A DESCRIPTION OF THE SKELETAL DEVELOPMENT PATTERN OF THE TEMPERATE CORAL CARYOPHYLLIA-SMITHI BASED ON INTERNAL GROWTH LINES

Citation
I. Nagelkerken et al., A DESCRIPTION OF THE SKELETAL DEVELOPMENT PATTERN OF THE TEMPERATE CORAL CARYOPHYLLIA-SMITHI BASED ON INTERNAL GROWTH LINES, Journal of the Marine Biological Association of the United Kingdom, 77(2), 1997, pp. 375-387
Citations number
29
Categorie Soggetti
Marine & Freshwater Biology
ISSN journal
00253154
Volume
77
Issue
2
Year of publication
1997
Pages
375 - 387
Database
ISI
SICI code
0025-3154(1997)77:2<375:ADOTSD>2.0.ZU;2-8
Abstract
Scanning electron microscopy was used to study the microstructure and internal growth lines of the temperate ahermatypic coral Caryophyllia smithi (Cnidaria: Anthozoa). The arrangement of internal growth lines in combination with the orientation of aragonite crystals were used to describe the pattern of skeletal development in C. smithi. The observ ed pattern was verified using observations from another study on skele tal development in C. smithi, but which was based only on external obs ervations of skeletons of living and dead specimens in different stage s of development. The pattern of skeletal development in C. smithi is suggested to be subdivided into three stages, based on the deposition of specific skeletal elements during the development of the skeleton. In the first 'juvenile' stage, various primary skeletal elements are f ormed: the basal plate, the septa and a primary and secondary septothe ca. The second 'half full grown' stage is characterized by development of apparently only an extended basal attachment, which enlarges the a ttachment area to the substratum. In the third 'full grown' stage, the edge zone of the polyp tissue is retracted from the extended basal at tachment to the calice, and upward growth of the coral predominates fo llowed by lateral thickening of the septotheca, costae, septa and colu mella. Internal growth lines were found throughout the skeleton and ma y be composed of, or resulting from the presence of organic matter. Th e septotheca and the extended basal attachment, which are important fo r a strong skeletal structure and a strong attachment to the substratu m, respectively, are probably thickened faster than the other skeletal elements. Attachment scars were found in areas where attachment of th e coral tissue to the skeleton is critical.