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www.elsevier.com/locate/hal
Harmful Algae 6 (2007) 93–103
The genus Pseudo-nitzschia (Bacillariophyceae) in continental
shelf waters of Argentina (Southwestern Atlantic Ocean, 38–558S)
Gaston O. Almandoz a,b,*, Martha E. Ferrario a,b, Gustavo A. Ferreyra c,Irene R. Schloss c,b, Jose L. Esteves d, Flavio E. Paparazzo d
a Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata, Paseo del Bosque s/n, 1900 La Plata, Argentinab CONICET, Argentina
c Instituto Antartico Argentino, Cerrito 1248, 1010 Ciudad de Buenos Aires, Argentinad CENPAT-CONICET, Bv. Brown 3000, 9120 Puerto Madryn, Argentina
Received 13 March 2006; received in revised form 4 July 2006; accepted 17 July 2006
Abstract
The distribution pattern of Pseudo-nitzschia species, associated phytoplankton flora and its relationships with main environ-
mental factors were studied for the first time in continental shelf surface waters of the Argentine Sea (Southwestern Atlantic Ocean,
38–558S). Both qualitative and quantitative samples, collected during summer and fall 2003, were examined using light and
scanning electron microscopy. Results indicated that the genus Pseudo-nitzschia has a wide distribution along the studied area. It
was present at low densities, with infrequent peak abundances and appeared most frequently as a minor component of the diatom
populations that typically develop on the continental shelf of the Argentine Sea. Moreover, phytoplankton communities were
numerically dominated by unidentified phytoflagellates (�5 mm) throughout almost all samples analyzed. Eight Pseudo-nitzschia
species were identified in our study: P. australis, P. fraudulenta, P. heimii, P. lineola, P. pungens, P. cf. subcurvata, P. turgidula and
P. turgiduloides. Of these, P. heimii, P. lineola and P. turgiduloides are new records for the Argentine Sea. Their presence in the area
is attributable to the influence of southerly cold water masses. Spatial and temporal variations of the environmental parameters
recorded in the study area generally determined the distribution of Pseudo-nitzschia species. P. pungens and P. australis were widely
distributed and reached high densities, especially in waters with elevated temperatures and salinities (around 15 8C, 33.8 psu) and
low nutrients concentrations. On the other hand, P. heimii, P. lineola, P. turgidula and P. turgiduloides showed a more restricted
distribution, with lower densities in relatively cold, less saline (8 8C, 32.45 psu) and nutrient-rich waters. From the Pseudo-nitzschia
species found throughout this survey, P. australis, P. fraudulenta, P. pungens and P. turgidula are known as domoic acid (DA)
producers around the world, but there is little information on the potential toxicity of these species in Argentina.
# 2006 Elsevier B.V. All rights reserved.
Keywords: Argentine sea; Diatoms; Distribution; Phytoplankton; Pseudo-nitzschia
* Corresponding autor at: Facultad de Ciencias Naturales y Museo,
Universidad Nacional de La Plata, Paseo del Bosque s/n, 1900 La
Plata, Argentina. Tel.: +54 221 4257744; fax: +54 221 4257527.
E-mail address: [email protected]
(G.O. Almandoz).
1568-9883/$ – see front matter # 2006 Elsevier B.V. All rights reserved.
doi:10.1016/j.hal.2006.07.003
1. Introduction
The diatom genus Pseudo-nitzschia was originally
proposed by Peragallo (Peragallo and Peragallo, 1897–
1908). Later, it was reduced to a section of the genus
Nitzschia (Hustedt, 1958) and again has been recently
recognized as a distinct genus by Hasle (1994).
Compared to Nitzschia, one of the closely related
G.O. Almandoz et al. / Harmful Algae 6 (2007) 93–10394
Fig. 1. Map of the study area showing the location of sampling
transects and stations. Transect 1 was tracked from 7 to 10 February
2003 and transect 2 from 15 to 19 May 2003.
genus with several hundred species (Mann, 1986),
Pseudo-nitzschia is a relatively small genus containing
about 30 species, some of them recently described
(Lundholm and Moestrup, 2002; Priisholm et al., 2002;
Lundholm et al., 2002, 2003). This genus occurs in
marine planktonic habitats and has a worldwide
distribution, including polar waters (Hasle and Medlin,
1990; Hasle and Syvertsen, 1997; Hasle, 2002).
From the discovery that several Pseudo-nitzschia
species are implicated in domoic acid (DA) outbreaks
(Bates et al., 1989), the genus has received more attention
and several studies on its taxonomy and eco-toxicology
have been conducted around the world (e.g. Orsini et al.,
2002; Lundholm et al., 2003, 2004; Cerino et al., 2005;
Fehling et al., 2005). DA is a neurotoxin that can be
transferred along the marine food web via feeding mainly
by shellfish. This can provoke amnesic shellfish
poisoning, which can have lethal effects in sea birds,
marine mammals and humans (Bates, 2000; Fehling
et al., 2004).
Harmful dinoflagellate events with significant eco-
nomical impacts and human casualties have been
observed along the Argentine Sea since the 1980s
(Carreto et al., 1981, 1985; Vecchio et al., 1986). The first
DA record for the Argentine Sea, although without
negative health consequences, was registered in July
2000 in Mar del Plata. The toxin was detected in
plankton, mussels and anchovy stomachs, during a bloom
of Pseudo-nitzschia australis (Negri et al., 2004).
Most of the early records of Pseudo-nitzschia species
in Argentinean waters correspond to works dealing with
general phytoplankton composition (Balech, 1971;
Carreto et al., 1974; Verona et al., 1974; Lange, 1985).
Nevertheless, P. australis was described as a new species
by Frenguelli (1939) based on material from San Matıas
Gulf, Argentina. More recent studies focused on Pseudo-
nitzschia species were conducted using both light and
electron microscopy (Negri and Inza, 1998; Ferrario
et al., 1999, 2002; Sastre et al., 2001). The latter
nowadays considered essential for a reliable identifica-
tion at the specific level (Fryxell and Hasle, 2003).
However, most of these studies were restricted to coastal
and space-limited areas, thus limiting the available
information on the occurrence of Pseudo-nitzschia
species in Argentinean shelf waters.
The continental shelf of Argentina has an extension
of about 106 km2, where the main source of the water
masses is the subantarctic water flowing from the
northern Drake Passage (Acha et al., 2004; Bianchi
et al., 2005). Access to an extensive and complete
sampling gave us the opportunity to obtain original
field information on the presence of Pseudo-nitzschia
spp. in a region with an extensive shoreline and a
considerable shellfish fishing industry. The main goal of
this research was to study the distribution pattern of
Pseudo-nitzschia species, associated phytoplankton
flora and its relationships with main environmental
factors in continental shelf surface waters of the
Argentine Sea.
2. Materials and methods
The continental shelf waters of the Argentine Sea
were sampled during summer and autumn 2003,
onboard the icebreaker A.R.A ‘‘Almirante Irizar’’ in
the frame of an Argentinean–French cooperative
research (‘‘ARGAU’’; Balestrini et al., 2000).
Samples were taken at 49 stations along 2 north–south
transects located approximately between 38–558S and
57–688W (Fig. 1). Transect 1 was tracked from 7 to 10
February 2003 and transect 2 from 15 to 19 May 2003.
Samples were collected at 9 m depth using a
continuous seawater pumping system (Balestrini
G.O. Almandoz et al. / Harmful Algae 6 (2007) 93–103 95
et al., 2000). Water temperature and salinity were
measured continuously with Sea-Bird SB 38 and 37
sensors, respectively. For chlorophyll a determination,
2–4 l of seawater were filtered onto GF/F filters and
frozen at �20 8C until analysis. Ninety percentage of
acetone pigment extracts were read in a Beckman DU
650 spectrophotometer, and corrected for phaeopig-
ments. Concentrations were calculated following
Strickland and Parsons (1972). Duplicate samples for
nitrate, nitrite, phosphate and silicate were taken from
the continuous seawater pumping system, kept frozen
(�20 8C) until analysis. Nitrate, nitrite and silicate were
measured with an automatic analyzer (Autonalyzer
Technicon II1), while phosphate was determined
manually, following methods proposed by Strickland
and Parsons (1972).
At each station, both qualitative and quantitative
samples were taken for phytoplankton analyses.
Qualitative samples were collected by filtering seawater
from the continuous system through a 20 mm mesh net,
whereas quantitative samples were collected in 250 ml
bottles. All samples were fixed with Lugol’s iodine
solution and kept in dark conditions at room tempera-
ture until analysis.
For species identification, net samples were cleaned
(Hasle and Fryxell, 1970) and dried onto cover glasses
for mounting in Naphrax for light microscopy (LM) and
onto stubs shadowed with gold-palladium for scanning
electron microscopy (SEM), according to Ferrario et al.
(1995). Observations were made with a phase contrast
Wild M20 microscope (equipped with an attached
camera) and a Jeol JSM-6360 LV (SEM). Species
identifications were confirmed by SEM studies, except
for P. subcurvata, which is called P. cf. subcurvata. In
order to avoid species misinterpretation during quanti-
fication, cell counts were always done after qualitative
analyses.
For quantitative estimations, cells were enumerated
with an Iroscope SI-PH inverted microscope according
Table 1
Minimum (min), mean and maximum (max) values of temperature, salinity, n
chlorophyll a (chl a) recorded during the sampling period in the Argentine
Date Temperature (8C) Salinity (psu) NO3� (mM) N
Summer 2003
Min 9.7 32.64 0.00 0
Mean 14.1 33.27 1.16 0
Max 22.5 33.92 6.06 0
Autumn 2003
Min 8.0 32.45 0.00 0
Mean 12.4 33.40 4.16 0
Max 15.9 34.05 13.48 0
to the procedures described by Utermohl (1958). During
cell counting, since flagellates generally loose their
flagella by the addition of fixatives, unidentified
phytoflagellates and round-shaped organisms with or
without flagella, were included in a single group as
‘‘phytoflagellates’’ and classified according to their
size.
3. Results
3.1. Environmental conditions
Temperature shows a marked latitudinal gradient
along the Patagonian coast (see Acha et al., 2004),
sharply decreasing southwards. Salinity in the coastal
most areas is heavily influenced by freshwater runoff
from various rivers, and increases offshore. Moreover,
in the southernmost stations, the influence of the cold
and saline subantarctic waters can be seen on the
Patagonian Shelf (Acha et al., 2004). On average, higher
temperatures and lower salinities were detected in
summer (Table 1). Nutrient distribution did not show
such a clear latitudinal pattern, although higher
concentrations were typically found in relation with
oceanographic fronts (data not shown). Average
nutrient concentrations were higher during autumn
transect (Table 1).
Highest chl a concentrations measured during
summer and autumn were 19 and 4.8 mg m�3
respectively (Table 1). They were found near 528Sand 418S, respectively, and associated with diatom
blooms. As described by Schloss et al. (in press), sectors
of maximum concentration of chl a were generally
located in the stratified side of the tidal fronts of Valdes
peninsula (428S), San Jorge Gulf (close to 468S), its
southern tip (Blanco Cape) and Grande Bay (close to
528S). Other high values were observed near De los
Estados Island (�558S) and south of Mar del Plata
(�398S).
itrate (NO3�), nitrite (NO2
�), phosphate (PO4BB), silicate (SiO3 ) and
Sea
O2� (mM) PO4
BB (mM) SiO3 (mM) chl a (mg m�3)
.00 0.33 0.00 0.32
.07 0.63 1.36 3.51
.28 0.90 3.38 19.22
.00 0.43 0.00 0.11
.18 0.78 2.03 1.59
.71 1.24 4.85 4.81
G.O. Almandoz et al. / Harmful Algae 6 (2007) 93–10396
Fig. 2. Light (LM) and scanning electron (SEM) micrographs of Pseudo-nitzschia species first reported in Argentinean waters. (1–4) P. heimii: (1–3)
SEM, internal valve views showing the cell shape, apical and central part details; (4) LM, colony in girdle view. (5–8) P. lineola: (5–7) SEM, internal
valve views showing the cell shape, apical and central part details; (8) LM, colony in girdle view. (9–12) P. turgiduloides: (9–11) SEM, internal valve
views showing the cell shape, apical and central part details; (12) LM, colony in girdle view.
3.2. Phytoplankton composition, abundance and
distribution
Unidentified tiny phytoflagellates (�5 mm) numeri-
cally dominated phytoplankton assemblages throughout
both transects and usually exceeded 70% of total cells.
During summer, its densities ranged between 0.18 � 106
and 5 � 106 cells l�1, with an average of 1.15 � 106
cells l�1 and the highest abundance recorded at 508400S.
During autumn, densities varied from 0.15 � 106 to
2.9 � 106 cells l�1, with an average of 0.55 � 106
cells l�1and the maximum located close to 488S.
Table 2
Number of stations where Pseudo-nitzschia species were recorded during
Date P. australis P. fraudulenta P. heimii P. line
Summer 2003 (N = 26) 6 0 0 0
Autumn 2003 (N = 23) 10 2 2 7
Total (N = 49) 16 2 2 7
Cryptophytes (8.5%), unidentified phytoflagellates
of 6–15 mm (6.4%), diatoms (6.3%), dinoflagellates
(2.1%), prasinophytes (1.4%) and silicoflagellates
(<0.1%) followed the small phytoflagellates in order
of decreasing mean relative abundance for both transects.
Diatom densities showed great variability among
summer samples. Total diatom abundances ranged from
80 (�448S) to 3 � 106 cells l�1 (�528S) where an
exceptional bloom of Chaetoceros debilis was observed.
The net summer diatom assemblage was dominated
(present in more than 80% of total samples) by Ditylum
brightwellii, Paralia sulcata, Chaetoceros decipiens,
the sampling period in the Argentine Sea
ola P. pungens P. cf. subcurvata P. turgidula P. turgiduloides
21 7 0 7
11 2 4 17
32 9 4 24
G.O. Almandoz et al. / Harmful Algae 6 (2007) 93–103 97
Pleurosigma sp., Thalassionema nitzschioides, Bacter-
iastrum delicatulum, Coscinodiscus jonesianus, Psam-
modictyon panduriforme and Raphoneis amphiceros.
Throughout the autumn, diatom densities varied from
9.5 � 102 to 1.45 � 105 cells l�1. Autumn maximum
was recorded close to 388S and was mainly composed of
C. debilis, Thalassiosira mala, Rhizosolenia pungens,
Fig. 3. Distribution patterns of Pseudo-nitzschia speci
Leptocylindrus minimus, Meuniera membranacea,
Chaetoceros decipiens and Guinardia delicatula. The
most frequent diatom species in net autumn samples were
Actinoptychus senarius, P. sulcata, Pleurosigma sp., P.
panduriforme, Thalassionema nitzschioides, R. amphi-
ceros, Asterionellopsis glacialis, Hyalodiscus radiatus
and Delphineis minutissima. Typical cold water species
es in surface shelf waters of the Argentine Sea.
G.O. Almandoz et al. / Harmful Algae 6 (2007) 93–10398
such as Chaetoceros dichaeta, Dactyliosolen antarcticus,
Thalassiosira gracilis and Corethron pennatum mainly
collected south of 498S, were particularly common along
this transect.
3.3. Occurrence of Pseudo-nitzschia spp.
The genus Pseudo-nitzschia showed a wide dis-
tribution along the studied area, being present in 90% of
the examined stations. However, Pseudo-nitzschia spp.
Table 3
Minimum (min), mean and maximum (max) values of temperature, salinity,
in which Pseudo-nitzschia species were recorded in the Argentine Sea
Temperature (8C) Salinity (psu) NO3� (m
P. australis
N 16 16 15
Min 9.7 32.6 0.000
Mean 12.7 33.4 2.398
Max 15.9 34.1 7.049
P. fraudulenta
N 2 2 2
Min 12.8 33.4 1.040
Mean 13.1 33.4 1.217
Max 13.4 33.4 1.395
P. heimii
N 2 2 2
Min 8.0 32.5 8.255
Mean 8.5 32.6 10.649
Max 9.0 32.8 13.044
P. lineola
N 7 7 7
Min 8.0 32.5 1.040
Mean 10.3 33.1 7.566
Max 13.4 33.4 13.476
P. pungens
N 32 32 31
Min 9.7 32.6 0.000
Mean 14.4 33.4 1.296
Max 22.5 34.1 7.049
P. cf. subcurvata
N 9 9 9
Min 8.0 32.5 0.022
Mean 13.7 33.2 1.639
Max 20.9 33.7 8.255
P. turgidula
N 5 5 5
Min 8.0 32.5 7.829
Mean 9.1 33.0 9.877
Max 9.6 33.3 13.476
P. turgiduloides
N 24 24 24
Min 8.0 32.5 0.000
Mean 12.3 33.3 3.943
Max 18.3 34.1 13.476
were usually present at low densities, ranging from 10
to 6.1 � 104 cells l�1 (average 3.3 � 103 cells l�1) and
accounting from 0.1 to 50% of total diatom densities,
with an average contribution of 4.3% (N: 27). In many
cases the genus was just recorded in concentrated
qualitative samples (N: 17).
Eight Pseudo-nitzschia species were identified in our
study: P. australis, P. fraudulenta, P. heimii, P. lineola,
P. pungens, P. cf. subcurvata, P. turgidula and P.
turgiduloides, of which P. heimii, P. lineola and P.
nitrate (NO3�), nitrite (NO2
�), phosphate (PO4BB) and silicate (SiO3 )
M) NO2� (mM) PO4
BB (mM) SiO3 (mM)
15 16 16
0.000 0.438 0.000
0.089 0.687 1.171
0.186 1.134 4.850
2 2 2
0.472 0.689 1.582
0.589 0.719 1.902
0.706 0.749 2.222
2 2 2
0.052 1.029 2.817
0.294 1.134 3.218
0.536 1.240 3.620
7 7 7
0.052 0.679 1.010
0.296 0.923 2.300
0.706 1.240 3.620
31 32 32
0.000 0.425 0.000
0.112 0.679 1.449
0.706 1.134 4.850
9 9 9
0.000 0.476 0.000
0.183 0.683 1.653
0.706 1.029 3.620
5 5 5
0.026 0.840 1.811
0.151 0.992 2.621
0.536 1.235 3.620
24 24 24
0.000 0.332 0.000
0.123 0.706 1.831
0.706 1.240 4.444
G.O. Almandoz et al. / Harmful Algae 6 (2007) 93–103 99
turgiduloides are new records for the Argentine Sea
(Fig. 2). Most of the morphological characters of the
Pseudo-nitzschia species observed fitted their descrip-
tions provided by Hasle (1964, 1965) and Ferrario et al.
(2002). Small and delicate specimens, either solitary
cells or grouped in stepped curved colonies resembling
P. subcurvata, were tentatively called P. cf. subcurvata.
The most commonly occurring species recorded were
P. pungens, P. turgiduloides and P. australis, present
respectively in 65, 49 and 33% of all samples examined.
An overview of each species presence is shown in
Table 2. The spatial and temporal distribution and
abundance of the Pseudo-nitzschia species is presented in
Fig. 3. Table 3 shows a summary of temperature, salinity
and nutrient values at which Pseudo-nitzschia species
were recorded during our study.
P. australis was discontinuously distributed from
388290S to 548260S (Fig. 3). Throughout summer, its
presence was restricted southward 518S where a
maximum of 6.1 � 104 cells l�1 was recorded close
to 528S (Table 4) during the mentioned C. debilis
bloom. During autumn, P. australis was recorded north-
ward 488180S. Relative high densities (up to 2–
3 � 103 cells l�1) were registered approximately
between 38 and 418S, at temperatures between 15.0
and 15.9 8C, salinities from 33.64 to 34.05 psu, nitrates
(0.00–0.11 mM), nitrites (0.04–0.18 mM), phosphates
(0.46–0.63 mM) and silicates (0.00–3.22 mM).
P. fraudulenta was just recorded in autumn between
438S and 458S (Fig. 3), but was present only in
Table 4
Environmental conditions recorded during peak abundances of Pseudo-nit
Argentine Sea
Date P. australis P. fraudulenta P. heimii P. line
Summer 2003
Abundance (cells l�1) 61111 n/d n/d n/d
Latitude (8S) 51842 – – –
Temperature (8C) 10.7 n/d n/d n/d
–Salinity (psu) 33.08 n/d n/d n/d
–NO3� (mM) 0.55 n/d n/d n/d
NO2� (mM) 0.00 n/d n/d n/d
PO4BB (mM) 0.44 n/d n/d n/d
SiO3 (mM) 0.00 n/d n/d n/d
Autumn 2003
Abundance (cells l�1) 2778 n/d 10 110
Latitude (8S) 38829 – 52819 52819
Temperature (8C) 15.2 n/d 8.0 8.0
Salinity (psu) 33.74 n/d 32.45 32.45
NO3� (mM) 0.11 n/d 8.26 8.26
NO2� (mM) 0.08 n/d 0.54 0.54
PO4BB (mM) 0.63 n/d 1.03 1.03
SiO3 (mM) 0.81 n/d 3.62 3.62
concentrated qualitative samples, never in the quanti-
tative ones.
P. heimii was recorded in autumn from 518350S to
528190S (Fig. 3). Its highest density (10 cells l�1) was
registered at 528190S (Table 4).
P. lineola was recorded in autumn between 438S and
538S (Fig. 3). Its highest density (110 cells l�1) was
reached at 528190S (Table 4).
P. pungens was recorded from 388290S to 548260S(Fig. 3). Throughout summer, it was widely distributed,
being present in 81% of total samples, but usually in
concentrations lower than 100 cells l�1. During autumn
its presence was restricted northward 488S, reaching the
highest abundances between approximately 38–418Swith a maximum of 4.2 � 103 cells l�1 (Table 4).
P. cf. subcurvata was recorded between 408200S and
548260S (Fig. 3). During summer reached high densities
(up to 6.6 � 103 cells l�1) especially between 458S and
548S whereas in autumn was poorly registered from
about 438S to 528S. Its highest density was reached in
summer, near 548S (Table 4).
P. turgidula was recorded in autumn between
approximately 498S and 528S (Fig. 3). The highest
density (20 cells l�1) was registered at 528190S (Table 4).
P. turgiduloides was recorded from 388470S to
528190S (Fig. 3). During summer, it was rarely detected
just in net samples from 438210S to 518420S. Through-
out autumn, it was the most common species recorded,
being present in 79% of all samples analyzed but
usually at concentrations lower than 100 cells l�1. It
zschia spp. reached throughout summer and autumn transects in the
ola P. pungens P. cf. subcurvata P. turgidula P. turgiduloides
926 6667 n/d n/d
47842 54826 – –
12.6 9.8 n/d n/d
32.91 32.64 n/d n/d
2.50 3.15 n/d n/d
0.28 0.16 n/d n/d
0.85 0.59 n/d n/d
2.07 0.00 n/d n/d
4167 40 20 130
41834 52819 52819 52819
15.4 8.0 8.0 8.0
33.83 32.45 32.45 32.45
0.00 8.26 8.26 8.26
0.18 0.54 0.54 0.54
0.75 1.03 1.03 1.03
0.40 3.62 3.62 3.62
G.O. Almandoz et al. / Harmful Algae 6 (2007) 93–103100
was distributed from 388470S to 528190S but highest
Pseudo-nitzschia turgiduloides densities were found
southward 428S, with a maximum of 130 cells l�1
recorded near 528S (Table 4).
4. Discussion and conclusions
Phytoplankton communities were numerically domi-
nated by unidentified phytoflagellates (�5 mm) through-
out almost all samples, which is in accordance with
previous surveys conducted in the area (Carreto et al.,
2003). In particular, the genus Pseudo-nitzschia appeared
most frequently as a minor component of diatom
populations that typically develop at the continental
shelf of the Argentine Sea.
We found the genus Pseudo-nitzschia widely dis-
tributed in surface shelf waters of the Argentine Sea,
being present in 90% of all samples analyzed. Cell
densities were generally low (<103 cells l�1) and often
undetectable in quantitative samples, with infrequent
peak abundances. Although distribution data on Pseudo-
nitzschia spp. for this vast area are sparse, our results
agree with those of Lange (1985) who found Pseudo-
nitzschia spp. widely distributed between 388S and 398Sduring the same seasons. Similar results were also found
by Negri and Inza (1998) in shelf waters between 358Sand 398S. However, these authors mention a sporadic cell
maximum of P. turgidula, which reached bloom
concentrations (>106 cells l�1). Unlike low densities
recorded in shelf waters, higher densities with peak
abundances up to 6 � 106 cells l�1 have been frequently
recorded for coastal and enclosed areas in the Argentine
Sea (Sastre et al., 2001).
The specific richness of the genus Pseudo-nitzschia
in the Argentine Sea was higher than that reported by
Odebrecht et al. (2001) for adjacent shelf surface waters
of Southern Brazil (32–348S).
We found a total of eight species, P. australis, P.
fraudulenta, P. heimii, P. lineola, P. pungens, P. cf.
subcurvata, P. turgidula and P. turgiduloides, from which
P. heimii, P. lineola and P. turgiduloides are first reported
in Argentina. P. australis was found throughout both
seasons, irregularly covering an ample zone of the
Argentine Sea and showing a strong seasonality in its
distribution patterns (Fig. 3). During summer, it was
restricted to the southernmost areas (51–558S), where
low cell concentrations were observed, except for a peak
abundance (6.1 � 104 cells l�1) recorded close to 528S(Fig. 3). This peak was the highest abundance reached by
a Pseudo-nitzschia species throughout our survey and the
highest abundance recorded for P. australis in Argen-
tinean waters (Negri and Inza, 1998; Sastre et al., 2001;
Negri et al., 2004). During autumn, P. australis was
principally found in the northernmost samples (�38–
428S) and generally at high densities (Fig. 3).
P. pungens was the most commonly recorded Pseudo-
nitzschia spp., present in 65% of all samples examined.
This result coincides with other observations in northern
Argentinean shelf waters (Lange, 1985; Negri and Inza,
1998). Moreover, P. pungens was widely distributed,
extending southward as far as 548260S (Fig. 3). This
record, compared to those reported by Hasle (2002),
represents the southernmost record for P. pungens,
transcending that of Rivera (1985) for Chilean coasts
(498520S) in the Pacific Ocean. P. pungens was present in
almost all samples analyzed during summer, whereas its
distribution was restricted to the northern area during
autumn (Fig. 3).
P. fraudulenta and P. cf. subcurvata did not show
clear distribution patterns. Our results, in agreement
with previous studies (Lange, 1985; Negri and Inza,
1998; Sastre, pers. com.), indicate that P. fraudulenta is
an uncommon species in the Argentine Sea. Conversely,
P. cf. subcurvata showed a widespread distribution,
reaching high densities in summer. Historically, P.
subcurvata has been considered to be restricted to
southern cold waters (Hasle and Syvertsen, 1997), and it
has recently been found north of the Polar Front in
Drake Passage (Ferrario and Licea, 2006).
P. heimii, P. lineola, P. turgidula and P. turgidu-
loides were mainly recorded in southerly autumn
samples, characterized by colder, less saline and
nutrient-rich waters. In addition, they were frequently
associated with typical cold water species such as C.
dichaeta, D. antarcticus, T. gracilis and C. pennatum
(Hasle and Syvertsen, 1997), suggesting the influence
of southerly cold water masses. These four Pseudo-
nitzschia species are a common phytoplankton com-
ponent in subantarctic and Antarctic waters (Manguin,
1960; Hasle, 1965; Ferrario et al., 2004; Fiala et al.,
2004). Furthermore, P. turgiduloides is considered to
be restricted to southern cold water regions (Hasle and
Syvertsen, 1997). The presence of Antarctic species in
this area has been seen previously in sediments between
358S and 508S, indicating the northward displacement
of Antarctic-source water masses, which are char-
acterized by high nutrient content and low salinity
(Romero and Hensen, 2002).
In conclusion, spatial and temporal variations of the
environmental parameters recorded in the study area
determined the distribution of Pseudo-nitzschia species.
In this sense, except for P. fraudulenta and P. cf.
subcurvata, two groups can be distinguished according
to their distributional patterns. The first group including
G.O. Almandoz et al. / Harmful Algae 6 (2007) 93–103 101
P. pungens and P. australis has a widespread distribu-
tion and reaches high densities, especially in waters
with elevated temperatures and salinities, and low
nutrient concentrations. In contrast, the other group,
including P. heimii, P. lineola, P. turgidula and P.
turgiduloides shows a more restricted distribution, with
lower densities in relatively cold, less saline and
nutrient-rich waters (Fig. 3 and Table 4).
Other Peudo-nitzschia species have been recorded
previously in the Argentine Sea: P. multiseries, P. seriata,
P. pseudodelicatissima, P. delicatissima and P. aff.
cuspidata (see summary in Ferrario and Galvan, 1989;
Ferrario et al., 2002). Except for the presence of P.
multiseries, these other species require further ultra-
structural analyses to confirm their identification and
presence in Argentinean waters. A particular case is P.
seriata, which is thought to be confined to the Northern
hemisphere (Fryxell and Hasle, 2003). Both previous
SEM studies in the area and the present field study failed
to identify P. seriata in Argentinean waters. Therefore,
we support the hypothesis of Ferrario et al. (2002), who
considered the records of P. seriata in Argentinean waters
to be a misidentification. Furthermore, we suggest that
these early records should have been referred to as P.
australis, a species similar when observed at LM, and
which has been repeatedly mentioned in this area since its
original description in Argentinean waters (Frenguelli,
1939; Hasle, 1965; Lange, 1985; Negri and Inza, 1998;
Ferrario et al., 1999; Sastre et al., 2001; Negri et al.,
2004). A different case is the record of P. pseudodeli-
catissima, whose identity has been recently reexamined,
allowing the description of two new species: P. calliantha
and P. caciantha (Lundholm et al., 2003). Based on this, it
was corroborated that specimens thought to be P.
pseudodelicatissima in Ferrario et al. (1999, 2002)
correspond to P. calliantha. Therefore, the presence of P.
pseudodelicatissima in Argentinean waters is not yet
confirmed.
From the eight Pseudo-nitzschia species found
throughout this survey, P. australis, P. fraudulenta, P.
pungens and P. turgidula are known to be potential DA
producers (Fryxell and Hasle, 2003; Cerino et al.,
2005). Moreover, P. australis has been indicated as a
DA producer in Argentinean waters (Negri et al., 2004).
Conversely, available information on the potential
toxicity of typical cold water species such as P. heimii,
P. lineola, P. subcurvata and P. turgiduloides is scarce,
and therefore further investigations are required on the
potential development of new toxic species.
Although much work is still necessary to understand
the mechanisms underlying their population dynamics,
the present study is the first assessment of the
distribution patterns of Pseudo-nitzschia species along
a vast area of Argentinean continental shelf.
Acknowledgments
We wish to thank technical personnel from the
Instituto Antartico Argentino (IAA), the Servicio de
Hidrografıa Naval and the crew of A.R.A. ‘‘Almirante
Irizar’’ for their support during sampling. Thanks are also
due to P. Sarmiento from the MEB service, Museo de La
Plata and two anonymous reviewers for their suggestions.
This survey was supported from the IAA, the Consejo
Nacional de Investigaciones Cientıficas y Tecnicas
(CONICET) PIP-5603 to M. Ferrario, PEI-2001, CON-
ICET, and PICTO 6524/1108/03-ANPCyT 01-11563 to
I. Schloss. G.O. Almandoz work was supported by a
doctoral fellowship of the CONICET, Argentina.
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