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
.jpg)
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/60231
Ver los metadatos del registro completo
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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 |
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2016-03 |
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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 |
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http://hdl.handle.net/11336/60231 |
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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 |
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eng |
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Nature Publishing Group |
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