Community structure of rhodolith-forming beds on the central Brazilian continental shelf

The community structure of rhodoliths beds in the central Brazilian continental shelf was studied under the hypothesis that nongeniculate coralline algae are the major contributors of the individual rhodoliths. Samples were collected from five localities within a single area at 17–18 m depth. At eac...

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Bibliographic Details
Published in:Helgoland marine research 2014-03, Vol.68 (1), p.27-35
Main Authors: Villas-Boas, Alexandre B, Riosmena-Rodriguez, Rafael, de Oliveira Figueiredo, Marcia Abreu
Format: Article
Language:English
Subjects:
Algae
Bryozoa
calcium carbonate
carbon dioxide
Cirripedia
Community ecology
community structure
continental shelf
corals
Invertebrates
Lithophyllum
Lithothamnion
Marine
Marine ecology
Neogoniolithon
Neogoniolithon brassica-florida
Peyssonnelia
Spongites
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Summary:The community structure of rhodoliths beds in the central Brazilian continental shelf was studied under the hypothesis that nongeniculate coralline algae are the major contributors of the individual rhodoliths. Samples were collected from five localities within a single area at 17–18 m depth. At each locality, rhodoliths were collected in 10 random quadrat samples along a 20-m transect. Our results show that dead cores of rhodoliths were significantly composed by nongeniculate coralline red algae rather than bryozoans, corals, or inorganic material. The live outer layers of the rhodoliths are composed mainly of 7 species of nongeniculate red coralline algae (Lithophyllum coralline, L. johansenii, L. depressum, L. stictaeformis, Neogoniolithon brassica-florida, Spongites fruticosus, and Lithothamnion muellerii) associated with other encrusting organisms such as bryozoans, sponges, corals, barnacles, and Peyssonnelia red algae. Significant differences were found in the proportion of Lithophyllum species in relation to other red coralline algae found in this study. Our results show that on the Brazilian continental shelf, the rhodolith-forming species are quite higher in size than in any other studied areas in the world. There was no difference in the proportion of live-to-dead rhodolith materials, suggesting an old bed deposit. Also, the amount of calcium carbonate material in the specimens is relevant to take in account in terms of the CO₂ balance worldwide.
ISSN:1438-387X
1438-3888
DOI:10.1007/s10152-013-0366-z