Telychian

Third stage of the Silurian and last stage of the Llandovery From Wikipedia, the free encyclopedia

In the geologic timescale, the Telychian is the third and final age of the Llandovery Epoch of the Silurian Period of the Paleozoic Era of the Phanerozoic Eon. The Telychian Age was between 438.6 ± 1.0 million years ago (Ma) and 432.9 ± 1.2 Ma. The Telychian Age succeeds the Aeronian Age and precedes the Sheinwoodian Age.[8] The name of the interval is derived from the Pen-lan-Telych Farm near Llandovery, Powys, Wales.

Name formalityFormal
Celestial bodyEarth
Regional usageGlobal (ICS)
Time scale(s) usedICS Time Scale
Quick facts Chronology, Etymology ...
Telychian
438.6 ± 1.0 – 432.9 ± 1.2 Ma
Paleogeography of the Telychian, 435 Ma
Chronology
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Paleozoic
 
 
 
Subdivision of the Silurian according to the ICS, as of 2024.[3]
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 Spirograptus guerichi
Lower boundary GSSPEl Pintado section, Seville, Spain
37.9853°N 5.9285°W / 37.9853; -5.9285[4]
Lower GSSP ratified2024[5][6]
Upper boundary definitionImprecise. Currently placed between acritarch biozone 5 and LAD of Pterospathodus amorphognathoides. See Llandovery for more info.
Upper boundary definition candidatesA conodont boundary (Ireviken datum 2) which is close to the murchisoni graptolite biozone.
Upper boundary GSSP candidate section(s)None
Upper boundary GSSPHughley Brook, Apedale, UK
52.5811°N 2.6389°W / 52.5811; -2.6389
Upper GSSP ratified1980[7]
Close

It ended with the Ireviken event.

Ireviken event

The Ireviken event was the first of three relatively minor extinction events (the Ireviken, Mulde, and Lau events) during the Silurian Period. It occurred at the Llandovery/Wenlock boundary (mid Silurian, 432.9 ± 1.2  million years ago). The event is best recorded at Ireviken, Gotland, where over 50% of trilobite species became extinct; 80% of the global conodont species also become extinct in this interval.

References

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