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MORPHOMETRIC ANALYSIS OF THE EDIACARAN FROND CHARNIODISCUS FROM THE MISTAKEN POINT FORMATION, NEWFOUNDLAND
by
NARBONNE, GUY M.
, LaFLAMME, MARC
, ANDERSON, MICHAEL M.
in
Analysis
/ Avalon Peninsula
/ biometry
/ Biota
/ Canada
/ Charniodiscus
/ Charniodiscus arboreus
/ Charniodiscus procerus
/ Charniodiscus spinosus
/ Eastern Canada
/ Ecological competition
/ Ecology
/ Ediacaran
/ feeding
/ Fossils
/ Fronds
/ Geology
/ Leaves
/ Mistaken Point Formation
/ morphometry
/ multivariate analysis
/ Neoproterozoic
/ new taxa
/ Newfoundland
/ Newfoundland and Labrador
/ Newfoundland Island
/ Paleobotany
/ paleoecology
/ Paleontology
/ Precambrian
/ Precambrian strata
/ Principal components analysis
/ problematic fossils
/ Proterozoic
/ Rare species
/ Social evolution
/ Specimens
/ Spine
/ statistical analysis
/ Statistical variance
/ Taxa
/ taxonomy
/ trophic analysis
/ upper Precambrian
/ Vendian
2004
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MORPHOMETRIC ANALYSIS OF THE EDIACARAN FROND CHARNIODISCUS FROM THE MISTAKEN POINT FORMATION, NEWFOUNDLAND
by
NARBONNE, GUY M.
, LaFLAMME, MARC
, ANDERSON, MICHAEL M.
in
Analysis
/ Avalon Peninsula
/ biometry
/ Biota
/ Canada
/ Charniodiscus
/ Charniodiscus arboreus
/ Charniodiscus procerus
/ Charniodiscus spinosus
/ Eastern Canada
/ Ecological competition
/ Ecology
/ Ediacaran
/ feeding
/ Fossils
/ Fronds
/ Geology
/ Leaves
/ Mistaken Point Formation
/ morphometry
/ multivariate analysis
/ Neoproterozoic
/ new taxa
/ Newfoundland
/ Newfoundland and Labrador
/ Newfoundland Island
/ Paleobotany
/ paleoecology
/ Paleontology
/ Precambrian
/ Precambrian strata
/ Principal components analysis
/ problematic fossils
/ Proterozoic
/ Rare species
/ Social evolution
/ Specimens
/ Spine
/ statistical analysis
/ Statistical variance
/ Taxa
/ taxonomy
/ trophic analysis
/ upper Precambrian
/ Vendian
2004
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MORPHOMETRIC ANALYSIS OF THE EDIACARAN FROND CHARNIODISCUS FROM THE MISTAKEN POINT FORMATION, NEWFOUNDLAND
by
NARBONNE, GUY M.
, LaFLAMME, MARC
, ANDERSON, MICHAEL M.
in
Analysis
/ Avalon Peninsula
/ biometry
/ Biota
/ Canada
/ Charniodiscus
/ Charniodiscus arboreus
/ Charniodiscus procerus
/ Charniodiscus spinosus
/ Eastern Canada
/ Ecological competition
/ Ecology
/ Ediacaran
/ feeding
/ Fossils
/ Fronds
/ Geology
/ Leaves
/ Mistaken Point Formation
/ morphometry
/ multivariate analysis
/ Neoproterozoic
/ new taxa
/ Newfoundland
/ Newfoundland and Labrador
/ Newfoundland Island
/ Paleobotany
/ paleoecology
/ Paleontology
/ Precambrian
/ Precambrian strata
/ Principal components analysis
/ problematic fossils
/ Proterozoic
/ Rare species
/ Social evolution
/ Specimens
/ Spine
/ statistical analysis
/ Statistical variance
/ Taxa
/ taxonomy
/ trophic analysis
/ upper Precambrian
/ Vendian
2004
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MORPHOMETRIC ANALYSIS OF THE EDIACARAN FROND CHARNIODISCUS FROM THE MISTAKEN POINT FORMATION, NEWFOUNDLAND
Journal Article
MORPHOMETRIC ANALYSIS OF THE EDIACARAN FROND CHARNIODISCUS FROM THE MISTAKEN POINT FORMATION, NEWFOUNDLAND
2004
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Overview
Charniodiscus is a leaf-shaped Ediacaran (terminal Neoproterozoic) fossil with a worldwide distribution, but the scarcity of complete specimens has previously hindered evaluation of its taxonomy and ecology. The presence of hundreds of complete (fronds with stem and disc attached) Charniodiscus specimens from the Avalon Zone of Newfoundland has allowed for detailed morphometric analysis of Charniodiscus specimens and permits determination of characteristics which vary with growth (e.g., stem length, frond width, and disc diameter) versus those that reflect taxonomic differences (e.g., number of primary segments, presence of a distal spine, shape ratios). This has led to the recognition of three species of Charniodiscus in the Mistaken Point biota, including numerous specimens of two new taxa, C. procerus n. sp. and C. spinosus n. sp., and rare specimens of the Australian species C. arboreus. C. procerus n. sp. and C. spinosus n. sp. represent similar, yet ecologically distinct forms of upper-level filter feeders with diverging feeding strategies in order to reduce the competition for resources. Ratio plots and principal components analyses (PCAs) confirm the existence of five (possibly six) morphologically distinct species of Charniodiscus worldwide.
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