Ediacaran rangeomorphs in the Mistaken Point biota, Newfoundland

Thesis (Master, Geological Sciences & Geological Engineering) -- Queen's University, 2009-02-06 09:38:13.177 The Ediacara biota is a cosmopolitan assemblage of the first macroscopic multicellular soft-bodied fossil organisms (Late Neoproterozoic, 575 – 542 Ma). The Avalon Peninsula of Newfo...

Full description

Bibliographic Details
Main Author: Flude, Lija
Other Authors: Narbonne, M. Guy, Geological Sciences and Geological Engineering
Format: Thesis
Language:English
Published: 2009
Subjects:
Online Access:http://hdl.handle.net/1974/13943
_version_ 1821625107575996416
author Flude, Lija
author2 Narbonne, M. Guy
Geological Sciences and Geological Engineering
author_facet Flude, Lija
author_sort Flude, Lija
collection Queen's University, Ontario: QSpace
description Thesis (Master, Geological Sciences & Geological Engineering) -- Queen's University, 2009-02-06 09:38:13.177 The Ediacara biota is a cosmopolitan assemblage of the first macroscopic multicellular soft-bodied fossil organisms (Late Neoproterozoic, 575 – 542 Ma). The Avalon Peninsula of Newfoundland preserves entire communities composed of hundreds of organisms in their natural life positions on decameter- to hectometer-scale bedding plane surfaces as impressions under a layer of ash. The communities are dominated by rangeomorphs, an extinct taxon with modular construction and fractal architecture. Bradgatia, a multibranched rangeomorph initially studied from 7 specimens from England, is represented by >200 specimens from 8 surfaces on the Avalon Peninsula. The Bradgatia petalage is a radial array of up to eight rangeomorph petals with four visible orders of rangeomorph branching. The petalage changes throughout ontogeny from juvenile I- or V-shaped organisms to larger U-shaped specimens to the largest and oldest O-shaped specimens. Counts of the number of petals within each taphomorph suggest that a constant number of petals was maintained throughout ontogeny. There is no significant variation in the number of frondlets with petal length suggesting that petals maintained a constant number of secondary branches throughout ontogeny. Culmofrondis new genus and species is a rangeomorph frond known from a single surface within the Mistaken Point Formation. It is constructed from non-rangeomorph primary branches which are subdivided by rangeomorph secondary and tertiary branches. The zigzagging central midline and non-rangeomorph primary branches are typical of Charnia-type branching whereas its rangeomorph secondary branches and flexible primary branches are typical of Rangea-type branching. Both Bradgatia and Culmofrondis were basally attached to the ocean floor by holdfasts suggesting they were sessile, epifaunal benthic organisms. Both were oriented parallel to contour current direction and display ...
format Thesis
genre Newfoundland
genre_facet Newfoundland
geographic Mistaken Point
geographic_facet Mistaken Point
id ftqueensuniv:oai:qspace.library.queensu.ca:1974/13943
institution Open Polar
language English
long_lat ENVELOPE(-55.774,-55.774,53.478,53.478)
op_collection_id ftqueensuniv
op_relation Canadian theses
http://hdl.handle.net/1974/13943
op_rights This publication is made available by the authority of the copyright owner solely for the purpose of private study and research and may not be copied or reproduced except as permitted by the copyright laws without written authority from the copyright owner.
publishDate 2009
record_format openpolar
spelling ftqueensuniv:oai:qspace.library.queensu.ca:1974/13943 2025-01-16T23:23:58+00:00 Ediacaran rangeomorphs in the Mistaken Point biota, Newfoundland Flude, Lija Narbonne, M. Guy Geological Sciences and Geological Engineering 2009-02-06 09:38:13.177 http://hdl.handle.net/1974/13943 eng eng Canadian theses http://hdl.handle.net/1974/13943 This publication is made available by the authority of the copyright owner solely for the purpose of private study and research and may not be copied or reproduced except as permitted by the copyright laws without written authority from the copyright owner. Ediacara rangeomorph Mistaken Point Bradgatia thesis 2009 ftqueensuniv 2023-06-17T18:07:03Z Thesis (Master, Geological Sciences & Geological Engineering) -- Queen's University, 2009-02-06 09:38:13.177 The Ediacara biota is a cosmopolitan assemblage of the first macroscopic multicellular soft-bodied fossil organisms (Late Neoproterozoic, 575 – 542 Ma). The Avalon Peninsula of Newfoundland preserves entire communities composed of hundreds of organisms in their natural life positions on decameter- to hectometer-scale bedding plane surfaces as impressions under a layer of ash. The communities are dominated by rangeomorphs, an extinct taxon with modular construction and fractal architecture. Bradgatia, a multibranched rangeomorph initially studied from 7 specimens from England, is represented by >200 specimens from 8 surfaces on the Avalon Peninsula. The Bradgatia petalage is a radial array of up to eight rangeomorph petals with four visible orders of rangeomorph branching. The petalage changes throughout ontogeny from juvenile I- or V-shaped organisms to larger U-shaped specimens to the largest and oldest O-shaped specimens. Counts of the number of petals within each taphomorph suggest that a constant number of petals was maintained throughout ontogeny. There is no significant variation in the number of frondlets with petal length suggesting that petals maintained a constant number of secondary branches throughout ontogeny. Culmofrondis new genus and species is a rangeomorph frond known from a single surface within the Mistaken Point Formation. It is constructed from non-rangeomorph primary branches which are subdivided by rangeomorph secondary and tertiary branches. The zigzagging central midline and non-rangeomorph primary branches are typical of Charnia-type branching whereas its rangeomorph secondary branches and flexible primary branches are typical of Rangea-type branching. Both Bradgatia and Culmofrondis were basally attached to the ocean floor by holdfasts suggesting they were sessile, epifaunal benthic organisms. Both were oriented parallel to contour current direction and display ... Thesis Newfoundland Queen's University, Ontario: QSpace Mistaken Point ENVELOPE(-55.774,-55.774,53.478,53.478)
spellingShingle Ediacara
rangeomorph
Mistaken Point
Bradgatia
Flude, Lija
Ediacaran rangeomorphs in the Mistaken Point biota, Newfoundland
title Ediacaran rangeomorphs in the Mistaken Point biota, Newfoundland
title_full Ediacaran rangeomorphs in the Mistaken Point biota, Newfoundland
title_fullStr Ediacaran rangeomorphs in the Mistaken Point biota, Newfoundland
title_full_unstemmed Ediacaran rangeomorphs in the Mistaken Point biota, Newfoundland
title_short Ediacaran rangeomorphs in the Mistaken Point biota, Newfoundland
title_sort ediacaran rangeomorphs in the mistaken point biota, newfoundland
topic Ediacara
rangeomorph
Mistaken Point
Bradgatia
topic_facet Ediacara
rangeomorph
Mistaken Point
Bradgatia
url http://hdl.handle.net/1974/13943