Framboidal pyrite shroud confirms the ‘death mask' model for moldic preservation of ediacaran soft-bodied organism

The mechanisms by which soft-bodied organisms were preserved in late Ediacaran deep-marine environments are revealed by petrographic and geochemical investigation of fossil-bearing surfaces from the Conception and St. John's groups (Newfoundland, Canada). Framboidal pyrite veneers are documente...

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Published in:PALAIOS
Main Author: Liu, Alexander G.
Format: Article in Journal/Newspaper
Language:English
Published: SEPM (Society of Sedimentary Geology) 2016
Subjects:
Online Access:http://eprints.esc.cam.ac.uk/3864/
http://eprints.esc.cam.ac.uk/3864/1/palo.2015.095.pdf
https://doi.org/10.2110/palo.2015.095
id ftucambridgeesc:oai:eprints.esc.cam.ac.uk:3864
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spelling ftucambridgeesc:oai:eprints.esc.cam.ac.uk:3864 2023-05-15T17:22:33+02:00 Framboidal pyrite shroud confirms the ‘death mask' model for moldic preservation of ediacaran soft-bodied organism Liu, Alexander G. 2016 text http://eprints.esc.cam.ac.uk/3864/ http://eprints.esc.cam.ac.uk/3864/1/palo.2015.095.pdf https://doi.org/10.2110/palo.2015.095 en eng SEPM (Society of Sedimentary Geology) http://eprints.esc.cam.ac.uk/3864/1/palo.2015.095.pdf Liu, Alexander G. (2016) Framboidal pyrite shroud confirms the ‘death mask' model for moldic preservation of ediacaran soft-bodied organism. Palaios, 31 (5). pp. 259-274. ISSN 0833-1351 DOI https://doi.org/10.2110/palo.2015.095 <https://doi.org/10.2110/palo.2015.095> 04 - Palaeobiology Article PeerReviewed 2016 ftucambridgeesc https://doi.org/10.2110/palo.2015.095 2020-08-27T18:09:49Z The mechanisms by which soft-bodied organisms were preserved in late Ediacaran deep-marine environments are revealed by petrographic and geochemical investigation of fossil-bearing surfaces from the Conception and St. John's groups (Newfoundland, Canada). Framboidal pyrite veneers are documented on fossil-bearing horizons at multiple localities. The pyrite is interpreted to have formed via microbial processes in the hours to weeks following burial of benthic communities. This finding extends the ‘death mask' model for Ediacaran soft-tissue preservation to deep-marine settings. Remineralization of pyrite to iron oxides and oxyhydroxides is recognized to result from recent oxidation by meteoric fluids in the shallow subsurface. Consideration of other global Ediacaran macrofossil occurrences reveals that pyrite is observed in association with Ediacaran macrofossils preserved in all four previously described styles of moldic preservation (Flinders-, Conception-, Fermeuse- and Nama-type). This suggests that replication of external morphology by framboidal pyrite was a widespread mechanism by which soft-bodied organisms and associated organic surfaces were preserved, in multiple facies and depositional environments, 580–541 million years ago. The extensive global burial of pyrite in medium- to coarse-grained clastics and carbonates is a previously unrecognized yet potentially significant geological sink of iron and sulfur, and may have contributed to rising atmospheric and marine oxygen concentrations across the late Ediacaran interval. Article in Journal/Newspaper Newfoundland University of Cambridge, Department of Earth Sciences: ESC Publications Canada Flinders ENVELOPE(-66.667,-66.667,-69.267,-69.267) PALAIOS 31 5 259 274
institution Open Polar
collection University of Cambridge, Department of Earth Sciences: ESC Publications
op_collection_id ftucambridgeesc
language English
topic 04 - Palaeobiology
spellingShingle 04 - Palaeobiology
Liu, Alexander G.
Framboidal pyrite shroud confirms the ‘death mask' model for moldic preservation of ediacaran soft-bodied organism
topic_facet 04 - Palaeobiology
description The mechanisms by which soft-bodied organisms were preserved in late Ediacaran deep-marine environments are revealed by petrographic and geochemical investigation of fossil-bearing surfaces from the Conception and St. John's groups (Newfoundland, Canada). Framboidal pyrite veneers are documented on fossil-bearing horizons at multiple localities. The pyrite is interpreted to have formed via microbial processes in the hours to weeks following burial of benthic communities. This finding extends the ‘death mask' model for Ediacaran soft-tissue preservation to deep-marine settings. Remineralization of pyrite to iron oxides and oxyhydroxides is recognized to result from recent oxidation by meteoric fluids in the shallow subsurface. Consideration of other global Ediacaran macrofossil occurrences reveals that pyrite is observed in association with Ediacaran macrofossils preserved in all four previously described styles of moldic preservation (Flinders-, Conception-, Fermeuse- and Nama-type). This suggests that replication of external morphology by framboidal pyrite was a widespread mechanism by which soft-bodied organisms and associated organic surfaces were preserved, in multiple facies and depositional environments, 580–541 million years ago. The extensive global burial of pyrite in medium- to coarse-grained clastics and carbonates is a previously unrecognized yet potentially significant geological sink of iron and sulfur, and may have contributed to rising atmospheric and marine oxygen concentrations across the late Ediacaran interval.
format Article in Journal/Newspaper
author Liu, Alexander G.
author_facet Liu, Alexander G.
author_sort Liu, Alexander G.
title Framboidal pyrite shroud confirms the ‘death mask' model for moldic preservation of ediacaran soft-bodied organism
title_short Framboidal pyrite shroud confirms the ‘death mask' model for moldic preservation of ediacaran soft-bodied organism
title_full Framboidal pyrite shroud confirms the ‘death mask' model for moldic preservation of ediacaran soft-bodied organism
title_fullStr Framboidal pyrite shroud confirms the ‘death mask' model for moldic preservation of ediacaran soft-bodied organism
title_full_unstemmed Framboidal pyrite shroud confirms the ‘death mask' model for moldic preservation of ediacaran soft-bodied organism
title_sort framboidal pyrite shroud confirms the ‘death mask' model for moldic preservation of ediacaran soft-bodied organism
publisher SEPM (Society of Sedimentary Geology)
publishDate 2016
url http://eprints.esc.cam.ac.uk/3864/
http://eprints.esc.cam.ac.uk/3864/1/palo.2015.095.pdf
https://doi.org/10.2110/palo.2015.095
long_lat ENVELOPE(-66.667,-66.667,-69.267,-69.267)
geographic Canada
Flinders
geographic_facet Canada
Flinders
genre Newfoundland
genre_facet Newfoundland
op_relation http://eprints.esc.cam.ac.uk/3864/1/palo.2015.095.pdf
Liu, Alexander G. (2016) Framboidal pyrite shroud confirms the ‘death mask' model for moldic preservation of ediacaran soft-bodied organism. Palaios, 31 (5). pp. 259-274. ISSN 0833-1351 DOI https://doi.org/10.2110/palo.2015.095 <https://doi.org/10.2110/palo.2015.095>
op_doi https://doi.org/10.2110/palo.2015.095
container_title PALAIOS
container_volume 31
container_issue 5
container_start_page 259
op_container_end_page 274
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