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Środkowotriasowa ichnofauna kręgowców z "warstw z Krynek" w Górach Świętokrzyskich : wstępny przegląd

Niedźwiedzki G., Kin A., Remin Z., Małkiewicz M.

Przegląd Geologiczny

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2007

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Vol. 55, nr 10

870-879

EN

Numerous specimens of vertebrate tracks were discovered in the uppermost Röt (uppermost Buntsandstein) deposits of "Krynki Beds" that crop out at Witulin, Parszów, Małe Jodło, Jarugi, Bliżyn, and Sorbin in the north-eastern and central margin of the Holy Cross Mountains, Poland. The following vertebrate ichnotaxa were identified in these localities: Chirotherium barthii Kaup, 1835; Chirotherium cf. sickleri; Synaptichnium cf. diabloense; Isochirotherium herculis (Egerton, 1839); ? Isochirotherium cf. herculis; Isochirotherium isp.; Chirotheriidae indet.; Rhynchosauroides isp., and Rhynchosauroidae indet. The ichnoassemblage from the "Krynki Beds" is very similar to ichnoassociations which are known from: 1) latest Early and early Middle Triassic (Upper Buntsandstein) deposits of the Central European Basin, 2) latest Early and early Middle Triassic Moenkopi Formation of USA, 3) Middle Triassic deposits of United Kingdom, France and Italy.

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Nowe stanowisko z tropami kręgowców z górnego pstrego piaskowca Gór Świętokrzyskich

Kuleta M., Niedźwiedzki G., Ptaszyński T.

Przegląd Geologiczny

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2005

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Vol. 53, nr 2

151--155

EN

Vertebrate footprints are abundant in the Buntsandstein of the Holy Cross Mountains (central Poland) and have been documented in numer-ous publications. A new site vertebrate trackside has been discovered in near Suchedniów. Chirotheriidae (Synaptichnium sp., Chirotherium barthii, and Brachychirotherium sp.), Rhynchosauroidae (Rhynchosauroides sp.), and probably amphibian footprints (cf. Capitosauroides sp.) are reported from the lower part of the Upper Buntsandstein Baranów Formation (complex of different fluvial deposits) exposed at Kopulak quarry. Differentiated invertebrate ichnofossils (Cruziana problematica, Scoyenia sp., Palaeophycus sp., Skolithos sp., Lockeia sp., and cf. Gordia sp.) and plant remains have been also found in this site. Three types of vertebrate subaqueous traces (footprints of swimming animals) are identified: (1) swim traces - structures preserved as digits or claws scratches; (2) partially preserved pes or manus imprints; (3) other enigmatic traces -referred to as “problematic forms”.

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New finds of vertebrate footprints from the Lower Permian of Wambierzyce, Poland

Ptaszyński T., Niedźwiedzki G.

Geological Quarterly

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2004

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Vol. 48, No 2

199--202

EN

New specimens of vertebrate footprints are reported from the Early Permian deposits in Poland. Footprints discovered in a well-known Early Permian Rotliegend tracksite at Wambierzyce (old German name Albendorf) represent ichnites of Hyloidichnus arnhardti Haubold, 1973.

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Tropy kręgowców z piaskowca tumlińskiego Góry Grodowej - Góry Świętokrzyskie

Ptaszyński T.

Przegląd Geologiczny

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2000

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Vol. 48, nr 5

418-421

PL

W utworach międzywydmowych piaskowców tumlińskich pstrego piaskowca, w kamieniołomie na Górze Grodowej, znaleziono bogaty zespół tropów kręgowców. Oznaczone dotychczas ichnotaksony: Amphisauropus cf. latus, Rhynchosauroides cf. pallini, Varanopus cf microdactylus, Palmichnus sp., Chelichnus ? sp., "Proterosuchia indet. " były dotychczas znane z utworów permu Europy i Ameryki Północnej. Zespół ten, niewiele starszy od zespołu tropów kręgowców z warstw łabiryntodontowych z Wiór koło Ostrowca Świętokrzyskiego zawierającego typową dla triasu ichnofaunę wskazuje, że wyraźna zmiana zespołu ichnofauny kręgowców w pobliżu granicy permu i triasu nastąpiła w Górach Świętokrzyskich dopiero we wczesnym triasie.

EN

Rich vertebrate track assemblage has been found in the interdune deposits of Tumlin sandstone of the Buntsandstein at the quarry of Grodowa Hill. The ichnotaxa which have been hitherto designated as Amphisauropus cf. latus, Rhynchosauroides cf. pallini Varanopus cf. microdactylus, Palmichnus sp., Chelichnus ? sp., "Proterosuchia indet. " have been hitherto known from the Permian of Europe and North America. This assemblage as only somewhat older than the vertebrate footprint assemblage from Labyrinthodontidae Beds from Wióry near the town of Ostrowiec Świętokrzyski containing typical Triassic ichnogenera representafives shows, that a distinct change of terrestrial vertebrate ichnofauna near the Permian/Triassic boundary occurred in the Holy Cross Mts. area in the Early Triassic time.