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Prada, F.

Publications and source records attributed to Prada, F..

2 recordsLinked to original sources

Novel insights into conserved biomineralization mechanisms revealed from a cold-water scleractinian coral skeletal proteome

Stony corals exhibit striking morphological plasticity across diverse environments and trophic strategies, raising fundamental questions about the conservation of their biomineralization machinery. Here, we characterize the skeletal organic matrix proteome of the cold-water, asymbiotic coral Desmophyllum pertusum and compare it with skeletal proteomes from a facultatively photosymbiotic temperate coral and an obligately photosymbiotic subtropical coral. Despite pronounced differences in habitat, symbiotic status, and skeletal micro-density, we observe convergence on a conserved "biomineralization toolkit". Comparative proteomics, genomics, and structural predictions reveal that this toolkit integrates diverse acidic matrix proteins, carbonic anhydrases, adhesion and structural proteins, and signaling components with multiple cellular export pathways. Together, these findings redefine coral biomineralization as a dynamic, coordinated network of cellular pathways rather than a static assemblage of matrix components. The symbiont-free model D. pertusum provides a mechanistic framework for dissecting coral calcification across environments and for assessing the resilience of this conserved machinery.

biochemistry↗

Insights on Chamelea gallina growth dynamics from the Holocene climate optimum in the Northern Adriatic Sea (Italy)

The fossil record documents ecological responses to past climate transitions, providing insights into future scenarios of marine ecosystems and taxa under climate change. In this study, we compared shell growth dynamics, specifically linear extension and net calcification rates, of the bivalve Chamelea gallina between Northern Adriatic Sea (NAS) assemblages from the Holocene Climate Optimum (HCO, 9-5 kyr cal. B.P.) and today. This species is a valuable economic resource, currently threatened by climate warming and numerous anthropogenic stressors. During the HCO, regional sea surface temperatures were warmer than today, making it a potential analog for exploring ecological responses to increasing seawater temperatures predicted in the coming decades. By combining standard aging methods with reconstructed sea surface temperatures, we observed a significant reduction in linear extension and net calcification rates in warmer HCO assemblages. During the HCO, immature C. gallina specimens developed a denser shell, especially during their early growth stages, at the expense of a linear extension rate, which was lower than modern specimens. This resulted in an average delay of 3-4 months in reaching sexual maturity, which is currently reached after ~ 13-14 months or at a length of ~18 mm. Several environmental factors are probably responsible for these differences between fossil and modern assemblages. Temperature indirectly impacted the geomorphologic evolution of the NAS over the Early-Mid Holocene, shaping the outlet structure of the Po and other NAS rivers. This, in turn, affected environmental factors such as nutrient load, seawater transparency, salinity, and phytoplankton. In addition, recent anthropogenically-derived decreases in natural NAS predators of infaunal bivalves may have reduced the natural predation pressure on modern C. gallina, thus favoring those populations characterized by faster linear extension rates (at the expense of a higher shell density), especially during the initial stages of life, hence facilitating a quicker attainment of sexual maturity.

paleontology↗