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Manganese and Biotic Debris Associations in Some Deep-Sea Sediments | J Greenslate
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8 Nov 1974 | Journal: | Science, 186 (4163), 529-531 | Abstract: | Incipient manganese concretions occur in microcavities of planktonic skeletal debris (especially diatom frustules) in some Pacific Basin deep-sea sediments. These concretions contain over 50 percent manganese and very little iron (< 1 percent). There is a continuum of growth stages in the concretions having a diameter between 0 and approximately 2 millimeters, and a genetic relationship is suggested between the very small and the centimeter sized concretions. | Source: | PubMed, pmid17790381 doi: 10.1126/science.186.4163.529 | Services: | Forum | Review | Favorites |
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