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Geochemical Aspect of Chemolithoautotrophic Bacterial Activity in the Role of Black Shale Hosted Mn Mineralization, Jurassic Age, Hungary, Europe
https://doi.org/10.24517/00010388
https://doi.org/10.24517/00010388b3a76a1e-d28d-4815-b832-6fec18955ea3
| 名前 / ファイル | ライセンス | アクション |
|---|---|---|
SC-PR-TAZAKI-K-233.pdf (20.2 MB)
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| Item type | 学術雑誌論文 / Journal Article(1) | |||||||
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| 公開日 | 2022-12-05 | |||||||
| タイトル | ||||||||
| タイトル | Geochemical Aspect of Chemolithoautotrophic Bacterial Activity in the Role of Black Shale Hosted Mn Mineralization, Jurassic Age, Hungary, Europe | |||||||
| 言語 | en | |||||||
| 言語 | ||||||||
| 言語 | eng | |||||||
| 資源タイプ | ||||||||
| 資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||||
| 資源タイプ | journal article | |||||||
| ID登録 | ||||||||
| ID登録 | 10.24517/00010388 | |||||||
| ID登録タイプ | JaLC | |||||||
| 著者 |
POLGARI, MARTA
× POLGARI, MARTA× Tazaki, Kazue× Watanabe, Hiroaki× VIGH, TAMAS× Gucsik, Arnold |
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| 著者別表示 |
田崎, 和江
× 田崎, 和江
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| 書誌情報 |
Clay Science 巻 12, 号 Supplement2, p. 233-239, 発行日 2006-01-01 |
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| ISSN | ||||||||
| 収録物識別子タイプ | ISSN | |||||||
| 収録物識別子 | 0009-8574 | |||||||
| NCID | ||||||||
| 収録物識別子タイプ | NCID | |||||||
| 収録物識別子 | AA00607148 | |||||||
| 出版者 | ||||||||
| 出版者 | 日本粘土学会 = The Clay Science Society of Japan | |||||||
| 内容記述 | ||||||||
| 内容記述タイプ | Other | |||||||
| 内容記述 | The black shale-hosted ÚRKÚT Mn-mineralization is among the 10 largest deposits in the World. In this study optical and electron microscopy demonstrated the biological formation of Mn-Fe minerals in Mn-carbonate ores. The ED-XRF elemental content maps and SEM-EDX observation of the ores showed distribution of Mn, Fe, and Si banded layer structure whereas the Mg, Al, and K are randomly distributed, as well as to explain the role of microorganisms associated with Ca and P. In both samples abundant microorganisms were found in the dark brown and white layers. Optical micrographs of thin sections clearly showed various shapes of cellular materials, such as spherule, oval, and filamentous morphologies. SEM-EDX observation revealed Fe-rich and P-Ca components around microorganisms showing spherule, tubular, and filamentous cells. The present investigation strongly suggests that the Mn-Fe and Si minerals were associated with microorganisms as a biological organic product. The identity of the bacteria responsible for Mn mineral formation is unknown, but is tentatively assigned to Mn and Fe bacteria on the basis of morphology. The genesis of rocks and minerals have played a pivotal role in Toarcian age, and they may even have acted as life genetic system. | |||||||
| 権利 | ||||||||
| 権利情報 | Copyright © 2011 The Clay Science Society of Japan 日本粘土学会 | |||||||
| 著者版フラグ | ||||||||
| 出版タイプ | VoR | |||||||
| 出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||||
| 関連URI | ||||||||
| 関連タイプ | isIdenticalTo | |||||||
| 識別子タイプ | URI | |||||||
| 関連識別子 | https://www.jstage.jst.go.jp/browse/jcssjclayscience | |||||||
| 関連URI | ||||||||
| 関連タイプ | isIdenticalTo | |||||||
| 識別子タイプ | URI | |||||||
| 関連識別子 | http://www.cssj2.org/ | |||||||
| 関連URI | ||||||||
| 関連タイプ | isIdenticalTo | |||||||
| 識別子タイプ | DOI | |||||||
| 関連識別子 | https://doi.org/10.11362/jcssjclayscience1960.12.Supplement2_233 | |||||||
