Pergamon
PII: S0025-326X(98)00161-6
Mamw Pollutiolt Bulletim Vol, 36, No. 3, pp. 193-2(10, 1998
© 1998 Elsevier Science Ltd. All rights reserved
Printed in Great Britain
0025-326X/98 $19.00+0.00
The Sandhopper Talitrus saltator as a
Trace Metal Biomonitor in the Gulf of
Gdansk, Poland
P. S. RAINBOW*:[:, W. FIALKOWSKIt and B. D. SMITH*
*School of Biological Sciences, Queen Mary and WestfieId College, London E1 4NS, UK
tDepartrnent of Hydrobiology, Jagiellonian University, ul. Oleandry 2a, 30-063 Krakow, Poland
There are significant differences between the accumu-
lated trace metal concentrations (Zn, Cd, Cu, Pb, Ag,
Ni, Fe, Mn) of the talitrid amphipod crustacean
Talitrus saitator collected from the strandline of sites
around the Gulf of Gdansk, Southern Baltic in July
1996, after allowance for size effects by analysis of
covariance. These have resulted from significant
geographical differences in the local bioavailabilities of
trace metals, which are variably dependent on outflows
from the River Vistula (Zn, Cd, Fe, Mn) or from local
sources around the Gulf (Cu, Pb). The use of an easily
collected littoral organism has established a baseline
measure of local trace metal pollution against which
future changes can be compared. © 1998 Elsevier
Science Ltd. All rights reserved
Keywords: biomonitoring; trace metals; Gulf of
Gdansk; Baltic; Talitrus; amphipod crustacean.
The Gulf of Gdansk on the northern coast of Poland
lies at the southern end of the Baltic Sea (Fig. 1). In
the north the Gulf is bordered by the Hel Peninsula
with the town of Hel at the tip. The western part is
represented by the Bay of Puck, the innermost shallow
part of which (Inner Bay of Puck or Puck Lagoon) is
separated with its own pattern of water circulation
(Cyberski and Nowacki, 1993). To the south lie the
three adjoining cities of Gdynia, Sopot and Gdansk. To
the immediate east of Gdansk are the three main
direct outlets of the River Vistula, the basin of which
occupies more than half the area of Poland and
includes the major industrial regions and cities of
Katowice, Krakow and Warsaw.
The Gulf of Gdansk has dissolved concentrations of
the trace metals zinc, copper, cadmium and lead that
are greater than those in the adjacent southern Baltic
SPresent address: Department of Zoology, The Natural History
Museum, Cromwell Road, London SW7 5DB, UK.
Sea proper (Korzeniewski and Neugebauer, 1991).
There is evidence of anthropogenic input of these four
trace metals (Szefer, 1990), copper and zinc via the
River Vistula and cadmium and lead via the
atmosphere (Korzeniewski and Neugebauer, 1991).
Furthermore analyses of bottom sediments in the
region of the Gulf of Gdansk indicate raised concen-
trations of zinc, lead and manganese in the vicinity of
Gdynia (Szczepanska and Uscinowicz, 1994).
Analyses of biological material also indicate the
presence of raised trace metal bioavailabilities in the
region of the Gulf of Gdansk. The green alga Clado-
phora mpestris collected in the Bay of Puck had higher
manganese contents than did specimens of the same
alga from the coast of the open Baltic Sea (Szefer and
Skwarzec, 1988). Mytilus edulis collected sublittorally
from two sites, one in the Bay of Puck and the other
south of Hel, appeared to have high soft tissue concen-
trations of zinc, cadmium, lead, nickel, manganese and
iron (but not of copper nor cobalt) in comparison with
mussels collected elsewhere in the world (Szefer and
Szefer, 1985). Szefer and Wolowicz (1993) reported
elevated levels of zinc and cadmium in another sublit-
toral bivalve Cerastoderma glaucum from the Gulf of
Gdansk, compared with the same cockle from sites in
France and the Mediterranean.
The aim of this study was therefore to carry out a
trace metal biomonitoring survey of the Gulf of
Gdansk using biomonitors easily collectable from the
shore to provide both a picture of present local
geographical variability in the bioavailabilities of trace
metals, and a baseline against which future surveys
could be measured. It will thus be possible to monitor
the efficacy of any future projects reducing metal
emissions into the River Vistula or limiting local
coastal emissions of metals in solution or atmospher-
ically. It was originally hoped to use a suite of biomoni-
tors in this study including for example littoral
seaweeds, barnacles and talitrid amphipods (see
Rainbow, 1995b), but in the event it was possible to
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