Syngenetic rapid growth of ellipsoidal silica concretions with bitumen cores

Abstract Isolated silica concretions in calcareous sediments have unique shapes and distinct sharp boundaries and are considered to form by diagenesis of biogenic siliceous grains. However, the details and rates of syngenetic formation of these spherical concretions are still not fully clear. Here w...

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Autores principales: Hidekazu Yoshida, Ryusei Kuma, Hitoshi Hasegawa, Nagayoshi Katsuta, Sin-iti Sirono, Masayo Minami, Shoji Nishimoto, Natsuko Takagi, Seiji Kadowaki, Richard Metcalfe
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Publicado: Nature Portfolio 2021
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Acceso en línea:https://doaj.org/article/127fcb93f04b49e38d737ceffc70cbf0
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spelling oai:doaj.org-article:127fcb93f04b49e38d737ceffc70cbf02021-12-02T12:11:28ZSyngenetic rapid growth of ellipsoidal silica concretions with bitumen cores10.1038/s41598-021-83651-w2045-2322https://doaj.org/article/127fcb93f04b49e38d737ceffc70cbf02021-02-01T00:00:00Zhttps://doi.org/10.1038/s41598-021-83651-whttps://doaj.org/toc/2045-2322Abstract Isolated silica concretions in calcareous sediments have unique shapes and distinct sharp boundaries and are considered to form by diagenesis of biogenic siliceous grains. However, the details and rates of syngenetic formation of these spherical concretions are still not fully clear. Here we present a model for concretion growth by diffusion, with chemical buffering involving decomposition of organic matter leading to a pH change in the pore-water and preservation of residual bitumen cores in the concretions. The model is compatible with some pervasive silica precipitation. Based on the observed elemental distributions, C, N, S, bulk carbon isotope and carbon preference index (CPI) measurements of the silica-enriched concretions, bitumen cores and surrounding calcareous rocks, the rate of diffusive concretion growth during early diagenesis is shown using a diffusion-growth diagram. This approach reveals that ellipsoidal SiO2 concretions with a diameter of a few cm formed rapidly and the precipitated silica preserved the bitumen cores. Our work provides a generalized chemical buffering model involving organic matter that can explain the rapid syngenetic growth of other types of silica accumulation in calcareous sediments.Hidekazu YoshidaRyusei KumaHitoshi HasegawaNagayoshi KatsutaSin-iti SironoMasayo MinamiShoji NishimotoNatsuko TakagiSeiji KadowakiRichard MetcalfeNature PortfolioarticleMedicineRScienceQENScientific Reports, Vol 11, Iss 1, Pp 1-11 (2021)
institution DOAJ
collection DOAJ
language EN
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
Hidekazu Yoshida
Ryusei Kuma
Hitoshi Hasegawa
Nagayoshi Katsuta
Sin-iti Sirono
Masayo Minami
Shoji Nishimoto
Natsuko Takagi
Seiji Kadowaki
Richard Metcalfe
Syngenetic rapid growth of ellipsoidal silica concretions with bitumen cores
description Abstract Isolated silica concretions in calcareous sediments have unique shapes and distinct sharp boundaries and are considered to form by diagenesis of biogenic siliceous grains. However, the details and rates of syngenetic formation of these spherical concretions are still not fully clear. Here we present a model for concretion growth by diffusion, with chemical buffering involving decomposition of organic matter leading to a pH change in the pore-water and preservation of residual bitumen cores in the concretions. The model is compatible with some pervasive silica precipitation. Based on the observed elemental distributions, C, N, S, bulk carbon isotope and carbon preference index (CPI) measurements of the silica-enriched concretions, bitumen cores and surrounding calcareous rocks, the rate of diffusive concretion growth during early diagenesis is shown using a diffusion-growth diagram. This approach reveals that ellipsoidal SiO2 concretions with a diameter of a few cm formed rapidly and the precipitated silica preserved the bitumen cores. Our work provides a generalized chemical buffering model involving organic matter that can explain the rapid syngenetic growth of other types of silica accumulation in calcareous sediments.
format article
author Hidekazu Yoshida
Ryusei Kuma
Hitoshi Hasegawa
Nagayoshi Katsuta
Sin-iti Sirono
Masayo Minami
Shoji Nishimoto
Natsuko Takagi
Seiji Kadowaki
Richard Metcalfe
author_facet Hidekazu Yoshida
Ryusei Kuma
Hitoshi Hasegawa
Nagayoshi Katsuta
Sin-iti Sirono
Masayo Minami
Shoji Nishimoto
Natsuko Takagi
Seiji Kadowaki
Richard Metcalfe
author_sort Hidekazu Yoshida
title Syngenetic rapid growth of ellipsoidal silica concretions with bitumen cores
title_short Syngenetic rapid growth of ellipsoidal silica concretions with bitumen cores
title_full Syngenetic rapid growth of ellipsoidal silica concretions with bitumen cores
title_fullStr Syngenetic rapid growth of ellipsoidal silica concretions with bitumen cores
title_full_unstemmed Syngenetic rapid growth of ellipsoidal silica concretions with bitumen cores
title_sort syngenetic rapid growth of ellipsoidal silica concretions with bitumen cores
publisher Nature Portfolio
publishDate 2021
url https://doaj.org/article/127fcb93f04b49e38d737ceffc70cbf0
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