The Lopingian is the uppermost series/last epoch of the Permian.[4] It is the last epoch of the Paleozoic. The Lopingian was preceded by the Guadalupian and followed by the Early Triassic.
| Lopingian | |||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
.png) A map of Earth as it appeared 255 million years ago during the Lopingian Epoch, Wuchiapingian Age | |||||||||||||
| Chronology | |||||||||||||
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| Etymology | |||||||||||||
| Name formality | Formal | ||||||||||||
| Synonym(s) | Late/Upper Permian | ||||||||||||
| Usage information | |||||||||||||
| Celestial body | Earth | ||||||||||||
| Regional usage | Global (ICS) | ||||||||||||
| Time scale(s) used | ICS Time Scale | ||||||||||||
| Definition | |||||||||||||
| Chronological unit | Epoch | ||||||||||||
| Stratigraphic unit | Series | ||||||||||||
| Time span formality | Formal | ||||||||||||
| Lower boundary definition | FAD of the Conodont Clarkina postbitteri postbitteri | ||||||||||||
| Lower boundary GSSP | Penglaitan Section, Laibin, Guangxi, China 23°41′43″N 109°19′16″E / 23.6953°N 109.3211°E | ||||||||||||
| Lower GSSP ratified | 2004[2] | ||||||||||||
| Upper boundary definition | FAD of the Conodont Hindeodus parvus. | ||||||||||||
| Upper boundary GSSP | Meishan, Zhejiang, China 31°04′47″N 119°42′21″E / 31.0798°N 119.7058°E | ||||||||||||
| Upper GSSP ratified | 2001[3] | ||||||||||||
The Lopingian is often synonymous with the informal terms late Permian or upper Permian.
The name was introduced by Amadeus William Grabau in 1931 and derives from Leping, Jiangxi in China.[5] It consists of two stages/ages. The earlier is the Wuchiapingian and the later is the Changhsingian.[6]
The International Chronostratigraphic Chart (v2018/07)[4] provides a numerical age of 259.1 ±0.5 Ma. If a Global Boundary Stratotype Section and Point (GSSP) has been approved, the lower boundary of the earliest stage determines numerical age of an epoch. The GSSP for the Wuchiapingian has a numerical age of 259.8 ± 0.4 Ma.[7][8]
Evidence from Milankovitch cycles suggests that the length of an Earth day during this epoch was approximately 22 hours.[9]
Geography
editDuring the Lopingian, most of the earth was in the supercontinent Pangaea. The Zechstein sea, would, at times, be connected to the Paleotethys; Other features of the earth during the time were the Microcontinent Cathaysia; And the Cimmerian superterrane, which divided the Tethys Ocean realm into the Paleo-Tethys Ocean and the slowly expanding Neotethys Ocean.
Life
editThe Lopingian ended with the Permian–Triassic extinction event, where over 95% of species went extinct.
The series follows the Guadalupian, which ended with the Capitanian mass extinction, during which many species of brachiopods, ammonoids and other groups went extinct.[10]
Conodonts would reach their all-time low during this period, despite this, they are recovered from most marine Permian localities.[11] Common conodonts from the Lopingian include the genera Clarkina and Hindeodus.
The Lopingian would see the decline of the Paleozoic ammonoid orders (Goniatitida and Prolecanitida) and the rise of the order Ceratitida, especially within the superfamily Xenodiscoidea.[12]
Only seven trilobites are known from the Lopingian, with only five by the end of the epoch. One of the last members of this clade was Kathwaia capitorosa.[13]
Eurypterids were nearly extinct by this point, consisting of the possibly Lopingian Campylocephalus permicus of Russia; and the Changhsingian Woodwardopterus? freemanorum of Australia.[14]
A member of the extant Horseshoe crab family, Limulidae; Guangyuanolimulus appears at the end of the period.[15]
On land, gorgonopsians would become the apex predators after the extinction of the Dinocephalians, Other predators include the Therocephalians. Herbivorous animals of the Lopingian include the pareiasaurs such as Scutosaurus or dicynodonts, such as Dicynodon.
Fossil gallery
edit-
Smilesaurus ferox, one of the most fearsome predators of the Lopingian
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Skull of Dicynodon, a dicynodont.
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Scutosaurus, a common herbivore during the late Permian
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See also
edit- Geologic time scale – System that relates geologic strata to time
- Cisuralian – First series of the Permian
References
edit- ^ "International Chronostratigraphic Chart" (PDF). International Commission on Stratigraphy. September 2023. Retrieved 10 November 2024.
- ^ Jin, Yugan; Shen, Shuzhong; Henderson, Charles; Wang, Xiangdong; Wang, Wei; Wang, Yue; Cao, Changqun; Shang, Qinghua (December 2006). "The Global Stratotype Section and Point (GSSP) for the boundary between the Capitanian and Wuchiapingian Stage (Permian)" (PDF). Episodes. 29 (4): 253–262. doi:10.18814/epiiugs/2006/v29i4/003. Retrieved 13 December 2020.
- ^ Hongfu, Yin; Kexin, Zhang; Jinnan, Tong; Zunyi, Yang; Shunbao, Wu (June 2001). "The Global Stratotype Section and Point (GSSP) of the Permian-Triassic Boundary" (PDF). Episodes. 24 (2): 102–114. doi:10.18814/epiiugs/2001/v24i2/004. Retrieved 8 December 2020.
- ^ a b International Commission on Stratigraphy. "Chart". Retrieved 10 July 2018.
- ^ Zhang, Shouxin (2009). Geological Formation Names of China (1866–2000). Beijing/Dordrecht: Higher Education Press/Springer. p. 681. ISBN 978-7-040-25475-4.
- ^ Allaby, Michael (2015). A Dictionary of Geology and Earth Sciences (4th ed.). Oxford University Press. doi:10.1093/acref/9780199653065.001.0001. ISBN 9780199653065.
- ^ International Commission on Stratigraphy. "GSSPs". Retrieved 10 July 2018.
- ^ Gradstein, Felix M.; Ogg, James G.; Smith, Alan G. (2004). A Geologic Time Scale 2004. Cambridge University Press. ISBN 9780521786737.
- ^ Wu, Huaichun; Zhang, Shihong; Hinnov, Linda A.; Jiang, Ganqing; Feng, Qinglai; Li, Haiyan; Yang, Tianshui (13 September 2013). "Time-calibrated Milankovitch cycles for the late Permian". Nature Communications. 4: 2452. Bibcode:2013NatCo...4.2452W. doi:10.1038/ncomms3452. PMC 3778519. PMID 24030138. S2CID 6477972.
- ^ Bond, David; Hilton, Jason; Wignall, Paul; Ali, Jason; Stevens, Liadan; Sun, Yadong; Lai, Xulong (2010). "The Middle Permian (Capitanian) mass extinction on land and in the oceans". Earth-Science Reviews. 102 (1–2): 100–116. Bibcode:2010ESRv..102..100B. doi:10.1016/j.earscirev.2010.07.004.
- ^ Wardlaw, R. B. (1995). "Permian Conodonts". In Scholle, P.A.; Peryt, T.M.; Ulmer-Scholle, D.S. (eds.). The Permian of Northern Pangea. Berlin, Heidelberg: Springer. pp. 186–195. doi:10.1007/978-3-642-78593-1_12. ISBN 978-3-642-78595-5.
- ^ Leonova, T.B. (2016). "Major trends in the evolution of Permian ammonoids". Paleontological Journal. 50 (2): 131–140. Bibcode:2016PalJ...50..131L. doi:10.1134/S0031030116020039.
- ^ "The last Trilobites". www.Trilobites.info.
- ^ Poschmann, Marjus J.; Rozefelds, Andrew (2022). "The last eurypterid – a southern high-latitude record of sweep-feeding sea scorpion from Australia constrains the timing of their extinction". Historical Biology. 34 (10): 2020–2030. Bibcode:2022HBio...34.2020P. doi:10.1080/08912963.2021.1998033.
- ^ Hu, Shixue; Feldmann, Rodney M.; Schweitzer, Carrie E.; Benton, Michael J.; Huang, Jinyuan; Wen, Wen; Min, Xiao; Zhang, Qiyue; Zhou, Changyong; Ma, Zhixin (15 September 2022). "A new horseshoe crab from the Permian-Triassic transition of South China: Xiphosurids as key components of post-extinction trophic webs". Palaeogeography, Palaeoclimatology, Palaeoecology. 602: 111178. doi:10.1016/j.palaeo.2022.111178. ISSN 0031-0182.