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Distribution Pattern of epilithic Macrozoobe... (1995)
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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

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