Origin of pyrite nodules at the top of the nantuo diamictites, Southern China

Abstract Pyrite nodules up to 20 cm in diameter are found at the top of the Marinoan (~ 635 Ma) Nantuo glacial diamictite as well as in the cap dolostones and shale/siltstones in the lower Doushantuo Formation in eastern Guizhou, southern China. Field occurrences, petrography, and stable sulfur isot...

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Autores principales: Changjie Liu, Ying Lin
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Publicado: Nature Portfolio 2021
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Acceso en línea:https://doaj.org/article/84ff846f1aae491a90a121541ac18f6a
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spelling oai:doaj.org-article:84ff846f1aae491a90a121541ac18f6a2021-12-02T15:14:48ZOrigin of pyrite nodules at the top of the nantuo diamictites, Southern China10.1038/s41598-021-97022-y2045-2322https://doaj.org/article/84ff846f1aae491a90a121541ac18f6a2021-09-01T00:00:00Zhttps://doi.org/10.1038/s41598-021-97022-yhttps://doaj.org/toc/2045-2322Abstract Pyrite nodules up to 20 cm in diameter are found at the top of the Marinoan (~ 635 Ma) Nantuo glacial diamictite as well as in the cap dolostones and shale/siltstones in the lower Doushantuo Formation in eastern Guizhou, southern China. Field occurrences, petrography, and stable sulfur isotopic compositions of pyrite nodules were studied from a section at Taoying, eastern Guizhou, China. Pyrite δ34S values from different nodules varied from 7.3 to 60.5‰ at different stratigraphic levels. No stratigraphic trend existed for the δ34S, supporting the scenario of pyrite formation in sediments before the precipitation of the cap dolostone. Pyrite δ34S values were also homogeneous within individual nodules at a 0.3 to 1 cm sampling scale, but were more heterogeneous at a 2 mm sampling scale. Homogeneity was not expected from the particular model for pyrite nodule formation in a largely closed or semi-closed environment. Thus, differential cementation and compaction of the pyrite-bearing sediments may have produced the nodular shape of the pyrite deposit.Changjie LiuYing LinNature PortfolioarticleMedicineRScienceQENScientific Reports, Vol 11, Iss 1, Pp 1-9 (2021)
institution DOAJ
collection DOAJ
language EN
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
Changjie Liu
Ying Lin
Origin of pyrite nodules at the top of the nantuo diamictites, Southern China
description Abstract Pyrite nodules up to 20 cm in diameter are found at the top of the Marinoan (~ 635 Ma) Nantuo glacial diamictite as well as in the cap dolostones and shale/siltstones in the lower Doushantuo Formation in eastern Guizhou, southern China. Field occurrences, petrography, and stable sulfur isotopic compositions of pyrite nodules were studied from a section at Taoying, eastern Guizhou, China. Pyrite δ34S values from different nodules varied from 7.3 to 60.5‰ at different stratigraphic levels. No stratigraphic trend existed for the δ34S, supporting the scenario of pyrite formation in sediments before the precipitation of the cap dolostone. Pyrite δ34S values were also homogeneous within individual nodules at a 0.3 to 1 cm sampling scale, but were more heterogeneous at a 2 mm sampling scale. Homogeneity was not expected from the particular model for pyrite nodule formation in a largely closed or semi-closed environment. Thus, differential cementation and compaction of the pyrite-bearing sediments may have produced the nodular shape of the pyrite deposit.
format article
author Changjie Liu
Ying Lin
author_facet Changjie Liu
Ying Lin
author_sort Changjie Liu
title Origin of pyrite nodules at the top of the nantuo diamictites, Southern China
title_short Origin of pyrite nodules at the top of the nantuo diamictites, Southern China
title_full Origin of pyrite nodules at the top of the nantuo diamictites, Southern China
title_fullStr Origin of pyrite nodules at the top of the nantuo diamictites, Southern China
title_full_unstemmed Origin of pyrite nodules at the top of the nantuo diamictites, Southern China
title_sort origin of pyrite nodules at the top of the nantuo diamictites, southern china
publisher Nature Portfolio
publishDate 2021
url https://doaj.org/article/84ff846f1aae491a90a121541ac18f6a
work_keys_str_mv AT changjieliu originofpyritenodulesatthetopofthenantuodiamictitessouthernchina
AT yinglin originofpyritenodulesatthetopofthenantuodiamictitessouthernchina
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