Mistaken Point Formation

Geologic formation in Newfoundland and Labrador, Canada From Wikipedia, the free encyclopedia

The Mistaken Point Formation[4] is a geologic formation in Newfoundland and Labrador. It is recognized as a Lagerstätte preserving fossils dating back to the Ediacaran period. It contains a stratum dated to 565 ± 3 million years ago.

Sub-unitsMurphy's Cove and Goodland Point Members [2]
Quick facts Type, Unit of ...
Mistaken Point Formation
Stratigraphic range: Ediacaran 565 Ma
TypeFormation
Unit ofConception Group[1]
Sub-unitsMurphy's Cove and Goodland Point Members [2]
UnderliesTrepassey Formation[3]
Overlies
Lithology
PrimaryTuffaceous siltstone[3]
OtherSandstone, Shale
Location
RegionNewfoundland
CountryCanada

Outcrop occurrence of the Mistaken Point formation in southeast Newfoundland
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Geology

Mistaken Point Formation includes many fine ash-beds, which are a good source of zircons used in the uranium-lead method of radiometric dating, allowing the site to be confidently dated to approximately 565 million years old.

These fine-grained volcanic ash beds also preserve finely detailed fossils.[5][6]

Fossils

cone shaped organism Thectardis

Mistaken Point contains some of the oldest ediacaran biota in an Avalon-type assemblage. They are commonly categorized as Spindle-shaped (Fractofusus), Frond-shaped (Charniodiscus), or Bush-like / Radiating (Bradgatia) in form. Spindles are the most common fossils in the assemblage. Other forms do exist, such as the conical Thectardis.

Some of the forms here appear to survive until the extinction of the Ediacaran biota at the base of the Cambrian. The evolutionary history of these forms is unknown, though hypotheses exist.[7]

comb shaped organism Pectinifrons

Discovery of Ediacaran fossils in the Avalon Peninsula

In the summer of 1967, Shiva Balak Misra, an Indian graduate student (1966–69) at Newfoundland's Memorial University discovered a rich assemblage of imprints of soft bodied organisms on the surface of large rock slabs, while mapping the Conception Group of Avalon Peninsula of Newfoundland near Cape Race, at a place called Mistaken Point.[8]

These unusual impressions of previously unknown soft-bodied sea animals on the surfaces of argillites (mudstone) included coelenterates and other metazoa of the Ediacarian period, 575 to 560 million years ago.[9] These fossils are records of the oldest known complex life forms that existed anywhere on Earth.[9] Misra was the first to prepare and present a systematic geological map of the region, to classify and describe the rock sequence of the area and to work out the depositional history of the rocks.

The description of the fossil assemblage together with their mode of occurrence, the cause of sudden death, ecological conditions and chronological position form part of Misra's detailed thesis submitted for the degree of Master of Science. The discovery was reported in a 1968 letter to Nature.[10] Misra described the Mistaken Point fauna in detail in 1969, in a paper published in the Bulletin of the Geological Society of America.[11] He sorted the fossil assemblage into five groups, namely spindle-shaped, leaf-shaped, round lobate, dendrite like, and radiating. Each group was defined in terms of distribution and form, sub-categories and biological affinity.[8]

The geological environment of the fossil-bearing rocks and the ecology of the animals that lived and died in the Conception Sea were described by Misra in two of his subsequent papers published in the Bulletin of the Geological Society of America in 1971[12] and in the Journal of the Geological Society of India in 1981.[5] Mistaken Point Ecological Reserve is a 5.7-square kilometer area of the coast that protects the fossils.[9]

The sudden appearance of Ediacaran soft bodied organisms in the Mistaken Point assemblage has been called the 'Ediacaran Explosion' or 'Avalon Explosion' [13]

Paleobiota

Like the other overlying and underlying formations, the Mistaken Point Formation represents a rare deep-marine paleoenviroment,[14] which was home to various sessile forms, most predominantly, the petalonamids like Fractofusus and Frondophyllas.

Color key
Taxon Reclassified taxon Taxon falsely reported as present Dubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.

Petalonamae

More information Genus, Species ...
Genus Species Notes Images
Arborea[15]
  • A. arborea
Sessile frondose organism.
Sessile frondose organism
Beothukis[15]
  • B. mistakensis
Sessile frondose organism.
Bradgatia[15]
  • B. linfordensis
Sessile frondose organism.
Broccoliforma[17]
  • B. alta
Sessile frondose organism.
Charnia[15]
  • C. masoni
Sessile frondose organism.
Charniodiscus[15]
  • C. procerus
Sessile frondose organism.
Frondophyllas[18][19][15]
  • F. grandis
Sessile tree-like frondose organism.
Fractofusus[19][15]
  • F. andersoni
  • F. misrai
Sessile spindle-like frondose organism.
Gigarimaneta[20]
  • G. samsoni
Sessile frondose organism.
Hapsidophyllas[15]
  • H. flexibilis
Sessile frondose organism.
Pectinifrons[15]
  • P. abyssalis
Sessile frondose organism.
Plumeropriscum[17][15]
  • P. hofmanni
Sessile frondose organism.
Primocandelabrum[15]
  • P. hiemaloranum
  • Primocandelabrum sp.
Sessile frondose organism.
Trepassia[15]
  • T. wardae
Sessile frondose organism.
Vinlandia[21]
  • V. antecedens
Sessile frondose organism.
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incertae sedis

More information Genus, Species ...
Genus Species Notes Images
Aspidella[22][15]
  • A. terranovica
Enigmatic discoidal fossil.
Parviscopa[23]
  • P. bonavistensis
Frondose organism.
Hadryniscala[24][15]
  • H. avalonica
Ladder-like organism.
Hadrynichorde[24]
  • H. catalinensis
Sea Whip-like frondose organism.
Hiemalora[15]
  • Hiemalora sp.
Discoid organism, possibly holdfasts of petalonamids.
Thectardis[15]
  • T. avalonensis
Sessile frondose organism.
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Ivesheadiomorphs

More information Genus, Species ...
Genus Species Notes Images
Ivesheadia[15]
  • Ivesheadia sp.
Poorly preserved organism.
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See also

References

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