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. 2022 Nov 18;8(46):eadd8141.
doi: 10.1126/sciadv.add8141. Epub 2022 Nov 16.

Ryugu's nucleosynthetic heritage from the outskirts of the Solar System

Timo Hopp  1 Nicolas Dauphas  1 Yoshinari Abe  2 Jérôme Aléon  3 Conel M O'D Alexander  4 Sachiko Amari  5   6 Yuri Amelin  7 Ken-Ichi Bajo  8 Martin Bizzarro  9 Audrey Bouvier  10 Richard W Carlson  4 Marc Chaussidon  11 Byeon-Gak Choi  12 Andrew M Davis  1 Tommaso Di Rocco  13 Wataru Fujiya  14 Ryota Fukai  15 Ikshu Gautam  16 Makiko K Haba  16 Yuki Hibiya  17   18 Hiroshi Hidaka  19 Hisashi Homma  20 Peter Hoppe  21 Gary R Huss  22 Kiyohiro Ichida  23 Tsuyoshi Iizuka  24 Trevor R Ireland  25 Akira Ishikawa  16 Motoo Ito  26 Shoichi Itoh  27 Noriyuki Kawasaki  8 Noriko T Kita  28 Kouki Kitajima  28 Thorsten Kleine  29 Shintaro Komatani  23 Alexander N Krot  22 Ming-Chang Liu  30   31 Yuki Masuda  16 Kevin D McKeegan  30 Mayu Morita  23 Kazuko Motomura  32 Frédéric Moynier  11 Izumi Nakai  32 Kazuhide Nagashima  22 David Nesvorný  33 Ann Nguyen  34 Larry Nittler  4   35 Morihiko Onose  23 Andreas Pack  13 Changkun Park  36 Laurette Piani  37 Liping Qin  38 Sara S Russell  39 Naoya Sakamoto  40 Maria Schönbächler  41 Lauren Tafla  30 Haolan Tang  30   42 Kentaro Terada  43 Yasuko Terada  44 Tomohiro Usui  15 Sohei Wada  8 Meenakshi Wadhwa  35 Richard J Walker  45 Katsuyuki Yamashita  46 Qing-Zhu Yin  47 Tetsuya Yokoyama  16 Shigekazu Yoneda  48 Edward D Young  30 Hiroharu Yui  49 Ai-Cheng Zhang  50 Tomoki Nakamura  51 Hiroshi Naraoka  52 Takaaki Noguchi  26 Ryuji Okazaki  52 Kanako Sakamoto  15 Hikaru Yabuta  53 Masanao Abe  15 Akiko Miyazaki  15 Aiko Nakato  15 Masahiro Nishimura  15 Tatsuaki Okada  15 Toru Yada  15 Kasumi Yogata  15 Satoru Nakazawa  15 Takanao Saiki  15 Satoshi Tanaka  15 Fuyuto Terui  54 Yuichi Tsuda  15 Sei-Ichiro Watanabe  19 Makoto Yoshikawa  15 Shogo Tachibana  55 Hisayoshi Yurimoto  8
Affiliations

Ryugu's nucleosynthetic heritage from the outskirts of the Solar System

Timo Hopp et al. Sci Adv. .

Abstract

Little is known about the origin of the spectral diversity of asteroids and what it says about conditions in the protoplanetary disk. Here, we show that samples returned from Cb-type asteroid Ryugu have Fe isotopic anomalies indistinguishable from Ivuna-type (CI) chondrites, which are distinct from all other carbonaceous chondrites. Iron isotopes, therefore, demonstrate that Ryugu and CI chondrites formed in a reservoir that was different from the source regions of other carbonaceous asteroids. Growth and migration of the giant planets destabilized nearby planetesimals and ejected some inward to be implanted into the Main Belt. In this framework, most carbonaceous chondrites may have originated from regions around the birthplaces of Jupiter and Saturn, while the distinct isotopic composition of CI chondrites and Ryugu may reflect their formation further away in the disk, owing their presence in the inner Solar System to excitation by Uranus and Neptune.

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Figures

Fig. 1.
Fig. 1.. Previously published isotopic anomalies of Ti, Cr, and O in Ryugu and other Solar System materials.
Plots of μ50Ti versus μ54Cr (A), μ50Ti versus Δ17O (B), and μ54Cr versus Δ17O (C). In these diagrams, Ryugu and CI represent an endmember to the CC array. Data for Ryugu are from Yokoyama et al. (6). The average Ti and Cr isotopic compositions of NC and CC meteorite groups and Earth’s mantle are from the data compilation of Burkhardt et al. (64) and O isotopic data from the compilation of Dauphas (65). Uncertainties for individual groups are the 95% confidence interval of the mean. If not visible, error bars are smaller than symbols.
Fig. 2.
Fig. 2.. Fe isotopic anomalies of returned samples from Cb-type asteroid (162173) Ryugu and carbonaceous chondrites (Table 1).
Ryugu samples and CI chondrites have identical μ54Fe values, which are distinct from all other carbonaceous chondrite groups [CM, CV, CO, CR, and Ung (ungrouped)]. The open triangle is the CI chondrite average from Schiller et al. (22).
Fig. 3.
Fig. 3.. Isotopic anomalies of Fe and Ti in Solar System materials.
Ryugu samples and CI chondrites have identical μ54Fe and μ50Ti values that are distinct from other meteorites. Red circles correspond to NC chondrite groups (E, enstatite; R, rumuruti; OC, ordinary chondrites), red diamonds to NC achondrites (Ure, ureilites; Dio, diogenites), and blue circles to CC chondrite groups (TL, Tagish Lake). The green square is Earth’s mantle. The average composition of Ryugu and CI chondrites is shown as triangles. Average compositions of meteorite groups and Earth’s mantle are calculated using data from this study (Table 1) and the data compilation of Burkhardt et al. (64) (table S1). If not visible, error bars are smaller than symbols.
Fig. 4.
Fig. 4.. Schematic of the possible source region of Cb-type asteroids and CI chondrites.
Planetesimals formed in different regions of the protoplanetary disk. Volatile-poor planetesimals (red circles) formed in the inner region, while volatile-rich planetesimals (blue circles) formed beyond Jupiter’s orbit. The growth and migration of the gas and ice giant planets implanted some of the planetesimals into the Main Belt (small arrows), while the majority of planetesimals were transported outward or ejected from the disk (large arrows) (39). A plausible explanation for the distinct Fe nucleosynthetic heritage and primitive chemical composition of CI chondrites and Ryugu is that they were implanted in the Main Belt by excitation from Uranus and Neptune (filled bright blue circles), while other CCs formed in more internal regions near Jupiter and Saturn (filled dark blue circles) (fig. S4). The icy planetesimals that were formed around Uranus and Neptune and were ejected outward went to populate the Oort cloud (44, 45). CI chondrites and Ryugu may thus share some parentage with long-period comets. Such a scenario could explain the trichotomy between NC, CC, and CI for nucleosynthetic anomalies (Fig. 3).

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