The macroalgal carbonate factory at a cool-to-warm temperate marine transition, Southern Australia

• Published in: Sedimentary Geology
• Main Authors: James, N., Reid, C., Bone, Y., Levings, A., Malcolm, I.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Elsevier Science BV 2013
• Subjects: Australia; Carbonates; Macroalgae; Temperate water; Bryozoans; Molluscs; Southern Ocean; New Zealand
• Online Access: http://hdl.handle.net/2440/79944; https://doi.org/10.1016/j.sedgeo.2013.03.007

The shallow neritic seafloor to depths of ~. 30. m along the coast of southwestern Victoria Australia, is the site of rocky reefs on volcanic and aeolianite bathymetric highs. The region, located near the warm- to cool-temperate environmental transition, is a site of prolific macroalgae (kelp) growth. Kelps are most prolific and diverse in high-energy, open-ocean environments whereas broad-leafed seagrasses, at their cold-water eastern limit, are restricted to local protected embayments. The seagrasses are reduced to one species of Amphibolis whereas the kelps are diverse and include the large intertidal bull kelp (Durvillaea), not present in warmer waters. The macroalgal forest extends from the intertidal to ~. 30. mwd (metres water depth) as a series of distinct biomes; 1) the Peritidal, 2) the Phaeophyte Forest (0-17. mwd), 3) the Rhodophyte Thicket (17-15. mwd), and 4) the Invertebrate Coppice (>. 25. mwd). The Phaeophyte Forest is partitioned into a Durvillaea zone (0-2. mwd), a Phyllospora zone (2-10. mwd) and an Ecklonia zone (10-17mwd). The two major habitats within each biome comprise 1) an upward facing illuminated surface that supports a macroalgal canopy over an understorey of coralline algae and herbivorous gastropods, and 2) a separate, cryptic, shaded habitat dominated by a diverse community of filter-feeding invertebrates. These communities produce two different sediments; 1) geniculate and encrusting corallines and diverse gastropods from the upper surface, and 2) bryozoans, molluscs, barnacles, chitons, serpulids, and benthic foraminifers from the shaded, cryptic habitats. These particles are blended together with the latter becoming proportionally more abundant with increasing depth. Results of this study, when integrated with recent investigations in warm-temperate (South Australia) and cool-temperate (New Zealand) environments now define carbonate sedimentology of the macroalgal reef depositional system in this part of the northern Southern Ocean. © 2013 Elsevier B.V. Noel P. James, ...