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1

Fauna of Bryozoa from Kongsfjorden, West Spitsbergen

100%
Kuklinski P.
Polish Polar Research
|
2002
|
tom 23
|
nr 2
193-206
2

Development of Schroedera plumatellae gen.n., sp.n. [Microsporidia] in Plumatella fungosa [Bryoza: Phylactolaemata]

100%
Morris D. J., Adams A.
Acta Protozoologica
|
2002
|
tom 41
|
nr 4
3

A new macroporid bryozoan from Eocene of Seymour Island, Antarctic Peninsula

84%
Hara U.
Polish Polar Research
|
2002
|
tom 23
|
nr 3-4
213-225
4
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Middle Carboniferous to Early Permian bryozoans from Spitsbergen

84%
Nakrem H. A.
Acta Palaeontologica Polonica
|
1994
|
tom 39
|
nr 1
45-116
Bryozoans from the Nordenskiöldbreen Formation (Middle Carboniferous Moscovian through Early Permian Sakmarian) and the Gipshuken Formation (late Sakmarian - late Artinskian), from central Spitsbergen, Svalbard, are represented by 36 species (22 genera). One species is new: Hinaclema svalbardensis of the order Trepostomata. The bryozoan fauna is typical Boreal and resembles those from the Timan-Pechora region (western Siberia) and the Urals. Similarity indices based on generic composition show that the Boreal fauna became more endemic by the late Early Permian, clearly separated from the Tethyan faunas. Several species have stratigraphic ranges in Spitsbergen longer than elsewhere.
5

Variability in trophic dominance of amphipods associated with the bryozoan Bugula neritina [ L.,1758 ] in Algeciras Bay [ Southern Iberian Peninsula ]

84%
Conradi M., Cervera J. L.
Polskie Archiwum Hydrobiologii
|
1995
|
tom 42
|
nr 4
6

Diversity and distribution of Bryozoa in Kongsfjorden, Svalbard

84%
Gontar V. I., Hop H., Voronkov A. Y.
Polish Polar Research
|
2001
|
tom 22
|
nr 3-4
7
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Lower Permian bryozoans from southern and central Spitsbergen, Svalbard

67%
Nakrem H. A., Blazejowski B., Gazdzicki A.
Acta Palaeontologica Polonica
|
2009
|
tom 54
|
nr 4
Bryozoans from the Lower Permian Treskelodden and Wordiekammen formations of southern and central Spitsbergen respectively, Svalbard, have been studied. Twenty species are identified, including one new genus, Toulapora gen. nov., with Toulapora svalbardense as type species and one new species, Ascopora birkenmajeri sp. nov. The taxonomic composition is typical Lower Permian, with species in common with Timan−Pechora and the Urals (Russia) and Ellesmere Island (the Canadian Arctic). Growth habits reflect a moderately to deeper shelf environment.
8

Bryozoan species Hyalinella punctata Hancock in the gut content of chub Leuciscus cephalus L.

67%
Markovic G., Karan-Znidarsic T., Simonovic P.
Polish Journal of Ecology
|
2009
|
tom 57
|
nr 1
201-205
Bryozoans are widely distributed benthic invertebrates which form colonies both in running and stagnant waters. There are 19 freshwater species of Bryozoa in Europe, and only three have been recorded in Serbia so far. Statoblasts (the dormant stages of these colonial animals) are relatively frequently found in the gut contents of fish, but those of the Hyalinella punctata species (Phylactolaemata) have not been registered. Statoblasts of H. punctata were determined for the first time in the gut content of chub Leuciscus cephalus sampled from the Zapadna Morava River (West Serbia, Danube River basin) in late summer and autumn. The intactness in form supports their viability after the passage through intestines, implying that the fish may be a vector of the dispersal of H. punctata in new aquatic habitats, as well as a risk factor in the transmission of certain salmonid fish disease agents into fish farms and natural habitats.
9
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Late Tortonian bryozoans from Mut Basin, Central Anatolian Plateau, southern Turkey

67%
Zagorsek K., Gordon D. P.
Acta Palaeontologica Polonica
|
2013
|
tom 58
|
nr 3
Sixteen bryozoan species have been identified in the Başyayla section, Mut Basin, southern Turkey. Five of these species are described here, including two new to science representing new genera: Basyaylella elsae gen. et sp. nov. and Ostrovskia triforamina gen. et sp. nov. The other three described species (Exidmonea sp., Biflustra savartii, and Margaretta sp.) show unusual features that have not been reported previously. Based on bryozoan data, the Başyayla sequence represents a tropical to subtropical, normal marine environment, with seafloor composed of fine sedimentary particles in a low−energy setting.
10

Przerostowa choroba nerek ryb łososiowatych (PKD) - nowe poglądy na etiologię i rozprzestrzenianie

67%
Prost M.
Medycyna Weterynaryjna
|
2002
|
tom 58
|
nr 08
11
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Trepostome bryozoans encrusting Silurian gastropods: A taphonomic window and its implications for biodiversity

67%
Buttler C. J., Cherns L., McCobb L. M. E.
Acta Palaeontologica Polonica
|
2022
|
tom 67
|
nr 3
12
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Exceptional soft-tissue preservation in boring ctenostome bryozoans and associated “fungal” borings from the Early Devonian of Podolia, Ukraine

67%
Olempska E.
Acta Palaeontologica Polonica
|
2012
|
tom 57
|
nr 4
Colonies of boring ctenostome bryozoans and microborings of “fungi” that occur in the Early Devonian (Lochkovian, ~416 Ma) of Podolia, western Ukraine, have soft−tissue preserved by phosphatization. These comprise exceptional three−dimensional body walls of feeding zooids with probable parietal muscles inserted on the cystid wall, and setigerous collars twisted within the vestibulum. The presence of collars in this Early Devonian ctenostomes proves the existence of this feature for more than 416 Ma of ctenostome evolution. Phosphatized remains of the zooid walls are interpreted as relicts of the originally chitinous cystid walls. This is the first record of soft−tissue fossilization in a boring bryozoan. The presence of cavities (specialized heterozooids), empty or filled with laminated calcium phosphate, is also documented in bryozoans for the first time. These cavities are interpreted as “store−rooms” in which the bryozoans accumulated nutrients. The new taxon, Podoliapora doroshevi gen. et sp. nov. is described. In additional, phosphatised fungi−like endoliths co−occur with bryozoans.
13
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Late Carboniferous bryozoans from La Hermida, Spain

67%
Ernst A., Minwegen E.
Acta Palaeontologica Polonica
|
2006
|
tom 51
|
nr 3
Fifteen bryozoan species belonging to thirteen genera have been identified from an outcrop of the Picos de Europa Formation (Moscovian, Upper Carboniferous) at La Hermida in northern Spain. Three species and one genus are new— Coscinium hermidensissp. nov., Cystodictya pustulosa sp. nov., and Cystocladia hispanica gen. et sp. nov. Rhabdomesid bryozoans are the most diverse order with seven species, followed by cystoporids (four species), fenestellids (three species) and trepostomids (one species). Bryozoans with erect branched or reticulate colonies dominate in the studied assemblage; only two species possess encrusting colonies. Together with associated crinoids, the bryozoan assemblage indicates a subtidal environment below the zone of vigorous water movement. The La Hermida bryozoan fauna confirms the Upper Carboniferous age of the Picos de Europa Formation and allows various biogeographical interpretations. All previously known species of the genus Coscinium were reported from the Lower Permian of Russia. Clausotrypa monticola is known from the Lower Permian of Russia and Arctic as well as from the Upper Carboniferous of Carnic Alps (Austria). Rhabdomeson cf. propatulissimum and Penniretepora pseudotrilineata are known from the same level of Italian Carnic Alps. Streblotrypa (Streblascopora) nikiforovae and Rhombocladia punctata are known from the Upper Carboniferous (Moscovian) of Ukraine. Fistulipora petaloida is known from Kasimovian Stage of Russian Plate. Several other species show connections with North America.
14

The Weddell Sea Formation: post-Late Pliocene terrestrial glacial deposits on Seymour Island, Antarctic Peninsula

67%
Gazdzicki A., Tatur A., Hara U., Del Valle R. A.
Polish Polar Research
|
2004
|
tom 25
|
nr 3-4
189-204
15
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Emergence and extinction of the Givetian to Frasnian bryozoan faunas in the Kostomloty facies zone, Holy Cross Mountains, Poland

67%
Morozova I. P., Weis O. B., Racki G.
Acta Palaeontologica Polonica
|
2002
|
tom 47
|
nr 2
Devonian bryozoans have been investigated from two Givetian to Frasnian localities in the Holy Cross Mts (Central Poland), representing fossiliferous ramp slope facies of the Kostomłoty facies zone (north−western periphery of the Kielce carbonate platform). Thirteen genera belonging to four families and three orders have been identified. Bryozoans show close relation to previously described Givetian and Frasnian bryozoan faunas of France, but also some affinities to easterly regions (e.g., Kuzbass). The main immigration episodes are related to late Givetian and middle Frasnian deepening pulses. The replacement of locally rich and diverse Givetian carbonate bank faunas by overall impoverished Frasnian reef−complex associations largely corresponds to a major extinction event in the evolutionary history of Bryozoa. Five new species are described by I. Morozova and O. Weis: Eridotrypella arguta, Eridotrypella exserta, Eostenopora nimia, Primorella nitida, Primorella indigena.
16
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Palaeoecology of free-lying domal bryozoan colonies from the Upper Eocene of Southeastern USA

67%
McKinney F. K., Taylor P. D.
Acta Palaeontologica Polonica
|
2003
|
tom 48
|
nr 3
Dome−shaped cheilostome bryozoan colonies, most commonly about 2 cm in diameter, are common in Upper Eocene offshore deposits of southeastern North Carolina, USA.This colony−form is anachronistic in the Eocene, being more typical of Palaeozoic bryozoans.There are three types of domes: individual colonies of Parasmittina collum (Canu and Bassler), individual colonies of Osthimosia glomerata (Gabb and Horn) and multispecies intergrowths.The bryozoans grew laterally beyond initial shell substrata to become free−lying. P. collum colonies grew by local eruptive budding, forming subcolonies that extended radially over the underlying layer of zooids.Undersides of subcolonies that extended beyond the original substratum have basal exterior walls that are more commonly fouled by encrusters than is the upper side of the colony.By contrast, lateral growth of O. glomerata colonies was limited by size of the original substratum, subcolonies were not developed, and colony growth occurred by prolific frontal budding over the entire upper surface of the colony. Undersides of colonies beyond the substratum consist of the lateral interior walls of marginal zooids and are much less commonly fouled than are undersurfaces of P. collum.The upper surfaces of multispecies domes by definition are always fouled, and their undersurfaces are also commonly fouled.
17
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Invertebrates fauna of the Lubiatowskie Lakes in the North-West part of the Notec Primeval Forest

67%
Agapow L., Nadobnik J., Koroscinski B.
Acta Agrophysica
|
2006
|
tom 07
|
nr 2[133]
18
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Middle Jurassic cyclostome bryozoans from the Polish Jura

59%
Zaton M., Taylor P. D.
Acta Palaeontologica Polonica
|
2009
|
tom 54
|
nr 2
267-288
New collections of bryozoans from the Middle Jurassic (Late Bajocian and Bathonian) of Poland add significantly to our knowledge of the diversity and biogeography of the Cyclostomata at a time when they were the dominant bryozoan order in the fossil record. A total of 16 species and one form−genus (“Berenicea”) are present. Most are encrusters, predominantly on hiatus concretions. A single erect species was found in deposits interpreted as regurgitates of a marine vertebrate. The following new species are described: Microeciella annae sp. nov., M. kuklinskii sp. nov., M. maleckii sp. nov., M. mokrskoensis sp. nov., M. magnopora sp. nov., Reptomultisparsa harae sp. nov., and Hyporosopora bugajensis sp. nov. The taxonomic importance of the morphology of both the gonozooids and pseudopores is underlined, especially for encrusting species of the “Berenicea” type that are otherwise difficult to distinguish from one another. The described bryozoan assemblage encrusting hiatus concretions from the Polish Middle Jurassic is the richest that has been documented globally from this kind of substrate.
19

Mszywioły

50%
Mis M.
Przyroda Polska
|
2014
|
nr 02
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