Cambrian Stage 3

Unnamed third stage of the Cambrian From Wikipedia, the free encyclopedia

Cambrian Stage 3 is the still unnamed third stage of the Cambrian. It succeeds Cambrian Stage 2 and precedes Cambrian Stage 4, although neither its base nor top have been formally defined. The plan is for its lower boundary to correspond approximately to the first appearance of trilobites, about 521 million years ago,[2] though the globally asynchronous appearance of trilobites warrants the use of a separate, globally synchronous marker to define the base.[3] The upper boundary and beginning of Cambrian Stage 4 is informally defined as the first appearance of the trilobite genera Olenellus or Redlichia around 514.5 million years ago.[4]

Name formalityInformal
Celestial bodyEarth
Regional usageGlobal (ICS)
Time scale(s) usedICS Time Scale
Quick facts Chronology, Etymology ...
Cambrian Stage 3
~521 – ~514.5 Ma
Chronology
540 
535 
530 
525 
520 
515 
510 
505 
500 
495 
490 
485 
Paleozoic
 
 
 
 
Orsten Fauna
Dresbachian extinction
Archaeocyatha extinction
SSF diversification, first brachiopods & archaeocyatha
Subdivision of the Cambrian according to the ICS, as of 2024.[1]
Vertical axis scale: Millions of years ago
Etymology
Name formalityInformal
Usage information
Celestial bodyEarth
Regional usageGlobal (ICS)
Time scale(s) usedICS Time Scale
Definition
Chronological unitAge
Stratigraphic unitStage
Time span formalityFormal
Lower boundary definitionNot formally defined
Lower boundary definition candidatesFAD of Trilobites
Lower boundary GSSP candidate section(s)None
Lower GSSP ratifiedNot formally defined
Upper boundary definitionNot formally defined
Upper boundary definition candidatesFAD of the Trilobites Olenellus or Redlichia
Upper boundary GSSP candidate section(s)None
Upper GSSP ratifiedNot formally defined
Close

Despite being unnamed, the Cambrian Stage 3 is notable for containing the Chengjiang biota.

Naming

The International Commission on Stratigraphy has not officially named the 3rd stage of the Cambrian. The stage approximately corresponds to the "Atdabanian", which is used by geologists working in Siberia.[5]

Biostratigraphy

The oldest trilobite known is Lemdadella which appears at the beginning of the Fallotaspis zone.[6] The Cambrian radiation of animal phyla ends here, after the diversification and origination of arthropods, molluscs, lophophorates, chordates (including vertebrates) among others.[7]

References

Further reading

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