Coevolution of phyllosilicate, carbon, sulfide, and apatite in Ryugu's parent body

Author:

Gainsforth Zack1ORCID,Dominguez Gerardo2,Amano Kana3ORCID,Matsumoto Megumi3,Fujioka Yuri3,Kagawa Eiichi3,Nakamura Tomoki3,Tachibana Shogo45ORCID,Morita Tomoyo3,Kikuiri Mizuha3,Yurimoto Hisayoshi6ORCID,Noguchi Takaaki7ORCID,Okazaki Ryuji8,Yabuta Hikaru9,Naraoka Hiroshi8,Sakamoto Kanako4,Yada Toru4,Nishimura Masahiro4,Nakato Aiko4,Miyazaki Akiko4,Yogata Kasumi4,Abe Masano4,Okada Tatsuaki4,Usui Tomohiro4,Yoshikawa Makoto4,Saiki Takanao4,Tanaka Satoshi4,Terui Fuyuto10,Nakazawa Satoru4,Watanabe Sei‐ichiro11,Tsuda Yuichi4,

Affiliation:

1. Space Sciences Laboratory University of California at Berkeley Berkeley California USA

2. Department of Physics California State University San Marcos California USA

3. Department of Earth Science Tohoku University Sendai Japan

4. Institute of Space and Astronautical Science (ISAS), Japan Aerospace Exploration Agency (JAXA) Sagamihara Japan

5. Department of Earth and Planetary Science The University of Tokyo Tokyo Japan

6. Division of Earth and Planetary Sciences Hokkaido University Sapporo Japan

7. Division of Earth and Planetary Sciences Kyoto University Kyoto Japan

8. Department of Earth and Planetary Sciences Kyushu University Fukuoka Japan

9. Department of Earth and Planetary Systems Science Hiroshima University Higashi‐Hiroshima Japan

10. Department of Mechanical Engineering Kanagawa Institute of Technology Atsugi Japan

11. Department of Earth and Environmental Sciences Nagoya University Nagoya Japan

Abstract

AbstractWe analyzed an asteroid Ryugu sample returned to Earth by JAXA's Hayabusa2 mission using nanoIR, SEM, and TEM microscopy. We identified multiple distinct carbon reservoirs within the phyllosilicate matrix and demonstrate infrared spectral affinities for some of the carbon to insoluble organic matter (IOM). TEM studies of Ryugu samples have allowed us to better understand the interrelationship between the crystallographic orientations of phyllosilicates and the secondary minerals such as carbonate, sulfide, and apatite. Transport of elements provides a unifying theme for understanding these interrelationships.

Funder

Institute of Space and Astronautical Science

Japan Aerospace Exploration Agency

National Aeronautics and Space Administration

Publisher

Wiley

Reference89 articles.

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3. The nature, origin and modification of insoluble organic matter in chondrites, the major source of Earth’s C and N

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