TY - JOUR
T1 - Chondrule-like objects and Ca-Al-rich inclusions in Ryugu may potentially be the oldest Solar System materials
AU - Nakashima, Daisuke
AU - Nakamura, Tomoki
AU - Zhang, Mingming
AU - Kita, Noriko T.
AU - Mikouchi, Takashi
AU - Yoshida, Hideto
AU - Enokido, Yuma
AU - Morita, Tomoyo
AU - Kikuiri, Mizuha
AU - Amano, Kana
AU - Kagawa, Eiichi
AU - Yada, Toru
AU - Nishimura, Masahiro
AU - Nakato, Aiko
AU - Miyazaki, Akiko
AU - Yogata, Kasumi
AU - Abe, Masanao
AU - Okada, Tatsuaki
AU - Usui, Tomohiro
AU - Yoshikawa, Makoto
AU - Saiki, Takanao
AU - Tanaka, Satoshi
AU - Nakazawa, Satoru
AU - Terui, Fuyuto
AU - Yurimoto, Hisayoshi
AU - Noguchi, Takaaki
AU - Yabuta, Hikaru
AU - Naraoka, Hiroshi
AU - Okazaki, Ryuji
AU - Sakamoto, Kanako
AU - Watanabe, Sei ichiro
AU - Tachibana, Shogo
AU - Tsuda, Yuichi
N1 - Publisher Copyright:
© 2023, The Author(s).
PY - 2023/12
Y1 - 2023/12
N2 - Chondrule-like objects and Ca-Al-rich inclusions (CAIs) are discovered in the retuned samples from asteroid Ryugu. Here we report results of oxygen isotope, mineralogical, and compositional analysis of the chondrule-like objects and CAIs. Three chondrule-like objects dominated by Mg-rich olivine are 16O-rich and -poor with Δ17O (=δ17O – 0.52 × δ18O) values of ~ –23‰ and ~ –3‰, resembling what has been proposed as early generations of chondrules. The 16O-rich objects are likely to be melted amoeboid olivine aggregates that escaped from incorporation into 16O-poor chondrule precursor dust. Two CAIs composed of refractory minerals are 16O-rich with Δ17O of ~ –23‰ and possibly as old as the oldest CAIs. The discovered objects (<30 µm) are as small as those from comets, suggesting radial transport favoring smaller objects from the inner solar nebula to the formation location of the Ryugu original parent body, which is farther from the Sun and scarce in chondrules. The transported objects may have been mostly destroyed during aqueous alteration in the Ryugu parent body.
AB - Chondrule-like objects and Ca-Al-rich inclusions (CAIs) are discovered in the retuned samples from asteroid Ryugu. Here we report results of oxygen isotope, mineralogical, and compositional analysis of the chondrule-like objects and CAIs. Three chondrule-like objects dominated by Mg-rich olivine are 16O-rich and -poor with Δ17O (=δ17O – 0.52 × δ18O) values of ~ –23‰ and ~ –3‰, resembling what has been proposed as early generations of chondrules. The 16O-rich objects are likely to be melted amoeboid olivine aggregates that escaped from incorporation into 16O-poor chondrule precursor dust. Two CAIs composed of refractory minerals are 16O-rich with Δ17O of ~ –23‰ and possibly as old as the oldest CAIs. The discovered objects (<30 µm) are as small as those from comets, suggesting radial transport favoring smaller objects from the inner solar nebula to the formation location of the Ryugu original parent body, which is farther from the Sun and scarce in chondrules. The transported objects may have been mostly destroyed during aqueous alteration in the Ryugu parent body.
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U2 - 10.1038/s41467-023-36268-8
DO - 10.1038/s41467-023-36268-8
M3 - Article
C2 - 36797235
AN - SCOPUS:85148263249
SN - 2041-1723
VL - 14
JO - Nature communications
JF - Nature communications
IS - 1
M1 - 532
ER -