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    Wyświetlanie 1-14 z 14
    Tytuł:
    Scleractinian corals of suborders Pachythecaliina and Rhipidogyrina: discussion on similar ities and description of species from Štramberk-type limestones, Polish Outer Carpathians
    Autorzy:
    Kołodziej, B.
    Powiązania:
    https://bibliotekanauki.pl/articles/191510.pdf
    Data publikacji:
    2003
    Wydawca:
    Polskie Towarzystwo Geologiczne
    Tematy:
    corals
    Pachythecaliina
    Rhipidogyrina
    taxonomy
    phylogeny
    Jurassic
    Cretaceous
    Outer Carpathians
    Opis:
    Similarities between scleractinian corals from extinct suborders Pachythecaliina Eliášová 1976 and Rhipidogyrina Roniewicz 1976 are discussed. Corals of the former suborder are considered by some authors as possible descendants of Palaeozoic Rugosa because of their unusual skeletal characters. Some rhipidogyrinans, especially the family Aulastraeoporidae, despite their different septal microstructure, share more common features with pachythecaliinans than with other scleractinians. The following skeletal features are discussed to show similarities between these two suborders: (1) wall microstructure and its relations to septa, (2) corallite bilateral symmetry, (3) marginarium, (4) lonsdaleoid and apophysal septa, and (5) internal septal margin. These similarities can be explained by convergence, although phylogenetic relationships of both suborders can not be excluded. This hypothesis needs to be verified by more studies, especially on early blastogeny of rhipidogyrinans and wall microstructure of pachythecaliinans. The systematic part gives descriptions of the discussed coral suborders occuring in the Štramberk-type limestones, the Polish Outer Carpathians (Tithonian-?Berriasian, ?Valanginian). Similarly as in the Štramberk Limestone (Moravia), pachythecaliinans are highly diversified (17 species, 12 genera, including Pachythecophyllia eliasovae n.gen., n.sp.). Rhipidogyrinans are represented by 4 species of 4 genera, including ?Ogilvinella morycowae n.sp.
    Źródło:
    Annales Societatis Geologorum Poloniae; 2003, 73, No 3; 193-217
    0208-9068
    Pojawia się w:
    Annales Societatis Geologorum Poloniae
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Jurajskie korale w Polsce
    Jurassic corals in Poland
    Autorzy:
    Roniewicz, E.
    Powiązania:
    https://bibliotekanauki.pl/articles/2077293.pdf
    Data publikacji:
    2004
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    jura
    facja korali
    środowisko
    skleraktinie
    korale
    Jurassic
    scleractinian corals
    environment
    coral facies
    Opis:
    In the epicontinental Jurassic of Poland, scleractinian corals appeared in the Bathonian, but only in the Middle Oxfordian-Lower Kimmeridgian became a significant element of the shallow-water fauna. Over the whole area, Upper Jurassic coral facies are situated above the Oxfordian sponge megafacies. Middle Oxfordian Jurassic corals are the best known from the NE margin of the Holy Cross Mts and represented chiefly by lamellate colonies. The Upper Oxfordian and Kimmeridgian coral facies extends from the Pomerania, through central Poland to the fore-Carpathian region. Taxonomical and morphotypical coral diversifications of the Upper Oxfordian and Kimmeridian were higher than that of the Middle Oxfordian. In the Tethyan region, corals are known from the exotic pebbles of the Stramberk-type Tithonian limestones in the Carpathian Flysh and Pieniny Klippen Belt. The arguments against the interpretation of epicontinental coral accumulations as reefs, are as follows: abundance of lamellate corals and epithecate phaceloid taxa (the latter incapable to repair skeletal damages), high taxonomical diversification and frequency of corals with menianes representing presumable adaptations to filtering mode of nutrition, comparable rate of growth of coral constructions and of accumulation of surrounding sediment, association of corals characterized above with soft bottom and turbid water.
    Źródło:
    Volumina Jurassica; 2004, 2, 1; 83-98
    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:
    Actinaraeopsis ventosiana, a new scleractinian species from the Lower Cretaceous of Provence (SE France)
    Nowy gatunek koralowca sześciopromiennego (scleractinia) z wczesnej kredy Prowansji (Se Francja)
    Autorzy:
    Morycowa, E.
    Masse, J.P.
    Powiązania:
    https://bibliotekanauki.pl/articles/191716.pdf
    Data publikacji:
    2007
    Wydawca:
    Polskie Towarzystwo Geologiczne
    Tematy:
    Scleractinian corals
    Haplaraeidae
    Actinaraeopsis ventosiana sp. nov.
    Lower Cretaceous
    France
    Opis:
    Actinaraeopsis ventosiana is a new scleractinian coral species from the Lower Cretaceous shallow- water limestones of the Mont Ventoux (Provence, SE France). To date only two Late Jurassic species of this genus have been known, i.e. Actinaraeopsis araneola Roniewicz and A. exilis Roniewicz. The new species shows some similarity to the Jurassic species A. araneola, but differs in microstructure details and morphometric parameters.
    W pracy opisano nowy gatunek koralowca kolonijnego Actinaraeopsis ventosiana, pochodzącego z płytkowodnych wapieni górnobarremskich Prowansji (SE Francja). Dotychczas tylko dwa gatunki tego rodzaju są znane z jury górnej, A. araneola Roniewicz i A. exilis Roniewicz. Nowy gatunek Actinaraeopsis ventosiana wykazuje pewne podobieństwo do jurajskiego gatunku A. araneola, ale różni się od niego parametrami morfometrycznymi i szczegółami budowy mikrostrukturalnej szkieletu.
    Źródło:
    Annales Societatis Geologorum Poloniae; 2007, 77, No 2; 141-145
    0208-9068
    Pojawia się w:
    Annales Societatis Geologorum Poloniae
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Corals from the Stramberk Limestone (Silesian Unit, Outer Western Carpathians, Czech Republic
    Autorzy:
    Eliasova, H.
    Powiązania:
    https://bibliotekanauki.pl/articles/184029.pdf
    Data publikacji:
    2008
    Wydawca:
    Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
    Tematy:
    koralowce
    Karpaty Zachodnie
    Karpaty zewnętrzne
    corals
    Outer Western Carpathians
    Stramberk Limestone
    Scleractinian corals
    Late Tithonian/Early Berriasian
    Opis:
    The submitted contribution informs about the present-day situation of the coral fauna occurring in the Stramberk Limestone at the Kotouc Quarry near Stramberk. 120 determined species belong to 50 genera that pertain to 7 suborders of order Scleractinia
    Źródło:
    Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie; 2008, 34, 3/1; 151-160
    0138-0974
    Pojawia się w:
    Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Koralowce Scleractinia z wapieni egzotykowych typu sztramberskiego polskich Karpat zewnętrznych
    Autorzy:
    Morycowa, E.
    Powiązania:
    https://bibliotekanauki.pl/articles/184037.pdf
    Data publikacji:
    2008
    Wydawca:
    Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
    Tematy:
    koralowce Scleractinia
    Karpaty zewnętrzne
    Scleractinian corals
    Outer Carpathians
    Źródło:
    Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie; 2008, 34, 3/1; 129-137
    0138-0974
    Pojawia się w:
    Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Rozwój faun koralowych od późnego kimerydu do walanżynu na N obrzeżeniu Tetydy: przykład Karpat zewnętrznych i SW Platformy Mezyjskiej
    Autorzy:
    Roniewicz, E.
    Powiązania:
    https://bibliotekanauki.pl/articles/183431.pdf
    Data publikacji:
    2008
    Wydawca:
    Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
    Tematy:
    facje koralowe
    corals clasts
    Źródło:
    Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie; 2008, 34, 3/1; 204-205
    0138-0974
    Pojawia się w:
    Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Lower Cretaceous Microsolenina (Scleractinia) from Provence (southern France)
    Autorzy:
    Morycowa, E.
    Masse, J. P.
    Powiązania:
    https://bibliotekanauki.pl/articles/191507.pdf
    Data publikacji:
    2009
    Wydawca:
    Polskie Towarzystwo Geologiczne
    Tematy:
    Scleractinian corals
    Microsolenina
    Barremian-Lower Aptian
    Provence
    SE France
    Opis:
    In the Lower Cretaceous (Urgonian) limestones of the Provence region (South France) shallow-water scleractinian corals are very common. This paper concentrates on corals from the suborder Microsolenina. They represent 34 taxa (including 5 new species) belonging to 14 genera from two families: Microsolenidae and Latomeandridae. This coral assemblage is representative for the late Early Cretaceous Tethyan realm but also shows some endemism. Its characteristic feature is the abundance of hydnophoroid specimens from the genus Hydnophoromeandraraea Morycowa. The Barremian–Early Aptian age of the studied corals is based on forami- nifera (mainly orbitolinids), dasycladale algae and rudists, and agrees with that of the whole studied coral fauna.
    Źródło:
    Annales Societatis Geologorum Poloniae; 2009, 79, No 2; 97-140
    0208-9068
    Pojawia się w:
    Annales Societatis Geologorum Poloniae
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Corals from the Tithonian carbonate complex in the Dąbrowa Tarnowska–Szczucin area (Polish Carpathian Foreland)
    Autorzy:
    Morycowa, E.
    Powiązania:
    https://bibliotekanauki.pl/articles/191286.pdf
    Data publikacji:
    2012
    Wydawca:
    Polskie Towarzystwo Geologiczne
    Tematy:
    Scleractinian corals
    carbonate platform
    Tithonian
    Carpathian Foreland
    Polska
    Opis:
    The studied corals have been collected from cores of boreholes located in the central part of the Polish Carpathian Foreland in the Dąbrowa Tarnowska–Szczucin area. The Jurassic complex in this area presents a continuous stratigraphic section from the Upper Callovian to Tithonian, locally passing to the Lower Cretaceous (Berriasian). Its thickness exceeds 1,100 m in this area. This complex is composed of marine, mainly shallow-water deposits. The corals occur within the upper part of the Upper Jurassic (Tithonian) deposits, almost entirely within the Swarzów Limestone Formation (= coral-algal limestone formation). This occurrence marks the northernmost extent of Tithonian shallow-water corals in Poland and one of the northernmost in Europe. 42 coral species (among them 14 in open nomenclature) were identified in deposits of this formation. They include two new species: Complexastrea magna and Complexastrea dabroviensis. All taxa, except one, belong to the order Scleractinia. The described assemblage displays a Late Jurassic character. The broader stratigraphic span is assigned to some species, which are quoted from the Middle Jurassic and some species lasted until the Early Cretaceous, Berriasian and/or Valanginian.
    Źródło:
    Annales Societatis Geologorum Poloniae; 2012, 82, 1; 1--38
    0208-9068
    Pojawia się w:
    Annales Societatis Geologorum Poloniae
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Prolific development of pachythecaliines in Late Barremian, Bulgaria: coral taxonomy and sedimentary environment
    Autorzy:
    Kołodziej, B.
    Ivanov, M.
    Idakieva, V.
    Powiązania:
    https://bibliotekanauki.pl/articles/191755.pdf
    Data publikacji:
    2012
    Wydawca:
    Polskie Towarzystwo Geologiczne
    Tematy:
    corals
    taxonomy
    carbonate platform
    palaeoecology
    Cretaceous
    Fore-Balkan
    Bulgaria
    Opis:
    Diversified and abundant corals of the suborder Pachythecaliina (order Hexanthiniaria) are described from Upper Barremian, biostromal reefs of the Emen Formation, Lovech Urgonian Group, north central Bulgaria. The corals are mostly of the phaceloid growth form and represent 14 species (six new), 12 genera (three new), belonging to five families. Pachythecaliines occur with the small, monopleurid cylindrical rudist Mathesia darderi. The rudists frequently are densely clustered, occur between coral branches or are in contact with them. Other corals, with the exception of the phaceloid Calamophylliopsis, and other rudists, are rare. Non-laminated microbialite crusts provided additional, structural support for bioconstruction development. Microbialites (automicrites) can be interpreted as a product of microbial activity, or alternatively, as a result of carbonate precipitation, brought about by non-living organic substrates (organomineralization s.s.). In addition to microbialites, metazoans are encrusted by heterotrophic skeletal microorganisms, while photophilic and oligotrophic microencrusters, usually common in other coral-bearing limestones of the Emen Formation, are very rare. The section at the Rusalya Quarry (NW of Veliko Tarnovo), about 42 m thick, provides the sedimentary and environmental context for the reefal biostromes. The vertical biotic and sedimentary succession displays a general shallowing trend: from the outer carbonate platform with bioclastic limestones containing small boundstone patches (corals, but not pachythecaliines, Lithocodium aggregatum), to the inner platform with rudist biostromes. The pachythecaliine-rich biostromes, 2.5 m thick, were developed in a low-energy environment, referred to the distal part of the rudist-dominated area of the platform. The development of microbialites was facilitated by a low sedimentation rate, and possibly by increased nutrient level. Only poorly diversified and non-phaceloid pachythecaliines occur in other coral-rich limestones and marls of the Urgonian complex in Bulgaria. The assemblage described is the most remarkable, Early Cretaceous coral community worldwide, with regard to pachythecaliines. Phaceloid pachythecaliines are only more common in the Upper Jurassic rocks, being particularly diversified in the Tithonian–Lower Berriasian Štramberk Limestone (Czech Republic) and its equivalent in the Polish Outer Carpathians. However, their sedimentary context differs from that described for the corals of the Emen Formation.
    Źródło:
    Annales Societatis Geologorum Poloniae; 2012, 82, 4; 291--330
    0208-9068
    Pojawia się w:
    Annales Societatis Geologorum Poloniae
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    The oldest species of ?Yavorskia (Tabulata) from the Upper Famennian of the Holy Cross Mountains (Poland)
    Autorzy:
    Zapalski, M.
    Berkowski, B.
    Powiązania:
    https://bibliotekanauki.pl/articles/138864.pdf
    Data publikacji:
    2012
    Wydawca:
    Polska Akademia Nauk. Czytelnia Czasopism PAN
    Tematy:
    famen
    Góry Świętokrzyskie
    korale
    migracje
    Tabulata
    corals
    Famennian
    Holy Cross Mountains
    migrations
    Opis:
    A single perfectly preserved colony of a tabulate coral assigned tentatively to the genus Yavorskia Fomitchev, 1931, collected from Upper Famennian beds (Palmatolepis expansa conodont Zone) in a trench located north of the Kowala Quarry (Holy Cross Mts., central Poland) is here described as a new species, ?Y. paszkowskii sp. nov. It differs from other representatives of the genus in the lack of dissepimental structures and in smaller corallite diameters, and may therefore represent the ancestral taxon of this typically early Carboniferous genus. Yavorskia tabulates were apparently migrating eastwards along the southern margin of Laurussia and farther east and north towards Siberia, as they appear in the Famennian in Europe and in the early Carboniferous in the Altaides. Such a conclusion is consistent with previous observations on Early.Middle Devonian pleurodictyform tabulate distribution.
    Źródło:
    Acta Geologica Polonica; 2012, 62, 2; 197-204
    0001-5709
    Pojawia się w:
    Acta Geologica Polonica
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Late Badenian zooxanthellate corals of the Medobory Hills (western Ukraine) and their environmental significance
    Autorzy:
    Górka, A.
    Powiązania:
    https://bibliotekanauki.pl/articles/191800.pdf
    Data publikacji:
    2018
    Wydawca:
    Polskie Towarzystwo Geologiczne
    Tematy:
    corals
    scleractinians
    palaeoenvironment
    Badenian
    Middle Miocene
    Ukraine
    Opis:
    Zooxanthellate corals in the Badenian (Langhian to lower Serravallian) of western Ukraine occur in different lithofacies, but are most abundant in the upper Badenian coralgal reefs of the Ternopil Beds. The coral assemblage consists of five genera, with two predominant (Tarbellastraea and Porites) and three strongly subordinate (Favia, Heliastraea, Siderastrea). The present study is the first record of Heliastraea defrancei in the Fore-Carpathian Basin. The taxonomic composition of the corals indicates that their development occurred in conditions of some ecological stress, most probably connected with climate (location at the northern limit of coral distribution) and sedimentary environment (possible influx of terrigenous material). The coral assemblage shows similarities to numerous fossil reefs of Miocene age from the Paratethyan and Mediterranean realms.
    Źródło:
    Annales Societatis Geologorum Poloniae; 2018, 88, 3; 243-256
    0208-9068
    Pojawia się w:
    Annales Societatis Geologorum Poloniae
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    New location of the known corals genera (Favosites Lamarck, 1816 and Halysites Fischer von Waldheim, 1828) in the Mineral Raw Materials Mine in Mielenko Drawskie, West Pomeranian Province, Poland
    Autorzy:
    Borowski, Tomasz
    Powiązania:
    https://bibliotekanauki.pl/articles/1031478.pdf
    Data publikacji:
    2021
    Wydawca:
    Przedsiębiorstwo Wydawnictw Naukowych Darwin / Scientific Publishing House DARWIN
    Tematy:
    Favosites
    Halysites
    Mielenko Drawskie
    Mineral Raw Materials Mine in Mielenko Drawskie
    fossilized coral
    palaeontological corals
    palaeozoic corals
    post-glacial materials
    Opis:
    This paper presents the new location of the known corals genera: Favosites Lamarck, 1816 and Halysites von Waldheim, 1828, in the Mineral Raw Materials Mine in Mielenko Drawskie, West Pomeranian Province, Poland. These corals were obtained as a result of many years of exploration in this mine, by searching individual lots of post-glacial materials extracted by this mine.
    Źródło:
    World News of Natural Sciences; 2021, 35; 102-117
    2543-5426
    Pojawia się w:
    World News of Natural Sciences
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Silurian rugose coral Schlotheimophyllum Smith, 1945 from the Upper Visby Beds of Gotland, Sweden
    Autorzy:
    Wrzołek, Tomasz
    Zatoń, Michał
    Powiązania:
    https://bibliotekanauki.pl/articles/24264691.pdf
    Data publikacji:
    2023
    Wydawca:
    Polskie Towarzystwo Geologiczne
    Tematy:
    Rugosa
    Corals
    coloniality
    variability
    Silurian
    Opis:
    A rich (about 60 specimens) collection of Schlotheimophyllum, large rugose corals from the Silurian of Gotland, Sweden, was studied. Although the material is mostly fragmentary (beach pebbles), the presence of growth lines, clearly seen in thin sections, provides reliable numerical data. Analyzed were corallum shape, septal numbers, and aspects of coloniality. Uniformity of variability spectra of these parameters indicates that all of the material studied belongs to a single, variable species, which is Schlotheimophyllum patellatum (Schlotheim, 1820).
    Źródło:
    Annales Societatis Geologorum Poloniae; 2023, 93, 3; 251--267
    0208-9068
    Pojawia się w:
    Annales Societatis Geologorum Poloniae
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
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