Comparing metal uptake between a halophyte and a glycophyte
Environ. Toxicol. Chem. 21, 2002
2703
consisting of 15% Fe, 2% Cu, 0.2% Pb, and 0.25% Zn, among
other metals. Very few plants are actually found growing di-
rectly in the mine tailings on site. It is presumed that the high
heavy metal loading found for this soil is solely responsible
for the lack of natural plant establishment in the contaminated
soil both in the greenhouse and on site. The contaminated soil
is slightly more acidic and saline than the uncontaminated soil,
but when mixed with mulch and soil conditioner, the contam-
inated soil supported adequate plant growth.
Effective phytoextraction requires that plants be both metal
tolerant and accumulate metal in the aboveground tissue. It
has been suggested that salt-tolerant plants may be better
adapted to coping with environmental stresses, including
heavy metals [7,21], than salt-sensitive (glycophytic) crop
shoots than the glycophyte, especially Zn. Likewise, Williams
et al. [23] report that a number of halophytes (Atriplex in-
cluded) growing in a heavy metal–polluted salt marsh in the
United Kingdom exhibited similar shoot-to-root ratios. The
selective translocation of Zn (among a variety of other metals
found in our soil) by Atriplex would suggest that salt tolerance
confers an advantage in regulating ion uptake over salt sen-
sitivity. Although we compared only one representative hal-
ophyte to one representative glycophyte in this study, a similar
study comparing the response to Cu stress between Messem-
bryathemum crystallinum (another halophyte) and Arabidop-
sis thaliana (a glycophyte) demonstrated enhanced Cu uptake
and higher Cu tolerance by M. crystallinum [7]. Taking into
consideration our data and those reported elsewhere [6–11], it
can be suggested that halophytes may be superior plants for
long-term establishment in co-metal-contaminated soils.
It could also be argued that since Z. mays is a monocot
and A. nummularia a dicot, the comparison in metal uptake
between these two plants is somehow complicated by the an-
atomical and physiological differences between these plants.
Nevertheless, our results are consistent with current salt-tol-
erance research [6,21,24]. In general, halophytes such as Atri-
plex are more restrictive in regulating salt/mineral intake via
the roots than glycophytes. Furthermore, some halophytes
characteristically translocate and store salts/minerals in vac-
uoles found in the leaf tissue, providing for greater osmotic
control/water movement [6,24]. Therefore, they tend to trans-
locate ions from roots to shoots more effectively than gly-
cophytes. Thus, the basic differences between halophytes and
glycophytes observed with respect to Na uptake and transport
appear to apply to heavy metals as well, though the differences
we observed were not nearly as large as those observed for
Na.
plants (Z. mays, B. juncea, P. sitivum, and so on) commonly
chosen for phytoextraction research. In this study, growth of
both the halophyte and the glycophyte was stunted in the con-
taminated soil:mulch mixture compared to the uncontaminated
soil:mulch mixture. When comparing the two plant types, the
glycophyte had a faster growth rate than the halophyte re-
gardless of the soil:mulch mixture. Despite their slower growth
rate, halophytes such as A. nummularia are known to achieve
biomass yields as high as 30 t/ha even under salt stress con-
ditions [6]. Further, unlike Z. mays, which is an annual plant,
A. nummularia is a perennial plant that continues to accu-
mulate biomass at an exponential rate throughout the growing
season (E.P. Glenn, personal communication). It should be
noted that the slower growth rate of the halophyte did not
correspond to a decrease in metal uptake. In fact, both plants
accumulated similar levels of metals (on a mass basis), but
the symptoms of metal toxicity (stunted growth and chlorosis)
demonstrated by the halophyte were far less severe than those
demonstrated by the glycophyte when sown in the contami-
nated soil:mulch mixture.
Results from this study confirm that EDTA can solubilize
metals from the soil and facilitate metal uptake by plants [1–
5,13]. One major drawback to the use of synthetic chelators
such as EDTA is that they are highly recalcitrant to microbial
degradation and may persist in the soil for decades [16,17].
In fact, concerns have been raised regarding the use of syn-
thetic chelators in the field [16–18]. In this study, we compared
the ability of EDTA and a biodegradable chelator, rhamnolipid,
to facilitate plant metal uptake. Rhamnolipid, like EDTA, com-
plexed soil-bound metals. However, rhamnolipid was not ef-
fective at enhancing metal uptake by either the halophyte or
the glycophyte, even though it was found in the shoot material
of both plants. One reason for this may be that, compared to
EDTA, rhamnolipid has a significantly lower binding affinity
for metals. For example, the stability constant for EDTA-Pb
is 17.88 compared to 8.58 for rhamnolipid-Pb, which repre-
sents a nine-order-of-magnitude difference in the relative
strength of the two complexes [19]. A second possibility is
that the metal-bound rhamnolipid complex is excluded from
the root entirely, whereas the free rhamnolipid molecule is not.
Continued research is required to identify environmentally
compatible metal chelators that may be used to aid in phy-
toextraction scenarios.
Both plants accumulated metals in the order Cu
Ͼ Zn Ͼ
Pb, reflecting the metal concentrations found in the contami-
nated soil and/or the bioavailability of the metal. Both Cu and
Zn are essential for maintaining plant metabolic processes, but
in excess concentrations both metals are phytotoxic. Lead, on
the other hand, is not an essential metal. In addition, Cu and
Zn are considerably more bioavailable than Pb in soils. Both
Zn and Cu tend to form ionic instead of covalent chemical
bonds, making them less stable and prone to resolubilization
[
22]. Conversely, Pb forms strong covalent complexes, such
as inorganic oxides, carbonates, or sulfides, that are much more
stable. Even though Pb (2,000 mg/kg dry soil) and Zn (2,500
mg/kg dry) are at similar concentrations in the soil, less Pb
(Ͻ0.01% of the total) was accumulated in the aboveground
plant material than Zn (0.1%). This was especially true for the
halophyte. Williams et al. [12] observed similar metal loading
of essential (Cu, Zn, Mn, and Fe) rather than nonessential
metals (Pb and Cd) for a group of salt marsh plants in the
United Kingdom. In our study, as in theirs, neither the halo-
phyte nor the glycophyte hyperaccumulated any one metal (Cu,
Pb, or Zn) from the contaminated soil:mulch mixture. In fact,
both plants accumulated significantly less than 1% of their
biomass in total (Pb
ϩ
Cu
ϩ
Zn) metal.
To summarize, our results provide further evidence that salt
tolerance may play a role in conferring metal tolerance in
halophytes. The fact that Atriplex spp. and other halophytes
selectively translocate Zn from contaminated soils and that an
increase in stress response factors was observed for M. crys-
tallinum when exposed to increasing Cu concentrations sug-
gests that halophytes may have an advantage over the gly-
Despite the fact that the halophyte did not hyperaccumulate
metals while growing in the highly metalliferrous soil (as it
ϩ
Ϫ
does Na and Cl in salty soils), its metal accumulation pattern
differed significantly from the glycophyte. These differences
became more pronounced when EDTA was applied to the soil.
The halophyte translocated more metal from the roots to the