Quantum redactiones paginae "Palaeozoicum" differant

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[[Fasciculus:Asaphiscuswheelerii.jpg|thumb|''[[Asaphiscus wheeleri]]'', [[fossile]] Palaeozoicum.]]
'''Palaeozoicum'''<ref>"Palaeozoicum": Robertus Koeppel, ''Praelectiones geologiae et praehistoriae'' pars 1 iii (Romae, 1933) p. 5 {{Google Books|zDbEpQ0QkUMC|Paginae selectae}}.</ref> est [[aerathema]] [[stratigraphia|stratigraphicum]] et [[aera (geologia)|aera]] geologica [[aeon]]is [[Phanerozoicum|Phanerozoici]] infima. Palaeozoicum incepit [[a.p.|abhinc]] 541&nbsp;000 ± 1&nbsp;000 milium annorum anni et abhinc 251&nbsp;902 ± 24 milium annorum finem habuit. In sex [[periodus (geologia)|periodos]] dividitur, quae ab infima ad supremam [[Cambrium]], [[Ordovicium]], [[Silurium]], [[Devonium]], [[Carboniferum]], [[Permium]] appellantur.
 
'''Palaeozoicum'''<ref>"Palaeozoicum": Robertus Koeppel, ''Praelectiones geologiae et praehistoriae'' pars 1 iii (Romae, 1933) p. 5 {{Google Books|zDbEpQ0QkUMC|Paginae selectae}}</ref> est [[aerathema]] [[stratigraphia|stratigraphicum]] et [[aera (geologia)|aera]] geologica [[aeon]]is [[Phanerozoicum|Phanerozoici]] infima. Palaeozoicum incepit [[a.p.|abhinc]] 541&nbsp;000 ± 1&nbsp;000 milium annorum anni et abhinc 251&nbsp;902 ± 24 milium annorum finem habuit. In sex [[periodus (geologia)|periodos]] dividitur, quae ab infima ad supremam [[Cambrium]], [[Ordovicium]], [[Silurium]], [[Devonium]], [[Carboniferum]], [[Permium]] appellantur.
 
[[Phanerozoicum]], Palaeozoicum, Cambrium omnia incepta ex antiquissimis [[ichnofossile|ichnofossilibus]] ''[[Treptichnus pedum|Treptichnus pedum]]'' dantur.
 
Nomen e [[verbum|verbis]] [[Lingua Graeca|Graecis]] παλαιός "'antiquus"' + ζῷον "'[[animal"]]' ab [[Adam Sedgwick|Adamo Sedgwick]] anno [[1838]] [[Anglice]] sub forma ''Palæozoic series'' compositum est ut [[systema (stratigraphia)|systema]]ta [[Cambrium]] et [[Silurium]] comprehendat.<ref>Adam Sedgwick, "A synopsis of the English series of stratified rocks inferior to the Old Red Sandstone, with an attempt to determine the successive natural groups and formations" in ''Proceedings of the Geological Society of London'' vol. 2 (1838), pp. 675–685675–85, vide [https://babel.hathitrust.org/cgi/pt?id=mdp.39015031294112&view=1up&seq=611 p. 685]</ref><ref>De historia nominis definitionisque vide: Mary Grace Wilmarth, ''The Geologic Time Classification of the United States Geological Survey Compared With Other Classifications, accompanied by the original definitions of era, period and epoch terms'' (''United States Geological Survey Bulletin'' no. 769. Vasingtoniae: U.S. Government Printing Office, 1925) {{Google Books|my7x_PBkpm4C|p. 10}}.</ref>
 
{{NexInt}}
*[[Panthalassa]]
 
== Notae ==
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== Bibliographia ==
* Donna M Jurdy, MKichael Stefanick, Christopher Scotese, "[https://www.academia.edu/9320052/Paleozoic_plate_dynamics Paleozoic plate dynamics.]" in ''Journal of Geophysical Research'' vol. 100 (1995) pp. 17965-17975.
* Shanan E. Peters, "[https://www.academia.edu/10649628/The_problem_with_the_Paleozoic The problem with the Paleozoic.]" in ''Paleobiology'' (2007).
* A. M. Ziegler et al., "[https://www.academia.edu/24159208/Paleozoic_Paleogeography Paleozoic Paleogeography.]" in ''Annual Review of Earth and Planetary Sciences'' vol. 7 (1979) pp. 473-502.
 
== Nexus externi ==
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[[Categoria:Aerae]]
[[Categoria:Aeva geologica]]
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{{Myrias|Physica}}