Original source · versioned page text
2016-12-12 General Committee - Attachments 1, 2, 3 to Item 10 - Oyster Restoration Project
The original of this document is very large (10.3 MB). Opening the original or downloading it may take a few minutes. Please be patient and don't click again. The page text is quick to read. If you are on mobile data, it is best to wait until you are on Wi-Fi.
Text sections have not been matched to the original PDF pages. Use the original document to check page numbers.
Ecological Service Professionals
Sustainable Science Solutions
By the late 1930s, the oyster fishery harvest in Southeast Queensland, including Noosa
Estuary, went into depression (Smith 1981). Ultimately it is thought the natural oyster banks
were unable to recover due to both the removal of live oysters and dead shell from the
Noosa system (Monks 2000, cited in Thurstan 2015; Smith 1985). Declining water quality
resulting in recruitment failure of oyster spat and disease has also been implicated in the
general decline of oyster banks in Moreton Bay (Diggles 2013).
Figure 6 Historical photo showing the large size of bagged oysters in 1908 (Smith 1981).
Identifying Current Oyster Accommodation Space
The accommodation space represents the area in an estuary with environmental conditions
suitable for growth of oysters (Volety 2013). Oysters grow from the intertidal to depths of at
least 20 metres and this is where much of the hand gathering or dredging of oysters has
historically occurred (Nell 2001). However, it is thought that due to changes in ambient
conditions and a variety of external factors, rock oysters in Southern Queensland are
typically found only in the intertidal zone and have been functionally lost from subtidal
habitats (Diggles 2013). Conditions suitable for optimal oyster growth are summarised in
Table 2, from Nell & Halliday (1988), Halliday (1995) and Rubio (2007).
Table 2 Temperature and salinity for optimum growth and tolerance limit
Parameter Units Life History Stage
Larvae Spat Adult
Temperature optimum growth °C 24-26 14-28 18-26
Temperature tolerance limit °C unknown 11-30 11-30
Salinity optimum growth ppt 23-39 20-40 25-35
Salinity tolerance limit ppt 15-39 0-40 0-50
Adult rock oysters are able to close their valve for several days if salinity is less than 15 ppt,
although prolonged periods of low salinity can cause death (Nell & Halliday 1988; Halliday
1995).
10
See the original
The page text is free to read. Viewing or downloading an original file needs an account.
Log in to see the originalVery large file: the download may take a few minutes. If you are on mobile data, it is best to wait until you are on Wi-Fi.
Searchable page text hides email addresses. Original files are unchanged and may show email addresses.