A new variant of saponite‐rich micrometeorites recovered from recent Antarctic snowfall

Abstract– Eight saponite‐rich micrometeorites with very similar mineralogy were found from the recent surface snow in Antarctica. They might have come to Earth as a larger meteoroid and broke up into pieces on Earth, because they were recovered from the same layer and the same location of the snow....

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Published in:Meteoritics & Planetary Science
Main Authors: SAKAMOTO, Kanako, NAKAMURA, Tomoki, NOGUCHI, Takaaki, TSUCHIYAMA, Akira
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2010
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Online Access:http://dx.doi.org/10.1111/j.1945-5100.2010.01019.x
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1945-5100.2010.01019.x
https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1945-5100.2010.01019.x
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spelling crwiley:10.1111/j.1945-5100.2010.01019.x 2024-06-23T07:47:25+00:00 A new variant of saponite‐rich micrometeorites recovered from recent Antarctic snowfall SAKAMOTO, Kanako NAKAMURA, Tomoki NOGUCHI, Takaaki TSUCHIYAMA, Akira 2010 http://dx.doi.org/10.1111/j.1945-5100.2010.01019.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1945-5100.2010.01019.x https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1945-5100.2010.01019.x en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Meteoritics & Planetary Science volume 45, issue 2, page 220-237 ISSN 1086-9379 1945-5100 journal-article 2010 crwiley https://doi.org/10.1111/j.1945-5100.2010.01019.x 2024-06-06T04:19:34Z Abstract– Eight saponite‐rich micrometeorites with very similar mineralogy were found from the recent surface snow in Antarctica. They might have come to Earth as a larger meteoroid and broke up into pieces on Earth, because they were recovered from the same layer and the same location of the snow. Synchrotron X‐ray diffraction (XRD) analysis indicates that saponite, Mg‐Fe carbonate, and pyrrhotite are major phases and serpentine, magnetite, and pentlandite are minor phases. Anhydrous silicates are entirely absent from all micrometeorites, suggesting that their parental object has undergone heavy aqueous alteration. Saponite/serpentine ratios are higher than in the Orgueil CI chondrite and are similar to the Tagish Lake carbonaceous chondrite. Transmission electron microscope (TEM) observation indicates that serpentine occupies core regions of fine‐grained saponite, pyrrhotite has a low‐Ni concentration, and Mg‐Fe carbonate shows unique concentric ring structures and has a mean molar Mg/(Mg + Fe) ratio of 0.7. Comparison of the mineralogy to hydrated chondrites and interplanetary dust particles (IDPs) suggests that the micrometeorites are most similar to the carbonate‐poor lithology of the Tagish Lake carbonaceous chondrite and some hydrous IDPs, but they show a carbonate mineralogy dissimilar to any primitive chondritic materials. Therefore, they are a new variant of saponite‐rich micrometeorite extracted from a primitive hydrous asteroid and recently accreted to Antarctica. Article in Journal/Newspaper Antarc* Antarctic Antarctica Tagish Wiley Online Library Antarctic Tagish ENVELOPE(-134.272,-134.272,60.313,60.313) Tagish Lake ENVELOPE(-134.233,-134.233,59.717,59.717) Meteoritics & Planetary Science 45 2 220 237
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract– Eight saponite‐rich micrometeorites with very similar mineralogy were found from the recent surface snow in Antarctica. They might have come to Earth as a larger meteoroid and broke up into pieces on Earth, because they were recovered from the same layer and the same location of the snow. Synchrotron X‐ray diffraction (XRD) analysis indicates that saponite, Mg‐Fe carbonate, and pyrrhotite are major phases and serpentine, magnetite, and pentlandite are minor phases. Anhydrous silicates are entirely absent from all micrometeorites, suggesting that their parental object has undergone heavy aqueous alteration. Saponite/serpentine ratios are higher than in the Orgueil CI chondrite and are similar to the Tagish Lake carbonaceous chondrite. Transmission electron microscope (TEM) observation indicates that serpentine occupies core regions of fine‐grained saponite, pyrrhotite has a low‐Ni concentration, and Mg‐Fe carbonate shows unique concentric ring structures and has a mean molar Mg/(Mg + Fe) ratio of 0.7. Comparison of the mineralogy to hydrated chondrites and interplanetary dust particles (IDPs) suggests that the micrometeorites are most similar to the carbonate‐poor lithology of the Tagish Lake carbonaceous chondrite and some hydrous IDPs, but they show a carbonate mineralogy dissimilar to any primitive chondritic materials. Therefore, they are a new variant of saponite‐rich micrometeorite extracted from a primitive hydrous asteroid and recently accreted to Antarctica.
format Article in Journal/Newspaper
author SAKAMOTO, Kanako
NAKAMURA, Tomoki
NOGUCHI, Takaaki
TSUCHIYAMA, Akira
spellingShingle SAKAMOTO, Kanako
NAKAMURA, Tomoki
NOGUCHI, Takaaki
TSUCHIYAMA, Akira
A new variant of saponite‐rich micrometeorites recovered from recent Antarctic snowfall
author_facet SAKAMOTO, Kanako
NAKAMURA, Tomoki
NOGUCHI, Takaaki
TSUCHIYAMA, Akira
author_sort SAKAMOTO, Kanako
title A new variant of saponite‐rich micrometeorites recovered from recent Antarctic snowfall
title_short A new variant of saponite‐rich micrometeorites recovered from recent Antarctic snowfall
title_full A new variant of saponite‐rich micrometeorites recovered from recent Antarctic snowfall
title_fullStr A new variant of saponite‐rich micrometeorites recovered from recent Antarctic snowfall
title_full_unstemmed A new variant of saponite‐rich micrometeorites recovered from recent Antarctic snowfall
title_sort new variant of saponite‐rich micrometeorites recovered from recent antarctic snowfall
publisher Wiley
publishDate 2010
url http://dx.doi.org/10.1111/j.1945-5100.2010.01019.x
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1945-5100.2010.01019.x
https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1945-5100.2010.01019.x
long_lat ENVELOPE(-134.272,-134.272,60.313,60.313)
ENVELOPE(-134.233,-134.233,59.717,59.717)
geographic Antarctic
Tagish
Tagish Lake
geographic_facet Antarctic
Tagish
Tagish Lake
genre Antarc*
Antarctic
Antarctica
Tagish
genre_facet Antarc*
Antarctic
Antarctica
Tagish
op_source Meteoritics & Planetary Science
volume 45, issue 2, page 220-237
ISSN 1086-9379 1945-5100
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1111/j.1945-5100.2010.01019.x
container_title Meteoritics & Planetary Science
container_volume 45
container_issue 2
container_start_page 220
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