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Cited by 175

The DOI matches its Crossref record; 1 of the 1 references it cites were found in a registry or an index.

Calcite precipitation by marine bacteria∗

Morita, Richard Y.·1980·Geomicrobiology Journal

Abstract

Calcite precipitation occurs when trimethylamino‐N‐oxide and medium are added to surface waters collected above Lodestone and Keeper Reefs of the Great Barrier Reef. The calcium content of the water was initially 430 ppm. After 30 days incubation at 28 °C, the pH had risen and only 90 ppm of calcium remained in solution. The precipitate was analyzed by X‐ray diffraction and was found to be calcite. During anaerobic incubation of the pure cultures of calcite precipitating bacteria in seawater containing TMAO and medium the pH rose rapidly, the Eh fell quickly, but the precipitation of calcite followed more slowly. Calcite precipitation also occurred aerobically. The binding of 45Ca by bacteria was demonstrated. 14C‐carbonate resulting from bacterial action on 14C‐aspartate was found to be present in the precipitated calcite.

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Crossref · 10.1080/01490458009377751

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Metadata

Authors
Morita, R. Y.
Venue
Geomicrobiology Journal
Published
1980-01
Volume
2
Issue
1
Pages
63-82
ISSN
  • 0149-0451 (ISSN-L)
  • 1521-0529
OpenAlex
W2081740039
Cited by
175
References
1
FWCI
2.99
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Calcite precipitation by marine bacteria∗. https://app.cochat.ai/papers/10.1080/01490458009377751
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Morita, R. Y. (1980). Calcite precipitation by marine bacteria∗. Geomicrobiology Journal. https://doi.org/10.1080/01490458009377751

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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.