<str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> central Pyrenees (Huesca, Spain): Dip. Sci. Terra, SienaUniv, Abstract Volume, p. 40-41.Glenister, B. F., Wardlaw, B. R., Lambert, L. L., Spinosa, C.,Bowring, S. A, Erwin, D. H., Menning, M. and Wilde, G. L.,1999. Proposal <str<strong>on</strong>g>of</str<strong>on</strong>g> Guadalupian and comp<strong>on</strong>ent Roadian,Wordian and Capitanian stages as Internati<strong>on</strong>al Standardsfor Middle <strong>Permian</strong>: Permophiles, no. 34, p. 3-11.Göncüoglu, M. C., Turhan, N. and Tekin, U. K., 2001. Newstratigraphic and pale<strong>on</strong>tologic results from <str<strong>on</strong>g>the</str<strong>on</strong>g> nor<str<strong>on</strong>g>the</str<strong>on</strong>g>rnedge <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> Tauride-Anatolide Platform: implicati<strong>on</strong>s for <str<strong>on</strong>g>the</str<strong>on</strong>g>Triassic rifting and opening <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> Neotethyan Izmir-Ankara ocean in Turkey: Dip. Sci. Terra, Siena Univ,Abstract Volume, p. 42-43.Ivakhnenko, M. F., Golubev, V. K., Gubin, Yu. M., Kalandadze, N.N., Novikov, I. V., Sennikov, A. G. and Rautian, A. S.,1997.<strong>Permian</strong> and Triassic tetrapods <str<strong>on</strong>g>of</str<strong>on</strong>g> Eastern Europe: Moscow,Ed. GEOS, 216 p.(In Russian).Kalandadze, N. N. and Rautian A. S., 1981. Interc<strong>on</strong>tinental relati<strong>on</strong>s<str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> terrestrial tetrapods and designati<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> problems<str<strong>on</strong>g>of</str<strong>on</strong>g> Scotch fauna, Elgin, Life <strong>on</strong> <str<strong>on</strong>g>the</str<strong>on</strong>g> old c<strong>on</strong>tinents, itsformati<strong>on</strong> and development: L. Ed,VSEGEI, 1981, p. 124-133(In Russian).Körner, F., Schneider, J. W., Hoernes, S., Gand, G. and KleebergR., 2001. Climate and c<strong>on</strong>tinental sedimentati<strong>on</strong> in <str<strong>on</strong>g>the</str<strong>on</strong>g> <strong>Permian</strong><str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> Lodève Basin (D-France) – Sedimentology, Geochemistry,Cyclostratigraphy: Dip. Sci. Terra, Siena Univ, AbstractVolume, p. 45-46.Kozur, H. W., Silantiev, V. V. and Chalimbadja, V. G., 1998. C<strong>on</strong>od<strong>on</strong>tsfrom <str<strong>on</strong>g>the</str<strong>on</strong>g> Kazanian <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> Russian platform: Internati<strong>on</strong>alSymposium Upper <strong>Permian</strong> Stratotypes <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> Volgaregi<strong>on</strong>, 27 July-4 August 1998, Kazan. Abstracts, p. 84-85.Lago, M., Gil, Imaz A., Galé, C., Arranz, E. and Pocoví, A., 2001.Lower <strong>Permian</strong> magmatism in <str<strong>on</strong>g>the</str<strong>on</strong>g> Iberian Chain and <str<strong>on</strong>g>the</str<strong>on</strong>g> AtienzaArea (Spanish central system): petrological relati<strong>on</strong>ships: Dip.Sci. Terra, Siena Univ, Abstract Volume, p. 47-48.Lazzarotto, A., Aldinucci, M., Cirilli, S., Costantini, A., Decandia,F.A., Pandeli, E., Sandrelli, F. and Spina, A., 2001. Stratigraphiccorrelati<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> Upper Palaeozoic-triassic successi<strong>on</strong>s inTuscany, Italy: a review. Dip. Sci. Terra, Siena Univ, AbstractVolume, p. 49-51.Lozovsky, V. R. ,1992. The <strong>Permian</strong>-Triassic boundary in <str<strong>on</strong>g>the</str<strong>on</strong>g> c<strong>on</strong>tinentalseries <str<strong>on</strong>g>of</str<strong>on</strong>g> Laurasia and its correlati<strong>on</strong> with <str<strong>on</strong>g>the</str<strong>on</strong>g> marinescale: Internati<strong>on</strong>al Geology Review, v. 34, no. 10, p. 1008-1014.Lozovsky, V. R., 2001. Some problems and new achievements in <str<strong>on</strong>g>the</str<strong>on</strong>g>l<strong>on</strong>g distant correlati<strong>on</strong>s <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> c<strong>on</strong>tinental <strong>Permian</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> Pangea:Dip. Sci. Terra, Siena Univ, Abstract Volume, p. 52-53.Lucas, S. G.,1998. <strong>Permian</strong> tetrapod biochr<strong>on</strong>ology: Permophiles,no. 32, p. 17-24.Lucas, S. G. and Hechert, A. B. (eds.), 1995. Early <strong>Permian</strong> footprintsand facies: Bulletin <str<strong>on</strong>g>of</str<strong>on</strong>g> New Mexico Museum <str<strong>on</strong>g>of</str<strong>on</strong>g> NaturalHistory and Science, v. 6, 301 p.Pandeli, E., Bagnoli, P. and Negri, M., 2001. The FornovolascoSchists <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> Apuan Alps (Nor<str<strong>on</strong>g>the</str<strong>on</strong>g>rn Tuscany, Italy): a newhypo<str<strong>on</strong>g>the</str<strong>on</strong>g>sis regarding <str<strong>on</strong>g>the</str<strong>on</strong>g>ir stratigraphic placement: Dip. Sci.Terra, Siena Univ, Abstract Volume, p. 54-56.Pascucci, V. and Gibling, M. R., 2001. Carb<strong>on</strong>iferous to Triassicevoluti<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> Maritimes Basin, Atlantic Canada: Dip. Sci.Terra, Siena Univ, Abstract Volume, p. 57-58.Permophiles Issue #38 20016Romer A. S.,1966. Vertebrate pale<strong>on</strong>tology: Third editi<strong>on</strong>. ChicagoPress, 468 p.Santi, G., 2001. Tetrapod ichnology <str<strong>on</strong>g>of</str<strong>on</strong>g> Early permian deposits in<str<strong>on</strong>g>the</str<strong>on</strong>g> Orobic Basin (Sou<str<strong>on</strong>g>the</str<strong>on</strong>g>rn Alps, Nor<str<strong>on</strong>g>the</str<strong>on</strong>g>rn Italy): Dip. Sci.Terra, Siena Univ, Abstract Volume, p. 59-60.Sciunnach, D., 2001. Benthic foraminifers from <str<strong>on</strong>g>the</str<strong>on</strong>g> Upper CollioFormati<strong>on</strong> (Lower <strong>Permian</strong>, Lombardy Sou<str<strong>on</strong>g>the</str<strong>on</strong>g>rn Alps): implicati<strong>on</strong>s<strong>on</strong> <str<strong>on</strong>g>the</str<strong>on</strong>g> palaeogeography <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> Pery-Tethyan area:Dip. Sci. Terra, Siena Univ, Abstract Volume, p. 61-62.Spina, A., Cirilli, S. and Baud, A., 2001. Palynological characterisati<strong>on</strong><str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> P/T boundary by comparis<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> Sverdrup basinsuccessi<strong>on</strong>s (High Arctic, Canada) and PTB G<strong>on</strong>dwanianlocalities: Dip. Sci. Terra, Siena Univ, Abstract Volume, p. 63-64.Spina, A., Cirilli, S., Decandia, F. A. and Lazzarotto, A., 2001. Palynologicaldata from <str<strong>on</strong>g>the</str<strong>on</strong>g> Poggio al Carpino sandst<strong>on</strong>es Fm.(Sou<str<strong>on</strong>g>the</str<strong>on</strong>g>rn Tuscany, Italy): Dip. Sci. Terra, Siena Univ, AbstractVolume, p. 65-66.Steyer, S., Escullié, F., Pouill<strong>on</strong>, J.-M., Broutin, J., Debriette, P.,Freytet, P., Gand, G., Poplin, C., Rage, J.-C., Rival, J., Schneider,J. W., Stamberg, S. T., Werneburg, R., and Cuny, G., 2000.New floras and faunas from <str<strong>on</strong>g>the</str<strong>on</strong>g> Lower Permin <str<strong>on</strong>g>of</str<strong>on</strong>g> Buxièresles-Mines,Bourb<strong>on</strong>-l´Archambault basin (Allier, France): Apreliminary report.: Bull. Soc. Géol. France, v. 171, no. 2, p.239-249.Traversa, G., R<strong>on</strong>ca, S., Del Moro, A., Pasquali, C., Buraglini, N.,Simei, S. and Barabino, G., 2001. Late to post-hercynian dykeactivity in <str<strong>on</strong>g>the</str<strong>on</strong>g> Sardinia-Corsica domain: A transiti<strong>on</strong> fromorogenic calc-alkaline to anorogenic alkaline magmatism: Dip.Sci. Terra, Siena Univ, Abstract Volume, p. 67-68.Virgili, C., Cassinis, G. and Broutinm, J., 2001. <strong>Permian</strong> to Triassicsequences and events from selected c<strong>on</strong>tinental areas <str<strong>on</strong>g>of</str<strong>on</strong>g>Southwestern Europe: Dip. Sci. Terra, Siena Univ, AbstractVolume, p. 69-70.Voigt, S., 2001. First occurence <str<strong>on</strong>g>of</str<strong>on</strong>g> fossil freshwater jellyfishes from<str<strong>on</strong>g>the</str<strong>on</strong>g> Tambach sandst<strong>on</strong>e (Lower <strong>Permian</strong>, Thuringia): Dip. Sci.Terra, Siena Univ, Abstract Volume, p. 71.Yanev, S. N., 2001. The Carb<strong>on</strong>iferous System in Bulgaria:stratigraphy, envir<strong>on</strong>ments and paleogeography: Dip. Sci.Terra, Siena Univ, Abstract Volume, p. 72-74.Has your address changed sinceyou last received Permophiles?Please email or send any address changes to:Email:henders<strong>on</strong>@geo.ucalgary.caMailing address:Dr. Charles Henders<strong>on</strong>University <str<strong>on</strong>g>of</str<strong>on</strong>g> CalgaryDepartment <str<strong>on</strong>g>of</str<strong>on</strong>g> Geology and GeophysicsCalgary, AB T2N 1N4 Canada
Some Problems and New Achievements in <str<strong>on</strong>g>the</str<strong>on</strong>g> L<strong>on</strong>gDistance Correlati<strong>on</strong>s <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> C<strong>on</strong>tinental <strong>Permian</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g>PangeaLozovsky V.R.Moscow Geological Prospecting Institute,RussiaAdopti<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> three-fold subdivisi<strong>on</strong> for <str<strong>on</strong>g>the</str<strong>on</strong>g> <strong>Permian</strong> Systemintensifies <str<strong>on</strong>g>the</str<strong>on</strong>g> problems <str<strong>on</strong>g>of</str<strong>on</strong>g> correlati<strong>on</strong> between <str<strong>on</strong>g>the</str<strong>on</strong>g> stages <str<strong>on</strong>g>of</str<strong>on</strong>g>Guadalupian and Lopingian series with <str<strong>on</strong>g>the</str<strong>on</strong>g> traditi<strong>on</strong>al Ufimian ,Kazanian and Tatarian <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> European Russia. The marine fauna<str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> Kazanian allows direct correlati<strong>on</strong>s to be made. Ufimian andTatarian are represented by <str<strong>on</strong>g>the</str<strong>on</strong>g> redbeds with diverse c<strong>on</strong>tinentalbiota. The finding <str<strong>on</strong>g>of</str<strong>on</strong>g> c<strong>on</strong>od<strong>on</strong>ts date <str<strong>on</strong>g>the</str<strong>on</strong>g> Kazanian as <str<strong>on</strong>g>the</str<strong>on</strong>g> UpperRoadian and lowermost Wordian (Kozur et al., 1998), that is a verygood co-ordinate with <str<strong>on</strong>g>the</str<strong>on</strong>g> latest discoveries <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> amm<strong>on</strong>oids.North American and European secti<strong>on</strong>s with interbedded marineand c<strong>on</strong>tinental facies are very important for world-wide <strong>Permian</strong>correlati<strong>on</strong>s. Tetrapod complexes play a primary role. Paleomagneticdata can also be used as an independent and objective c<strong>on</strong>trol.Three distinctive stages in <str<strong>on</strong>g>the</str<strong>on</strong>g> evoluti<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> <strong>Permian</strong> tetrapods(“Edaphosaurid”, “Tapinocephalid” and “Dicynod<strong>on</strong>tid” empires<str<strong>on</strong>g>of</str<strong>on</strong>g> Anders<strong>on</strong> and Cruickshank, 1978) were first defined by Romer(1966) and <str<strong>on</strong>g>the</str<strong>on</strong>g>n well developed by Lucas (1998). The records <str<strong>on</strong>g>of</str<strong>on</strong>g><str<strong>on</strong>g>the</str<strong>on</strong>g> first stage come from <str<strong>on</strong>g>the</str<strong>on</strong>g> Upper Pennsylvanian to Lower <strong>Permian</strong><str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> western USA. Analogous faunas are known fromRotliegend <str<strong>on</strong>g>of</str<strong>on</strong>g> Western Europe, Dolomite Alps and Caucasus.Le<strong>on</strong>ardian tetrapod bearing formati<strong>on</strong>s <str<strong>on</strong>g>of</str<strong>on</strong>g> Ariz<strong>on</strong>a (Lucas andHeckert, 1995) are overlain by <str<strong>on</strong>g>the</str<strong>on</strong>g> Guadalupian Kaibab Limest<strong>on</strong>e.Aquatic Eryopoid supercomplex from Ufimian <str<strong>on</strong>g>of</str<strong>on</strong>g> Timano-Petchorabasin (Ivachnenko et al., 1997) is very close to <str<strong>on</strong>g>the</str<strong>on</strong>g> European Early<strong>Permian</strong>. The Ufimian-Kazanian boundary approximately corresp<strong>on</strong>dsto <str<strong>on</strong>g>the</str<strong>on</strong>g> Le<strong>on</strong>ardian-Guadalupian boundary (Lozovsky,1992). The transiti<strong>on</strong> from <str<strong>on</strong>g>the</str<strong>on</strong>g> first stage to <str<strong>on</strong>g>the</str<strong>on</strong>g> sec<strong>on</strong>d is markedby <str<strong>on</strong>g>the</str<strong>on</strong>g> appearance <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g>rapsids, anomod<strong>on</strong>ts and parareptilians,which coexisted with <str<strong>on</strong>g>the</str<strong>on</strong>g> holdover pelycosaurids,seymouriamorths, captorhinids and temnosp<strong>on</strong>dil amphibians.East European records from <str<strong>on</strong>g>the</str<strong>on</strong>g> Kazanian and Lower Tatarian are<str<strong>on</strong>g>the</str<strong>on</strong>g> more complete, where five tetrapod faunas were distinguished,including <str<strong>on</strong>g>the</str<strong>on</strong>g> Mezen <strong>on</strong>e (Ivachnenko et al., 1997). Recently <str<strong>on</strong>g>the</str<strong>on</strong>g>typical forms <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> Mezen fauna were discovered in <str<strong>on</strong>g>the</str<strong>on</strong>g>Guadalupian Chikasha Formati<strong>on</strong>, in particular Macroleter, a formlike Mesenosaurus, but much bigger, and caseids like Ennatosaurus(written communicati<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> R.R.Reisz, Canada). So not <strong>on</strong>ly are <str<strong>on</strong>g>the</str<strong>on</strong>g>same animals present in North America as in European Russia, butalso similarities in faunal compositi<strong>on</strong> support that <str<strong>on</strong>g>the</str<strong>on</strong>g>y are c<strong>on</strong>temporaneous.The Chikasha Formati<strong>on</strong> is correlated with <str<strong>on</strong>g>the</str<strong>on</strong>g>Wordian. The positi<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> Illawarra / Reversal Megaz<strong>on</strong>es isapproximately near <str<strong>on</strong>g>the</str<strong>on</strong>g> Capitanian-Wordian level (Glenister et al.,1999) and dem<strong>on</strong>strates <str<strong>on</strong>g>the</str<strong>on</strong>g> analogy <str<strong>on</strong>g>of</str<strong>on</strong>g> this paleomagnetic markerin comparis<strong>on</strong> with <str<strong>on</strong>g>the</str<strong>on</strong>g> tetrapod-bearing beds in both c<strong>on</strong>tinents.The absence <str<strong>on</strong>g>of</str<strong>on</strong>g> deinocephalian tetrapods in Western Europe canbe explained by <str<strong>on</strong>g>the</str<strong>on</strong>g> break in sedimentati<strong>on</strong> during <str<strong>on</strong>g>the</str<strong>on</strong>g> Variscanmovements, well proved in Sou<str<strong>on</strong>g>the</str<strong>on</strong>g>rn Alps (Cassinis and Neri ,1999).Permophiles Issue #38 2001REPORTS7The above menti<strong>on</strong>ed facts <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> broad exchange between <str<strong>on</strong>g>the</str<strong>on</strong>g>North American and European faunas refute <str<strong>on</strong>g>the</str<strong>on</strong>g> wide-spread opini<strong>on</strong>about <str<strong>on</strong>g>the</str<strong>on</strong>g> complete isolati<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> North American c<strong>on</strong>tinentfrom <str<strong>on</strong>g>the</str<strong>on</strong>g> European <strong>on</strong>e. The third stage is characterized by <str<strong>on</strong>g>the</str<strong>on</strong>g>widespread distributi<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> herbivorous anomod<strong>on</strong>ts (Dicynod<strong>on</strong>),parareptilians Pareiasaurids, carnivorous <str<strong>on</strong>g>the</str<strong>on</strong>g>riod<strong>on</strong>ts,gorg<strong>on</strong>opsoids and by <str<strong>on</strong>g>the</str<strong>on</strong>g> first appearance <str<strong>on</strong>g>of</str<strong>on</strong>g> archosaurids andcynod<strong>on</strong>ts with some holdover. This fauna characterizes <str<strong>on</strong>g>the</str<strong>on</strong>g> UpperTatarian <str<strong>on</strong>g>of</str<strong>on</strong>g> East Europe, which paleomagnetically corresp<strong>on</strong>dsto <str<strong>on</strong>g>the</str<strong>on</strong>g> Illawarra Megaz<strong>on</strong>e. The close compositi<strong>on</strong> has <str<strong>on</strong>g>the</str<strong>on</strong>g>ichn<str<strong>on</strong>g>of</str<strong>on</strong>g>auna from Val Gardena Formati<strong>on</strong> (Dolomites), where <str<strong>on</strong>g>the</str<strong>on</strong>g>most typical are <str<strong>on</strong>g>the</str<strong>on</strong>g> Pareiasaurs Pachypes dolomiticus andGorg<strong>on</strong>opsians (Ceol<strong>on</strong>i et al., 1986). The overlying Belleroph<strong>on</strong>Formati<strong>on</strong> c<strong>on</strong>tains <str<strong>on</strong>g>the</str<strong>on</strong>g> Changhsingian marine fauna. Last year atrackway <str<strong>on</strong>g>of</str<strong>on</strong>g> large forms, very close to Pachypes, was found byPetukhov S.V in <str<strong>on</strong>g>the</str<strong>on</strong>g> Upper Tatarian <str<strong>on</strong>g>of</str<strong>on</strong>g> European Russia. Someelements <str<strong>on</strong>g>of</str<strong>on</strong>g> this fauna are known from Western Europe. There areno <str<strong>on</strong>g>the</str<strong>on</strong>g> finds <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> Dicynod<strong>on</strong>tid fauna in North America.C<strong>on</strong>clusi<strong>on</strong>sDuring <str<strong>on</strong>g>the</str<strong>on</strong>g> <strong>Permian</strong> period broad exchange between <str<strong>on</strong>g>the</str<strong>on</strong>g> NorthAmerican and European tetrapod communities took place. The tetrapodbiochr<strong>on</strong>ology provides a threefold divisi<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> <strong>Permian</strong>,however <str<strong>on</strong>g>the</str<strong>on</strong>g>ir boundaries do not corresp<strong>on</strong>d with <str<strong>on</strong>g>the</str<strong>on</strong>g> CisUralian,Guadalupian and Lopingian series. The more distinctive changesoccur at <str<strong>on</strong>g>the</str<strong>on</strong>g> Ufimian-Kazanian boundary, which approximately corresp<strong>on</strong>dsto <str<strong>on</strong>g>the</str<strong>on</strong>g> Le<strong>on</strong>ardian-Guadalupian <str<strong>on</strong>g>of</str<strong>on</strong>g> North America. Thecurrent Guadalupian-Lopingian boundary is clearly younger thanLower-Upper Tatarian <strong>on</strong>e, where <str<strong>on</strong>g>the</str<strong>on</strong>g> transiti<strong>on</strong> between“Tapinocephalid” and “Dicynod<strong>on</strong>tid” empires and <str<strong>on</strong>g>the</str<strong>on</strong>g> Illawarra/Reversal Megaz<strong>on</strong>e are registered.ReferencesAnders<strong>on</strong>, J. M., Cruickshank, A. R.,1978. The biostratigraphy <str<strong>on</strong>g>of</str<strong>on</strong>g><str<strong>on</strong>g>the</str<strong>on</strong>g> <strong>Permian</strong> and <str<strong>on</strong>g>the</str<strong>on</strong>g> Triassic, Part 5: A review <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g>classsificati<strong>on</strong> and distributi<strong>on</strong> <str<strong>on</strong>g>of</str<strong>on</strong>g> Permo-Triassic tetrapods:Palae<strong>on</strong>tologica Africana, v. 21, p. 15-44.Cassinis, G., Neri, C., 1999. Outline <str<strong>on</strong>g>of</str<strong>on</strong>g> <strong>Permian</strong> <strong>Stratigraphy</strong> in <str<strong>on</strong>g>the</str<strong>on</strong>g>Sou<str<strong>on</strong>g>the</str<strong>on</strong>g>rn Alps. <strong>Stratigraphy</strong> and facies <str<strong>on</strong>g>of</str<strong>on</strong>g> <str<strong>on</strong>g>the</str<strong>on</strong>g> <strong>Permian</strong>deposits between Eastern Lombardy and <str<strong>on</strong>g>the</str<strong>on</strong>g> WesternDolomites: Field Trip Guidebook, September 23-25, 1999. EarthSciences Department, Pavia Univ., p. 7-10.Ceol<strong>on</strong>i, P. C., C<strong>on</strong>ti, M. A., Mariotti, N., Nicosia, U., 1986. NewLate <strong>Permian</strong> tetrapod footprints from Sou<str<strong>on</strong>g>the</str<strong>on</strong>g>rn Alps:Mem.Soc.Geol.It.,v. 34, p. 45-65.Glenister, B. F., Wardlaw, B. R., Lambert, L. L., Spinosa, C.,Bowring, S. A, Erwin, D. H., Menning, M., Wilde, G. L., 1999.Proposal <str<strong>on</strong>g>of</str<strong>on</strong>g> Guadalupian and comp<strong>on</strong>ent Roadian, Wordianand Capitanian stages as Internati<strong>on</strong>al Standards for Middle<strong>Permian</strong>: Permophiles, no. 34, p. 3-11.Ivakhnenko, M. F., Golubev, V. K., Gubin, Yu. M., Kalandadze, N.N., Novikov, I.V., Sennikov, A. G., Rautian A. S., 1997. <strong>Permian</strong>and Triassic tetrapods <str<strong>on</strong>g>of</str<strong>on</strong>g> Eastern Europe: Moscow, Ed. GEOS,216 pp.
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