| Literature DB >> 5610118 |
Abstract
X-ray diffraction patterns show that the mature denticles of three extant chiton species are composed of the mineral lepidocrocite and an apatite mineral, probably francolite, in addition to magnetite. Each of the three minerals forms a discrete microarchitectural unit of the chiton denticles. This is the first indication that lepidocrocite is precipitated by marine organisms and an apatite mineral by chitons.Entities:
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Year: 1967 PMID: 5610118 DOI: 10.1126/science.156.3780.1373
Source DB: PubMed Journal: Science ISSN: 0036-8075 Impact factor: 47.728