4.7 Article

53Mn-53Cr CHRONOMETRY OF CB CHONDRITE: EVIDENCE FOR UNIFORM DISTRIBUTION OF 53Mn IN THE EARLY SOLAR SYSTEM

Journal

ASTROPHYSICAL JOURNAL
Volume 723, Issue 1, Pages 20-24

Publisher

IOP PUBLISHING LTD
DOI: 10.1088/0004-637X/723/1/20

Keywords

astrochemistry; meteorites, meteors, meteoroids; minor planets, asteroids: general; nuclear reactions, nucleosynthesis, abundances; protoplanetary disks

Funding

  1. Japan Society for the Promotion for Science (JSPS)
  2. Ministry of Education, Culture, Sports, Science, and Technology (MEXT)

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High-precision Cr isotope ratios for chondrules and metal grain separated from CB chondrite Gujba were determined. The epsilon Cr-54 values (epsilon Cr-i = [(Cr-i/Cr-52)(sample)/(Cr-i/Cr-52)(standard) - 1] x 104) for all samples were identical within the analytical uncertainty, with a mean value of +1.29 +/- 0.02. Uniform epsilon Cr-54 signatures of both chondrules and metal grains imply that the Cr isotope systematics of the meteorite was once completely equilibrated. The epsilon Cr-53 values of the chondrules and metal grain, on the other hand, display a strong correlation with the Mn-55/Cr-52 ratio. The Mn-53/Mn-55 calculated from the slope of the isochron is (3.18 +/- 0.52) x 10(-6). This corresponds to absolute ages of 4563.7 +/- 1.2 Ma and 4563.5 +/- 1.1 Ma using angrites D'Orbigny and LEW 86010, respectively, as time anchors. These ages are consistent with the ages obtained using other short-and long-lived radio nuclides, supporting the uniform distribution of Mn-53 in the early solar nebula.

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