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Microscale Hydrogen, Carbon, and Nitrogen Isotopic Diversity of Organic Matter in Asteroid Ryugu

Authors :
Nittler, Larry R
Barosch, Jens
Burgess, Katherine
Stroud, Rhonda M
Wang, Jianhua
Yabuta, Hikaru
Enokido, Yuma
Matsumoto, Megumi
Nakamura, Tomoki
Kebukawa, Yoko
Yamashita, Shohei
Takahashi, Yoshio
Bejach, Laure
Bonal, Lydie
Cody, George D
Dartois, Emmanuel
Dazzi, Alexandre
De Gregorio, Bradley
Deniset-Besseau, Ariane
Duprat, Jean
Engrand, Cécile
Hashiguchi, Minako
Kilcoyne, A. L. David
Komatsu, Mutsumi
Martins, Zita
Mathurin, Jérémie
Montagnac, Gilles
Mostefaoui, Smail
Okumura, Taiga
Quirico, Eric
Remusat, Laurent
Sandford, Scott
Shigenaka, Miho
Suga, Hiroki
Takeichi, Yasuo
Tamenori, Yusuke
Verdier-Paoletti, Maximilien
Wakabayashi, Daisuke
Abe, Masanao
Kamide, Kanami
Miyazaki, Akiko
Nakato, Aiko
Nakazawa, Satoru
Nishimura, Masahiro
Okada, Tatsuaki
Saiki, Takanao
Tanaka, Satoshi
Terui, Fuyuto
Usui, Tomohiro
Yada, Toru
Yogata, Kasumi
Yoshikawa, Makoto
Yurimoto, Hisayoshi
Noguchi, Takaaki
Okazaki, Ryuji
Naraoka, Hiroshi
Sakamoto, Kanako
Tachibana, Shogo
Watanabe, Sei-ichiro
Tsuda, Yuichi
Publication Year :
2024

Abstract

We report the H, C, and N isotopic compositions of microscale (0.2 to 2$\mu$m) organic matter in samples of asteroid Ryugu and the Orgueil CI carbonaceous chondrite. Three regolith particles of asteroid Ryugu, returned by the Hayabusa2 spacecraft, and several fragments of Orgueil were analyzed by NanoSIMS isotopic imaging. The isotopic distributions of the Ryugu samples from two different collection spots are closely similar to each other and to the Orgueil samples, strengthening the proposed Ryugu-CI chondrite connection. Most individual sub-$\mu$m organic grains have isotopic compositions within error of bulk values, but 2-8% of them are outliers exhibiting large isotopic enrichments or depletions in D, $^{15}$N, and/or $^{13}$C. The H, C and N isotopic compositions of the outliers are not correlated with each other: while some C-rich grains are both D- and $^{15}$N-enriched, many are enriched or depleted in one or the other system. This most likely points to a diversity in isotopic fractionation pathways and thus diversity in the local formation environments for the individual outlier grains. The observation of a relatively small population of isotopic outlier grains can be explained either by escape from nebular and/or parent body homogenization of carbonaceous precursor material or addition of later isotopic outlier grains. The strong chemical similarity of isotopically typical and isotopically outlying grains, as reflected by synchrotron x-ray absorption spectra, suggests a genetic connection and thus favors the former, homogenization scenario. However, the fact that even the least altered meteorites show the same pattern of a small population of outliers on top of a larger population of homogenized grains indicates that some or most of the homogenization occurred prior to accretion of the macromolecular organic grains into asteroidal parent bodies.<br />Comment: Accepted for publication in Earth and Planetary Science Letters. 8 figures (plus 3 supplementary figs), two tables

Details

Database :
arXiv
Publication Type :
Report
Accession number :
edsarx.2404.08795
Document Type :
Working Paper