The role of non-skeletal carbonate component in Mediterranean Coralligenous: new insight from the CRESCIBLUREEF project

Mara Cipriani¹, Daniela Basso^2,3, Pietro Bazzicalupo², Marco Bertolino⁴, Valentina Alice Bracchi^2,3, Fabio Bruno⁵, Gabriele Costa^2,4, Rocco Dominici¹, Alessandro Gallo⁵, Maurizio Muzzupappa⁵, Antonietta Rosso^3,6, Francesco Perri¹, Rossana Sanfilippo^3,6, Francesco Sciuto^3,6 & Adriano Guido^1
1Department of Biology, Ecology and Earth Sciences, University of Calabria, Rende, Cosenza, Italy. ²Department of Earth and Environmental Sciences, University of Milano-Bicocca, Milan, Italy. ³CoNISMa-Italian National Inter-University Consortium for Sea Sciences, Roma, Italy. ⁴Department of Earth, Environmental and Life Sciences (DISTAV), University of Genoa Genoa, Italy. ⁵Department of Mechanical, Energy and Management Engineering, University of Calabria, Rende, Cosenza, Italy. 6 Department of Biological, Geological and Environmental Sciences, University of Catania, Catania, Italy.
Corresponding author e-mail: mara.cipriani@unical.it

In the frame of the project FISR_04543 “CRESCIBLUREEF - Grown in the blue: new technologies for knowledge and conservation of Mediterranean reefs”, we present preliminary data on the ecological and depositional implications of micritic sediments in a coralligenous bioconstruction formed along the Mediterranean shelf in front of the Marzamemi village (Sicily, Italy). The framework of the build- up is mainly built by crustose coralline algae, which in turn create the substrate for a high-diversified epi- and infaunal community. Two types of microcrystalline calcite, tentatively interpreted as allochthonous and autochthonous micrite, strictly related to fine skeletal debris, have been detected. The allochthonous micrite derive from abiotic accumulation of fine sediments in the framework cavities. The autochthonous micrite is deposited in situ through organic-mediated processes. The occurrence of this component allows hypothesizing a possible contribution of non-skeletal carbonate in the strengthening of the primary framework due to its syndepositional cementation.

Coralligenous reef, bioconstruction, micrites, Ionian Sea.