ArticlePDF Available

Development, application and evaluation of a 1-D full life cycle anchovy and sardine model for the North Aegean Sea (Eastern Mediterranean)

PLOS
PLOS ONE
Authors:

Abstract and Figures

A 1-D full-life-cycle, Individual-based model (IBM), two-way coupled with a hydrodynamic/biogeochemical model, is demonstrated for anchovy and sardine in the N. Aegean Sea (Eastern Mediterranean). The model is stage-specific and includes a 'Wisconsin' type bioenergetics, a diel vertical migration and a population dynamics module, with the incorporation of known differences in biological attributes between the anchovy and sardine stocks. A new energy allocation/egg production algorithm was developed, allowing for breeding pattern to move along the capital-income breeding continuum. Fish growth was calibrated against available size-at-age data by tuning food consumption (the half saturation coefficients) using a genetic algorithm. After a ten-years spin up, the model reproduced well the magnitude of population biomasses and spawning periods of the two species in the N. Aegean Sea. Surprisingly, model simulations revealed that anchovy depends primarily on stored energy for egg production (mostly capital breeder) whereas sardine depends heavily on direct food intake (income breeder). This is related to the peculiar phenology of plankton production in the area, with mesozooplankton concentration exhibiting a sharp decrease from early summer to autumn and a subsequent increase from winter to early summer. Monthly changes in somatic condition of fish collected on board the commercial purse seine fleet followed closely the simulated mesozooplankton concentration. Finally, model simulations showed that, when both the anchovy and sardine stocks are overexploited, the mesozooplankton concentration increases, which may open up ecological space for competing species. The importance of protecting the recruit spawners was highlighted with model simulations testing the effect of changing the timing of the existing 2.5-months closed period. Optimum timing for fishery closure is different for anchovy and sardine because of their opposite spawning and recruitment periods.
Content may be subject to copyright.
RESEARCH ARTICLE
Development, application and evaluation of a
1-D full life cycle anchovy and sardine model
for the North Aegean Sea (Eastern
Mediterranean)
Athanasios GkanasosID
1,2
, Stylianos Somarakis
3
, Kostas Tsiaras
2
,
Dimitrios Kleftogiannis
4
, Marianna Giannoulaki
3
, Eudoxia Schismenou
3
,
Sarantis Sofianos
1
, George TriantafyllouID
2
*
1Department of Environmental Physics, University of Athens, Athens, Greece, 2Hellenic Centre for Marine
Research (HCMR), Mavro Lithari, Anavyssos, Greece, 3Hellenic Centre for Marine Research (HCMR),
Thalassocosmos Gournes, Heraklion, Crete, Greece, 4Genome Institute of Singapore (GIS), Agency for
Science Technology and Research, Singapore
These authors contributed equally to this work.
*gt@hcmr.gr
Abstract
A 1-D full-life-cycle, Individual-based model (IBM), two-way coupled with a hydrodynamic/
biogeochemical model, is demonstrated for anchovy and sardine in the N. Aegean Sea
(Eastern Mediterranean). The model is stage-specific and includes a ‘Wisconsin’ type bioen-
ergetics, a diel vertical migration and a population dynamics module, with the incorporation
of known differences in biological attributes between the anchovy and sardine stocks. A new
energy allocation/egg production algorithm was developed, allowing for breeding pattern to
move along the capital-income breeding continuum. Fish growth was calibrated against
available size-at-age data by tuning food consumption (the half saturation coefficients)
using a genetic algorithm. After a ten-years spin up, the model reproduced well the magni-
tude of population biomasses and spawning periods of the two species in the N. Aegean
Sea. Surprisingly, model simulations revealed that anchovy depends primarily on stored
energy for egg production (mostly capital breeder) whereas sardine depends heavily on
direct food intake (income breeder). This is related to the peculiar phenology of plankton pro-
duction in the area, with mesozooplankton concentration exhibiting a sharp decrease from
early summer to autumn and a subsequent increase from winter to early summer. Monthly
changes in somatic condition of fish collected on board the commercial purse seine fleet fol-
lowed closely the simulated mesozooplankton concentration. Finally, model simulations
showed that, when both the anchovy and sardine stocks are overexploited, the mesozoo-
plankton concentration increases, which may open up ecological space for competing spe-
cies. The importance of protecting the recruit spawners was highlighted with model
simulations testing the effect of changing the timing of the existing 2.5-months closed
period. Optimum timing for fishery closure is different for anchovy and sardine because of
their opposite spawning and recruitment periods.
PLOS ONE | https://doi.org/10.1371/journal.pone.0219671 August 15, 2019 1 / 24
a1111111111
a1111111111
a1111111111
a1111111111
a1111111111
OPEN ACCESS
Citation: Gkanasos A, Somarakis S, Tsiaras K,
Kleftogiannis D, Giannoulaki M, Schismenou E, et
al. (2019) Development, application and evaluation
of a 1-D full life cycle anchovy and sardine model
for the North Aegean Sea (Eastern Mediterranean).
PLoS ONE 14(8): e0219671. https://doi.org/
10.1371/journal.pone.0219671
Editor: Jose M. Riascos, Universidad del Valle,
COLOMBIA
Received: February 13, 2019
Accepted: June 30, 2019
Published: August 15, 2019
Copyright: ©2019 Gkanasos et al. This is an open
access article distributed under the terms of the
Creative Commons Attribution License, which
permits unrestricted use, distribution, and
reproduction in any medium, provided the original
author and source are credited.
Data Availability Statement: Adult fish length and
weight data as well as acoustic data are owned the
Greek Ministry of Rural Development and Food and
are available from the Greek European Data
Collection Framework (Greek DCF). Authors
Stylianos Somarakis, Eudoxia Schismenou, and
Marianna Giannoulaki are affiliated with the Greek
DCF and have access to these data for research
purposes, but are unable to share these data due to
legal restrictions. However, interested researchers
may obtain access to these data by contacting the
Introduction
Small pelagic fishes (SPF), like anchovies and sardines, are short-lived, highly fecund, plankti-
vorous fishes that play a key role in marine food webs and are very important for fisheries and
human communities worldwide [1]. They are very sensitive to environmental changes and
extremely variable in their abundance at both inter-annual and inter-decadal scales ([2], [3]).
An effective management system for these resources would require better understanding of
the mechanisms controlling rapid variations in abundance and productivity of populations,
and the consequences that these variations may have for ecological interactions ([4], [5]).
In European waters, stocks of SPF have historically exhibited large variations in abundance
but, in contrast to the Northwest Pacific and in Eastern boundary currents, co-occurring Euro-
pean anchovy Engraulis encrasicolus and European sardine Sardina pilchardus stocks have not
exhibited large, out-of-phase fluctuations [6]. In the Mediterranean Sea, most anchovy and
sardine stocks have been declining in recent years (e.g. [7], [8]; [9], showing also decreasing
trends in maximum size and somatic condition ([10], [11]). For example, in the Gulf of Lions,
where fishing pressure on anchovy and sardine stocks is very low, the reductions in biomass,
body condition and maximum size/age have been attributed to increasing temperature and
reduced water mixing, affecting planktonic productivity ([10], [11], [12]).
The aim of the present study was to develop a multispecies (anchovy-sardine) full life cycle,
individual based model (IBM) for stocks inhabiting the N. Aegean Sea (Eastern Mediterra-
nean) (Fig 1). Full-life-cycle, bioenergetics IBMs, coupled with hydrodynamic/biogeochemical
models allow for a mechanistic understanding of how the physics, biogeochemistry, and biol-
ogy combine to result in patterns of variability in growth, egg production, recruitment and
spawning stock biomass ([6], [13], [14]).
For European anchovy, coupled bioenergetics or bioenergetics-IBMs have been successfully
implemented in the Black Sea [15], the Bay of Biscay ([16], [17]), the North Aegean Sea ([18],
[19]) and the Gulf of Lions [20]. A European sardine model has also been developed in the Bay
of Biscay [17]. These models were based on either the ‘Wisconsin’ [21] or the Dynamic Energy
Budget (DEB) [22] framework, and they were offline or, occasionally, online coupled with
regional hydrodynamic-biogeochemical models. They were generally implemented in a 1-D
configuration, thus lacking a horizontal movement module, except for a 3-D application to the
N. Aegean Sea anchovy stock [19].
1-D models lack the horizontal dimension, i.e. a movement/migration module, yet they
comprise an initial step useful for calibrating growth, egg production and/or population bio-
mass to the average thermal and trophic conditions of the ecosystem (e.g. [23], [24]). They
have also been used effectively in basin-scale or latitudinal comparisons between stocks (e.g.
[25], [26]). Finally, 1-D IBMs provide a means to test straightforwardly the outcomes of man-
agement measures (e.g. temporal fishing bans, reductions of fishing mortality), especially in
the Mediterranean Sea where the collection of spatially explicit fisheries data has only recently
been started and the utility of the collected information has often been questioned [27].
The main biological differences between anchovy and sardine in the N. Aegean Sea include
their reproductive traits (winter spawning, low daily fecundity in sardine–summer spawning,
high daily fecundity in anchovy ([28], [14]) and the generally longer life span and maximum
size of sardine [29]. On the other hand, the two stocks have many similarities, i.e., high diet
overlap, closely correlated diel feeding patterns/food consumption rates ([30], [31], [32]), and
similar diel vertical migration behavior ([33], [34]). Finally, temperature optima for growth
are almost identical for the two species, at least during the juvenile stage ([35], [36], [14]).
The Mediterranean sardine is considered to be primarily a capital breeder, i.e. it stores
energy and uses it later for egg production ([37], [38], [14]). In contrast, the Mediterranean
A 1-D full life cycle anchovy and sardine model for the North Aegean Sea
PLOS ONE | https://doi.org/10.1371/journal.pone.0219671 August 15, 2019 2 / 24
Greek Ministry of Rural Development and Food
(email: syg023@minagr.gr). Larval length data are
available from Harvard Dataverse at [https://doi.
org/10.7910/DVN/ISDZOE].
Funding: The present work was financially
supported by the General Secretariat for Research
and Technology (GSRT) and the Hellenic
Foundation for Research and Innovation (HFRI)
through the project CLIMAFISH ‘CLIMAte change
and FISHeries impacts on small pelagic fish:
dynamic, spatially explicit models in the service of
the ecosystem-based fisheries management’ within
the framework of the “1st Call for the support of
Postdoctoral Researchers."
Competing interests: The authors have declared
that no competing interests exist.
anchovy is thought to be more close to the income breeding pattern, i.e. egg production is
mainly fueled by direct food intake during the spawning period ([39], [14]). Breeding pattern
has consequences for recruitment [14] and coupled bioenergetics models provide capability
for directly assessing it, by linking energy acquisition and allocation to egg production to the
seasonal cycle of food production (zooplankton) as simulated by the biogeochemical model
[17].
The IBM model for anchovy and sardine presented in this paper was based on an existing
model for anchovy in the N. Aegean Sea [19]. We have built a new energy allocation/egg pro-
duction algorithm that allows for breeding pattern to move along the capital-income contin-
uum (sensu [17]). Fish growth was calibrated against available size-at-age field data using a
genetic algorithm. Finally, the model was used to test the outcomes of different management
measures, such as changes in the exploitation rate of the stocks as well as shifts in the timing of
an existing fishery ban (closed period for the purse seine fishery: 15 Dec–Feb, [40]).
Materials and methods
Low trophic level model
The fish model is on-line, two-way coupled with a 1-D (water column) lower trophic level
model (LTL) implemented in the Thracian Sea (Fig 1). The Thracian Sea is one of the major
habitats of anchovy and sardine in the Aegean Sea ([41], [42], [43]).
The LTL provides the prey fields (zooplankton) and temperature conditions to the fish
model (Fig 2) and consists of a hydrodynamic model, based on POM (Princeton Ocean
Fig 1. Map of the North Aegean Sea showing the model domain. The box indicates the location of Thracian Sea.
https://doi.org/10.1371/journal.pone.0219671.g001
A 1-D full life cycle anchovy and sardine model for the North Aegean Sea
PLOS ONE | https://doi.org/10.1371/journal.pone.0219671 August 15, 2019 3 / 24
Model; [44]) and a biogeochemical model, based on the European Regional Seas Ecosystem
Model (ERSEM, [45]). It has already been implemented in the Cretan Sea [46], the North
Aegean Sea ([47], [48]), as well as the entire Mediterranean Sea, as part of the POSEIDON
forecasting system (www.poseidon.hcmr.gr). The ERSEM follows the functional group
approach, with organisms being classified according to their trophic role (producers, consum-
ers, etc.) and size. It describes the planktonic food web with four groups of primary producers
(picophytoplankton, nanophytoplankton, diatoms, dinoflagellates), bacteria, and three zoo-
plankton groups (heterotrophic nanoflagellates, microzooplankton, mesozooplankton), as well
as the particulate and dissolved organic matter pools. Carbon dynamics are coupled with
nitrogen (nitrate, ammonium), phosphorus (phosphate) and silicate cycles, with all plankton
groups having dynamically varying C:N:P:Si pools.
The biogeochemical model is forced by temperature and daily vertical diffusivity profiles,
averaged for the 2003–2008 period, over the Thracian Sea. These were obtained off-line from a
3-D simulation of the hydrodynamic model [48]. Given that the coupling with hydrodynamics
is only one-way, using the full 3-D hydrodynamic output was preferable. A 1-D hydrodynamic
model does not resolve horizontal processes and has important limitations in this area where
lateral water inputs (Black Sea Water, rivers etc) are very important. Water column properties
(temperature, salinity) are therefore not realistically simulated with a 1-D hydrodynamic
model. A monthly varying input of dissolved inorganic nutrients (phosphate, nitrate, ammo-
nium, silicate) was adopted at the surface layer to mimic river/Black Sea Water (BSW) nutrient
inputs in the Thracian Sea. This nutrient input follows the seasonal variability of riverine/BSW
inputs, peaking during spring and is tuned so that the simulated plankton productivity (Chl-a,
zooplankton) is similar to the one simulated with the 3-D version of the biogeochemical
model [48].
Fish model
The fish model is a full-life cycle, individual based model (IBM) and includes two species, the
European anchovy (Engraulis encrasicolus) and the European sardine (Sardina pilchardus). It
was based on the anchovy model developed by Politikos [19]. The sardine IBM was built from
the existing anchovy model by progressively integrating traits that are known to differ between
the two species (Table 1).
The model describes the life cycle of both species, from the egg to the adult stage. The life
span is divided into seven stages/age classes for anchovy (embryo, early larva, late larva, juve-
nile, adult age-1 to age-3) and eight stages for sardine (with an additional adult age class: adult
age-1 to age-4) (Table 1). The number of age classes was defined based on otolith age readings
made on samples collected in the field ([42], see below).
Although this version of the multispecies model is 1-D, i.e. it lacks a horizontal movement
algorithm, it includes all other modules described in [19], namely a bioenergetics, a diel verti-
cal migration (DVM) and a population module. The populations of the two species are repre-
sented by a fixed number of super-individuals (SIs) [54], in each stage/age-class. Each SI
consists of individuals that share the same attributes (length, weight, age etc.). During a spawn-
ing event, a new (egg) SI is created. For computational efficiency, the maximum number of SIs
per stage is maintained constant throughout the simulations. It is higher (150 SIs) for the early
life stages (embryos, early and late larvae) and lower for the juvenile stage and adult age classes
(10 SIs). A higher number of SIs was necessary for the egg and larval stages in order to resolve
adequately the dynamics of these stages during the prolonged spawning periods of the two
species.
A 1-D full life cycle anchovy and sardine model for the North Aegean Sea
PLOS ONE | https://doi.org/10.1371/journal.pone.0219671 August 15, 2019 4 / 24
Fish growth is calculated with a Wisconsin-type bioenergetics model taking into account all
important physiological processes, i.e. consumption, respiration, egestion, specific dynamic
action, excretion and reproduction (Table 2). A piece-wise length-weight relationship is used
to convert weight to length (see [18] for details).
As already mentioned, the fish model is on-line coupled with the LTL model (Fig 2). Early
larvae feed on microzooplankton, late larvae consume micro- and mesozooplankton and
Fig 2. Representation of the anchovy and sardine model coupled with the lower trophic level (LTL) model.
https://doi.org/10.1371/journal.pone.0219671.g002
Table 1. Main differences and similarities in model parameters between anchovy and sardine.
Parameter Anchovy Sardine
Length range (mm), [49] Early larvae 4–11 5–13
Late larvae 11–42 13–50
Juvenile 42–100 50–105
Length at maturity (L
m,
mm), [49] 100 105
Egg energy, [17] 0.66 1.11
Daily specific fecundity (eggs g
-1
), [42], [28] 46 20.1
Batch Energy (g prey per g fish per day) 0.012 0.0086
Spawning period SST threshold, [50], [51] SST >15˚C SST <16˚C
Natural mortalities, [19], [52], [53] The natural mortality of
juveniles was calibrated (see text for details).
0.4, embryos
0.2, early larvae
0.05, late larvae
0.012, juveniles
0.002, adults
Fishing mortalities, [19], [52], [53] 0.00136, adults 0.002, adults
Reference biomass (t), [19], [52], [53] 40000 25000
https://doi.org/10.1371/journal.pone.0219671.t001
A 1-D full life cycle anchovy and sardine model for the North Aegean Sea
PLOS ONE | https://doi.org/10.1371/journal.pone.0219671 August 15, 2019 5 / 24
juveniles/adults interact only with the mesozooplankton compartment of the ERSEM. The
plankton biomass (micro- and mesozooplankton) that is consumed by the fish is removed in
ERSEM, while fish bio-products from egestion, excretion and specific dynamic action are
directed to the ERSEM particulate organic matter and dissolved inorganic nutrient pools. The
individuals that each SI represents are assumed to have a vertical distribution (position in the
water column) that is maximized around the depth of peak prey availability. Eggs and early lar-
vae are distributed in the surface layer (0-30m), while late larvae, juveniles and adults perform
diel vertical migrations between the surface (0-30m, night) and the sub-surface (>30m, day).
In order to predict the duration of the embryonic stages (egg+yolk sac larva), which are tem-
perature dependent, we use the equations developed by [17].
Table 2. Equations and parameters of the bioenergetics model.
Energy Process Equations Parameters Anchovy Parameters Sardine
Somatic growth 1
WSI dWSI
dt ¼C ðRþEG þSDA þEX þEbufferÞ
h iCALz
CALf
W
SI
= fish wet weight (g), t = time (days), C = consumption, R = respiration,
EG = egestion, SDA = specific dynamic action, EX = excretion, E
buffer
= the
energy allocated to reproduction, CAL
z
= caloric equivalent of zooplankton,
CAL
f
= caloric equivalent of fish
Maximum
Consumption
(C
max
)
Cmax ¼acWbC
SI fCðTÞ,f
C
(T) = V
X
e
X(1V)
, a
c
= Intercept for consumption, b
c
=
Exponent for consumption
a
c
= 0.41, b
c
= 0.31
Temperature
function
V¼TmaxT
TmaxTopt ;S= (lnQ
c
)(T
max
T
opt
), Y= (lnQ
c
)(T
max
T
opt
+2),
X¼S2ð1þð1þ40=YÞ1=22
400 , Q
c
= Slope for temperature dependence, T
opt
= Optimum
Temperature (
o
C), T
max
= Maximum Temperature (
o
C)
Q
c
= 2.22
a,b
, 2.4
c,d
, T
opt
=
17.25
a
,16.25
b
,15.8
c,d
, T
max
= 27
T
opt
= 14.5
a
,14.75
b
,15.8
c,d
Consumption
(C) Ci ¼P2
i¼1Cj;i;Cj;i¼CmaxðPDj;ivj;i
kj;iÞ
1þP2
i¼1ðPDk;ivk;i
kk;iÞ, PD
j,i
= density of prey type i (i = 1
corresponds to microzooplankton and i = 2 to mesozooplankton) (g-prey
m
-3
) for life stage/age class j, v
j,i
= vulnerability of prey type i to life stage/age
class j (dimensionless), k
j,i
half saturation function (g-prey m
-3
) for life stage j
feeding on prey type i.
v
2,1
= 1.0, v
3,1
= 0.5, v
4,1
= v
5,1
= v
6,1
=
v
7,1
= 0, v
2,2
= 0.0, v
3,2
= 0.5, v
4,2
= v
5,2
=
v
6,2
= v
7,2
= 1.0
Respiration (R) R¼arWbr
SI fRTð ÞA;fRTð Þ ¼ Q
TTm
10
10 ;A¼edrU;U¼aAWbAeðCATÞ, a
r
= Intercept
for respiration, b
r
= Exponent for respiration, Q
10
= Temperature dependence
parameter, T
m
= Mean annual temperature, d
r
= Coefficient for R for
swimming speed, a
A
= Intercept U (<12.0
o
C), a
A
= Intercept U (12.0
o
C),
a
A
= Intercept U (12.0
o
C), (during low feeding activity), b
A
= Coefficient U
for weight, c
A
= Coefficient U vs. temperature (<12.0
o
C), c
A
= Coefficient U
vs. temperature (12:0
o
C)
a
r
= 0.003, b
r
= 0.34, Q
10
= 1.3, T
m
=
16
a,b,c,d
, d
r
= 0.022, a
A
= 2.0 (U<
12.0
o
C), a
A
= 12.25
a,b
, 11.98
c
, 14.21
d
(U12.0
o
C), a
A
= 9.97
c
(U12.0
o
C),
(during low feeding activity), b
A
=
0.27
a,b
, 0.33
c
, 0.27
d
, c
A
= 0.149
(U<12.0
o
C), c
A
= 0.0 (U12:0
o
C)
Egestion (EG) F=a
f
C, a
f
= Proportion of food egested a
f
= 0.15
a,b
, 0.126
c,d
Excretion (EX) E=a
e
(CF)+b
e
, a
e
= Excretion coefficient, b
e
= Proportion of food excreted a
e
= 0.41, b
e
= 0.01
Specific
Dynamic Action
(SDA)
SDA =a
sda
(CF), a
sda
= Specific dynamic action coefficient a
sda
= 0.10
Length-weight
relationship
y = b
o
+b
1
x+b
2
(x-d
1
)(x>d
1
)+b
3
(x-d
2
)(x>d
2
), y, x (log-transformed fish wet
weight and length), b
o
= y-intercept, b
1
= slope of the function for the larval
stage, b
2
= slope change for the juvenile stage, d
1
= slope change inflexion
point, b
3
= subsequent slope change for the adult stage, d
2
= corresponding
length for this slope respectively
b
o
= -6.1158, b
1
= 3.5764, b
2
= -0.616, d
1
= 1.5798, b
3
= 0.7137, d
2
= 1.954
b
o
= -9.229, b
1
= 5.391,
b
2
= -2.281, d
1
= 1.699,
b
3
= 0.106, d
2
= 2.02
a
Early larval stage (j = 2).
b
Late larval stage (j = 3).
c
Juvenile stage (j = 4).
d
Adult age-classes (j = 5,6,7 & 8 for sardine).
https://doi.org/10.1371/journal.pone.0219671.t002
A 1-D full life cycle anchovy and sardine model for the North Aegean Sea
PLOS ONE | https://doi.org/10.1371/journal.pone.0219671 August 15, 2019 6 / 24
The number of individuals in each SI is computed by taking into account the natural and
fishing mortality. Specifically, at each time step, the number of individuals within each SI (N)
is reduced using the equation:
dN
dt ¼ MþFð Þ N
where Mis the assigned natural mortality and Fis the fishing mortality rate, applied only to
adult SIs (see Table 1).
For the embryonic and larval stages, the adopted M values for anchovy were based on pub-
lished estimates ([41]; [55]; [42]). In the case of European sardine, literature information was
very limited. The few existing values for egg and early larval mortality, estimated for the Ibe-
rian sardine in the Atlantic ([56], [57]) were very similar to the values adopted for the Mediter-
ranean anchovy. We therefore used the same values of natural mortality for the early life stages
of the two species (Table 1).
The natural mortality during the juvenile stage is largely unknown. Yet, mortality during
the juvenile stage has a great impact on subsequent population biomass due to the stage’s long
duration. The natural mortality rate of juveniles was therefore calibrated, so as the simulated
anchovy and sardine populations to fluctuate around 40000 t and 25000 t respectively, which
are approximate mean biomasses of the two species in the N. Aegean Sea (based on acoustic
data biomass estimations for the period 2003–2008 ([52], [53], Table 1). The mean natural and
fishing mortalities of adults were adopted from the aforementioned stock assessment papers
(Table 1). Except from natural and fishing mortalities, additional starvation mortality is
imposed for all stages (i.e., the SI vanishes) in case that the cumulative weight loss exceeds
35%. This 35% threshold was defined empirically based on residual variation of existing
length-weight relationships (see [19] for details).
Spawning is regulated by an energy allocation/egg production algorithm, embedded in the
bioenergetics equation (Fig 3). This algorithm is different from the one described in [19]. The
latter assumed an extreme income breeding mode for the Mediterranean anchovy. The new
algorithm (Fig 3) is now allowing for breeding pattern to move along the capital-income con-
tinuum [38]. A similar approach was followed in [17]. Briefly, the energy available from con-
sumption is first used to satisfy the needs of maintenance (M) that accounts for respiration,
egestion, specific dynamic action, excretion. The remainder energy (A) is then channeled to
only growth (increase in weight), if fish is smaller than length at maturity (L
m
). This is justified
from measurements in European sardine showing that, in juvenile fish, growth is prioritized
and immature fish do not store fat [58]. If fish is larger than L
m
, the surplus energy (A) is chan-
neled to both growth and reproduction. Energy allocated to reproduction is stored, all year
round, in the so-called ‘reproductive buffer’ [16]. The amount of A allocated to reproduction
is (1-k)A. The parameter k is largely unknown and therefore assumed to be k = 0.5 in both
species. If A<0, energy already in the reproductive buffer (first) and fish soma (secondly) goes
to maintenance (to meet daily maintenance costs) (Fig 3). Regarding spawning, each SI
releases an egg batch (egg SI) on a daily basis, if a (species specific) SST criterion is satisfied,
fish length is larger than L
m
and energy stored in the buffer (E
buffer
) is sufficient for producing
the egg batch.
The number of eggs released (the population of the egg SI) is equal to the product of daily
specific fecundity (DSF, number of eggs per gram of the adult SI) and the SI’s weight. Different
values of DSF were adopted for anchovy and sardine, based on published literature ([42],
[28]). The batch energy (E
egg
) is calculated from DSF and egg energy. We used the values of
anchovy and sardine egg energy calculated in [17] (Table 1).
A 1-D full life cycle anchovy and sardine model for the North Aegean Sea
PLOS ONE | https://doi.org/10.1371/journal.pone.0219671 August 15, 2019 7 / 24
Based on the fact that the two species have different spawning periods in the Mediterranean
Sea, with anchovy spawning from spring to autumn and sardine from autumn to spring [14],
anchovy is set to spawn when sea surface temperature (SST) is above 15˚C [50] while sardine
spawns only if SST <16˚C [51]. Given the different spawning periods, we also adopted differ-
ent optimum temperatures for larval consumption ([6], Table 2). These were selected so as to
lay close to the actual average temperatures that larvae experience. Apart from SST, an addi-
tional criterion (not shown in Fig 3) was also applied to define the end of the spawning period.
It is known that, in the lack of food, fish stop releasing eggs and start to absorb their gonads (a
process known as atresia). If food shortage is prolonged (8–9 days in Northern anchovy) the
spawning period of the fish comes to an end [59]. We therefore assumed that if food consump-
tion is insufficient to meet metabolic requirements for 9 consecutive days the SI stops releasing
eggs for that particular spawning season.
Field data for the construction and calibration of the fish model included length-weight
measurements and length/weight-at-age estimates. For anchovy, these data are described in
[18], [19] and [26]. For sardine, we used data available from [49] and [36] for larvae and
Fig 3. Schematic illustration of the energy allocation and egg production algorithm. SST: Sea surface temperature. L
m
: length at maturity. E
buffer
: energy in
reproduction buffer. E
egg
: batch energy.
https://doi.org/10.1371/journal.pone.0219671.g003
A 1-D full life cycle anchovy and sardine model for the North Aegean Sea
PLOS ONE | https://doi.org/10.1371/journal.pone.0219671 August 15, 2019 8 / 24
juveniles, and data from the acoustic and daily egg production surveys carried out in the N.
Aegean Sea from 2003 to 2008 [42].
Additionally, we studied the monthly variation of the somatic condition of two species
using length-weight measurements made on fish collected from the commercial purse seine
fleet from 2003 to 2008 (S1 File). No samples were available for January and February, which is
a closed period for the purse seine fishery [40]. Size-adjusted monthly mean weights were esti-
mated for each species using a general linear model approach (S1 File). The rationale for study-
ing the monthly variation of fish condition (which reflects energy storage [see [11] and
references therein] was to compare its changes with model predictions for the seasonal zoo-
plankton cycle and fish breeding patterns (income-capital).
For this purpose, a ‘capital index’ similar to the one developed in [17] was computed for
each age class:
ðdEbuffer X
e
s
ARÞ=X
e
s
Eegg
It corresponds to the quotient of the division between the energetic loss from the reproductive
buffer between the start (s) and the end (e) of the spawning season (after the subtraction of the
cumulative emergency maintenance costs paid from the reproductive buffer, as described in
Fig 3) and the cumulative energy spent for egg production during the spawning season. The
higher is the capital index, the closer is the species to the capital breeding pattern, i.e. it is more
dependent on stored energy for the production of eggs.
Calibration of the bioenergetics model
The bioenergetics module was calibrated against the available length- and weight-at-age field
data by applying a heuristic optimization technique based on a genetic algorithm (GA). GAs
are inspired from the principles of natural selection and they are effective when dealing with
large and complicated search spaces or when there is no other analytical solution for the prob-
lem. GAs are often characterized as population based evolutionary processes, starting with a
population of candidate solutions (called chromosomes) that are evolved in time via a number
of cycles (called generations) and genetic operations (i.e., crossover and mutation) towards a
specific goal that is described by a problem-specific optimization function (called fitness func-
tion). Chromosomes consist of genes, which in our application are the model parameters to be
tuned. For every generation, the fitness function is evaluated for every chromosome estimating
in this way the quality of the candidate solution (e.g., highest score indicates better solution).
While passing from one generation to another, solutions that achieve the highest score are
selected to survive. The process is continued until some termination criteria are fulfilled or a
user-defined number of generations is reached [60]. Here, for simplicity and in order to
achieve reproducibility of our results, we deployed a simple genetic algorithm adopted by the
implementation described in [61].
Since the objective was to tune the model and achieve average weights-at-age for each spe-
cies as close as possible to field data, we introduced a simple fitness function:
Fitness ¼1=ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi
Xðprediction referenceÞ2
q
This fitness function takes into account the Euclidean distance between weight data and the
predicted weight of the species for one or more predefined dates. Thus, given two weight out-
puts for a specific age, derived from different model runs using different parameter values, the
higher ranked output is the one that has smaller distance with respect to the reference weight.
A 1-D full life cycle anchovy and sardine model for the North Aegean Sea
PLOS ONE | https://doi.org/10.1371/journal.pone.0219671 August 15, 2019 9 / 24
Regarding the termination criteria, we set a maximum number of generations equal to
1000. To reduce the execution time, the algorithm is equipped with an additional stopping cri-
terion, which considers the population as converged (i.e., steady-state) if there is no difference
in the average fitness value of the population for 150 consecutive generations.
The genetic algorithm was applied to the stage-/age-specific half saturation coefficients (see
equation for consumption in Table 2) that regulate food consumption [26]. For this purpose,
we used an IBM version that included only one super-individual from each species. By experi-
menting with the GA setup, we compared a simultaneous parameter tuning (all stage-/age-spe-
cific half saturation coefficients) to a sequential parameters tuning. The later involved the
tuning of the half saturation constant first for the larvae, then for the juveniles etc. until the ter-
minal adult age class. The sequential tuning approach proved more successful in predicting
the available growth data.
Model simulations setup and testing of management measures
The anchovy-sardine IBM, with a time-step 1200 sec, was run for a 30 year period in order to
evaluate its performance in terms of population and reproductive characteristics of the two
species in the North Aegean Sea. The first ten years were considered as model spin up. Hence,
only the remaining period (11–30 years) was taken into account for model evaluation and
analysis.
Subsequently, we used the model to test the sensitivity of the anchovy and sardine popula-
tions to (a) changes in fishery exploitation rates, and (b) changes in the timing of the existing
2.5 months closure period.
In the first set of simulations, we examined the effect of changing the levels of fishing
mortality on the populations of anchovy and sardine as well as on their mesozooplankton
prey. The fishing mortality of each species was allowed to vary, so that the Paterson’s exploi-
tation rate (E.R. = fishing mortality/[natural mortality + fishing mortality]) fluctuated
around 0.4 (0.23 to 0.51 and 0.32 to 0.46 for anchovy and sardine respectively). The value of
0.4 (as empirically defined by [62]), is currently considered as the exploitation rate corre-
sponding to the maximum sustainable yield for the Mediterranean small pelagic fish stocks
[63] and is a reference point for their management, i.e. stocks exploited above 0.4 are con-
sidered overexploited.
In the second set of simulations, we examined the effect of changing the timing of the exist-
ing 2.5 months purse-seine fishery ban, now scheduled between 15 December and end of Feb-
ruary, by shifting it by one month along the year, i.e. 15 January-March, 15 February-April etc.
Results
The seasonal variability of the water column temperature and mesozooplankton concentration
is shown in Fig 4, highlighting the development of a strong thermal stratification during sum-
mer, coupled with the formation of a deep mesozooplankton maximum (corresponding to the
deep chlorophyll maximum). The simulated mesozooplankton concentration is comparable
with that of the 3-D model output [48] that has been validated against in situ data [64].
Starting from the onset of the mixing period in winter, the mean mesozooplankton concen-
tration exhibits an increasing trend that lasts till early summer (Fig 5). Thereafter, it decreases
sharply and remains low until mid-December. The mean monthly somatic condition of
anchovy and sardine in the Thracian Sea (estimated from the field samples, S1 File) appears to
follow closely the seasonal variability of the simulated mesozooplankton concentration (Fig 5).
Although no samples were available in the January-February period to estimate somatic condi-
tion, results showed that the latter increased from December to spring in both species (more
A 1-D full life cycle anchovy and sardine model for the North Aegean Sea
PLOS ONE | https://doi.org/10.1371/journal.pone.0219671 August 15, 2019 10 / 24
sharply in anchovy with the summer spawning period, more slowly in the winter spawning
sardine). Interestingly, somatic condition starts to decrease sharply after July, i.e. approxi-
mately one month after the strong decrease in the simulated mesozooplankton concentration.
Fig 4. Seasonal evolution of temperature and simulated mesozooplankton concentration.
https://doi.org/10.1371/journal.pone.0219671.g004
A 1-D full life cycle anchovy and sardine model for the North Aegean Sea
PLOS ONE | https://doi.org/10.1371/journal.pone.0219671 August 15, 2019 11 / 24
The application of the genetic algorithm to tune the half saturation coefficients resulted in
growth trajectories that were in close agreement with available lengths- and weights-at-age
data from field samples, in both larvae (Fig 6) and adults (Fig 7).
Finally, after the 10-years spin-up period, the modelled biomasses of the anchovy and sar-
dine populations fluctuated around 40000 t and 25000 t respectively, i.e. the adopted reference
biomass values (Fig 8).
Model outputs regarding the spawning period and daily egg production of the two species
were in agreement with known patterns (Fig 9): Anchovy starts spawning in late April and its
population continues to release eggs up to late September, but with decreasing numbers, espe-
cially after early summer, when SST reaches high values (Fig 4) and the mesozooplankton con-
centration decreases (Fig 5). No obvious difference in spawning timing/duration was observed
between recruit (age-1) and repeat spawners (age 2+) (Fig 9). In sardine, spawning starts in
November and lasts until the end of April, i.e. spawning mainly coincides with the period of
Fig 5. Top panel: Simulated average mesozooplankton concentration (mgC m
-3
) in the water column (0-100m)
against calendar day. Bottom panel: length-adjusted monthly mean weight (somatic condition) of fish samples
collected onboard the Thracian Sea purse seine fleet in 2003–2008.
https://doi.org/10.1371/journal.pone.0219671.g005
A 1-D full life cycle anchovy and sardine model for the North Aegean Sea
PLOS ONE | https://doi.org/10.1371/journal.pone.0219671 August 15, 2019 12 / 24
increase in mesozooplankton concentration (Fig 5). The model also predicts that, in sardine,
recruit spawners have a delayed and shorter spawning period than the repeat spawners.
In contrast to expectations [14], the mean values of the ‘capital index’ are much higher in
anchovy than in sardine (Table 3). This implies that the sardine in the North Aegean Sea
derives most energy for egg production from direct food intake rather than energy stored
prior to the spawning period. Indeed, the field estimates of mean monthly condition (Fig 5)
indicated that sardine has the lowest somatic weight in autumn prior to the start of its winter
spawning season.
Changes in fishery exploitation rates
Changing the fishing mortality imposed on the two species, so as to vary the Patterson’s exploi-
tation rate above and below the 0.4 reference point (Fig 10), showed that the biomass of each
individual species is relatively insensitive to changes in the exploitation rate of the other species
and concomitant changes of its biomass. However, an obvious effect of the combined fishing
rates on the two species could be seen on mesozooplankton, which is the fish prey. Sustainable
exploitation of both species (E.R. <0.4) results in the decrease of mesozooplankton availability
and overexploitation (E.R.>0.4) leads to the increase of mesozooplankton concentration.
Changes in the timing of the fishery closure period
Shifting the timing of the fishery ban affects the biomass of both species (Fig 11); however suit-
able timing (i.e., leading to the increase in average biomass) differs between anchovy (spring)
and sardine (autumn). In both species, the most favorable closure period is the period of (and
around) peak recruitment, as evidenced by the decline of mean fish weight in the population
(Fig 11, lower panel). When protecting the recruiting fish prior and/or during the initial phase
Fig 6. Mean length-at-age (±SD) of anchovy and sardine larvae, calibrated using the genetic algorithm and field data ([49], [65], [36]).
https://doi.org/10.1371/journal.pone.0219671.g006
A 1-D full life cycle anchovy and sardine model for the North Aegean Sea
PLOS ONE | https://doi.org/10.1371/journal.pone.0219671 August 15, 2019 13 / 24
of their first spawning period population biomass is positively affected, clearly owing to the
increased annual population fecundity (Fig 11, middle panel). In other words, due to the
numerical dominance of recruit spawners in the population (>70% in both species, not
shown), allowing a higher number of them to spawn results in the increase of egg production
and the subsequent increase of population biomass.
Discussion
The full life cycle IBM model developed and evaluated in this paper describes the population
dynamics of two species, using a water column model. It can easily be extended to a model
that includes more pelagic species (e.g. forage species, predators) and intraguild predation
Fig 7. Evolution of mean weight and mean length of fish, calibrated using the genetic algorithm and mean weight- and length-at-age of adult fish (±SD)
estimated from samples collected during the acoustic and egg production surveys in the North Aegean Sea, 2003–2008 [42].
https://doi.org/10.1371/journal.pone.0219671.g007
A 1-D full life cycle anchovy and sardine model for the North Aegean Sea
PLOS ONE | https://doi.org/10.1371/journal.pone.0219671 August 15, 2019 14 / 24
(predation on the eggs of the competing species). Furthermore, with the addition of a move-
ment-migration module, it can become a 3-D fully coupled model, allowing for the direct link-
ing of growth, mortality, movement and spawning processes to the detailed spatial and
temporal scales of the hydrodynamic/biogeochemical model (e.g. [13]).
With the exemption of such spatial dimension, our model includes all other processes nec-
essary to simulate growth, egg production and population dynamics and it is two-way coupled
with the LTL model. It should be noted here that, in non-upwelling systems like the North
Aegean Sea, in which a strong vertical heterogeneity in temperature and zooplankton develops
during the thermally stratified period (e.g. Fig 4), it is important to incorporate a diel vertical
migration (DVM) behavior in the fish model because temperature and food availability, and
consequently consumption and metabolic rates, will change between day and night. In our
region anchovy and sardine have a very similar DVM with fish moving above the thermocline
during the night and below it, during the day ([33], [34]). The simple vertical migration algo-
rithm developed in [19] and also used here, accounts for the consequences of DVM behavior
on consumption and respiration due to thermal stratification and the formation of deep chlo-
rophyll/zooplankton maxima.
Fig 8. Model-simulated anchovy and sardine biomass. The mean biomasses of the two species in the N. Aegean Sea (based on acoustic data biomass estimations for
the period 2003–2008) are also shown.
https://doi.org/10.1371/journal.pone.0219671.g008
A 1-D full life cycle anchovy and sardine model for the North Aegean Sea
PLOS ONE | https://doi.org/10.1371/journal.pone.0219671 August 15, 2019 15 / 24
In developing the model for sardine we started with the already existing parameterization
for anchovy ([18], [19]), changing only those parameters that are known to differ between the
two species, i.e. the length-weight relationships, the length ranges of early life stages and num-
ber of age classes, but most importantly, their reproductive characteristics, i.e. spawning
period, fecundity and egg size. The genetic algorithm applied to tune the bioenergetics model
resulted in simulating growth trajectories that were very close to size-at-age data from the
field.
Genetic algorithms have previously been applied by [66] and [67] for tuning the weights of
an artificial neural network used for habitat choice, energy allocation and spawning strategy/
spawning migration, respectively. In our study, tuning the bioenergetics model involved the
adjustment of the half saturation parameters so that the simulated fish growth matched the
mean size-at-age data estimated from field samples. This computationally demanding process
was effectively tackled by a heuristic optimization technique based on a genetic algorithm. The
deployed algorithm minimizes the execution time and produces solutions close to optimal (i.e.
Fig 9. Model-simulated daily egg production (total number of eggs produced by the population) for recruit (age 1) and repeat spawners (age 2+). The seasonal
evolution of sea surface temperature (SST) is also shown.
https://doi.org/10.1371/journal.pone.0219671.g009
Table 3. Mean value of the capital index per age class.
Age 1 Age 2 Age 3 Age 4
Anchovy 0.47 0.71 0.75 -
Sardine 0.006 0.28 0.34 0.09
https://doi.org/10.1371/journal.pone.0219671.t003
A 1-D full life cycle anchovy and sardine model for the North Aegean Sea
PLOS ONE | https://doi.org/10.1371/journal.pone.0219671 August 15, 2019 16 / 24
if not the overall best from all feasible solutions, it finds one very close to the best). Our experi-
mentation showed that the best tuning is achieved, when applying the process sequentially
from the younger to older stage/age rather than when concurrently considering all stages/ages,
which can be attributed to the dependence of each life stage on previous growth history. The
Fig 10. Biomass of anchovy and sardine and mean mesozooplankton concentration for different combinations of
exploitation rate (E.R.) of the two species. E.R. = 0.4 is the reference point (maximum sustainable yield proxy)
currently used in the management of small pelagic fish stocks in the Mediterranean Sea.
https://doi.org/10.1371/journal.pone.0219671.g010
A 1-D full life cycle anchovy and sardine model for the North Aegean Sea
PLOS ONE | https://doi.org/10.1371/journal.pone.0219671 August 15, 2019 17 / 24
deployed method was very effective and accurate and depending on available hardware, it
could be applied to tune more fish processes such as population parameters and temperature
dependence.
When calibrating parameters such as the half saturation constants one assumes that food
consumption is adapted to local prey availability [26]. Given the similarity of the two species in
the North Aegean Sea, e.g. the similar lengths-/weights-at-age (Fig 7), as well as the lack of
information on how temperature affects their energetic rates, we adopted the same parameteri-
zation for temperature dependences, except for the optimum temperatures for food consump-
tion, which were stage specific and were assumed to be close to the average temperature of the
larval, juvenile and adult habitats [6]. In this logic, the major difference between the two spe-
cies was that the optimum temperature for consumption was lower in sardine larvae (that
grow in winter-spring) and higher for anchovy larvae (that grow in summer). This is some-
what consistent with the ‘optimal growth temperature hypothesis’: [68] demonstrated that the
larvae of anchovy and sardine have different temperature optima for growth in the NW Pacific,
Fig 11. Mean anchovy and sardine biomass (upper panel) and annual population fecundity (middle panel) in relation to the timing of the
2.5 months fishing ban. Months 1, 2, 3,. . . etc correspond to closed period 15 Jan-Mar, 15 Feb-Apr, 15 Mar-May, ...etc. The mean weight of
individuals during the respective closed period is also plotted (lower panel).
https://doi.org/10.1371/journal.pone.0219671.g011
A 1-D full life cycle anchovy and sardine model for the North Aegean Sea
PLOS ONE | https://doi.org/10.1371/journal.pone.0219671 August 15, 2019 18 / 24
which might be an explanation for the anchovy and sardine population alternations in this
region.
Field data on somatic condition showed that both anchovy and sardine increase their
energy reserves from winter to early summer, when the simulated mesozooplankton concen-
tration is also increasing (Fig 5). However, from mid-summer onwards, somatic condition
declines sharply, lagging the modelled mesozooplankton decline by approximately one month.
This finding was unexpected. Several other sardine stocks have been shown to increase their
condition all along the summer months, exhibiting maximum condition and lipid storage
prior to the onset of gonadal maturation in autumn ([28], [14], and references therein). These
sardine stocks are mostly capital breeders using primarily stored energy to produce eggs [14].
In contrast, both the observed seasonal variation of somatic condition and the calculation of
the capital index from the model simulation suggest that the sardine stock in the North Aegean
Sea is closer to the income breeding mode. On the contrary, anchovy, which starts to spawn in
a period of increased zooplankton concentration and continues to release eggs in the subse-
quent period of maximal surface temperatures/sharply decreasing food availability, is primar-
ily a capital breeder. This can be attributed to the peculiar pelagic production cycle and
stressful summer temperatures in the oligotrophic Aegean Sea, where the first half of the year
(winter-spring) is the period of increasing zooplankton concentration, in contrast to other
ecosystems like those inhabited by the Atlantic anchovy and sardine stocks in which the zoo-
plankton concentration is high in spring-summer and very low in the autumn-winter period
[26]. Indeed, in the Bay of Biscay, European anchovy is primarily income whereas European
sardine, capital breeder [17]. The indications that the North Aegean Sea anchovy is mostly cap-
ital breeder contradict an earlier suggestion, based on data from the early 90’s, that it is income
breeder [39]. Recent papers suggest that the period of maximal SPF energy storage in the Med-
iterranean has changed in recent years (from autumn to early summer) probably reflecting a
change in the phenology of plankton production ([10], [11]). As shown by the modelling study
of [17], and supported by a review paper on fish breeding patterns [38], the capital-income
mode can be plastic in many species; fish can move along the capital-income breeding contin-
uum, in response to their physiological condition and the match-mismatch between the pro-
duction of food and the production of eggs.
The energy allocation and reproduction algorithm developed in this study resulted in
spawning periods that were consistent with observed spawning periods of the two species in
the Eastern Mediterranean ([37], [14]). In sardine that spawns in the period of increasing zoo-
plankton concentration both the onset and the end of the spawning period is determined by
its SST threshold, whereas in anchovy the SST threshold triggers only the onset of the spawn-
ing period. The end of spawning simply results from the exhaustion of reserves from the repro-
ductive buffer and energy intake insufficient to meet the needs of maintenance towards the
end of summer. It should be noted here that because the model is 1-D, temperature or other
thresholds imposed concurrently to all SIs result in the abrupt starting and ending of spawning
periods. However, in a 3-D extension of such model, the population egg production is
expected to increase and decrease more smoothly due to the spatial heterogeneity in tempera-
ture and food (e.g. [19]). The simulated egg production highlighted that sardine age-1 (recruit
spawners) start to spawn later than repeat spawners (age 2+) and have a shorter spawning
period. This is well documented for sardine in the Eastern Mediterranean [37] and elsewhere
([28] and references therein), but has never been reported for anchovy in the Eastern Mediter-
ranean, nor resulted from the model simulations. This difference can be explained from the
contrasted trophic conditions that anchovy and sardine experience before the onset of their
first spawning period, i.e. high food concentration in spring vs low in autumn and the
A 1-D full life cycle anchovy and sardine model for the North Aegean Sea
PLOS ONE | https://doi.org/10.1371/journal.pone.0219671 August 15, 2019 19 / 24
subsequent delay in reaching the size at maturity and acquiring energy for reproduction in sar-
dine, but not in anchovy.
The current application assumes that the fraction of energy allocated to reproduction is
equal to the fraction allocated to growth. This choice was considered reasonable given the lack
of information on energy allocation. Furthermore, there is some evidence that the fraction k is
plastic: Tank experiments in Japanese anchovy have demonstrated that energy allocation to
reproduction versus growth changes depending on per capita food availability [69].
A 1-D fish model is particularly useful in testing simple management scenarios, especially
when spatially explicit fisheries data (e.g. catches, fishing effort) are scant or unreliable, as is
the case for Greek and most other Mediterranean stocks [27]. Testing management options
with coupled full life cycle models is attractive because the bottom-up control of population
fluctuations is directly taken into consideration.
The current model formulation assumed that the diet of the two species is alike. This
assumption is supported by recent trophodynamic studies showing that, in contrast to upwell-
ing systems, the daily ration and diet composition of anchovy and sardine in the N. Aegean
Sea are remarkably similar ([30], [31], [32]). Although adult sardines ingest phytoplankton as
well, the contribution of phytoplankton to dietary carbon is negligible ([70], [31]) and cope-
pods are the main energy source for both species [32]. Despite the high diet overlap and, con-
sequently, food competition between anchovy and sardine in the N. Aegean Sea, the
simulations with varying fishing mortalities showed that the biomass of each species was
insensitive to changes in the biomass of the other species caused by changes in its exploitation
rate. This implies that the simulated mesozooplankton concentration suffices to support the
populations of the two species with no obvious trophic competition. Interestingly, what could
be seen from the two-species simulations and the two-way coupling of the fish with the lower
trophic level model was the top-down control of mesozooplankton by anchovy and sardine.
The combined fishing rates on the two species affected the concentration of mesozooplankton,
with sustainable exploitations leading to the decrease of mesozooplankton and unsustainable
exploitations to its increase. This can eventually have implications for the pelagic ecosystem
and fishery in the area. Removal of small pelagic fish may open up ecological space for other
species competing with small pelagics for the same zooplankton prey such as jellyfish [71]. For
example, in the Benguela system, off the coast of Namibia, overfishing of the sardine stocks in
the 60s and 70s led to the outbreak of jellyfish such as Chrysaora [72]. Episodes of anchovy
Engraulis encrasicolus collapse and ctenophore Mnemiopsis leidyi explosion occurred in the
Black Sea and the Caspian Sea ([73],[74]).
Testing the effect of timing of the 2.5-month closed period highlighted that the most effec-
tive timing for both species is the recruitment period which, however, is different for anchovy
(spring) and sardine (autumn). The simulations showed that protecting the numerically domi-
nant recruits prior and/or during the initial phase of their first spawning season contributes to
the increase in population fecundity and subsequently the increase in population biomass. The
current timing of the fishing ban (15 December-February) seems to be more suitable (although
not optimal) for sardine and less effective for anchovy. The periods 15 February-April or 15
March-May seems to be the most beneficial for anchovy.
It should be noted here that our simulations were based on fixed natural mortality rates and
averaged environmental conditions. However, natural mortalities can vary greatly in time and
space in relation to a variety of ecological factors, such as water temperature, fish condition
and size of prey and predator stocks. Such variability as well as inter-annual variability in envi-
ronmental conditions were not considered in this study and the results of the analyses repre-
sent average conditions.
A 1-D full life cycle anchovy and sardine model for the North Aegean Sea
PLOS ONE | https://doi.org/10.1371/journal.pone.0219671 August 15, 2019 20 / 24
Summarizing, the 1D anchovy-sardine IBM developed and calibrated in this study repro-
duced well the main characteristics of the two stocks in the N. Aegean Sea. The model was use-
ful in assessing the breeding pattern of the stocks as well as the outcomes of simple
management measures. The calibration of the anchovy-sardine model to the characteristics of
other Mediterranean stocks and the development and application of a 3D version are expected
to improve our understanding of the mechanisms controlling variations in abundance, distri-
bution and productivity of SPF populations in the Mediterranean Sea.
Supporting information
S1 File. Estimation of mean monthly somatic condition of anchovy and sardine.
(DOCX)
Author Contributions
Conceptualization: Athanasios Gkanasos.
Data curation: Marianna Giannoulaki, Eudoxia Schismenou.
Methodology: Stylianos Somarakis.
Software: Kostas Tsiaras, Dimitrios Kleftogiannis.
Supervision: Sarantis Sofianos, George Triantafyllou.
References
1. Checkley DM Jr., Bakun A, Barange M, Castro LR, Freon P, Guevara R, Herrick SF Jr., McCall AD,
Ommer R, Oozeki Y, Roy C, Shannon L, Van der Lingen CD. 2009. Synthesis and perspective. Climate
change and small pelagic fish. (Checkley DM Jr., Alheit J, Oozeki Y, Roy C, Eds.).:344–351., Cam-
bridge, UK; New York: Cambridge University Press
2. Alheit J., Roy C., & Kifani S. (2009). Decadal-scale variability in populations. In Checkley D., Alheit J.,
Oozeki Y., & Roy C. (Eds.), Climate Change and Small Pelagic Fish (pp. 64–87). Cambridge: Cam-
bridge University Press. https://doi.org/10.1017/CBO9780511596681.007
3. Checkley D., Asch R. and Rykaczewski R. (2017). Climate, Anchovy, and Sardine. Annual Review of
Marine Science, 9(1), pp.469–493.
4. Bakun A., Babcock E.A., Lluch-Cota S.E., Santora C., Salvadeo C.J. 2010. Issues of ecosystem-based
management of forage fisheries in ‘‘open” non-stationary ecosystems: the example of the sardine fish-
ery in the Gulf of California. Rev Fish Biol Fisheries 20: 9–29.
5. Pikitch, E., Boersma, P.D., Boyd, I.L., Conover, D.O., Cury, P., Essington, T., et al, 2012. Little fish, big
impact: managing a crucial link in ocean food webs. In: Lenfest Ocean Program, Washington, DC,
p. 108.
6. Peck M., Reglero P., Takahashi M. and Catala
´n I. (2013). Life cycle ecophysiology of small pelagic fish
and climate-driven changes in populations. Progress in Oceanography 116: 220–245.
7. Tsikliras A., Dinouli A., Tsiros V. and Tsalkou E. (2015). The Mediterranean and Black Sea Fisheries at
Risk from Overexploitation. PLOS ONE, 10(3), p.e0121188. https://doi.org/10.1371/journal.pone.
0121188 PMID: 25793975
8. Vasilakopoulos P., Maravelias C., Tserpes G. (2014). The Alarming Decline of Mediterranean Fish
Stocks. Current Biology, 24: 1643–1648. https://doi.org/10.1016/j.cub.2014.05.070 PMID: 25017210
9. VILIBIC
´I., ČIKES
ˇKEČV., ZORICA B., S
ˇEPIC
´J., MATIJEVIC
´S. and DZ
ˇOIC
´T. (2016). Hydrographic
conditions driving sardine and anchovy populations in a land-locked sea. Mediterranean Marine Sci-
ence, 17(1), p.1.
10. Brosset P., Me
´nard F., Fromentin J., Bonhommeau S., Ulses C., Bourdeix J., et al. (2015). Influence of
environmental variability and age on the body condition of small pelagic fish in the Gulf of Lions. Marine
Ecology Progress Series, 529: 219–231.
11. Brosset P., Fromentin J., Van Beveren E., Lloret J., Marques V., Basilone, et al. (2017). Spatio-temporal
patterns and environmental controls of small pelagic fish body condition from contrasted Mediterranean
areas. Progress in Oceanography, 151: 149–162.
A 1-D full life cycle anchovy and sardine model for the North Aegean Sea
PLOS ONE | https://doi.org/10.1371/journal.pone.0219671 August 15, 2019 21 / 24
12. Saraux C., Van Beveren E., Brosset P., Queiros Q., Bourdeix J., Dutto G., et al. (2019). Small pelagic
fish dynamics: A review of mechanisms in the Gulf of Lions. Deep Sea Research Part II: Topical Studies
in Oceanography, 159: 52–61.
13. Rose K.A., Fiechter J., Curchitser E.N., Hedstrom K., Bernal M., Creekmore S., et al. 2015. Demonstra-
tion of a fully-coupled end-to-end model for small pelagic fish using sardine and anchovy in the Califor-
nia Current. Prog. Oceanogr. 138: 348–380.
14. Somarakis S., Tsoukali S., Giannoulaki M., Schismenou E., Nikolioudakis N. 2019. Spawning stock,
egg production and larval survival in relation to small pelagic fish recruitment. Marine Ecology Progress
Series 617–618: 113–136.
15. Oguz T., Salihoglu B. and Fach B. (2008). A coupled plankton–anchovy population dynamics model
assessing nonlinear controls of anchovy and gelatinous biomass in the Black Sea. Marine Ecology
Progress Series 369: 229–256.
16. Pecquerie L., Petitgas P. and Kooijman S. (2009). Modeling fish growth and reproduction in the context
of the Dynamic Energy Budget theory to predict environmental impact on anchovy spawning duration.
Journal of Sea Research 62: 93–105.
17. Gatti P., Petitgas P. and Huret M. (2017). Comparing biological traits of anchovy and sardine in the Bay
of Biscay: A modelling approach with the Dynamic Energy Budget. Ecological Modelling, 348: 93–109.
18. Politikos D.V., Triantafyllou G.N., Petihakis G., Tsiaras K., Somarakis S., Ito S-I., et al, 2011. Application
of a bioenergetics growth model for European anchovy (Engraulis encrasicolus) linked with a lower tro-
phic level ecosystem model. Hydrobiologia, 670, 141–164.
19. Politikos D., Somarakis S., Tsiaras K.P., Giannoulaki M., Petihakis G., Machias A., et al. 2015. Simulat-
ing anchovy’s full life cycle in the northern Aegean Sea (eastern Mediterranean): A coupled hydro-bio-
geochemical-IBM model. Progress in Oceanography, 138: 399–416.
20. Pethybridge H., Roos D., Loizeau V., Pecquerie L. and Bacher C. (2013). Responses of European
anchovy vital rates and population growth to environmental fluctuations: An individual-based modeling
approach. Ecological Modelling 250: 370–383.
21. Kitchell J., Stewart D. Weininger D. (1977). Applications of a Bioenergetics Model to Yellow Perch
(Perca flavescens) and Walleye (Stizostedion vitreum vitreum). Journal of the Fisheries Research
Board of Canada, 34: 1922–1935.
22. Kooijman S. (2010). Dynamic energy budget theory for metabolic organisation. Cambridge University
Press. Cambridge
23. Ito S., Megrey B., Kishi M., Mukai D., Kurita Y., Ueno Y., et al. (2007). On the interannual variability of
the growth of Pacific saury (Cololabis saira): A simple 3-box model using NEMURO.FISH. Ecological
Modelling, 202: 174–183.
24. Megrey B., Rose K., Klumb R., Hay D., Werner F., Eslinger D., et al. (2007). A bioenergetics-based pop-
ulation dynamics model of Pacific herring (Clupea harengus pallasi) coupled to a lower trophic level
nutrient–phytoplankton–zooplankton model: Description, calibration, and sensitivity analysis. Ecological
Modelling, 202: 144–164.
25. Ito S., Rose K., Megrey B., Schweigert J., Hay D., Werner F., et al. (2015). Geographic variation in
Pacific herring growth in response to regime shifts in the North Pacific Ocean. Progress in Oceanogra-
phy, 138: 331–347.
26. Huret M., Tsiaras K., Daewel U., Skogen M.D., Gatti P., Petitgas P., et al. 2019. Variation in life-history
traits of European anchovy along a latitudinal gradient: a bioenergetics modelling approach. Marine
Ecology Progress Series, 617–618: 95–112.
27. Damalas D. 2017. A brief reflection on the Mediterranean fisheries: bad news, good news and no news.
Journal of Fisheries Research 1: 27–30.
28. Ganias K., Somarakis S., Nunes C., 2014. Reproductive potential. In: Biology and Ecology of Sardines
and Anchovies. CRC Press, Taylor & Francis Group, Boca Raton, pp. 79–121.
29. Somarakis S., Tsianis D.E., Machias A., Stergiou K.I. 2006. An overview of biological data related to
anchovy and sardine stocks in Greek waters. In Palomares M.L.D., K.I. Stergiou & D. Pauly (eds),
Fishes in Database and Ecosystems Fisheries Centre Research Reports 14: 56–64. Fisheries Centre,
University of British Columbia.
30. Nikolioudakis N., Palomera I., Machias A. and Somarakis S. (2011). Diel feeding intensity and daily
ration of the sardine Sardina pilchardus. Marine Ecology Progress Series 437: 215–228.
31. Nikolioudakis N., Isari S., Pitta P. and Somarakis S. 2012. Diet of sardine Sardina pilchardus: an ‘end-
to-end’ field study. Mar. Ecol. Progr. Ser. 453: 173–188.
32. Nikolioudakis N., Isari S. and Somarakis S. (2014). Trophodynamics of anchovy in a non-upwelling sys-
tem: direct comparison with sardine. Marine Ecology Progress Series 500: 215–229.
A 1-D full life cycle anchovy and sardine model for the North Aegean Sea
PLOS ONE | https://doi.org/10.1371/journal.pone.0219671 August 15, 2019 22 / 24
33. Giannoulaki M., Machias A., Tsimenides N. (1999). Ambient luminance and vertical migration of the sar-
dine Sardina pilchardus. Marine Ecology Progress Series, 178, pp.29–38.
34. Tsagarakis K., Giannoulaki M., Somarakis S. and Machias A. (2012). Variability in positional, energetic
and morphometric descriptors of European anchovy Engraulis encrasicolus schools related to patterns
of diurnal vertical migration. Marine Ecology Progress Series 446: 243–258.
35. Schismenou E., Giannoulaki M., Tsiaras K., Lefkaditou E., Triantafyllou G., Somarakis S., 2014. Disen-
tangling the effects of inherent otolith growth and model-simulated ecosystem parameters on the daily
growth rate of young anchovies. Marine Ecology Progress Series, 515, 227–237.
36. Schismenou E., Palmer M., Giannoulaki M., Alvarez I., Tsiaras K., Triantafyllou G., et al. 2016. Sea-
sonal changes in otolith increment width trajectories and the effect of temperature on the daily growth
rate of young sardines. Fisheries Oceanography, 25: 362–372.
37. Ganias K., Somarakis S., Koutsikopoulos C. and Machias A. (2007). Factors affecting the spawning
period of sardine in two highly oligotrophic Seas. Marine Biology 151: 1559–1569.
38. McBride R., Somarakis S., Fitzhugh G., Albert A., Yaragina N., Wuenschel M., et al. (2015). Energy
acquisition and allocation to egg production in relation to fish reproductive strategies. Fish and Fisheries
16: 23–57.
39. Somarakis S., 2005. Marked inter-annual differences in reproductive parameters and daily egg produc-
tion of anchovy in the northern Aegean Sea. Belg. J. Zool. 135, 247–252.
40. Machias A., Stergiou K.I., Somarakis S., Karpouzi V.S., Kapantagakis A. (2008) Trends in trawl and
purse seine catch rates in the north-eastern Mediterranean. Mediterranean Marine Science 9: 49–65
41. Somarakis S., Nikolioudakis N., 2007. Oceanographic habitat, growth and mortality of larval anchovy
(Engraulis encrasicolus) in the northern Aegean Sea (eastern Mediterranean). Marine Biology 152:
1143–1158.
42. Somarakis S., Schismenou E., Siapatis A., Giannoulaki M., Kallianiotis A. and Machias A. (2012). High
variability in the Daily Egg Production Method parameters of an eastern Mediterranean anchovy stock:
Influence of environmental factors, fish condition and population density. Fisheries Research, 117–
118: 12–21.
43. Giannoulaki M., Iglesias M., Tugores M.P., Bonanno A., Patti B., De Felice A., et al. 2013. Characteriz-
ing the potential habitat of European anchovy Engraulis encrasicolus in the Mediterranean Sea, at dif-
ferent life stages. Fisheries Oceanography 22, 69–89.
44. Blumberg A. and Mellor G. (1983). Diagnostic and prognostic numerical circulation studies of the South
Atlantic Bight. Journal of Geophysical Research: Oceans, 88(C8), pp.4579–4592.
45. Baretta J., Ebenho
¨h W. and Ruardij P. (1995). The European regional seas ecosystem model, a com-
plex marine ecosystem model. Netherlands Journal of Sea Research, 33(3–4), pp.233–246.
46. Petihakis G., Triantafyllou G., Allen I. J., Hoteit I. & Dounas C., 2002. Modelling the spatial and temporal
variability of the Cretan Sea ecosystem. Journal of Marine Systems 36: 173–196.
47. Tsiaras K., Kourafalou V.H., Raitsos D., Triantafyllou G., Petihakis G., Korres G., 2012. Inter-annual
productivity variability in the North Aegean Sea: influence of thermohaline circulation during the Eastern
Mediterranean Transient. J. Mar. Syst. 96– 97: 72–81.
48. Tsiaras K., Petihakis G., Kourafalou V., Triantafyllou G., 2014. Impact of the river nutrient load variability
on the N. Aegean ecosystem functioning over the last decades. J. Sea Res. 86: 97–109.
49. Schismenou, E., 2012. Modern approaches in biology and ecology of reproduction and growth of
anchovy (Engraulis encrasicolus) in the North Aegean Sea. PhD thesis, University of Crete, Greece.
50. Somarakis S. 1999. Ichthyoplankton of the NE Aegean with emphasis on anchovy, Engraulis encrasico-
lus (Linnaeus, 1758) (June 1993, 1994, 1995, 1996). PhD thesis, University of Crete
51. Tsikliras A.C. 2007. Thermal threshold of the onset of maturation in clupeid fishes using quotient analy-
sis. Rapport du Congrès de la Commission Internationale pour l’Exploration Scientifique de la Mer Me
´d-
iterrane
´e 38: 623.
52. ANTONAKAKIS K., GIANNOULAKI M., MACHIAS A., SOMARAKIS S., SANCHEZ S., IBAIBARRIAGA
L. et al. (2011). Assessment of the sardine (Sardina pilchardus Walbaum, 1792) fishery in the eastern
Mediterranean basin (North Aegean Sea). Mediterranean Marine Science, 12(2), p.333.
53. Giannoulaki M., Ibaibarriaga L., Antonakakis K., Uriarte A., Machias A., Somarakis S., et al. 2014.
Applying a two-stage Bayesian dynamic model to a short-lived species, the anchovy in the Aegean Sea
(Eastern Mediterranean): Comparison with an integrated catch at age stock assessment model. Medi-
terranean Marine Science 15: 350–365
54. Scheffer M., Baveco J. M., DeAngelis D. L., Rose K. A., and van Nes E. H. 1995. Super-individuals: a
simple solution for modelling large populations on an individual basis. Ecological Modelling 80: 161–
170.
A 1-D full life cycle anchovy and sardine model for the North Aegean Sea
PLOS ONE | https://doi.org/10.1371/journal.pone.0219671 August 15, 2019 23 / 24
55. Mantzouni I., Somarakis S., Moutopoulos D.K., Kallianiotis A., Koutsikopoulos C., 2007. Periodic, spa-
tially structured matrix model for the study of anchovy (Engraulis encrasicolus) population dynamics in
N Aegean Sea (E. Mediterranean). Ecological Modelling 208: 367–377.
56. Bernal M., Stratoudakis Y., Wood S., Ibaibarriaga L., Uriarte A., Valde
´s L., et al. 2011. A revision of
daily egg production estimation methods, with application to Atlanto-Iberian sardine. 1. Daily spawning
synchronicity and estimates of egg mortality. ICES Journal of Marine Science, 68: 519–527.
57. Alvarez P., Chifflet M. 2012. The fate of eggs and larvae of three pelagic species, mackerel (Scomber
scombrus), horse mackerel (Trachurus trachurus) and sardine (Sardina pilchardus) in relation to pre-
vailing currents in the Bay of Biscay: Could they affect larval survival? Sci. Mar. 76: 573–586.
58. Machias A, Tsimenides N (1995) Biological factors affecting the swimbladder volume of sardine (Sar-
dina pilchardus). Marine Biology 123:59–867
59. Hunter JR, Macewicz B (1985) Measurement of spawning frequency in multiple spawning fishes. In:
Lasker R (ed) An egg production method for estimating spawning biomass of pelagic fish: application to
the northern anchovy, Engraulis mordax. NOAA Tech Rep NMFS 36:79–93
60. Soufan O., Kleftogiannis D., Kalnis P. and Bajic V. (2015). DWFS: A Wrapper Feature Selection Tool
Based on a Parallel Genetic Algorithm. PLOS ONE 10(2), p.e0117988. https://doi.org/10.1371/journal.
pone.0117988 PMID: 25719748
61. Kleftogiannis D., Theofilatos K., Likothanassis S. and Mavroudi S. (2015). YamiPred: A Novel Evolu-
tionary Method for Predicting Pre-miRNAs and Selecting Relevant Features. IEEE/ACM Transactions
on Computational Biology and Bioinformatics, 12: 1183–1192. https://doi.org/10.1109/TCBB.2014.
2388227 PMID: 26451829
62. Patterson K. R., 1992. An improved method for studying the condition of fish, with an example using
Pacific sardine Sardinops sagax (Jenyns). Journal of Fish Biology, 40: 821–831.
63. STECF 2017. Scientific, Technical and Economic Committee for Fisheries. Mediterranean Stock
Assessments 2017 part I (STECF-17-15). Publications Office of the European Union, Luxembourg,
2017, ISBN 978-92-79-67487-7, https://doi.org/10.2760/897559, JRC109350
64. Isari S., Ramfos A., Somarakis S., Koutsikopoulos C., Kallianiotis A. and Fragopoulu N. (2007). Meso-
zooplankton distribution in relation to hydrology of the Northeastern Aegean Sea, Eastern Mediterra-
nean. Journal of Plankton Research, 28(3), pp.241–255.
65. Schismenou E., Tsiaras K., Kourepini M.I., Lefkaditou E., Triantafyllou G., Somarakis S. (2013) Sea-
sonal changes in growth and condition of anchovy late larvae explained with a hydrodynamic-biogeo-
chemical model simulation. Marine Ecology Progress Series 478: 197–209
66. Huse G. and Giske J. (1998). Ecology in Mare Pentium: an individual-based spatio-temporal model for
fish with adapted behaviour. Fisheries Research, 37: 163–178.
67. Okunishi T., Yamanaka Y. and Ito S. (2009). A simulation model for Japanese sardine (Sardinops mela-
nostictus) migrations in the western North Pacific. Ecological Modelling 220: 462–479.
68. Takasuka A., Oozeki Y. and Aoki I. (2007). Optimal growth temperature hypothesis: Why do anchovy
flourish and sardine collapse or vice versa under the same ocean regime? Canadian Journal of Fisher-
ies and Aquatic Sciences, 64: 768–776.
69. Tsuruta Y., Hirose K., 1989. Internal regulation of reproduction in the Japanese anchovy (Engraulis
japonica) as related to population fluctuation. In: Beamish R.J., McFarlane G.A. (Eds.), Effects of ocean
variability on recruitment and an evaluation of parameters used in stock assessment models. Can.
Spec. Publ. Fish. Aquat. Sci., NRC Research Press, vol. 108, pp. 111–119.
70. Costalago D., Palomera I. (2014). Feeding of European pilchard (Sardina pilchardus) in the northwest-
ern Mediterranean: from late larvae to adults. Scientia Marina 78: 41–54.
71. Richardson A., Bakun A., Hays G. and Gibbons M. (2009). The jellyfish joyride: causes, consequences
and management responses to a more gelatinous future. Trends in Ecology and Evolution, 24: 312–
322. https://doi.org/10.1016/j.tree.2009.01.010 PMID: 19324452
72. Lynam C., Gibbons M., Axelsen B., Sparks C., Coetzee J., Heywood B., et al (2006). Jellyfish overtake
fish in a heavily fished ecosystem. Current Biology, 16: R492–R493. https://doi.org/10.1016/j.cub.
2006.06.018 PMID: 16824906
73. Shiganova T. (1998). Invasion of the Black Sea by the ctenophore Mnemiopsis leidyi and recent
changes in pelagic community structure. Fisheries Oceanography 7: 305–310.
74. Daskalov G., Mamedov E. (2007). Integrated fisheries assessment and possible causes for the collapse
of anchovy kilka in the Caspian Sea. ICES Journal of Marine Science, 64: 503–511.
A 1-D full life cycle anchovy and sardine model for the North Aegean Sea
PLOS ONE | https://doi.org/10.1371/journal.pone.0219671 August 15, 2019 24 / 24
... These regions provide suitable habitats for small pelagic fish, characterized by enhanced food availability, increased larval retention and, consequently, largely overlapping spawning and nursery grounds . However, changes in oceanographic conditions may affect differently the two species, since an-chovy and sardine spawn and recruit in different seasons: Sardine mainly spawns during autumn and winter, whilst anchovy spawns in spring and summer Gkanasos et al., 2019). ...
... Such models have been implemented successfully for anchovy and sardine in the California Current (Rose et al., 2015) and for the Canary Current ecosystem (Sánchez-Garrido et al., 2019). Politikos et al. (2015) developed a 3-D individual based model (IBM), describing the full-life cycle of anchovy in the N. Aegean, while Gkanasos et al. (2019) extended the existing anchovy model to a 1-D multispecies (anchovy and sardine) model for the N. Aegean. ...
... Nutrient inputs from local rivers and Black Sea Water (BSW) discharge at the Dardanelles straits contribute to enhanced plankton productivity (Frangoulis et al., 2010;Siokou-Frangou et al., 2002). The previous implementation of a 1-D model (Gkanasos et al., 2019) was particularly useful for setting up the main attributes of the dynamics of the two species, despite its limitation in resolving horizontal processes. In this study, a more realistic description of the dynamics is provided, using a 3-D spatially explicit model that includes the spatial variability induced by fish movement and egg/larval advection by ocean currents. ...
Article
Full-text available
We present the development of a 3D full-lifecycle, individual-based model (IBM) for anchovy and sardine, online coupled to an existing hydrodynamic/biogeochemical low-trophic level (LTL) model for the North Aegean Sea. It was built upon an existing 1D model for the same species and area, with the addition of a horizontal movement scheme. In the model, both species evolve from the embryonic stage (egg+yolk sac larva) to the larval, juvenile, and adult stages. Somatic growth is simulated with the use of a “Wisconsin” type bioenergetics model and fish populations with an adaptation of the ‘super individuals’ (SI) approach. For the reference simulation and model calibration, in terms of fish growth and population biomass, the 2000-2010 period was selected. Interannual biomass variability of anchovy was successfully represented by the model, while the simulated biomass of sardine exhibited low variability and did not satisfactorily reproduce the observed interannual variability from acoustic surveys. The spatial distribution of both species’ biomass was in relatively good agreement with field data. Additional single-species simulations revealed that species compete for food resources. Temperature sensitivity experiments showed that both species reacted negatively to a temperature increase. Anchovy, in particular, was more affected since its spawning and larval growth periods largely overlap with the period of maximum yearly temperature and low prey concentration. Finally, simulation experiments using IPCC climatic scenarios showed that the predicted temperature increase and zooplankton concentration decrease in the future will negatively affect anchovy, resulting in sardine prevalence.
... Many of these non-indigenous Erythraean species are now established, and have proliferated and expanded from the east towards the central and western Mediterranean. Lessepsian migrants have been recognized as an important threat to native species, biodiversity and ecosystem functioning (Golani, 1998;Otero et al., 2013;Katsanevakis et al., 2014). Nevertheless, the establishment of certain non-indigenous species can also have positive impacts, particularly when they provide additional resources to local fisheries (e.g., Farrag et al., 2014). ...
... Seasonal changes in gonadal and somatic condition of males and females were analyzed with an "integrated" (sensu Plaza et al., [2007]) approach, using general linear models (see also Somarakis et al., [2012]; Geladakis et al., [2018]; Gkanasos et al., [2019]): Monthly leastsquare means (average monthly condition) were estimated by fitting the model: ...
... Only significant terms (p < 0.05) were retained in the final models (backward stepwise selection) (Geladakis et al., 2018;Gkanasos et al., 2019). Females with hydrated ovaries were excluded from the analysis of gonadal condition because they were collected inconsistently. ...
Article
Full-text available
The Golani’s round herring Etrumeus golanii is an Erythraean small pelagic fish (lessepsian migrant) that entered into the Mediterranean Sea through the Suez Canal. It has expanded its distribution from the east to the western Mediterranean with well-established local populations. We investigated basic aspects of its reproductive biology off the island of Crete (eastern Mediterranean) using ovarian histology and analysis of oocyte size-frequency distributions. The species exhibited a protracted breeding period (winter to early summer), with all ovaries examined during the main spawning season having markers of recent (postovulatory follicles, POFs) or imminent spawning (advanced oocyte batch in germinal vesicle migration or hydration). The advanced batch (AB) increased rapidly in size and was fully separated from the remainder, less developed oocytes in 95% of females with “old” POFs (POFs with signs of degeneration) and all females in final maturation. The growth of the subsequent batch (SB) was arrested at sizes <630 µm until full maturation of the AB. Mean diameter of hydrated oocytes ranged from 1181 to 1325 µm and relative batch fecundity was low ranging from 56 to 157 eggs g-1. The simulation of a coupled hydrodynamic/biogeochemical model (POM/ERSEM) provided evidence that E. golanii takes advantage of the seasonal cycle of planktonic production to reproduce and exhibits monthly changes in batch fecundity that appear to be closely related with the seasonal cycle of mesozooplankton concentration.
... All the GLM analyses were performed using backward stepwise selection and only significant terms (p < 0.05) were retained in the final models. All assumptions, i.e., normal distribution of errors and homogeneity of variance, were met [16,31,32]. When no significant model could be fitted, sample means were used. ...
Article
Full-text available
Fish with indeterminate fecundity spawn multiple times throughout a protracted reproductive period. During that period several ovulation events succeed one another, and different oocyte developmental stages co-occur in the ovaries with new oocytes consistently recruiting from one growth phase to the next to form the sequential batches. In this study, we examined in detail the oocyte recruitment and development pattern of the sequential batches in a commercially important fish with indeterminate fecundity, the European sardine. The numbers and sizes of oocytes at different developmental stages were estimated for four phases of the ovulatory cycle (ovarian stages) and during the main spawning season (November–March) by applying the oocyte packing density theory in combination with stereological techniques. General linear models (GLMs) were used to test for changes in oocyte sizes as well as relative oocyte numbers per developmental stage within the different ovarian stages in the successive spawning months. A temporal association between several transition events of the oocyte development process was revealed. Specifically, the final maturation of the advanced batch triggered (a) the recruitment of oocytes from primary to secondary growth phase, (b) de novo vitellogenesis and (c) a surge of yolk deposition in primary vitellogenic oocytes. Oocyte recruitment was completed two days after the ovulation of the advanced batch and relative numbers of primary and secondary growth oocytes were thereafter stable until the next final maturation event. This pattern of oocyte recruitment and growth remained unchanged during the course of the spawning season. This study advances our knowledge on oocyte recruitment and development in fish with indeterminate fecundity, which is key to understanding reproduction and its drivers at the individual and population level.
... This study employed the structure of spawning algorithms developed for Atlantic mackerel (Gkanasos et al., 2019) with several modifications and parameter replacements for the applicability of chub mackerel (Figure 2). The spawning season was assumed to be from January to June, based on observations (Watanabe, 1970). ...
Article
Full-text available
A bioenergetics and population dynamics coupled model that includes a full life cycle and size/growth-dependent mortality function was developed to better understand stock fluctuations. As an example, the model was applied to chub mackerel (Scomber japonicus) as it shows large stock fluctuations in the western North Pacific. The mortality dependency parameters for growth/size were adjusted to achieve realistic stock fluctuations in the model from 1998 to 2018. Two types of mortality functions were used in the model: one based on both size and growth, and the other based solely on size. An increasing trend of stock fluctuation of chub mackerel in the 2010s was reproduced in the simulation by contributions of several strong monthly cohorts that formed strong year classes using both types of mortality functions. The reproducibility of the stock fluctuation was not markedly different between the models with the two types of mortality functions, which indicates the importance of size-dependent mortality on the stock fluctuations of chub mackerel. The influence of sea surface temperature (SST) and chlorophyll-a was evaluated separately by using the climatological values for one of the forcings, and the model results revealed that the stock fluctuations of chub mackerel during 1998–2018 were mainly controlled by chlorophyll-a, whereas the increasing stock during 2010–2014 was strongly influenced by chlorophyll-a, and that after 2014 was influenced by SST. When integrated with different fishing pressures, the model showed that high fishing pressure hinders the recovery of chub mackerel stocks, highlighting the importance of effective fishery management.
... Anchoviella lepidentostole (Fowler 1911) stood out as abundant in April 2013 (44% of captured larvae), August 2013 (43% of collected larvae), March 2014 (43% of the captured individuals), January 2014 (35% of the collected individuals), May 2014 (34% of the captured larvae) and July 2014 (11% of the collected larvae) (Fig. 7.18). Thus, Anchoviella lepidentostole presented its greatest abundance during the rainy months, a favorable period for its reproductive cycle (Gkanasos et al. 2019). However, Anchoviella lepidentostole was also abundant during a dry month (August 2013), which suggests a longer reproductive period for this species, with reproductive peaks throughout the year. ...
Chapter
Full-text available
Zoo- and ichthyoplankton are key components of pelagic ecosystems. This study investigates zoo- and ichthyoplankton communities in seven Brazilian tropical marine environments that differ considerably in their abiotic and biological settings. The two study areas off Pará and Maranhão (Northern Brazil) present extremely wide continental shelves lined by mangroves. Two narrow oligotrophic shelf areas are located in northeastern Brazil (Pernambuco and Bahia). Three oceanic areas make up the unique Brazilian island systems (Rocas Atoll, Fernando de Noronha and St. Peter and St. Paul’s Archipelagos). The waters off Salvador (Bahia) are influenced by oceanic water masses, resulting in the occurrence of tropical oceanic species. Higher temperatures and salinities that fluctuate seasonally lead to a lower density and diversity of copepods. Off Tamandaré (Pernambuco), ichthyoplankton, copepods, and decapods abounded inshore, especially during the dry season. In northern shelf systems (Pará and Maranhão), fish larvae were more abundant during the rainy season. Off Pará, caridean shrimp larvae were found closer to the coast, while penaeids abounded offshore. Off oceanic islands, some groups, such as fish eggs, were significantly more abundant downstream (island biomass effect). In general, strong inshore-offshore gradients in plankton communities were observed, and for some taxa, seasonal variations in their density were observed.KeywordsContinental shelfOceanic islandsDiversityEcology
... Recently, Tsiaras et al. (2017a) examined the performance of the model assimilating satellite derived Chl-a with regard to the assimilated data (Chl-a) and non-assimilated model variables, such as dissolved inorganic nutrients (nitrates, phosphates). Given the experience obtained by the widespread use of the generic POSEIDON ecosystem model in the Mediterranean Sea at both research and operational arenas (Petihakis et al., 2009(Petihakis et al., , 2002(Petihakis et al., , 2012Triantafyllou et al., 2000Triantafyllou et al., , 2003Tsiaras et al., 2010Tsiaras et al., , 2014Tsiaras et al., , 2017aTsiaras et al., , 2017bPolitikos et al., 2011;Kalaroni et al., 2016;Hatzonikolakis et al., 2017;Gkanasos et al., 2019), and the growing availability of observational data, is now mature for an in-depth model skill assessment in simulating the main components of the pelagic ecosystem (nutrients, Chl-a, phytoplankton, zooplankton bacteria, dissolved and particulate organic matter). ...
Article
Ecosystem models are recognized as valuable tools to understand marine ecosystem dynamics and address management questions, requiring an integrated approach of physical and biotic processes. In the present study, a three-dimensional basin scale Mediterranean hydrodynamic/biogeochemical model, currently operational as part of the POSEIDON forecasting system, was extensively validated against available in-situ and satellite data. The generic POSEIDON ecosystem model skill was objectively assessed, in capturing the observed seasonal variability of the main chemical ecosystem components within the planktonic food web. A cluster K-means analysis was applied to obtain an objective ‘biogeography’ of the Mediterranean Sea, allowing a more efficient validation of model outputs against observational data. The model presented a reasonable skill in reproducing the seasonal cycle and observed patterns of the Mediterranean inorganic nutrients and chlorophyll-a, characterized by a prominent west-to-east gradient and their increase in areas receiving lateral nutrient inputs. Despite some model deviations, validation results have demonstrated the capability of the model to represent the Mediterranean ecosystem, ranging from oligotrophic open ocean to mesotrophic conditions in productive coastal areas.
Article
Full-text available
A Wisconsin type bioenergetics model was developed to investigate the growth and reproduction of the Mediterranean swordfish Xiphias gladius L., 1758. Reproduction was simulated using an energy allocation algorithm with a fixed part of assimilated energy stored for egg production. Stomach contents were used to estimate the daily ration of swordfish (3% of body weight for adults) in order to calibrate the consumption compartment. The model outputs of growth were in agreement with fisheries observation data, with estimates of annual egg production (~17.5 million eggs) per individual similar to those stemming from stock assessment datasets. Our study highlights the importance of bioenergetics in the reproduction of swordfish, suggesting that each individual is reproductively active for ~15 d, while the commonly reported spawning season of the whole population lasts ~90 d. Sensitivity analysis showed that swordfish growth and reproduction is largely controlled by consumption and respiration parameters. We provide a detailed description of a full life cycle swordfish bioenergetics model that could be embedded as a module in an end-to-end modelling framework, ultimately describing the population dynamics of the Mediterranean swordfish stock in relation to environmental variability.
Article
Full-text available
Anchovy Engraulis encrasicolus distribution in European waters spans from the Mediterranean Sea to the North Sea, and is expected to expand further north with global warming. Observations from the eastern Mediterranean (North Aegean Sea), the Bay of Biscay and the North Sea reveal latitudinal differences in growth, maximum size, fecundity and timing of reproduction. We set up a mechanistic framework combining a bioenergetics model with regional physical-biogeochemical models providing temperature and zooplankton biomass to investigate the underlying mechanisms of variation in these traits. The bioenergetics model, based on the Dynamic Energy Budget theory and initially calibrated in the Bay of Biscay, was used to simulate growth and reproduction patterns. Environment partly explained the increased growth rate and larger body size towards the north. However, regional calibration of the maximum assimilation rate was necessary to obtain the best model fit. This suggests a genetic adaptation, with a pattern of cogradient variation with increasing resource towards the north, in addition to a countergradient thermal adaptation. Overall, the seasonal energy dynamics supports the pattern of body-size scaling with latitude, i.e. food-limited growth but low maintenance costs in the warm Aegean Sea, and larger size in the North Sea allowing sufficient storage capacity for overwintering. Further, the model suggests a synchronisation of reproductive timing with environmental seasonality as a trade-off between thresholds of temperature and reserves for spawning and overwintering, respectively. Finally, low temperature, short productive and spawning seasons, and insufficient reserves for overwintering appear to be current limitations for an expansion of anchovy to the Norwegian Sea.
Article
Full-text available
Anchovy and sardine populated productive ocean regions over hundreds of thousands of years under a naturally varying climate, and are now subject to climate change of equal or greater magnitude occurring over decades to centuries. We hypothesize that anchovy and sardine populations are limited in size by the supply of nitrogen from outside their habitats originating from upwelling, mixing, and rivers. Projections of the responses of anchovy and sardine to climate change rely on a range of model types and consideration of the effects of climate on lower trophic levels, the effects of fishing on higher trophic levels, and the traits of these two types of fish. Distribution, phenology, nutrient supply, plankton composition and production, habitat compression, fishing, and acclimation and adaptation may be affected by ocean warming, acidification, deoxygenation, and altered hydrology. Observations of populations and evaluation of model skill are essential to resolve the effects of climate change on these fish.
Article
Full-text available
The aim of this paper is to establish a relationship between long-term variability in sardine and anchovy populations in the Adriatic Sea and ocean dynamics and processes that occur over interannual and decadal timescales in the Adriatic-Ionian basin. Basis for such analysis are annual time series of sardine and anchovy landings and recruits at age 0 and annual time series of environmental parameters observed at a representative Adriatic station between 1975 and 2010. Pearson correlations and robust Dynamic Factor Analysis (DFA) were applied to quantify the connections between fisheries and environmental parameters. Variations and trends in fisheries series were best explained by changes in near-bottom temperature and salinity, being an appropriate proxy for tracking changes in water masses' dynamics and hydrographic conditions in the basin. It seems that a prolonged period of decreasing sardine population was characterized by low oxygen availability and environmental conditions in the deep Adriatic waters, triggered by an extraordinary basin-wide event called the Eastern Mediterranean Transient. A collapse in anchovy population has been observed after an exceptional cooling event followed by dense water formation.
Chapter
The Food and Agriculture Organization (FAO) defines reduction fisheries as fisheries that are geared towards the reduction of the catch to fishmeal and/or fish oil. These fisheries are relatively recent. Excess of seasonal catches of herring and sardines started to be processed in northern Europe and North America at the beginning of the 19th century to obtain fish oil to produce non-food products such as soap and lubricants for machinery. Once the benefit of fishmeal as an inexpensive food supplement for animal feeds was realized, their demand increased. Fisheries began to target anchovies and sardines worldwide, among other clupeoids, for reduction into fishmeal, fish oil being its by-product. After the 1950‘s, huge reduction fisheries and fishmeal production factories were developed in several countries such as the US, Norway, Peru, Japan (Watson et al. 2006). In the late 1980‘s, the global production of marine fish dedicated to produce fishmeal and oil peaked at more than 30 mt according to FAO estimates, which has remained relatively stable until the last years, and can be generally considered as the maximum catch that reduction fisheries can sustainably extract from the global oceans. Therefore, the amount of raw material to produce fishmeal is limited by marine ecosystems’ productivity and their capacity to sustain small pelagic fisheries. However, according to global databases (Fig. 7.1), overall small pelagic fisheries production has declined moderately since 2000. The conversion ratio of live fish into fishmeal has been reduced, enabling production of fishmeal to be maintained despite the decline of total small pelagic fisheries production. However, further increases of fishmeal and oil production are unlikely unless other species are used as raw material (Watson et al. 2006). Further comments on the historic development of reduction fisheries, their fishing methods, reduction process and a brief description of the ecological relevance of small pelagic fish are presented here.
Article
Under the general framework of existing recruitment hypotheses, knowledge on the drivers and mechanisms involved in the determination of the year class strength of small pelagic fish (SPF) is briefly reviewed with focus on selected aspects of the adult and larval stages, related to breeding patterns, egg production, spawning habitats, reproductive potential and early life survival. An analysis of stock-recruitment time series data is carried out, showing that the maximum recruitment capacity of clupeoid stocks increases with the strength of temporal autocorrelation in recruitment (R) and decreases as the coefficient of variation of R becomes larger. Reproductive strategy in combination with the thermal and trophic conditions of the ecosystem and the life cycle pattern of the stock can influence the relative importance of high and low frequency variability in recruitment that combine to generate the population fluctuations of SPF. Selective fishing can reduce the reproductive potential and alter the spawning phenology of the stocks. To understand the ways by which the distribution, abundance and survival of larval stages are influenced by trophodynamic and physical factors, it is important to recognize all those milestones in fish ontogeny associated with significant changes in capabilities and behavior (e.g. onset of schooling). Temperature affects many parameters related to egg production and early life survival, but the relative importance of such temperature effects is expected to differ substantially in contrasting SPF habitats. Open access publication available at: https://www.int-res.com/articles/theme/AdvanceView/M12642_Somarakis_SPF.pdf
Article
Around 2008, an ecosystem shift occurred in the Gulf of Lions, highlighted by considerable changes in biomass and fish mean weight of its two main small pelagic fish stocks (European anchovy, Engraulis encrasicolus; European sardine, Sardina pilchardus). Surprisingly these changes did not appear to be mediated by a decrease in fish recruitment rates (which remained high) or by a high fishing pressure (exploitation rates being extremely low). Here, we review the current knowledge on the population's dynamics and its potential causes. We used an integrative ecosystem approach exploring alternative hypotheses, ranging from bottom-up to top-down control, not forgetting epizootic diseases. First, the study of multiple population characteristics highlighted a decrease in body condition for both species as well as an important decrease in size resulting both from a slower growth and a progressive disappearance of older sardines. Interestingly, older sardines were more affected by the decrease in condition than younger ones, another sign of an unbalanced population structure. While top-down control by bluefin tuna or dolphins, emigration and disease were mostly discarded as important drivers, bottom-up control mediated by potential changes in the plankton community appeared to play an important role via a decrease in fish energy income and hence growth, condition and size. Isotopic and stomach content analyses indicated a dietary shift pre- and post-2008 and modeled mesozooplankton abundance was directly linked to fish condition. Despite low energy reserves from 2008 onwards, sardines and anchovies maintained if not increased their reproductive investment, likely altering the life-history trade-off between reproduction and survival and resulting in higher natural mortality. The current worrying situation might thus have resulted from changes in plankton availability/diversity, which remains to be thoroughly investigated together with fish phenotypic plasticity.
Article
Similar or very contrasted puzzling population dynamics between anchovy and sardine occur worldwide. Underlying factors are not well understood, but insights towards different biological traits are suggested, in particular trophic specialisation, leading to different responses to environmental conditions. Based on most striking differences in biological and life history traits, i.e. size, spawning and feeding, we calibrated a bioenergetics model, based on the Dynamic Energy Budget theory, for Engraulis encrasicolus and Sardina pilchardus in the Bay of Biscay. Starting from the anchovy model, differences in traits were successively integrated to build the sardine model through a novel exploratory approach by scenarios. We used a robust method for parameter estimation, the Evolution Strategies, with a large dataset of length and mass at age, as well as energy density, which is the first time in such a model calibration. Energy density data proved to be particularly well suited to assess the quality of DEB model predictions and parameter set estimates. Insights in respective physiology were drawn from analysis of parameter values and predictions of the model. We showed that anchovy and sardine have distinct strategies with respect to energy acquisition and especially to allocation to spawning. Anchovy are characterised by higher metabolic rates and requirements. This species is more likely to benefit from periods of high food availability to carry out both growth, spawning and reserve storage. Sardine have less demanding food requirements and metabolic costs. Sardine take advantage of larger reserves storage capacity to decouple spawning and prey blooms and to lengthen spawning period, and thus display a more capital breeding spawning behaviour. Overall, our model outputs distinguish between anchovy that tend towards an almost “all or nothing” energetic strategy, and sardine that tend to carry out lower metabolic activities but on a more regular basis. This first modelling demonstration of a bioenergetics difference between these two species, and the explanation it brings in the understanding of their respective reproduction strategies, opens new perspectives in the interpretation of their differential responses at the population scale to environment variability.
Article
Small pelagic fish are among the most ecologically and economically important marine fish species and are characterized by large fluctuations all over the world. In the Mediterranean Sea, low catches and biomass of anchovies and sardines have been described in some areas during the last decade, resulting in important fisheries crises. Therefore, we studied anchovy and sardine body condition variability, a key index of population health and its response to environmental and anthropogenic changes. Wide temporal and spatial patterns were investigated by analyzing separately data from scientific surveys and fisheries in eight Mediterranean areas between 1975 and 2015.
Article
We studied the otolith microstructure and growth of sardine, Sardina pilchardus, in the North Aegean Sea (eastern Mediterranean Sea), using samples of larvae and juveniles that had hatched in winter (November-January) and winter-spring (February-May), respectively. The juveniles had developed during an extended period coinciding with marked pelagic ecosystem changes (from winter, mixed conditions to summer, stratified waters). To examine the relationship between environmental changes and the observed variability in their otolith increment-width trajectories (width-at-age), we summarized the shape of trajectories with a four-parameter set estimated from a growth model fit to each width trajectory. The individual parameter sets were then related to the potential oceanographic conditions that fish experienced during their development, derived from a hydrodynamic-biogeochemical model (POM-ERSEM), implemented in the sampling area. Substantial seasonal effects were demonstrated on the otolith microstructure (platykurtic versus leptokurtic trajectories in winter-mixed versus summer-stratified conditions), which were related to the progressive sea surface warming. In a subsequent step, in order to study the effect of oceanographic conditions on larval and juvenile daily growth rates, a GAM (Generalized Additive Model) analysis of otolith increment widths was carried out, using model-derived oceanographic parameters and taking into account the 'inherent otolith growth', expressed by the explanatory variables 'previous increment width' and 'Age'. Results showed a strong and positive, linear effect of temperature on the growth rate of winter-caught larvae, whereas in juveniles, which had developed within a wide range of temperatures, an optimum temperature for growth was observed at around 24°C.