When the rains come and the land floods, the springs are often connected and historically this allows for colonisation of new springs and the maintenance of genetic diversity. Unfortunately, these flood events have also provided a foothold for the invasive Eastern mosquito fish to get into the last stronghold of the endemic fish.
There was a noticeable decline of the endemic fish on the property before Bush Heritage acquired it but through the efforts of staff and volunteers, these species have been preserved.
The largest threat to these endemic fish is the Eastern mosquito fish. The main techniques for protecting the endemics include translocation of endemic fish to new springs, fencing of endemic occupied springs and eradication of the mosquito fish.
The fish have all been studied before, to varying degrees, but there's a gap in our knowledge that I attempted to fill in my honours year, which can be broken into three parts.
Part 1: understanding their environment
If you look at large bodies of water like lakes, the physiochemistry of the water is relatively stable and while things such as temperature or pH change seasonally, there aren’t normally dramatic changes over very short time periods.
These gradual seasonal changes are normally slow enough that the species living in the water can slowly adjust as sudden changes can be lethal. Edgbaston springs are nothing like that. They fluctuate so much!
The most consistent area of the springs is around the vent, where ancient water from the Great Artesian Basin bubbles up alkaline, devoid of oxygen at approximately 24°C.
Once in the spring, the physiochemistry fluctuate massively across both time and the spring itself, far more than what most fish are ever exposed to.
I measured the temperature, dissolved oxygen, conductivity and pH of the springs and saw large changes both seasonally and over 24 hours. Part of this is because of how shallow they are. My sense of depth changed rapidly working in these springs – I saw baby gobies in water only millimetres deep and depths greater than 300mm felt like the Mariana’s trench of arid springs.
As the sun baked the ground during the day, the springs changed depth and size. As water evaporated, the dissolved minerals in the waters join the salt crusts (trona) already edging the springs.
I saw water temperatures as high as 48°C and pH ranged from pH7- pH9.83. They were nearly devoid of oxygen at night and hyper saturated during the day. In the space of 24 hours, the springs have been recorded fluctuating as much as 27°C and are known to be close to freezing in winter. For many species, these sort of extreme values and fluctuation would be lethal!