Aeronian
Aeronian | |||||||||||||
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440.8 ± 1.2 – 438.5 ± 1.1 Ma PreꞒ Ꞓ O S D C P T J K Pg N ↓ | |||||||||||||
Chronology | |||||||||||||
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Etymology | |||||||||||||
Name formality | Formal | ||||||||||||
Usage information | |||||||||||||
Celestial body | Earth | ||||||||||||
Regional usage | Global (ICS) | ||||||||||||
Time scale(s) used | ICS Time Scale | ||||||||||||
Definition | |||||||||||||
Chronological unit | Age | ||||||||||||
Stratigraphic unit | Stage | ||||||||||||
Time span formality | Formal | ||||||||||||
Lower boundary definition | FAD of the graptolite Demirastrites triangulatus | ||||||||||||
Lower boundary GSSP | Hlásná Třebaň section, Czech Republic | ||||||||||||
Lower GSSP ratified | 2024[4][5] | ||||||||||||
Upper boundary definition | FAD of the graptolite Spirograptus guerichi | ||||||||||||
Upper boundary GSSP | El Pintado section, Seville, Spain | ||||||||||||
Upper GSSP ratified | 2024[4][6] |
In the geologic timescale, the Aeronian is an age of the Llandovery Epoch of the Silurian Period of the Paleozoic Era of the Phanerozoic Eon that began 440.8 ± 1.2 Ma and ended 438.5 ± 1.1 Ma (million years ago). The Aeronian Age succeeds the Rhuddanian Age and precedes the Telychian Age, all in the same epoch.[7]
During the Aeronian the Sedgwickii Event occurred in which graptolite diversity was greatly reduced.[8] This event has been attested in locations such as today's Canada, Libya as well as in La Chilca Formation in Argentina (then part of Gondwana).[8]
GSSP
The GSSP is located in the Trefawr Track section, 500m north of Cwm-coed-Aeron Farm, Wales, UK.[9] The GSSP lies within the gently-dipping blocky mudstones of the Trefawr Formation, which principally yield abundant and diverse shelly faunas, but also contain enough graptolites to allow recognition of several biozones.[10]
References
- ^ Jeppsson, L.; Calner, M. (2007). "The Silurian Mulde Event and a scenario for secundo—secundo events". Earth and Environmental Science Transactions of the Royal Society of Edinburgh. 93 (02): 135–154. doi:10.1017/S0263593300000377.
- ^ Munnecke, A.; Samtleben, C.; Bickert, T. (2003). "The Ireviken Event in the lower Silurian of Gotland, Sweden-relation to similar Palaeozoic and Proterozoic events". Palaeogeography, Palaeoclimatology, Palaeoecology. 195 (1): 99–124. doi:10.1016/S0031-0182(03)00304-3.
- ^ "Chart/Time Scale". www.stratigraphy.org. International Commission on Stratigraphy.
- ^ a b "Silurian Telychian and Aeronian stage GSSPs have been relocated". stratigraphy.org. International Commission on Stratigraphy. Retrieved 1 March 2024.
- ^ Štorch, Petr. "Formal proposal for a new Global Boundary Stratotype Section and Point (GSSP) for the Aeronian Stage at Hlásná Třebaň, Czech Republic" (PDF). International Commission on Stratigraphy. Retrieved 16 April 2024.
- ^ Gutierrez-Marco, Juan Carlos (August 2022). "SILURIAN TREASURES IN SPANISH UNESCO GLOBAL GEOPARKS. Silurian Times, 29 (for 2021), 16-21. -Aparecido en 2022-". doi:10.13140/RG.2.2.13314.15044. Retrieved 1 March 2024.
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(help) - ^ "GSSP Table - All Periods". International Commission on Stratigraphy. Retrieved 2018-09-15.
- ^ a b Lopez, Fernando Enrique; Kaufmann, Cintia (2023). "New insights on the Silurian graptolite biostratigraphy of the La Chilca Formation, Poblete Norte section, Central Precordillera of San Juan, Argentina: faunal replacement and paleoenvironmental implications". Andean Geology. 50 (2). doi:10.5027/andgeov50n2-3617.
- ^ Gradstein, Felix M.; Ogg, James G.; Smith, Alan G. (2004). A Geologic Time Scale 2004. ISBN 9780521786737.
- ^ "GSSP for Aeronian Stage". International Commission on Stratigraphy. Retrieved September 15, 2018.
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(present–66.0 Ma)
Quaternary (present–2.58 Ma) | |
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Neogene (2.58–23.0 Ma) | |
Paleogene (23.0–66.0 Ma) |
(66.0–252 Ma)
Cretaceous (66.0–145 Ma) | |
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Jurassic (145–201 Ma) | |
Triassic (201–252 Ma) |
(252–539 Ma)
Permian (252–299 Ma) | |
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Carboniferous (299–359 Ma) |
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Devonian (359–419 Ma) | |
Silurian (419–444 Ma) | |
Ordovician (444–485 Ma) | |
Cambrian (485–539 Ma) |
(539 Ma–2.5 Ga)
Neoproterozoic (539 Ma–1 Ga) | |
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Mesoproterozoic (1–1.6 Ga) | |
Paleoproterozoic (1.6–2.5 Ga) |
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