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Source regions and timescales for the delivery of water to the Earth
Open accessAbstract
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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“2”
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“…that is in the habitable zone, however, will not necessarily have surface water because of the vagaries of water delivery during planet formation (Morbidelli et al. 2000) and poorly understood processes that determine the distribution of water between the surface and the mantle (Cowan & Abbot…”
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“[13] Current modelling of planetary formation predicts that terrestrial precursors originated from a variety of heliocentric distances and that the Earth was built from the accretion of this odd assortment [Morbidelli et al., 2000].”
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“h uncertain by a factor of ˘5), suggesting that the planetesimals in its neighborhood were mostly dry and that water was delivered only by the small amount of planetesimals accreted from farther out (Morbidelli et al., 2000; Raymond et al., 2004; O’Brien et al., 2014). The very dry enstatite chondrites have been propo…”
BackgroundInfluentialSelf-citationBeyond the Principle of Plentitude: A Review of Terrestrial Planet Habitability
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“5 AU were the source of Earth’s water (Morbidelli et al., 2000).”
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“They may also have been an important source of water for the protoEarth (e.g., Chyba and Sagan, 1992; Morbidelli et al., 2000; Marty, 2012; Trigo-Rodriguez and Martin-Torres, 2012).”
BackgroundModern Integrations of Solar System Dynamics
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“…(Muralidharan et al. 2008; King et al. 2010; Machida & Abe 2010), chemical reactions between nebula gas and silicate melts (Sasaki 1990; Ikoma & Genda 2006), and delivery via ice-bearing bodies from the outer orbital region (Morbidelli et al. 2000; Raymond et al. 2007; Walsh et al. 2011).”
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“ic distance of the comet r. According to figure 1 generated from equation 2, we note that the activity begins to be significative toward the sun around 2.7 au wich is the snow line of the Solar System ([1, 11]). According to [12], the activity of 67P/C-G began before the snow line but was very weak and not enough strong…”
BackgroundInfluentialHierarchical Earth accretion and the Hadean Eon
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“Modelling has shown that gravitational disturbances by the giant planets probably caused the outer asteroid belt, home to most asteroids of carbonaceous chondritic character, to lose the bulk of its mass towards the end of planetary formation, and it is thus likely that most bodies striking the Earth at this late stag…”
BackgroundInfluentialA Spatially Resolved au-scale Inner Disk around DM Tau
Kudo, T., Hashimoto, J., Muto, T., Liu, H. B., Dong, R., Hasegawa, Y., Tsukagoshi, T., & Konishi, M. (2018) · Astrophysical Journal · doi:10.3847/2041-8213/aaeb1c · Cited by 41
“The main belt, located beyond the water snowline at 2.7 AU (e.g., Abe et al. 2000), is thought to have profoundly impacted water delivery onto Earth (e.g., Morbidelli et al. 2000).”
BackgroundInfluentialOn the formation and evolution of asteroid belts and their potential significance for life
Martin, R. G., & Livio, M. (2012) · Monthly Notices of the Royal Astronomical Society Letters · doi:10.1093/mnrasl/sls003 · Cited by 41
“The inner asteroids, closest to Earth, are water devoid, while outside a radius of about 2.7 au the asteroids are icy C-class objects (e.g. Abe et al. 2000; Morbidelli et al. 2000).”
BackgroundInfluentialMain Belt Comets: A new class of small bodies in the solar system
Bertini, I. (2011) · Planetary and Space Science · doi:10.1016/j.pss.2011.01.014 · Cited by 41
The split fate of the early Earth, Mars, Venus, and Moon
Albarède, F., & Janne Blichert-toft, B. (2007) · Comptes Rendus Géoscience · doi:10.1016/j.crte.2007.09.006 · Cited by 51
Asteroid Family Associations of Active Asteroids
Hsieh, H. H., Novaković, B., Kim, Y., & Brasser, R. (2018) · The Astronomical Journal · doi:10.3847/1538-3881/aaa5a2 · Cited by 52
“…inventory could have been supplied by the accretion of icy objects either from the outer asteroid belt or from more distant regions of the solar system that were scattered onto Earth-impacting orbits (e.g., Morbidelli et al. 2000; Raymond et al. 2004; O’Brien et al. 2006; Raymond & Izidoro 2017).”
BackgroundHydrogen isotopic composition of water from fossil micrometeorites in howardites
Gounelle, M., Engrand, C., Alard, O., Bland, P., Zolensky, M., Russell, S., & Duprat, J. (2005) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2004.12.021 · Cited by 39
Nitrogen isotope evidence for Earth’s heterogeneous accretion of volatiles
Shi, L., Lu, W., Kagoshima, T., Sano, Y., Gao, Z., Du, Z., Liu, Y., Fei, Y., & Li, Y. (2022) · Nature Communications · doi:10.1038/s41467-022-32516-5 · Cited by 50
Solar wind contributions to Earth’s oceans
Daly, L., Lee, M., Hallis, L. J., Ishii, H. A., Bradley, J. P., Bland, P. A., Saxey, D. W., Fougerouse, D., Rickard, W. D. A., Forman, L. V., et al. (2021) · Nature Astronomy · doi:10.1038/s41550-021-01487-w · Cited by 50
Origin of Light Noble Gases (He, Ne, and Ar) on Earth: A Review
Péron, S., Moreira, M., & Agranier, A. (2018) · Geochemistry Geophysics Geosystems · doi:10.1002/2017gc007388 · Cited by 52
“…models also support the late delivery of material coming from the outer solar system due to the inward and outward migrations of Jupiter and Saturn, scattering some asteroids or planetesimals to the terrestrial planets (e.g., Morbidelli et al., 2000; O’Brien et al., 2014; Walsh et al., 2011).”
BackgroundEarth-like habitats in planetary systems
Fritz, J., Bitsch, B., Kührt, E., Morbidelli, A., Tornow, C., Wünnemann, K., Fernandes, V. A., Grenfell, J. L., Rauer, H., Wagner, R., et al. (2014) · Planetary and Space Science · doi:10.1016/j.pss.2014.03.003 · Cited by 38
“For the Sun it is expected that in the early phases of the proto-planetary disk the temperature at the location which eventually becomes the HZ was initially too high for the condensation of water (e.g. Morbidelli et al., 2000).”
BackgroundSelf-citationTHE HDO/H2O RATIO IN GAS IN THE INNER REGIONS OF A LOW-MASS PROTOSTAR
Jørgensen, J., & van Dishoeck, E. (2010) · doi:10.1088/2041-8205/725/2/l172 · Cited by 38
“…of water was brought to Earth at later times through cometary impacts compared to being accreted during the formation of the planet itself (e.g., Morbidelli et al. 2000; Raymond et al. 2004) and whether water undergoes signficant processing in warm regions of protostellar envelopes or disks…”
BackgroundHorner, J., Mousis, O. J., Petit, J.-M., & Jones, B. W. (2009) · Planetary and Space Science · doi:10.1016/j.pss.2009.06.006 · Cited by 37
“The authors consider the scenario in which the bulk of the water provided to the Earth is sourced by a small number of collisions between the Earth and planet-sized embryos, rich in water, sourced from the asteroid belt (Morbidelli et al., 2000).”
BackgroundSelf-citationThe Survival Rate of Ejected Terrestrial Planets with Moons
Debes, J., & Sigurdsson, S. (2007) · The Astrophysical Journal · doi:10.1086/523103 · Cited by 38
“The delivery of volatiles from further out in the proto-planetary disk seems to be a natural outcome of planet formation (Morbidelli et al. 2000; Raymond et al. 2004).”
BackgroundWater in Space: The Water World of ISO
Cernicharo, J., & Crovisier, J. (2005) · doi:10.1007/s11214-005-8058-x · Cited by 38
Notsu, S., Nomura, H., Ishimoto, D., Walsh, C., Honda, M., Hirota, T., & Millar, T. J. (2016) · doi:10.3847/0004-637x/827/2/113 · Cited by 37
“Icy planetesimals, comets, and/or icy pebbles coming from outside the H2O snowline may bring water to rocky planets including the Earth (e.g., Morbidelli et al. 2000, 2012; Caselli & Ceccarelli 2012; van Dishoeck et al. 2014; Matsumura et al. 2016; Sato et al. 2016).”
BackgroundFornasier, S., Lantz, C., Perna, D., Campins, H., Barucci, M., & Nesvorný, D. (2016) · doi:10.1016/j.icarus.2016.01.002 · Cited by 37
“These discoveriessupport the suggestion that at least some of Earth’s current supply of water wasdelivered by asteroids some time following the collision that produced the Moon (Morbidelli et al. 2000, Lunine 2006).”
BackgroundInfluentialThe carbon cycle on early Earth—and on Mars?
Grady, M. M., & Wright, I. P. (2006) · Philosophical Transactions of the Royal Society B Biological Sciences · doi:10.1098/rstb.2006.1898 · Cited by 37
“Water arrived from the latestage accretion of planetesimals and dust—present models suggest ca 90% from asteroidal materials and ca 10% from comets (Morbidelli et al. 2000).”
Magma Ocean, Water, and the Early Atmosphere of Venus
Salvador, A., Avice, G., Breuer, D., Gillmann, C., Lammer, H., Marcq, E., Raymond, S. N., Sakuraba, H., Scherf, M., & Way, M. J. (2023) · Space Science Reviews · doi:10.1007/s11214-023-00995-7 · Cited by 55
Compression of Fe–Si–H alloys to core pressures
Tagawa, S., Ohta, K., Hirose, K., Kato, C., & Ohishi, Y. (2016) · Geophysical Research Letters · doi:10.1002/2016gl068848 · Cited by 45
“Indeed, such an effect has been enhanced if Jupiter migrated inward in the early stage of Earth’s formation [Walsh et al., 2011].”
BackgroundInfluentialPathways to Earth-Like Atmospheres
Lammer, H., Kislyakova, K. G., Odert, P., Leitzinger, M., Schwarz, R. P., Pilat‐Lohinger, E., Kulikov, Y. N., Khodachenko, M. L., Güdel, M., & Hanslmeier, A. (2011) · Origins of Life and Evolution of Biospheres · doi:10.1007/s11084-012-9264-7 · Cited by 56
Secular variations of N-isotopes in terrestrial reservoirs and ore deposits
Kerrich, R., Jia, Y., Manikyamba, C., & Naqvi, S. M. (2006) · Geological Society of America eBooks · doi:10.1130/2006.1198(05 · Cited by 30
The “Water Problem”(sic), the Illusory Pond and Life’s Submarine Emergence—A Review
Russell, M. J. (2021) · Life · doi:10.3390/life11050429 · Cited by 46
Zhang, Y.-J., Sekine, T., Lin, J.-F., He, H.-L., Liu, F.-S., Zhang, M.-J., Sato, T., Zhu, W., & Yu, Y. (2018) · doi:10.1002/2017jb014723 · Cited by 35
“The onset melting temperatures (solidus) of the lower mantle materials, including peridotite, chondrite, natural mid-oceanic ridge basalt (Morbidelli et al., 2000), and pyrolite, have been compared to the temperature of the core at the pressure conditions of the CMB (Figure 7; Andrault et al.,…”
BackgroundTransfer, loss and physical processing of water in hit-and-run collisions of planetary embryos
Burger, C., Maindl, T., & Schäfer, C. (2017) · Celestial mechanics & dynamical astronomy · doi:10.1007/s10569-017-9795-3 · Cited by 35
“In a scenario where the majority of these volatiles is delivered by only a relatively small number of large impactors (Morbidelli et al 2000), hit-and-run can play a decisive role, because it is a frequent outcome in such similar-sized collisions (∼ 50%; Kokubo and Genda 2010; Genda et al 2017).”
BackgroundTeske, J. K., Shectman, S. A., Vogt, S. S., Díaz, M., Butler, R. P., Crane, J. D., Thompson, I. B., & Arriagada, P. (2016) · The Astronomical Journal · doi:10.3847/0004-6256/152/6/167 · Cited by 48
“…in the dynamical shaping of the Asteroid belt (Walsh et al. 2011; Morbidelli et al. 2010), and to their migratory dance toward and away from the Sun as the cause of a late delivery of volatile material to the inner rocky planets (Horner & Jones 2010; Morbidelli et al. 2000; Owen & Bar-Nun 1995).”
BackgroundXenon isotope constraints on the thermal evolution of the early Earth
Coltice, N., Marty, B. M., & Yokochi, R. (2009) · Chemical Geology · doi:10.1016/j.chemgeo.2009.04.017 · Cited by 36
Jørgensen, U. G., Appel, P. W. U., Hatsukawa, Y., Frei, R., Oshima, M., Toh, Y., & Kimura, A. (2009) · Icarus · doi:10.1016/j.icarus.2009.07.015 · Cited by 40
“mets (Halley, Hale-Bopp, and Hayakutake) all have been measured to have a D/H ratio twice the value of the ocean water. Several papers have summarised the D/H problematics; e.g. Robert et al. (2000), Morbidelli et al. (2000), Delsemme (1999, 2006). We will therefore here only very shortly summarise the relevant number…”
BackgroundThe Astrobiology Primer: An Outline of General Knowledge—Version 1, 2006
Editors: L.J. Mix, J. C. A. (2006) · Astrobiology · doi:10.1089/ast.2006.6.735 · Cited by 58
“Models show that Earth could have received its current volatile inventory via incorporation of planetesimals formed in the outer Solar System and gravitationally perturbed inward (Morbidelli et al., 2000; Raymond et al., 2004).”
BackgroundMethodVolatile element abundance patterns and an early liquid water ocean on Earth
Kramers, J. (2003) · Precambrian Research · doi:10.1016/s0301-9268(03)00106-2 · Cited by 35
Formation of Venus, Earth and Mars: Constrained by Isotopes
Lammer, H., Brasser, R., Johansen, A., Scherf, M., & Leitzinger, M. (2020) · Space Science Reviews · doi:10.1007/s11214-020-00778-4 · Cited by 49
Bekaert, D. V., Avice, G., Marty, B. M., Henderson, B. L., & Gudipati, M. S. (2017) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2017.08.041 · Cited by 36
“Such a dichotomy between Earth’s mantle and atmosphere leaves little space for a genetic link between the two reservoirs and an exotic origin of the progenitor of atmospheric Xe has often been advocated (e.g. Swindle and Kring, 1997; Morbidelli et al., 2000; Dauphas, 2003; Raymond et al., 2004; Marty and Meibom, 2007;…”
BackgroundOrigin and Evolution of Water in the Moon's Interior
Hauri, E. H., Saal, A. E., Nakajima, M., Anand, M., Rutherford, M. J., Orman, J. A. V., & Voyer, M. L. (2017) · Annual Review of Earth and Planetary Sciences · doi:10.1146/annurev-earth-063016-020239 · Cited by 50
TERRESTRIAL PLANET FORMATION IN THE PRESENCE OF MIGRATING SUPER-EARTHS
Izidoro, A., Morbidelli, A., & Raymond, S. N. (2014) · The Astrophysical Journal · doi:10.1088/0004-637x/794/1/11 · Cited by 71
“The degree of radial mixing deter- mines each planet’s feeding zone, and the feeding zone is the most important factor in determining each planet’s composition (e.g., Morbidelli et al 2000; Raymond et al 2007a, b; Izidoro et al 2013; 2014).”
BackgroundSelf-citationFORMATION, TIDAL EVOLUTION, AND HABITABILITY OF THE KEPLER-186 SYSTEM
Bolmont, É., Raymond, S. N., von Paris, P., Selsis, F., Hersant, F., Quintana, E. V., & Barclay, T. (2014) · The Astrophysical Journal · doi:10.1088/0004-637x/793/1/3 · Cited by 70
“In the classical model of in situ terrestrial planet formation in the solar system, water is delivered to Earth from primitive C-type asteroidal material (Morbidelli et al. 2000; Raymond et al. 2004, 2007a, 2013).”
BackgroundDeuterated water in the solar-type protostars NGC 1333 IRAS 4A and IRAS 4B
Coutens, A., Vastel, C., Cabrit, S., Codella, C., Kristensen, L., Ceccarelli, C., van Dishoeck, E., Boogert, A., Bottinelli, S., Castets, A., et al. (2013) · doi:10.1051/0004-6361/201322400 · Cited by 34
“…on dry silicate grains in the protosolar nebula (Stimpfl et al. 2004), delivery through asteroids, comets, planetary embryos, and planetesimals (Morbidelli et al. 2000; O’Brien et al. 2006; Raymond et al. 2004, 2006, 2009; Lunine et al. 2003; Drake & Campins 2006), and water production through…”
BackgroundYang, X.-Z. (2012) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2012.08.036 · Cited by 34
Mezger, K., Maltese, A., & Vollstaedt, H. (2021) · Icarus · doi:10.1016/j.icarus.2021.114497 · Cited by 38
The fate of water within Earth and super-Earths and implications for plate tectonics
Tikoo-Schantz, S. M., & Elkins-Tanton, L. T. (2017) · Philosophical Transactions of the Royal Society A Mathematical Physical and Engineering Sciences · doi:10.1098/rsta.2015.0394 · Cited by 42
“A majority of terrestrial water may have been carried by a few planetary embryos from the outer asteroid belt, which then combined to form the Earth during the final stages of planetary accretion [6].”
BackgroundFarihi, J., Koester, D., Zuckerman, B., Vican, L., Gänsicke, B., Smith, N., Walth, G., & Breedt, E. (2016) · doi:10.1093/mnras/stw2182 · Cited by 33
“Of the total iron mass present in the Earth, metallic Fe in the core is thought to represent 87%, whereas Fe in the mantle and crust is only 13% (McDonough 2000), some of which is also metal.”
BackgroundInfluential4. Building of a Habitable Planet
Martin, H., Albarède, F., Claeys, P., Gargaud, M., Marty, B. M., Morbidelli, A., & Pinti, D. L. (2006) · Earth Moon and Planets · doi:10.1007/s11038-006-9088-4 · Cited by 42
“It is a modern concept based on orbital dynamics and on D/H ratios across the solar system that water was added to the surface from the outer solar system (Morbidelli et al., 2000).”
BackgroundInfluentialSelf-citationA gap in HD 92945’s broad planetesimal disc revealed by ALMA
Marino, S., Yelverton, B., Booth, M., Faramaz, V., Kennedy, G., Matrá, L., & Wyatt, M. (2019) · Monthly notices of the Royal Astronomical Society · doi:10.1093/mnras/stz049 · Cited by 32
“If the gap was of secondary origin and cleared by a planet on an orbit at 73 au, some of the planetesimals would get scattered inwards where they could deliver volatiles such as water to inner planets that potentially formed dry (e.g. like Earth, Morbidelli et al. 2000).”
BackgroundAsteroid–comet continuum objects in the solar system
Hsieh, H. H. (2017) · Philosophical Transactions of the Royal Society A Mathematical Physical and Engineering Sciences · doi:10.1098/rsta.2016.0259 · Cited by 33
“the primordial delivery of water to the terrestrial planets [52,95,96,101].”
BackgroundP/2010 A2 LINEAR - I. An impact in the asteroid main belt
Hainaut, O., Kleyna, J., Sarid, G., Hermalyn, B., Zenn, A., Meech, K., Schultz, P., Hsieh, H., Trancho, G., Pittichová, J., et al. (2011) · Astronomy and Astrophysics · doi:10.1051/0004-6361/201118147 · Cited by 32
“C1143(A), and at the University of Hawai‘i 2.2-m telescope, Mauna Kea, Hawai‘i, USA. envelope and oxides in a magma ocean Genda & Ikoma (2007, 2008), or (iii) delivery by volatile-rich planetesimals (asteroids or comets) formed beyond the snow line (Morbidelli et al. 2000).”
BackgroundInfluentialA SEARCH FOR WATER VAPORIZATION ON CERES
Rousselot, P., Jehin, E., Manfroid, J., Mousis, O., Dumas, C., Carry, B., Marboeuf, U., & Zucconi, J. (2011) · The Astronomical Journal · doi:10.1088/0004-6256/142/4/125 · Cited by 32
“In our model, we have assumed that Ceres has an average bulk density of ∼2206 kg m−3 (Carry et al. 2008) and a global ice content of ∼ 10% (Morbidelli et al. 2000).”
MethodSetting the Stage: Planet Formation and Volatile Delivery
Venturini, J., Ronco, M. P., & Guilera, O. M. (2020) · Space Science Reviews · doi:10.1007/s11214-020-00700-y · Cited by 44
Rubie, D. C., Nimmo, F., & Melosh, H. J. (2015) · Elsevier eBooks · doi:10.1016/b978-0-444-53802-4.00154-8 · Cited by 75
DISCOVERY OF A TRANSITING PLANET NEAR THE SNOW-LINE
Kipping, D., Torres, G., Buchhave, L. A., Kenyon, S. J., Henze, C. E., Isaacson, H. T., Kolbl, R., Marcy, G. W., Bryson, S., Stassun, K. G., et al. (2014) · The Astrophysical Journal · doi:10.1088/0004-637x/795/1/25 · Cited by 33
“In the Solar System, evidence from the asteroid belt suggests a “canonical” snow-line distance of around 2.7AU (Abe et al. 2000; Morbidelli et al. 2000; Rivkin et al. 2002).”
The Cytomatrix as a Cooperative System of Macromolecular and Water Networks
Shepherd, V. A. (2006) · Current topics in developmental biology/Current Topics in Developmental Biology · doi:10.1016/s0070-2153(06)75006-2 · Cited by 74
Jennings, E. S., Jacobson, S. A., Rubie, D. C., Nakajima, Y., Vogel, A. K., Rose-Weston, L., & Frost, D. J. (2020) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2020.09.035 · Cited by 33
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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