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- Anders Meibom
- Department of Geological and Environmental Sciences Stanford University Stanford California USA
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- Jean‐Pierre Cuif
- Geology UMR IDES Faculty of Science Orsay France
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- François Hillion
- Cameca Courbevoie France
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- Brent R. Constantz
- Biomechanical Engineering Division Stanford University Stanford California USA
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- Anne Juillet‐Leclerc
- Laboratoire de Sciences du climat et de l'Environnement CNRS‐CEA Gif sur Yvette France
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- Yannicke Dauphin
- Geology UMR IDES Faculty of Science Orsay France
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- Tsuyoshi Watanabe
- Laboratoire de Sciences du climat et de l'Environnement CNRS‐CEA Gif sur Yvette France
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- Robert B. Dunbar
- Department of Geological and Environmental Sciences Stanford University Stanford California USA
書誌事項
- 公開日
- 2004-12-11
- 権利情報
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- http://onlinelibrary.wiley.com/termsAndConditions#vor
- DOI
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- 10.1029/2004gl021313
- 公開者
- American Geophysical Union (AGU)
この論文をさがす
説明
<jats:p>Ion micro‐probe imaging of the aragonite skeleton of <jats:italic>Pavona clavus</jats:italic>, a massive reef‐building coral, shows that magnesium and strontium are distributed very differently. In contrast to strontium, the distribution of magnesium is strongly correlated with the fine‐scale structure of the skeleton and corresponds to the layered organization of aragonite fibers surrounding the centers of calcification, which have up to ten times higher magnesium concentration. This indicates a strong biological control over the magnesium composition of all structural components within the skeleton. Magnesium may be used by the coral to actively control the growth of the different skeletal crystal components.</jats:p>
収録刊行物
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- Geophysical Research Letters
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Geophysical Research Letters 31 (23), L23306-, 2004-12-11
American Geophysical Union (AGU)

