Academic literature on the topic 'Colospongia'

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Journal articles on the topic "Colospongia"

1

Rigby, J. K., Fan Jiasong, and Zhang Wei. "Sphinctozoan sponges from the Permian reefs of South China." Journal of Paleontology 63, no. 4 (1989): 404–39. http://dx.doi.org/10.1017/s002233600001965x.

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Middle and Late Permian sphinctozoan sponges described here are from the Middle Permian Maokou and the Upper Permian Wujiaping and Changxing Formations. Most are from near Xiangbo, northwestern Guangxi, but a few are from Upper Permain patch reefs from Laolongdong in eastern Sichuan. The new genera, the porateImbricatocoeliaand the aporateGlomocystospongia, are described, the latter as the type genus for the new family Glomocystospongiidae. New species described includeAmblysiphonella specialis, Amblysiphonella spinosa, Amblysiphonellasp. A,Amblysiphonellasp. B,Colospongia maxima, Colospongias
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2

Senowbari-Daryan, Baba, and R. Pamela Reid. "Upper Triassic sponges (Sphinctozoa) from southern Yukon, Stikinia terrane." Canadian Journal of Earth Sciences 24, no. 5 (1987): 882–902. http://dx.doi.org/10.1139/e87-087.

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The first Tethyan-type Upper Triassic sponge reefs in North America have recently been discovered in the southern Yukon, in Stikinia terrane. Sphinctozoa from these reefs and inter-reef limestones are represented by 18 species and 12 genera belonging to six families. The genus Yukonella with one species, Y. rigbyi, and the species Polytholosia ramosa and Polycystocoelia norica are described for the first time. Some of the Yukon sponges were previously known only from the Tethyan realm (Colospongia, Dictyocoelia, Polycystocoelia, and Uvanella?); others, from Tethyan and North American localitie
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3

Малышева, Е. Н. "НОВЫЙ ВИД СФИНКТОЗОА (PORIFERA) COLOSPONGIA LENIS SP. NOV. ИЗ ВЕРХНЕПЕРМСКИХ РИФОВ ЮЖНОГО ПРИМОРЬЯ, "Палеонтологический журнал"". Палеонтологический журнал, № 3 (2018): 10–12. http://dx.doi.org/10.7868/s0031031x18030029.

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4

Rigby, J. Keith, Fan Jiasong, and Han Nairen. "Upper Permian silicified sponges from central Guangxi and western Hubei, South China." Journal of Paleontology 69, no. 2 (1995): 232–50. http://dx.doi.org/10.1017/s0022336000034570.

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Well-preserved silicified sponges have been recovered from the Upper Permian Changxing Formation at Huangnitang in western Hubei province. The new species Cystauletes grossa and Cystothalamia irregulara are associated with Cystothalamia sp., Colospongia salinaria irregularis Zhang, 1983, Sollasia ostiolata Steinmann, 1882, Virgola? osiensis (de Gregorio, 1930), a questionable inozoan species, and a form questionably referred to the genus Hikorodium? sp. These sponges were detrital fragments that accumulated at the toe of the forereef, at the margin of slope fades and basin fades, at Huangnitan
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5

Weidlich, Oliver, and Baba Senowbari-Daryan. "Late Permian “sphinctozoans” from reefal blocks of the Ba'id area, Oman Mountains." Journal of Paleontology 70, no. 1 (1996): 27–46. http://dx.doi.org/10.1017/s0022336000023088.

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Late Permian reefal blocks exposed in the Ba'id area of the Eastern Oman Mountains yield a sphinctozoan assemblage that has not been studied previously. The sphinctozoan fauna described here is the first report of such an assemblage from the Arabian Peninsula. Approximately 70 samples were studied with respect to systematic paleontology, as well as frequency of taxa based on presence/absence lists. The sphinctozoans include 14 genera and 25 species. One genus (Rahbahthalamia) and five species (Amblysiphonella omanica, Salzburgia? irregularis, Welteria? hawasinensis, Thaumastocoelia? irregulari
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6

Malysheva, E. N., and T. A. Punina. "PALEOECOLOGICAL AND FACIAL CHARACTERISTICS OF THE ORGANOGENIC STRUCTURE OF SESTRA MOUNTAIN IN SOUTHERN PRIMORYE." Bulletin of Kamchatka Regional Association «Educational-Scientific Center». Earth Sciences 2(58) (2023): 93–48. http://dx.doi.org/10.31431/1816-5524-2023-2-58-39-48.

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A lithological-paleoecological description of the organogenic structure of Mountain Sestra is given. A macro- and microscopic study of the fauna composing the structure was carried out, its percentage content in limestones and the role of each group of organisms in the reef formation process were determined. Based on the data obtained, six genetic types of limestones were identified: biohermic, biomorphic, detrital, biohemogenic, clastic and granular. Studies of the taxonomic composition and the structure of communities allowed us to identify three distinct stages in the development of organog
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7

Senowbari-Daryan, Baba, and George D. Stanley. "Triassic sponges (Sphinctozoa) from Hells Canyon, Oregon." Journal of Paleontology 62, no. 3 (1988): 419–23. http://dx.doi.org/10.1017/s0022336000059187.

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Two Upper Triassic sphinctozoan sponges of the family Sebargasiidae were recovered from silicified residues collected in Hells Canyon, Oregon. These sponges are Amblysiphonella cf. A. steinmanni (Haas), known from the Tethys region, and Colospongia whaleni n. sp., an endemic species. The latter sponge was placed in the superfamily Porata by Seilacher (1962). The presence of well-preserved cribrate plates in this sponge, in addition to pores of the chamber walls, is a unique condition never before reported in any porate sphinctozoans. Aporate counterparts known primarily from the Triassic Alps
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8

Senowbari-Daryan, Baba, Sándor Kovács, and Felicitász Velledits. "Sponges from the Middle Triassic reef limestone of the Aggtelek Karst (NE Hungary)." Geologica Carpathica 62, no. 5 (2011): 397–412. http://dx.doi.org/10.2478/v10096-011-0029-4.

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Sponges from the Middle Triassic reef limestone of the Aggtelek Karst (NE Hungary) The hypercalcified sponge fauna of the Middle Triassic (Anisian-Ladinian) reef limestone exposed between Aggtelek-Jósvafő-Égerszög (northern Hungary) is described. Almost all the identified species are chambered sponges ("sphinctozoa"). Only two fragments of a not determinable species of non-chambered species ("inozoa") were identified. Hexactinellid sponges are not found. The majority of the Middle Anisian "sphinctozoans" are absolutely different genera, not known from the Permian reefs. The sponge fauna of the
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9

Malysheva, E. N. "A New Sphinctozoan Species (Porifera), Colospongia lenis sp. nov., from the Upper Permian Reefs of Southern Primorye." Paleontological Journal 52, no. 3 (2018): 231–33. http://dx.doi.org/10.1134/s0031030118030085.

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10

Senowbari-Daryan, B., M. Link, and P. Riedel. "Colospongia cribrifera nov. sp. and Parastylothalamia minima nov. sp. ("Sphinctozoa" Porifera) from the Norian of Taurus Mountains, Turkey." Revue de Paléobiologie 34, no. 1 (2015): 1–9. https://doi.org/10.5281/zenodo.18891.

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