Synonyms
Red algal nodules (balls or macroids); Rhodoids
Definition
Rhodoliths are defined as free-living nodules that are dominantly composed of calcifying red algae (mostly corallinaceae, occasionally peyssonneliaceae) commonly associated with other encrusters (foraminifera, bryozoans, bivalves, serpulid worms and/or corals). Their size ranges from less than 30 mm to about 300 mm (Bosellini and Ginsburg, 1971).
Habitat and biotic composition: Rhodolith deposits occur worldwide along shelves at euphotic depths (generally less than 150 m). The shape, internal structure, composition and growth rate of rhodoliths vary according to environment, water energy and depth. In reef provinces, the nodules from shallower, high to moderate energy environments (e.g., reef flats, proximal back-reefs and channels) exhibit massive spheroidal to branching ellipsoidal types, made up of mastophoroid (Hydrolithon, Neogoniolithon) and/or lithophylloid (Lithophyllum, Dermatolithon, Titanoderma)laminar...
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Bibliography
Bosence, D. W. J., 1983. The occurrence and ecology of recent rhodoliths – a review. In Peryt, T. M. (ed.), Coated Grains. Berlin: Springer, pp. 225–242.
Bosellini, A., and Ginsburg, R. N., 1971. Form and internal structure of recent algal nodules (Rhodolites) from Bermuda. Journal of Geology, 79, 669–682.
Reid, R. P., and Macintyre, I. G., 1988. Foraminiferal-algal nodules from the Eastern Caribbean: growth history and implications on the value of nodules as paleoenvironmental indicators. Palaios, 3, 424–435.
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Montaggioni, L.F. (2011). Rhodoliths. In: Hopley, D. (eds) Encyclopedia of Modern Coral Reefs. Encyclopedia of Earth Sciences Series. Springer, Dordrecht. https://doi.org/10.1007/978-90-481-2639-2_249
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