Element substitution by living organisms: The case of manganese in mollusc shell aragonite

Autores
Soldati, Analía Leticia; Jacob, Dorrit E.; Glatzel, Pieter; Swarbrick, Janine C.; Geck, Jochen
Año de publicación
2016
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Determining the manganese concentration in shells of freshwater bivalves provides a unique way to obtain information about climate and environmental changes during time-intervals that pre-date instrumental data records. This approach, however, relies on a thorough understanding of how manganese is incorporated into the shell material-a point that remained controversial so far. Here we clarify this issue, using state-of-the-art X-ray absorption and X-ray emission spectroscopy in combination with band structure calculations. We verify that in the shells of all studied species manganese is incorporated as high-spin Mn 2+, i.e. manganese always has the same valence as calcium. More importantly, the unique chemical sensitivity of valence-to-core X-ray emission enables us to show that manganese is always coordinated by a CO 3-octahedron. This, firstly, provides firm experimental evidence for manganese being primarily located in the inorganic carbonate. Secondly, it indicates that the structure of the aragonitic host is locally altered such that manganese attains an octahedral, calcitic coordination. This modification at the atomic level enables the bivalve to accommodate many orders of magnitude more manganese in its aragonitic shell than found in any non-biogenic aragonite. This outstanding feature is most likely facilitated through the non-classical crystallization pathway of bivalve shells.
Fil: Soldati, Analía Leticia. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Johannes Gutenberg-Universität; Alemania. Comisión Nacional de Energía Atómica. Centro Atómico Bariloche; Argentina
Fil: Jacob, Dorrit E.. Macquarie University; Australia
Fil: Glatzel, Pieter. European Synchrotron Radiation Facility; Francia
Fil: Swarbrick, Janine C.. European Synchrotron Radiation Facility; Francia
Fil: Geck, Jochen. Paris Lodron University Salzburg; Austria
Materia
PALEOCLIMATE
TRACE ELEMENTS
XANES
MICROSCOPY
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/60231

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spelling Element substitution by living organisms: The case of manganese in mollusc shell aragoniteSoldati, Analía LeticiaJacob, Dorrit E.Glatzel, PieterSwarbrick, Janine C.Geck, JochenPALEOCLIMATETRACE ELEMENTSXANESMICROSCOPYhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Determining the manganese concentration in shells of freshwater bivalves provides a unique way to obtain information about climate and environmental changes during time-intervals that pre-date instrumental data records. This approach, however, relies on a thorough understanding of how manganese is incorporated into the shell material-a point that remained controversial so far. Here we clarify this issue, using state-of-the-art X-ray absorption and X-ray emission spectroscopy in combination with band structure calculations. We verify that in the shells of all studied species manganese is incorporated as high-spin Mn 2+, i.e. manganese always has the same valence as calcium. More importantly, the unique chemical sensitivity of valence-to-core X-ray emission enables us to show that manganese is always coordinated by a CO 3-octahedron. This, firstly, provides firm experimental evidence for manganese being primarily located in the inorganic carbonate. Secondly, it indicates that the structure of the aragonitic host is locally altered such that manganese attains an octahedral, calcitic coordination. This modification at the atomic level enables the bivalve to accommodate many orders of magnitude more manganese in its aragonitic shell than found in any non-biogenic aragonite. This outstanding feature is most likely facilitated through the non-classical crystallization pathway of bivalve shells.Fil: Soldati, Analía Leticia. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Johannes Gutenberg-Universität; Alemania. Comisión Nacional de Energía Atómica. Centro Atómico Bariloche; ArgentinaFil: Jacob, Dorrit E.. Macquarie University; AustraliaFil: Glatzel, Pieter. European Synchrotron Radiation Facility; FranciaFil: Swarbrick, Janine C.. European Synchrotron Radiation Facility; FranciaFil: Geck, Jochen. Paris Lodron University Salzburg; AustriaNature Publishing Group2016-03info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/60231Soldati, Analía Leticia; Jacob, Dorrit E.; Glatzel, Pieter; Swarbrick, Janine C.; Geck, Jochen; Element substitution by living organisms: The case of manganese in mollusc shell aragonite; Nature Publishing Group; Scientific Reports; 6; 3-2016; 22514-225242045-2322CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1038/srep22514info:eu-repo/semantics/altIdentifier/url/https://www.nature.com/articles/srep22514info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-12-23T13:26:05Zoai:ri.conicet.gov.ar:11336/60231instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-12-23 13:26:05.804CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Element substitution by living organisms: The case of manganese in mollusc shell aragonite
title Element substitution by living organisms: The case of manganese in mollusc shell aragonite
spellingShingle Element substitution by living organisms: The case of manganese in mollusc shell aragonite
Soldati, Analía Leticia
PALEOCLIMATE
TRACE ELEMENTS
XANES
MICROSCOPY
title_short Element substitution by living organisms: The case of manganese in mollusc shell aragonite
title_full Element substitution by living organisms: The case of manganese in mollusc shell aragonite
title_fullStr Element substitution by living organisms: The case of manganese in mollusc shell aragonite
title_full_unstemmed Element substitution by living organisms: The case of manganese in mollusc shell aragonite
title_sort Element substitution by living organisms: The case of manganese in mollusc shell aragonite
dc.creator.none.fl_str_mv Soldati, Analía Leticia
Jacob, Dorrit E.
Glatzel, Pieter
Swarbrick, Janine C.
Geck, Jochen
author Soldati, Analía Leticia
author_facet Soldati, Analía Leticia
Jacob, Dorrit E.
Glatzel, Pieter
Swarbrick, Janine C.
Geck, Jochen
author_role author
author2 Jacob, Dorrit E.
Glatzel, Pieter
Swarbrick, Janine C.
Geck, Jochen
author2_role author
author
author
author
dc.subject.none.fl_str_mv PALEOCLIMATE
TRACE ELEMENTS
XANES
MICROSCOPY
topic PALEOCLIMATE
TRACE ELEMENTS
XANES
MICROSCOPY
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Determining the manganese concentration in shells of freshwater bivalves provides a unique way to obtain information about climate and environmental changes during time-intervals that pre-date instrumental data records. This approach, however, relies on a thorough understanding of how manganese is incorporated into the shell material-a point that remained controversial so far. Here we clarify this issue, using state-of-the-art X-ray absorption and X-ray emission spectroscopy in combination with band structure calculations. We verify that in the shells of all studied species manganese is incorporated as high-spin Mn 2+, i.e. manganese always has the same valence as calcium. More importantly, the unique chemical sensitivity of valence-to-core X-ray emission enables us to show that manganese is always coordinated by a CO 3-octahedron. This, firstly, provides firm experimental evidence for manganese being primarily located in the inorganic carbonate. Secondly, it indicates that the structure of the aragonitic host is locally altered such that manganese attains an octahedral, calcitic coordination. This modification at the atomic level enables the bivalve to accommodate many orders of magnitude more manganese in its aragonitic shell than found in any non-biogenic aragonite. This outstanding feature is most likely facilitated through the non-classical crystallization pathway of bivalve shells.
Fil: Soldati, Analía Leticia. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Johannes Gutenberg-Universität; Alemania. Comisión Nacional de Energía Atómica. Centro Atómico Bariloche; Argentina
Fil: Jacob, Dorrit E.. Macquarie University; Australia
Fil: Glatzel, Pieter. European Synchrotron Radiation Facility; Francia
Fil: Swarbrick, Janine C.. European Synchrotron Radiation Facility; Francia
Fil: Geck, Jochen. Paris Lodron University Salzburg; Austria
description Determining the manganese concentration in shells of freshwater bivalves provides a unique way to obtain information about climate and environmental changes during time-intervals that pre-date instrumental data records. This approach, however, relies on a thorough understanding of how manganese is incorporated into the shell material-a point that remained controversial so far. Here we clarify this issue, using state-of-the-art X-ray absorption and X-ray emission spectroscopy in combination with band structure calculations. We verify that in the shells of all studied species manganese is incorporated as high-spin Mn 2+, i.e. manganese always has the same valence as calcium. More importantly, the unique chemical sensitivity of valence-to-core X-ray emission enables us to show that manganese is always coordinated by a CO 3-octahedron. This, firstly, provides firm experimental evidence for manganese being primarily located in the inorganic carbonate. Secondly, it indicates that the structure of the aragonitic host is locally altered such that manganese attains an octahedral, calcitic coordination. This modification at the atomic level enables the bivalve to accommodate many orders of magnitude more manganese in its aragonitic shell than found in any non-biogenic aragonite. This outstanding feature is most likely facilitated through the non-classical crystallization pathway of bivalve shells.
publishDate 2016
dc.date.none.fl_str_mv 2016-03
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/60231
Soldati, Analía Leticia; Jacob, Dorrit E.; Glatzel, Pieter; Swarbrick, Janine C.; Geck, Jochen; Element substitution by living organisms: The case of manganese in mollusc shell aragonite; Nature Publishing Group; Scientific Reports; 6; 3-2016; 22514-22524
2045-2322
CONICET Digital
CONICET
url http://hdl.handle.net/11336/60231
identifier_str_mv Soldati, Analía Leticia; Jacob, Dorrit E.; Glatzel, Pieter; Swarbrick, Janine C.; Geck, Jochen; Element substitution by living organisms: The case of manganese in mollusc shell aragonite; Nature Publishing Group; Scientific Reports; 6; 3-2016; 22514-22524
2045-2322
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.1038/srep22514
info:eu-repo/semantics/altIdentifier/url/https://www.nature.com/articles/srep22514
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv Nature Publishing Group
publisher.none.fl_str_mv Nature Publishing Group
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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