Evidence of photosymbiosis in Palaeozoic tabulate corals

• Published in: Proceedings of the Royal Society. B, Biological sciences Vol. 281; no. 1775; p. 20132663
• Main Author: Zapalski, Mikołaj K.
• Format: Journal Article
• Language: English
• Published: England The Royal Society 22-01-2014
• Subjects: Algae; Alveolata - physiology; Animals; Anthozoa - physiology; Palaeozoic; Photosymbiosis; Photosynthesis; Scleractinia; Stable Isotopes; Symbiodinium; Symbiosis; Tabulata; Zooxanthellae; ANE, Europe; Africa; zooxanthellae; stable isotopes; tabulata; Palaeozoic; photosymbiosis; Symbiodinium
• ISSN: 0962-8452; 1471-2945; 1471-2954
• DOI: 10.1098/rspb.2013.2663

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 to four orders (Favositida, Heliolitida, Syringoporida and Auloporida) from Silurian to Permian strata of Europe and Africa shows these characteristic carbon and oxygen stable isotope signatures. The δ18O to δ13C ratios in recent photosymbiotic scleractinians are very similar to those of Palaeozoic tabulates, thus providing strong evidence of such symbioses as early as the Middle Silurian (ca 430 Ma). Corals in Palaeozoic reefs used the same cellular mechanisms for carbonate secretion as recent reefs, and thus contributed to reef formation.