Bioerosion of the coralline alga Hydrolithon onkodes by microborers in the coral reefs of Moorea, Fr

By A. Tribollet, C. Payri. 2001

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In Ecology

In Oceanography

Citations in the corpus

Response of Mediterranean coralline algae to ocean acidification and elevated temperature (2009, background): “Dead thalli of coralline algae are calcareous substrate colonized by endolithic microorganisms in which the euendoliths (i.e. microboring cyanobacteria, algae, and fungi) promote high carbonate removal (Tribollet & Payri, 2001; Ghirardelli, 2002).”
Effects of elevated pCO2 on dissolution of coral carbonates by microbial euendoliths (2009, background): “Euendoliths can also dissolve carbonates of live organisms, but their boring activity is much greater in dead substrates [Le Campion-Alsumard et al., 1995; Tribollet and Payri, 2001].”
ENDOLITHIC MICROFLORA ARE MAJOR PRIMARY PRODUCERS IN DEAD CARBONATE SUBSTRATES OF HAWAIIAN CORAL REEFS 1 (2006, background): “…substrate including skeletons of live and dead corals (Le Campion-Alsumard et al. 1995, Tribollet et al. 2002), live and dead calcareous algae (Tribollet and Payri 2001), mollusc shells (Mao Che et al. 1996), and tests of foraminifera (Golubic et al. 1984) as well as compact limestone…”
Ocean acidification and warming decrease calcification in the crustose coralline alga Hydrolithon onkodes and increase susceptibility to grazing (2012, background): “onkodes was chosen as the study organism because it is a dominant species of coralline algae throughout the shallow reefs of the Indo-Pacific, where it is especially important in the accretion of reef caps (algal ridges) (Camoin and Montaggioni, 1994) and it can account for up to 90% of the living c”