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Second stage of the Upper Ordovician
Katian
453.0 ± 0.7 – 445.2 ± 1.4 Ma PreꞒ Ꞓ O S D C P T J K Pg N
Paleogeography of the Katian, 450 Ma
Chronology
−485 —–−480 —–−475 —–−470 —–−465 —–−460 —–−455 —–−450 —–−445 —– P
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eLStage 10TremadocianFloianDapingianDarriwilianSandbianKatianHirnantianRhuddanian   
←First land plant spores
←Ordovician meteor event
Subdivision of the Ordovician according to the ICS, as of 2023.
Vertical axis scale: Millions of years ago
Etymology
Name formalityFormal
Usage information
Celestial bodyEarth
Regional usageGlobal (ICS)
Time scale(s) usedICS Time Scale
Definition
Chronological unitAge
Stratigraphic unitStage
Time span formalityFormal
Lower boundary definitionFAD of the graptolite Diplacanthograptus caudatus
Lower boundary GSSPBlack Knob Ridge section, Oklahoma, United States
34°25′50″N 96°04′29″W / 34.4305°N 96.0746°W / 34.4305; -96.0746
Lower GSSP ratified2006
Upper boundary definitionFAD of the graptoliteNormalograptus extraordinarius
Upper boundary GSSPWangjiawan section, Wangjiawan, Yichang, China
30°59′03″N 111°25′11″E / 30.9841°N 111.4197°E / 30.9841; 111.4197
Upper GSSP ratified2006

The Katian is the second stage of the Upper Ordovician. It is preceded by the Sandbian and succeeded by the Hirnantian Stage. The Katian began 453 million years ago and lasted for about 7.8 million years until the beginning of the Hirnantian 445.2 million years ago. During the Katian the climate cooled which started the Late Ordovician glaciation.

Naming

The name Katian is derived from Katy Lake (Atoka County, Oklahoma, United States).

GSSP

The GSSP of the Katian Stage is the Black Knob Ridge Section in southeastern Oklahoma (United States). It is an outcrop of the Womble Shale and the Bigfork Chert, the latter containing the lower boundary of the Katian. The lower boundary is defined as the first appearance datum of the graptolite species Diplacanthograptus caudatus. This horizon is 4.0 m above the base of the Bigfork Chert.

References

  1. Wellman, C.H.; Gray, J. (2000). "The microfossil record of early land plants". Phil. Trans. R. Soc. B. 355 (1398): 717–732. doi:10.1098/rstb.2000.0612. PMC 1692785. PMID 10905606.
  2. Korochantseva, Ekaterina; Trieloff, Mario; Lorenz, Cyrill; Buykin, Alexey; Ivanova, Marina; Schwarz, Winfried; Hopp, Jens; Jessberger, Elmar (2007). "L-chondrite asteroid breakup tied to Ordovician meteorite shower by multiple isochron 40 Ar- 39 Ar dating". Meteoritics & Planetary Science. 42 (1): 113–130. Bibcode:2007M&PS...42..113K. doi:10.1111/j.1945-5100.2007.tb00221.x.
  3. Lindskog, A.; Costa, M. M.; Rasmussen, C.M.Ø.; Connelly, J. N.; Eriksson, M. E. (2017-01-24). "Refined Ordovician timescale reveals no link between asteroid breakup and biodiversification". Nature Communications. 8: 14066. doi:10.1038/ncomms14066. ISSN 2041-1723. PMC 5286199. PMID 28117834. It has been suggested that the Middle Ordovician meteorite bombardment played a crucial role in the Great Ordovician Biodiversification Event, but this study shows that the two phenomena were unrelated
  4. "International Chronostratigraphic Chart" (PDF). International Commission on Stratigraphy. September 2023. Retrieved December 16, 2024.
  5. Goldman, Daniel; Leslie, Stephen; Nõlvak, Jaak; Young, Seth; Bergström, Stig; Huff, Warren (December 2007). "The Global Stratotype Section and Point (GSSP) for the base of the Katian Stage of the Upper Ordovician Series at Black Knob Ridge, Southeastern Oklahoma, USA". Episodes. 30 (4): 258–270. doi:10.18814/epiiugs/2007/v30i4/002. Retrieved 13 December 2020.
  6. Chen, Xu; Rong, Jiayu; Fan, Junxuan; Zhan, Renbin; Mitchell, Charles; Harper, David; Melchin, Michael; Peng, Ping'an; Finney, Stan; Wang, Xiaofeng (September 2006). "The Global Boundary Stratotype Section and Point (GSSP) for the base of the Hirnantian Stage (the uppermost of the Ordovician System)". Episodes. 29 (3): 183–195. doi:10.18814/epiiugs/2006/v29i3/004.
  7. "GSSP Table - Paleozoic Era". Geologic Timescale Foundation. Retrieved 2 December 2012.
  8. Bergström, Stig; Finney, Stanley; Xu, Chen; Goldman, Daniel; Leslie, Stephen (31 August 2006). "Three new Ordovician global stage names". Lethaia. 39 (3): 287–288. doi:10.1080/00241160600847439.
  9. Goldman, Daniel; Stephen A. Leslie; Jaak Nõlvak; Seth Young; Stig M. Bergström; Warren D. Huff (2007). "The Global Stratotype Section and Point (GSSP) for the base of the Katian Stage of the Upper Ordovician Series at Black Knob Ridge, Southeastern Oklahoma, USA" (PDF). Episodes. 30 (4): 258–270. doi:10.18814/epiiugs/2007/v30i4/002. Retrieved 20 September 2012.
  10. "GSSP for Katian Stage". Geologic Timescale Foundation. Retrieved 2 December 2012.
Geological history of Earth
Cenozoic Era
(present–66.0 Ma)
Quaternary (present–2.58 Ma)
Neogene (2.58–23.0 Ma)
Paleogene (23.0–66.0 Ma)
Mesozoic Era
(66.0–252 Ma)
Cretaceous (66.0–145 Ma)
Jurassic (145–201 Ma)
Triassic (201–252 Ma)
Paleozoic Era
(252–539 Ma)
Permian (252–299 Ma)
Carboniferous (299–359 Ma)
Devonian (359–419 Ma)
Silurian (419–444 Ma)
Ordovician (444–485 Ma)
Cambrian (485–539 Ma)
Proterozoic Eon
(539 Ma–2.5 Ga)
Neoproterozoic (539 Ma–1 Ga)
Mesoproterozoic (1–1.6 Ga)
Paleoproterozoic (1.6–2.5 Ga)
Archean Eon (2.5–4 Ga)
Hadean Eon (4–4.6 Ga) 
ka = kiloannum (thousand years ago); Ma = megaannum (million years ago); Ga = gigaannum (billion years ago).
See also: Geologic time scale  • icon Geology portal  • World portal


34°25′50″N 96°04′29″W / 34.4305°N 96.0746°W / 34.4305; -96.0746


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