Chemical Classification of Spherules Recovered From The Pacific Ocean Site of The CNEOS 2014-01-08 (IM1) Bolide

Fuente: arXiv
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Main Authors: Loeb, A., Jacobsen, S. B., Tagle, R., Adamson, T., Bergstrom, S., Cloete, R., Cohen, S., Domine, Laura, Fu, H., Hoskinson, C., Hyung, E., Kelly, M., Lard, E., Laukien, F., Lem, J., McCallum, R., Millsap, R., Parendo, C., Pataev, M. I., Peddeti, C., Pugh, J., Samuha, S., Sasselov, D. D., Schlereth, M., Siler, J., Siraj, A., Smith, P. M., Taylor, J., Weed, R., Wright, A., Wynn, J.
Format: Preprint
Published: 2024
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author Loeb, A.
Jacobsen, S. B.
Tagle, R.
Adamson, T.
Bergstrom, S.
Cloete, R.
Cohen, S.
Domine, Laura
Fu, H.
Hoskinson, C.
Hyung, E.
Kelly, M.
Lard, E.
Laukien, F.
Lem, J.
McCallum, R.
Millsap, R.
Parendo, C.
Pataev, M. I.
Peddeti, C.
Pugh, J.
Samuha, S.
Sasselov, D. D.
Schlereth, M.
Siler, J.
Siraj, A.
Smith, P. M.
Taylor, J.
Weed, R.
Wright, A.
Wynn, J.
author_facet Loeb, A.
Jacobsen, S. B.
Tagle, R.
Adamson, T.
Bergstrom, S.
Cloete, R.
Cohen, S.
Domine, Laura
Fu, H.
Hoskinson, C.
Hyung, E.
Kelly, M.
Lard, E.
Laukien, F.
Lem, J.
McCallum, R.
Millsap, R.
Parendo, C.
Pataev, M. I.
Peddeti, C.
Pugh, J.
Samuha, S.
Sasselov, D. D.
Schlereth, M.
Siler, J.
Siraj, A.
Smith, P. M.
Taylor, J.
Weed, R.
Wright, A.
Wynn, J.
contents We have conducted an extensive towed-magnetic-sled survey during the period of June 14-28, 2023, over the seafloor about 85 km north of Manus Island, Papua New Guinea, centered around the calculated path of the bolide CNEOS 2014-01-08 (IM1). We found about 850 spherules of diameter 0.1-1.3 millimeters in our samples. The samples were analyzed by micro-XRF, Electron Probe Microanalyzer and ICP Mass spectrometry. Here we report major and trace element compositions of the samples and classify spherules based on that analysis. Spherules comprising 22% of the collection, appear to all reflect planetary igneous differentiation and are all different from previously described spherules. A subset of the differentiated-spherules show an excess of Be, La and U, by up to three orders of magnitude relative to the solar system standard of CI chondrites. Detailed mass spectrometry of 12 of these "BeLaU"-type spherules, the population of which may constitute up to ~10% of our entire collected sample, suggests that they are derived from material formed by planetary igneous fractionation. Their chemical composition is unlike any known solar system material. The "BeLaU"-type spherules reflect a highly differentiated, extremely evolved composition of an unknown source.
format Preprint
id arxiv_https___arxiv_org_abs_2401_09882
institution arXiv
publishDate 2024
record_format arxiv
spellingShingle Chemical Classification of Spherules Recovered From The Pacific Ocean Site of The CNEOS 2014-01-08 (IM1) Bolide
Loeb, A.
Jacobsen, S. B.
Tagle, R.
Adamson, T.
Bergstrom, S.
Cloete, R.
Cohen, S.
Domine, Laura
Fu, H.
Hoskinson, C.
Hyung, E.
Kelly, M.
Lard, E.
Laukien, F.
Lem, J.
McCallum, R.
Millsap, R.
Parendo, C.
Pataev, M. I.
Peddeti, C.
Pugh, J.
Samuha, S.
Sasselov, D. D.
Schlereth, M.
Siler, J.
Siraj, A.
Smith, P. M.
Taylor, J.
Weed, R.
Wright, A.
Wynn, J.
Earth and Planetary Astrophysics
We have conducted an extensive towed-magnetic-sled survey during the period of June 14-28, 2023, over the seafloor about 85 km north of Manus Island, Papua New Guinea, centered around the calculated path of the bolide CNEOS 2014-01-08 (IM1). We found about 850 spherules of diameter 0.1-1.3 millimeters in our samples. The samples were analyzed by micro-XRF, Electron Probe Microanalyzer and ICP Mass spectrometry. Here we report major and trace element compositions of the samples and classify spherules based on that analysis. Spherules comprising 22% of the collection, appear to all reflect planetary igneous differentiation and are all different from previously described spherules. A subset of the differentiated-spherules show an excess of Be, La and U, by up to three orders of magnitude relative to the solar system standard of CI chondrites. Detailed mass spectrometry of 12 of these "BeLaU"-type spherules, the population of which may constitute up to ~10% of our entire collected sample, suggests that they are derived from material formed by planetary igneous fractionation. Their chemical composition is unlike any known solar system material. The "BeLaU"-type spherules reflect a highly differentiated, extremely evolved composition of an unknown source.
title Chemical Classification of Spherules Recovered From The Pacific Ocean Site of The CNEOS 2014-01-08 (IM1) Bolide
topic Earth and Planetary Astrophysics
url https://arxiv.org/abs/2401.09882