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Wyświetlanie 1-7 z 7
Tytuł:
Gąbki wapienne Elasmostoma lomes W. Mliller, 1984, z dolnego kimerydu Karsów koło Korytnicy, ich ekofenotypia i tafonomia
Behavioural palaeobiology and taphonomy of the Late Jurassie calcareous sponge Elasmostoma fomes W. Muller, 1984
Autorzy:
Radwański, A.
Powiązania:
https://bibliotekanauki.pl/articles/2077310.pdf
Data publikacji:
2005
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Calcispongea
phenotype
eco-taphonomy
Kimmeridgian
Karsy
Małogoszcz
Polska
fenotyp
ekotafonomia
Polska
Opis:
Calcareous sponges Elastostoma !'omes W MUller, 1984, from the Lower Kimmeridgian marly onkolitic limestones exposed at Karsy in the Holy Cross Mountains, Central Poland, are studied in terms of their settlement, growth, behaviour, and resulting phenotypy. The lichen-shaped auriculate specimens are interpreted as growing upwardly, at a higher angle to the bottom surface, in order to involve passive flow carrying suspended nutrients up on which they fed. Unstable bottom and hydrodynamie conditions, under which the growth of sponges progressed, we re basic prerequisites that controlled ecophenotypic variability of the studied specimens, A peculiar case of regeneration is discussed, to postulaie the skeleton parts having been lithified during the sponge's life, and healed after an accidental injury. Aviolent event that caused catastrophic burial of the studied sponge assemblage is ascribed to high-energy agents, most likely of storm origin.
Źródło:
Volumina Jurassica; 2005, 3, 1; 109--121
1896-7876
1731-3708
Pojawia się w:
Volumina Jurassica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
A contribution to the knowledge of Miocene Elasmobranchii from Pinczow (Poland)
Przyczynek do znajomości mioceńskich spodoustych (Elasmobranchii) z Pińczowa
K voprosu o znanii miocenovykh elasmobrankhijj iz Pin'chova (Pol'sha)
Autorzy:
Radwanski, A.
Powiązania:
https://bibliotekanauki.pl/articles/20868.pdf
Data publikacji:
1965
Wydawca:
Polska Akademia Nauk. Instytut Paleobiologii PAN
Tematy:
contribution
knowledge
paleontology
remains
Lower Tortonian
Tortonian
fish
elasmobranch fish
Miocene
Elasmobranchii
Pinczow town
Polska
Źródło:
Acta Palaeontologica Polonica; 1965, 10, 2
0567-7920
Pojawia się w:
Acta Palaeontologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Upper Cambrian trilobite ichnocoenosis from Wielka Wisniowka (Holy Cross Mountains, Poland)
Górnokambryjska ichnocenoza trylobitowa z Wielkiej Wiśniówki w Górach Świetokrzyskich
Verkhne-kembrijjskijj trilobitovyjj ikhnocenoz iz Vel'kojj Vis'njuvki v Sventokrzhiskikh Gorakh (Pol'sha)
Autorzy:
Radwanski, A.
Roniewicz, P.
Powiązania:
https://bibliotekanauki.pl/articles/21862.pdf
Data publikacji:
1963
Wydawca:
Polska Akademia Nauk. Instytut Paleobiologii PAN
Tematy:
paleontology
Cambrian
Upper Cambrian
trilobite
ichnocoenosis
fauna community
deposit
Wisniowka Wielka village
Holy Cross Mountains
Polska
Źródło:
Acta Palaeontologica Polonica; 1963, 08, 2
0567-7920
Pojawia się w:
Acta Palaeontologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Chore i okaleczone zwierzęta jako ofiary pasożytów i drapieżców w jurze Polski - przegląd stanu wiedzy
Disease and trauma in Jurassic invertebrate animals of Poland – an updated review
Autorzy:
Radwańska, U.
Radwański, A.
Powiązania:
https://bibliotekanauki.pl/articles/2077301.pdf
Data publikacji:
2004
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
paleopatologia
pasożyty
drapieżniki
jura
Polska
palaeopathology
parasites
predators
Jurassic
Polska
Opis:
The parasitism of, and predation upon, the diverse Middle and Late Jurassic invertebrates of Poland, personally recognised by the authors, are reviewed. All cases are discussed either in the biological (anatomical, ethological), or ecological terms, to show the mode of infection, or injury, and the relationship between the engaged taxa. The preys to parasites are exemplified by the prosopid crabs infested by bopyrid isopods, the crinoids infested by myzostomid polychaetes (both disk-shaped, and wormlike), and the echinoids attacked by copepod arthropods involving either swellings of spines, or gall-shaped cysts upon the test outerly. Of traumatic events, discussed is regeneration of injuries in the belemnite hooked guards, and in the ammonite shells of distorted ribbing. The pearl-like structures in belemnite guards (the “belemnite pearls”) are interpreted as caused by a tiny parasite encapsulated during further growth of the belemnite. Heaps of ammonite shell hash are thought to represent the ,“kitchen middens” of a larger predator which has feasted upon the fleshy tidbits alone, the beaten shell having been left. The post mortem damage of shells is remarked (taphonomic feedback and/or aftermath) to be distinguished from that one acted in shells of alive specimens of the Middle and Late Jurassic of Poland.
Źródło:
Volumina Jurassica; 2004, 2, 1; 99-112
1896-7876
1731-3708
Pojawia się w:
Volumina Jurassica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Kolonie korali z muszlowców ostrygowych i oolitów dolnego kimerydu Małogoszcza
Coral lumps in Early Kimmeridgian oyster shellbeds and oolites ot Małogoszcz
Autorzy:
Radwański, A.
Roniewicz, E.
Powiązania:
https://bibliotekanauki.pl/articles/2077312.pdf
Data publikacji:
2005
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Scleractinian corals
oyster shellbed
eco-taphonomy
environment
Kimmeridgian
Małogoszcz
Polska
koralowce Scleractinia
muszlowiec ostrygowy
ekotafonomia
środowisko
Polska
Opis:
Scleractinian corals occurring scarcely in the Lower Kimmeridgian Actinostl'eon (=Lopha, =Alectryonia) shellbeds at Malogoszcz in the Holy Cross Mountains, Central Poland, are represented by abraded colonies densely riddled by rock-boring bivalves (Lithophaga inclusa Phillips, GastTOchaena sp.) and polychaetes (potamilla sp.). The taxonomically recognised specimens include C01nplexastrea bUJ'gundiae (de Blainville, 1830), D 'imorphocoenia sp., Ovalastrea caryophylloides (Goldfuss, 1826), and Thamnasteria graeilis (Miinster, 1826). AlI colonies are preserved in the form of hollows, the wall s of which bear moulds of coral calyces, and of bivalve and polychaete borings. Taking into account the structural features of shellbeds and their faunistic content (uprooted crinoids Apioerinites, dug-out deeply-infaunal bivalves), stormy agitation is postulated as a basic agent responsible for damaging AeUnostreon communities, and their associates. The studied corals are thought to have lived aside the Aetinostreon gardens, up on a muddy bottom, from where they have been stirred-up during the storm cataclysm, having been then abraded and riddled by rock-borers repeatedly until laid down in a shellbed and transferred in to the fossil record. The extremely shallow-water conditions, under which the ostreid Actinostreon has lived, suggest the typically opportunistic nature or the associated corals, the same as of Ovalastrea caryophylloides (Goldfuss, 1826) from oolitic shoals, and the only colony of which completes the coral assemblage of Malogoszcz. The opportunism or ali these corals differs them from the habit of hermatypie forms from coeval and Oxfordian patch-reef communities of the Holy Cross Mountains (ef. Roniewicz & Roniewicz 1968, 1971).
Źródło:
Volumina Jurassica; 2005, 3, 1; 97--107
1896-7876
1731-3708
Pojawia się w:
Volumina Jurassica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
The Middle Miocene of the Fore-Carpathian Basin (Poland, Ukraine and Moldova)
Autorzy:
Wysocka, A.
Radwański, A.
Górka, M.
Bąbel, M.
Radwańska, U.
Złotnik, M.
Powiązania:
https://bibliotekanauki.pl/articles/138689.pdf
Data publikacji:
2016
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Lithofacies
fossil assemblages
Middle Miocene
Fore-Carpathian Basin
Polska
Ukraine
Litofacje
miocen
zbiornik przedkarpacki
Polska
Ukraina
Opis:
Studies of Miocene sediments in the Fore-Carpathian Basin, conducted by geologists from the University of Warsaw have provided new insights on the distribution of the facies infilling the basin, particularly in the forebulge and back-bulge zones. The origin of the large-scale sand bodies, evaporitic deposits and large-scale organic buildups is discussed, described and verified. These deposits originated in variable, shallow marine settings, differing in their water chemistry and the dynamics of sedimentary processes, and are unique with regard to the fossil assemblages they yield. Many years of taxonomic, biostratigraphic, palaeoecologic and ecotaphonomic investigations have resulted in the identification of the fossil assemblages of these sediments, their age, sedimentary settings and post-mortem conditions. Detailed studies were focused on corals, polychaetes, most classes of molluscs, crustaceans, echinoderms, and fishes.
Źródło:
Acta Geologica Polonica; 2016, 66, 3; 351-401
0001-5709
Pojawia się w:
Acta Geologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Campanian and Maastrichtian mosasaurid reptiles from central Poland
Autorzy:
Machalski, M
Jagt, J.W.M.
Dortangs, R.W.
Mulder, E.W.A.
Radwanski, A.
Powiązania:
https://bibliotekanauki.pl/articles/21053.pdf
Data publikacji:
2003
Wydawca:
Polska Akademia Nauk. Instytut Paleobiologii PAN
Tematy:
Reptilia
Polska
Cretaceous
food chain
Platynota
marine lizard
Squamata
mosasaurid reptile
reptile
fossil
Upper Cretaceous
Mosasauridae
lizard
paleontology
Opis:
Isolated marginal teeth and tooth crowns of Late Campanian and Late Maastrichtian mosasaurid reptiles (Squamata, Platynota) from the Wisła River valley area, central Poland, are described and illustrated. These comprise two Late Campanian taxa from Piotrawin quarry: Prognathodon sp. and Plioplatecarpinae sp. A., and four late Late Maastrichtian taxa from Nasiłów quarry: Mosasaurus cf. hoffmanni Mantell, 1829, M. cf. lemonnieri Dollo, 1889c, “Mosasaurus (Leiodon) cfr. anceps” sensu Arambourg (1952), and Plioplatecarpinae sp. B. In addition, the previously described fragmentary jaw with associated teeth of the Late Campanian age from Maruszów quarry (west of the Wisła River area), is reassigned to Mosasaurus cf. hoffmanni. This specimen suggests that M. hoffmanni or a closely related (ancestral?) species already appeared in Europe during the Late Campanian (well−documented European occurrences of M. hoffmanni are Late Maastrichtian in age). At least part of the described mosasaur material is likely to stem from periodic feeding in the area (broken−off or shed tooth crowns) or from floating carcasses (complete teeth and jaw fragments).
Źródło:
Acta Palaeontologica Polonica; 2003, 48, 3
0567-7920
Pojawia się w:
Acta Palaeontologica Polonica
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-7 z 7

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