Study of coastal freshwater lakes in southern New South Wales

1997 ◽  
Vol 48 (3) ◽  
pp. 249 ◽  
Author(s):  
B. V. Timms
Keyword(s):  
Indicator Species ◽  
New South ◽  
New South Wales ◽  
Coastal Dunes ◽  
Coastal Dune ◽  
Freshwater Lakes ◽  
South Wales ◽  
Dune Lakes ◽  
Coastal Sand ◽  
Southern Species

There are few freshwater lakes associated with coastal dunes in southern New South Wales (NSW). Lake Nargal near Narooma, Bondi Lake near Bega, and a small lagoon near Pambula have little in common limnologically with coastal dune lakes of northern NSW and southern Queensland. They differ in mode of origin, are less dominated by NaCl, are less acidic, are more speciose, have few characteristic dune-lake indicator species, and moreover contain certain southern species. However, a re-examination of data for Lakes Windermere and McKenzie further north at Jervis Bay suggest that these are classic dune-contact lakes rather similar to those in northern NSW. Differences and similarities are largely influenced by the extent and therefore the hydrological influence of the contextural coastal sand mass and by biogeography.

Dragonflies (Odonata) of coastal sand-dune fresh waters of South-eastren Queensland and North-eastern New South Wales

1982 ◽  
Vol 33 (1) ◽  
pp. 77 ◽  
Author(s):  
AH Arthington ◽  
JAL Watson
Keyword(s):  
Physicochemical Properties ◽  
Sand Dune ◽  
New South ◽  
New South Wales ◽  
Physicochemical Characteristics ◽  
Coastal Sand Dune ◽  
Freshwater Streams ◽  
South Wales ◽  
North Eastern ◽  
Coastal Sand

The Odonata and physicochemical properties of freshwater streams, lakes, ponds and bogs in the sand-dune systems of Fraser, Moreton and North Stradbroke Islands and Cooloola, Queensland: and Wooli, New South Wales, are described. The odonate faunas of these dune masses show some differences from those of nearby areas, and there are close associations between some species and particular types of dune fresh water. Although no physicochemical characteristics were identified that might limit these dune dragonflies to their specific habitats, the lake-dwellers in particular may be useful indicators of environmental change.

Chemical composition of some inland surface waters and lake deposits of New South Wales, Australia

1970 ◽  
Vol 21 (2) ◽  
pp. 103 ◽  
Author(s):  
WD Williams ◽  
KF Walker ◽  
GW Brand
Keyword(s):  
Major Ions ◽  
New South ◽  
New South Wales ◽  
Salt Lakes ◽  
Salinity Range ◽  
Freshwater Lakes ◽  
South Wales ◽  
Major Cations ◽  
Rivers And Lakes ◽  
Lake Deposits

Chemical data are presented for several lakes and two impoundments on the Kosciusko and Monaro plateaux in south-eastern New South Wales, and for two rivers (Paroo and Darling), several freshwater lakes, and deposits from some dry salt lakes in western New South Wales. The concentrations of the major cations and anions, nitrate plus nitrite, and orthophosphate were investigated. For lake deposits, only major ions were investigated. The Kosciusko lakes were extremely fresh (salinity <3 p.p.m.) and chemically dominated by sodium and either bicarbonate, chloride or sulphate ions ; the Monaro peneplain lakes had a considerable salinity range (69-21,244 p.p.m.), and, with increasing salinity, sodium and chloride quickly assumed dominance. The Paroo and Darling Rivers had salinities <400 p.p.m, and the western freshwater lakes <850 p.p.m.; in both rivers and lakes, sodium and bicarbonate were the dominant ions. Deposits from dry salt lakes were mainly sodium chloride.

Late Quaternary Evolution of Coastal Sand Barriers, Port Stephens-Myall Lakes Area, Central New South Wales, Australia

1981 ◽  
Vol 15 (3) ◽  
pp. 345-364 ◽  
Author(s):  
B.G. Thom ◽  
G.M. Bowman ◽  
P.S. Roy
Keyword(s):  
Late Quaternary ◽  
New South ◽  
Tectonic Setting ◽  
New South Wales ◽  
Coastal Dunes ◽  
Last Interglacial ◽  
South Wales ◽  
Westerly Winds ◽  
Coastal Embayments ◽  
History Of

AbstractThe geomorphic and stratigraphic history of six coastal embayments has been studied in the vicinity of Newcastle, New South Wales (N.S.W.), Australia, in order to determine modes of deposition, and the degree to which marine and estuarine deposits can be correlated and dated. Each embayment possesses its own distinctive suite of landforms ranging from those dominated by coastal dunes to those in which beach ridges occur. In four of the bays dual sand barriers, comprising an Inner Barrier and an Outer Barrier, provide the framework for correlation between embayments. Six stages are recognized in the deposition of late Quaternary sediments in this area: (i) Pre-Last Interglacial, involving accumulation of separate composite units consisting of estuarine clays and transgressive dune complexes; (ii) Last Interglacial stage during which Inner Barriers were formed; (iii) Last Glacial reworking of barrier and dune sands by westerly winds; (iv) Postglacial Marine Transgression during which the Outer Barriers were initiated; (v) Mid-Holocene stage following cessation of sea-level rise ca. 6000–6500 yr B.P. on this coast, and involving progradation of Outer Barriers in some embayments; and (vi) Late Holocene episodic eolian reworking of dune complexes and Outer Barriers. The relatively high wave and wind energy as well as the tectonic setting of the central N.S.W. coast results in somewhat different geomorphic histories from barrier-island coasts in North America and Europe.

Mycorrhizas and Root Attributes of Plants of Coastal Sand-Dunes of New South Wales

1989 ◽  
Vol 16 (1) ◽  
pp. 141 ◽  
Author(s):  
VS Logan ◽  
PJ Clarke ◽  
WG Allaway
Keyword(s):  
Root Length ◽  
Sand Dune ◽  
New South ◽  
Sand Dunes ◽  
New South Wales ◽  
Arbuscular Mycorrhizal ◽  
Coastal Sand Dunes ◽  
South Wales ◽  
Vesicular Arbuscular ◽  
Coastal Sand

Root samples of 41 sand-dune plant species in 28 families were collected from sites along the coast of New South Wales during spring 1987. Of the species, 36 had vesicular-arbuscular mycorrhizas, with vesicles and internal and external hyphae. Among these species there was great variation in the pro- portion of root length colonised by vesicular-arbuscular mycorrhizal fungi (from 1 to 96%); in 33 species over 10% of root length was infected. Of the vesicular-arbuscular mycorrhizal species, 21 showed arbuscules, and 16 had intracellular hyphal coils. In four plant species mycorrhizas were not found in the single samples examined; ericoid mycorrhizas were present in the remaining species, Leucopogon parviflorus, but its vesicular-arbuscular mycorrhizal status could not be assessed. The results, though preliminary, may reflect a high vesicular-arbuscular mycorrhizal status of vegetation of coastal sand-dunes of New South Wales. This would be likely to enhance plant nutrition and sandbinding, and to have implications for sand-dune management.

Coastal dune waterbodies of north-eastern New South Wales

1982 ◽  
Vol 33 (2) ◽  
pp. 203 ◽  
Author(s):  
BV Timms
Keyword(s):  
New South ◽  
Coastal Dunes ◽  
South Wales ◽  
Eastern Australia ◽  
Water Tables ◽  
North Eastern ◽  
Dune Lakes ◽  
Littoral Invertebrates ◽  
Physicochemical Features ◽  
Solids Content

Twenty-two lakes, swamps and ponds on, or adjacent to, siliceous coastal dunes from Newcastle to Tweed Heads were investigated. Most of the waterbodies originated by deflation, with organic accumulation and development of perched water-tables involved in establishing those in higher dunes inland. Some were located in depressions in hard rock, blocked by dunes. Most had low total dissolved solids content with Na+ and Cl- dominant, but in and near frontal dunes Ca2+ and HCO3- were important and salinity was higher. Dissolved organic matter coloured the water of those with swampy environs. Humic waters were markedly acidic, frontal dune ponds alkaline, and lakes in contact with dunes near neutral. The physicochemical features of the only waterbody connected to the sea, Blue Lagoon, varied spatially and temporally with rainfall. Lake muds were dys. The dominant plants were all emergents, with Lepironia auriculata (Retz) prominent in most waterbodies on or near leached dunes. Calamoecia tasmanica (Smith) dominated the plankton; species diversity was higher in lakes in contact with dunes than in those surrounded by leached dunes. No euzooplankters were recovered from frontal dune ponds or Blue Lagoon. Overall, littoral invertebrates were reasonably diverse but limited in frontal dune ponds. Most notable was the restriction of molluscs and ostracods to sites on or adjacent to frontal dunes, the presence of some characteristic microcrustaceans in sites on or near leached dunes, and the ubiquity of many insect groups, particularly hemipterans and coleopterans. Benthos was depauperate in species and numbers in lakes surrounded by leached dunes; diversity and standing crops were higher in lakes in contact with dunes. <P.A typology scheme, based on, and showing the interrelationships between, mode of origin, water chemistry and salient biological features, showed much greater heterogeneity among dune lakes in eastern Australia than previously thought.

Endogone spores in Australian sand dunes

1975 ◽  
Vol 53 (7) ◽  
pp. 668-672 ◽  
Author(s):  
R. E. Koske
Keyword(s):  
New South ◽  
Sand Dunes ◽  
New South Wales ◽  
Coastal Sand Dunes ◽  
South Wales ◽  
Coastal Sand ◽  
Mobile Dunes

Five types of spores of the endomycorrhizal fungus, Endogone, were abundant in the coastal sand dunes of New South Wales. Spores of Endogone have seldom been reported from marine dunes, and at least two of the spore types recovered from Australian dunes have not previously been reported from this continent. The density of spores in sand was greater in older, more stabilized dunes than in younger foredunes and mobile dunes.

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