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Cambrian Stage 3

From Wikipedia, the free encyclopedia
(Redirected fromAtdabanian)
Unnamed third stage of the Cambrian
Cambrian Stage 3
~521 – ~514.5Ma
Chronology
−540 —
−535 —
−530 —
−525 —
−520 —
−515 —
−510 —
−505 —
−500 —
−495 —
−490 —
−485 —
 
 
 
 
 
 
 
Orsten Fauna
Archaeocyatha extinction
SSF diversification, firstbrachiopods &archaeocyatha
Dresbachian extinction
Subdivision of the Cambrian according to theICS, 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 ofTrilobites
Lower boundary GSSP candidate section(s)None
Upper boundary definitionNot formally defined
Upper boundary definition candidatesFAD of theTrilobitesOlenellus orRedlichia
Upper boundary GSSP candidate section(s)None

Cambrian Stage 3 is the still unnamed third stage of theCambrian. It succeedsCambrian Stage 2 and precedesCambrian 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 oftrilobites, 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 ofCambrian Stage 4 is informally defined as the first appearance of thetrilobite generaOlenellus orRedlichia around 514.5 million years ago.[4]

Naming

[edit]

TheInternational 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 inSiberia.[5]

Biostratigraphy

[edit]

The oldesttrilobite known isLemdadella which appears at the beginning of theFallotaspis zone.[6] TheCambrian radiation of animal phyla ends here, after the diversification and origination ofarthropods,molluscs,lophophorates,chordates (includingvertebrates) among others.[7]

References

[edit]
  1. ^"International Chronostratigraphic Chart"(PDF).International Commission on Stratigraphy. December 2024. RetrievedJanuary 2, 2025.
  2. ^Ahlberg, Per; Babcock, Loren E."Subcommission on Cambrian Stratigraphy Annual Report 2017"(PDF). International Commission on Stratigraphy.Archived(PDF) from the original on 2023-07-16. Retrieved2024-03-27.
  3. ^"ISCS Working Groups: Working Group on the Stage 3 GSSP". International Subcommission on Cambrian Stratigraphy.Archived from the original on 2023-09-26.
  4. ^"GSSP Table - Paleozoic Era". Geologic Timescale Foundation.Archived from the original on 2023-10-08. Retrieved2024-03-27.
  5. ^"The 13th International Field Conference of the Cambrian Stage Subdivision Working Group"(PDF).Episodes.31 (4):440–441. Archived fromthe original(PDF) on 2014-11-05. Retrieved2024-03-27.
  6. ^Yuan, J.L.; Zhu, X.J.; Lin, J.P.; Zhu, M.Y. (22 September 2011)."Tentative correlation of Cambrian Series 2 between South China and other continents"(PDF).Bulletin of Geosciences:397–404.doi:10.3140/bull.geosci.1274. Archived fromthe original(PDF) on 2024-01-18. Retrieved2024-03-27.
  7. ^Degan Shu, Yukio Isozaki, Xingliang Zhang, Jan Han, Shigenori Maruyama (2014)."Birth and early evolution of metazoans".Gondwana Research.25 (3): 884—895.Bibcode:2014GondR..25..884S.doi:10.1016/j.gr.2013.09.001.{{cite journal}}: CS1 maint: multiple names: authors list (link)

External links

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Cenozoic Era
(present–66.0 Ma)
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Permian(252–299 Ma)
Carboniferous(299–359 Ma)
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