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L. Campanella et al. / Environmental Pollution 111 (2001) 117±126  123

  The mean metal concentrations in biota and seawater       rather than in rhizomes is a well-established pattern,
are shown in Table 8, where only data from the four         our results matching those of many previous studies
clean sites are averaged. From these data it results that   (Sanchiz et al., 1990; Warnau et al., 1995; Schlacher-
accumulation ratios of the ®ve metals di€er both in         Hoenlinger and Schlacher, 1998a).
macrophytes and in molluscs. In P. oceanica metal
concentrations decrease in the following order:               In the present study, the opposite behaviour was
Zn>Cu>Cd>Pb>Cr while in P. pavonica the                     observed in the case of Cr and Pb. This ®nding matches
sequence is Zn>Cu>Pb>Cr>Cd. As for molluscs,                those of Warnau et al. (1995) and Schlacher-Hoenlinger
the following sequences were observed: Zn>Cu>Cd>            and Schlacher (1998a). However, Sanchiz et al. (1990)
Cr5Pb in M. turbinata; Zn>Cd>Cu>Cr>Pb in P.                 described the sequence old leaves>rhizomes>young
caerulea.                                                   leaves, while Catsiki and Panayotidis (1993) reported
                                                            somewhat erratic results, with inversions of the accu-
  As far as net accumulation is concerned, P. caerulea      mulation ratio between leaves and rhizomes depending
turned out to be the strongest accumulator for Cd, P.       on the sampling area.
pavonica for Cr and Pb, M. turbinata, P. oceanica and P.
pavonica for Cu, P. oceanica for Zn. Very high con-           The almost constant Cu content observed in all plant
centration factors (1.0Â104Ä 3.4Â104) can be calculated     tissues (as in Warnau et al., 1995), can be supposed to
in these cases with reference to soluble metal concentra-   arise from a certain regulation capability of the phaner-
tions in ambient seawater. Anyway it must be kept in        ogam. Again, con¯icting results can be found in the lit-
mind that in the studied organisms the actual uptake        erature (Catsiki and Panayotidis, 1993; Schlacher-
mechanisms are probably rather complicated because          Hoenlinger and Schlacher, 1998a), so that further stu-
their exposure to trace elements is not limited to soluble  dies are needed to fully elucidate this point.
metals in the aquatic medium. The metal uptake from
food, in the case of molluscs, and from sediments             In leaf material Cd, Cr, Pb and Zn concentrations
(through the roots) in the case of seagrasses, cannot be    decrease in the following order: leaf tip>whole leaf
ignored. As both mollusc species here considered are        >leaf basal tissue. This trend is consistent with the
herbivorous, it can be supposed that the metals accumu-     observation that the seagrass leaves grow by formation
lated in the algae on which they graze fairly a€ect their   of new tissue at the base. Therefore, the tip becomes the
overall uptake.                                             older part of the leaf, hence the tissue with a longer
                                                            exposure to metal loads in the ambient habitat.
4. Discussion
                                                              As regards absolute metal contents, levels recorded in
  The picture of bioavailable metal loads in the di€erent   this study at clean stations, generally fall in the range of
sites of the experimental area provided by the four         the lowest values available in the literature.
selected organisms is rather univocal. An overall trend
of increased metal concentrations in station 5 is clear,      In detail, our data concerning the leaves of Posidonia
especially for Cd, Pb and Zn. Moreover, many correla-       oceanica are well below those previously reported in the
tions between metal contents were observed in the four      case of Cr and Pb, while for Cu and Zn the results we
species.                                                    obtained are only slightly lower than the mean values
                                                            described elsewhere (Table 9). As for Cd, our mean
  The results of the study on metal distribution in the     level is lower than those previously reported, with the
tissues of Posidonia oceanica are particularly mean-        exception of the surprisingly small one observed by
ingful. In fact the di€erent behaviour of the metal cou-    Schlacher-Hoenlinger and Schlacher (1998a) in speci-
ple Cd±Zn on the one hand, and Cr±Pb on the other,          mens collected at Ischia (Bay of Naples, Italy). In Padina
suggests di€erent uptake and distribution routes for        pavonica the observed levels of Cd and Cr are generally
these elements. The highest concentration of Cd and Zn      lower than those previously reported, while Pb, Cu and
in leaves versus rhizomes leads to the hypothesis of a      Zn contents are higher (Catsiki et al., 1991; Tariq et al.,
preferential uptake of these elements from water to the     1991; Schlacher-Hoenlinger and Schlacher, 1998b).
photosynthetic tissue. Warnau et al. (1996) reported
that Cd and Zn were linearly accumulated from ambient         Very few data are currently available on trace metals
water by seagrass shoots during a 15-day experiment.        concentrations in the gastropod molluscs selected in the
However, in a ®eld study on a contaminated area,            present study. However, our values, except for Cd, are
Malea et al. (1994) described a signi®cant positive cor-    lower than those reported by other authors (Ozretic et
relation between Cd concentrations in leaves and those      al., 1990; Nicolaidou, 1994).
in sediments. Therefore, an ecient distribution from
roots to green tissues cannot be excluded. Anyway,            In the light of the foregoing remarks, the metal con-
the preferential accumulation of Cd and Zn in leaves        centrations in the organisms collected at the `clean' sta-
                                                            tions may be considered as useful background levels to
                                                            which to refer for intraspeci®c comparison within the
                                                            Mediterranean area. It must be noted that in the pres-
                                                            ent context the notion of `background levels' has a
                                                            somewhat relative meaning, as local geochemical or
                                                            hydrodynamic conditions may always shift `natural'
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