There are samples being taken and a research project being put together right now I understand that is designed to answer exactly that question. Surface salinity now around Bribie is 15ppt (9 ppt close to the island) and 23ppt on the surf beach with suspended solids and clarity that suggests pelagics will take a while to come back. The bottom sediments will be exposed to the same sort of muck that people have been sweeping out of flooded houses. Yes, its a one off event, but expecting recovery when the underlying problems with the bay remain unaddressed and unchanged is very optimistic and not at all realistic.
Studies of cores from 400 year old corals shows that sedimentation during floods was historically not a problem up until around 1870, after which european land use practices (tree clearing, agriculture and urban development) in river catchments along the QLD coast resulted in increased in sedimentation (around an order of magnitude or more) higher than historical backgrounds prior to european settlement, resulting in sedimentation problems that stifle coral, oyster and other biogenic reef habitat. These issues continue to get worse as population grows and development progresses. Same for toxic Lyngbya blooms, they were not recorded before the late 1990's but since then have increased in frequency and severity, due to increased nutrient availability (mainly P) and also increased availability of complexed iron (the latter from disturbance of acid sulphate oils by development).
re: Moreton and Stradbroke Islands, Ward (1978) shows they were actually formed during the previous glacial period and represent holocene drowning of mainly Quaternary sediment deposits that were many miles inland, not due to sediments from the river. Oldboot, you could do worse than look at
http://espace.library.uq.edu.au/eser...rd-dgp-8-2.pdf
Oh, and if waterflows were twice as much as the 1974 floods, why was the river height at the brisbane city gauge around a meter less than 1974 ? Yes, rainfall may have been twice as much, but the river flows were mitigated by Wivenhoe dam. And re: the dam, the engineers don't lie, you could clearly see looking at http://www.bom.gov.au/fwo/IDQ65389/I...0177.plt.shtml how close it got, and you could track how once the level exceeded 74 meters, they opened up the dam fully and even then, the height climbed for a while before the rain slowed down and they got control back. That is why they have a fuse plug in the dam to form a secondary spillway as a safety valve - when it rains very heavily in such a large catchment it is possible for dam inflows to exceed the outflow capacity of the 5 gates, and the dam is not designed to be overtopped. It is also very clear and widely covered in the media they were releasing water from all 5 gates (partially open) in the leadup to the severe rain events of the 10 and 11 jan, check it out here http://www.seqwater.com.au/public/dam-levels , select wivenhoe and go to a month timescale to see the releases leading up to the severe rain event.