–0.1% water by mass (Morbidelli et al. 2000).”
BackgroundInfluentialA SENSITIVE SEARCH FOR DEUTERATED WATER IN COMET 8P/TUTTLE
Villanueva, G., Mumma, M., Bonev, B., DiSanti, M., Gibb, E., Böhnhardt, H., & Lippi, M. (2008) · The Astrophysical Journal · doi:10.1088/0004-637x/690/1/l5 · Cited by 126
“Meanwhile, the slightly lower D/H values observed in carbonaceous chondrites (ranging from 0.8 to 2.1 VSMOW; Lecuyer et al. 1998) stimulated a hypothesis that water was delivered by proto-asteroids rich in chondritic material (Morbidelli et al. 2000; Dauphas et al. 2000).”
InfluentialAsteroidal impacts and the origin of terrestrial and lunar volatiles
Albarède, F., Ballhaus, C., Janne Blichert-toft, B., Lee, C. A., Marty, B. M., Moynier, F., & Yin, Q. (2012) · Icarus · doi:10.1016/j.icarus.2012.10.026 · Cited by 128
“Addition of volatiles from the outer Solar System carried by debris of undifferentiated planetesimals, the so-called late veneer, during the clearing stages of the debris disk, is consistent with current understanding of accretion dynamics (Albarède, 2009; Morbidelli et al., 2000; Robert, 2001).”
ResultFormation of Earth‐like Planets During and After Giant Planet Migration
Mandell, A. M., Raymond, S. N., & Sigurðsson, S. (2007) · The Astrophysical Journal · doi:10.1086/512759 · Cited by 182
“This mode of transport is similar to the model of Morbidelli et al. (2000) except that it is substantially enhanced by the large eccentricities induced by close encounters between the migrating giant planet and the smaller bodies.”
BackgroundResult
Metadata
- Authors
- Morbidelli, A., Chambers, J., Lunine, J. I., Petit, J. M., Robert, F., Valsecchi, G. B., & Cyr, K. E.
- Affiliations
- Observatoire de la Côte d’Azur (FR)
- Armagh Observatory & Planetarium (GB)
- University of Arizona (US)
- Muséum national d'Histoire naturelle (FR)
- National Aeronautics and Space Administration (US)
- Corresponding author
- Morbidelli, A.
- Venue
- Meteoritics & Planetary Science
- Publisher
- Wiley
- Published
- 2000-11
- Volume
- 35
- Issue
- 6
- Pages
- 1309-1320
- ISSN
- 1086-9379 (ISSN-L)
- 1945-5100
- OpenAlex
- W2014359877
- Cited by
- 881
- References
- 0
- Citations by year
- 2026: 17 · 2025: 31 · 2024: 29 · 2023: 36 · 2022: 34 · 2021: 29 · 2020: 43 · 2019: 33 · 2018: 71 · 2017: 38 · 2016: 49 · 2015: 39 · 2014: 52 · 2013: 42 · 2012: 39
- FWCI
- 12.13
- Type
- journal article
- Language
- en
- Open access
- bronze
- doi.org
- Locations
- Meteoritics and Planetary Science (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Space and Planetary Science › Astro and Planetary Science
- Physical Sciences › Earth and Planetary Sciences › Space and Planetary Science › Planetary Science and Exploration
- Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Astrophysics and Star Formation Studies
- Keywords
- origin of Earth's water, water delivery, outer asteroid belt, Kuiper belt, planetary embryos, late veneer, hydrogen/deuterium ratio, carbonaceous chondrites, water inclusions, solar nebula, planetesimal accretion, giant planet migration
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