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Life history and population dynamics of the marine cladoceran Penilia avirostris (Branchiopoda: Cladocera) in the Catalan Sea (NW Mediterranean)

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  • Institut de Ciències del Mar - CSIC, Barcelona, Spain

Abstract and Figures

Penilia avirostris is a cosmopolitan marine cladoceran that inhabits coastal and shelf waters of most low and mid latitude ecosystems. In this study, we describe the life history and population dynamics of P. avirostris at a fixed coastal station in the NW Mediterranean Sea. This marine cladoceran was very seasonal, having population maxima in summer (2500-3000 ind m(-3)), and being practically absent from the water column for the rest of the year. The population typically collapsed in late summer-early autumn, and this decline was accompanied by a shift to gametogenetic reproduction, allowing the production of resting eggs to ensure the continuity of the species in the following season. Estimated birth rates of P. avirostris in the Catalan Sea ranged between 0.097 and 0.46 day(-1) and seemed to be decoupled from changes in P. avirostris standing stocks. Birth rates were mainly dependent on the changes in abundance of embryo-carrying females and their brood size, because during the period of population plateau the temperature-dependent embryonic developmental time was rather similar (2.3-2.7 days). Neonates are like miniature adults and need a very short period of growth and moulting to reach the reproductive stage. This life-history trait can explain the fast blooming and dominance of plankton communities by P. avirostris under suitable conditions. Finally, the causes for the seasonal decline of P. avirostris populations are also discussed.
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Life history and population dynamics of
the marine cladoceran Penilia avirostris
(Branchiopoda: Cladocera) in the
Catalan Sea (NW Mediterranean)
D. ATIENZA1*, E. SAIZ1, A. SKOVGAARD2, I. TREPAT1AND A. CALBET1
1
INSTITUT DE CIE
`NCIES DEL MAR (CSIC), PASSEIG MARI
´TIM DE LA BARCELONETA 37-49,08003 BARCELONA,SPAIN AND
2
DEPARTMENT OF BIOLOGY,SECTION
OF PHYCOLOGY
,UNIVERSITY OF COPENHAGEN,ØSTER FARIMAGSGADE 2D,DK-1353 COPENHAGEN,DENMARK
*CORRESPONDING AUTHOR: datienza@icm.csic.es
Received December 13, 2007; accepted in principle December 13, 2007; accepted for publication December 18, 2007; published online
February 1, 2008
Corresponding editor: Roger Harris
Penilia avirostris is a cosmopolitan marine cladoceran that inhabits coastal and shelf waters of
most low and mid latitude ecosystems. In this study, we describe the life history and population
dynamics of P. avirostris at a fixed coastal station in the NW Mediterranean Sea. This marine
cladoceran was very seasonal, having population maxima in summer (2500 3000 ind m
23
),
and being practically absent from the water column for the rest of the year. The population typi-
cally collapsed in late summer early autumn, and this decline was accompanied by a shift to
gametogenetic reproduction, allowing the production of resting eggs to ensure the continuity of the
species in the following season. Estimated birth rates of P. avirostris in the Catalan Sea ranged
between 0.097 and 0.46 day
21
and seemed to be decoupled from changes in P. avirostris standing
stocks. Birth rates were mainly dependent on the changes in abundance of embryo-carrying females
and their brood size, because during the period of population plateau the temperature-dependent
embryonic developmental time was rather similar (2.3 2.7 days). Neonates are like miniature
adults and need a very short period of growth and moulting to reach the reproductive stage. This
life-history trait can explain the fast blooming and dominance of plankton communities by P. avir-
ostris under suitable conditions. Finally, the causes for the seasonal decline of P. avirostris popu-
lations are also discussed.
INTRODUCTION
Cladocerans play a major role in freshwater ecosystems
(Richman, 1958; Lampert, 1987), but have not been
very successful in colonizing the marine environment.
Such colonization requires the evolution of adaptation
mechanisms at the morphological, physiological and
behavioral level (Critescu and Hebert, 2002). The
acquisition of a closed brood pouch to keep the
embryos in a suitable nourishing environment, the pre-
sence of a resting egg provided with a thick wall instead
of an ephippium and the predatory grasping mode in
most species instead of filter-feeding seem to be essential
features linked to this colonization by cladocerans
(Lochhead, 1954; Aladin and Potts, 1995; Critescu and
Hebert, 2002). In this sense, P. avirostris is a rarity within
marine cladocerans for being the only filter-feeding
representative, in clear contrast to the broad presence of
this feeding strategy in freshwater cladocerans.
Penilia avirostris is a seasonally abundant and widely
distributed cladoceran in neritic tropical and subtropical
waters, expanding its distribution towards northern tem-
perate latitudes since the mid-20th century (Lochhead,
doi:10.1093/plankt/fbm109, available online at www.plankt.oxfordjournals.org
#The Author 2008. Published by Oxford University Press. All rights reserved. For permissions, please email: jour nals.permissions@oxfordjournals.org
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1954; Della Croce and Venugopal, 1973; Johns et al.,
2005). When abundant, P.avirostris may play an import-
ant role in marine food webs by concentrating organic
energy of small plankton and making it available to
consumers at higher trophic levels (Paffenho
¨fer and
Orcutt, 1986; Turner et al., 1988; Atienza et al., 2006a).
In this regard, previous field work showed that P.aviros-
tris feed on a wide range of prey, mostly nanoplankton
(2–20 mm), but also larger cells such as dinoflagellates
and diatoms (Atienza et al., 2006a). Moreover, P.avirostris
plays an important role in the recycling of nutrients in
the upper water column, actually contributing to the
limitation by P to phytoplankton growth by excreting
only N derivatives (Atienza et al., 2006b).
In spite of the relevance of this species in the biogeo-
chemical cycles, the information about its population
dynamics is mostly limited to their abundance and sea-
sonal distribution (Della Croce, 1964; Onbe
´and Ikeda,
1995; Tang et al., 1995; Marazzo and Valentin, 2003a;
Valentin and Marazzo, 2003; Wong et al., 2004). These
studies revealed that the temporal distribution of marine
cladocerans is discontinuous during the year, with peaks
of very high abundance followed by rapid decline and
eventual absence from the plankton. Until now, the
factors controlling this pattern remain unclear. Some
authors suggest that temperature may play an important
role in the population dynamics of P. avirostris (Onbe
´and
Ikeda, 1995); however, other factors such as food avail-
ability, chemical composition of seston and photoperiod
might be also relevant (Egloff et al., 1997).
Although the general pattern of its population seaso-
nal cycle is known, the difficulty of rearing these organ-
isms in the laboratory has complicated the estimation of
most of their reproductive parameters (Della Croce,
1964; Tang et al., 1995; Marazzo and Valentin, 2003b;
Wong et al., 2004). The life cycle of P. avirostris is charac-
terized by an alternation between gamogenesis and
parthenogenesis. Their populations are initiated by the
hatching of resting eggs, followed by peaks of high
abundance when parthenogenetic females reproduce
(Onbe
´, 1973, 1978). In marine cladoceran populations,
gamogenetic individuals usually appear immediately
after population maxima, coinciding with decreasing
parthenogenetic reproduction. Gametogenetic repro-
duction produces resting eggs, which sink and remain
on the sea bottom during the seasonal disappearance of
the parental population from the water column (Onbe
´,
1985; Egloff et al., 1997).
The general trend of population dynamics of P. aviros-
tris, briefly described here, resembles that of many fresh-
water cladocerans (Threlkeld, 1987). However, in
contrast to them, we lack deep knowledge about the
reproductive characteristics of P.avirostris at each of the
different phases of its seasonal cycle. Consequently, our
objective was to study the seasonal distribution of the
population of P.avirostris in the Catalan Sea (NW
Mediterranean), taking special care to describe in detail
the reproductive condition of the females during the
seasonal cycle. We believe that certain aspects of P.avir-
ostris life cycle should contribute to explain the explosive
growth and sudden disappearance of this species from
the water column. We also discuss here the influence
that some biological and physical factors could have on
the temporal variation of this species.
METHOD
Penilia avirostris population dynamics were studied from
June 2003 to December 2004 at a near shore station
located half a nautical mile off Port Olı
´mpic, Barcelona
(Spain, NW Mediterranean), characterized by shallow
open sea waters. Zooplankton samples were collected
biweekly, when it was possible, by hand pulling a micro-
plankton net (53 mm mesh, 25 cm mouth diameter;
without flowmeter) vertically from the bottom (38 m
deep). The content of the cod end was preserved in
borax-buffered formaldehyde at 4% final concentration.
In addition, water was collected at a depth of 1 m with a
transparent hydrographic bottle, temperature measured
and the water transported in dark plastic jars to the lab-
oratory for Chlorophyll a(Chl a) determination. Chl a
was measured by filtering 75 and 150 mL onto GF/F
Whatman and 5 mm pore-size polycarbonate nucleopore
filters, respectively. The filters were analyzed fluorometri-
cally after 24 h acetone extraction in darkness and cold.
Further details on sampling and description of the zoo-
plankton community can be found in Skovgaard and
Saiz (Skovgaard and Saiz, 2006).
The total abundance of P. a v i r o s t r i s was determined by
stereomicroscope counts of two 5 mL aliquots from each
sample (sample volume: 250 mL), resulting in at least 300
individuals counted per sample. In addition, for each
sample, 50 individuals of P.avirostris were randomly sorted,
sized and staged. Organisms were classified into the fol-
lowing stages: juveniles (,500 mm), non-reproducing
females, parthenogenetic female (with embryos), gameto-
genetic female (with resting eggs) and males. Body length
(BL, from the tip of the head to the base of the caudal
setae; Uye, 1982) was converted to dry weight (DW, mgC)
using the length– weight relationship log (DW) = 2.66
log BL27.369 (Atienza et al., 2006a) and assuming that
carbon content was 50% of DW (Uye, 1982).
For each of the 50 individual sorted groups, all repro-
ducing females (i.e. carrying embryos or resting eggs)
were dissected carefully with thin needles under the
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stereomicroscope, and the embryos or eggs in the brood
pouch were removed, counted, examined and sized (BL
for embryos; major axis for eggs). Resting eggs were
easily identified because they are ovoid, flattened, with
a thick chitinous membrane and are opaque (Fig. 1E),
occupying the entire brood pouch. Parthenogenetic
embryonic development was divided into four different
stages based on the external morphology of the embryo,
following the detailed description by Della Croce and
Bettanin (Della Croce and Bettanin, 1965) and the sim-
plified approach of Wong et al. (Wong et al., 2004). Stage
1 corresponds to the parthenogenetic egg, ellipsoidal
(although the posterior border of the head can be distin-
guished in the advanced phase), surrounded by an
elastic membrane and almost completely filled with yolk
granules (Fig. 1A). In stage 2, the cover membrane dis-
appears, the second antenna starts to develop and the
thorax region is differentiated (Fig. 1B). During stage 3,
the embryo elongates, the second antenna is fully
formed and the first antenna starts to elongate (Fig. 1C).
At this stage, all the thoracic segments are visible, and
sometimes rudiments of thoracic appendages are
evident. Stage 4 embryos are similar to adults, with all
the thoracic appendages completely formed, and the
carapace and the eye fully developed (Fig. 1D).
Recruitment from parthenogenetical eggs was esti-
mated from the population egg ratio (E/N, where Eis
the number of parthenogenetic eggs and embryos
recorded and Nthe total population size), using the
Paloheimo (Paloheimo, 1974) equation for the instan-
taneous per capita birth rate (b,day
21
),
b¼lnððE=NÞþ1Þ=Dð1Þ
where Dis the egg development time (in days). Dwas
estimated from surface temperature in the water column
using the equation of Bottrell (Bottrell, 1975) for fresh-
water cladocerans,
log D¼0:847ðlog TÞ23:609 log Tþ3:796 ð2Þ
where Tis the temperature in degrees Celsius. The use
of Bottrell’s equation for P. avirostris seems to be war-
ranted since Valentin and Marazzo (Valentin and
Marazzo, 2004) compared field estimates of develop-
mental time for P.avirostris at 24 268C with Bottrell’s
equation predictions, and obtained similar values (2–3
days); other empirical estimations of embryo develop-
mental time in the literature for P.avirostris embryos in
natural conditions also fall in a similar range of values
(ca. 2 days; Mullin and Onbe
´, 1992; Atienza et al.,
2007).
Fig. 1. Developmental stages of P. avirostris defined for this study. (A) stage 1; (B) stage 2; (C) stage 3; (D) stage 4; (E) resting egg. a
1
, first
antenna; a
2
, second antenna; ca, carapace; ey, eye; h, head; m, membrane; ta, thoracic appendices; ts, thoracic segments; yg, yolk granules.
Scale bar denotes 100 mm.
D. ATIENZA ET AL.
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LIFE HISTORY AND POPULATION DYNAMICS OF PENILIA AVIROSTRIS
347
RESULTS
Figure 2 shows the temporal variation of surface temp-
erature and Chl aconcentration and P. avirostris densities
during the study period. Temperature ranged from ca.
128C in winter up to ca. 288C in summer, and Chl a
concentration showed peaks in winter, spring and early
summer, depicting the typical pattern for the northwes-
tern Mediterranean (Calbet et al., 2001; Ribera
D’Alcala et al., 2004). During most of the year, P.avirostris
was absent from the water column, the first individuals
starting to appear at the beginning of July and reaching
peak values by the end of the month (ca. 2500
3000 ind m
23
, Fig. 2C). This population of P.avirostris
maintained until the end of August (2003) or
September (2004), when suddenly declining in the
water column to almost complete absence (followed in
2003 for sporadic low peaks, ,500 ind m
23
, until
December).
The temporal variation of P. avirostris population com-
position is shown in Fig. 3. During the phases of
increase and the peaks of high abundance, the popu-
lations were evenly dominated by juveniles, non-
reproducing females and parthenogenetic females (i.e.
with embryos). When the populations were in the
waning phase, males appeared followed by gametoge-
netic females (i.e. with resting eggs). This general
pattern was common for both years, although in 2003
P.avirostris presence in plankton extended under very
low levels until their complete disappearance (Fig. 3).
During this period, juveniles represented a much lower
fraction of the population compared with other periods,
and the relative contribution of non-reproducing
females was higher, indicating that recruitment during
those peaks failed. Regarding females with resting eggs,
they typically carried only one egg, except for two
females carrying two eggs in 2003 (accounting for 12%
of the gametogenetic females).
Table I and Fig. 4 show the BL of P. avirostris adults.
Gametogenetic females were significantly larger than
males and the other two female types. Mean sizes in
2003 were significantly larger (two-tailed t-test, Welch’s
correction, P,0.01), partly as a consequence of the
fact that the late autumn females in 2003 (absent in
2004) inhabited colder waters and were significantly
larger than the summer ones (Fig. 4, Table II).
Brood size ranged from one to eight embryos per
female and was positively correlated to female body size
(2003: r= 0.85, P,0.001; 2004: r= 0.86, P,0.005;
Fig. 5). Most females typically carried two to four
embryos (Fig. 6), and the two-tailed t-test, Welch’s cor-
rection confirms that there is no significant difference in
mean brood size between 2003 and 2004 (P,0.01). In
terms of population dynamics, there was no clear
change in the proportion of parthenogenetic females
with embryos (relative to the total parthenogenic
females) in the waning phases of P. avirostris populations
(Fig. 7A), nor in female brood size through the popu-
lation development (Fig. 7B). Interestingly, during the
decllining phases, and even during the late peaks in
2003, a significant number of parthenogenic females
were carrying embryos (Fig. 7C).
Embryo length increased with developmental stage
(Table III), ranging from 86 to 315 mm. The latter stage
set the smallest body size for the free living P.avirostris in
Fig. 2. Seasonal variation of surface water temperature (A),
chlorophyll aconcentrations (B) and P. avirostris abundance (C) in the
coastal Catalan Sea during the study.
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the water column. No significant differences were found
in embryo length between both years (two-tailed t-test,
Welch’s correction, P,0.05). There was a negative cor-
relation between embryo stage and brood size (2003: r
=20.95, P,0.001; 2004: r=20.90, P,0.001;
Fig. 8).
Finally, the estimated population egg ratios and the
birth rates were very variable with values ranging
between 0.54 and 3.64 embryos ind
21
and between
0.097 and 0.46 day
21
, respectively (Figs 9A and 9B).
This variability reflected mainly the changes in abun-
dance of embryo-carrying females and female brood
size, whereas the embryonic developmental time, which
depended on the changes in surface water temperature
during the seasonal occurence of P. avirostris, varied
between 2.3 and 2.7 days. Birth rates were highest
during the initial blooming period, thereafter showing
diverse peaks not associated with changes in P.avirostris
density (Fig. 9B). Actually, during the declining phases,
the population birth rates were rather high.
Finally, we found that P. avirostris abundance, egg pro-
duction, birth rates and mean brood size were positively
correlated (P,0.05) with temperature; also there was a
negative correlation between temperature and the size
of none-reproducing females and females with embryos.
Chl aconcentration was negatively correlated (P,0.05)
with P. avirostris abundance, size of none-reproducing
females, egg production, birth rates and mean brood
size (Table IV).
DISCUSSION
Penilia avirostris shows a pronounced seasonality in the
Catalan Sea, with a sudden appearance in the water
column in July due to rapid population growth until a
dense population is established and maintained until
the end of August–September, when standing stocks
diminish. Whereas P.avirostris can be continuously
present in the zooplankton community in tropical and
subtropical latitudes (Della Croce and Venugopal,
Fig. 3. Population composition (as %) of P. avirostris during summer 2003 (left panel) and 2004 (right panel). Abundance of P.avirostris from
Fig. 2 is in the upper panels (dashed line) for the sake of the comparison.
Ta b l e I :Penilia avirostris comparative size
(
m
m) of the different adult reproductive stages
between years
Reproductive
stage
2003 2004
Avg SE nn Avg S E nn
Non-reproducing
females
632.3 5.01 353 606.03 5.31 188 *
Females with
embryos
673.4 4.99 298 641.46 4.56 228 *
Males 651.1 8.93 31 629.05 16.71 23
Females with
resting eggs
799.8 16.66 8 721.92 11.41 19 *
Avg, average; SE, standard error; n, sample size.
*Significant at 0.01.
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LIFE HISTORY AND POPULATION DYNAMICS OF PENILIA AVIROSTRIS
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1973), in temperate ecosystems and specifically in the
Mediterranean, the observed unimodal seasonal pattern
is the typical one (Alcaraz, 1970; Siokou-Frangou, 1996;
Calbet et al., 2001; Ribera D’Alcala
`et al., 2004).
The abrupt appearance and disppearance of the
populations is very characteristic for marine cladocerans
and reflects a typical opportunistic life history. In this
regard, the life cycle of P. avirostris is characterized by
two modes of reproduction, parthenogenesis and game-
togenesis, which follows the general pattern exhibited
by other marine and freshwater cladocerans (Egloff
et al., 1997). Related to both types of reproduction, two
kinds of eggs are also produced by this marine clado-
ceran, a parthenogenetic egg and a thick-walled resting
egg. Parthenogenetic eggs are thin-walled and relatively
small (86 mm), gametogenetic females lay resting eggs,
which are larger (279 mm), fewer in numbers, and
contain yolk (Egloff et al., 1997). In agreement with pre-
vious evidence, gametogenetic females in our study gen-
erally carried only one resting egg, except for the
observation of two individuals carrying two resting eggs
in the brood pouch. The outer membrane of the resting
egg is calcified, which may enhance survival through
the digestive system of potential predators (Onbe
´, 1985),
and facilitates its fast sinking after release, which might
act as an adaptation to prevent predation in the water
column and reduce dispersal by advection (Egloff et al.,
1997). Resting eggs are capable of undergoing diapause,
Fig. 4. Changes in BL of parthenogenetic females (non-reproducing and embryo-carrying) through the seasonal presence of P. avirostris in the
Catalan Sea. Filled circles: summer samples (July–August); open circles: autumn samples (September– October– November). Dotted line is
surface water temperature (from Fig. 2).
Ta b l e I I :Comparative size (
m
m) of P.
avirostris parthenogenetic females (females with
and without embryos) between different periods
in the same year
Reproductive
stage
Summer Autumn
Avg S E nn Avg S E nn
2003 Summer Autumn
Non-reproducing
females
583.4 5.68 142 666.1 6.56 211 *
Females with
embryos
624.7 5.16 161 730.6 6.08 137 *
2004 Summer Autumn
Non-reproducing
females
585.5 5.69 96 627.5 8.57 92 *
Females with
embryos
635.6 6.33 122 648.2 6.55 106
Avg, average; SE, standard error; n, sample size.
*Significant at 0.01.
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carrying the populations through overwintering periods
(Egloff et al., 1997), and their distribution and abun-
dance is a critical factor influencing the overall distri-
bution, seasonal population dynamics, and long-term
variations in the abundance of cladocerans (Viitasalo
and Katajisto, 1994). In some regions, such as the
Inland Sea of Japan, the seasonal fluctuations in the
abundance of resting eggs of this marine cladoceran
have been described in detail (Onbe
´, 1985), but data for
the Mediterranean are more scarce. Moscatello and
Belmonte (Moscatello and Belmonte, 2004) reported
the presence of cladoceran resting eggs in
Mediterranean sediments, and Sioko-Frangou et al.
(Sioko-Frangou et al., 2005) observed that P.avirostris
resting eggs were more abundant (63 76 eggs m
22
)
in September and October, in agreement with the pre-
sence of gametogenetic females in the water column
found in our study.
The observed brood sizes for parthenogenetic P. avir-
ostris in the Catalan Sea are similar to previous reports
for this species (Della Croce and Venugopal, 1973;
Angelino and Della Croce, 1975; Tang et al., 1993;
Marazzo and Valentin, 2003a, b), although our highest
values did not reach the 13 embryos per female
recorded by Angelino and Della Croce (Angelino and
Della Croce, 1975) in the Agulhas Bank and Knysna
Lake (South Africa). Although brood size of marine cla-
docerans typically appears to be higher during the
initial phases of population growth and decreases
rapidly as population increases (Platt and Yamamura,
1986; Mullin and Onbe
´, 1992; Fofonoff, 1994), we did
not find any clear relation during our study between
either female brood size or population egg ratio and P.
avirostris standing stocks. An interesting result was
the negative correlation between the brood size and the
brood stage of development (Fig. 8), which suggests the
abortion and likely re-abortion of embryos, as described
for podonids by Egloff et al. (Egloff et al., 1997).
Fast recruitment of P. avirostris will depend on the
actual birth rates, which in our study were rather vari-
able and did not seem to be reflected in changes in
population abundance (Fig. 9). However, one must be
cautious with such interpretation, because much of the
variability in P.avirostris abundance may merely reflect
spatial variability (sampling was carried out at a single
fixed station, see below). Evidence that spatial varibility
exists was found in the data obtained by a parallel zoo-
plankton survey study conducted during summer 2003
and 2004 covering the whole Catalan Sea shelf ( four
CACO cruises; Atienza et al., in preparation). During
those cruises, we found a high variability in P.avirostris
abundance between station for the same sampling
period, and, for example, through CACO-1 (July 2003)
abundances ranged between 41 and 2491 ind m
23
between stations. The variability between stations was
the same for the other three cruises and clearly indi-
cated that spatial variability should be considered to
explain the variation in the abundance of P.avirostris.
For this reason, no attempt to estimate population
growth and mortality rates has been made. In this
regard, it is important to note that the observed varia-
bility in birth rates reflects essentially the variability in
the population egg ratio, since during the periods of
high standing stocks embryonic developmental times
were rather similar (2.3– 2.7 days).
Penilia avirostris must likely rely on the hatching of
resting eggs to establish the new population annually
because this marine cladoceran is practically absent
Fig. 5. Scatterplot of BL (mm) and brood size (number embryos
female
21
)ofP. avirostris.
Fig. 6. Frequency distribution of brood size (number embryos
female
21
) in the P. avirostris population in the Catalan Sea. Avg,
average; SE, standard error; n, sample size.
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LIFE HISTORY AND POPULATION DYNAMICS OF PENILIA AVIROSTRIS
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from the water column in winter and spring. Once
certain threshold values in environmental variables are
reached, parthenogenetic growth can explain the rapid
development of the population. For instance, there is a
4-fold increase in volume between the egg (stage 1) and
the neonate (stage 4), neonates being one-half to
two-thirds to their eventual length as adults (Egloff et al.,
1997). This development allows the newly born P.aviros-
tris to reach adulthood (reproductive period) in about 1
day (Atienza et al., 2007). A simple calculation consider-
ing an average initial brood size of 4, an embryonic
developmental time of 2 days (Mullin and Onbe
´, 1992;
Fig. 7. (A) Proportion of parthenogenetic females carrying embryos in relation to total parthenogenetic females during the seasonal presence of
P. avirostris in the Catalan Sea. Abundance of P.avirostris from Fig. 2 is overlaid (dashed line) for the sake of the comparison. (B) Variation of
brood size (average+1SE). (C) Brood size class distribution (as %).
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Atienza et al., 2007) and a period of 1 day from the
neonate to the reproductive stage, suggests that every
female may produce near 100 young individuals in 8
days. Atienza et al (2007) suggested that it was this short
developmental time to the reproductive stage which
allowed P.avirostris to rapidly appear and bloom in
coastal environments in comparison with copepods,
which have similar embryonic development times but
much slower development to the reproductive adult
stage.
The possible causes for the sudden disappearance of
P. avirostris from the water column are not well under-
stood. The decline in the annual population of clado-
cerans is typically accompanied by the onset of
gamogenetic reproduction and the production of over-
wintering resting eggs. In natural populations, only a
fraction of parthenogenetic females turn into gametoge-
netic females (i.e. Evadne spp.: 8– 25%, Pseudoevadne terges-
tina: 5–10%, Onbe
´and Ikeda, 1995; Pleopis
polyphemoides: 10 46%, Fofonoff, 1994; 20 23% P. terges-
tina: Onbe
´, 1978; 50 80% Podon leuckarti: Egloff et al.,
1997; and 25–60% Evadne nordmanni: Fofonoff, 1994).
The fraction of gametogenetic P.avirostris females
observed in our study is in the low range of values
found for other marine cladocerans (4 8% in 2003; 1
20% in 2004), as also observed by Marazzo and
Valentin (Marazzo and Valentin, 2003b) for P.avirostris
in Brazilian waters (11– 24%).
This shift from parthenogenetic to gametogenetic
reproduction is an interesting phenomenon. In fresh-
water cladocerans, it is known that the appearance of
males seems to be under hormonal regulation (Minelli
and Fusco, 2006) and that crowding, photoperiod,
temperature and food availability act as stimuli to
induce gamogenesis in parthenogenetic females (Stross
and Hill, 1968; Kleiven et al., 1992; Carvalho and
Hughes, 1983; Stross, 1987; Berg and Pa
´lsson, 2001).
Stross (Stross, 1965) suggested that at least two stimuli
are necessary to induce gametogenetic reproduction.
However, the causes that induce this shift from parthe-
nogenetic to gametogenetic reproduction in marine cla-
docera are not fully understood (Fofonoff, 1994). Recent
attempts to find evidence in freshwater cladocerans of
the presence of the endobacterium Wolbachia, which is
involved in the onset of parthenogenetic reproduction
in many invertebrates (Stouthamer et al., 1999) have
failed (Fitzsimmons and Innes, 2005).
Environmental conditions seem to play a key role in
the decline of populations at the end of the season (e.g.
decrease in temperature, photoperiod, food availability,
turbulence, crowding, predation; Frey, 1982; Fofonoff,
1994; Stross and Hill, 1968). Penilia avirostris populations
in the Mediterranean Sea typically vanish in late
summer–early autumn (Alcaraz, 1970; Lipej et al.,
1997; Calbet et al., 2001; Ribera D’Alcala
`et al., 2004).
The decline in P.avirostris population observed in 2003
(with some limited blooming in October and
November) was premature in comparison with the 2004
data. Although a priori this fact could suggest variability
in the timing of the onset of the factors triggering it,
however, a parallel zooplankton survey conducted during
summer 2003 and 2004 covering the whole Catalan
Sea shelf (CACO cruises; Atienza et al., in preparation)
shows that the observed decline was a local event at our
sampling station, associated with the intrusion of high
saline oceanic waters into the central (and compara-
tively narrower) shelf of the Catalan Sea. Very likely the
late peaks of P.avirostris in autumn 2003 reflect the
receding of these oceanic waters in this area. Similar
late peak events have been observed previously in the
NW Mediterranean (Castello
´n waters, Alcaraz, 1970;
Gulf of Trieste, Lipej et al., 1997), although it is not
known if the causes are similar.
Temperature has been proposed as the main physical
factor that controls P. avirostris populations (Gieskes,
Table III:Size (large axis,
m
m) of the
different embryo stages of P. avirostris
Embryos
stage
2003 2004
Avg SE nn Avg SE nn
Stage 1 86.5 4.61 88 85.5 4.22 68
Stage 2 179.8 3.68 57 179.4 3.31 50
Stage 3 221.4 2.75 103 219.9 3.69 87
Stage 4 315.4 6.88 51 305.0 8.63 23
Resting
eggs
282.3 14.97 8 277.2 2.99 1
Avg, average; SE, standard error; n, sample size. No significant
differences were found.
Fig. 8. Scatterplot of embryo stage and brood size of P. avirostris.
D. ATIENZA ET AL.
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LIFE HISTORY AND POPULATION DYNAMICS OF PENILIA AVIROSTRIS
353
1971; Onbe
´and Ikeda, 1995). In general, populations
of P.avirostris are often associated with warmer waters in
the northern (Lipej et al., 1997; Calbet et al., 2001) and
southern hemisphere (Resgalla and Montu´, 1993), and
we also found a positive correlation between the abun-
dance of this marine cladoceran and temperature.
However, this optimum range of warm temperatures
where P.avirostris can reproduce and grow successfully
appears to vary geographically. Some authors have
pointed out that the distribution of P.avirostris is mostly
restricted to waters above 188C but can range between
128C and 308C (Kim et al., 1994; Kim and Onbe
´,
1995), and it is known that this species has an optimum
temperature around 258C (China: Tang et al., 1995;
Japan: Onbe
´et al., 1996). Recently, Johns et al. (Johns
et al., 2005) showed that this species is increasing in
prevalence in the North Sea, where the sea surface
temperature has been increasing over the last decade
(more than 38C, and reaching temperatures higher than
198C).
Food availability has also been suggested to affect the
seasonal dynamics of P. avirostris. Lipej et al. (Lipej et al.,
1997) and Calbet et al. (Calbet et al., 2001) indicated
that during warm periods (summer), the water column
was stratified and the concentrations of nutrients and
chlorophyll above the pycnocline are rather low,
whereas pico- and nanoplanktonic autotrophs are abun-
dant. Penilia avirostris is a filter feeder that ingests nano-
flagellates preferentially (Atienza et al., 2006a), and the
higher abundance of these organisms results in a higher
availability of food that is rapidly exploited. It is also
important to notice that P.avirostris occurs mainly in
coastal and shelf waters, where chain-forming diatoms
Fig. 9. (A) Population egg ratio (average number of eggs/embryos ind
21
) and (B) estimated birth rates (day
21
)ofP.avirostris in the Catalan Sea.
Dotted line, abundance of P.avirostris.
Ta b l e I V:Spearman’s correlations between
different P. avirostris population parameters
and some environmental variables
TT Chl aa tot Chl aa >5mm
Abundance 0.78* 20.43* 20.46*
Size of non-reproducing females 20.79* 20.17 20.56*
Size of females with embryos 20.85* 20.15 20.43
Egg production 0.77* 20.44* 20.47*
Birth rates 0.72* 20.51* 20.51*
Mean brood size 0.44* 20.43* 20.47*
T, sea temperature; Chl atot, total chlorophyll aconcentration; Chl a.
5mm, chlorophyll a.5mm concentration.
*Significant at P,0.05.
JOURNAL OF PLANKTON RESEARCH
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PAGES 345357
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354
are typically an important component of autotrophic
biomass during the non-stratified periods. Penilia avirostris
is a typical filter feeder (Paffenho
¨fer and Orcutt, 1986),
and even though it shows some degree of prey selection
(Atienza et al., 2006a), it most likely experiences detri-
mental effects and clogging when exposed to long
chains of diatoms. It may well be that the preference for
warmer waters exhibited by P.avirostris is not only
related to temperature per se but also to the degree of
stratification of the water column as pointed out by
Alcaraz (Alcaraz, 1970); higher stratification in summer
would be accompanied by a relatively lower abundance
of long chain-forming diatoms and relatively higher
abundance of nanoflagellates. This hypothesis agrees
with the fact that in the Western Mediterranean the
decline of P.avirostris populations is typically associated
with a seasonal regime of thunderstorms and heavy
rainfall in late summer early autumn (Duarte et al.,
1999) with associated wind stress and increased run-off
that must affect water column stability.
Finally, an additional cause for the disappearance of
P. avirostris populations in late summer early autumn
could be predation pressure, which has shown to be
very important in freshwater systems affecting cladocer-
ans morphology, size, composition and abundance
(Grant and Bayly, 1981; Thys and Hoffmann, 2005).
The importance of predation in shaping marine zoo-
plankton communities has been traditionally neglected
(Verity and Smetacek, 1996). There is evidence that pre-
dators such as ctenophores, chaetognaths and fish
larvae have the potential to decimate marine cladoceran
populations (Canino and Grant, 1985; Duro
´and Saiz,
2000; Nip et al., 2003; Barz and Hirche, 2005).
However, in the NW Mediterranean, no studies have
addressed the effects of predation on the population
dynamics of P.avirostris.
ACKNOWLEDGEMENTS
The authors also wish to thank the help of Pepito and
Ramon for boat facilities and assistance at sea.
FUNDING
This work was supported by the Spanish projects
REN2001-1693 and CTM2004-02 575/MAR. D.A.
benefitted from fellowships from the Spanish Ministerio
de Educacio
´n y Ciencia, and from the Grup d’Ecologia del
Zoopla
`ncton Marı
´funded by the Generalitat de
Catalunya.
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... Contrasting its diversity, only eight Cladocera species are marine forms (Onbe, 1977), having a wide distribution in the world's seas. Although seasonal abundance peaks of marine cladocerans are well known, studies investigating that their reproductive strategies and fecundity are limited Valentin, 2003a, 2004a;Atienza et al., 2008;Dvoretsky and ve Dvoretsky, 2020). Their life cycle is characterized by the alternation between gamogenesis and parthenogenesis. ...
... The temperature is associated with the percentage of Cladocera in zooplankton communities and the cyclicity in their reproductive strategy Valentin, 2003a,b, 2004a,b;Atienza et al., 2008). Penilia avirostris as the most dominant Cladocera species in the SoM, were found between 11.6-24.8 ...
... During the peak abundance period, only PF individuals were recorded, but GF and M individuals were observed lowest in the periods of decline that followed. Dominant PF individuals was reported in previous studies for other regions, but also with higher GF and M ratios than our results (Marazzo and Valentin, 2001, 2003a, 2004bAtienza et al., 2008). This kind of expected temporality in the cyclical reproductive strategy of Cladocera was only evident for P. avirostris in the SoM. ...
Article
Zooplankton is an essential component of marine ecosystems, with Copepoda and Cladocera being the most important zooplankton groups in all the world's seas. In the Sea of Marmara, Cladocera has the highest participation in zooplankton abundance. Here we investigated reproductive strategies and population characteristics of four Cladocera species; Penilia avirostris, Pleopis polyphemoides, Evadne nordmanni, and Pseudoevadne tergestina in the Sea of Marmara, northeastern part of Mediterranean Sea. Reproduction strategy, fecundity, and embryonic development of four Cladocera species were achieved. During our study period from 2004 to 2008, there was an extreme jellyfish bloom caused by Liriope tetraphylla and following mucilage event occurred between the years 2006 and 2008. Thus, we also compared the change in phenology and reproductive strategy of cladocerans amongst periods characterized by extreme events and against a suite of environmental parameters. The most dominant Cladocera species in the Sea of Marmara were Penilia avirostris and Pleopis polyphemoides. The population structures of Cladocera species according to their reproductive strategies, parthenogenetic female individuals provided rapid exponential reproduction, and were dominant at 60-100%. Parthenogenetic fecundity success was found significantly different among Cladocera species. The most remarkable result during the study period was observation of increase in embryo production while populations were in decrease.
... This heightened sensitivity may be particularly significant in the context of Tinto-Odiel inner zone, where the concentrations of these heavy metals are elevated (González-Ortegón et al., 2019). Therefore, tolerance to pollutants, along with other environmental factors that significantly influence the population dynamics of P. avirostris, such as food availability, turbulence, and predation (Atienza et al., 2008), could collectively contribute to the observed niche segregation within this estuary. In addition, the dominance of A. tonsa in the inner zone of TO may also contribute to the taxonomic differentiation of its mesozooplankton assemblages. ...
... The association between P. avirostris and lower oxygen concentrations may be an indirect effect of water turbulence induced by river freshwater flow, as suggested by other researchers (Della Posta and de Leme, 2015). Notably, the Tinto-Odiel estuary, characterized by the lowest mean river flow (3.5 m 3 /s) compared to Guadiana (13.5 m 3 /s) and Guadalquivir (39.7 m 3 /s) features calm waters that, coupled with other influencing factors described above, could create an optimal habitat for the observed cladoceran outbreaks, particularly those of P. avirostris, which has been reported to be negatively affected by turbulence (Atienza et al., 2008). ...
... However, historical records showed Penilia avirostris was dominated in summer since 1984 (Al-Azri et al., 2014;Lian et al., 2011). Food availability and temperature are crucial for the population dynamics of P. avirostris (Atienza et al., 2008;Onbé and Ikeda, 1995). In 2001, an outbreak of P. avirostris was occurred in Dapeng Cove, and the dominant phytoplankton species were Nitzschia sp. and Skeletonema costatum (Li et al., 2014;Song et al., 2004). ...
... The surface seawater temperature in this study ranged from 29.3 to 32.2 • C, and the maximum temperature reached 32.2 • C near the Nuclear Power Station. However, seawater temperature below 30 • C is optimal for P. avirostris bloom (Ambler et al., 2013;Atienza et al., 2008). Summarily, plenty of studies have shown the long-term change of hydrological environments and phytoplankton community composition in Daya Bay (Song et al., 2004;Wu et al., 2017;Yang and Tan, 2019), but how zooplankton community composition responds to these changes remains unclear. ...
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Daya Bay is a eutrophic coastal region with dynamic physico-chemical conditions influenced by terrestrial inputs and seawater intrusion. Zooplankton is a crucial trophic intermediary for energy transfer and fishery resources. In this study, we assessed the distribution and composition of zooplankton in Daya Bay during summer and winter of 2015. We found that zooplankton diversity was the lowest and dominated by small copepods (Acartia spp. and Paracalanus spp.) and gelatinous Oikopleura spp. under terrestrial inputs in the Dan'ao River estuary and Aotou barbour. The highest zooplankton diversity was observed at the bay mouth that influenced by salty intruded seawater, and the dominant oceanic species (such as Euchaeta concinna and Subeucalanus subcrassus invaded into the top of the bay in winter. The dominant species in the estuary shift from Penilia avirostris to Acartia spp. compared with historical researches, indicating the effect of human activities on the succession of dominant species.
... Regarding other marine zooplankton groups, they overall show similar C:N molar ratios to those of copepods, with mean value close to 5 (Kiørboe, 2013;Uye, 1982); information on their P content, however, is much scarcer. Marine cladocerans, similarly to the freshwaters counterparts, have reproductive rates much higher than those of copepods (Atienza et al., 2008) and may be more prone to P limitation given their comparatively lower C:P and N:P ratios (Gismervik, 1997;Hébert et al., 2016) and high retention rates (Atienza et al., 2006). Appendicularians, a very important group of filter-feeding zooplankters, also have fast growth rates (Deibel and Lowen, 2012) and are potentially very sensitive to phosphorus availability; the existent data suggests lower C:P and N:P molar ratios than those of co-existing copepod species (Sommer et al., 2004). ...
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We assessed the effects of nutrient imbalanced diets on the feeding, reproduction and gross-growth efficiency of egg production of the copepod Paracartia grani. The cryptophyte Rhodomonas salina, cultivated under balanced (f/2) and imbalanced growth conditions (N and P limitation), served as prey. Copepod C:N and C:P ratios increased in the imbalanced treatments, particularly under P limitation. Feeding and egg production rates did not differ between the balanced and N-limited treatments but decreased under P limitation. We found no evidence of compensatory feeding in P. grani. C gross-growth efficiency averaged 0.34 in the balanced treatment and declined to values of 0.23 and 0.14 for the N- and P-limited treatments, respectively. Under N limitation, N gross-growth efficiency increased significantly to a mean value of 0.69, likely as a result of increasing the nutrient absorption efficiency. P gross-growth efficiency reached values > 1 under P limitation, involving the depletion of body P. Hatching success was >80%, with no differences among diets. Hatched nauplii, however, had lower size and slower development when the progenitor was fed a P-limited diet. This study highlights the effects of P limitation in copepods, which are more constraining than N, and the presence of maternal effects driven by prey nutritional composition that ultimately may affect population fitness.
... For example, the population of copepods may increase in weeks or months (Hansen et al., 2006), whereas the population of cladocerans may increase in days or weeks (Egloff et al., 1997;Park and Marshall, 2000). Particularly, cladocerans have a very short generation time compared to copepods, and therefore determining their seasonal abundance requires an in-depth understanding of their reproductive characteristics through frequent sampling (Omorii and Ikeda, 1984;Mullin and Onbe, 1992;Atienza et al., 2008). Therefore, to quantitatively evaluate mesozooplankton populations and communities, the survey period and interval must be considered by reflecting the reproductive characteristics of taxonomic groups (Omorii and Ikeda, 1984;Klais et al., 2016). ...
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Gamak Bay is frequently affected by hypoxia in summer. Therefore, this study aimed to examine the effect of hypoxia on the mesozooplankton community of this region. Mesozooplankton samples were obtained biweekly (28 times) at a hypoxic station (inner bay) and a normoxic station (middle bay) using a conical net (mesh size 200 μm; mouth diameter 30 cm) from April 2020 to April 2021. In the inner bay, hypoxia was observed a total of five times between early June and late September, whereas no instances of hypoxia were detected in the middle bay. During the hypoxic period, mesozooplankton abundance was higher in the inner bay than the middle bay ( p < 0.05). During the normoxic period, there was no difference between the inner bay and the middle bay ( p > 0.05). The dominant species in the hypoxic period were three species of cladocerans ( Pleopis polyphemoides , Pseudoevadne tergestina , Penilia avirostris ) and the copepod Acartia sinjiensis . The abundance of cladocerans was higher in the inner bay, and that of A . sinjiensis was higher in the middle bay ( p < 0.05). In addition to water temperature, salinity, and size-fractionated Chl- a concentration, mesozooplankton abundance was also significantly correlated with the bottom DO concentration. Collectively, our findings suggest that hypoxia can affect mesozooplankton abundance and occurrence times.
... Predation pressure is considered an important factor affecting cladoceran abundance Atienza et al. 2008;Oghenekaro and Chigbu 2019). Cladocerans have been found in the gut contents of pelagic fish larvae collected in open ocean, such as Pacific saury (Morita and Arima 2022), billfish (Llopiz and Cowen 2008), and Pacific bluefin tuna (Kodama et al. 2017). ...
Article
Although marine cladocerans are known as coastal zooplankton, they sometimes appear in offshore waters in large numbers. In Suruga Bay, located in the center of Japan and opens to the Pacific Ocean, cladocerans occur abundantly in offshore waters during the spring and summer seasons. However, the mechanisms by which these offshore populations form in the bay are still unknown. The aim of this study was to clarify the factors that explain these offshore cladoceran populations by combining field sampling and numerical experiments, using particle-tracking methods. Cladocerans showed different occurrence patterns in coastal and offshore areas. Abundance of Penilia avirostris, the dominant offshore species, was much higher in offshore than in coastal areas. The unique filter feeding of Pe. avirostris may enable it to survive in offshore Suruga Bay with less abundant food conditions. On the other hand, while Pleopis polyphemoides and Podon leuckartii occurred abundantly in coastal areas, they appeared in very small numbers in offshore areas. This suggests that offshore environments are unfavorable for them to maintain populations. Particle-tracking experiments demonstrated that particles released from the coast of Suruga Bay were transported to and accumulated at the inner offshore region of the Bay from March to August. Those patterns were not observed in other months. Our results suggest that a combination of transport of coastal populations by surface circulation currents and biological characteristics of the species to survive in oligotrophic and high-salinity offshore environments contribute to form periodic mass occurrences of cladocerans in offshore Suruga Bay.
... This indicates a regime shift in the Mediterranean (Conversi et al., 2010), warmer surface temperatures accelerate the reproductive cycle of Penilia spp. (Atienza et al., 2008) and lead to an earlier attainment of sexual maturity for Evadne spp. (Egloff et al., 1997). ...
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The Strait of Gibraltar is known as the gate between the North East Atlantic and the Mediterranean Sea with still expanding heavy marine traffic, utilising the port in the Bay of Gibraltar. This can lead to a heavily modified waterbody, with an increase of pollution and nutrient input. The water masses in the Bay of Gibraltar are modulated by strong winds, currents and tides, creating an inflow of Atlantic waters during the rising tide and an eastward stream of outflowing waters during the lowering tide. Zooplankton is a key player in marine ecosystems, linking the energy transfer between primary production and higher trophic levels. Because zooplankton directly responds to variability in their environment, their dynamics are affected by anthropogenic pressures and hydroclimatic changes, which can be monitored by regularly sampling zooplankton in the water column. In the Mediterranean Sea zooplankton is well and widely studied, with temporal and spatial studies in numerous regions around the Sea. In the Bay of Gibraltar however, zooplankton has been essentially overlooked, which has implications for assessing and maintaining good environmental status in the waters of the Bay. The aim of this study was to create the first baseline study of zooplankton distribution in the Bay of Gibraltar, while observing the tidal influences. Before, a critical literature review was conducted to identify gaps in knowledge and emerging trends in the study of zooplankton in the Mediterranean Sea region, which confirmed the presumption of a lack of zooplankton studies in the Gibraltar area and revealed among other things the ZooScan image analysis methodology and normalised biomass spectrum theory as emerging trends in the Mediterranean waters. With the collected and digitised zooplankton data a learning set for the Bay of Gibraltar was created using the web application EcoTaxa, the final precision and recall rate of the learning set proved high, which makes it suitable for usage in future monitoring studies (under the condition of using the same image analysis methodology). The zooplankton community in the Bay was taxonomically diverse, showing spatial patterns with differences in predominating taxa and highest total abundances in the head of the Bay. The influence of the tides and currents created differences in environmental and biological conditions, with the low tide indicating increased water temperature, dissolved oxygen and zooplankton abundance. The inflow of water during high tide decreased water temperature, dissolved oxygen and zooplankton abundance and the currents flush eggs and smaller species in and out of the Bay. The surface waters in the Bay of Gibraltar are therefore a heterogenous system with various prevailing environmental and anthropogenic influences that need to be measured to interpret the zooplankton dynamics. Total abundances ranged from 81.5 ind. m3 outside of the Bay during high tide, to 250.8 ind. m3 at the head of the Bay during low tide. Copepods generally dominated the zooplankton community, however, on the east side of the Rock of Gibraltar the copepod community was overtaken by Cladocera. Evadne and Penilia showed differences in their distribution between high and low tide sampling and their dominant appearance might mirror a regime shift in the Mediterranean that has been observed in other regions and can be related to an increase in water temperatures. Acartia and Paracalanus dominated the copepod community at all stations. While the abundance of Acartia was stable throughout the inflow and outflow of water masses, Paracalanus abundance grew with the lowering of the tide, possibly because of different migration behaviours. The proposed methodology for future zooplankton monitoring studies in the Bay of Gibraltar provides many benefits (such as saving time and simplifying the taxonomic identification). Some aspects however, need to be reconsidered; for a representative presentation of the zooplankton community it is recommended to sample more layers of the waterbody, using at least two nets with differences in their mesh size to sample smaller and larger zooplankton species. The timing of sampling needs to be adapted as well, to precisely measure the influences of in- and outflowing waters, and a wider range of environmental factors at the time of sampling need to be measured in the future. This study is the first to give a taxonomic overview of zooplankton in the Bay of Gibraltar and with the proposed methodology forms the basis for initiating long-term zooplankton monitoring in the Bay of Gibraltar. Regular monitoring could create many opportunities, such as measuring and maintaining good environmental status and detecting potential threats: a regime shift in the Mediterranean, an introduction of foreign species through the ballast waters of shipping and uncontrolled proliferation of microalgae.
... This species appears during the warm-water season in temperate water (Onbé 1968, Lipej et al. 1997, Viñas et al. 2007. As some previous studies reported (Atienza et al. 2008, Miyashita et al. 2010, Kane 2013, we also observed a positive correlation between Pe. avirostris abundance and water temperature. On the other hand, negative correlations between Penilia abundances and chlorophyll a concentrations are probably due to the sporadic high chlorophyll a concentrations observed during the cold-water season from November to March, when this species rarely appeared (Table 2, Fig. 2). ...
Article
Seasonal occurrences of marine cladocerans in offshore Suruga Bay, Japan, were studied from 2014 to 2019. Zooplankton samples were collected monthly from a station (depth: ca. 1000 m) located in the offshore area of the bay. Cladocerans appeared each year from February to December, and disappeared in January. Their abundance in- creased drastically from April to September and comprised a substantial portion of the offshore mesozooplankton com- munity during this period. Maximum cladoceran abundance occurred from June to August, ranging from 65.9–1341.9 individuals m−3. These patterns in cladoceran abundances were basically repeated each year throughout the study pe- riod. This result suggests that mass occurrences of cladocerans in offshore regions of the bay during the spring-summer are regular events rather than sporadic. Seven species, which have previously been reported from Japanese waters, were identified, and successional changes in the dominant species were observed. The most abundant species, Penilia aviros- tris, carried parthenogenetic embryos in brood pouches, suggesting that they were not simply transported from coastal areas, but that they also reproduce in the offshore waters. Regular mass occurrences of marine cladocerans in offshore Suruga Bay could have an important impact on the offshore ecosystem of the bay, and factors enabling these population cycles need to be determined.
Chapter
Plankton are organisms not able to swim against water currents. They live in every aquatic environment and stand at the base of food webs and biogeochemical cycles on our planet. Plankton include prokaryotes (unicellular organisms without a nucleus), protists, and protozoans (unicellular eukaryotes or organisms with a proper nucleus) and metazoans (multicellular eukaryotes). These groups feature a huge biological diversity, which cascades into a myriad of different sizes, forms, behaviors, and, ultimately, roles played in aquatic ecosystems. The interaction of different plankton species produce complex ecological networks encompassing multiple feeding connections, or trophic links. The complexity of interactions among plankton is an emergent property whose investigation is made possible by ecological‐network models. Long‐term ecological research programs aiming at assessing ocean health can profit from these modeling tools to integrate (i) plankton biodiversity explorations and (ii) the search for the role played by the entangled plankton webs in the functioning of our planet's largest environment, i.e. the ocean.
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Mesozooplankton abundance and community composition are influenced by hydrography and biological interactions. In subtropical systems influenced by seasonal monsoons, seasonal cycle of plankton communities could be disrupted and restructured by short but intense weather events. Our survey of a shallow subtropical embayment to the northern part of the South China Sea demonstrated temporal variations in zooplankton biomass and composition between monsoon periods: not only were the wet (summer monsoon) and dry (winter monsoon) periods distinctive from each other, but also the transition phase between the two. The meroplankton communities were distinct between the monsoon periods with fish, decapods and echinoderm peaked during the wet season and cirripedia bloomed in dry season. This pattern can be attributed to both changes in growth conditions and influx of individuals through monsoon-driven water currents. The community shift during the transitional phase, defined by the rapid changes in salinity and temperature, corresponded to the reported reproductive cycles of marine organisms, including commercially important fishes, crustaceans, and echinoderms. The interannual variability observed during the wet period reflected changes in rainfall between consecutive years, highlighting the importance of having a long time series with which to establish a baseline information to better manage nursery habitats like the one surveyed, particularly in light of increasing coastal development. Subtropical coastal zooplankton communities are highly dynamic with multiple pulses and interruptions driven by weather events.
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The distribution of marine cladocerans was investigated in summer at 8 stations in Otsuchi Bay in the northeastern part of Honshu, Japan. Two species occurred abundantly on 3-4 September 1973: Penilia avirostris and Evadne tergestina, of which the former was most abundant with a density of 300 indiv. m-3, while the latter occurred at a density of at most 90 indiv. m-3. During this period, the water in Otsuchi Bay was predominantly warm and originated mainly from branches of the Kuroshio Current. On 26 August 1975, all seven species of marine cladocerans hitherto known from Japanese waters were detected in smaller numbers than occurred in September 1973; i.e., Penilia avirostris, Evadne tergestina, Evadne nordmanni, Evadne spinifera, Podon leuckarti, Podon schmackeri and Podon polyphemoides. This highly diverse cladoceran fauna probably occurred as a result of the coexistence of different water masses within the bay, deriving from branches of both the cold Oyashio Current and the warm Kuroshio Current, together with an incursion of Tsushima Warm Water from the Sea of Japan through the Tsugaru Strait.
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A method is described whereby ephippia (sexual eggs plus protective membranes) are experimentally induced at low food levels (= or <0.05 mg spinach D. magna-1), high female culture-densities (= or >0.4 D. magna ml-1) and in short-day photoperiods (L:D <12:12, 12oC). The density-dependent ephippial response was related to an increased encounter rate between females at the higher densities.-from Authors