Microspectroscopic evidence of cretaceous bone proteins.

Low concentrations of the structural protein collagen have recently been reported in dinosaur fossils based primarily on mass spectrometric analyses of whole bone extracts. However, direct spectroscopic characterization of isolated fibrous bone tissues, a crucial test of hypotheses of biomolecular p...

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Main Authors: Johan Lindgren, Per Uvdal, Anders Engdahl, Andrew H Lee, Carl Alwmark, Karl-Erik Bergquist, Einar Nilsson, Peter Ekström, Magnus Rasmussen, Desirée A Douglas, Michael J Polcyn, Louis L Jacobs
Format: Article
Language:English
Published: Public Library of Science (PLoS) 2011-04-01
Series:PLoS ONE
Online Access:https://www.ncbi.nlm.nih.gov/pmc/articles/pmid/21559386/pdf/?tool=EBI
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spelling doaj-601a19b4678547648efeaf764ebf6f442021-03-04T01:55:50ZengPublic Library of Science (PLoS)PLoS ONE1932-62032011-04-0164e1944510.1371/journal.pone.0019445Microspectroscopic evidence of cretaceous bone proteins.Johan LindgrenPer UvdalAnders EngdahlAndrew H LeeCarl AlwmarkKarl-Erik BergquistEinar NilssonPeter EkströmMagnus RasmussenDesirée A DouglasMichael J PolcynLouis L JacobsLow concentrations of the structural protein collagen have recently been reported in dinosaur fossils based primarily on mass spectrometric analyses of whole bone extracts. However, direct spectroscopic characterization of isolated fibrous bone tissues, a crucial test of hypotheses of biomolecular preservation over deep time, has not been performed. Here, we demonstrate that endogenous proteinaceous molecules are retained in a humerus from a Late Cretaceous mosasaur (an extinct giant marine lizard). In situ immunofluorescence of demineralized bone extracts shows reactivity to antibodies raised against type I collagen, and amino acid analyses of soluble proteins extracted from the bone exhibit a composition indicative of structural proteins or their breakdown products. These data are corroborated by synchrotron radiation-based infrared microspectroscopic studies demonstrating that amino acid containing matter is located in bone matrix fibrils that express imprints of the characteristic 67 nm D-periodicity typical of collagen. Moreover, the fibrils differ significantly in spectral signature from those of potential modern bacterial contaminants, such as biofilms and collagen-like proteins. Thus, the preservation of primary soft tissues and biomolecules is not limited to large-sized bones buried in fluvial sandstone environments, but also occurs in relatively small-sized skeletal elements deposited in marine sediments.https://www.ncbi.nlm.nih.gov/pmc/articles/pmid/21559386/pdf/?tool=EBI
collection DOAJ
language English
format Article
sources DOAJ
author Johan Lindgren
Per Uvdal
Anders Engdahl
Andrew H Lee
Carl Alwmark
Karl-Erik Bergquist
Einar Nilsson
Peter Ekström
Magnus Rasmussen
Desirée A Douglas
Michael J Polcyn
Louis L Jacobs
spellingShingle Johan Lindgren
Per Uvdal
Anders Engdahl
Andrew H Lee
Carl Alwmark
Karl-Erik Bergquist
Einar Nilsson
Peter Ekström
Magnus Rasmussen
Desirée A Douglas
Michael J Polcyn
Louis L Jacobs
Microspectroscopic evidence of cretaceous bone proteins.
PLoS ONE
author_facet Johan Lindgren
Per Uvdal
Anders Engdahl
Andrew H Lee
Carl Alwmark
Karl-Erik Bergquist
Einar Nilsson
Peter Ekström
Magnus Rasmussen
Desirée A Douglas
Michael J Polcyn
Louis L Jacobs
author_sort Johan Lindgren
title Microspectroscopic evidence of cretaceous bone proteins.
title_short Microspectroscopic evidence of cretaceous bone proteins.
title_full Microspectroscopic evidence of cretaceous bone proteins.
title_fullStr Microspectroscopic evidence of cretaceous bone proteins.
title_full_unstemmed Microspectroscopic evidence of cretaceous bone proteins.
title_sort microspectroscopic evidence of cretaceous bone proteins.
publisher Public Library of Science (PLoS)
series PLoS ONE
issn 1932-6203
publishDate 2011-04-01
description Low concentrations of the structural protein collagen have recently been reported in dinosaur fossils based primarily on mass spectrometric analyses of whole bone extracts. However, direct spectroscopic characterization of isolated fibrous bone tissues, a crucial test of hypotheses of biomolecular preservation over deep time, has not been performed. Here, we demonstrate that endogenous proteinaceous molecules are retained in a humerus from a Late Cretaceous mosasaur (an extinct giant marine lizard). In situ immunofluorescence of demineralized bone extracts shows reactivity to antibodies raised against type I collagen, and amino acid analyses of soluble proteins extracted from the bone exhibit a composition indicative of structural proteins or their breakdown products. These data are corroborated by synchrotron radiation-based infrared microspectroscopic studies demonstrating that amino acid containing matter is located in bone matrix fibrils that express imprints of the characteristic 67 nm D-periodicity typical of collagen. Moreover, the fibrils differ significantly in spectral signature from those of potential modern bacterial contaminants, such as biofilms and collagen-like proteins. Thus, the preservation of primary soft tissues and biomolecules is not limited to large-sized bones buried in fluvial sandstone environments, but also occurs in relatively small-sized skeletal elements deposited in marine sediments.
url https://www.ncbi.nlm.nih.gov/pmc/articles/pmid/21559386/pdf/?tool=EBI
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