Jump to content

Permium

E Vicipaedia
SceletusAulacephalodontis peavoti(Therapsida):fossileesupergrege Karooeensi(en)systematis Permii inAfrica Australirepertum.Museum Historiae Naturalis FieldChicagoënse.

Permium[1][2]estsystemastratigraphicumetperiodusgeologica.

Divisio suprema constituitaeraePalaeozoicae,sexta autem ab infimaaeonisPhanerozoicae.Abhinc2989 ± 1.5 centies milium annorum coepit, antecessoreCarbonifero.Finem habuit abhinc 2521.7 ± 0.6 centies milium annorum, successoreTriassico,secundumscalam aevorum geologicorumCommissionis Internationalis Stratigraphicae.[3]Permium inceptum ab antiquissimisfossilibusStreptognathodus isolatusdatur.[4]TerminusPermius Triassicuseodem tempore quo maxima specierumexstinctioincidit.

Forma orbis terrarum sicut stadioSakmarioeratabhinccirciter 290 milies milium annorum.
Inostrancevia(laeva parte)Scutosaurumpetit. Scaena coniecturalis.

In trisseriesdividitur, quae ab infima ad supremamCisuralium,Guadalupium,Lopingiumappellantur. In novemstadiadividitur, quae ab infimo ad supremumAsselium,Sakmarium,Artinskium,Kungurium,Roadium,Wordium,Capitanium,Wuchiapingium,Changhsingiumappellantur.[5]

Nomenanno1841egubernio Permiensiimperii Russici(territorio Permiensihodierno) deduxitRodericus Murchisonsub forma AnglicaPermian system.In illo gubernio cumEduardo de Verneuilstrata amplissima huius systematis nuper exploravit.[6][7]

Animaliaex Permio opinabile restituta.

  1. "Oberes Permium (259,8–252,2 Mill Jahre)" contextu Theodiscohichabes.
  2. "Perm": Christof Kuhn, "Etymology of Geological Time Units".Rarissime" Permicum. "
  3. "International Chronostratigraphic Chart."
  4. Ita de:wiki.
  5. "Internationale Chronostratigraphische Tabelle"(2017).
  6. "Permian System(Zechsteinof Germany—Magnesian limestoneof England): Some introductory remarks explain why the authors have ventured to use a new name in reference to a group of rocks which, as a whole, they consider to be on the parallel of the Zechstein of Germany and magnesian limestone of England. They do so, not merely because a portion of deposits has long been known by the name "grits of Perm," but because, being enormously developed in the governments of Perm andOrenburg,they there assume a great variety of lithological features ": R. I. Murchison, E. de Verneuil, A. von Keyserling,On the Geological Structure of the Central and Southern Regions of Russia in Europe and of the Ural Mountains(Londinii: Richard and John E. Taylor, 1842)p. 14
  7. 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 Bulletinno. 769. Vasingtoniae: U.S. Government Printing Office, 1925) (p. 70apudGoogle Books).
  • Aceñolaza, F. G., et al.1991."El Sistema Pérmico en la República Argentina y en laRepública Oriental del Uruguay (Pre-Impresión)."II° Congr. Int. Estrat. y Geol. Carbonífero y Pérmico.Bonaeropoli: Acad. Nac. Ci. Córdoba.
  • Frey, Wolfgang, et Rainer Lösch.1998.lLehrbuch der Geobotanik.Stutgardiae: Gustav Fischer.ISBN 3-437-25940-7.
  • Lucas, Spencer G., Joerg W. Schneider, et Giuseppe Cassinis.2006."Non-Marine Permian Biostratigraphy and Biochronology]."Geological Society Special Publications265: 1–14.PDF.
  • Oschmann, Wolfgang.2016.Evolution der Erde: Geschichte der Erde und des Lebens.Bernae: Haupt Verlag. UTB basics, 4401.ISBN 978-3-8252-4401-9.
  • Rößler, Ronny.2003."Farnwälder, Glutwolken und Salzwüsten: Das Perm."Biologie in unserer Zeit33 (4): 244–51. ISSN 0045-205X.
  • Schneebeli-Hermann, Elke.2012."Extinguishing a Permian World."Geology40 (3): 287–88. doi:10.1130/focus032012.1 |bibcode=2012Geo....40..287S.
  • Schneider, Jörg W., Frank Körner, Marco Roscher, et Uwe Kroner.2006."Permian climate development in the northern peri-Tethys area: The Lodève basin, French Massif Central, compared in a European and global context."Palaeogeography, Palaeoclimatology, Palaeoecology240 (1-2): 161–83. ISSN 0031-0182.
  • Vasicek, Werner.1983.280 Millionen Jahre alte Spuren der Steinkohlewälder von Zöbing.Eggenburgi: Katalogreihe des Krahuletz-Museums 4.
  • Vasicek, Werner, et Fritz F. Steininger.1999."Jungpaläozoikum von Zöbing."Schriftenreihe des Waldviertler Heimatbundes38: 63ff.

Nexus interni

Vicimedia Communiaplura habent quae adPermiumspectant.