Endolithic Algae (Ostreobium) Diversity in Porites Corals at the Western Atlantic and Tropical Eastern Pacific

ABSTRACT Ostreobium comprises endolithic algae commonly seen in conjunction with scleractinian corals. In the past, it was solely recognized as a coral skeleton bioeroder. Their relationship with corals is critical because they give photosynthetic byproducts and help the coral when it loses its prim...

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Bibliographic Details
Published in:Marine ecology (Berlin, West) West), 2024-12, Vol.45 (6), p.n/a
Main Authors: Giraldo‐Vaca, Juan Sebastián, Sánchez, Juan Armando
Format: Article
Language:English
Subjects:
Algae
Biogeography
Caribbean
coral reefs
Corals
Endolithic algae
euendolithic algae
Genetic diversity
Genetic variation
Host specificity
Ordovician
Origins
Ostreobium
Photosynthesis
Porites
reef‐building corals
Scleractinia
symbiont
Symbionts
Tropical Eastern Pacific
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Summary:ABSTRACT Ostreobium comprises endolithic algae commonly seen in conjunction with scleractinian corals. In the past, it was solely recognized as a coral skeleton bioeroder. Their relationship with corals is critical because they give photosynthetic byproducts and help the coral when it loses its primary symbionts due to stress. The variety of these algae in coral species of the genus Porites in the Tropical Eastern Pacific and western Atlantic was investigated. Ostreobium samples from seven Porites species including two from the Tropical Eastern Pacific (TEP) (P. panamensis and P. lobata) and five from the Caribbean (P. furcata, P. porites, P. colonensis, P. branneri, and P. astreoides) were extracted. Published rbcL sequences from algae found within various coral species from other parts of the world were also compared. A biogeographic analysis and two methodologies, PTP (Poisson tree process) and GMYC (general mixed Yule‐coalescent), were used to delineate the different species. The findings revealed a significant degree of genetic diversity within Ostreobium, with more than 15 groups of not more than three individuals and 40 individual lineages. Its origins date back to the Ordovician, 500 Ma, and it does not appear to preserve host specificity. The sampled locations still have a wide variety of Ostreobium. Biogeographically patterns were also confirmed, making it impossible to pinpoint the precise origins of most clades. The ancestry analyses revealed convergent events for not only the emergence of Ostreobium in a few genera of local corals, but also the phenomenon occurred in genera from far‐off places.
ISSN:0173-9565
1439-0485
DOI:10.1111/maec.12832