Japanese Antarctic Meteorite Collection

Japan

The storage room for Antarctic Meteorites at NIPR. Antarctic meteorites are stored in cabinets.

The storage room for Antarctic Meteorites at NIPR. Antarctic meteorites are stored in cabinets.

Housing institution

National Institute of Polar Research

Location

10-3 Midori-cho, Tachikawa, Tokyo 190-8518, Japan
35°42′ 44.6″N, 139° 24′ 32″ E

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The storage room for Antarctic Meteorites at NIPR. Antarctic meteorites are stored in cabinets.

The Antarctic meteorite collection represents a wide range of Solar System materials, including a few from Mars and Moon.

The Antarctic Meteorite Research Center at the National Institute of Polar Research (NIPR) in Japan houses a collection of approximately 17,400 meteorites, primarily recovered from the ice fields near the Yamato and Sor Rondane mountains in Antarctica by 24 expeditions. The expeditions were initiated in response to the discovery of areas of the dense concentration of meteorites in 1969-1974 [1,2]. Upon recovery in Antarctica, these frozen meteorites are transported to Japan, where they undergo a thawing process to prevent any precipitation, ensuring their pristine condition. The NIPR’s protocols include initial descriptions and classifications of each meteorite, followed by careful cataloging. About 13,000 meteorites have been classified, published in Meteorite Newsletter [3], and registered to the Meteoritical Society Database. To preserve their integrity and minimize contamination, the meteorites are stored in a Class-10000 clean room at approximately 20°C with a relative humidity below 50%. After cataloging, meteorite samples are distributed for research, education, and public outreach.

Since 1969, the Japanese Antarctic Research Expeditions initiated a groundbreaking venture by discovering meteorite concentrations in Antarctica, marking the beginning of systematic extraterrestrial material collection in the region. These meteorites offer a pristine glimpse into the early Solar System and the geological evolution of planetary bodies, the Moon and Mars [4,5], owing to Antarctica’s minimal contamination and favorable preservation conditions [2]. The contributions of Antarctic meteorites extend beyond enhancing our catalog of Solar System materials. Furthermore, these collections complement space missions by serving as geochemical and mineralogical standards, thus supporting a broader understanding of planetary history and evolution. Overall, Antarctic meteorite recovery represents a significant, cost-effective resource for planetary science, highlighting Antarctica’s role as a vital repository of extraterrestrial materials. This collection not only serves the global scientific community by providing valuable samples for research but also extends its reach to educational institutions and local museums. Through these efforts, the NIPR plays a crucial role in fostering a deeper understanding of our planetary community within the academic world and the broader public.

National Institute of Polar Research, Tachikawa, Japan.

  1. Yoshida, M. (2010): Discovery of the Yamato meteorites in 1969. Polar Science 3, 272–284. https://doi.org/10.1016/j.polar.2009.11.001
  2. Yamaguchi, A., Shiraishi K., Harvey R. (2021) The discovery of meteorites near the Yamato Mountains: How the 1969 discoveries changed planetary science. Meteorit. Planet. Sci. 1, 11-12, https://doi.org/10.1111/maps.13624
  3. Meteorite Newsletter. https://nipr.repo.nii.ac.jp/search?page=1&size=20&sort=controlnumber&search_type=2&q=1418
  4. Kimura, M., Imae N., Komatsu, M., Barrat, J.A., Greenwood, R.C., Yamaguchi, A. and Noguchi, T. (2020): The most primitive CM chondrites, Asuka 12085, 12169, and 12236, of subtypes 3.0–2.8: Their characteristic features and classification. Polar Sci. 26, 100565. https://doi.org/10.1016/j.polar.2020.100565
  5. Kojima, H., Miyamoto, M. and Warren, P.H. (1997) The Yamato-793605 Martian meteorite consortium. Antarct. Meteorite Res. 10-3-12.