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Journal articles on the topic 'Favositidae'

Author: Grafiati

Published: 4 June 2021

Last updated: 29 July 2025

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1

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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2

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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3

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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5

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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6

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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7

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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8

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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9

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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10

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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11

KaŹmierczak, JÓzef. "Sclerite-bearing alveolitid favositids from the Devonian of central Poland." Paläontologische Zeitschrift 67, no. 1-2 (1993): 27–44. http://dx.doi.org/10.1007/bf02985868.

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12

Zapalski, Mikołaj K., Benoît L. M. Hubert, Jean-Pierre Nicollin, Bruno Mistiaen, and Denise Brice. "The palaeobiodiversity of stromatoporoids, tabulates and brachiopods in the Devonian of the Ardennes – Changes through time." Bulletin de la Société Géologique de France 178, no. 5 (2007): 383–90. http://dx.doi.org/10.2113/gssgfbull.178.5.383.

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Abstract The specific biodiversity of stromatoporoids, tabulates and brachiopods from the Ardennes (707 taxa) has been analyzed stage-by-stage from the Lochkovian up to the Famennian. The diversity of each group may be correlated with external factors (e.g. facies), but it varied individually (e.g. decline of brachiopods in the Givetian). The faunas are discussed at the order level, however some more diversified orders are analyzed at family level. Biodiversity shows a single peak centered on the Givetian for the bioconstructors, and two major peaks (Emsian-Eifelian and Frasnian) for the brach

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13

Young, Graham A., and Robert J. Elias. "The relationship between growth form and internal morphology in favositid corals." Paleontological Society Special Publications 6 (1992): 323. http://dx.doi.org/10.1017/s2475262200008832.

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Growth form in Paleozoic colonial corals is commonly used as an indicator of paleoenvironmental conditions. However, this character was also influenced by genetic factors, and it must be recognized that aspects of internal morphology were significant in the development of external form. In favositids a primary control on growth form was exerted by rates of corallite divergence, offsetting, and vertical growth, since the shape of the corallum base and growth surface resulted largely from these factors. This relationship worked in both directions; modifications of external shape that were appare

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14

PANDOLFI, JOHN M., and COLLETTE DICK BURKE. "Environmental distribution of colony growth form in the favositid Pleurodictyum americanum." Lethaia 22, no. 1 (1989): 69–84. http://dx.doi.org/10.1111/j.1502-3931.1989.tb01170.x.

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15

GIBSON, MICHAEL A., and THOMAS W. BROADHEAD. "Species-specific growth responses of favositid corals to soft-bottom substrates." Lethaia 22, no. 3 (1989): 287–99. http://dx.doi.org/10.1111/j.1502-3931.1989.tb01343.x.

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16

Zapalski, Mikołaj K. "Evidence of photosymbiosis in Palaeozoic tabulate corals." Proceedings of the Royal Society B: Biological Sciences 281, no. 1775 (2014): 20132663. http://dx.doi.org/10.1098/rspb.2013.2663.

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Coral reefs form the most diverse of all marine ecosystems on the Earth. Corals are among their main components and owe their bioconstructing abilities to a symbiosis with algae ( Symbiodinium ). The coral–algae symbiosis had been traced back to the Triassic ( ca 240 Ma). Modern reef-building corals (Scleractinia) appeared after the Permian–Triassic crisis; in the Palaeozoic, some of the main reef constructors were extinct tabulate corals. The calcium carbonate secreted by extant photosymbiotic corals bears characteristic isotope (C and O) signatures. The analysis of tabulate corals belonging

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17

SEILACHER, ADOLF, and ROGER D. K. THOMAS. "Self-organization and emergent individuality of favositid corals adapted to live on soft substrates." Lethaia 45, no. 1 (2011): 2–13. http://dx.doi.org/10.1111/j.1502-3931.2011.00287.x.

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18

Krutykh, A. A., G. V. Mirantsev, and S. V. Rozhnov. "Sutherlandia gzheliensis sp. nov.—a New Species of Favositid Coral from the Gzhelian Stage of the Moscow Syneclise." Paleontological Journal 58, no. 11 (2024): 1208–15. https://doi.org/10.1134/s0031030124601075.

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19

Long, D. G. F., and Paul Copper. "Late Ordovician sand-wave complexes on Anticosti Island, Quebec: a marine tidal embayment?" Canadian Journal of Earth Sciences 24, no. 9 (1987): 1821–32. http://dx.doi.org/10.1139/e87-173.

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Laterally discontinuous, mixed carbonate–siliciclastic sandstones in the upper Vaureal and lower Ellis Bay formations of Anticosti Island were deposited on an equatorial carbonate ramp with a slope of less than 1°. The 10–18 m thick sandstones are interpreted as subaqueous sand-wave complexes analogous to detached parts of modern shoreface-connected sand ridges. These record storm-enhanced, tidal modification of a northerly derived shoal retreat massif that may have formed in response to recovery from global sea-level lowstands in the Late Ordovician (Ashgill: late Rawtheyan – Hirnantian). The

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20

Ernst, Andrej, and Axel Munnecke. "A Hirnantian (latest Ordovician) reefal bryozoan fauna from Anticosti Island, eastern Canada: taxonomy and chemostratigraphy." Canadian Journal of Earth Sciences 46, no. 3 (2009): 207–29. http://dx.doi.org/10.1139/e09-017.

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The Natiscotec outcrop on Anticosti Island, Canada (Ellis Bay Formation, Laframboise Member, Hirnantian, Late Ordovician), exposes a patch reef some 20–30 m in diameter, 2–3 m thick, with abundant rugose corals, as well as favositids and heliolitids. Reef capping and flanking sediments include typical Hirnantian brachiopods, such as Hirnantia , Hindella , and Eospirigerina . Within the reef peloidal microbialites encrusting bryozoan colonies are common. The bryozoan fauna includes three cystoporates, seven trepostomes, and three phylloporines. Two genera and two species are new: the cystoporat

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21

Lee, Dong-Jin, and Robert J. Elias. "Paleobiologic and evolutionary significance of corallite increase and associated features inSaffordophyllum newcombae(Tabulata, Late Ordovician, southern Manitoba)." Journal of Paleontology 74, no. 3 (2000): 404–25. http://dx.doi.org/10.1017/s0022336000031681.

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Saffordophyllum newcombaeFlower, 1961, displays unique abilities and an unprecedented range in types of corallite increase. Cerioid growth was characteristic, but colonies on soft substrates could grow in a tollinaform manner during early astogeny. The capacity for recovery from damage and partial mortality is amazing. Rejuvenation may have been accompanied by peripheral expansion in some cases. Rapid regeneration could involve axial increase. Circular lacunae that formed during recovery became sites of rapid lateral increase or corallite decrease.Two types of axial increase occurred within co

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22

Miller, Keith B., and Ronald R. West. "Chaetetid skeletons as short-term records of physical disturbance events." Paleontological Society Special Publications 6 (1992): 212. http://dx.doi.org/10.1017/s2475262200007723.

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The growth records of spongiomorph and colonial skeletons have great potential for revealing the short-term depositional dynamics of ancient shallow marine environments. The utility of such skeletons for understanding the type and frequency of physical disturbance is illustrated by chaetetid-bearing limestones from Pennsylvanian (Desmoinesian) cyclothems of southeastern Kansas. Individual chaetetids frequently contain growth-interruption surfaces that are marked by clay partings or encrusting overgrowths of epibionts. Such interruptions occur irrespective of the growth form of the chaetetids,

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23

Thomka, James, and Lilian Gunderson. "Multiple forms of bioimmuration in a coral-crinoid-bryozoan association from the Middle Devonian Onondaga Formation of southeastern Ontario." Canadian Journal of Earth Sciences, June 1, 2023. http://dx.doi.org/10.1139/cjes-2023-0002.

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A large favositid tabulate coral colony from the Middle Devonian Edgecliff Member of the Onondaga Formation, collected from Port Colborne, southernmost Ontario, is described herein because of several noteworthy paleontological features preserved via overgrowth by the coral. The initial substratum colonized and subsequently overgrown by the favositid was a large solitary rugose coral; and outward growth resulted in overgrowth of multiple macrofossils, including relatively long portions of large-diameter (probably camerate) crinoid columns. The crinoid columns, which likely represent portions of

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24

Zatoń, Michał, Rafał Nawrot, Jan J. Król, et al. "Skeletobiosis on favositid corals: a case study from the Middle Devonian of the Mader Basin, Morocco." Acta Geologica Polonica, December 17, 2024, 30. https://doi.org/10.24425/agp.2024.152655.

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25

Thomka, James, and Thomas E. Bantel. "Paleoecological Significance of a Pre-Mortem Crinoid-Coral Interaction from the Silurian of Southeastern Indiana." Indiana Journal of Earth Sciences 3 (April 7, 2021). http://dx.doi.org/10.14434/ijes.v3i1.31283.

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A noteworthy specimen recording a syn vivo interaction between a stalked echinoderm and a tabulate coral is described herein from the middle Silurian (Wenlock: Sheinwoodian) Massie Formation of Ripley County, southeastern Indiana. Part of the column of the camerate crinoid Eucalyptocrinites is encrusted around the entirety of its lateral margin by a favositid colony. The radially outward orientation of corallites on both the upper and lower surfaces of the colony show that the coral was elevated completely above the seafloor and, more importantly, that the crinoid column had to be vertical at

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