Amorphous layer around aragonite platelets in nacre

dc.contributor.authorNassif, Nadinedeu
dc.contributor.authorPinna, Nicoladeu
dc.contributor.authorGehrke, Nicoledeu
dc.contributor.authorAntonietti, Markusdeu
dc.contributor.authorJäger, Christiandeu
dc.contributor.authorCölfen, Helmut
dc.date.accessioned2011-11-11T10:52:41Zdeu
dc.date.available2011-11-11T10:52:41Zdeu
dc.date.issued2005-09-06
dc.description.abstractWe reveal that the aragonite CaCO3 platelets in nacre of Haliotis laevigata are covered with a continuous layer of disordered amorphous CaCO3 and that there is no protein interaction with this layer. This finding contradicts classical paradigms of biomineralization, e.g., an epitaxial match between the structural organic matrix and the formed mineral. This finding also highlights the role of physicochemical effects in morphogenesis, complementing the previously assumed total control by biomolecules and bioprocesses, with many implications in nanotechnology and materials science.eng
dc.description.versionpublished
dc.identifier.citationProceedings of the National Academy of Sciences of the United States of America ; 102 (2005), 36. - S. 12653-12655deu
dc.identifier.doi10.1073/pnas.0502577102deu
dc.identifier.pmid16129830
dc.identifier.ppn401128334deu
dc.identifier.urihttp://kops.uni-konstanz.de/handle/123456789/16647
dc.language.isoengdeu
dc.legacy.dateIssued2011-11-11deu
dc.rightsterms-of-usedeu
dc.rights.urihttps://rightsstatements.org/page/InC/1.0/deu
dc.subjectamorphous calcium carbonatedeu
dc.subjectbiomineralizationdeu
dc.subjecthigh-resolution transmission EMdeu
dc.subjectsolid-state NMRdeu
dc.subject.ddc540deu
dc.titleAmorphous layer around aragonite platelets in nacreeng
dc.typeJOURNAL_ARTICLEdeu
dspace.entity.typePublication
kops.citation.bibtex
@article{Nassif2005-09-06Amorp-16647,
  year={2005},
  doi={10.1073/pnas.0502577102},
  title={Amorphous layer around aragonite platelets in nacre},
  number={36},
  volume={102},
  issn={0027-8424},
  journal={Proceedings of the National Academy of Sciences},
  pages={12653--12655},
  author={Nassif, Nadine and Pinna, Nicola and Gehrke, Nicole and Antonietti, Markus and Jäger, Christian and Cölfen, Helmut}
}
kops.citation.iso690NASSIF, Nadine, Nicola PINNA, Nicole GEHRKE, Markus ANTONIETTI, Christian JÄGER, Helmut CÖLFEN, 2005. Amorphous layer around aragonite platelets in nacre. In: Proceedings of the National Academy of Sciences. 2005, 102(36), pp. 12653-12655. ISSN 0027-8424. Available under: doi: 10.1073/pnas.0502577102deu
kops.citation.iso690NASSIF, Nadine, Nicola PINNA, Nicole GEHRKE, Markus ANTONIETTI, Christian JÄGER, Helmut CÖLFEN, 2005. Amorphous layer around aragonite platelets in nacre. In: Proceedings of the National Academy of Sciences. 2005, 102(36), pp. 12653-12655. ISSN 0027-8424. Available under: doi: 10.1073/pnas.0502577102eng
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    <dcterms:abstract xml:lang="eng">We reveal that the aragonite CaCO3 platelets in nacre of Haliotis laevigata are covered with a continuous layer of disordered amorphous CaCO3 and that there is no protein interaction with this layer. This finding contradicts classical paradigms of biomineralization, e.g., an epitaxial match between the structural organic matrix and the formed mineral. This finding also highlights the role of physicochemical effects in morphogenesis, complementing the previously assumed total control by biomolecules and bioprocesses, with many implications in nanotechnology and materials science.</dcterms:abstract>
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kops.sourcefieldProceedings of the National Academy of Sciences. 2005, <b>102</b>(36), pp. 12653-12655. ISSN 0027-8424. Available under: doi: 10.1073/pnas.0502577102deu
kops.sourcefield.plainProceedings of the National Academy of Sciences. 2005, 102(36), pp. 12653-12655. ISSN 0027-8424. Available under: doi: 10.1073/pnas.0502577102deu
kops.sourcefield.plainProceedings of the National Academy of Sciences. 2005, 102(36), pp. 12653-12655. ISSN 0027-8424. Available under: doi: 10.1073/pnas.0502577102eng
kops.submitter.emailkaren-ann.lindner@uni-konstanz.dedeu
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source.identifier.issn0027-8424
source.periodicalTitleProceedings of the National Academy of Sciences

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