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The Solar System calcium isotopic composition inferred from Ryugu samples

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Title: The Solar System calcium isotopic composition inferred from Ryugu samples
Authors: Moynier, F. Browse this author
Dai, W. Browse this author
Yokoyama, T. Browse this author
Hu, Y. Browse this author
Paquet, M. Browse this author
Abe, Y. Browse this author
Aleon, J. Browse this author
Alexander, C. M. O'D. Browse this author
Amari, S. Browse this author
Amelin, Y. Browse this author
Bajo, K. -I. Browse this author
Bizzarro, M. Browse this author
Bouvier, A. Browse this author
Carlson, R. W. Browse this author
Chaussidon, M. Browse this author
Choi, B. -G. Browse this author
Dauphas, N. Browse this author
Davis, A. M. Browse this author
Di Rocco, T. Browse this author
Fujiya, W. Browse this author
Fukai, R. Browse this author
Gautam, I. Browse this author
Haba, M. K. Browse this author
Hibiya, Y. Browse this author
Hidaka, H. Browse this author
Homma, H. Browse this author
Hoppe, P. Browse this author
Huss, G. R. Browse this author
Ichida, K. Browse this author
Iizuka, T. Browse this author
Ireland, T. R. Browse this author
Ishikawa, A. Browse this author
Ito, M. Browse this author
Itoh, S. Browse this author
Kawasaki, N. Browse this author
Kita, N. T. Browse this author
Kitajima, K. Browse this author
Kleine, T. Browse this author
Komatani, S. Browse this author
Krot, A. N. Browse this author
Liu, M. -C. Browse this author
Masuda, Y. Browse this author
McKeegan, K. D. Browse this author
Morita, M. Browse this author
Motomura, K. Browse this author
Nakai, I. Browse this author
Nagashima, K. Browse this author
Nesvorny, D. Browse this author
Nguyen, A. Browse this author
Nittler, L. Browse this author
Onose, M. Browse this author
Pack, A. Browse this author
Park, C. Browse this author
Piani, L. Browse this author
Qin, L. Browse this author
Russell, S. S. Browse this author
Sakamoto, N. Browse this author
Schoenbaechler, M. Browse this author
Tafla, L. Browse this author
Tang, H. Browse this author
Terada, K. Browse this author
Terada, Y. Browse this author
Usui, T. Browse this author
Wada, S. Browse this author
Wadhwa, M. Browse this author
Walker, R. J. Browse this author
Yamashita, K. Browse this author
Yin, Q. -Z. Browse this author
Yoneda, S. Browse this author
Young, E. D. Browse this author
Yui, H. Browse this author
Zhang, A. -c. Browse this author
Nakamura, T. Browse this author
Naraoka, H. Browse this author
Noguchi, T. Browse this author
Okazaki, R. Browse this author
Sakamoto, K. Browse this author
Yabuta, H. Browse this author
Abe, M. Browse this author
Miyazaki, A. Browse this author
Nakato, A. Browse this author
Nishimura, M. Browse this author
Okada, T. Browse this author
Yada, T. Browse this author
Yogata, K. Browse this author
Nakazawa, S. Browse this author
Saiki, T. Browse this author
Tanaka, S. Browse this author
Terui, F. Browse this author
Tsuda, Y. Browse this author
Watanabe, S. -I. Browse this author
Yoshikawa, M. Browse this author
Tachibana, S. Browse this author
Yurimoto, H. Browse this author →KAKEN DB
Issue Date: 19-Oct-2022
Publisher: European Association of Geochemistry
Journal Title: Geochemical Perspectives Letters
Volume: 24
Start Page: 1
End Page: 6
Publisher DOI: 10.7185/geochemlet.2238
Abstract: CO CV CM CI Ryugu A Ryugu C 0.0 0.5 1.0 1.5 44/40CaSRM915a (age corrected) The Hayabusa2 spacecraft has returned samples from the Cb-type asteroid (162173) Ryugu to Earth. Previous petrological and chemical analyses support a close link between Ryugu and CI chondrites that are presumed to be chemically the most primitive meteorites with a solar-like composition. However, Ryugu samples are highly enriched in Ca compared to typical CI chondrites. To identify the cause of this discrepancy, here we report stable Ca isotopic data (expressed as delta 44/40CaSRM915a) for returned Ryugu samples collected from two sites. We found that samples from both sites have similar delta 44/40CaSRM915a (0.58 +/- 0.03 parts per thousand and 0.55 +/- 0.08 parts per thousand, 2 s.d.) that fall within the range defined by CIs. This isotopic similarity suggests that the Ca budget of CIs and Ryugu samples is dominated by carbonates, and the variably higher Ca contents in Ryugu samples are due to the abundant carbonates. Precipitation of carbonates on Ryugu likely coincided with a major episode of aqueous activity dated to have occurred similar to 5 Myr after Solar System formation. Based on the pristine Ryugu samples, the average delta 44/40CaSRM915a of the Solar System is defined to be 0.57 +/- 0.04 parts per thousand (2 s.d.).
Type: article
URI: http://hdl.handle.net/2115/87402
Appears in Collections:理学院・理学研究院 (Graduate School of Science / Faculty of Science) > 雑誌発表論文等 (Peer-reviewed Journal Articles, etc)

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