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Aspects of the Biogeochemistry of Magnesium 1. Calcareous Marine Organisms

Chave, Keith E.·1954·The Journal of Geology

Abstract

A study was made of the factors controlling the distribution of magnesium in the calcareous skeletons of marine organisms. The mineralogy of the carbonate appears to be the most important influence, with large amounts of magnesium occurring in solid solution in the calcitic forms and generally lesser amounts in the aragonitic forms. The complexity of the organisms and the temperature of the water in which they lived are also controlling factors in the amount of magnesium present. A large part of the study, both mineralogical and chemical, was made with X-ray diffraction techniques.

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Metadata

Authors
Chave, K. E.
Venue
The Journal of Geology
Published
1954-05
Volume
62
Issue
3
Pages
266-283
ISSN
  • 0022-1376 (ISSN-L)
  • 1537-5269
OpenAlex
W2053129771
Cited by
629
References
0
FWCI
5.15
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Aspects of the Biogeochemistry of Magnesium 1. Calcareous Marine Organisms. https://app.cochat.ai/papers/10.1086/626162
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Chave, K. E. (1954). Aspects of the Biogeochemistry of Magnesium 1. Calcareous Marine Organisms. The Journal of Geology. https://doi.org/10.1086/626162

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.