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Relevant bibliographies by topics / Syringoporidae

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Journal articles

Academic literature on the topic 'Syringoporidae'

Author: Grafiati

Published: 28 July 2024

Last updated: 31 July 2025

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Journal articles on the topic "Syringoporidae"

1

Young, G. A., and J. P. A. Noble. "The Llandovery–Wenlock Syringoporidae from New Brunswick, Canada." Journal of Paleontology 61, no. 2 (1987): 268–83. http://dx.doi.org/10.1017/s0022336000028456.

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A large collection of Silurian Syringoporidae, mainly from the Limestone Point and La Vieille formations of northern New Brunswick, includes one new species and three species previously described from this area. Syringopora lambei n. sp. is distinguished from the superficially similar S. bifurcata Lonsdale by its larger corallites with much broader axial tubes and less frequent corallite contacts. Similar problems which have existed in the past in the distinction of S. compacta Billings and S. reteformis Billings can be resolved, as shown in this study, on the basis of the larger, geniculate a

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2

CORONADO, ISMAEL, and SERGIO RODRÍGUEZ. "Biomineral structure and crystallographic arrangement of cerioid and phaceloid growth in corals belonging to the Syringoporicae (Tabulata, Devonian–Carboniferous): a genetic reflection." Geological Magazine 153, no. 4 (2016): 718–42. http://dx.doi.org/10.1017/s0016756815000862.

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AbstractAn extensive study of the microstructure, nanostructrure and crystallographic properties of six taxa belonging to four different genera of Devonian and Carboniferous Syringoporicae showing dense phaceloid (Pleurosiphonella), pseudocerioid (Neomultithecopora) and cerioid growth patterns (Roemeria and Roemeripora) has been done in order to disclose the similarities and differences in the growth processes at the biomineral scale and understand the growth processes that provide organisms with an evolutionary advantage to colonize different habitats. All the skeletons have similarities rega

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3

Lukin, V. Yu. "New species of syringoporids from Eifelian deposits of the Subpolar Ural Mountains." Paleontological Journal 40, no. 4 (2006): 369–74. http://dx.doi.org/10.1134/s0031030106040022.

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4

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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5

Coronado, Ismael, Alberto Pérez-Huerta, and Sergio Rodríguez. "Crystallographic orientations of structural elements in skeletons of Syringoporicae (tabulate corals, Carboniferous): implications for biomineralization processes in Palaeozoic corals." Palaeontology 58, no. 1 (2014): 111–32. http://dx.doi.org/10.1111/pala.12127.

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6

Coronado, Ismael, Alberto Pérez-Huerta, and Sergio Rodríguez. "Computer-integrated polarisation (CIP) in the analysis of fossils: a case of study in a Palaeozoic coral (Sinopora, Syringoporicae, Carboniferous)." Historical Biology 27, no. 8 (2014): 1098–112. http://dx.doi.org/10.1080/08912963.2014.938236.

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