Limnologica 25 (2)
(1995)129-140
LIMNOLOGICA
© by Gustav Fischer Verlag Jena
Institut für Zoologie und Limnologie
Universität Innsbruck, Österreich
Distribution Pattern of epilithic Macrozoobenthos in a small
meromictic Lake (Piburger See, Tyrol, Austria)*)
Leopold Füreder
With 6 Figures and 4 Tables
Key words: Lake benthos, hard Substrate, epilithic zoobenthos, epilithic algae, depth distribution,
littoral fauna, Oligochaeta, Crustacea, Chironomidae.
Abstract
For several years Piburger See, a mesotrophic meromictic Tyro-
lean lake, has been the subject of a comprehensive ecosystem
study, designed to produce a holistic picture of the structure and
function of the lake. In earlier investigations of the benthic
Community structure of Piburger See the hard Substrates, which
comprise about 16% of the whole lake bottom, were excluded
because of methodological difficulties. Here a modification of a
sampling method is described which enabled sampling the hard
Substrate quantitatively in a proper way. Zoobenthos was sampled
at six different depths from March to September 1990 by SCUBA
diving. 79 taxa of aquatic invertebrates were found to the hard
Substrates, however, only a few species dominated the benthic
Community. The benthic Community structure was charaterised
by three major taxonomic groups: benthic crustaceans, oligo-
chaetes and chironomid larvae.
Canthocamptus staphylinus
show-
ed the highest densities,
Vejdovskyella comata
and
Corynoneura
arctica
were important taxa within the Oligochaeta and the
Chironomidae. A comparison with earlier studies carried out in
the soft Sediments demonstrates the pecularity and characteristic
of the hard Substrate fauna.
Introduction
Since 1960, Piburger See has been the site of numerous
scientific investigations. Several projects have examined
the Community structure and production of invertebrate
meio- and macrozoobenthos: Chironomidae
(Schlott
1976), benthic Crustacea, especially Ostracoda and Cope-
poda
(Thaler
1977), Nematoda
(Pehofer
1977 & 1989),
Oligochaeta
(Girtler
1987), and the benthic Rotatoria
(Buhmann
1981;
Gabriel
1981;
Pinter
1981).
With the exception of the Rotatoria, which were sampled
from different Substrates of shallow areas in the littoral
zone, all of these investigations were restricted to soft
Sediments. The benthic communities populating hard sub-
strates (i.e. rocks, boulders, stones), which comprise about
16% of the lake area, have not been studied to date.
The surfaces of large rock faces and fields of boulders,
stones, and cobble are probably the most difficult of all
Substrates to sample
(Downing
1984). Rock faces must be
cleared of living material
in situ,
therefore, a diver is required,
especially in deeper water. A hydraulic sampler is probably
the best method for sampling the hard Substrates.
Table 1.
Piburger See (Tyrol, Austria): (A) Morphometric para-
meters, according to
Girtler
(1987), and (B) water budget (values
in mm water column per year, means from 1975 — 1980, according
to
Girtler
1987).
(A)
(B)
Surface area (m
2
)
133690
Evaporation
466
Volume (m
3
)
1835000
Surface outflow
3666
Length (m)
800
Oslzewsjy tube
2116
Width (m)
250
Precipitation
751
Shoreline (m)
1900
Surface inflow
3487
Maximum depth (m)
24.6
Groundwater inflow
2102
Mean depht (m)
13.7
Relative depth (%)
5.96
Dedicated to Professor Roland Pechlaner on the occasion of
his 60th birthday
Limnologica 25 (1995) 2
129
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