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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Bibliographic Details
Main Author: Shaw, Emily Caitlin
Format: Doctoral or Postdoctoral Thesis
Language:unknown
Published: UNSW Sydney 2012
Subjects:
Online Access:https://dx.doi.org/10.26190/unsworks/16021
http://hdl.handle.net/1959.4/52490