Morphological limits to diversification of the rugose and tabulate corals

Palaeoworld ◽  
2010 ◽  
Vol 19 (3-4) ◽  
pp. 389-400 ◽  
Author(s):  
Edouard Poty
Keyword(s):  
Tabulate Corals

Tabulate corals from the Lower Silurian of Jämtland (Sweden)

GFF ◽  
2004 ◽  
Vol 126 (4) ◽  
pp. 339-352
Author(s):  
Mari-Ann Mötus
Keyword(s):  
Lower Silurian ◽  
Tabulate Corals

Coral microatolls and a probable Middle Ordovician example

1990 ◽  
Vol 64 (1) ◽  
pp. 39-43 ◽  
Author(s):  
David R. Kobluk ◽  
Iqbal Noor
Keyword(s):  
Coral Reefs ◽  
Fossil Record ◽  
Scleractinian Coral ◽  
Regional Scale ◽  
Southern Ontario ◽  
Middle Ordovician ◽  
Reef Environments ◽  
Maximum Water ◽  
Water Depths ◽  
Tabulate Corals

A disk-shaped massive colony of Tetradium, from the Middle Ordovician Bobcaygeon Formation in southern Ontario, displays features of a coral microatoll. This is the first pre-Holocene coral microatoll yet described, indicating that some tabulate corals in level-bottom communities were growing as microatolls as do many modern colonial skeleton-secreting organisms.The microatoll therefore is not strictly a Quaternary or even Cenozoic phenomenon, but has a fossil record that may span most of the Phanerozoic. This indicates that the special conditions necessary for microatoll growth have existed outside of reef environments, and were present before the advent of scleractinian coral reefs. It may be possible to use ancient microatolls to estimate absolute water depths at low tide, thereby providing a means for estimating maximum water depths on a local and regional scale.

Corallite increase in the Late Ordovician coral Agetolites, and its taxonomic implication

2019 ◽  
Vol 93 (5) ◽  
pp. 839-855
Author(s):  
Ning Sun ◽  
Robert J. Elias ◽  
Dong-Jin Lee
Keyword(s):  
South China ◽  
Typical Feature ◽  
Late Ordovician ◽  
Growth Characteristics ◽  
Taxonomic Position ◽  
Phylogenetic Relation ◽  
Axial Mode ◽  
Rugose Corals ◽  
Lateral Mode ◽  
Tabulate Corals

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 recognized. By far the most common mode involves the development of an offset from a connective mural pore, without a clear relationship to a particular parent corallite. This mode of increase is usually associated with corner pores, but in one case occurs at a wall pore. The lateral mode of increase, which is relatively uncommon, is a typical feature in corallites along the boundary of intergrowths with stromatoporoids. The axial mode of increase is rare, occurring during rejuvenation of a damaged corallite or during regeneration following termination of a corallite. The mode of corallite increase that is characteristic of Agetolites, involving a connective mural pore and occurring without evidence of a particular parent, supports the interpretation that this genus is not a rugosan or a typical favositid tabulate. Mural pores are unknown in rugosans, and offsets arise from distinct parent corallites in favositids. The Ordovician genus Lichenaria, considered a representative of the most primitive stock of tabulate corals, shows the closest similarities with types of increase in Agetolites. Certain aspects of lateral and axial increase in Agetolites are comparable to features in a few more genera of Ordovician tabulates, further supporting a tabulate affinity. The phylogenetic relation of Agetolites to those and other tabulate genera, however, remains unresolved.

SYMBIOSIS OF RUGOSE CORALS WITH THE CYSTOPORATE BRYOZOAN FISTULIPORA PRZHIDOLENSIS IN THE PRIDOLI (LATEST SILURIAN) OF SAAREMAA, ESTONIA

Palaios ◽  
2020 ◽  
Vol 35 (6) ◽  
pp. 237-244
Author(s):  
OLEV VINN ◽  
ANDREJ ERNST ◽  
MARK A. WILSON ◽  
URSULA TOOM
Keyword(s):  
Late Ordovician ◽  
Growth Surface ◽  
Symbiotic Association ◽  
Negative Effects ◽  
Perpendicular Orientation ◽  
Rugose Corals ◽  
The Relationship ◽  
Tabulate Corals

ABSTRACT In the Silurian, the most common hosts of endobiotic rugose corals were stromatoporoids followed by tabulate corals. Here we describe the relationship between rugose corals and a bryozoan. Solitary rugosans and the cystoporate bryozoan Fistulipora przhidolensis Kopajevich, 1990 formed a symbiotic association in the late Silurian (Pridoli) of Saaremaa, Estonia. The syn vivo nature of the association is indicated by complete intergrowth of both organisms and the perpendicular orientation of the rugosans to the bryozoan growth surface. There are one to seven endobiotic rugosans per bryozoan colony. This is the first detailed study of coral-bryozoan symbiosis from the Silurian; all previous reports describe Late Ordovician, Devonian, or Cenozoic material. The lack of malformations and decrease in the size of bryozoan zooids near the rugosans suggest there were no strong negative effects of the rugosans on the bryozoan. The rugosans likely benefited from their association with the bryozoan, which served as an anchor to stabilize them in hydrodynamically active waters, and the bryozoan may have benefited by protection against some types of predators. The associations described here were most likely mutualistic.

Nicholson's Tabulate Corals

Nature ◽  
1880 ◽  
Vol 21 (543) ◽  
pp. 490-491
Keyword(s):  
Tabulate Corals

Tabulate corals across the Frasnian/Famennian boundary: architectural turnover and its possible relation to ancient photosymbiosis

2017 ◽  
Vol 487 ◽  
pp. 416-429 ◽  
Author(s):  
Mikołaj K. Zapalski ◽  
Jakub Nowicki ◽  
Michał Jakubowicz ◽  
Błażej Berkowski
Keyword(s):  
Tabulate Corals
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