Post-fossilization processes and their implications for understanding Ediacaran macrofossil assemblages
Fossil assemblages from Newfoundland’s Avalon Peninsula preserve diverse examples of the enigmatic Ediacaran macrobiota, offering some of the earliest evidence for large and complex multicellular life. These fossils are exposed on extensive coastal bedding planes in extraordinary abundances, permitt...
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ftdatacite:10.17863/cam.7357 2023-05-15T17:22:04+02:00 Post-fossilization processes and their implications for understanding Ediacaran macrofossil assemblages Matthews, JJ Liu, Alexander McIlroy, D 2017 https://dx.doi.org/10.17863/cam.7357 https://www.repository.cam.ac.uk/handle/1810/262112 unknown Apollo - University of Cambridge Repository Creative Commons Attribution 4.0 International Creative Commons Attribution 4.0 International Creative Commons Attribution 4.0 International Creative Commons Attribution 4.0 International Attribution 4.0 International Attribution 4.0 International Attribution 4.0 International Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY Text Article article-journal ScholarlyArticle 2017 ftdatacite https://doi.org/10.17863/cam.7357 2021-11-05T12:55:41Z Fossil assemblages from Newfoundland’s Avalon Peninsula preserve diverse examples of the enigmatic Ediacaran macrobiota, offering some of the earliest evidence for large and complex multicellular life. These fossils are exposed on extensive coastal bedding planes in extraordinary abundances, permitting palaeoecological studies based on census data from spatially extensive palaeocommunities. Such studies have been used to constrain the reproductive strategy and phylogenetic placement of Ediacaran organisms. Geological mapping and stratigraphic correlation in the Mistaken Point Ecological Reserve reveal that some fossil-bearing surfaces can be tracked over distances of several kilometres. These laterally extensive surfaces reveal that the modern processes by which the sediment overlying a fossil surface is removed may impose important controls on the observed composition of fossil assemblages. Weathering and erosion – along with factors associated with tectonics, metamorphism and discovery – are here grouped as ‘post-fossilization processes’ and introduce biases that are often not explicitly accounted for in palaeoecological studies. Specifically, post-fossilization processes may differentially influence the preservational fidelity of individual specimens on a given surface and generate features that could be mistaken for original morphological characters. We therefore recommend that post-fossilization processes must be considered when undertaking palaeoecological studies in Ediacaran successions in Newfoundland and, potentially, elsewhere. : This research was supported by the Natural Environment Research Council [grant numbers NE/J5000045/1 to JJM, and NE/L011409/1 to AGL]. Joe Stewart and Tom Hearing are thanked for assistance in gathering field data. Thanks are also extended to Martin Brasier, without whom this research would never have taken place. Reviews from Matthew Clapham and one anonymous reviewer greatly improved the manuscript. The Parks and Natural Areas Division, Department of Environment and Conservation, Government of Newfoundland and Labrador, provided permits to conduct research within the Mistaken Point Ecological Reserve. Access to fossil localities within the Mistaken Point Ecological Reserve for research is by permit only. The fossils around Cape Race are protected by the Paleontological Resource Regulations 67/11, under the Historic Resources Act, 1990. Text Newfoundland DataCite Metadata Store (German National Library of Science and Technology) Newfoundland Mistaken Point ENVELOPE(-55.774,-55.774,53.478,53.478) |
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Fossil assemblages from Newfoundland’s Avalon Peninsula preserve diverse examples of the enigmatic Ediacaran macrobiota, offering some of the earliest evidence for large and complex multicellular life. These fossils are exposed on extensive coastal bedding planes in extraordinary abundances, permitting palaeoecological studies based on census data from spatially extensive palaeocommunities. Such studies have been used to constrain the reproductive strategy and phylogenetic placement of Ediacaran organisms. Geological mapping and stratigraphic correlation in the Mistaken Point Ecological Reserve reveal that some fossil-bearing surfaces can be tracked over distances of several kilometres. These laterally extensive surfaces reveal that the modern processes by which the sediment overlying a fossil surface is removed may impose important controls on the observed composition of fossil assemblages. Weathering and erosion – along with factors associated with tectonics, metamorphism and discovery – are here grouped as ‘post-fossilization processes’ and introduce biases that are often not explicitly accounted for in palaeoecological studies. Specifically, post-fossilization processes may differentially influence the preservational fidelity of individual specimens on a given surface and generate features that could be mistaken for original morphological characters. We therefore recommend that post-fossilization processes must be considered when undertaking palaeoecological studies in Ediacaran successions in Newfoundland and, potentially, elsewhere. : This research was supported by the Natural Environment Research Council [grant numbers NE/J5000045/1 to JJM, and NE/L011409/1 to AGL]. Joe Stewart and Tom Hearing are thanked for assistance in gathering field data. Thanks are also extended to Martin Brasier, without whom this research would never have taken place. Reviews from Matthew Clapham and one anonymous reviewer greatly improved the manuscript. The Parks and Natural Areas Division, Department of Environment and Conservation, Government of Newfoundland and Labrador, provided permits to conduct research within the Mistaken Point Ecological Reserve. Access to fossil localities within the Mistaken Point Ecological Reserve for research is by permit only. The fossils around Cape Race are protected by the Paleontological Resource Regulations 67/11, under the Historic Resources Act, 1990. |
format |
Text |
author |
Matthews, JJ Liu, Alexander McIlroy, D |
spellingShingle |
Matthews, JJ Liu, Alexander McIlroy, D Post-fossilization processes and their implications for understanding Ediacaran macrofossil assemblages |
author_facet |
Matthews, JJ Liu, Alexander McIlroy, D |
author_sort |
Matthews, JJ |
title |
Post-fossilization processes and their implications for understanding Ediacaran macrofossil assemblages |
title_short |
Post-fossilization processes and their implications for understanding Ediacaran macrofossil assemblages |
title_full |
Post-fossilization processes and their implications for understanding Ediacaran macrofossil assemblages |
title_fullStr |
Post-fossilization processes and their implications for understanding Ediacaran macrofossil assemblages |
title_full_unstemmed |
Post-fossilization processes and their implications for understanding Ediacaran macrofossil assemblages |
title_sort |
post-fossilization processes and their implications for understanding ediacaran macrofossil assemblages |
publisher |
Apollo - University of Cambridge Repository |
publishDate |
2017 |
url |
https://dx.doi.org/10.17863/cam.7357 https://www.repository.cam.ac.uk/handle/1810/262112 |
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ENVELOPE(-55.774,-55.774,53.478,53.478) |
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Newfoundland Mistaken Point |
geographic_facet |
Newfoundland Mistaken Point |
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Newfoundland |
genre_facet |
Newfoundland |
op_rights |
Creative Commons Attribution 4.0 International Creative Commons Attribution 4.0 International Creative Commons Attribution 4.0 International Creative Commons Attribution 4.0 International Attribution 4.0 International Attribution 4.0 International Attribution 4.0 International Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
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CC-BY |
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https://doi.org/10.17863/cam.7357 |
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1766108317578428416 |