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Abstract(s)
From the early days of phycology, coralline algae (CA) have been considered the most formidable
and widely distributed algae (Woelkerling, 1988). They compose an abundant and highly diverse
group, divided into geniculate (articulated) and non-geniculate species (crusts and rhodolith/maërl
forms). CA are present in almost every coastal ecosystem around the world, from the intertidal
to mesophotic zones (Johansen et al., 1981; Steneck, 1986; Foster, 2001). They are important
ecosystem engineers that provide hard, three-dimensional substrates for a highly diverse fauna
and flora (Nelson, 2009), building habitats like the globally distributed rhodolith (or maërl)
beds (Foster, 2001), and the large algal bioconstructions that abound in the Mediterranean
(coralligenous assemblages, intertidal rims; Ingrosso et al., 2018). In addition, the CaCO3
precipitation within cell walls leads to a high fossilization potential of CA, which are considered
the best fossil record among macrobenthic autotrophs since they first appeared in the Lower
Cretaceous (Aguirre et al., 2000). It also makes CA major carbonate producers (van der Heijden
and Kamenos, 2015), which, considering their abundance and wide distribution, gives them an
important role in oceanic carbon cycling and reef building (Adey, 1998; Chisholm, 2003; Martin
et al., 2006; Perry et al., 2008) and makes them a group of significant economic interest (Coletti
and Frixa, 2017). Like many other marine ecosystems, CA habitats will be negatively affected by
future climate change, e.g., due to reduced CA calcification/growth (Martin andHall-Spencer, 2017;
Cornwall et al., 2019) that may eventually lead to ecosystem degradation and reduction of habitat
complexity and biodiversity.
Description
Keywords
Biodiversity Photosynthesis Calcification Genetic and genotypic diversity Climate change Coralline algae
Citation
Publisher
Frontiers Media