Neolithic animal management practices and stable isotope studies in the Adriatic
Toxin profile of Alexandrium ostenfeldii (Dinophyceae) from the Northern Adriatic Sea revealed by...
Transcript of Toxin profile of Alexandrium ostenfeldii (Dinophyceae) from the Northern Adriatic Sea revealed by...
Toxin profile of Alexandrium ostenfeldii (Dinophyceae)
from the Northern Adriatic Sea revealed by liquid
chromatography–mass spectrometry
Patrizia Ciminiello a,*, Carmela Dell’Aversano a, Ernesto Fattorusso a,
Silvana Magno a, Luciana Tartaglione a, Monica Cangini b, Marinella Pompei b,
Franca Guerrini c, Laurita Boni c, Rossella Pistocchi c
a Dipartimento di Chimica delle Sostanze Naturali, Universita degli Studi di Napoli ‘Federico II’, via D. Montesano 49, 80131 Napoli, Italyb Centro Ricerche Marine, Viale Vespucci 2, 47042 Cesenatico(FC), Italy
c Scienze Ambientali, Universita di Bologna, Via Tombesi Dall’Ova 55, 48100 Ravenna, Italy
Available online 24 March 2006
Abstract
This paper reports on the first occurrence of fairly high numbers of Alexandrium ostenfeldii along the Emilia Romagna coasts
(Italy). Detailed liquid chromatography–mass spectrometry (LC–MS) analyses of the toxin profile were performed on a strain
of the organism collected in November 2003, isolated during the event and grown in culture. Selected ion monitoring (SIM) and
multiple reaction monitoring (MRM) experiments were carried out for detection of spirolides and paralytic shellfish poisoning
(PSP) toxins. They revealed that the Adriatic A. ostenfeldii produces mainly spirolide 13-desmethyl C at levels of 3.7 pg/cell but
not PSP toxins. Interestingly, low levels of some spirolide isomers that have not been reported so far in other strains of the
dinoflagellate were also detected. This represents the first report of spirolide-type toxins in the Adriatic Sea.
q 2006 Elsevier Ltd. All rights reserved.
Keywords: Alexandrium ostenfeldii; Spirolide 13-desmethyl C; Spirolides; LC–MS; Liquid chromatography–mass spectrometry; Adriatic Sea
1. Introduction
The spirolides are a group of marine toxins detected in
European and North American seas. First episodes of this
kind of toxicity were reported in early 1990s in bivalve
mollusks collected along the eastern shore of Nova Scotia,
Canada (Hu et al., 1995). Intraperitoneal injection (IP) of
lipophilic shellfish extracts in mice caused an unusual toxin
syndrome expressed as piloerection, hyperextension of the
back, arching of the tail, neuro-convulsions and rapid death
(3–20 min). Toxicity studies in mice gave an LD50 of 40 mg/kg and 1 mg/kg for IP and oral dosing, respectively (Richard
0041-0101/$ - see front matter q 2006 Elsevier Ltd. All rights reserved.
doi:10.1016/j.toxicon.2006.02.003
* Corresponding author. Tel.: C39 081 678507; fax: C39 081
678552.
E-mail address: [email protected] (P. Ciminiello).
et al., 2000). Some evidence indicates that spirolides are
muscarinic acetylcholine receptor antagonists and weak
L-type transmembrane calcium channel activators in
mammalian systems (Hu et al., 1995). Human toxicity is
still unknown, even if gastric distress and tachycardia,
following consumption of contaminated shellfish, were
reported in the period when spirolides were detected in
Nova Scotian shellfish.
Structurally, spirolides are characterized by a spiro-
linked tricyclic ether ring system and an unusual seven-
membered spiro-linked cyclic iminium moiety. The number
of toxins belonging to this class has grown significantly over
the years to include several isomers and compounds with
slightly modified structures (Fig. 1) (Hu et al., 1995, 2001).
Six major spirolides are known, namely spirolide A, B,
C, D, E and F, in addition to certain desmethyl derivatives
Toxicon 47 (2006) 597–604
www.elsevier.com/locate/toxicon
Fig. 1. Chemical structures of major spirolides and related protonated ions (m/z) and Q1OQ3 transitions (m/zOm/z) monitored in selected ion
monitoring (SIM) and multiple reaction monitoring (MRM) experiments (positive ions), respectively.
P. Ciminiello et al. / Toxicon 47 (2006) 597–604598
of spirolides C (13-desMeC) and D (13-desMeD). Small
alteration in structure can result in large differences in
toxicity. In fact, the bioactive part structure of these
compounds has been identified as the cyclic imine.
Consequently, hydrolysis to a keto-amine functional
group, such as in spirolides E and F, results in non-toxic
metabolites in shellfish (Hu et al., 1996).
Recently, the causative organism producing spirolide
toxins was identified as the dinoflagellate Alexandrium
ostenfeldii (Paulsen) Balech and Tangen (1985) from Ship
Harbour, Nova Scotia (Cembella et al., 1999, 2000, 2001),
even if no cases of human poisoning have been definitively
linked to blooms of such organism. A. ostenfeldii has been
found widely distributed in north temperate waters, occurring
off the coasts of Denmark (Moestrup and Hansen, 1988),
Norway (Aasen et al., 2005), Scotland (John et al., 2003),
Atlantic Canada (Cembella et al., 2001) and New Zealand
(Mackenzie et al., 1996). Crude extracts from different strains
of A. ostenfeldii collected from different coastal regions have
shown important and in some cases dramatic differences in
toxicity and toxin profile. Particularly, in Nova Scotia,
A. ostenfeldii cells contain a high level of spirolides A, B, C,
D, 13-desMeCand 13-desMeD, but these compoundshavenot
been found in populations from New Zealand, where they
produce, instead, toxins involved in paralytic shellfish
poisoning (PSP) (Mackenzie et al., 1996). Even more
confusing is that certain populations found in Scandinavia
produce both spirolides and PSP toxins, but at very low levels
(Cembella et al., 2000). In Italy, the presence of A. ostenfeldii
has not been reported so far.
This paper reports on the first occurrence of fairly high
numbers of A. ostenfeldii along the Emilia Romagna coasts
(Italy). Detailed analysis of the toxin profile was performed
by liquid chromatography–mass spectrometry (LC–MS) on
a strain of this organism collected in November 2003,
isolated during the event and grown in culture.
2. Materials and methods
2.1. Chemicals
All organic solvents were of distilled-in-glass grade (Carlo
Erba, Milan, Italy). Water was distilled and passed through a
MilliQ water purification system (Millipore Ltd, Bedford,
MA, USA). Formic acid (95–97%, Laboratory grade) and
ammonium formate (AR grade) were purchased from Sigma
Aldrich, Steinheim, Germany. Spirolide 13-desMeC standard
solution and aCanadianA. ostenfeldiiplankton extract, used as
references, were kindly provided by Dr Michael Quilliam
(Institute for Marine Biosciences, National Research Council
of Canada, Halifax, NS, Canada).
P. Ciminiello et al. / Toxicon 47 (2006) 597–604 599
2.2. Sampling and cultures of A. ostenfeldii (Paulsen)
Balech et Tangen
The sampling area is located in the North-Western
Adriatic Sea along Emilia Romagna coasts (Italy) and, since
1978, it is subjected to careful monitoring for toxic
phytoplankton and algal toxins in farmed shellfish.
Qualitative and quantitative analysis of phytoplankton
was performed by the Utermohl method (Utermohl, 1931)
on water samples stored in dark glass bottles. A. ostenfeldii
(Paulsen) Balech and Tangen (1985) was isolated by the
capillary pipette method (Hoshaw and Rosowski, 1973)
from a natural sample of phytoplankton collected in the
coastal waters of Emilia Romagna, in the nearby of
Cesenatico (FC), in November 2003. After an initial growth
in microplates, the unialgal cultures were grown in sterile
Erlenmeyer flasks sealed with cotton plugs at 20 8C under a
16:8 h LD cycle (ca. 166 mmol/m2 per s from cool white
lamp); nutrients were added at the f/2 concentration
(Guillard and Ryther, 1962), and water salinity was adjusted
to 30 psu. For toxicity studies, A. ostenfeldii was cultured in
two Erlenmeyer flasks each containing 1.5 l of medium.
Cells were collected at stationary phase on the 30th day of
growth first by gravity filtration through 0.45 mm Millipore
filters and then by centrifugation at 3000g for 15 min at
10 8C. Both cell pellets and growth mediums were saved for
analyses. Cell counts were made every other day in settling
chambers by the Utermohl method (Utermohl, 1931).
2.3. Sample extraction and clean-up
Cultured cells (49!106 cells in 3 l culture) were
suspended in methanol/water (8:2, v/v) solution (9 ml) and
sonicated for 5 min in pulse mode, while cooling in ice bath.
The mixture was centrifuged at 5000 rpm for 10 min and the
pellet was washed twice each with 9 ml of methanol. The
supernatants were combined and the volume was adjusted to
27 ml with extracting solvent. A 1 ml aliquot of the crude
extract was analyzed directly by LC–MS (5 ml injected).A 6 ml aliquot of the extract was evaporated to dryness. The
residue was dissolved in 1 ml of acetonitrile–water (1:9,
v/v), and the solution was loaded on a Sep-Pak C-18 plus
cartridge (Waters Corporation, Milford, MA, USA) equili-
brated with the same solution. The column was sequentially
eluted with 10 ml of acetonitrile–water (1:9, 3:7, 1:1, v/v)
solutions and acetonitrile 100%. The toxins were eluted with
the acetonitrile–water (1:1, v/v) solution. The residue in the
eluate was evaporated, redissolved in 1 ml of methanol and
directly injected into the LC–MS system.
2.4. Liquid chromatography–mass spectrometry analyses
Mass spectral experiments were performed by using an
API-2000 triple quadrupole mass spectrometer equipped
with a turbo-ionspray source (Applera, Thornhill, ON,
Canada), coupled to an Agilent (Palo Alto, CA, USA) model
1100 LC which included a solvent reservoir, in-line
degasser, binary pump and refrigerated autosampler. LC–
MS analyses for spirolides (Quilliam et al., 2001) were
performed using a 3 mm Hypersil C8 BDS, 50!2.00 mm
column (Phenomenex, Torrance, CA, USA) at room
temperature. Eluent A was water and B was 95%
acetonitrile–water solution, both eluents containing 2 mM
ammonium formate and 50 mM formic acid. The flow rate
was 200 ml/min. Either a gradient elution, 10–100% B in
10 min followed by 100% B for 15 min, or an isocratic
elution with 35% B were used. Selected ion monitoring
(SIM) experiments were carried out in positive ion mode by
selecting the ions reported in Fig. 1 for known spirolides.
Dwell time was generally set at 100 ms and a maximum
number of 10 ions per experiment were monitored. Four
MRM experiments were carried out by selecting the
following groups of transitions (692O150, 692O164,
692O444, 692O458), (694O150, 694O164, 694O444,
694O458), (706O150, 706O164, 706O444, 706O458)
and (708O150, 708O164, 708O444, 708O458), respect-
ively. Dwell time of 250 ms for each transition was used.
In these studies, a temperature of 100 8C, an ionspray
voltage of 5400 V, a declustering potential of 90 V, a
focusing potential of 230 V, and an entrance potential of
12 V were used. A collision energy of 53 eV and a cell exit
potential of 13 V were used in MRM experiments. Spirolide
13-desMeC was quantitatively determined in the crude
extract by direct comparison to individual standard solutions
of spirolide 13-desMeC at similar concentrations injected in
the same experimental conditions.
HILIC–MS analyses for PSP toxins (Dell’Aversano
et al., 2005) were performed using a 250!2.00 mm column
packed with 5 mm Tosohaas TSK-GEL Amide-80 material
at room temperature. Eluent A was water and B was 95%
acetonitrile–water solution, both eluents containing 2 mM
ammonium formate and 3.6 mM formic acid (pH 3.5).
Isocratic elution with 65% B at a flow rate of 200 ml/min
was used. A sample injection volume of 5 ml was used.
Selected ion monitoring (SIM) and multiple reaction
monitoring (MRM) experiments were carried out in positive
ion mode. The following ions were monitored in SIM mode:
m/z 300 for saxitoxin (STX) and gonyautoxin 5 (GTX5),m/z
316 for neosaxitoxin (NEO), gonyautoxins 2/3 (GTX2/3)
and N-sulfogonyautoxins 1/2 (C1/2), m/z 380 for GTX5, m/z
396 for GTX2/3 and C1/2, m/z 412 and 332 for both
gonyautoxins 1/4 (GTX1/4) and N-sulfogonyautoxins 3/4
(C3/4). The following transitions (precursor ion)O(frag-
ment ion) were monitored in MRMmode: m/z 300O282 for
STX, m/z 316O298 for NEO, m/z 380O300 for GTX5, m/z
396O316 and 396O298 for both GTX2/3 and C1/2, m/z
412O332 and 412O314 for both GTX1/4 and C3/4. Dwell
time of 150 ms for each ion or transition was used. For these
studies, a temperature of 50 8C, an ionspray voltage of
4500 V, a declustering potential of 55 V, a focusing
potential of 270 V, an entrance potential of 5 V, a collision
energy of 25 eV and a cell exit potential of 7 V were used.
P. Ciminiello et al. / Toxicon 47 (2006) 597–604600
3. Results and discussion
In the period November 2003–February 2004, increasing
concentrations of A. ostenfeldii cells were detected along
Emilia Romagna coasts, in the Cesenatico area, where
previously we had sporadically observed only a few A.
ostenfeldii cells. The highest concentration was recorded at
the end of November 2003 (15,612 cells/l) and then
decreased.
The cells presented the following morphological features
(Fig. 2), fully consistent with the morphology reported for
the dinoflagellate A. ostenfeldii (Balech and Tangen, 1985):
the cell was large and nearly spherical, with thin thecal
plates and a characteristic large ventral pore on the first
apical plate (1 0); the cingulum and the sulcus were shallow.
Unialgal cultures of A. ostenfeldii, after an initial lag
phase of about a week, reached a maximum density of about
18,500 cells/ml in 25–30 days. A sample containing
49,000,000 cells was provided for evaluation of toxin
profile by LC–MS analyses, which were directed to
detection of toxins so far identified in A. ostenfeldii cultures,
namely PSP toxins and spirolides (Mackenzie et al., 1996;
Cembella et al., 1999).
Cultured cells were extracted by sonicating with
methanol/water (8:2, v/v) and the crude extract was directly
analyzed by hydrophilic interaction liquid chromatography–
mass spectrometry (HILIC–MS). The chromatographic
separation was carried out by using a TSK gel Amide 80
column and a mobile phase containing ammonium formate
and formic acid, as recently reported for rapid, sensitive and
selective determination of PSP toxins (Dell’Aversano et al.,
2005). The MS was equipped with a turboionspray interface
and operated in positive ion mode. Selected ion monitoring
(SIM) experiments were carried out in positive ion mode for
major PSP toxins (saxitoxin, neosaxitoxin, gonyautoxins 1–
5 and N-sulfogonyautoxins 1–4). No peak corresponding to
PSP toxins was detected in the chromatogram. In order to
definitively exclude the presence of saxitoxin and its
Fig. 2. Vegetative cells of A. ostenfeldii (400!) at the optical microscope:
ventral pore on the first apical plate. Scale barZ10 mm.
derivatives, an aliquot of cultured cells was extracted with
0.1 M acetic acid, as recommended for exhaustive extrac-
tion of PSP toxins from phytoplankton (Ravn et al., 1995).
The crude extract was analyzed by HILIC–MS in multiple
reaction monitoring (MRM) mode and showed again not to
contain any of the most common PSP toxins.
The methanol/water (8:2, v/v) crude extract of the
Adriatic A. ostenfeldii was analyzed by LC–MS for most of
the known spirolides. LC–MS is the most common
analytical technique used for detection of spirolides, by
allowing the monitoring of known spirolides as well as the
identification of some unknown derivatives through
interpretation of the fragmentation pattern shown in
MS/MS product ion spectra (Sleno et al., 2004a,b).
The chromatographic separation was carried out by
using a reversed phase Hypersil C8 BDS column and a
mobile phase containing ammonium formate and formic
acid, as suggested by Quilliam et al. (2001) for the analyses
of spirolides and various lipophilic toxins. SIM experiments
were carried out by selecting [MCH]C ions for the
spirolides contained in Fig. 1. In fact, preliminary full
scan MS1 experiments on a standard solution of spirolide
13-desmethyl C, the only spirolide solution commercially
available, had shown that formation of the only pseudo-
molecular ion [MCH]C at m/z 692.5 was favored (Fig. 3a)
under the used ionization process parameters.
SIM traces of the A. ostenfeldii crude extract showed the
presence of a dominant chromatographic peak eluting at
7.48 min for m/z 692.5. This peak could be assigned to
spirolide 13-desMeC, based on the comparison of its
retention time and MW with those of an authentic sample
of 13-desMeC. In order to gain further evidence for the
obtained result we also used, as reference sample,
A. ostenfeldii extract provided by the Institute for Marine
Biosciences (IMB), Canada, which contained spirolide 13-
desMeC in addition to spirolide C, C3, D, and 13-desMeD
(Maclean et al., 2003). Comparison between SIM results for
the two plankton samples provided further support for the
A, not stained cell; B, cell stained with Calcofluor white showing the
OO
N
O
OO
HOOH
m/z
408
Inte
nsity
, cps - H2O
- H2O
- H2O
- H2O- H2O
- H2O
(b)
692
100 200 300 400 500 600 7000
1e+5
2e+5
3e+5
4e+5
674
656
638
462
444
426
164
(a)
500 600 700 800 9000
2e+5
4e+5
6e+5
8e+5 [M+H]+
692.5
m/z
Inte
nsity
, cps
NH+
O
OO OH
fragment aO
O
O
OO OH
fragment b
NH+
Fig. 3. Full scan MS1 (a) and MS2 product ion (b) spectra of a standard solution of spirolide 13-desMeC. MS2 product ion spectrum of the [MCH]C ion atm/z 692 was obtained using a collision
energy of 53 eV.
P.Ciminiello
etal./Toxico
n47(2006)597–604
601
P. Ciminiello et al. / Toxicon 47 (2006) 597–604602
presence of spirolide 13-desMeC in the Adriatic strain and
allowed to rule out the presence of other spirolides produced
by the Canadian strain.
Final confirmation for the identity of spirolide 13-
desMeC in the Adriatic A. ostenfeldii sample was obtained
by multiple reaction monitoring. Such experiment was set
up based on the results of the full scan MS2 product ion
spectrum of a standard solution of spirolide 13-desMeC
that was obtained using the [MCH]C ion at m/z 692.5 as
precursor ion and a collision energy of 53 eV (Fig. 3b). It
contained three characteristic fragment ion clusters: (i)
ions at m/z 674, 656, and 638 due to loss of water
molecules from the pseudo-molecular ion; (ii) ions at m/z
462, 444, 426, 408 due to loss of the structural ‘fragment
a’ and associated water loss from the pseudo-molecular
ion; (iii) an abundant ion at m/z 164 which derives from
the ion at m/z 444 by loss of the structural ‘fragment b’
(Sleno et al., 2004a). The most abundant ions (m/z 674,
444 and 164) were selected as product ions of the ion at
m/z 692 in MRM transitions. MRM traces of the
A. ostenfeldii crude extract (Fig. 4) showed the presence
of peaks eluting at 7.48 min for all three diagnostic
transitions (m/z 692O674, 692O444, and 692O164); the
observed ion ratios were identical to those obtained by
MRM analysis of the spirolide 13-desMeC standard
solution.
The whole of the above experiments were fully
consistent with the presence of spirolide 13-desMeC in the
analyzed sample. Quantitation was carried out by compari-
son of the peak area for the most abundant transition at m/z
692O164 with that obtained by injecting a standard solution
of spirolide 13-desMeC at similar concentration. This
revealed a concentration value for spirolide 13-desMeC of
3.7 pg/cell.
0 2 4 6 8Time, mi
7,
Fig. 4. MRM analysis in positive ion mode of the Adriatic A. ostenfeldii sa
fragmentation pattern of spirolide 13-desMeC (see Fig. 3b). *Chromatogr
Under the same ionization and fragmentation process
parameters optimized for spirolide 13-desMeC, a number of
MRM experiments were carried out by selecting transitions
characteristic for the known spirolides A, B, C, 13-desMeC,
D and 13-desMeD. As a result, the presence of such
spirolides could be definitively excluded in the crude
extract.
It has to be noted that in most of the analyzed strains
of A. ostenfeldii, the 13-desMeC derivative represents
by far the major spirolide component, usually constituting
O90% of the total spirolide content (Sleno et al.,
2004a,b). Since such toxin appeared to be present in
our crude extract at a relatively low level, a doubt
aroused about the possibility that matrix suppression
effect could have hampered detection of minor spirolides.
Thus, a clean-up step by solid phase extraction (SPE)
was carried out.
SPE was accomplished by using a C18 stationary
phase eluted with water–acetonitrile solutions of decreas-
ing polarity. All SPE eluates were analyzed by LC–MS
in MRM mode according to the following procedure: the
protonated ions for spirolides A and 13-desMeC (m/z
692), B and 13-desMeD (m/z 694), C (m/z 706), and D
(m/z 708) were selected as precursor ions and combined
with the four possible fragment ions at m/z 150, 164,
444, and 458. Such transitions were monitored in four
MRM experiments using 250 ms as dwell time in order
to gain highest sensitivity. Such a kind of experiment
gave the opportunity to check for the presence of the
above known derivatives as well as to individuate some
unknown spirolide analogues which differ in substitution
at part structures giving rise to ‘fragment a’ and
‘fragment b’ (Fig. 3b).
10 12 14
m/z 692 > 674
m/z 692 > 444
m/z 692 > 164
n
48
mple was performed on a series of ion transitions consistent with the
aphic conditions were as in Section 2.
692 > 164
692 > 444
Time, min6 10 12
desMeC
692 > 150692 > 458
X1
694 >164 694 >444
desMeC
X2
X3
708 > 458
708 > 164
x 600
x 20
x 300
8
Fig. 5. MRM analyses in positive ion mode of the acetonitrile–water (1:1) SPE eluate of A. ostenfeldii. For the m/z 694O444 and 694O164
transitions, a peak due to 13C isotope of spirolide desMeC is present. Chromatographic conditions were as in Section 2.
P. Ciminiello et al. / Toxicon 47 (2006) 597–604 603
The results of MRM analyses of the acetonitrile–water
(1:1) SPE eluate are shown in Fig. 5. They suggested
the presence of three novel spirolide analogues (X1, X2
and X3) in theA. ostenfeldii extract. Particularly, two of them
(X2 and X3) had the same fragmentation pattern as spirolide
13-desMeD (m/z 694O164 and 694O444) and D (m/z 708O164 and 708O458), respectively, but remarkably
different retention times, namely Rt(X2)Z6.77 min versus
Rt(13-desMeD)Z8.84 min and Rt(X3)Z7.36 min versus
Rt(D)Z7.79 min. On the contrary, X1 had the same retention
time as spirolide 13-desMeC (7.50 min) but different
fragmentation (m/z 692O150 and 692O458), suggesting
that it was a new derivative possibly with R1ZH, R2ZCH3,
and an additional methyl in the ‘fragment b’ moiety of the
molecule.
Mass spectral behavior of X1, X2 and X3 was
clearly indicative of spirolide structures. Unfortunately,
the small amount of available material prevented us to
fully assign their structures by extensive spectral
analyses.
4. Conclusions
This report highlights, for the first time, the presence of
toxic dinoflagellate A. ostenfeldii in the Adriatic Sea. The
careful LC–MS analysis of a culture of this organism
revealed that the Adriatic strain of A. ostenfeldii produces
spirolides but not PSP toxins, which were instead produced
by strains from New Zealand and Scandinavia (Mackenzie
et al., 1996; Cembella et al., 2000). Interestingly, the
Adriatic A. ostenfeldii in addition to spirolide 13-desMeC
also produces some unknown spirolide isomers. This
represents the first report of spirolide-type toxins in the
Adriatic Sea. The variety of spirolide isomers detected can
be explained in light of a classical poliketide synthesis
through joint participation of acetate and propionate units
which could occur by different coupling sequences acetate/
propionate. The aims of our future research are (i) verifying
whether spirolides were retained and accumulated in
mussels cultivated in Adriatic Sea; (ii) large-scale culturing
of A. ostenfeldii in order to isolate sufficient amount of the
P. Ciminiello et al. / Toxicon 47 (2006) 597–604604
new derivatives for structure elucidation both by MS/MS
and NMR means.
Acknowledgements
The authors wish to thank Dr Michael Quilliam and
William Hardstaff (NRC/IMB, Halifax, NS, Canada) for
providing the standard of 13-desMeC and the plankton
extract containing spirolides. This work is a result of a
research supported by MURST PRIN, Rome, Italy. LC–MS
experiments were performed at ‘Centro di Servizi Inter-
dipartimentale di Analisi Strumentale’, Universita degli
Studi di Napoli ‘Federico II’. The assistance of the staff is
gratefully appreciated.
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