The Naturally Saline Environment of the Lower Lakes
An analysis refuting the ‘freshwater ecological character’ claims made by the SA Government DENR (and the RLCAG) - plant observations
It has been claimed by those advocating a ‘freshwater only’ policy for the management of the Lower Lakes of the River Murray, that for the past several thousands of years these lakes have been predominantly, if not virtually always, a freshwater wetlands environment.
The South Australian Government’s Securing the future ‘A long term plan for securing the Coorong, Lower Lakes and Murray Mouth’ (13 MB) for management of these 800 plus of square kilometres of lake and surrounding shorelines included these words through draft after draft of the public consultation process, (despite strong evidence to the contrary)
“ ---there is solid evidence that the Lower Lakes were predominantly freshwater, and the established ecological character reflects that history.”
‘Securing the future’ draft for public comment, December 2009, p82 and the final plan, June 2010, pg 139, see link above.
This short paper analyses the historical ecological character of the Lower Lakes shorelines through the descriptions given to ‘common plant species’ which have been deemed relevant to the grazing of stock on these lakeside lands.
A Reliable Source of Environmental Data?
The ‘Lower Lakes Plant Guide’ was published in 2009 (revised 2010) by the very groups responsible for promoting and implementing the ‘freshwater only’ policy stance outlined above, through the Lakes Hub community centre program of the SA Government Murray Futures project, and the Goolwa to Wellington Local Action Planning Board Inc,
And yet, analysis of the plant data contained in this publication demonstrates a historical ‘ecological character’ for these Lower Lakes shores which clearly was not predominantly fresh.
A Fair Consideration
The Lower Lakes Plant Guide (a 42 page ‘spring bound’ booklet, 2.67MB) describes itself as, “A Field Guide of Common Plant Species in the Lower Lakes, South Australia.”
It notes in its Introduction that,
“Livestock grazing is a major land use around the Lower Lakes region of South Australia, and has traditionally provided graziers with ideal conditions to establish their properties due to the availability of permanently fresh water.”
And it might be acknowledged here that following the construction of the barrages in the 1930s for the purpose of preventing incursions of saline water from the Southern Ocean when river flows were low, the lakes have for the past 70 years been artificially maintained as permanently fresh.
Not-with-standing the inevitable conflicts between the grazing of domestic stock and the maintenance of historic ecological character (which these groups claim to support), this plant guide booklet is aimed at graziers around the lake shores with fodder information and forage analysis as derived from a ‘Sustainable Grazing Trial’ which collected data from 11 sites around the Lakes to investigate “the effects of various grazing regimes on the lake edge and floodplain.”
The 39 plants included in the guide, “were those most commonly observed at the 11 trial sites, and around the Lower Lakes area.”
Thus the sample under consideration here can be considered to fairly represent the environment in which they grow, with common and widespread native plant species in particular giving an insight to the ‘historic ecological character’ of their habitats. Thus, they have not been selected by this author in a dishonest attempt to sway opinion away from the ‘freshwater only’ ideology.
Taking the whole sample of 39 plant species, 24 (61.5%) are noted to have salinity associations and/or tolerance.
23 plants (59% of the sample) are natives with 18 of these deemed to be particularly common and/or widespread in the Murray/Darling basin environment.
Of these 23, 14 (61%) of the natives under consideration, are noted to be associated with salinity in some way. (eg berry saltbush, coast spear-grass, salt club rush, Australian salt-marsh grass, salt couch, seablite, sea rush, etc).
Of the 16 introduced plant species commonly found around the Lakes, 10 (62.5%) are similarly noted to be associated with salinity.
The native species identified as being salt tolerant/salt associated are the more significant because their ecological development over the past several thousand years indicates an ongoing salinity component which must therefore have been a feature of the ecological character of this lakeside environment over that time.
To have 61% of the plants in this sample clearly identified as being salt tolerant/salt associated, (a sample selected very objectively for the purposes of an investigation devised by the very groups who insist in other contexts upon a ‘freshwater ecological character’ for these wetlands), confronts the claims for a ‘freshwater only’ history upon which the SA Government’s Department of Environment and Natural Resources has based its whole rationale for the long term future of the Lower Lakes
The evidence of ‘Bent Science’ presented in this paper is but one of a whole series of factual inconsistencies which independently refute the DENR contention that these lake environs have been “predominantly fresh water” with an “established ecological character that reflects that history” (Securing the future document DENR June 2010, pg 139)
It is time that the Murray Futures Project team of the SA Government’s DENR acknowledged these facts and modified the ‘long term plan’ accordingly with an objective analysis of the ecological advantages and disadvantages of allowing an estuarine system to develop when river flows are so reduced by drought that the alternative is to allow lake water levels to fall below sea level (as they did in the recent drought).
The disastrous ecological, social and economic consequences of acid sulphate soils, wind blown erosion of exposed lake bed, corrosion of structures, sand drift deposition along shore lines, emergency construction of bunds and regulators, slumping banks and impact on lakeside communities – all could have been avoided by opening the barrages appropriately to allow hydraulic connectivity between the ocean and the lakes and the development of a dynamic estuary at sea level for the duration of the drought.
It is perhaps ironic that the Goolwa to Wellington Local Action Planning Board and the DENR Lakes Hub/Murray Futures groups which jointly published this ‘Lower Lakes Plant Guide’ and provided the data which so clearly refutes the ‘historic freshwater ecological character’ claim, are also responsible for the publication and continued promotion of ‘A Fresh History of the Lakes: 1800s to 1935’ (Sim/Muller 2004) – a publication which sets out to prove the ‘freshwater only’ position. That the Sim/Muller document has been discredited and dismissed by this author on a number of occasions for its clearly demonstrated bias in selection and interpretation of data is perhaps not surprising given the contradictory evidence that abounds and yet it has been used as a key reference by the DENR in their ‘Securing the Future’ Long Term Plan to support of their ‘freshwater only’ policy.