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Magnetic spherules in coastal plain sediments, Sullivan's Island, South Carolina, USA
Author(s) -
Taylor Pamela L.,
Nusbaum Robert L.,
Fronabarger A. Kem,
Katuna Michael P.,
Summer Neil
Publication year - 1996
Publication title -
meteoritics and planetary science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.09
H-Index - 100
eISSN - 1945-5100
pISSN - 1086-9379
DOI - 10.1111/j.1945-5100.1996.tb02056.x
Subject(s) - geology , sediment , geochemistry , abyssal plain , benthic zone , coastal plain , volcano , paleontology , oceanography
— We extracted black, magnetic spherules from well cuttings of Oligocene sediments in the coastal plain of South Carolina, USA. Three possible origins were considered: industrial, volcanic, and extraterrestrial. An extraterrestrial origin by ablation of parent meteoroid material is proposed, based on the spherule morphologies, the presence of metallic Fe cores in many of the spherules, and the detection of wüstite in some of the oxide rims. Low Ni contents are problematic but may be attributed to the ablation of a low‐Ni parental body, such as hexahedrite. The presence of spherules in somewhat clay‐like, sandy sediments is unusual, as most magnetic spherules are found in abyssal muds. Based on benthic foraminiferal assemblages and sediment distribution above, within, and below the beds containing spherules, it is unlikely that the spherules were transported from a deep‐sea environment.

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