Taphonomic and Diagenetic Pathways to Protein Preservation, Part I: The Case of <i>Tyrannosaurus rex</i> Specimen MOR 1125

Many recent reports have demonstrated remarkable preservation of proteins in fossil bones dating back to the Permian. However, preservation mechanisms that foster the long-term stability of biomolecules and the taphonomic circumstances facilitating them remain largely unexplored. To address this, we...

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Autores principales: Paul V. Ullmann, Kyle Macauley, Richard D. Ash, Ben Shoup, John B. Scannella
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Publicado: MDPI AG 2021
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spelling oai:doaj.org-article:9c0732e5b7684c2fa98fff00845a27d92021-11-25T16:47:52ZTaphonomic and Diagenetic Pathways to Protein Preservation, Part I: The Case of <i>Tyrannosaurus rex</i> Specimen MOR 112510.3390/biology101111932079-7737https://doaj.org/article/9c0732e5b7684c2fa98fff00845a27d92021-11-01T00:00:00Zhttps://www.mdpi.com/2079-7737/10/11/1193https://doaj.org/toc/2079-7737Many recent reports have demonstrated remarkable preservation of proteins in fossil bones dating back to the Permian. However, preservation mechanisms that foster the long-term stability of biomolecules and the taphonomic circumstances facilitating them remain largely unexplored. To address this, we examined the taphonomic and geochemical history of <i>Tyrannosaurus rex</i> specimen Museum of the Rockies (MOR) 1125, whose right femur and tibiae were previously shown to retain still-soft tissues and endogenous proteins. By combining taphonomic insights with trace element compositional data, we reconstruct the postmortem history of this famous specimen. Our data show that following prolonged, subaqueous decay in an estuarine channel, MOR 1125 was buried in a coarse sandstone wherein its bones fossilized while interacting with oxic and potentially brackish early-diagenetic groundwaters. Once its bones became stable fossils, they experienced minimal further chemical alteration. Comparisons with other recent studies reveal that oxidizing early-diagenetic microenvironments and diagenetic circumstances which restrict exposure to percolating pore fluids elevate biomolecular preservation potential by promoting molecular condensation reactions and hindering chemical alteration, respectively. Avoiding protracted interactions with late-diagenetic pore fluids is also likely crucial. Similar studies must be conducted on fossil bones preserved under diverse paleoenvironmental and diagenetic contexts to fully elucidate molecular preservation pathways.Paul V. UllmannKyle MacauleyRichard D. AshBen ShoupJohn B. ScannellaMDPI AGarticleREE<i>Tyrannosaurus rex</i>molecular paleontologygeochemical taphonomydiagenesisboneBiology (General)QH301-705.5ENBiology, Vol 10, Iss 1193, p 1193 (2021)
institution DOAJ
collection DOAJ
language EN
topic REE
<i>Tyrannosaurus rex</i>
molecular paleontology
geochemical taphonomy
diagenesis
bone
Biology (General)
QH301-705.5
spellingShingle REE
<i>Tyrannosaurus rex</i>
molecular paleontology
geochemical taphonomy
diagenesis
bone
Biology (General)
QH301-705.5
Paul V. Ullmann
Kyle Macauley
Richard D. Ash
Ben Shoup
John B. Scannella
Taphonomic and Diagenetic Pathways to Protein Preservation, Part I: The Case of <i>Tyrannosaurus rex</i> Specimen MOR 1125
description Many recent reports have demonstrated remarkable preservation of proteins in fossil bones dating back to the Permian. However, preservation mechanisms that foster the long-term stability of biomolecules and the taphonomic circumstances facilitating them remain largely unexplored. To address this, we examined the taphonomic and geochemical history of <i>Tyrannosaurus rex</i> specimen Museum of the Rockies (MOR) 1125, whose right femur and tibiae were previously shown to retain still-soft tissues and endogenous proteins. By combining taphonomic insights with trace element compositional data, we reconstruct the postmortem history of this famous specimen. Our data show that following prolonged, subaqueous decay in an estuarine channel, MOR 1125 was buried in a coarse sandstone wherein its bones fossilized while interacting with oxic and potentially brackish early-diagenetic groundwaters. Once its bones became stable fossils, they experienced minimal further chemical alteration. Comparisons with other recent studies reveal that oxidizing early-diagenetic microenvironments and diagenetic circumstances which restrict exposure to percolating pore fluids elevate biomolecular preservation potential by promoting molecular condensation reactions and hindering chemical alteration, respectively. Avoiding protracted interactions with late-diagenetic pore fluids is also likely crucial. Similar studies must be conducted on fossil bones preserved under diverse paleoenvironmental and diagenetic contexts to fully elucidate molecular preservation pathways.
format article
author Paul V. Ullmann
Kyle Macauley
Richard D. Ash
Ben Shoup
John B. Scannella
author_facet Paul V. Ullmann
Kyle Macauley
Richard D. Ash
Ben Shoup
John B. Scannella
author_sort Paul V. Ullmann
title Taphonomic and Diagenetic Pathways to Protein Preservation, Part I: The Case of <i>Tyrannosaurus rex</i> Specimen MOR 1125
title_short Taphonomic and Diagenetic Pathways to Protein Preservation, Part I: The Case of <i>Tyrannosaurus rex</i> Specimen MOR 1125
title_full Taphonomic and Diagenetic Pathways to Protein Preservation, Part I: The Case of <i>Tyrannosaurus rex</i> Specimen MOR 1125
title_fullStr Taphonomic and Diagenetic Pathways to Protein Preservation, Part I: The Case of <i>Tyrannosaurus rex</i> Specimen MOR 1125
title_full_unstemmed Taphonomic and Diagenetic Pathways to Protein Preservation, Part I: The Case of <i>Tyrannosaurus rex</i> Specimen MOR 1125
title_sort taphonomic and diagenetic pathways to protein preservation, part i: the case of <i>tyrannosaurus rex</i> specimen mor 1125
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/9c0732e5b7684c2fa98fff00845a27d9
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