D. Hodgson et al., THE PALEOLIMNOLOGY OF LAKE FIDLER, A MEROMICTIC LAKE IN SOUTH-WEST TASMANIA AND THE SIGNIFICANCE OF RECENT HUMAN IMPACT, Journal of paleolimnology, 18(4), 1997, pp. 313-333
Three meromictic lakes in the World Heritage Area of south-west Tasman
ia possess unusual microbiological communities. Their meromixis is mai
ntained by periodic incursions of brackish water from the nearby Gordo
n River which, in its lower reaches, is a salt-wedge estuary. In 1977
the construction of a dam in the middle reaches of the river restricte
d penetration of the salt-wedge and meromixis rapidly declined in all
three lakes. A palaeolimnological study was carried out on one of the
lakes, Lake I;idler, firstly to determine the history of meromixis and
its associated microbiological communities, and secondly to assess wh
ether the recent and rapid decline of meromixis is inconsistent with n
atural rates of development of the Gordon River meromictic lakes. One
part of this study included the analysis of the stratigraphy of fossil
diatoms from a 17-metre sediment core dating back 8000 yrs. Detrended
Correspondence Analysis and Analog Matching were used to compare diat
om species assemblages in core samples with diatom samples from a refe
rence dataset consisting of a selection of lake and river sites in the
lower Gordon River valley. Five distinct stratigraphic zones were ide
ntified in the core. These zones indicated specific stages in the deve
lopment of the Gordon River lakes from river backwaters to ectogenical
ly-maintained meromictic lakes which will, finally, become terrestrial
ised by encroaching rainforest. The onset of a stratified water column
was identified by the emergence of a dominant freshwater algal flora
which suggested that the lake had developed a mixolimnion and become m
eromictic ca. 2070 +/- 50 C-14 yrs ago. In the context of this long hi
story of meromixis, the rapid demise in meromictic stability following
construction of the dam is judged to be inconsistent with natural rat
es of development. The palaeolimnological studies, of which this paper
is one part, prompt recommendations for a management strategy to prev
ent the further decay of these meromictic lakes in the World Heritage
Area.