Maerl (also rhodolith) is a collective name for non-geniculatecorallinered algae with a certain growth habit.[1] Maerl grows at a rate of c. 1 mm per year.[2] It accumulates as unattached particles and forms extensive beds in suitable sublittoral sites.[3] The term maerl originally refers to the branched growth form of Lemoine (1910)[4] and rhodolith is a sedimentological or genetic term for both the nodular and branched growth forms (Basso et al., 2015).[5] The terms rhodolith and maerl are used in very similar ways. A study in 2023 clarifies that maerl refers to only living, branched coralline thalli, while rhodolith includes unattached coralline red algae, both dead and alive.[6]
^Steneck, R. S. (1986). "The Ecology of Coralline Algal Crusts: Convergent Patterns and Adaptative Strategies". Annual Review of Ecology and Systematics. 17: 273–303. doi:10.1146/annurev.es.17.110186.001421. JSTOR2096997.
^Vize, S.; Blake, C.; Hinojosa, G. and Maggs, C.A. 2003. The distribution and composition of maerl beds in Northern Ireland. PMNHS Newsletter No.13 p.26
^Lemoine (1910). "Répartition et mode de vie du maërl ( Lithothamnium calcareum) aux environs de Concarneau (Finistère)". Annales de l'Institut Océanographique. 1: 1–29.