Zobrazeno 1 - 10
of 79
pro vyhledávání: '"PIOTR SZREK"'
Publikováno v:
Estonian Journal of Earth Sciences, Vol 73, Iss 1, Pp 1-14 (2024)
New studies on Frasnian ptyctodonts, including the revision of historic material in addition to the description of new material, have resulted in the detailed description of two species of Ptyctodus (Ptyctodus obliquus, Ptyctodus kielcensis), eight i
Externí odkaz:
https://doaj.org/article/b661d2a5f12743f5b916de24960379fd
Autor:
Melina Jobbins, Martin Rücklin, Marcelo R. Sánchez Villagra, Hervé Lelièvre, Eileen Grogan, Piotr Szrek, Christian Klug
Publikováno v:
Royal Society Open Science, Vol 11, Iss 1 (2024)
Jaws are a key vertebrate feature that arose early in our evolution. Placoderms are among the first jawed vertebrates; their fossils yield essential knowledge about the early diversification of gnathostome feeding strategies, diets and modularity. Mo
Externí odkaz:
https://doaj.org/article/6a7dc0567b1142e4a8f1c999d60a395c
Publikováno v:
Acta Palaeontologica Polonica, Vol 66, Iss 2, Pp 337-347 (2021)
Externí odkaz:
https://doaj.org/article/39053bd6d84e4793aa2b32e110e18d85
Autor:
Piotr Szrek, Olga Wilk
Publikováno v:
Estonian Journal of Earth Sciences, Vol 67, Iss 1, Pp 33-42 (2018)
The arthrodire placoderm, Dunkleosteus sp., is reported from the Upper Devonian (Frasnian) of the Holy Cross Mountains, Poland. The material comprises partially preserved remains of two individuals found in the Kellwasser-like horizon of the Płucki
Externí odkaz:
https://doaj.org/article/f66919c93563447a8be15d0f793befbf
Autor:
Piotr Szrek, Vincent Dupret
Publikováno v:
Acta Palaeontologica Polonica, Vol 62, Iss 4, Pp 789-800 (2017)
The siliciclastic sequence of the Lower Devonian of the southern part of the Holy Cross Mountains in Poland is renown for abundant vertebrate fossils, including ostracoderm, sarcopterygian, acanthodian, chondrichthyan, and placoderm remains. Study of
Externí odkaz:
https://doaj.org/article/8f53f1a341064abeba99c8f39396a3cc
Publikováno v:
Estonian Journal of Earth Sciences, Vol 64, Iss 1, Pp 95-98 (2015)
The depositional environment of the Lower Devonian of the Holy Cross Mountains has only been studied and interpreted in part, particularly for the lower portion of the profile. Recent fieldwork findings suggest a considerable change with regard to ea
Externí odkaz:
https://doaj.org/article/b9c5baff846f4007b19208f536ab0cf9
Publikováno v:
Geological Quarterly.
Among the hundreds of collected Devonian vertebrate macrofossils in the Holy Cross Mountains, placoderms dominate and provide data on their morphology, distribution and taphonomy. So far 17 out of more than 500 studied specimens have revealed bones w
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e3686a651ab2ac2f66ace6cc24f2a6e1
https://doi.org/10.1101/2021.07.23.453559
https://doi.org/10.1101/2021.07.23.453559
Publikováno v:
Geological Magazine. 157:119-133
The age of granophyric diorite from the Sosnowiec IG-1 borehole (Brunovistulia Terrane) was studied by means of U–Pb single-grain zircon analysis performed on a SHRIMP (sensitive high-resolution ion microprobe) IIe device. The isotope ages and prov
Publikováno v:
Journal of Vertebrate Paleontology. 41
The remains of Late Devonian placoderms from the Holy Cross Mountains area have already been established and widely recognized thanks to the diligent studies of Gorizdro-Kulczycka (1934) and Kulczy...