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. 2025 Sep 10.
doi: 10.1038/s41586-025-09483-0. Online ahead of print.

Late fluid flow in a primitive asteroid revealed by Lu-Hf isotopes in Ryugu

Tsuyoshi Iizuka  1 Takazo Shibuya  2 Takehito Hayakawa  3 Tetsuya Yokoyama  4 Ikshu Gautam  4 Makiko K Haba  4 Kengo T M Ito  5 Yuki Hibiya  6   7 Akira Yamaguchi  8   9 Yoshinari Abe  10 Jérôme Aléon  11 Conel M O'D Alexander  12 Sachiko Amari  5   13 Yuri Amelin  14 Ken-Ichi Bajo  15 Martin Bizzarro  16 Audrey Bouvier  17 Richard W Carlson  12 Marc Chaussidon  18 Byeon-Gak Choi  19 Nicolas Dauphas  20   21 Andrew M Davis  20 Tommaso Di Rocco  22 Wataru Fujiya  23 Ryota Fukai  24 Hiroshi Hidaka  25 Hisashi Homma  26 Gary R Huss  27 Trevor R Ireland  28 Akira Ishikawa  4 Shoichi Itoh  29 Noriyuki Kawasaki  30 Noriko T Kita  31 Koki Kitajima  31 Thorsten Kleine  32 Shintaro Komatani  33 Alexander N Krot  27 Ming-Chang Liu  34 Yuki Masuda  4   16 Kazuko Motomura  35 Frédéric Moynier  18 Kazuhide Nagashima  27 Izumi Nakai  36 Ann Nguyen  37 Larry Nittler  12 Andreas Pack  22 Changkun Park  38 Laurette Piani  39 Liping Qin  40 Sara Russell  41 Naoya Sakamoto  42 Maria Schönbächler  43 Lauren Tafla  34 Haolan Tang  40 Kentaro Terada  44 Yasuko Terada  45 Tomohiro Usui  24 Sohei Wada  30 Meenakshi Wadhwa  46 Richard J Walker  47 Katsuyuki Yamashita  48 Qing-Zhu Yin  49 Shigekazu Yoneda  50 Hiroharu Yui  51 Ai-Cheng Zhang  52 Tomoki Nakamura  53 Hiroshi Naraoka  54 Takaaki Noguchi  29 Ryuji Okazaki  54 Kanako Sakamoto  24 Hikaru Yabuta  55 Masanao Abe  24 Akiko Miyazaki  24 Aiko Nakato  8   24 Masahiro Nishimura  24 Tatsuaki Okada  24 Toru Yada  24 Kasumi Yogata  24 Satoru Nakazawa  24 Takanao Saiki  24 Satoshi Tanaka  24 Fuyuto Terui  56 Yuichi Tsuda  24 Sei-Ichiro Watanabe  25 Makoto Yoshikawa  24 Shogo Tachibana  24   57 Hisayoshi Yurimoto  30
Affiliations

Late fluid flow in a primitive asteroid revealed by Lu-Hf isotopes in Ryugu

Tsuyoshi Iizuka et al. Nature. .

Abstract

Carbonaceous asteroids are the source of the most primitive meteorites1 and represent leftover planetesimals that formed from ice and dust in the outer Solar System and may have delivered volatiles to the terrestrial planets2-5. Understanding the aqueous activity of asteroids is key to deciphering their thermal, chemical and orbital evolution, with implications for the origin of water on the terrestrial planets. Analyses of the objects, in particular pristine samples returned from asteroid Ryugu, have provided detailed information on fluid-rock interactions within a few million years after parent-body formation6-11. However, the long-term fate of asteroidal water remains poorly understood. Here we present evidence for fluid flow in a carbonaceous asteroid more than 1 billion years after formation, based on the 176Lu-176Hf decay systematics of Ryugu samples, which reflect late lutetium mobilization. Such late fluid flow was probably triggered by an impact that generated heat for ice melting and opened rock fractures for fluid migration. This contrasts the early aqueous activity powered by short-lived radioactive decay, with limited fluid flow and little elemental fractionation12. Our results imply that carbonaceous planetesimals accreted by the terrestrial planets could have retained not only hydrous minerals but also aqueous water, leading to an upwards revision of the inventory of their water delivery by a factor of two to three.

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Conflict of interest statement

Competing interests: The authors declare no competing interests.

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