Experimental studies on microbial bioerosion at Lee Stocking Island, Bahamas and One Tree Island, Great Barrier Reef, Australia: implications for paleoecological reconstructions

By K. Vogel, M. Gektidis, S. Golubić, W. Kiene, Gudrun Radtke. 2000

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Effects of elevated pCO2 on dissolution of coral carbonates by microbial euendoliths (2009, background): “O. quekettii is oligophotic [Lukas, 1978] and penetrates the deepest into carbonate substrates, mostly perpendicular to the surface [Chazottes et al., 1995; Kiene et al., 1995; Vogel et al., 2000; Tribollet, 2008b].”
Shallow-water Desmophyllum dianthus (Scleractinia) from Chile: characteristics of the biocoenoses, the bioeroding community, heterotrophic interactions and (paleo)-bathymetric implications (2005, background): “terebrans occurrences down to 100 m depth (Vogel et al. 2000).”
Bioerosion: the other ocean acidification problem: Towards a Broader Perspective on Ocean Acidification Research Part 2 A special issue of the ICES Journal of Marine Science (2017, background): “…substrate to a depth of several mm, depending on the translucency of the material and their specific ability to use a given light environment for photosynthesis (Highsmith, 1981; Chazottes et al., 1995; Shashar et al., 1997; Gektidis, 1999; Vogel et al., 2000; Ralph et al., 2007; Tribollet, 2008a).”
The boring microflora in modern coral reef ecosystems: a review of its roles (2008, background): “In general, the bathymetric distribution of euendolithic assemblages in coral reefs has been well documented and will not be detailed here (see Golubic et al. 1975; Kiene et al. 1995; Radtke et al. 1996; Radtke et al. 1997a; Gektidis 1999; Hoffmann 1999; Vogel et al. 2000).”