A universal curve of apatite crystallinity for the assessment of bone integrity and preservation.
Identifieur interne : 000893 ( Main/Exploration ); précédent : 000892; suivant : 000894A universal curve of apatite crystallinity for the assessment of bone integrity and preservation.
Auteurs : Gregorio Dal Sasso [Italie] ; Yotam Asscher [Italie] ; Ivana Angelini [Italie] ; Luca Nodari [Italie] ; Gilberto Artioli [Italie]Source :
- Scientific reports [ 2045-2322 ] ; 2018.
Descripteurs français
- KwdFr :
- MESH :
- analyse : Apatites.
- composition chimique : Apatites, Os et tissu osseux.
- méthodes : Archéologie, Spectroscopie infrarouge à transformée de Fourier.
- Animaux, Diffraction des rayons X, Fossiles, Humains.
English descriptors
- KwdEn :
- MESH :
- chemical , analysis : Apatites.
- chemical , chemistry : Apatites.
- chemistry : Bone and Bones.
- methods : Archaeology, Spectroscopy, Fourier Transform Infrared.
- Animals, Fossils, Humans, X-Ray Diffraction.
Abstract
The reliable determination of bioapatite crystallinity is of great practical interest, as a proxy to the physico-chemical and microstructural properties, and ultimately, to the integrity of bone materials. Bioapatite crystallinity is used to diagnose pathologies in modern calcified tissues as well as to assess the preservation state of fossil bones. To date, infrared spectroscopy is one of the most applied techniques for bone characterisation and the derived infrared splitting factor (IRSF) has been widely used to practically assess bioapatite crystallinity. Here we thoroughly discuss and revise the use of the IRSF parameter and its meaning as a crystallinity indicator, based on extensive measurements of fresh and fossil bones, virtually covering the known range of crystallinity degree of bioapatite. A novel way to calculate and use the infrared peak width as a suitable measurement of true apatite crystallinity is proposed, and validated by combined measurement of the same samples through X-ray diffraction. The non-linear correlation between the infrared peak width and the derived ISRF is explained. As shown, the infrared peak width at 604 cm-1 can be effectively used to assess both the average crystallite size and structural carbonate content of bioapatite, thus establishing a universal calibration curve of practical use.
DOI: 10.1038/s41598-018-30642-z
PubMed: 30104595
PubMed Central: PMC6089980
Affiliations:
Links toward previous steps (curation, corpus...)
Le document en format XML
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Gradenigo 6, 35131, Padova, Italy. gregorio.dalsasso@ic.cnr.it.</nlm:affiliation><country xml:lang="fr">Italie</country><wicri:regionArea>Dipartimento di Geoscienze, Università degli Studi di Padova, Via G. Gradenigo 6, 35131, Padova</wicri:regionArea><orgName type="university">Université de Padoue</orgName><placeName><settlement type="city">Padoue</settlement><region type="region" nuts="2">Vénétie</region></placeName></affiliation></author><author><name sortKey="Asscher, Yotam" sort="Asscher, Yotam" uniqKey="Asscher Y" first="Yotam" last="Asscher">Yotam Asscher</name><affiliation wicri:level="4"><nlm:affiliation>Dipartimento di Geoscienze, Università degli Studi di Padova, Via G. Gradenigo 6, 35131, Padova, Italy.</nlm:affiliation><country xml:lang="fr">Italie</country><wicri:regionArea>Dipartimento di Geoscienze, Università degli Studi di Padova, Via G. Gradenigo 6, 35131, Padova</wicri:regionArea><orgName type="university">Université de Padoue</orgName><placeName><settlement type="city">Padoue</settlement><region type="region" nuts="2">Vénétie</region></placeName></affiliation></author><author><name sortKey="Angelini, Ivana" sort="Angelini, Ivana" uniqKey="Angelini I" first="Ivana" last="Angelini">Ivana Angelini</name><affiliation wicri:level="4"><nlm:affiliation>Dipartimento dei Beni Culturali: archeologia, storia dell'arte, del cinema e della musica, Università degli Studi di Padova, Piazza Capitaniato 7, 35139, Padova, Italy.</nlm:affiliation><country xml:lang="fr">Italie</country><wicri:regionArea>Dipartimento dei Beni Culturali: archeologia, storia dell'arte, del cinema e della musica, Università degli Studi di Padova, Piazza Capitaniato 7, 35139, Padova</wicri:regionArea><orgName type="university">Université de Padoue</orgName><placeName><settlement type="city">Padoue</settlement><region type="region" nuts="2">Vénétie</region></placeName></affiliation></author><author><name sortKey="Nodari, Luca" sort="Nodari, Luca" uniqKey="Nodari L" first="Luca" last="Nodari">Luca Nodari</name><affiliation wicri:level="1"><nlm:affiliation>Istituto di Chimica della Materia Condensata e di Tecnologie per l'Energia - ICMATE - Consiglio Nazionale delle Ricerche, Corso Stati Uniti 4, 35127, Padova, Italy.</nlm:affiliation><country xml:lang="fr">Italie</country><wicri:regionArea>Istituto di Chimica della Materia Condensata e di Tecnologie per l'Energia - ICMATE - Consiglio Nazionale delle Ricerche, Corso Stati Uniti 4, 35127, Padova</wicri:regionArea><wicri:noRegion>Padova</wicri:noRegion></affiliation></author><author><name sortKey="Artioli, Gilberto" sort="Artioli, Gilberto" uniqKey="Artioli G" first="Gilberto" last="Artioli">Gilberto Artioli</name><affiliation wicri:level="4"><nlm:affiliation>Dipartimento di Geoscienze, Università degli Studi di Padova, Via G. Gradenigo 6, 35131, Padova, Italy.</nlm:affiliation><country xml:lang="fr">Italie</country><wicri:regionArea>Dipartimento di Geoscienze, Università degli Studi di Padova, Via G. Gradenigo 6, 35131, Padova</wicri:regionArea><orgName type="university">Université de Padoue</orgName><placeName><settlement type="city">Padoue</settlement><region type="region" nuts="2">Vénétie</region></placeName></affiliation></author></analytic><series><title level="j">Scientific reports</title><idno type="eISSN">2045-2322</idno><imprint><date when="2018" type="published">2018</date></imprint></series></biblStruct></sourceDesc></fileDesc><profileDesc><textClass><keywords scheme="KwdEn" xml:lang="en"><term>Animals (MeSH)</term><term>Apatites (analysis)</term><term>Apatites (chemistry)</term><term>Archaeology (methods)</term><term>Bone and Bones (chemistry)</term><term>Fossils (MeSH)</term><term>Humans (MeSH)</term><term>Spectroscopy, Fourier Transform Infrared (methods)</term><term>X-Ray Diffraction (MeSH)</term></keywords><keywords scheme="KwdFr" xml:lang="fr"><term>Animaux (MeSH)</term><term>Apatites (analyse)</term><term>Apatites (composition chimique)</term><term>Archéologie (méthodes)</term><term>Diffraction des rayons X (MeSH)</term><term>Fossiles (MeSH)</term><term>Humains (MeSH)</term><term>Os et tissu osseux (composition chimique)</term><term>Spectroscopie infrarouge à transformée de Fourier (méthodes)</term></keywords><keywords scheme="MESH" type="chemical" qualifier="analysis" xml:lang="en"><term>Apatites</term></keywords><keywords scheme="MESH" type="chemical" qualifier="chemistry" xml:lang="en"><term>Apatites</term></keywords><keywords scheme="MESH" qualifier="analyse" xml:lang="fr"><term>Apatites</term></keywords><keywords scheme="MESH" qualifier="chemistry" xml:lang="en"><term>Bone and Bones</term></keywords><keywords scheme="MESH" qualifier="composition chimique" xml:lang="fr"><term>Apatites</term><term>Os et tissu osseux</term></keywords><keywords scheme="MESH" qualifier="methods" xml:lang="en"><term>Archaeology</term><term>Spectroscopy, Fourier Transform Infrared</term></keywords><keywords scheme="MESH" qualifier="méthodes" xml:lang="fr"><term>Archéologie</term><term>Spectroscopie infrarouge à transformée de Fourier</term></keywords><keywords scheme="MESH" xml:lang="en"><term>Animals</term><term>Fossils</term><term>Humans</term><term>X-Ray Diffraction</term></keywords><keywords scheme="MESH" xml:lang="fr"><term>Animaux</term><term>Diffraction des rayons X</term><term>Fossiles</term><term>Humains</term></keywords></textClass></profileDesc></teiHeader><front><div type="abstract" xml:lang="en">The reliable determination of bioapatite crystallinity is of great practical interest, as a proxy to the physico-chemical and microstructural properties, and ultimately, to the integrity of bone materials. Bioapatite crystallinity is used to diagnose pathologies in modern calcified tissues as well as to assess the preservation state of fossil bones. To date, infrared spectroscopy is one of the most applied techniques for bone characterisation and the derived infrared splitting factor (IRSF) has been widely used to practically assess bioapatite crystallinity. Here we thoroughly discuss and revise the use of the IRSF parameter and its meaning as a crystallinity indicator, based on extensive measurements of fresh and fossil bones, virtually covering the known range of crystallinity degree of bioapatite. A novel way to calculate and use the infrared peak width as a suitable measurement of true apatite crystallinity is proposed, and validated by combined measurement of the same samples through X-ray diffraction. The non-linear correlation between the infrared peak width and the derived ISRF is explained. As shown, the infrared peak width at 604 cm<sup>-1</sup> can be effectively used to assess both the average crystallite size and structural carbonate content of bioapatite, thus establishing a universal calibration curve of practical use.</div></front></TEI><pubmed><MedlineCitation Status="MEDLINE" Owner="NLM"><PMID Version="1">30104595</PMID><DateCompleted><Year>2019</Year><Month>10</Month><Day>28</Day></DateCompleted><DateRevised><Year>2019</Year><Month>10</Month><Day>28</Day></DateRevised><Article PubModel="Electronic"><Journal><ISSN IssnType="Electronic">2045-2322</ISSN><JournalIssue CitedMedium="Internet"><Volume>8</Volume><Issue>1</Issue><PubDate><Year>2018</Year><Month>08</Month><Day>13</Day></PubDate></JournalIssue><Title>Scientific reports</Title><ISOAbbreviation>Sci Rep</ISOAbbreviation></Journal><ArticleTitle>A universal curve of apatite crystallinity for the assessment of bone integrity and preservation.</ArticleTitle><Pagination><MedlinePgn>12025</MedlinePgn></Pagination><ELocationID EIdType="doi" ValidYN="Y">10.1038/s41598-018-30642-z</ELocationID><Abstract><AbstractText>The reliable determination of bioapatite crystallinity is of great practical interest, as a proxy to the physico-chemical and microstructural properties, and ultimately, to the integrity of bone materials. Bioapatite crystallinity is used to diagnose pathologies in modern calcified tissues as well as to assess the preservation state of fossil bones. To date, infrared spectroscopy is one of the most applied techniques for bone characterisation and the derived infrared splitting factor (IRSF) has been widely used to practically assess bioapatite crystallinity. Here we thoroughly discuss and revise the use of the IRSF parameter and its meaning as a crystallinity indicator, based on extensive measurements of fresh and fossil bones, virtually covering the known range of crystallinity degree of bioapatite. A novel way to calculate and use the infrared peak width as a suitable measurement of true apatite crystallinity is proposed, and validated by combined measurement of the same samples through X-ray diffraction. The non-linear correlation between the infrared peak width and the derived ISRF is explained. As shown, the infrared peak width at 604 cm<sup>-1</sup> can be effectively used to assess both the average crystallite size and structural carbonate content of bioapatite, thus establishing a universal calibration curve of practical use.</AbstractText></Abstract><AuthorList CompleteYN="Y"><Author ValidYN="Y"><LastName>Dal Sasso</LastName><ForeName>Gregorio</ForeName><Initials>G</Initials><Identifier Source="ORCID">0000-0002-2176-5446</Identifier><AffiliationInfo><Affiliation>Dipartimento di Geoscienze, Università degli Studi di Padova, Via G. Gradenigo 6, 35131, Padova, Italy. gregorio.dalsasso@ic.cnr.it.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Asscher</LastName><ForeName>Yotam</ForeName><Initials>Y</Initials><AffiliationInfo><Affiliation>Dipartimento di Geoscienze, Università degli Studi di Padova, Via G. Gradenigo 6, 35131, Padova, Italy.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Angelini</LastName><ForeName>Ivana</ForeName><Initials>I</Initials><Identifier Source="ORCID">0000-0002-7970-3416</Identifier><AffiliationInfo><Affiliation>Dipartimento dei Beni Culturali: archeologia, storia dell'arte, del cinema e della musica, Università degli Studi di Padova, Piazza Capitaniato 7, 35139, Padova, Italy.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Nodari</LastName><ForeName>Luca</ForeName><Initials>L</Initials><AffiliationInfo><Affiliation>Istituto di Chimica della Materia Condensata e di Tecnologie per l'Energia - ICMATE - Consiglio Nazionale delle Ricerche, Corso Stati Uniti 4, 35127, Padova, Italy.</Affiliation></AffiliationInfo></Author><Author ValidYN="Y"><LastName>Artioli</LastName><ForeName>Gilberto</ForeName><Initials>G</Initials><Identifier Source="ORCID">0000-0002-8693-7392</Identifier><AffiliationInfo><Affiliation>Dipartimento di Geoscienze, Università degli Studi di Padova, Via G. Gradenigo 6, 35131, Padova, Italy.</Affiliation></AffiliationInfo></Author></AuthorList><Language>eng</Language><PublicationTypeList><PublicationType UI="D016428">Journal Article</PublicationType></PublicationTypeList><ArticleDate DateType="Electronic"><Year>2018</Year><Month>08</Month><Day>13</Day></ArticleDate></Article><MedlineJournalInfo><Country>England</Country><MedlineTA>Sci Rep</MedlineTA><NlmUniqueID>101563288</NlmUniqueID><ISSNLinking>2045-2322</ISSNLinking></MedlineJournalInfo><ChemicalList><Chemical><RegistryNumber>0</RegistryNumber><NameOfSubstance UI="D001031">Apatites</NameOfSubstance></Chemical></ChemicalList><CitationSubset>IM</CitationSubset><MeshHeadingList><MeshHeading><DescriptorName UI="D000818" MajorTopicYN="N">Animals</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D001031" MajorTopicYN="N">Apatites</DescriptorName><QualifierName UI="Q000032" MajorTopicYN="Y">analysis</QualifierName><QualifierName UI="Q000737" MajorTopicYN="N">chemistry</QualifierName></MeshHeading><MeshHeading><DescriptorName UI="D001106" MajorTopicYN="N">Archaeology</DescriptorName><QualifierName UI="Q000379" MajorTopicYN="Y">methods</QualifierName></MeshHeading><MeshHeading><DescriptorName UI="D001842" MajorTopicYN="N">Bone and Bones</DescriptorName><QualifierName UI="Q000737" MajorTopicYN="Y">chemistry</QualifierName></MeshHeading><MeshHeading><DescriptorName UI="D005580" MajorTopicYN="Y">Fossils</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D006801" MajorTopicYN="N">Humans</DescriptorName></MeshHeading><MeshHeading><DescriptorName UI="D017550" MajorTopicYN="N">Spectroscopy, Fourier Transform Infrared</DescriptorName><QualifierName UI="Q000379" MajorTopicYN="N">methods</QualifierName></MeshHeading><MeshHeading><DescriptorName UI="D014961" MajorTopicYN="N">X-Ray Diffraction</DescriptorName></MeshHeading></MeshHeadingList></MedlineCitation><PubmedData><History><PubMedPubDate 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uniqKey="Angelini I" first="Ivana" last="Angelini">Ivana Angelini</name><name sortKey="Artioli, Gilberto" sort="Artioli, Gilberto" uniqKey="Artioli G" first="Gilberto" last="Artioli">Gilberto Artioli</name><name sortKey="Asscher, Yotam" sort="Asscher, Yotam" uniqKey="Asscher Y" first="Yotam" last="Asscher">Yotam Asscher</name><name sortKey="Nodari, Luca" sort="Nodari, Luca" uniqKey="Nodari L" first="Luca" last="Nodari">Luca Nodari</name></country></tree></affiliations></record>Pour manipuler ce document sous Unix (Dilib)
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