Bacterial deposition of iron and manganese oxides in North American caves.

Peck, Stewart

Deposits of hydrated iron and manganese oxides are common as stalactites, wall crusts, and as thick layers in sediment in caves at Dubuque, Iowa. The metal oxide deposits are concluded to be at least partly the result of organic (bacterial) rather than inorganic precipitation reactions. -from Author

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Journal	NSS Bulletin
Organisation	Department of Biology
Citation APA Style AAA Style APA Style Cell Style Chicago Style Harvard Style IEEE Style MLA Style Nature Style Vancouver Style American-Institute-of-Physics Style Council-of-Science-Editors Style BibTex Format Endnote Format RIS Format CSL Format DOIs only Format	Peck, S. (1986). Bacterial deposition of iron and manganese oxides in North American caves. NSS Bulletin, 48(1), 26–30.

Bacterial deposition of iron and manganese oxides in North American caves.

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Bacterial deposition of iron and manganese oxides in North American caves.

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