Trace elemental imaging of rare earth elements discriminates tissues at microscale in flat fossils.

The interpretation of flattened fossils remains a major challenge due to compression of their complex anatomies during fossilization, making critical anatomical features invisible or hardly discernible. Key features are often hidden under greatly preserved decay prone tissues, or an unpreparable sed...

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Autores principales: Pierre Gueriau, Cristian Mocuta, Didier B Dutheil, Serge X Cohen, Dominique Thiaudière, OT1 Consortium, Sylvain Charbonnier, Gaël Clément, Loïc Bertrand
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Publicado: Public Library of Science (PLoS) 2014
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Acceso en línea:https://doaj.org/article/98eca160914b4138a074447d28204c25
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spelling oai:doaj.org-article:98eca160914b4138a074447d28204c252021-11-18T08:35:07ZTrace elemental imaging of rare earth elements discriminates tissues at microscale in flat fossils.1932-620310.1371/journal.pone.0086946https://doaj.org/article/98eca160914b4138a074447d28204c252014-01-01T00:00:00Zhttps://www.ncbi.nlm.nih.gov/pmc/articles/pmid/24489809/?tool=EBIhttps://doaj.org/toc/1932-6203The interpretation of flattened fossils remains a major challenge due to compression of their complex anatomies during fossilization, making critical anatomical features invisible or hardly discernible. Key features are often hidden under greatly preserved decay prone tissues, or an unpreparable sedimentary matrix. A method offering access to such anatomical features is of paramount interest to resolve taxonomic affinities and to study fossils after a least possible invasive preparation. Unfortunately, the widely-used X-ray micro-computed tomography, for visualizing hidden or internal structures of a broad range of fossils, is generally inapplicable to flattened specimens, due to the very high differential absorbance in distinct directions. Here we show that synchrotron X-ray fluorescence spectral raster-scanning coupled to spectral decomposition or a much faster Kullback-Leibler divergence based statistical analysis provides microscale visualization of tissues. We imaged exceptionally well-preserved fossils from the Late Cretaceous without needing any prior delicate preparation. The contrasting elemental distributions greatly improved the discrimination of skeletal elements material from both the sedimentary matrix and fossilized soft tissues. Aside content in alkaline earth elements and phosphorus, a critical parameter for tissue discrimination is the distinct amounts of rare earth elements. Local quantification of rare earths may open new avenues for fossil description but also in paleoenvironmental and taphonomical studies.Pierre GueriauCristian MocutaDidier B DutheilSerge X CohenDominique ThiaudièreOT1 ConsortiumSylvain CharbonnierGaël ClémentLoïc BertrandPublic Library of Science (PLoS)articleMedicineRScienceQENPLoS ONE, Vol 9, Iss 1, p e86946 (2014)
institution DOAJ
collection DOAJ
language EN
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
Pierre Gueriau
Cristian Mocuta
Didier B Dutheil
Serge X Cohen
Dominique Thiaudière
OT1 Consortium
Sylvain Charbonnier
Gaël Clément
Loïc Bertrand
Trace elemental imaging of rare earth elements discriminates tissues at microscale in flat fossils.
description The interpretation of flattened fossils remains a major challenge due to compression of their complex anatomies during fossilization, making critical anatomical features invisible or hardly discernible. Key features are often hidden under greatly preserved decay prone tissues, or an unpreparable sedimentary matrix. A method offering access to such anatomical features is of paramount interest to resolve taxonomic affinities and to study fossils after a least possible invasive preparation. Unfortunately, the widely-used X-ray micro-computed tomography, for visualizing hidden or internal structures of a broad range of fossils, is generally inapplicable to flattened specimens, due to the very high differential absorbance in distinct directions. Here we show that synchrotron X-ray fluorescence spectral raster-scanning coupled to spectral decomposition or a much faster Kullback-Leibler divergence based statistical analysis provides microscale visualization of tissues. We imaged exceptionally well-preserved fossils from the Late Cretaceous without needing any prior delicate preparation. The contrasting elemental distributions greatly improved the discrimination of skeletal elements material from both the sedimentary matrix and fossilized soft tissues. Aside content in alkaline earth elements and phosphorus, a critical parameter for tissue discrimination is the distinct amounts of rare earth elements. Local quantification of rare earths may open new avenues for fossil description but also in paleoenvironmental and taphonomical studies.
format article
author Pierre Gueriau
Cristian Mocuta
Didier B Dutheil
Serge X Cohen
Dominique Thiaudière
OT1 Consortium
Sylvain Charbonnier
Gaël Clément
Loïc Bertrand
author_facet Pierre Gueriau
Cristian Mocuta
Didier B Dutheil
Serge X Cohen
Dominique Thiaudière
OT1 Consortium
Sylvain Charbonnier
Gaël Clément
Loïc Bertrand
author_sort Pierre Gueriau
title Trace elemental imaging of rare earth elements discriminates tissues at microscale in flat fossils.
title_short Trace elemental imaging of rare earth elements discriminates tissues at microscale in flat fossils.
title_full Trace elemental imaging of rare earth elements discriminates tissues at microscale in flat fossils.
title_fullStr Trace elemental imaging of rare earth elements discriminates tissues at microscale in flat fossils.
title_full_unstemmed Trace elemental imaging of rare earth elements discriminates tissues at microscale in flat fossils.
title_sort trace elemental imaging of rare earth elements discriminates tissues at microscale in flat fossils.
publisher Public Library of Science (PLoS)
publishDate 2014
url https://doaj.org/article/98eca160914b4138a074447d28204c25
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