Three-dimensional reconstruction, taphonomic and petrological data suggest the oldest record of bioturbation is a body fossil coquina ...

Fossil material assigned to Nenoxites from the late Ediacaran Khatyspyt Formation of Arctic Siberia (550–544 Ma) has been presented as evidence for bioturbation prior to the basal Cambrian boundary. However, that ichnological interpretation has been challenged, and descriptions of similar material f...

Full description

Bibliographic Details
Main Authors: Psarras, Christos, Donoghue, Philip, Garwood, Russell, Grazhdankin, Dmitriy V, Parry, Luke A, Rogov, Vladimir I, Liu, Alexander
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
Subjects:
Online Access:https://dx.doi.org/10.17863/cam.100076
https://www.repository.cam.ac.uk/handle/1810/354167
id ftdatacite:10.17863/cam.100076
record_format openpolar
spelling ftdatacite:10.17863/cam.100076 2024-02-04T09:58:08+01:00 Three-dimensional reconstruction, taphonomic and petrological data suggest the oldest record of bioturbation is a body fossil coquina ... Psarras, Christos Donoghue, Philip Garwood, Russell Grazhdankin, Dmitriy V Parry, Luke A Rogov, Vladimir I Liu, Alexander 2023 https://dx.doi.org/10.17863/cam.100076 https://www.repository.cam.ac.uk/handle/1810/354167 en eng Wiley open.access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 http://purl.org/coar/access_right/c_abf2 Ediacaran, sedimentology, taphonomy, Nenoxites, bioturbation, petrology Article ScholarlyArticle JournalArticle article-journal 2023 ftdatacite https://doi.org/10.17863/cam.100076 2024-01-05T14:28:33Z Fossil material assigned to Nenoxites from the late Ediacaran Khatyspyt Formation of Arctic Siberia (550–544 Ma) has been presented as evidence for bioturbation prior to the basal Cambrian boundary. However, that ichnological interpretation has been challenged, and descriptions of similar material from other global localities support a body fossil origin. Here we combine X-ray computed tomography (μCT), scanning electron microscopy (SEM), and petrographic methods to evaluate the body- or tracefossil nature of Nenoxites from the Khatyspyt Formation. The fossilised structures comprise densely-packed chains of three-dimensionally preserved silicic, bowl-shaped elements surrounded by distinct sedimentary halos, within a dolomitized matrix. Individual bowl-shaped elements can exhibit diffuse mineralogical boundaries and bridging connections between elements, both considered here to result from silicification and dolomitization during diagenesis. This new morphological and petrological evidence, in conjunction ... Article in Journal/Newspaper Arctic Siberia DataCite Metadata Store (German National Library of Science and Technology) Arctic
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Ediacaran, sedimentology, taphonomy, Nenoxites, bioturbation, petrology
spellingShingle Ediacaran, sedimentology, taphonomy, Nenoxites, bioturbation, petrology
Psarras, Christos
Donoghue, Philip
Garwood, Russell
Grazhdankin, Dmitriy V
Parry, Luke A
Rogov, Vladimir I
Liu, Alexander
Three-dimensional reconstruction, taphonomic and petrological data suggest the oldest record of bioturbation is a body fossil coquina ...
topic_facet Ediacaran, sedimentology, taphonomy, Nenoxites, bioturbation, petrology
description Fossil material assigned to Nenoxites from the late Ediacaran Khatyspyt Formation of Arctic Siberia (550–544 Ma) has been presented as evidence for bioturbation prior to the basal Cambrian boundary. However, that ichnological interpretation has been challenged, and descriptions of similar material from other global localities support a body fossil origin. Here we combine X-ray computed tomography (μCT), scanning electron microscopy (SEM), and petrographic methods to evaluate the body- or tracefossil nature of Nenoxites from the Khatyspyt Formation. The fossilised structures comprise densely-packed chains of three-dimensionally preserved silicic, bowl-shaped elements surrounded by distinct sedimentary halos, within a dolomitized matrix. Individual bowl-shaped elements can exhibit diffuse mineralogical boundaries and bridging connections between elements, both considered here to result from silicification and dolomitization during diagenesis. This new morphological and petrological evidence, in conjunction ...
format Article in Journal/Newspaper
author Psarras, Christos
Donoghue, Philip
Garwood, Russell
Grazhdankin, Dmitriy V
Parry, Luke A
Rogov, Vladimir I
Liu, Alexander
author_facet Psarras, Christos
Donoghue, Philip
Garwood, Russell
Grazhdankin, Dmitriy V
Parry, Luke A
Rogov, Vladimir I
Liu, Alexander
author_sort Psarras, Christos
title Three-dimensional reconstruction, taphonomic and petrological data suggest the oldest record of bioturbation is a body fossil coquina ...
title_short Three-dimensional reconstruction, taphonomic and petrological data suggest the oldest record of bioturbation is a body fossil coquina ...
title_full Three-dimensional reconstruction, taphonomic and petrological data suggest the oldest record of bioturbation is a body fossil coquina ...
title_fullStr Three-dimensional reconstruction, taphonomic and petrological data suggest the oldest record of bioturbation is a body fossil coquina ...
title_full_unstemmed Three-dimensional reconstruction, taphonomic and petrological data suggest the oldest record of bioturbation is a body fossil coquina ...
title_sort three-dimensional reconstruction, taphonomic and petrological data suggest the oldest record of bioturbation is a body fossil coquina ...
publisher Wiley
publishDate 2023
url https://dx.doi.org/10.17863/cam.100076
https://www.repository.cam.ac.uk/handle/1810/354167
geographic Arctic
geographic_facet Arctic
genre Arctic
Siberia
genre_facet Arctic
Siberia
op_rights open.access
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
http://purl.org/coar/access_right/c_abf2
op_doi https://doi.org/10.17863/cam.100076
_version_ 1789962487493296128