Academic literature on the topic 'Favositidae'

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Journal articles on the topic "Favositidae"

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Pohler, Susanne M. L. "Favositidae (Tabulata) from Emsian to Middle Devonian limestones of the Tamworth Group (N.S.W., Australia)." Paläontologische Zeitschrift 76, no. 1 (2002): 1–19. http://dx.doi.org/10.1007/bf02988181.

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Noble, J. P. A., and D. J. Lee. "Ontogenies and astogenies and their significance in some favositid and heliolitid corals." Journal of Paleontology 64, no. 4 (1990): 515–23. http://dx.doi.org/10.1017/s0022336000042542.

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The level of colony integration in tabulate corals is the degree of colony unity with respect to behavior, physiology, and development of individual organs or organ complexes within colonies. These are difficult to assess in fossils, but the level of colony integration can be tested by analyzing ontogenies and astogenies of two common Paleozoic tabulate coral groups, favositids and heliolitids. Favositids have been previously interpreted as highly integrated colonies, but results of the present examination suggest that the level of colony integration in favositids was rather lower than hithert
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Pohler, Susanne M. L. "Paleoecology, biostratigraphy and paleogeography of Favositidae (Tabulata) from the Emsian to Middle Devonian Tamworth Group (New South Wales, Australia)." Senckenbergiana Lethaea 81, no. 1 (2001): 91–109. http://dx.doi.org/10.1007/bf03043296.

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4

Zaika, Yury. "Structure of the corallite wall of the Upper Ordovician and Silurian Favositidae (Tabulata) and its possible use in stratigraphic correlation." Palaeoworld 19, no. 3-4 (2010): 256–67. http://dx.doi.org/10.1016/j.palwor.2010.09.015.

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Lee, D. J., and J. P. A. Noble. "Evaluation of corallite size as a criterion for species discrimination in favositids." Journal of Paleontology 62, no. 01 (1988): 32–40. http://dx.doi.org/10.1017/s0022336000058844.

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Of all the morphologic characters used in favositid taxonomy, corallite size has most frequently been given more weight than others because of its relative ease of measurement and because it has been generally believed to be less variable. This study evaluates the reliability of corallite size as a criterion by a statistical treatment of several populations of favositids in the Upper Silurian West Point Reef Complex in Gaspé, Québec. Calculation of corallite cross-sectional area was made feasible by computer-based image analysis which provides a quick and accurate measure of size. The present
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Lee, D. J., and J. P. A. Noble. "Evaluation of corallite size as a criterion for species discrimination in favositids." Journal of Paleontology 62, no. 1 (1988): 32–40. http://dx.doi.org/10.1017/s0022336000017960.

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Of all the morphologic characters used in favositid taxonomy, corallite size has most frequently been given more weight than others because of its relative ease of measurement and because it has been generally believed to be less variable. This study evaluates the reliability of corallite size as a criterion by a statistical treatment of several populations of favositids in the Upper Silurian West Point Reef Complex in Gaspé, Québec. Calculation of corallite cross-sectional area was made feasible by computer-based image analysis which provides a quick and accurate measure of size. The present
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Sun, Ning, Robert J. Elias, and Dong-Jin Lee. "Corallite increase in the Late Ordovician coral Agetolites, and its taxonomic implication." Journal of Paleontology 93, no. 5 (2019): 839–55. http://dx.doi.org/10.1017/jpa.2019.14.

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AbstractAgetolites is a problematic Late Ordovician genus possessing traits of both tabulate and rugose corals. The presence of numerous mural pores has often been considered to indicate a relation to tabulates, although an affinity to rugosans has also been proposed, based mainly on well-developed septa that alternate in length. To further consider the taxonomic position of Agetolites, growth characteristics of coralla representing three species from the Xiazhen Formation in South China are documented and assessed, focusing on modes of corallite increase. Three major modes of increase are rec
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Wolosz, Thomas H. "Patterns of reef growth in the Middle Devonian Edgecliff Member of the Onondaga Formation of New York and Ontario, Canada, and their ecological significance." Journal of Paleontology 66, no. 1 (1992): 8–15. http://dx.doi.org/10.1017/s0022336000033436.

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Reefs of the Middle Devonian Edgecliff Member of the Onondaga Formation in New York and Ontario, Canada, contain three distinct paleocommunities: the Phaceloid Colonial Rugosan Paleocommunity, the Favositid/Crinoidal Sandstone Paleocommunity, and the rare Delicate Branching Tabulate Paleocommunity. The reefs may be classified as mounds or composite structures based on the degree of intergrowth of the rugosan and favositid paleocommunities. Composite structures may be further subdivided into mound/bank, thicket/bank, and ridge/bank structures based on the degree of development of the rugosan pa
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Edwards, Jeffrey C. "Lamottia (Favositida, Tabulata) from the Decorah Formation (Kirkfieldian, Ordovician) of Iowa." Journal of Paleontology 62, no. 3 (1988): 424–26. http://dx.doi.org/10.1017/s0022336000059199.

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The early tabulate coral Lamottia heroensis has been identified from the Ion Member of the Decorah Formation (Upper Ordovician) in northeast Iowa. This extends the stratigraphic range of this species upward from Lower Chazyan to Kirkfieldian, and extends the geographic range from the Vermont-New York border area to include the north-central Midcontinent. Thin section and SEM studies strongly support the contention that the longitudinal pattern of alternating light and dark bands observed in corallite walls reflects a primary structural grain rather than a secondary diagenetic feature.
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Plusquellec, Yves, and Francis Tourneur. "Persistance de Favositides microlamellaires (Cnidaria, Tabulata) dans le Dévonien." Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science 326, no. 4 (1998): 283–89. http://dx.doi.org/10.1016/s1251-8050(97)86819-x.

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Book chapters on the topic "Favositidae"

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Kaźmierczak, J. "Further Evidence for Poriferan Affinities of Favositids." In Fossil and Recent Sponges. Springer Berlin Heidelberg, 1991. http://dx.doi.org/10.1007/978-3-642-75656-6_16.

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