Carbonate chemistry variability in the southern Great Barrier Reef: implications for future ocean acidification
Ocean acidification occurs as a consequence of the absorption of anthropogenic CO2 emissions by the ocean, which lowers sea surface pH and carbonate ion concentrations over time. Ocean acidification has the potential to alter marine biogeochemical cycling and biological processes. Coral reefs are be...
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Format: | Doctoral or Postdoctoral Thesis |
Language: | English |
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UNSW, Sydney
2012
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Online Access: | http://hdl.handle.net/1959.4/52490 https://unsworks.unsw.edu.au/bitstreams/21921e3d-52b8-45f5-a24b-4282fc5fdc89/download https://doi.org/10.26190/unsworks/16021 |