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The role of small pelagic fish in the ecosystem
25 January 2007
Lynne Shannon, Marta Coll, Sergio Neira, Philippe Cury and Jean-Paul Roux
==========================
Abstract
Small pelagic fish are termed “wasp-waist” species as they dominate mid-trophic
levels, comprise relatively few species but attain large abundances that can vary
drastically in size. They have been shown to exert top-down control on their prey
species and bottom-up control on their predators and, in this way, appear to induce
unsuspected ecosystem dynamics. This chapter explores these effects and associated
dynamics, not only to reveal the importance of small pelagic fish in structuring marine
ecosystems but also to examine the consistency of the role of small pelagic fish across
various upwelling systems. The Northern and Southern Benguela, Southern
Humboldt, South Catalan Sea and North and Central Adriatic Sea ecosystems are
compared in terms of the importance and role of small pelagic fish using information
gained from landings: i) Trophic level of the catch, ii) the Fishing-in-Balance (FiB)
index and iii) the ratio of pelagic:demersal fish. Indicators derived from trophic
models of these ecosystems are selected to assist in defining the effects of small
pelagic fisheries, and include: i) Catch/Biomass ratios for small pelagic fish, ii)
Exploitation rate E=F/Z, where F is fishing mortality and Z is total mortality (natural
and fishing mortality combined) for the main commercial fish species in each system,
iii) Sum of all flows to detritus. Models of the Southern Benguela, Southern
Humboldt and South Catalan Sea are used to perform two simulations: 1) Closure of
fishery on small pelagic fish and 2) Collapse of small pelagic fish, to further explore
the roles of small pelagic fish in the dynamics of these ecosystems.
Tracking pelagic:demersal fish catch and biomass ratios over time is a means of
detecting collapse in the small pelagic fish stocks, and comparing these ratios across
ecosystems highlights the greater importance of small pelagic fish in the Humboldt
compared to other ecosystems. The trophic level of the catch severely declined in the
Northern Benguela and Southern Humboldt ecosystems, reflecting collapses in small
pelagic and/or other fisheries in these regions. In the Mediterranean Sea, fluctuations
in TL of the catch, in conjunction with the FiB index, reflects the collapse of the small
pelagic fish and disruption of the ecosystem. Small pelagic fishing mortalities are
smallest in the Adriatic (maximum F = 0.2 y-1), and the Southern Benguela
(maximum F= 0.3 y-1 for anchovy and sardine in the 1980s), whereas fishing
mortality rates exceeding 0.3 y-1 and 0.5 y-1 are estimated for anchovy in the South
Catalan and Northern Benguela, respectively. Estimated fishing mortalities are greater
than 0.6 y-1 for sardine in the South Catalan, and F of anchovy and common sardine is
estimated to have exceeded 0.7 y-1 in the Southern Humboldt ecosystem in 1992. Thus
it appears that smaller fishing mortalities can be supported in the systems exhibiting
greater biodiversity (shallow bank and upwelling area of the Southern Benguela;
diverse environmental conditions responsible for diverse habitats in the Adriatic).
Models analyzed in this study show how a decrease in small pelagic fish abundance
will have detrimental effects on both higher and lower trophic levels of the food web,
causing a decrease in predators and the proliferation of other species that are preys or
competitors of small pelagic fish, but which do not constitute an alternative pathway
for the flow of primary productivity to higher trophic levels. Trophic model
simulations showed consistently that gelatinous zooplankton increase when small
pelagic fish stocks decline and conversely, there is a decrease in jellyfish abundance
when closure of the pelagic fisheries is simulated. Model simulations of small pelagic
fishery collapses in the southern Benguela, Southern Humboldt and South Catalan Sea
all emphasize the dependency of avian and to a lesser extent more opportunistic
mammalian and fish predators, on healthy stocks of small pelagic fish. Moreover,
collapses of small pelagic fish generally disrupt energy flows, which could result in an
increase in flows to detritus, demersal processes within the system becoming more
important, stronger overall mixed trophic interactions of the pelagic component on the
demersal component in more recent periods (usually when fishing has increased), and
often reduced summed impacts of the demersal compartment on the degraded pelagic
food web. Examination of summed mixed trophic impacts of detritus on both the
pelagic and demersal food webs further supported the hypothesis that detritus
becomes increasingly more important as ecosystems are fished and/or degraded.
However, in the Northern Benguela, the near-total collapse of the pelagic ecosystem
has weakened detritus-pelagic food web linkages, whereas detritus-demersal linkages
have strengthened.
==========================
Chapter contents:
1. INTRODUCTION: ROLE OF SMALL PELAGIC FISH IN MARINE ECOSYSTEMS
1.1. Small pelagic fish as the wasp-waist of ecosystems
1.2. Outline of the chapter
2. THE ECOSYSTEMS EXAMINED
2. 1. Benguela upwelling region
2.2. Humboldt upwelling system
2.3. Mediterranean ecosystems of the Catalan and Adriatic seas
3. METHODS
3.1. Catch and abundance data series
3.2. “Static” (“Snapshot”) models
3.3. Models fitted to time series data
3.4. Simulations
4. MODEL RESULTS
4.1 Catch ratios and abundances
4.2 Fishing mortality, predation and exploitation rates
4.3 Gelatinous zooplankton and proliferation of other species
4.4. Effects of small pelagic fish on top predators
4.5. Flows to detritus
4.6 Coupling demersal-pelagic compartments
5. DISCUSSION
5.1. Trophic flow controls, fishing and the environment
5.2. Generic effects of fishing on small pelagic fish
5.3. Proliferation of species
5.4. Effects of small pelagic fish on top predators
5.5. Increased pelagic-benthic coupling and flow to detritus
5.6. Enhancing catches of commercially valuable predatory fish by reducing small
pelagic fish catches?
6. SMALL PELAGIC FISH AS INDICATORS OF ECOSYSTEM COLLAPSE?
6.1. Ecosystem indicators
6.2. Recommended exploitation rates
6.3. Disruption of trophic pathways
1. INTRODUCTION: ROLE OF SMALL PELAGIC FISH UP AND DOWN
THE FOOD WEB
1.1 Small pelagic fish as the wasp-waist of ecosystems
Small pelagic fish, dominating mid-trophic levels and being comprised of relatively
few species but attaining large abundances that can vary drastically in size, have been
named “wasp-waist” species (Rice, 1995; Bakun 1996, Fig. 1). Small pelagic fish
have been shown to exert top-down control on their prey species and bottom-up
control on their predators, which has been described as a ‘wasp-waist’ control (Cury
et al., 2000). The ‘‘boom-bust’’ dynamics of pelagic fish and populations that interact
trophically with them suggests a ‘‘predator pit’’ type of dynamics according to Bakun
(2006). This special configuration in certain marine food webs and the role and
dynamics of pelagic fish appears to induce unsuspected ecosystem dynamics. These
effects and associated dynamics need to be explored in detail, not only to reveal the
importance of small pelagic fish in structuring marine ecosystems but also to examine
the consistency of their role in various upwelling systems.
Regime shifts or switches in pelagic fish species abundance may be initiated or
sustained by changes in zooplankton availability (Schwartzlose et al., 1999). On the
other hand, changes in abundance of small pelagic fish may have top-down effects on
the abundance and community structure of zooplankton prey (Schwartzlose et al.,
1999). Between the 1950s and the 1990s, the proportion of small cyclopoid copepods
off the west coast of South Africa increased, compared to a decrease in the relative
abundance of large calanoid copepods, and the biomass of copepods increased tenfold
whereas total copepod abundance increased 100-fold (Verheye and Richardson, 1998;
Verheye et al., 1998). Both bottom-up and top-down effects of small pelagic fish on
zooplankton in this region have been proposed (Verheye et al., 1998), although Cury
et al. (2000) showed that the general rule in upwelling systems, including the
Benguela, is that small pelagic fish exert top-down control on their zooplankton prey.
Small pelagic fish have been shown to exert important controls over their predators
too. Seabirds, in particular, have been found to respond strongly to changes in pelagic
fish abundances. Seabird guano harvests off South Africa and Peru reflected changes
in pelagic fish abundance (Crawford and Jahncke, 1999) and several population
parameters measured for African penguins, Cape cormorants and swift terns off South
Africa have been related to stock fluctuations of anchovy and sardine (Best et al.,
1997). These have been verified through changes in seabird diet compositions in
response to changes in pelagic fish abundance (e.g. that of the Cape gannet Morus
capensis, Crawford and Dyer, 1995). Similarly, off Namibia, as sardine abundance
decreased, pelagic goby replaced sardine as the important prey item in the diets of
Cape Gannets, Cape Cormorants Phalacrocorax capensis and African Penguins
Spheniscus demersus (Crawford et al., 1985). Off Namibia, sardine were an important
prey of the Cape fur seal, Arctocephalus pusillus pusillus in earlier years whereas
goby, supplemented by myctophids in the southern part of the Northern Benguela, and
horse mackerel in the central and northern parts of the Northern Benguela, became the
main prey of seals in later years (Mecenero and Roux, 2002; J.-P. Roux, NMFR,
Namibia, pers. comm.). The dominant large pelagic fish predator in the southern
Benguela, namely snoek (Thyrsites atun), preys non-selectively on pelagic fish (M.
Griffiths, Marine and Coastal Management, pers. obs.) and diet studies have shown
that snoek feed on anchovy and sardine in accordance with their relative abundances
in the ocean (Crawford et al., unpublished ms). In the Mediterranean Sea, small
pelagic fish have been shown to be important prey for demersal fish, marine mammals
and seabirds (Bozzano et al., 1997; Ríos, 2000; Arcos, 2001; Blanco et al., 2001;
Stergiou and Karpouzi, 2002).
Empirical studies reveal patterns of interaction with small pelagic fish (e.g. with top
predators such as birds and seals or with zooplankton prey) that have been obtained at
different spatial and temporal resolutions. Thus the time series used to study the effect
of changes in biomass of small pelagic fish on seals or birds are estimated at the level
of the ecosystem and on an annual basis, while the time series of plankton have
usually been collected locally at a fine temporal scale. These differences in the
resolution can substantially bias the way we analyze control versus what might be
regarded as a local depletion with no effect on the overall population, and such
interactions need to be explored in a broader perspective.
Piscivorous fish (such as snoek and hake) support fisheries of high commercial value
and thus the linkages between small pelagic fisheries and these fisheries can be very
important. It is often debated as to whether there would be value in fishing more
lightly on small pelagic fish in order to leave more forage fish for predatory fish,
thereby potentially benefiting fisheries on these predatory fish. This is still an open
question, to which answers may be provided through model simulations or the
implementation of carefully designed experimental fishing scenarios. It is the former
option that is very briefly explored in this study, although more rigorous and detailed
modelling is recommended.
As we are now fishing down marine food webs (Pauly and Palomares, 2005), fishing
pressure is increasing on organisms at lower trophic levels, such as small pelagic fish
(FAO, 2005). Therefore, their increased exploitation is expected to have a wide
impact on the pelagic food web and might provoke the dysfunction of the ecosystem
and the further depletion of populations of dependent predators at higher trophic
levels. This can cause, as has already been observed when top predators are
overfished (Springer et al., 2004; Frank et al., 2005), large trophic cascades and
proliferation of species located at lower trophic levels or having shorter life spans
(Daskalov, 2002; Cury et al., 2005b). All these changes on exploited marine
ecosystems point to the existence of a sequence of flow controls as ecosystems are
fished down or as community turn-over rates increase, which is of great relevance in
terms of recovery of intense exploited ecosystems (Fig. 2). There is thus a need to
characterize what changes are occurring where and why, as well as which ecosystem
elements favour these changes in relation to fishing pressure, control mechanisms and
environmental variability. An essential element is to analyze to what extent observed
ecosystem changes due to the collapse of the pelagic system and changes in flow
control are reversible.
1.2. Outline of the chapter
In this chapter, we focus on the following ecosystems in which small pelagic fish play
important roles, both commercially and within the food web: the Benguela (South
Africa and Namibia), the Southern Humboldt (Chile), the Mediterranean Sea (South
Catalan and the North and Central Adriatic), and to a lesser extent also the Northern
Humboldt (Peruvian) system, representing a gradient of exploited ecosystems.
In a previous study, comparative trophic models of upwelling ecosystems have been
considered, and taking into account the exploitation history of these ecosystems,
selected indicators were analysed to test an initial hypothesis that an ecological model
representing the South Catalan Sea (Northwestern Mediterranean) would be ranked
within the high impacted areas of Namibia and Peru, which were differentiated in
terms of ecosystem impact from the moderately impacted regions of Chile and South
Africa (Moloney et al., 2005; Coll et al., 2006a).
This chapter aims to define, in a quantifiable respect, the disruption of food webs
(Fig. 2) as a result of small pelagic fish collapse (by comparing with healthy situations
where small pelagic fish are considered to be sustainably exploited), and to show how
small pelagic fish can be used as indicators or warning signs of a future ecosystem
collapse or change.
2. THE ECOSYSTEMS EXAMINED
2.1. Benguela upwelling region
The Benguela upwelling region is subdivided by the permanent Lűderitz upwelling
cell around 26oS into two systems, namely the Southern Benguela ecosystem off
South Africa and the Northern Benguela ecosystem off Namibia. The Northern
Benguela ecosystem extends from the Angola-Benguela front located between 14oS
and 16oS (Meeuwis and Lutjeharms, 1990) southwards to Lűderitz. In addition to an
upwelling region along the south-western coast, the Southern Benguela ecosystem is
uniquely characterised by a shallow bank region, the Agulhas Bank in the south. This
is the reason for the more abundant and ecologically important demersal and benthic
biota in the Southern Benguela ecosystem compared to “traditional” (and non-
collapsed) upwelling systems (Shannon and Jarre-Teichmann, 1999a, b).
Although fisheries in the Northern and Southern Benguela ecosystems target similar
demersal (Cape hake, Merluccius capensis and M. paradoxus) and pelagic fish
species (sardine, Sardinops sagax, anchovy, Engraulis encrasicolus, horse mackerel,
Trachurus t. capensis), they have experienced different exploitation histories and
environmental perturbations, and contrast in their species compositions, community
structures and abundance trajectories.
Total catches in the Southern Benguela ecosystem have fluctuated around 0.5 million
tonnes since the early 1960s. Since the 1950s and even before then, hake off South
Africa have been targeted by bottom trawlers. Catches of hake increased slowly from
about 50 000 tonnes to about 140 000 tonnes between 1950 and 1977, when a 200-
mile Fishing Zone was proclaimed by South Africa (Payne, 1989), and have remained
relatively stable since. Most of the catch was comprised of sardine from 1950 until
1965, thereafter the fishing industry used nets of smaller mesh size to target anchovy,
which dominated the catches until the mid 1990s, and in the early 2000s, significant
quantities of both small pelagic species have been caught. The sustainability of
catches off South Africa is largely attributable to relatively conservative management
measures, for example pelagic fish catches have been maintained well below 25% of
estimated annual biomass since the early 1990s (Cury et al., 2005a), although the
initialization of the unusually high abundance of both anchovy and sardine off South
Africa in the early 2000s has been attributed to a favourable sequence of short-lived
environmental events (Roy et al., 2001).
Sardine, anchovy and hake off Namibia have been sequentially exploited and
depleted, largely because effective management measures could not be implemented
until Namibia’s independence and proclamation of a 200-mile EEZ in 1990.
Subsequently, there has been a modest recovery of hake catches but sardine have
remained at very low levels. Catches have been dominated by horse mackerel since
the 1970s although there has been a slight decline since the late 1980s. There has been
a steady decline in total catches, which peaked in 1968 at more than 2 million tonnes
and decreased to around 0.5 million tonnes in the late 1990s.
Sardine were abundant off Namibia in the early 1960s, but year-classes were poor
from 1965, whereas catches were still large from 1967–1969, and sardine biomass
thus declined (Crawford et al., unpublished ms). Unlike off South Africa, anchovy
alone did not replace sardine, rather a suite of planktivorous fish, including horse
mackerel, bearded goby Sufflogobius bibarbatus and to a lesser degree anchovy, filled
the previously occupied niche from the late 1970s and early 1980s (Boyer and
Hampton, 2001). Between 1986 and 1991, sardine and hake biomass increased
(Crawford et al., unpublished ms). However, two environmental anomalies occurred
in the Northern Benguela between 1993 and 1995 (a low oxygen event in 1993/4 and
an intrusion of warm water-Benguela Niño-in 1995), and were linked to distributional
shifts in several fish species, poor sardine recruitment, declines to low biomass levels
of most commercial species and reduced catch rates of hake (Boyer et al., 2001),
which migrated offshore between 1993 and 1995 (Hamukuaya et al., 1998), monkfish
(Maartens, 1999) and horse mackerel (Boyer and Hampton, 2001). Concomitant
declines were also observed in top predators such as seals, which, due to starvation,
declined by a third in the mid-1990s (Roux, 1998) and Bank cormorants,
Phalacrocorax neglectus (Crawford et al., 1999).
2.2. Humboldt upwelling system
The upwelling system off central Chile is located in the southern section of the
Humboldt Current System, which is one of the four major eastern boundary
ecosystems of the world. This system supports one of the highest levels of primary
productivity recorded for the open Ocean (1.7 gC/m-2 year-1; Daneri et al., 2000) and
globally significant landings (>4.5 million tons in 1995). Despite this high biological
productivity, the state of exploited stocks is far from healthy (Arancibia and Neira,
2003). In fact, the main target species have been fully exploited or even overexploited
for many years, leading to a series of recent stock collapses, for example of horse
mackerel (1998), red squat lobster and yellow squat lobster (1999), and Chilean hake
(2004).
The Southern Humboldt system off central Chile, as considered in this chapter,
extends from 33ºS to 39ºS and from the coast line up to 30 nautical miles offshore,
covering a total area of approximately 50 000 km2. This geographical unit
corresponds to the “Mediterranean District” and is ecologically independent from the
“Peruvian Province” and the “Austral District” located northward and southward,
respectively (Camus, 2001). The main oceanographic and biogeographic patterns that
characterize the Southern Humboldt are: a rather narrow continental shelf (<30
nautical miles), strongly seasonal upwelling (September to March) and high levels of
primary productivity (Strub et al., 1998; Daneri et al., 2000; Escribano et al., 2004).
Oceanographically, four main water masses are present, which leads to a very diverse
marine environment along the central Chilean coast: Subtropical Surface Water
(STSW), Subantarctic Water (SAW), Antarctic Intermediate Water (AAIW), and
Equatorial Subsurface Water (ESSW) (for a review of the physical and chemical
characteristics of each water mass see Strub et al. 1998). Wind driven coastal
upwelling brings the ESSW to the surface in the coastal zone, causing a persistent and
characteristic shallow oxygen minimum zone (> 0.5 ml O2.l-1). Based on the
correlation between the low frequency coastal modes and the Pacific and Atlantic sea
surface temperature (SST), Montecinos et al. (2003) suggest that the coastal SST
seems to comprise two main large-scale climate processes affecting the Southern
Humboldt. At the inter-annual scale the main source of variability is the El Niño
Southern Oscillation cycle. At the long-term scale, an inter-decadal oscillation occurs
at a basin-wide, and maybe even global, scale.
In terms of the main biological components, the Southern Humboldt sustains a diverse
and productive food web. The phytoplankton group is dominated by large diatoms for
most of the year (Avaria and Muñoz, 1982), while the zooplankton is dominated by
herbivorous copepods and euphausiids. Jellyfish (Hydrozoa) also constitute an
important group in the plankton domain (Palma and Rosales, 1995).
Macrocrustaceans are significant benthic components and some species such as red
squat lobster (Pleuroncodes monodon), yellow squat lobster (Cervimunida johni) and
pink shrimp (Heterocarpus reedi) support important fisheries. The fish community is
dominated by pelagic species. Small pelagic fishes such anchovy (E. ringens) and the
endemic common sardine (S. bentincki) are present at high biomass levels in the
Southern Humboldt and dominate landings. These species feed primarily on
phytoplankton and secondarily on zooplankton (Arrizaga et al., 1993). The horse
mackerel (Trachurus symmetricus) is a major fishery resource in the study area. This
highly migratory species performs large-scale migrations in the Pacific Ocean. Off
Chile, horse mackerel feed mainly on euphausiids (Miranda et al., 1998). The
demersal fish community is dominated by the Chilean hake (Merluccius gayi) both in
biomass and landings. Hake inhabits mid-depth waters (200-400 m), feeds on
euphausiids, galatheid crustaceans and small pelagic fish (Meléndez 1983; Arancibia
1989; Cubillos et al., 2003) and is highly cannibalistic (Arancibia et al., 1998).
The Southern Humboldt ecosystem also represents an independent management unit,
comprising the main fishing ground for the Chilean purse seine and trawling fleets,
both industrial and small scale operations and accounting for approximately 75% of
the total landings in Chile (Neira and Arancibia, 2004; Neira et al., 2004). The
industrial fishery, based on fish and crustacean species, started in the 1940s, when
demersal trawlers targeted Chilean hake (Merluccius gayi). However, landings of this
fleet were significant only from mid 1950s onwards. By the early 1960s, an industrial
pelagic fishery came into operation, targeting small pelagic fishes, mainly common
sardine (Strangomera bentincki) and anchovy (Engraulis ringens). At the same time,
an industrial fleet operated on a medium-sized pelagic fish, namely horse mackerel
(Trachurus symmetricus), landings only becoming globally significant from 1975
onwards.
When expanding the trophic analysis to the whole food web, Arancibia and Neira
(2005) found a significant decrease in the mean trophic level of the catch, which
indicates a likely change in community structure induced by fishing. The current
status and basic ecology of top predators such marine birds, sea lions and cetaceans
are poorly known, but it is likely that their abundances are very low compared to the
period at the start of the industrial fisheries in Central Chile (1940s).
The Northern Humboldt system (Peruvian system) is world famous because it
supports one of the most productive fisheries of the world (Ryther, 1969).
Specifically, during the 1960s and 1970s, it supported the largest single-species
fishery in the world, targeting anchovy (Engraulis ringens). The Peruvian system is
dominated by the dynamics of anchovy and subject to frequent direct environmental
perturbations of the El Niño Southern Oscillation (ENSO). The long-term dynamics
of the Humboldt Current ecosystem off Peru are controlled by shifts between
alternating anchovy (cool) and sardine (warm) regimes that restructure the entire
ecosystem from phytoplankton to top predators (Alheit and Niquen, 2004).
The Peruvian food web, considered to be the northern-central subsystem of the
Humboldt that extends from 4º-14ºS and west up top 60 nautical miles, and covering
approximately 82 000 km2, has previously been modelled (Jarre-Teichmann et al.,
1998). That model represents the period 1973-1981, corresponding to the period
following the collapse of the huge anchoveta fishery of the late 1960s, while sardine
biomass was increasing, and did not span any major El Niño events. The model
considers the main distribution area of small pelagic fish such as anchovy and sardine,
i.e., over the Peruvian continental shelf. This geographic delimitation means that only
part of the biomass of horse mackerel, mackerel, and mesopelagic fish are included,
since these species are distributed farther offshore (Jarre-Teichmann, 1998).
One of the most remarkable features of the Peruvian system is the rise and collapse of
the Peruvian anchovy fishery from 700 thousand tonnes in 1958 to a maximum of 12
million tonnes in 1973 (Walsh, 1981). The evolution in the Peruvian anchovy fishery
was accompanied by marked changes in fluxes in the carbon budget of the food web
(Walsh, 1981). Similar results can be found in Jarre-Teichmann (1998). The
significant drop in anchovy biomass led to a decrease in grazing pressure, allowing
plankton biomass to increase. These changes were accompanied by increased stocks
of sardine and hake, increased carbon loading and sulphate reduction at the
downstream sea bed, and a decline in oxygen and nitrate content of the water column
(Walsh, 1981). Trophic flows in the system decreased in one order of magnitude
between the periods 1964-1971 (anchovy dominated) and 1973-1981 (before the
anchovy collapse), and the flow to detritus from the phytoplankton compartment
increased of two orders of magnitude between the same periods (Jarre-Teichmann,
1998)
2.3. Mediterranean ecosystems of the Catalan and Adriatic seas
The South Catalan Sea (NW Mediterranean Sea) is an oligotrophic area, where
enrichment occurs due to regional environmental events, mainly related to wind
conditions, the existence of a temporal thermocline and a shelf-slope current and river
discharges (Estrada 1996; Salat 1996; Agostini and Bakun, 2002). These episodes
greatly influence the productivity and fishing activity of the area (Agostini and
Bakun, 2002; Lloret et al., 2004), which yields almost half of the total landings of the
Catalan coast (Lleonart, 1990) and which is especially relevant for the reproduction of
small pelagic fishes, mainly the European anchovy (Engraulis encrasicolus).
Moreover, this is also a strategic area for marine vertebrate conservation, sheltering
important colonies of terns and gulls (Zotier et al., 1998; Abelló et al. 2003). Some of
these species forage actively on the marine shelf and find a complementary food
source in the discards generated by the trawling and purse seine fleets (Oro et al.,
1997; Oro and Ruíz, 1997; Arcos, 2001).
Although artisanal gears are still important, most fleets have developed towards a
nearly industrial type of activity fully exploiting continental shelves and upper slopes
of the area, associated with the highest landings and mainly composed of bottom
trawlers, purse seines and longliners. Small pelagic fishes, overcoat sardine (Sardina
pilchardus) and anchovy (Engraulis encrasicolus), constitute the principal component
of the catch in terms of biomass and are mainly caught by purse seiners and bottom
trawlers. Increasing concern about recruitment overfishing is related to the
Northwestern Mediterranean anchovy stocks (Papaconstantinou and Farrugio, 2000).
Moreover, sardine has decreased steadily since the 1980s apparently due to fishing
and environmental factors (Coll et al., 2005; Palomera et al., accepted). Other small
and medium-sized pelagic fish (e.g. horse mackerel Trachurus spp., mackerel
Scomber spp. and sardinella Sardinella aurita) are much less exploited. The demersal
fishery comprises mainly juveniles of several target species, e.g. hake (Merluccius
merluccius), red mullet (Mullus barbatus) and blue whiting (Micromesistius
poutassou), caught principally by the trawling fleet. Growth overfishing affects some
demersal resources because for many species the sizes at first catch are very similar to
those at which the fish recruit (Lloret and Lleonart, 2002; Sardà et al., 2005).
Moreover, the introduction of new fishing procedures such as modern longlines, e.g.
for adult hake, has eliminated the spawning refugia of some species and has lead to an
increasing concern for recruitment overfishing of some demersal stocks (Lleonart and
Maynou, 2003). Large demersal fish (e.g. adult hake) and large pelagic fish (e.g.
Atlantic bonito Sarda sarda, bluefin tuna Thunnus thynnus and swordfish Xiphias
gladius) are caught by longline and troll bait fleets and show low population levels.
Official landings from the area increased dramatically from the early 1960s to the
early 1980s, mainly due to governmental aids to the fishing sector. Marked
fluctuations in landings occurred thereafter until catches progressively declined from
1994 to the present. Total official landings from 2003 were similar to those reached in
the late 1970s. From 1994 to 2003 a decrease of 55% on total official landings has
been observed. This reduction is mainly based on the pelagic fraction. Demersal
landings have been maintained at similar levels since 1983 with a reduction of 18% in
landings and underwent smaller fluctuations over the period of decline in the pelagic
fraction. Pelagic and demersal landings reached similar values for the first time in
2003 (Coll et al., 2006b).
The Northern and Central Adriatic Sea constitutes the widest continental shelf in the
Mediterranean Sea (Pinardi et al., 2006) and is of great value for fishing within the
Italian and the European context (Bombace, 1992; Mannini and Massa, 2000). Owing
to river runoff and oceanographic conditions, nutrient concentration and production in
the Adriatic diminishes from north to south and from west to east (Fonda Umani,
1996; Zavatarelli et al., 1998), where northern parts related with shallow waters and
river runoff are considered eutrophic, the central area is considered mesotrophic and
the southern region, oligotrophic. The area is characterized by a high diversity of
environmental conditions that is translated into a high biodiversity (Ott, 1992).
Numerous studies describe the distribution and abundance of marine fauna and flora
of the Adriatic Sea (e.g. Riedl, 1986; Zupanovic and Jardas, 1989; Jukic-Peladic et
al., 2001). Moreover, it is also a strategic area for marine vertebrate conservation,
sheltering important seabird populations (Zotier et al., 1998; Baccetti et al., 2002) as
well as endangered marine mammals and turtles (Manoukian et al., 2001; Bearzi et
al., 2004).
Small pelagic fish, mainly sardine (Sardina pilchardus) and anchovy (Engraulis
encrasicolus), constituted the principal component of the catch in terms of biomass in
the 1990s and are mainly caught by purse seiners and mid water trawlers (Arneri,
1996; Mannini and Massa, 2000). The demersal fishery is highly multispecific and
mainly comprises juveniles of several target species, e.g. hake (Merluccius
merluccius) and red mullet (Mullus barbatus), caught principally by the trawling fleet.
Invertebrates (cephalopods and crabs) also constitute an important proportion of the
catch.
Important changes in landings have been recorded in the Adriatic, with a dramatic
increase from the mid 1970s to the mid 1980s, mainly due to the increase of small
pelagic fish in the catch. This was followed by marked fluctuations in landings until
catches progressively declined from late 1980s to the present; primarily because of the
decrease in small pelagic fish, especially of European anchovy (Engraulis
encrasicolus) and sardine (Sardina pilchardus) (Cingolani et al., 1996; Azzali et al.,
2002; Santojanni et al., 2003, 2005). Total official landings from 2000 are lower than
those reached in the late 1970s and existing data show a significant decrease in fish
landings, coupled with an increase of invertebrate landings (Coll et al., 2007). Various
target demersal species have been reported to be overexploited (e.g. Papaconstantinou
and Farrugio, 2000; Jukic-Peladic et al., 2001), and significant quantities are
discarded (Pranovi et al., 2000, 2001; Tudela, 2004). Simultaneously, proliferation of
some jellyfish species in the Adriatic Sea since the 1980s has been reported (e.g.
Rottini-Sandrini and Stravini, 1981; Zavodnik, 1991; Arai, 2001; Mills, 2001), in
parallel with the decrease in small pelagic fish and the increase in eutrophication.
Likewise, in the Black Sea, overfishing and eutrophication have been related to
massive jellyfish explosions during the 1970s and 1980s (Daskalov, 2002; Gucu,
2002).
3. METHODS
Data series and selected models available for the Benguela, Humboldt and
Mediterranean regions were compared in terms of indicators quantifying the roles of
small pelagic fish in the respective ecosystems examined.
3.1. Catch and abundance data series
Landings have been compiled for the selected ecosystems and are summarised in the
indicators i) Trophic level of the catch, ii) the Fishing-in-Balance (FiB) index and iii)
the ratio of pelagic:demersal fish in reported landings. Where available, research
survey biomass indices of pelagic and demersal species are used to illustrate how the
pelagic:demersal fish species ratios have changed over time. This was only possible
for the Southern Benguela and South-Central Chile.
3.2. “Static” (“Snapshot”) models
Several available trophic models representing each of the five ecosystems discussed
above are used. To facilitate meaningful comparisons between systems, these models
were standardized according to the methods described by Moloney et al. (2005).
Here, with the aim of exploring the effects of small pelagic fish on different
ecosystems, we select some of these models as a representative and comparable set
capturing the main characteristic periods within each system.
For the Southern Benguela, trophic models of the period 1980-1989 and 1990-1997
are available (Shannon and Jarre-Teichmann, 1999b; Shannon et al., 2003) and an
additional, comparable model of the period 2000-2004 has been developed. For the
Northern Benguela, several models have been constructed (Roux and Shannon 2004;
Shannon and Jarre-Teichmann, 1999a, b; Heymans et al., 2004). For purposes of this
chapter, standardized, updated models have been constructed for the 1960s, 1980s and
1995-1999, and are used to illustrate the main ecosystem changes that have occurred
off Namibia. For the Southern Humboldt ecosystem, models have been constructed
for 1992 and 1998 (Neira and Arancibia 2004; Neira et al. 2004) and more recently,
also for 2004-2005 (Neira in prep.). For the South Catalan Sea, trophic models
calibrated with time series of data and representing 1978 and 1994 have been used,
while in the case of the North and Central Adriatic Sea, models representing the
1980s and 1990s are available (Coll, 2006; Coll et al., 2005, 2006b, 2007).
Indicators derived from the static models and which were selected to assist in defining
the effects of small pelagic fish in the five ecosystems considered, include:
i) Catch/Biomass ratios for small pelagic fish (this is an index of the level of
exploitation and essentially equates to fishing mortality),
ii) Exploitation rate E=F/Z, where F is fishing mortality and Z is total mortality
(natural and fishing mortality combined) for the main commercial fish species in each
system,
iii) Sum of all flows to detritus.
In addition, Mixed Trophic Impact (MTI) analysis (Christensen and Walters, 2004) is
also used to quantify the variation in benthic-pelagic coupling of trophic interactions
in the ecosystems. Two (oldest and most recent) snapshot models from the Southern
and Northern Benguela, Southern Humboldt and the Mediterranean Sea are used and
the squared sum of all trophic impacts from the pelagic compartment on the demersal
one and vice versa, computed and compared by means of percentage variation in the
squared sum of the MTIs between the early and most recent modelled periods. The
sum of all trophic impacts from detritus on the demersal and pelagic compartment is
considered.
3.3. Models fitted to time series data
Models of the Southern Benguela, the South Catalan Sea and South-Central Chile
have been fitted to time series data and are used here to quantify, in ecosystem terms,
the changes in these three ecosystems since the 1970s.
A trophic model of the Southern Benguela ecosystem has been fitted to catch and
abundance time series data for 1978-2002 by means of forcing by fishing effort over
time, and environmental forcing of primary productivity, using flow control
parameters for model tuning (Shannon et al., 2004). This model is being updated for
revised and additional data series (Shannon et al., in prep. a). The ecological model
developed for the South Catalan Sea was fitted with time series of data from 1978 to
2003 and was able to satisfactorily reproduce the dynamics of several target species
considering fishing, trophic interactions and the environment (Coll et al., 2005; Coll,
2006, Coll et al., in prep.). Similarly, an ecosystem model of the Southern Humboldt
has been fitted to time series data from 1970-2004 (Neira et al., in prep.).
The advantage of using fitted models is that they can provide an estimate of the
abundance trajectories of species for which time series data are not available, and can
be used to quantify likely changes in predation mortality as a result of biomass and
fishery fluctuations. Biomass estimates of small pelagic fish and other important
groups are plotted over time using the three fitted time series models.
3.4. Simulations
One “snapshot” (static) model was selected for each of the following ecosystems (see
section 3.2): Southern Benguela (1980s), South Catalan (1994), North and Central
Adriatic Sea (1990s) and South-Central Chile (1992), and two hypothetical extreme
fishing scenarios were simulated to explore whether the effects of small pelagic fish
were similar across the systems and to identify any system specific attributes relating
to the role of small pelagic fish in these ecosystems.
All three models fitted to time series data (see section 3.3) as explained before
(Southern Benguela, South Catalan Sea and Southern Humboldt) showed that wasp-
waist flow control emerges when trying to fit our models to time series data. In the
model scenarios presented here, we adopt a standardized “wasp-waist flow control”
assumption, setting vulnerabilities (v’s, the model parameter describing the
availability of a prey species to a predator, see Walters et al., 1997; Christensen and
Walters, 2004) for wasp-waist control by small pelagic fish: v=1000 for top down
control of small pelagic fish on their plankton prey; v=1 for bottom up control of
small pelagic fish on their predators. These vulnerabilities are applied to trophic
interactions of the main small pelagic fish in the ecosystems considered: for Southern
Benguela simulations, wasp-waist settings were adopted for anchovy, sardine, “other
small pelagic fish” (e.g. flying fish, saury) and redeye; for Southern Humboldt and
Mediterranean simulations, wasp-waist settings are assumed for anchovy and sardine
only. V’s for all other interactions are set to the default v=2 for mixed flow controls.
Simulations are run for an initial 5-year period, during which no alterations to fishing
are simulated (for ease of visualization of model results and extraction of parameter
values in year 1). Two fishing scenarios are subsequently simulated for an additional
15-year period and model results extracted for the final year of simulation. Two main
simulations are performed:
Simulation 1: Closure of fishery on small pelagic fish
For each of the four models, the fishery on small pelagic fish is closed and biomass
trajectories plotted to examine which species benefited or are deleteriously affected.
Changes in the ratios of pelagic:demersal fish biomass are tracked over the simulation
periods.
Simulation 2: Collapse of small pelagic fish
For each of the four snapshot models selected for simulation purposes, the
exploitation rate E (E=F/Z) in year 5, required to collapse anchovy and sardine stocks
by year 16, are compared. Changes in biomass of the main groups responding to the
collapse of anchovy and sardine are plotted over the 15-year simulation period. As
above, pelagic:demersal fish biomass ratios are compared.
4. MODEL RESULTS
4.1 Catch and abundances
The ratio of small pelagic fish to demersal fish catches ranged between 1 and 9 in the
Northern and Southern Benguela, the South Catalan Sea and the North and Central
Adriatic, whereas in the Southern Humboldt, the ratio ranges from 1 all the way up to
60 (if horse mackerel, of which a significant portion are caught in the open ocean, are
included as pelagic fish) and 18 when horse mackerel are excluded (Fig. 3a-c),
reflecting the far greater importance of small pelagic fish in the Humboldt compared
to other fisheries examined.
TL of the catch (Fig. 4a) increased in the 1990s in the Northern Benguela, and from
1999 onwards in the Southern Humboldt, as a result of the collapse of small pelagic
fish, and thus the increase in the FiB index that was observed in these two cases are
misleading as they do not reflect an expansion of the fisheries but rather an underlying
collapse (Namibia) or at least a reduction in catches (Chile) of small pelagic fish. Off
South Africa, the recent short-term decline in the FiB reflects the high abundances of
small pelagic fish, in particular sardine, in the early 2000s, rather than the traditional
“fishing down the food web” situation.
By the late 1970s, horse mackerel became the most important fishery resource off
Central Chile due to the development and later westward expansion of an important
offshore fishery, mainly composed of an industrial purse-seine fleet. Consequently,
landings of horse mackerel have influenced total landings in Central Chile in the last
decades (Fig. 3b). The high landings of horse mackerel during the 1980s and 1990s
also masked the process of fishing down the food web from being detected in the
exploited community inhabiting the continental shelf (Arancibia and Neira, 2005).
Therefore, the indicators are presented with and without including landings of horse
mackerel for the Southern Humboldt ecosystem (Fig. 4b). The TL excluding horse
mackerel shows an increase in 2001, probably due to a combined decrease in landings
of common sardine and anchovy and an increase in landings of hake. The FiB shows
an increasing trend until mid 1990s that reflects the westward expansion of the fleet
targeting horse mackerel (Fig. 4c). Conversely, FiB excluding horse mackerel shows a
decreasing trend since the mid 1980s to minimum (negative) values in late 1990s (Fig.
4c). During early 2000s, both series of FiB (with and without horse mackerel)
increase (Fig 4c), probably owing to high landings of hake during this period.
However, this trend should not be interpreted as ecosystem recovery since Chilean
hake has recently collapsed and it is expected that the trend in FiB will strongly
decline in the next few years.
In the Catalan Sea (Fig. 4c), TL of the catch and the FiB index show the dynamics of
small pelagic fisheries, reflecting the expansion of the fishery and subsequent local
depletion of pelagic fish stocks (Coll et al., 2006a). In the case of the North and
Central Adriatic Sea (Fig. 4c) catch data suggest an increase of the TL of the catch
(due to decrease of small pelagic fisheries during the 1980s and a fishery based on
demersal species) and a following decrease due to increased invertebrate landings
(Coll et al. 2007). From the 1990s the decrease in the FiB indices reflected
deteriorating ecosystems and fisheries.
It is of interest to highlight that simulations of closures of small pelagic fisheries show
that after ten years, the pelagic:demersal biomass ratios increase from around 1 to
over 2.5 in the Southern Benguela, following a steady recovery of anchovy and
sardine over the ten-year simulation period (Fig. 5a). By contrast, the
pelagic:demersal biomass ratios for the South Catalan Sea, the Adriatic Sea and the
Southern Humboldt, which are all higher to begin with (around 5 for Chile and 14 for
the Mediterranean), increase following the pelagic fishery closure, as expected, but
subsequently decline to original levels or below as a result of increased hake biomass
levels in response to increased availability of sardine and anchovy prey (Fig. 5b,c,d).
Previous simulations of the Northern Benguela (Shannon et al., 2001; Roux and
Shannon, 2004) showed that a moratorium on sardine catches would have some
benefit to sardine but only small effects on other groups unless abundance of pelagic
goby was also reduced. These results provide an interesting contrast to those for other
upwelling systems, suggesting that the Benguela may operate differently to the others
examined, possibly because both Southern and Northern Benguela sub-systems have
an additional, largely unfished and abundant small pelagic fish resource (round
herring in the south and pelagic goby in the north, both forage fish species).
Alternatively, it is possible that after the intense exploitation of small pelagic fish in
the Southern Humboldt and Mediterranean systems, the subsequent sudden simulated
release of fishing pressure allows small pelagic fish to increase very fast initially,
whereas at least in the case of the Southern Benguela, small pelagic fish were not too
heavily exploited to begin with. However, in the northern Benguela, the observed
pelagic:demersal catch ratio increased over time as a result of increase in catches of
horse mackerel relative to piscivorous hake. Overall, the ratios indicate a shift towards
greater importance of demersal fish in the Benguela since the 1950s.
When simulating the collapse of small pelagic fish, the pelagic:demersal biomass
ratios decrease in the Southern Benguela, South Catalan Sea and North and Central
Adriatic Sea (Fig. 6) due to the decrease of pelagic biomasses. Decreases of 33% and
46% are observed in the Catalan and Adriatic cases respectively, while the Southern
Benguela shows a smaller reduction in the pelagic: demersal biomass ratio of 25%. In
the Southern Humboldt case, the simulated collapse of small pelagic fish results in a
decrease in the pelagic demersal biomass ratio and in the small pelagic fish/hake
biomass ratio of 25% and 100%, respectively (Fig. 6b).
4.2 Fishing mortality, predation and exploitation rates
Catch/biomass ratios are equivalent to fishing mortality rates and are compared in Fig.
7. Fishing mortalities are smallest in the Adriatic (maximum F = 0.2 y-1 for sardine
and anchovy), and the Southern Benguela (maximum F= 0.3 y-1 for anchovy and
sardine in the 1980s), whereas fishing mortality rates exceeding 0.3 y-1 and 0.5 y-1 are
estimated for anchovy in the South Catalan and Northern Benguela, respectively.
Estimated fishing mortalities are greater than 0.6 y-1 for sardine in the South Catalan,
and F of anchovy and common sardine is estimated to have exceeded 0.7 y-1 in the
Southern Humboldt ecosystem in 1992. It appears that smaller fishing mortalities can
be supported in the systems exhibiting greater biodiversity (shallow bank and
upwelling area of the Southern Benguela; diverse environmental conditions
responsible for diverse habitats in the Adriatic).
Using ecosystem models fitted to time series data to estimate predation mortality rates
on small pelagic fish, it was found that in the Southern Benguela, predators exerted
between 0.6 and 1.2 y-1 predation mortality over the last 25 years, between 0.2 and 1.6
y-1 in the Catalan and are higher, between 0.7 and 1.4 y-1 off Chile (Fig. 8a,b,c). This,
combined with the high fishing pressure on small pelagic fish off Chile, suggests high
total mortality exerted on small pelagic fish in the Southern Humboldt especially
during the late 1990s and early 2000s, and reiterates the fact that model results need to
be considered in the context of species dominance and abundance regimes.
Exploitation rates, equivalent to the ratio of fishing mortality to total mortality
(E=F/Z), are shown in Fig. 9. Sardine exploitation rates are higher in the South
Catalan Sea during the 1980s and 1990s, Southern Benguela during the 1980s and
1990s and Northern Benguela during 1980s and 1995 than in the other periods
modelled per system (Fig. 9a,c). Anchovy in the Southern Humboldt were also
subjected to high exploitation rates in 1998 (Fig. 9c). Exploitation rates registered for
hake and anglerfish in the South Catalan Sea during the 1990s, as well as for mullets
and demersal sharks during the 1980s and 1990s in the Adriatic Sea (Fig. 9e), are
higher than the maximum 0.8 recommended for groundfish stocks (Mertz and Myers,
1998; Rochet and Trenkel, 2003).
In Southern Benguela model simulations, in order to collapse the pelagic fishery
within the 10- year simulation period, fishing mortalities need to be increased by a
factor of 2.5 of the 1980s levels, corresponding to F=0.8y-1 for anchovy and F=0.3y-1
for sardine in that period (Fig. 6a), which corresponded to exploitation rates of 0.57
for anchovy and 0.25 for sardine. Note that the purse seine fishery is modelled as a
single unit so that anchovy and sardine fishing mortalities are not adjusted
independently in these simulations, and thus only provide a very rough guideline of
what would have been required to collapse these stocks at that time.
In the Southern Humboldt model (Fig. 6b), in order to collapse the pelagic fishery
within the 10- year simulation period, fishing mortalities need to be increased by a
factor of 1.7 of the 1992s levels, corresponding to F=0.73 y-1 for anchovy and F=0.77
y-1 for common sardine in that period (with E = 0.25 for anchovy and 0.32 for
common sardine). In this simulation, the purse seine fishery targeting small pelagic
fish is modelled as a single unit, so that anchovy and common sardine fishing
mortalities are not adjusted independently.
In the South Catalan Sea, the pelagic fishery of anchovy and sardine collapse within
10 years of simulation when fishing mortality are hypothetically increased by a factor
of 2, corresponding to an exploitation rate of 0.62 for anchovy and 0.64 for sardine,
with F=1.70 y-1 and F=2.15 y-1, respectively. In the North and Central Adriatic Sea,
fishing mortality is increased by a factor of 2.3 and exploitation rate resulted in 0.78
and 0.79 for anchovy and sardine (F= 1.57 y-1 and F= 1.61 y-1), respectively (Fig. 6c).
These high fishing mortalities may mean that the Mediterranean ecosystems would be
likely to show much higher levels of exploitation than the Chilean and South African
systems (Coll et al. 2006a).
4.3. Gelatinous zooplankton and proliferation of other species
Simulations yield relatively consistent results where gelatinous zooplankton increase
when small pelagic fish stocks collapse and conversely, there is a decrease in jellyfish
abundance when closure of the pelagic fisheries is simulated (Table 1). In Southern
Benguela simulations, macro-zooplankton follows similar trajectories to gelatinous
zooplankton, increasing by 8% when a collapse of the purse seine fishery is
simulated, and declining to 68% of original levels when the purse seine fishery is
closed. Phytoplankton biomass remained unchanged. In the case of the Catalan Sea,
jellyfish increase when a collapse of the small pelagic fishery is simulated, while there
is also an increase in micro-mesozooplankton and macrozooplankton of 21% and
35%, respectively. On the contrary, the model simulation predicts an 8% decrease in
phytoplankton biomass. Similarly, in the North and Central Adriatic Sea, simulations
suggest an increase in jellyfish biomass when small pelagic fisheries collapse, while
micro-meso and macrozooplankton show an increase of 18% and 2%, respectively.
Phytoplankton biomass decreases by 5% in the Adriatic. Similar results were found
by Roux and Shannon (2004) when a hypothetical fishery on jellyfish was modelled,
in that anchovy and several predatory fish species were favoured when 50% of
gelatinous zooplankton production was “removed” through “fishing”.
Simulations also show the proliferation of other species when small pelagic fish
stocks collapse (Fig. 6). Both ecological models from the Catalan and Adriatic Sea
highlight the increase in abundance of other small pelagic fish and benthopelagic fish
(Fig. 6a). Similar results were also seen when fitting the models to time series of data
(Fig. 10). In the South Catalan Sea (Coll et al., 2005, Coll et al., in prep.) a general
decrease in the biomass of small pelagic fishes was predicted in parallel with an
increase of the biomass of bentho-pelagic fish, cephalopods, as well as jellyfish, all of
them showing important fluctuations in terms of abundance (Fig. 10c).
Table 1. Ratio of biomass of gelatinous zooplankton groups in year 15 compared to
year 1 (expressed as a percentage) when a collapse of small pelagic fisheries is
simulated (scenario 1) and when closure of small pelagic fisheries is simulated
(scenario 2).
Scenario S. Benguela S. Catalan Adriatic S. Humboldt
1. Collapse 108% 164% 118% 109%
2. Closure 76% 32% 75% 16%
4.4. Effects of small pelagic fish on top predators
In the southern Benguela, simulation of a collapse in small pelagic fish suggest severe
declines in large pelagic fish (48% reduction in biomass), seals (17% decline), birds
(33% decline) and cetaceans (27% decline). On the contrary, model biomass of seals,
seabirds, cetaceans and large pelagic fish predators all increase (by factors of between
1.5 and 2.2 of original levels by year 15) when closure of the South African purse
seine fishery is simulated. In the Southern Humboldt simulation of small pelagic
fishery collapse, seabirds collapsed and sea lions decline to 29% of original values,
whereas simulated closure of the fishery suggests huge increases in seabirds and sea
lions, by a factor of 9 and 12 respectively over the 15 year simulation period.
Similarly, in the South Catalan Sea, seabirds declined to less than half their biomass,
and totally collapsed in the North and Central Adriatic. The ecological model of the
South Catalan Sea also highlights that the decline of small pelagic fish biomass occurs
in parallel with a decrease of abundance of demersal and pelagic predators such as
European hake, anglerfish, demersal sharks and large pelagic fish (Fig. 10c). This
could exemplify the importance bottom-up flow control on predators by their small
pelagic fish prey.
In the case of the South Catalan Sea, however, seabirds have shown an increase in
abundance since the 1980s, even though the fishing effort (and thus bycatch) has
increased in the region. This is also partially reproduced by the model fitted to data
through a mediation function (Coll et al. 2005; Coll et al. in prep.) (Fig. 10c) and it is
mainly due to the increase in discards from trawling and the protection of breeding
colonies in the area since the beginning of the 1980s, which compensated for a
decrease in forage fish available on the continental shelf (Oro, 1996; Oro et al., 1996;
Oro and Ruíz, 1997). In the Southern Humboldt, simulations suggest that when small
pelagic fishing is stopped, small pelagic fish increase in biomass, followed by a rapid
increase in the biomass of sea lions, marine birds and Chilean hake. By comparison, a
simulated collapse of small pelagic fish is followed by a sharp decline of the same
groups, reflecting the role of small pelagic fish as important drivers of ecosystem
dynamics.
4.5 Flows to detritus
From the snapshot models it appears that flows to detritus tend to increase when small
pelagic fish biomass declines. In the Northern Benguela, total flow to detritus was
lower in the earlier period (1960s), before small pelagic fish had collapsed (Fig. 11a).
Similarly, in the Southern Humboldt, pelagic fish declined in the 2000s and this was
the period for which flows to detritus were highest (Fig. 11b). By comparison, there
was little change in the total flows to detritus in the three periods examined in the
Southern Benguela (Fig. 11a), although total flows to detritus were marginally smaller
in the recent period when pelagic fish abundance was exceptionally high. Nor were
their marked differences between flows to detritus in the two periods considered for
the South Catalan or the Adriatic Sea (Fig. 11c).
The general trend of reduced flows to detritus when small pelagic fish are abundant
was less well illustrated through simulations, probably as a result of possible model
competitor release of other small pelagic fish or mesopelagic fish when anchovy and
sardine decline. In fact, flows to detritus increased slightly when closure of the small
pelagic fishery of the South Catalan, North and Central Adriatic and Southern
Benguela ecosystems were simulated (Table 2). By comparisons, the Southern
Humboldt simulations suggested that flows to detritus decreased to 76% when the
pelagic fishery was closed (and pelagic fish abundance increased), and increased
slightly when the modelled pelagic fishery collapsed anchovy and sardine stocks
(Table 2). Overall, standardized snapshot models revealed that flows to detritus were
three times larger off Chile than in the other ecosystems considered, reflecting the
high productivity of this ecosystem in comparison to the others.
Table 2 Ratio of total flows (all combined) to detritus in year 15 compared to year 1
(expressed as a percentage) when a collapse of small pelagic fisheries is simulated
(scenario 1) and when closure of small pelagic fisheries is simulated (scenario 2).
Scenario S. Benguela S. Catalan Adriatic S. Humboldt
1. Collapse 99% 95% 97% 102%
2. Closure 100% 113% 108% 76%
Differences between ecosystems were found in the sum squared of all trophic impacts
of detritus on the demersal and pelagic compartments. In the Southern and Northern
Benguela and South Catalan Sea, the sum squared of the mixed trophic impacts of
detritus on the demersal compartments increased over time, while in the Adriatic Sea,
this measure declined (Table 3). The sum squared of the mixed trophic impacts of
detritus on the pelagic compartment increased in the case of the Southern Benguela
and the Mediterranean Sea case studies. In the southern Humboldt models, no changes
were observed in the impacts of detritus on the demersal groups. On the other hand, a
small increase in the impacts of detritus on pelagic groups was observed (Table 3).
The likely explanation for these results is a strong decrease in the biomass of the main
demersal fish species in the system (hake) and the low biomass levels of detritivorous
groups such red squat lobster and yellow squat lobster in the most recent model.
Table 3 Variation (%) of the sum (squared) of all trophic impacts of detritus on the
demersal and pelagic components, derived from the Mixed Trophic Impact analysis of
snapshot models of Southern and Northern Benguela, Southern Humboldt and
Mediterranean Sea case studies.
Scenario S. Benguela
(early 2000s
compared to
1980s)
N. Benguela
(1960s
compared to
late 1990s)
S. Catalan
(1994
compared
to 1978)
Adriatic
(1990s
compared
to 1975)
S. Humboldt
(2004-05
compared to
1992)
1.
Detritus-
demersal
252.5% 52.8% 6.0% -30.7% 0.0%
2.
Detritus-
pelagic
246.6% -32.7% 7.5% 13.8% 6.7%
4.6 Coupling demersal-pelagic compartments
Aggregated MTI analysis was also used to quantify the changes in the mixed trophic
impacts for demersal and pelagic compartments. In the Southern Benguela, Catalan
and Adriatic Sea, the sum of all mixed trophic impacts of the pelagic compartment on
the demersal one increased over time (and in the Mediterranean case, with increasing
fishing pressure), while the demersal impacts on the pelagic compartment decreased
in the Southern and Northern Benguela, Southern Humboldt and Catalan Sea, but
showed little change in the Adriatic (Table 4). The collapse of the pelagic ecosystems
in the northern Benguela and the recent collapses of horse mackerel, squat lobsters
and hake in the Southern Humboldt are exemplified by the noticeable decreases in
demersal-pelagic MTIs.
Table 4 Variation (%) of the sum (squared) of all trophic impacts of the pelagic
component on the demersal component, and vice versa, derived from the Mixed
Trophic Impact analysis of snapshot models of Southern and Northern Benguela,
Southern Humboldt and Mediterranean Sea case studies.
Scenario S. Benguela
(early 2000s
compared to
1980s)
N. Benguela
(1960s
compared to
late 1990s)
S. Catalan
(1994
compared
to 1978)
Adriatic
(1990s
compared
to 1975)
S. Humboldt
(2004-05
compared to
1992
1. Pelagic
on
Demersal
32.2% -15.2% 4.8% 70.0% -32.0%
2.
Demersal
on Pelagic
-18.7% -50.7% -19.6 0.5% -36.0%
5. DISCUSSION
5.1. Trophic flow controls, fishing and environment
An ecosystem model of trophic flows in the Southern Benguela was fitted to time
series data from 1978-2002 (Shannon et al., 2004b) and is currently being revised and
improved by incorporation of updated and revised time series (Shannon et al., in prep.
a). These studies support the findings of a hypothetical simulation study (Shannon et
al., 2004a) showing that off South Africa, environmental factors have been more
important drivers of ecosystem dynamics than fishing over the latter part of the 20th
century, explaining up to 23% of observed variability in the major ecosystem
components examined (Shannon et al., in prep. a). In particular, model simulation
studies suggest that environmental forcing changing the relative availability of
mesozooplankton to anchovy and sardine may be a key factor in driving changes in
the abundance of small pelagic fish in the southern Benguela (Shannon et al., 2004c).
These mechanisms and their physical forcings are still being explored in more detail
(Shannon et al., in prep. b). As mentioned earlier, Verheye et al. (1998) found both
bottom-up and top-down effects of small pelagic fish on zooplankton off the South
African west coast. The latter model result would be a case for bottom-up control of
small pelagic fish. Shannon et al. (2004b) found that model parameterisation
describing prey vulnerability to predators accounted for over 40% of the observed
variability in the time series examined, and suggested clear wasp-waist flow control
by small pelagic fish as a characteristic of this upwelling system.
A model representing the Southern Humboldt upwelling system in the year 1970 was
fitted to available time series of relative biomass, catch and fishing mortality for the
period 1970 to 2004 (Neira et al., in prep.). Fishing mortality explained 28% of the
variability in the times series, whereas vulnerability (v) parameters estimated using
EwE explained an additional 21%. When a function affecting primary production is
calculated by Ecosim to minimize the Sum of Squares (SS) of the time series, a
further 11% to 16% of variability is explained. The best fit model indicated that a
long-term change in primary production might have affected the dynamics of groups
in the Southern Humboldt system since no statistical evidence was found to support
the null hypothesis that all of the deviations between model and predicted abundances
are due to chance alone (p value<0.05), indicating that there is a consistent pattern in
the deviations. This result is reinforced when the primary productivity anomaly
proposed by the model is compared with independent time series of sea surface
temperature and an upwelling index in the system for the period 1970 to 2000 (Neira
et al., in prep). The fitting process revealed that changes in the SS are sensitive to,
amongst others, trophic relationships involving common sardine and anchovy as
predators, but not as prey, in agreement with the hypothesis of wasp-waist control in
upwelling ecosystems (Cury et al., 2000; Cury et al., 2005b). Although the
combination of v values for the best fit model seems to indicate a pattern in terms of
small pelagic fish controlling their prey (top-down), bottom-up control of small
pelagics on their predators was not as clear, which could be related to the lack of time
series for top predators. However, independent analysis indicates that in last 15 years
the biomass of hake was positively and significantly correlated to the biomass of
small pelagic fish (likely bottom-up control; Neira et al., 2006). Using Generalized
Linear Models, these authors show that the only explanatory variable affecting the
biomass of small pelagic fish in last 15 years is sea surface temperature (S. Neira,
University of Cape Town, South Africa, unpublished data; Neira, in prep.). The above
results are in agreement with the hypothesis of wasp-waist where the dynamics of
small pelagics are not controlled by predation (hake biomass and fishing mortality) or
food availability but are rather affected by environmental variability.
When fitting the ecological model of the South Catalan Sea to available time series of
data (Coll, 2006; Coll et al., 2005, Coll et al., in prep.) similar results were found.
Trophic interactions accounted for half of the observed data variability, while fishing
and the environment had similar contributions (approximately 7%) to explaining the
variability in time series data. Moreover, small pelagic fish were found to be exerting
wasp-waist (sardine) and bottom-up (anchovy) flow control, also in line with previous
hypotheses. The function affecting primary production calculated by Ecosim to
minimize the Sum of Squares of the time series was significant, and later negatively
correlated with sea surface temperature and the NAO index.
Therefore, configuration of the trophic web seems to play a major role in explaining
the dynamics of marine ecosystems and small pelagic fish, and its modification by
fishing and the environment can have important impacts on the whole ecosystem. The
synchrony in the dynamics of small pelagic stocks around the world (Kawasaki, 1983;
Lluch-Belda et al., 1992) may mean that the link between environmental and
ecosystem change could be less complex than initially expected (the environment is
acting either directly on small pelagic fish or their main food, and through small
pelagic fish these effects are propagated up and down the food web). On the other
hand, the effects of overexploiting small pelagic fish could lead to dramatic and
possibly even irreversible ecosystem change, since collapse due to overfishing small
pelagic fish can exacerbate “natural” fluctuations induced by the environment. For
example, there has been a drastic change in the pelagic ecosystem of the Northern
Benguela since the 1980s (Bakun and Weeks, 2004), including a collapse of anchovy
and sardine stocks and proliferation of jellyfish, as a result of a series of unfavourable
environmental events which have been exacerbated by heavier fishing than was in fact
sustainable at the low stock biomasses at the time (Boyer et al., 2001). Similarly, in
the Black Sea (Daskalov, 2002) a regime shift has been described in relation to both
overexploitation (causing a trophic cascades down the food web), and eutrophication,
and a collapse of small pelagic fish has been followed by the proliferation of
jellyfishes. However, other factors may account for jellyfish outbreaks, such as the
beneficial impacts of bottom trawling to benthic-spawning jellyfish. Mills (2001) has
reported outbreaks of new non-indigenous jellyfish species in certain areas linked to
changes in climatic conditions.
5.2. Generic effects of fishing on small pelagic fish
Frank (2006) showed a north-south geographical gradation in flow controls in the
North Atlantic, with more productive and diverse ecosystems better able to deal with
top-down perturbations (such as fishing) and instead rather showing stronger bottom-
up influences, whereas he showed that top-down effects are large in less productive
and less diverse ecosystems of the northern North Atlantic. Carr (2002), when
examining productivity of eastern boundary current ecosystems, found a mismatch
between the estimated fish yield (given productivity estimates in these upwelling
ecosystems) and the reported landings of small pelagic fish, suggesting that the
trophic structure of upwelling ecosystems differ from one another. In particular, Carr
(2002) contrasted the high productivity of the Benguela and the lower productivity of
the Humboldt, noting that small pelagic fish production was much higher in the
Humboldt than in the Benguela ecosystem. Nevertheless, our model comparisons
seem to suggest the overarching commonality of upwelling systems being wasp-waist
controlled. The major coastal upwelling systems are characterized by variability in
their chemical-physical conditions over a wide range of spatial and temporal scales
(Hill et al., 1998) (and, to a lesser extent, also the Mediterranean, Bosc et al., 2004).
Individuals, populations and food webs respond in different ways to this variability.
On the other hand, fishing has more generic effects on populations and communities
such as decreasing trophic level and size structure of populations and exploited
communities (i.e., Pauly et al., 1998). Therefore, despite the importance of different
environmental drivers in each system, we expect that the “generic” effects of fishing
in driving changes in the systems analysed could be comparable given the common
wasp-waist ecosystem structure pivoting around small pelagic fish. In particular,
strong changes in the abundance of small pelagic fish (populations located in the
waist of the food webs where they occur, see introduction), induced by fishing, could
have comparable effects on ecosystem structure and function.
Models analyzed in this study show how a decrease in small pelagic fish abundance
will have important effects on both higher and lower trophic levels of the food web,
causing a decrease in predators and the proliferation of other species that are preys or
competitors. Changes in small pelagic fish disrupt energy flows, which could result in
an increase in flows to detritus, demersal processes within the system becoming more
important and stronger coupling of pelagic to demersal trophic compartments.
In addition, the collapse of small pelagic fish could lead to a change in the kind of
trophic control in a food web, for example from the generic wasp-waist control
characteristic of several upwelling ecosystems, to a system that is more bottom-up
influenced by the environment or by replacement of opportunistic species that benefit
from excess plankton production but do not transfer this production to upper trophic
levels, either because they are not widely edible (i.e., jellyfish) or because their
bathymetric distributions (e.g. of mesopelagic fish) make them inaccessible to
predators with limited diving capacity (seabirds). Modelling can improve our
understanding of these changes although admittedly we are only beginning to
understand how fishing changes the structure and functioning of ecosystems.
5.3. Proliferation of species
The simulations explored in this chapter suggest that jellyfish may proliferate when
small pelagic fish are heavily fished (Table 1). In the four models used for simulation
purposes, jellyfish biomass increased after modelled small pelagic stocks were
collapsed. The proliferation of gelatinous zooplankton is linked not only to the
availability of a trophic niche, but also to their higher turnover rate (and possibly also
environmental conditions). Fishing, by disturbing the structure and functioning of
marine ecosystems, tends to result in communities dominated by small bodied and
rapidly reproducing species. According to Odum (1985), in stressed ecosystems it is
expected that a decrease in K-selected species will be followed by an increase in
opportunistic r-selected species. Therefore, classic food web analysis based on trophic
relationships may not be sufficient to analyze extreme scenarios such as ecosystem
collapse. The effect of turnover rate of functional groups should also be taken into
account when modelling and analyzing strong ecosystem changes (Leibol et al, 1997).
Further understanding of these processes is essential to predict jellyfish outbreaks,
which are of high concern in tourist areas.
Although there is not empirical data available, the fitted South Catalan Sea model
shows that some non target species could have also proliferated in the area. This
would be the case for benthopelagic fish, due to the decline of competitors (e.g. small
pelagic fish) and predators (e.g. demersal fish) and increased availability of prey (e.g.
phytoplankton). The Alboran Sea, Southwestern Mediterranean, has shown a
proliferation of boarfishes Capros aper (Linnaeus, 1758) after the collapse of small
pelagic fisheries due to high fishing intensity and environmental changes (Abad and
Giraldez, 1990). Improved understanding of these processes is of special interest for
fisheries and coastal management.
Simulation results also show that changes on small pelagic fish abundance have
important impacts on other zooplanktonic species and support the idea that pelagic
fish exert top-down control on their zooplanktonic preys (Cury et al., 2000).
5.4. Effects of small pelagic fish on top predators
Fluctuations of small pelagic fish have an important impact on predator populations,
as can be seen from model simulations that illustrate the importance of these
organisms as prey for demersal and pelagic feeders such as tunas, seabirds, marine
mammals and groundfish predators.
In the southern Benguela, a system in which marine mammals and birds are relatively
abundant, a simulated collapse of the small pelagic fish suggests severe declines in
large pelagic fish, seals, birds and cetaceans. In addition to “simple” direct predator-
prey effects that have been modelled are other indirect influences; African penguin
breeding success has been found to be significantly related to fish prey abundance
(Crawford et al. 2006), and the proportion of penguins choosing to breed in any
particular year has also been found to be prey related (Crawford et al. 1999).
In the case of the South Catalan Sea, top predators feeding on small pelagic fish (e.g.
hake, anglerfish and dolphins) also show decreasing biomass when these prey
organisms collapse. However, seabirds have shown an increase in abundance due to
the increase of discards, as already discussed, highlighting the indirect effects of
fishing. A moratorium on trawling activities in the Catalan Sea affected populations
of seabirds due to reduced food availability during the breeding season (Oro et al.,
1996).
Moreover, and not yet considered in ecological modelling studies such as the
simulations presented in this chapter, it is not only the quantity of food available to
predators that is an important factor affecting trophic mechanisms up the food web,
but also the quality of that food. Not only do predators and prey need to overlap in
time (Cushing’s [1990] match/mismatch hypothesis) and in space, but the quality of
the prey needs to be of a suitable quality (Beaugrand et al., 2003). For example, in
2004, the common guillemot (Uria aalge), which usually feeds on sandeel
(Ammodytes marinus) during its breeding season, fed sprat (Sprattus sprattus) to its
chicks; breeding success was poor and the chicks produced were in poor condition
(Wanless et al., 2005). Although daily food intake by the chicks in 2004 did not differ
from previous years, the nutritional content of sprat was found to be much lower than
that of sandeel, pointing to food quality as an important factor in seabird breeding
success (Wanless et al., 2005). Changes in the availability of essential fatty acids has
been shown to have drastic effects on fish population dynamics, as they contribute to
regime shift effects on fish populations (Litzow, 2006). Environmentally-induced
decreases in availability of lipid-rich fish to seabirds can also justify dramatic declines
in number of breeding marine kittiwakes (Kitaysky et al., 2006). Another example is
the Alaskan Steller sea lion (Eumetopias jubatus). Sea lion pups have been found to
starve in times when alternative prey such as gadids appear to be abundant, because
the energy density and digestibility of gadid prey is low, whereas forage fish are a
high energy source that is more digestible (Winship and Trites, 2003). Pup mortalities
increased when South American sea lion adjusted their diets and maternal attendance
patterns in response to El-Nino-induced annual changes in the abundance and
distribution of fish prey (Soto, 2006). Following the 1970s Pacific Decadal
Oscillation regime shift, walleye pollock Theragra chalcogramma, a lipid-poor
species, increased in abundance, while capelin Mallotus villosus, a lipid-rich species,
declined.
Changes in stock sizes of small pelagic fish are often associated with shifts in the
geographical distribution of these fish (Lluch-Belda et al., 1989). This has been found
to be true of anchovy (Barange et al., 1999) and sardine (Janet Coetzee, MCM, South
Africa, pers. comm.) off South Africa; their distributions are expanded at large stock
sizes. Thus, small pelagic fish cause, or at least themselves are associated with shifts
in the distributions of several other ecosystem components, in particular their
predators. This is particularly well illustrated off southern Africa, where changes in
the distribution of small pelagic fish, and therefore also the availability of prey to
predators such as seabirds, have been observed. There has been an eastward shift in
the distribution of pelagic fish resources off South Africa (van der Lingen et al.,
2006), which has led to a large reduction in size of the African penguin colonies along
the South African west coast as a result of severely reduced availability of prey to
land-bound breeders (Crawford, 2006). The eastward distributional shift of small
pelagic fish in the southern Benguela in recent years has been matched by a similar
southward geographical shift in west coast rock lobster (Mayfield and Branch, 2000),
attributed to large scale environmental forcing (Cochrane et al., 2004). Off Namibia,
there has been a northward distributional shift on seals and seabirds such as African
penguins between the early 1980s and the 2000s, which is concurrent with northward
contraction of anchovy and sardine spawning stocks in that region (van der Lingen et
al., 2006).
Unfortunately, no biomass/abundance time series for top predators such as marine
birds and marine mammals are available off central Chile. Therefore, the effects of
changes in the abundance of small pelagics in their populations are practically
unknown. Off Peru, changes in population size of guano-producing seabirds
(cormorant, Phalacrocorax bougainvillii; booby, Sula variegata; pelican, Pelecanus
thagus) could be a response to changes in primary and secondary production of the
Peruvian upwelling system, likely mediated by anchovy (Jhanke et al., 2004). Using a
modelling approach, these authors indicate that seabirds would have consumed 14.4%
of the available anchovy resource during the period prior to the development of the
fishery targeting anchovy. Once the fishery was in full operation, seabirds only
accessed 2.2% of the available anchovy resource (Jhanke et al., 2004)
5.5. Increased pelagic-benthic coupling and flow to detritus
Benthic-pelagic coupling is viewed as an important process in highly exploited
ecosystems. For example, this was found to be important in the Namibian upwelling
ecosystem after depletion of stocks due to industrial fishing and environmental events,
an important feature that appears to set this system apart from other upwelling
ecosystems (Moloney et al., 2005). The Namibian region shows some similarities
with the South Catalan Sea (Coll et al., 2006a), and this is also characteristic of highly
fished temperate regions (Sánchez and Olaso, 2004).
Results from the North and Central Adriatic Sea model also highlight the importance
of coupling between the pelagic and demersal compartments in that ecosystem,
mainly due to the link between detritus and benthic and pelagic invertebrates (Coll et
al., 2007). This is likely explained by the shallow waters and the oceanographic
features of the area (Ott, 1992). For example, zooplankton production that is directed
to detritus is high and has an impact on benthic production, underlining the
importance of pelagic production for the maintenance of benthic production within
the ecosystem (Ölscher and Fedra, 1977; Ott, 1992). Moreover, benthic invertebrates
are partially fished but there is an overall low use of their production, which is also
converted into detritus, favouring zooplankton dynamics further. This also indicates
the importance of detritus from the benthic compartment in favour of planktonic
production (Giordani et al., 1992).
The Humboldt system, comprised by the northern (Peru) and southern (Chile) sub-
systems, is probably the largest in terms of size when compared to other upwelling
systems (Jarre-Teichmann and Christensen, 1998; Neira et al., 2004). In addition, this
system has probably exhibited the most pronounced changes in system size after the
collapse of the anchovy stock off Peru, and horse mackerel off Chile. After the
collapse of anchovy, the Peruvian system became similar to the northern Benguela
system, the latter decreasing in size from the mid-1970 to the early 1980s due to the
strong decrease of small pelagics (mainly sardine), which was not compensated for by
the increased abundance of horse mackerel (Jarre and Christensen (1998). The simple
simulations examined here suggest that reducing small pelagic fish abundance will
most likely result in an increase in flows to detritus, probably due to the disruption of
energy transfer from low to high trophic levels (i.e. excess primary production that is
not efficiently transferred up the food web). These results are in line with Peruvian
ecosystem (Northern Humboldt) (Walsh, 1981) where trophic flows to detritus from
1966 to 1979 were seen to increase due to overfishing of anchovy. Therefore, flows to
detritus may be of importance and could be seen as a measure of increasing pelagic-
benthic coupling.
The increase in flows to detritus in the Mediterranean was smaller than in other
ecosystems analysed, most probably due to the fact that fluctuations of small pelagic
fish abundances are smaller in the Mediterranean and that this area has a history of
being heavily fished (Margalef, 1985; Pauly et al., 1998).
5.6. Enhancing catches of commercially valuable predatory fish by reducing
small pelagic fish catches?
Simulation of closed small pelagic fisheries in the Southern Benguela suggests that
higher demersal fish biomasses would be unlikely to be supported despite the
increased abundances of forage fish (Fig. 5a). By comparison, closed small pelagic
fisheries in the South Catalan, North and Central Adriatic and Southern Humboldt
models suggest that larger stocks of demersal fish, especially hake, would be
supported (Fig. 5b,c,d), thus benefiting the demersal fisheries. This was especially
noticeable in the Chilean case, where the potential benefits of closing the small
pelagic fishery appear to be larger, and projected model hake biomass increases
almost nine-fold (compared to 3-4-fold increases in hake biomass in the Catalan and
Adriatic models respectively). As the demersal fishery is of greater economic
importance in the Mediterranean areas than the small pelagic fisheries, temporal
closure of the small pelagic fish fishery could be economically beneficial. However,
formal simulations based on sound economic data would need to be carefully
designed and examined to analyze this. Specifically, in these simulation results,
demersal groups might benefit from an increase in small pelagic fish provided their
own fishery is kept at a constant level during the simulation period, suggesting that
benefits of increased small pelagic fish abundance may only be reaped if the predator
stocks are also sustainable managed (or maintained at healthy levels, in the case of
charismatic species).
As previously mentioned (section 4.1), the Benguela ecosystems (north and south)
differ from the others by also supporting large stocks of a third abundant small
pelagic, namely round herring in the Southern Benguela and pelagic goby in the
Northern Benguela. It is unlikely that round herring and pelagic goby are strong
competitors with anchovy and sardine for zooplankton food as they exhibit different
feeding behaviours. Tanaka (2006) found that feeding behaviour of filter-feeding
Japanese anchovy, and thus zooplankton composition in its diet, differs from that of
particulate-feeding Pacific round herring and Japanese jack mackerel in the East
China Sea, bringing about a certain degree of trophic partitioning in this pelagic
ecosystem. Round herring off South Africa feed on different species and sizes of
zooplankton to anchovy and sardine (Wallace-Fincham, 1987; C. van der Lingen,
MCM, South Africa, pers. comm.). Diet analyses of pelagic goby off Namibia have
recently shown that this species can feed on macrobenthos as well as on zooplankton
in the water column (J.-P. Roux, NMFR, Namibia, pers. comm.). However, despite
the largely limited competition for food amongst these small pelagic fish, model
simulations suggest an indirect effect of anchovy and sardine on other small pelagic
fish, possibly through predator niche overlaps.
In the closed pelagic fishery simulation using the Southern Benguela model, the round
herring stock declines to a mere 13% of its original 1980s level, and the “other small
pelagic fish” group is reduced to 28% of starting biomass, in response to competition
with the expanding populations of anchovy and sardine. In addition, the Southern
Benguela ecosystem also differs from the Catalan, Adriatic and Humboldt ecosystems
by supporting relatively large stocks of large, predatory pelagic fish, in particular
snoek. Trophodynamic responses of the latter to a closed purse seine fishery may
explain the apparent lack of favourable effects on demersal predatory fish species
when the modelled purse seine fishery is closed, given that projected large pelagic
fish biomass increased by a factor of 2.3 over the ten year simulation period (Fig. 5a).
It is also probable that in the Southern Benguela, the simulated biomass of small
pelagic fish and thus also some of their predators do not increase substantially when
the model purse seine fishery is closed because small pelagic Fishing mortalities were
relatively low to begin with (F of around 0.3 y-1), compared to Fs of anchovy and
sardine in the Mediterranean and Chilean models. Another relevant factor to consider
is how heavily fished hake are in the various ecosystems. In the Southern Benguela,
the exploitation rate of hake was between one quarter and one tenth of that in the
Chilean and Mediterranean systems (Fig. 9), so this would not lend support for the
argument that hake are more heavily fished in the Benguela and thus less likely to be
able to respond to increased forage fish abundance. A final point of consideration
must be the relative importance of small pelagic fish in the diets of hake and other
predatory fish in the different modelled ecosystems. In the Southern and Northern
Benguela, small pelagic fish comprise around a third of the diet of hake, and even less
than this in the 1980s model of the Southern Benguela (before both anchovy and
sardine were abundant in the early 2000s). On the other hand, large pelagic fish such
as snoek are estimated to be relying on anchovy and sardine for 30-40% of their diet
off South Africa. By comparison, hake in the Mediterranean and Humboldt
ecosystems are estimated to fill 50-60% in the Mediterranean (see Stergiou and
Karpouzi, 2002 for a review) and between 30 and 50% of their diet composition with
small pelagic fish.
6. SMALL PELAGIC FISH AS INDICATORS OF ECOSYSTEM COLLAPSE?
6.1 Ecosystem Indicators
By comparing ecosystem indicators between systems in different time periods when
the ecosystems were considered to have functioned “normally” or at least to have
been sustainably fished, to those that have been over-exploited or that have collapsed
because of the synergistic effects of the environment and exploitation, we examined
the values/trends exhibited by overexploited ecosystems. Ideally, we would have liked
to be in a position to propose levels/ ranges/ limits of indicators which should be
avoided when managing systems that are not yet overexploited/collapsed.
Exploitation rates applicable to certain kinds of fish, such as small pelagic fish, may
be one of the better examples available. However, most indicators, especially those
quantifying trophodynamics, are largely still descriptive and reference points are yet
to be agreed upon. Cury et al. (2005a) concluded that a suite of trophodynamic
indicators is needed to track complex fisheries and ecosystem changes and that,
although helpful in understanding ecosystem and fisheries dynamics that arise as a
result of interactions between species, these kinds of indicators tend to respond
relatively slowly to structural change. Instead of trying to propose values and limits
for indicators, Garcia and Staples (2000) propose focussing on how indicators can be
implemented in fisheries management to minimize the adverse effects of fishing.
There is currently much effort being put into development of “indicator dashboards”
that attempt to bring together information and management guidance based on
indicators derived from a variety of sources (Shin, 2006).
Ecological modelling is a key tool to monitor and quantify proposed indicators, as has
been illustrated by virtue of trophic models considered in this chapter. However,
models rely on sufficient high quality data, and the need for real time sampling
integrated at the level of ecosystem-based management of marine ecosystems has
been strongly recognized (Shannon et al., 2006).
6.2 Recommended exploitation rates
Managing fisheries by maintaining fishing mortality (Fmax) to achieve maximum
sustainable yield (MSY) is not necessarily applicable to small pelagic fisheries
because recruitment is likely to decline at such reduced stock sizes as those under
Fmax, leading to stock collapse (Patterson 1992). Patterson (1992) analysed 28 pelagic
fish stocks comprising 11 species, fitting a model to 10-year periods of fishing to
estimate the likelihood of stocks declining at different exploitation levels. For mature
fisheries and assuming that small pelagic fish stocks from temperate and tropical
systems behave in a similar way, Patterson (1992) estimated a 50% probability of
stock decline at an exploitation level (E=F/Z where F is fishing mortality and Z is
total mortality) of 0.4. On a decadal scale, he found E>0.5 to be associated with stock
decline whereas E<0.3 allowed stocks to recover.
Taking into account Patterson’s (1992) E=0.4 target reference point for pelagic fish,
and Clarke’s (1991) finding that target fishing mortality rate calculated on the basis of
life history parameters approximated natural mortality (i.e. E=0.5), Rochet and
Trenkel (2003), in their review of community indicators that measure the impacts of
fishing, considered E=0.5 to be the limit reference point above which stocks should be
considered over-exploited. Mertz and Myers (1998) presented a simplified
formulation for calculating fish production, showing that yield/production is
approximated by F/Z. The authors showed that it is possible to harvest half the virgin
production of a fish stock under certain conditions e.g. that juveniles are not fished
(which is not the case in many small pelagic fisheries such as the Cape anchovy
recruit fishery off South Africa, the anchovy and common sardine fishery off central
Chile or Mediterranean fisheries). Mertz and Myers (1998) calculated E across a
broad range of taxa and found E=0.8 for piscivorous fish (largely groundfish), E=0.5
for prey species.
In the Northern Benguela Fs rose to high levels between the 1970s and 1980s (Cury et
al. in prep) and have decreased since as a result of the collapsed ecosystem in the late
1990s. In the Southern Benguela, decadal average exploitation rates from trophic
models all fell below 0.5, with small pelagic Es less than 0.3 over the last few decades
(Fig. 9a, Cury et al., in prep.). This is in agreement with Fairweather et al’s (2006)
findings. From acoustic survey abundance estimates (since 1984), catch records and
trophic model estimates of total mortality Z, the authors were able to calculate E for
sardine from 1984 to 2005, finding that sardine E generally fell well below the 0.4
target reference point and concluding that the indicator reflects successful sardine
fishery management. In the Northern Benguela, exploitation rates of anchovy, sardine,
and horse mackerel are notably higher than in the Southern Benguela, although Es fell
below 0.32 for anchovy and sardine. In the case of the South Catalan Sea, the
exploitation rate for sardine was higher than the maximum 0.5 recommended for
small pelagic fish during both 1978 and 1990s, and in fact there has been a decline
reported for sardine catches and biomass in this area (Palomera et al., in press), while
anchovy values for both Catalan and Adriatic Sea were also high (E>0.3).
In Central Chile, the stocks of common sardine and anchovy have been decreasing,
especially common sardine, since early 2000s. The highest landing for this species in
last 15 years was found in 1999 with >900 thousand tonnes of common sardine and
>700 thousand tonnes of anchovy. Landing for these species has decreased since then.
Fishing mortality (landing/total biomass) for these species was around 0.3 year-1
during the most of the 1990s, except for years 1999 and 2000 when F was >0.6 year-1.
Since then, F has returned to the levels found during the 1990s.
The two major drivers of fluctuations and collapses in small pelagic fish stocks, and
thus, by virtue of their wasp-waist role in the food web, the propagation of these
effects up and down the food web, are i) climatic effects on small pelagic fish, and ii)
fishing effects on small pelagic fish. The three models fitted to time series data and
discussed above (section 5.1) all illustrated the importance of considering the often
synergistic effects of the environment and fishing. Interactions between the
environment and marine resources can be synergistic or antagonistic, and van der
Lingen et al. (2006) point out that a change in the structure of an ecosystem is likely
to result in a change in the response of the ecosystem to environmental forcing.
In the face of severe environmental perturbations, it may simply not be sufficient to
ensure exploitation rates are well below critical levels. According to the guidelines
discussed above in terms of exploitation rates (Fig. 9), the Northern Benguela would
not have been classified as over exploited in the 1980s, despite the collapse of the
small pelagic fishery in the 1990s, pointing to the importance of taking into account
synergistic effects of environmental conditions and fishing pressure. Sardine in the
Catalan Sea would rightfully be considered overexploited in the 1990s (Lleonart and
Maynou, 2003), whereas in the Adriatic, exploitation rates of small pelagic fish
appear to have been within sustainable levels but large stock declines were observed
at the end of 1980s (Azzali et al., 2002; Santojanni et al, 2003, 2005).
6.3. Disruption of trophic pathways
Monitoring of pelagic:demersal fish biomass ratios over time shows the general trend
in recent decades to have been a shift towards more demersally-dominated
ecosystems (Fig. 3) as pelagic fisheries have expanded and small pelagic fish stocks
have undergone large declines. Proliferation of non-commercial species such as
jellyfish, and changes in diet and populations of predators in ecosystems where small
pelagic fish are heavily exploited could be seen as signs of disruption of the trophic
structure. Snapshot model results and dynamic model simulations of severely altered
fishing on small pelagic fish in the different ecosystems examined support these
hypotheses. Changes in energy transfer can be quantified in terms of increased energy
flowing to detritus when pelagic fish are heavily exploited (see sections 4.5) and a
higher coupling between pelagic and demersal compartments (sections 4.6 and 5.5).
No important changes were found in the Southern Humboldt models in terms of the
impact of the detritus on the pelagic and demersal components. This could be likely
attributed to a decrease in the biomass of the demersal fish (i.e. hake) and benthic
detritivorous crustaceans in recent years, and thus full advantage is not being taken of
the observed increased flow to detritus. On the other hand, large increases in the
summed mixed trophic impacts of detritus on both the pelagic and demersal food
webs were observed over time in the Southern Benguela, and small increases were
observed in the South Catalan Sea, further supporting the hypothesis that detritus can
become increasingly more important as ecosystems are fished and/or degraded.
However, in the Northern Benguela, the near-total collapse of the pelagic ecosystem
has weakened detritus-pelagic food web linkages, whereas detritus-demersal linkages
have strengthened. The dominant small pelagic fish is now the non-commercial
bearded goby Sufflogobius bibarbatus, which, by virtue of being able to feed
benthically as well as pelagically, appears to have been able to survive the frequent
low oxygen events that have been detrimental to the pelagic food web off the coast of
Namibia. In the Adriatic, the decline in the impact of detritus on the demersal
compartment could be due to the high rates of exploitation of commercial scallops
and other invertebrates after the decrease of fish catches (Coll et al. 2007) and the
lower biomasses of these groups in the ecosystem during the 1990s compared to the
1980s.
Comparison of snapshot models also suggests an increase in the pelagic-benthic
coupling through stronger overall mixed trophic interactions of the pelagic component
on the demersal component in more recent periods (usually when fishing has
increased), and often reduced summed impacts of the demersal compartment on the
pelagic food web (sections 4.6 and 5.5). Although this needs further investigation and
more careful quantification, and recognizing that results would depend on whether
certain omnivorous groups are categorised as pelagic or demersal, changes in flows
between benthic and pelagic compartments may be considered a measure of the
impacts of fishing.
Figure captions:
Fig. 1: Number of species (on a logarithmic scale) in the Southern Humboldt and
Southern Benguela in the main taxa represented in these ecosystems, to show the
wasp-waist at the level of small pelagic fish.
Fig. 2: Schematic plot showing expected changes across different trophic levels when
the typical wasp-waist ecosystem is disrupted by fishing.
Fig. 3 Ratios of pelagic:demersal fish in catches in a) the Benguela, b) the Southern
Humboldt, c) South Catalan Sea and North and Central Adriatic Sea. Figures aii) and
bii) show pelagic:demersal biomass ratios from research surveys for the Southern
Benguela and Southern Humboldt respectively. The ratio of demersal:total fish in
catches in the Northern Benguela is plotted in Fig. 3a (iiii).
Fig. 4 i) Trophic level (TL) of the catch and ii) Fishing in balance (FiB) index
calculated from catches in the a) Southern and Northern Benguela (after Cury et al.,
2005a; van der Lingen et al., 2006), b) Southern Humboldt (plotted with and without
horse mackerel, see text for reason), and c) South Catalan Sea and North and Central
Adriatic Sea.
Fig. 5 i) Simulation 1: closure of the purse seine fishery i) Projected modelled
biomass trajectories (biomass plotted relative to biomass at start of simulation) and ii)
ratio of the biomasses of small pelagic fish to demersal fish (including hake), for the
a) Southern Benguela (small pelagic fish include anchovy, sardine, round herring and
other small pelagic fish), b) Southern Humboldt (small pelagic fish include only
anchovy and sardine), c) South Catalan Sea (small pelagic fish include anchovy,
sardine and other small pelagic fish), and d) North and Central Adriatic (small pelagic
fish include anchovy, sardine and other small pelagic fish).
Fig. 6 Simulation 2: collapse of the purse seine fishery i) Projected modelled
biomass trajectories (biomass plotted relative to biomass at start of simulation) and ii)
ratio of the biomasses of small pelagic fish to demersal fish (including hake), for the
a) Southern Benguela (small pelagic fish include anchovy, sardine, round herring and
other small pelagic fish), b) Southern Humboldt (small pelagic fish includes only
anchovy and sardine), c) South Catalan Sea (small pelagic fish include anchovy,
sardine and other small pelagic fish), and d) North and Central Adriatic (small pelagic
fish include anchovy, sardine and other small pelagic fish).
Fig. 7 Modelled catch:biomass ratios (equivalent to fishing mortality, F) for anchovy,
sardine and all the main small pelagic fish in a) Southern and Northern Benguela, b)
Southern Humboldt, and c) South Catalan Sea, and North and Central Adriatic.
Fig. 8 Estimated predation mortality rates of small pelagic fish in a) Southern
Benguela, b) Southern Humboldt and c) South Catalan Sea and (from models fitted to
time series data).
Fig. 9 Exploitation rates (E=F/Z) for main fish species in the a) Southern Benguela,
and b) Northern Benguela, estimated using models for three periods in each system; c)
Northern Humboldt, estimated using models of three periods; d) South Catalan,
estimated using a model for 1978 (blue) and the 1990s (red); and e) North and Central
Adriatic Sea, estimated using a model for the 1980s (blue) and the 1990s (red).
Fig. 10 Estimated biomass trajectories (t.km-2.y-1) of main groups from a) Southern
Benguela trophic model fitted to time series data (Shannon et al., 2004), b) Southern
Humboldt trophic model fitted to time series data (Neira et al., in prep.), and c) South
Catalan trophic model fitted to time series data (Coll et al., in prep.). Because the
relative increase in sardine in the Southern Benguela was so large, the plot including
sardine is presented as an insert in Fig. 10 a. For the South Catalan Sea, species are
grouped according to their scale of relative biomass change over time in Fig. 10 c.
Fig. 11 Sum of all modelled flows to detritus in different periods for the a) Southern
and Northern Benguela, b) Southern Humboldt, and c) South Catalan Sea, and North
and Central Adriatic Sea.
Acknowledgements
Authors would like to thank all researchers involved in ecological models used in this
work: Isabel Palmera, Enrico Arneri, Alberto Santojanni, Sergi Tudela, and Frances
Sardà (South Catalan Sea and North and Central Adriatic Sea), Astrid Jarre and
Coleen Moloney (Southern Benguela upwelling), Hugo Arancibia and Luis Cubillos
(Southern Humboldt upwelling).
References
Abad, R. and Giraldez, A. (1990) Concentrations de Capros aper dans la Mer
d’Alboran (Mediterranée Espagnole). Rapports et Process-Verbaux des Reunions du
la Commission Internationale Pour l’Exploration Scientique de la Mer Méditerranée,
32(1): 256.
Abelló, P., Arcos, J. M. and Gil de Sola, L. (2003) Geographical patterns of
attendance to trawling by breeding seabirds along the Iberian Peninsula
Mediterranean Coasts. Scientia Marina, 67 (Suppl. 2): 69-75.
Alheit. J. and Niquen, M. (2004) Regime shifts in the Humboldt Current System.
Progress in Oceanography, 60: 201-222.
Agostini, V. and Bakun, A. (2002) “Ocean triads” in the Mediterranean Sea: physical
mechanisms potentially structuring reproductive habitat suitability (with example
application to European anchovy, Engraulis encrasiclous). Fisheries Oceanography,
11(3): 129-142.
Arai, M.N. (2001) Pelagic coelenterates and eutrophication: a review. Hydrobiologia,
451: 69-87.
Arancibia, H. (1989) Distribution patterns, trophic relationships and stock
interactions in the demersal fish assemblage off central Chile. Dr. rer. Nat. Thesis.
University of Bremen, German, 221 pp.
Arancibia H. and Neira, S. (2003) Simulación de cambios en la biomasa de los
principales recursos pesqueros de Chile central (V – IX región) bajo el marco de la
ley de pesca N° 19.713 y sus posteriores modificaciones. Informe Final. Universidad
de Concepción, 53 pp.
Arancibia, H. and Neira, S. (2005) Long-term analysis of the trophic level of fisheries
landings in Central Chile. Scientia Marina, 69(2): 295-300.
Arancibia, H., Catrilao, M. and Farías, B. (1998) Evaluación de la demanda de
alimento en merluza común y análisis de su impacto en pre - reclutas. Informe
Final Proyecto FIP 95- 17, 98 pp.
Arcos, J. M. (2001) Foraging ecology of seabirds at sea: significance of commercial
fisheries in the Northwestern Mediterranean. PhD thesis. University of Barcelona.
109 pp.
Arneri, E. (1996) Fisheries resources assessment and management in Adriatic and
Ionian Seas. FAO Fisheries Report, 533: 7-20.
Arrizaga, A., Fuentealba, M., Espinoza, C., Chong, J. and Oyarzún, C. (1993)
Trophic habits of two pelagic fish species: Strangomera bentincki (Norman, 1936)
and Engraulis ringens (Jenyns, 1842), in the littoral of the Biobio Region, Chile. Bol.
Soc. Biol. Concepción (Chile) 64: 27– 35.
Avaria, S. and Muñoz, P. (1982) Producción actual, biomasas y composición
específica del fitoplancton de la bahía de Valparaíso en 1979. Revista de Biología
Marina de Valparaíso 18: 129-157.
Azzali, M., De Felice, A., Luna, M., Cosimi, G. and Parmiggiani, F. (2002) The State
of the Adriatic Sea Centered on the Small Pelagic Fish Populations. P. S. Z. N.:
Marine Ecology, 23 (Supl.1): 78-91.
Baccetti, N., Dall’Antonia, P., Magagnoli, P., Melega, L., Serra, L., Soldatini, C. and
Zenatello, M. (2002) Risultati dei censimenti degli uccelli acquatici svernanti in Italia:
distribuzione, stima e trend delle popolazioni nel 1991-2000. Instituto Nazionale per
la fauna selvatica Alessandro Ghigi. Vol. 111. 234.
Bakun, A. (1996) Patterns in the Ocean: Ocean Processes and Marine Population
Dynamics. University of California Sea Grant, San Diego, California, USA, in
cooperation with Centro de Investigaciones Biologicas de Noroeste, La Paz, Baja
California Sur, Mexico. 323 pp.
Bakun A. (2006) Wasp-waist populations and marine ecosystem dynamics:
Navigating the ‘‘predator pit’’ topographies. Progress in Oceanography, 68 (2006)
271–288.
Bakun, A. and S. Weeks, 2004, Greenhouse gas buildup, sardines, submarine
eruptions and the possibility of abrupt degradation of intense marine upwelling
systems. Ecology Letters 7: 1015-1023.
Barange, M., Hampton, I. and Roel, B.A. (1999) Trends in the abundance and
distribution of anchovy and sardine on the South African continental shelf in the
1990s, deduced from acoustic surveys. South African Journal of Marine.Science, 19:
367-391.
Bearzi, G., Holcer, D. and Notarbartolo Di Sciara, G. (2004) The role of historical
dolphin takes and habitat degradation in shaping the present status of northern
Adriatic cetaceans. Aquatic Conservation of Marine and Freshwater Ecosystems, 14:
363–379.
Blanco, C., Salomón, O. and Raga, J.A. (2001) Diet of the bottlenose dolphin
(Tursiops truncatus) in the western Mediterranean Sea. Journal of the Marine
Biological Association of the United Kingdom, 81: 1053-1058.
Barkai, A. and McQuaid, C. (1988) Predator-prey reversal in a marine benthic
ecosystem. Science, 242: 62-64.
Beaugrand, G., Brander, K.M., Alistair Lindley, J. Soussi, S. and Reid, P. C. (2003)
Plankton effect on cod recruitment in the North Sea. Nature, 426: 661-664.
Best, P.B., Crawford, R.J.M. and Van der Elst, R.P. (1997) Top predators in southern
frica’s marine ecosystems. Transactions of the Royal Society of South Africa, 52(1):
177-225.
Bombace, G. (1992) Fisheries of the Adriatic Sea. In. Marine Eutrophication and
Population Dynamics. 25th European Marine Biology Symposium. Olsen and Olsen,
Fredensborg: 379-389.
Bosc, E., Bricau, A. and Antoine., D. (2004) Seasonal and interannual variability in
algal biomass and primary production in the Mediterranean Sea, as derived from 4
years of SeaWiFS observations. Global Biogeochemical Cycles, 18(GB1005): 17p.
Boyer, D.C., Boyer, H.J,. Fossen, I and Kreiner, A. (2001) Changes in abundance of
the northern Benguela sardine stock during the decade 1990 to 2000 with comments
on the relative importance of fishing and the environment. South African Journal of
Marine Science, 23: 67-84.
Boyer, D.C. and Hampton, I. (2001) An overview of the living marine resources of
Namibia. South African Journal of Marine Science, 23: 5-35.
Bosc, E., Bricau, A. and Antoine, D. (2004) Seasonal and interannual variability in
algal biomass and primary production in the Mediterranean Sea, as derived from 4
years of SeaWiFS observations. Global Biogeochemical Cycles, 18(GB1005): 17p.
Bozzano, A., Recasens, L. and Sartor, P. (1997) Diet of the European hake
Merluccius merluccius (Pisces: Merluciidae) in the Western Mediterranean (Gulf of
Lions). Scientia Marina, 61(1): 1-8.
Carr. E.-M. (2002) Estimation of potential productivity in eastern boundary currents
using remote sensing. Deep Sea Research II, 49: 59-80.
Camus, P. (2001) Biogeografía marina de Chile continental. Revista Chilena de
Historia Natural, 74: 587-617.
Christensen, V. and Walters, C. J. (2004) Ecopath with Ecosim: methods, capabilities
and limitations. Ecological Modelling, 172: 109-139.
Cingolani, N., Giannetti, G.G and Arneri, E. (1996) Anchova fisheries in the Adriatic
Sea. Scientia Marina, 60(Suppl. 2): 269-277.
Clarke, W.G. (1991) Groundfish exploitation rates based upon life-history parameters.
Canadian Journal of Fisheries and Aquatic Science, 48: 734-750.
Cochrane, K.L., Augustyn, C.J., Cockcroft, A.C., David, J.H.M., Griffiths, M.H.,
Groeneveld, J.C., Lipinski, M.R., Smale, M.J., Smith, C.D. and Tarr, R.J.Q. (2004)
An ecosystem approach to fisheries in the southern Benguela context. African Journal
of Marine Science, 26: 9-35.
Coll, M., Palomera, I. Tudela, S. and Sardà, F. (2005) Assessing the impact of fishing
activities and environmental forcing on a Northwestern Mediterranean ecosystem
along the last decades of intense exploitation. Advances in Marine Ecosystem
Modelling Research. International Symposium at Plymouth Marine Laboratory 27 -
29 June 2005, Plymouth, UK. 148 p.
Coll, M. (2006) Trophic web modelling and ecological indicators for assessing
ecosystem impacts of fishing in the Mediterranean Sea. PhD thesis. Autonomous
University of Barcelona. Spain. Unpublished.
Coll, M., Shannon, L.J., Moloney, C. L., Palomera, I. and Tudela, S. (2006a)
Comparing trophic flows and fishing impacts of a NW Mediterranean ecosystem with
coastal upwellings by means of standardized ecological models and indicators.
Ecological Modelling, 198: 53-70.
Coll, M., Palomera, I., Tudela, S. and Sardà, F. (2006b) Trophic flows, ecosystem
structure and fishing impacts in the South Catalan Sea, Northwestern Mediterranean.
Journal of Marine Systems, 59: 63-96.
Coll, M., Santojanni, A., Arneri, E. and Palomera, I. (2007) An ecosystem model of
the Northern and Central Adriatic Sea: analysis of ecosystem structure and fishing
impacts. Journal of Marine Systems, in press.
Coll, M., Palomera, I., Tudela, S. and Sardà, F. Hindcasting the dynamics of exploited
marine resources in the South Catalan Sea by means of trophodynamic modelling.
Scientia Marina, In prep.
Crawford, R.J.M. and Dyer, B.M. (1995) Responses by four seabirds to a fluctuating
availability of Cape anchovy Engraulis capensis off South Africa. Ibis, 137: 329-339.
Crawford, R.J.M. and Jahncke, J. (1999) Comparison of trends in abundance of
guano-producing seabirds in Peru and southern Africa. South African Journal of
Marine Science, 21:145-156.
Crawford, R.J.M., Cruichshank, R.A., Shelton, P.A. and Kruger, I. (1985) Partitioning
of a goby resource amongst four avian predators and evidence for altered trophic flow
in the pelagic community of an intense perennial upwelling system. South African
Journal of Marine Science, 3: 215-228.
Crawford, R.J.M., Dyer, B.M., Cordes, I. and Williams, A.J. (1999) Seasonal pattern
of breeding, population trends and conservation status of bank cormorants
Phalacrocorax neglectus off south western Africa. Biological Conservation, 87: 49-58.
Crawford, R.J.M., Shannon, L.J., Kreiner, A., van der Lingen, C.D., Alheit, J., Bakun,
A., Boyer, D., Cury, P., Dunne, T., Durand, M.-H , Field, J.G, Fréon, P., Griffiths,
M.H., Hagen, E., Hutchings, L., Klingelhoeffer, E., Moloney, C.L., Mouton, D., Roy,
C., Roux, J.-P , Shannon, L.V., Shillington, F.A., Underhill, L.G. and Verheye, H.M.
Periods of major change in the structure and functioning of the pelagic component of
the Benguela ecosystem, 1950-2000. Unpublished manuscript.
Crawford, R.J.M. (2006) Closure of areas to purse-seine fishing around the St Croix
and Dyer island African penguin colonies. Unpublished report
SWG/OCT2006/PEL/06, Marine and Coastal Management, Department of
Environmental Affairs and Tourism, South Africa, 10pp.
Cubillos, L., Rebolledo, H., Hernández, A. (2003) Prey composition and estimation
of Q/B for the Chilean hake, Merluccius gayi (Gadiformes-Merluccidae), in the
central-south area off Chile (34º-40ºS), Archive of Fishery and Marine Research, 50,
271-286.
Cury, P.M. and Shannon, L.J. (2004) Regime shifts in upwelling ecosystems:
observed changes and possible mechanisms in the northern and southern Benguela.
Progress in Oceanography, 60: 223-243.
Cury, P., Bakun, A., Crawford, R.J.M., Jarre-Teichmann, A., Quinones, R.A , Shannon,
L.J. and Verheye, H.M. (2000) Small pelagic fish in upwelling systems: patterns of
interaction and structural changes in “wasp-waist” ecosystems. ICES Journal of Marine
Science Symposium Edition, 57(3): 603-618.
Cury, P.M., Shannon, L.J. and Shin, Y.-J. (2003) The functioning of marine
ecosystems: a fisheries perspective p. 103-123 In Sinclair, M., and Valdimarsson, G.
Responsible Fisheries in the Marine Ecosystem. FAO and CABI Publishing, UK.
426pp.
Cury, P.M., Shannon, L.J., Roux, J.-P., Daskalov, G.M., Jarre, A., Moloney, C.L. and
Pauly, D. (2005a) Trophodynamic Indicators for an Ecosystem Approach to Fisheries.
ICES Journal of Marine Science, 62: 430-442.
Cury, P., Fréon, P., Moloney, C., Shannon L. J and Shin, Y. (2005b) Processes and
patterns of interactions in marine fish populations: an ecosystem perspective. In The
SEA: Ideas and Observations on Progress in the study of the Seas. The global coastal
ocean: multiscale interdisciplinary processes (A. Robinson and K. Brink Eds.).
Chapter 14, Harvard University Press, Cambridge: 475-554.
Cury, P.C., Shannon, L.J., Roux, J.-P. In prep. 0.3 for an ecosystem approach to
marine resources? In preparation.
Cushing, D.H. (1990) Plankton production and year-class strength in fish populations: an
update of the match/mismatch hypothesis. Advances in Marine Biology, 26: 249-293.
Daneri, G., Dellarossa, V., Quiñones, R., Jacob, B., Montero, P. and Ulloa, O. (2000)
Primary production and community respiration in the Humboldt Current System off
Chile and associated oceanic areas. Marine Ecology Progress Series, 197: 41-49.
Daskalov, G. M. (2002) Overfishing drives a trophic cascade in the Black Sea.
Marine Ecology Progress Series, 225: 53-63.
De Villiers, G. (1985) Simpsoa internacional sobre las areas de afloramiento mas
importantes del oeste Africano (Cabo Blanco y Benguela). Int. Symp. Upw. W. Afr., Inst.
Inv. Pesq., Barcelona 1985, 2: 1005-1039.
Escribano, E., Fernández, M. and Aranís, A. (2003) Physical-chemical processes and
patterns of biodiversity of the Chilean eastern boundary pelagic and benthic marine
ecosystems: an overview. Gayana, 67(2):190-205.
Estrada, M. (1996) Primary production in the Northwestern Mediterranean. Scientia
Marina, 60 (Supl.2): 55-64.
FAO (2005) Review of the state of the world marine fishery resources. FAO Marine
Resources Service, Fishery Resources Division. Fisheries Technical Paper, nº 457,
246p.
Fairweather TP, van der Lingen CD, Booth AJ, Drapeau L, van der Westhuizen JJ
(2006) Indicators of sustainable fishing for South African sardine (Sardinops sagax)
and anchovy (Engraulis encrasicolus). African Journal of Marine Science, 28: 1-40
Fonda Umani, S. (1996) Pelagic production and biomass in the Adriatic Sea. Scientia
Marina, 60 (Supl. 2): 65-77.
Frank, K.T., Choi, J.S., Petrie, B. and Leggett, W.C. (2005) Trophic cascades in a
formerly cod dominated ecosystem. Science, 308: 1621-1623.
Frank, K.T., Petrie, B., Shackell, N.L. and Choi, J.S. (2006) Reconciling differences
in trophic control in mid-latitude marine ecosystems. Ecology Letters, 9: 1-10.
García, S. M. and Staples, D.J. (2000) Sustainability reference systems and indicators
for responsible marine capture fisheries: a review of concepts and elements for a set
of guidelines. Marine Freshwater Research, 51: 385-426.
Giordani, P., Hammond, D., Berelson, G., Montanari, G., Poletti, R. Milandri, A.,
Frignani, M., Langone, L., Ravaioli, M., Rovatti, G and Rabbi, E. (1992) Benthic
fluxes and nutrient budgets of the sediments in the Northern Adriatic Sea. The
Science of Total Environment (Suppl.): 251-256.
Griffiths, C.L., van Sittert, L., Best, P.B., Brown, A.C., Cook, P.A., Crawford, R.J.M.,
David, J.H.M., Davies, B.R., Griffiths, M.H., Hutchings, K., Jerardino, A., Kruger,
N., Lamberth, S., Leslie, R., Melville-Smith, R., Tarr, R. and van der Lingen, C.D.
(2004) Impacts of human activities on marine animal life in the Benguela – a
historical overview. Oceanography and Marine Biology Annual Reviews, 42: 303-
392.
Gucu, A.C. (2002) Can overfishing be responsible for the successful establishment of
Mnemiopsis leidyi in the Black Sea? Estuarine, Coastal and Shelf Science, 54: 439-
451.
Hamukuaya, H., O’Toole, M.J. and Woodhead, P.M.J. (1998) Observations of severe
hypoxia and offshore displacement of Cape hake over the Namibian shelf in 1994.
South African Journal of Marine Science, 19: 57-59.
Hill, A., Hickey, B., Shillington, F., Strub, T., Brink, K. , Barton, E. and Thomas, A.
(1998) Eastern ocean boundaries coastal segment. Chapter 2. In The sea: The global
coastal ocean, regional studies and syntesis. 11 A. R.B.K H. Robinson (Eds.). John
Wiley and Sons, Inc., New York. 29-67 pp. [8]
Heymans, J.J., Shannon, L.J., and Jarre, A. (2004) Changes in the northern Benguela
ecosystem over three decades: 1970s, 1980s and 1990s. Ecological Modelling, 172:
175-195.
Jahncke, J., Checkley Jr, D.M., Hunt Jr, G.L. (2004) Trends in carbon flux to seabirds
in the Peruvian upwelling system: effects of wind and fisheries on population
regulation. Fisheries Oceanography, 13 (3): 208–223.
Jarre-Teichmann (1998) The potential role of mass-balanced models for the
management of upwelling ecosystems. Ecological Applications, 8(1): 93-103.
Jarre-Teichmann, A. and Christensen, V. (1998) Comparative modelling of trophic
flows in four Large Marine Ecosystems; Global versus local effects. In Durand, M.-
H., Cury, P., Mendelssohn, R., Roy, C., Bakun, A. and Pauly, D. Global versus local
changes in upwelling systems. Editions de l’Orstom, 423-443.
Jarre-Teichmann, A., Shannon, L.J., Moloney, C.L. and Wickens, P.A. (1998)
Comparing trophic flows in the southern Benguela to those in other upwelling
ecosystems. In Pillar, S.C., Moloney, C.L., Payne, A.I.L. and Shillington, F.A.
Benguela dynamics: impacts of variability on shelf-sea environments and their living
resources. South African Journal of Marine Science, 19:391-414.
Jukic-Peladic, S., Vrgoc, N., Krstulovic-Sifner, S., Piccinetti, C., Piccinetti-Manfrin,
G., Marano, G. and Ungaro, N. (2001) Long-term changes in demersal resources of
the Adriatic Sea: comparison between trawl surveys carried out in 1948 and 1998.
Fisheries Research, 53(1): 95-104.
Kawasaki, T. (1983) Why do some pelagic fish have wide fluctuations in their
numbers? Biological basis from the viewpoint of evolutionary ecology. FAO
Fisheries Reports, 291(3):1065-1080.
Kytaysky A.S., Kitauskaia E.V., Piatt J.F. and Wingfield, J.C. (2006) A mechanistic
link between chick diet and decline in seabirds? Proceedings of the Royal Society B,
273: 445-40.
Leibol, M.A., Chase, J.M., Shurin, J.B. and Downing, A.L. (1997) Species turnover
and the regulation of trophic structure. Annual Review of Ecology and Systematics,
28: 467-94.
Lleonart, J. and Maynou, F. (2003) Fish stock assessments in the Mediterranean: state
of the art. Scientia Marina, 67(Suppl. 2): 37-49.
Lluch-Belda, D., Crawford, R.J.M., Kawasaki, T., MacCall, A.D., Parrish, R.H.,
Schwartlose, R.A. and Smith, P.E. (1989) World-wide fluctuations of sardine and
anchovy stocks: the regime problem. South Africa Journal of Marine Science, 8: 195-
205.
Lluch-Belda, D., Schwartlose, R.A., Serra, R., Parrish, R., Kawasaki, T., Hedgecock, D.
and Crawford, R.J.M. (1992a) Sardine and anchovy regime fluctuations of abundance in
four regions of the world oceans: a workshop report. Fisheries Oceanography, 1(4): 339-
347.
Lewis, S. , Sherratt, T. N., Hamer, K. C. and Wanless, S. (2001) Evidence of intra-
specific competition for food in a pelagic seabird. Nature, 412: 816-819.
Litzow M.A., Bailey K.M., Prahl F.G. and Heintz, R. (2006) Climate regime shifts
and reorganization of fish communities: the essential fatty acid limitation hypothesis.
Marine Ecology Progress Series, 315: 1-11.
Lleonart, J. and Maynou, F. (2003) Fish stock assessments in the Mediterranean: state
of the art. Scientia Marina, 67 (Suppl. 2): 37-49.
Lloret, J. and Lleonart, J. (2002) Recruitment dynamics of eight fishery species in the
Northwestern Mediterranean Sea. Scientia Marina, 66(1): 77-82.
Lloret, J., I. Palomera, J. Salat and Sole, I. (2004) Impact of freshwater input and
wind on landings of anchovy (Engraulis encrasiclous) and sardine (Sardina
pilchardus) in shelf waters surrounding the Ebro River delta (northwestern
Mediterranean). Fisheries Oceanography, 13 (2): 102-110.
Maartens, L. (1999) An assessment of the monkfish resource of Namibia. Ph.D.
thesis. Rhodes University: Grahamstown: 190pp.
Margalef, R. (1985) Introduction to the Mediterranean. In. Margalef, R. (Ed.). Key
Environments: Western Mediterranean. Pergamon Press. New York. 362 pp.
Mertz G. and Myers, R.A. (1998) A simplified formulation for fish production.
Canadian Journal of Fisheries and Aquatic Science, 55: 478-484.
Mecenero, S. and Roux, J.-P. (2002) Spatial and temporal variability in the diet of a
top predator in the northern Benguela. GLOBEC Report, 16: 62-64.
Meeuwis, J.M. and Lutjeharms, J.R.E. (1990) Surface thermal characteristics of the
Angola-Benguela Front. South African Journal of Marine Science, 9: 261-279.
Meléndez, R. (1984) Alimentación de Merluccius gayi (Guichenot) frente a Chile
central (32°05’S-36°50’S). Bol. Mus. Nac. Hist. Nat. Chile, 54 pp.
Mills, C. E. (2001) Jellifish blooms: are populations increasing globally in response to
changing ocean conditions? Hydrobiologia, 41: 55-68.
Miranda, L., Hernández, A., Sepúlveda, A., Landaeta, M. (1998) Alimentación de
jurel y análisis de la selectividad en la zona centro-sur de Chile. In: Arcos, D. (Ed.),
Biología y Ecología del Jurel en Aguas Chilenas. Instituto de Investigación Pesquera,
Talcahuano-Chile, pp. 173– 187.
Moloney, C.L., Jarre, A., Arancibia, H., Bozec, Y.-M., Neira, S., Roux, J.-P. and
Shannon, LJ. (2005) Comparing the Benguela and Humboldt marine upwelling
ecosystems with indicators derived from inter-calibrated models. ICES Journal of
Marine Science, 62 (3): 493-502.
Mannini, P. and Massa, F. (2000) Brief Overview of Adriatic fisheries landings trends
(1972-97). In. Massa F. and P. Mannini (eds). Report of the First Meeting of
Adriamed Coordination Comité. FAO-MiPAF Scientific Cooperation to Support
Responsable Fisheries in the Adriatic Sea. GCP/RER/010/ITA/TD-01: 31-49.
Manoukian, M., Azzali, M., Farchi, C., Giovagnoli, L., La Bella, G. and Rivas, G.
(2001) Sightings distribution and variability in species composition of cetaceans in
the Adriatic Sea ecosystem in one decade of study. Rapports et Process-Verbaux des
Reunions du la Commission Internationale Pour l’Exploration Scientique de la Mer
Méditerranée, 36: 297.
Mayfield, S. and Branch, G.M. (2000) Interrelations among rock lobsters, sea urchins,
and juvenile abalone: implications for community management. Canadian Journal of
Fisheries and Aquatic Science, 57: 2175-2185.
Moloney, C., Jarre, A., Arancibia, H., Bozec, Y-M., Neira, S., Roux, J-P and
Shannon, L. J. (2005) Comparing the Benguela and Humboldt marine upwelling
ecosystems with indicators derived from inter-calibrated models. ICES Journal of
Marine Science, 62 (3): 493-502.
Montecinos, A., Purca, S. and Pizarrro, O. (2003) Interannual-to-interdecadal sea
surface temperature variability along the western coast of South America. Gophisical
Research Letters, 30(11): 1570-1573.
Neira, S. and Arancibia, H. (2004) Trophic interactions and community structure in
the Central Chile marine ecosystem (33º S-39º S). Journal of Experimental Marine
Biology and Ecology, 312: 349-366.
Neira, S., Arancibia, H. and Cubillos, L. (2004) Comparative analysis of trophic
structure of commercial fishery species off Central Chile in 1992 and 1998.
Ecological Modelling, 172 (2-4): 233-248.
Neira, S., Moloney, C., Cury, P. and Arancibia, H. In prep a. Analyzing changes in
the southern Humboldt ecosystem for the period 1970-2004 by means of trophic/food
web modeling (in preparation to be submitted to Fish and Fisheries)
Neira, S., Moloney, C., Cury, P., Arancibia, H. and Cubillos, L. In prep b. Analyzing
interactions in the southern Humboldt upwelling system, who controls whom? (in
preparation to be submitted to Progress in Oceanography)
Odum, E.P. (1985) Trends expected in stressed ecosystems. BioScience, 35(7):419-
422.
Ölscher, E. M. and Fedra, K. (1977) On the ecology of a suspension feeding benthic
community: filter efficiency and behavior. In: B. F. Keegan, P. O'Ceidigh and P. J. S.
Boaden (Eds.), Biology of Benthic Organisms. 11th Eur. Mar. Biol. Symp., Galway.
Pergamon Press, Oxford: 549-558.
Oro, D. (1996) Effects of trawler discard availability on egg laying and breeding
success in the lesser black-backed gull Larus fuscus in the western Mediterranean.
Marine Ecology Progress Series, 132: 43-46.
Oro, D., Jover, Ll. and Ruíz, X. (1996) Influence of trawling activity on the breeding
ecology of a threatened seabird, Audouin’s gull Larus auduinii. Marine Ecology
Progress Series, 139: 19-29.
Oro, D. and Ruíz, X. (1997) Exploitation of trawler discards by breeding seabirds in
the north-western Mediterranean: differences between the Ebro Delta and the Balearic
Islands areas. ICES Journal of Marine Science, 54: 695-707.
Ott, J. (1992) The Adriatic benthos: problems and perspectives. In. Marine
Eutrophication and Population Dynamics. 25th European Marine Biology Symposium.
Olsen and Olsen, Fredensborg: 367-378.
Palma, S. and Rosales, S. (1995) Composición, distribución y abundancia estacional
del macroplancton de la bahía de Valparaíso. Investigaciones Marinas, 23: 49-66.
Palomera, I., Olivar, M.P., Salat, J., Sabatés, A., Coll, M., García, A. and Morales-
Nin, B. Role of Small Pelagic Fish in the NW Mediterranean Ecosystems. Progress in
Oceanography, accepted for publication.
Papaconstantinou, C. and Farrugio, H. (2000) Fisheries in the Mediterranean.
Mediterranean Marine Science, 1(1): 5-18.
Patterson, K. (1992) Fisheries for small pelagic species: an empirical approach to
management targets. Reviews in Fish Biology and Fisheries, 2: 321-338
Pauly, D., Christensen, V., Dalsgaard, J., Froese, R. and Torres Jr., F. (1998) Fishing
down marine food webs. Science, 279: 860-863.
Pauly, D. and Palomares, M.L. (2005) Fishing down marine food web: it is far more
pervasive than we thought. Bulletin of Marine Science, 76 (2): 197-211.
Patterson, K. (1992) Fisheries for small pelagic species: an empirical approach to
management targets. Reviews in Fish Biology and Fisheries, 2: 321-338
Pauly, D., Christensen, V. and Walters, C. (2000) Ecopath, Ecosim, and Ecospace as
tools for evaluating ecosystem impact of fisheries. ICES Journal of Marine Science,
57: 697-706.
Payne A.I.L. (1989) Cape hakes. In: Payne AIL, Crawford RJM (eds) Oceans of Life
off Southern Africa, Vlaeberg, Cape Town, p. 136-147.
Pinardi, N., Arneri, E., Crise, A., Ravaioli, M. and Zavatarelli, M. in press. The
physical, sedimentary and ecological structure and variability of shelf areas in the
Mediterranean sea (27,s). The Sea ,Volume 14, edited by Allan R Robinson and
Kenneth H.Brink. Harvard University Press.
Pitcher, T.J. (2000) Rebuilding as a new goal for fisheries management:
reconstructing the past to salvage the future. Ecological Applications, 11: 601-617.
Pitcher, T.J. and Pauly, D. (1998) Rebuilding ecosystems, not sustainability, as the
proper goal of fishery management. In Pitcher, T.J., Hart, P., and D. Pauly 1998.
Reinventing fisheries management. Kluwer Academic Publishers, London. Fish and
Fisheries Series, 23: 311-329.
Pranovi, F., Raicevich, S., Franceschini, G., Farrace, M.G. and Giovanardi, O. (2000)
Rapido trawling in the northern Adriatic Sea: effects on benthic communities in an
experimental area. ICES Journal of Marine Science, 57: 517-524.
Pranovi, F., Raicevich, S., Franceschini, G., Torricelli, P. and Giovanardi, O. (2001)
Discard analysis and damage to non-target species in the rapido trawl fishery. Marine
Biology, 139: 863-875.
Punt, A.E. and Butterworth, D.S. (1995) The effects of future consumption by the
Cape fur seal on catches and catch rates of the Cape hakes. 4. Modelling the
biological interaction between Cape fur seals Arctocephalus pusillus pusillus and the
Cape hakes Merluccius capensis and M. paradoxus. South African Journal of Marine
Science, 16: 255-285.
Rice, J. (1995) Food web theory, marine food webs, and what climate change may do
to northern marine fish populations. In Climate Change and Northern Fish
Populations, pp. 516–568. Ed. by R. J. Beamish. Canadian Special Publication of
Fisheries and Aquatic Sciences, 121.
Riedl, R. (1986) Fauna y Flora del Mar Mediterráneo. Ed. Omega. Barcelona.
Ríos, J. (2000) Feeding habits and trophic relationships in a demersal fish community
in the Catalan sea (Western Mediterranean). MSc. Thesis. School of Ocean Sciences,
University of Wales, Bangor. 100 pp.
Rochet, M.–J. and Trenkel, V.M. (2003) Which community indicators can measure
the impact of fishing? A review and proposals. Canadian Journal of Fisheries and
Aquatic Science, 60: 86–99.
Rottini-Sandrini, R.L. and Stravisi, F. (1981) Preliminary report on the occurrence of
Pelagia noctiluca (Semaestomae, pelagidae) in Northern Adriatic. Rapports et
Process-Verbaux des Reunions du la Commission Internationale Pour l’Exploration
Scientique de la Mer Méditerranée, 27(7): 147.
Roux, J-P. (1998) The impact of environmental variability on the seal population.
Namibia Brief, Special Issue 18: Focus on Fisheries and Research: 138-140.
Roux, J-P. (2003) Risks. In Namibia’s Marine Environment. Eds. F.J. Molloy and T.
Reinikainen. Directorate of Environmental Affairs, MET, Windhoek, Namibia: 137-
152.
Roux, J.-P. and Shannon, L.J. (2004) Ecosystem approach to fisheries management in
the northern Benguela: the Namibian experience. In Ecosystem Approaches to
Fisheries in the Southern Benguela. Shannon, L.J., Cochrane, K.L. and S.C. Pillar
(Eds). African Journal of Marine Science, 26: 79-93.
Roy, C.P., Weeks, S.C., Roualt, M., Nelson, G., Barlow, R. and van der Lingen C.D.
(2001) Extreme oceanographic events recorded in the Southern Benguela during the
1999-2000 summer season. South African Journal of Science, 97: 465-471.
Ryther, J.H. (1969) Photosynthesis and fish production in the sea. Science, 166:72-76.
Salat, J. (1996) Review of hydrographic environmental factors that may influence
anchovy habitats in Northwestern Mediterranean. Scientia Marina, 60 (2): 21-32.
Sánchez, F. and Olaso, I. (2004) Effects of fisheries on the Cantabrian Sea shelf
ecosystem. Ecological Modelling, 172(2-4): 151-174.
Santojanni, A., Arneri, E., Barry, C., Belardinelli, A., Cingolani, N., Giannetti, G. and
Kirkwood, G. (2003) Trends of anchovy (Engraulis encrasicolus, L.) biomass in the
northern and central Adriatic Sea. Scientia Marina, 67(3): 327-340.
Santojanni, A., Cingolani, N., Arneri, E., Kirkwood, G., Belardinelli, A., Giannetti,
G., Colella, S., Donato, F., and Barry, C. (2005) Stock assessment of sardine (Sardina
pilchardus, Walb.) in the Adriatic Sea, with an estimate of discards. Scientia Marina,
69 (4): 603-617.
Sardà, F., Bahamón N., Sardà-Palomera F. and Molí B. (2005) Commercial testing of
a sorting grid to reduce catches of juvenile hake (Merluccius merluccius, L.) in the
western Mediterranean demersal trawl fishery. Aquatic Living Resources, 18:87-91.
Schwartzlose, R.A., Alheit, J., Bakun, A., Baumgartner, T.R., Cloete, R., Crawford,
R.J.M., Fletcher, W.J., Green-Ruiz, Y., Hagen, E., Kawasaki, T. , Lluch-Belda, D.,
Lluch-Cota, S.E., MacCall, A.D., Matsuura, Y., Nevarez-Maryinez, M.O., Parrish, H.,
Roy, C., Serra, R., Shust, K.V., Ward M.N., and Zuzunaga, J.Z. (1999) Worldwide
large-scale fluctuations of sardine and anchovy populations. South African Journal of
Marine Science, 21: 289-347.
Shannon, L.J., Roux, J.-P. and Jarre, A. (2001) Trophic interactions in the Benguela
ecosystem and their implications for multispecies management of fisheries. Report on
progress to January 2001: exploring multispecies management options using the
completed northern Benguela ecosystem model. BENEFIT/FAO/Government of
Japan Cooperative Programme GCP/INT/JPN, Report no. 2.4. 56 pp.
Shannon, L.J., Moloney, C.L., Jarre, A. and Field, J.G. (2003) Trophic flows in the
southern Benguela during the 1980s and 1990s. Journal of Marine Systems, 39 (1-
2):83-116.
Shannon, L.J. and Jarre-Teichmann, A. (1999a) A model of the trophic flows in the
northern Benguela upwelling system during the 1980s. South African Journal of
Marine Science, 21: 349-366.
Shannon, L.J. and Jarre-Teichmann, A. (1999b) Comparing models of trophic flows
in the northern and southern Benguela upwelling systems during the 1980s. p. 527-
541 in Ecosystem approaches for fisheries management. University of Alaska Sea
Grant, AK-SG-99-01, Fairbanks. 756pp.
Shannon, L.J., Cury, P and Jarre, A. (2000) Modelling effects of fishing in the
southern Benguela ecosystem. ICES Journal of Marine Science, Symposium Edition
57(3):720-722.
Shannon, L.J. and Cury, P. (2003) Indicators quantifying small pelagic fish
interactions: application using a trophic model of the southern Benguela ecosystem.
Ecological Indicators, 3(4): 305-321.
Shannon, L.J., Moloney, C.L., Jarre, A. and Field, J.G. (2003) Trophic flows in the
southern Benguela during the 1980s and 1990s. Journal of Marine Systems 39 (1-
2):83-116.
Shannon, L.J., Field, J.G. and Moloney, C.L. (2004a) Simulating anchovy-sardine
regime shifts in the southern Benguela ecosystem. Ecological Modelling, 172: 269-
281.
Shannon, L.J., Christensen, V. and Walters, C. (2004b) Modelling stock dynamics in
the southern Benguela ecosystem for the period 1978-2002. In Ecosystem Approaches
to Fisheries in the Southern Benguela. Shannon, L.J., Cochrane, K.L. and S.C. Pillar
(Eds). African Journal of Marine Science, 26:179-196.
Shannon, L.J., Cury, P.M., Nel, D., van der Lingen, C.D., Leslie, R.W., Brouwer,
S.L., Cockcroft, A.C. and Hutchings, L. (2006) How can science contribute to an
ecosystem approach to pelagic, demersal and rock lobster fisheries in South Africa?
African Journal of Marine Science, 28(1): 115-157.
Shannon, L.J., Neira, S., Moloney, C.L., Roy, C., Cury. P.M. in prep. a. Comparing
internal and external drivers in the southern Benguela and southern Humboldt
Upwelling ecosystems. Paper in preparation.
Shannon, L.J., Moloney, C.L. and Roy, C. in prep. b. Tuning a trophic model of the
southern Benguela ecosystem to updated time series data. Paper in preparation.
Shin, Y. (2006) EAF Indicators: a comparative approach across ecosystems. Report of
the Third Workshop: 1-3 February 2006, CRH, Sète, France. EUR-OCEANS
Working Group for Tjeme WP6-Ecosystem Approach for Marine Resources. 9pp.
Soto K.H., Trites A.W. and Arias-Schreiber, M. (2006) Changes in diet and maternal
attendance of South American sea lions indicate changes in the marine environment
and prey abundance. Marine Ecology Progress Series, 312: 277-290.
Springer, A.M., Estes, J.A., van Vliet, G.B., Williams, T.M., Doak, D.F., Danner,
E.M., Forney, K.A. and Pfister, B. (2003) Sequential megafaunal collapse in the
North Pacific Ocean: an ongoing legacy of industrial whaling? Proceedings of the
National Academy of Sciences of the United States of America, 100, 12223-12228.
Stergiou, K. I. and Karpouzi, V. (2002) Feeding habits and trophic levels of
Mediterranean fish. Reviews in Fish Biology and Fisheries, 11: 217–254.
Strub P., Mesías, J.M., Montrecino, V., Ruttlant, J. and Salinas, S. (1998) Coastal
ocean circulation off western South America. In: Brink KH & AR Robinson (eds)
The global coastal ocean: the sea 11: 273-313. Wiley and Sons, Inc., New York, New
York.
Tanaka, H., Aoki, I. and Ohshimo, S. (2006). Feeding habits and gill raker
morphology of three planktivorous pelagic fish species off the coast of northern and
western Kyushu in summer. Journal of Fish Biology 68, 1041-1061.
Trenkel V.M.,and Rochet, M. (2003) Performance of indicators derived from
abundance estimates for detecting the impact of fishing on a fish community.
Canadian Journal of Fisheries and Aquatic Science, 60: 67-85
Tudela, S. (2004) Ecosystem effects of fishing in the Mediterranean: An analysis of
the major threats of fishing gear and practices to biodiversity and marine habitats.
General Fisheries Commission for the Mediterranean (FAO). Studies and Reviews,
74. 58 pp.
Van der Lingen, C.D., Shannon, L.J., Cury, P., Kreiner, A., Moloney, C.L., Roux, J.-
P. and Vaz-Velho, F. (2006) p. 147-184, Chapter 8 Resource and ecosystem
variability, including regime shifts, in the Benguela Current system. In: Shannon,
L.V., Hempel, G., Malanotte-Rizzoli, P., Moloney, C.L. and Woods, J. (Eds).
Benguela: Predicting a Large Marine Ecosystem. Elsevier, USA, Large Marine
Ecosystems Series 14. 410pp.
Verheye, H. M., Richardson, A. J., Hutchings, L., Marska, G. and Gianakouras, D.
(1998) - Long-term trends in the abundance and community structure of the coastal
zooplankton in the southern Benguela system, 1951-1996. In Pillar, S.C., Moloney,
C.L., Payne, A.I.L. and Shillington, F.A. (Eds). Benguela dynamics: impacts of
variability on shelf-sea environments and their living resources. South African Journal
of Marine Science, 19: 317-332.
Verheye, H.M., and Richardson, A.J. (1998) Long-term increase in crustacean
zooplankton abundance in the southern Benguela upwelling region (1951–1996):
bottom-up or top-down control? ICES Journal of Marine Science, 55: 803–807.
Wallace-Fincham, B.P. (1987) The food and feeding of Etrumeus whiteheadi
Wongratana 1983, off the Cape Province of South Africa. M.Sc. thesis, University of
Cape Town. 117 pp.
Walsh, J.J. (1981) A carbon budget for overfishing off Peru. Nature, 290: 300-304.
Walters, C., Christensen, V. and Pauly, D. (1997) Structuring dynamic models of
exploited ecosystems from trophic mass-balance assessments. Reviews in Fish
Biology and Fisheries, 7: 139-172.
Walters, C. and Kitchell, J.F. (2001) Cultivation/depensation effects on juvenile
survival and recruitment: implications for the theory of fishing. Canadian Journal of
Fisheries and Aquatic Science, 58: 39-50.
Wanless, S., Harris, M.P., Redman, P., and Speakman, J.R. (2005) Low energy values
of fish as a probable cause of major seabird breeding failure in the North Sea. Marine
Ecology Progress Series, 204: 1-8.
Winship, A.J. and Trites, A.W. (2003) Prey consumption of Steller sea lions
(Eumetopias jubatus) off Alaska: How much prey do they require? Fishery Bulletin,
101: 147-167.
Zavatarelli, M., Raicich, F., Bregant, D., Russo, A., Artegiani, A. (1998)
Climatological biogeochemical characteristics of the Adriatic Sea. Journal of Marine
Systems, 18: 227-263.
Zavodnik, D. (1991) On the food and feeding in the Northern Adriatic of Pelagica
noctiluca (Scyphozoa). Jellyfish blooms in the Mediterranean. Proc. of 2nd workshop
on Jellyfish in the Mediterranean Sea. UNEP, MAP technical reports series, 47: 212-
216.
Zotier, R., Bretagnolle, V. and Thibault, J.-C. (1999) Biogeography of the marine
birds of a confined sea, the Mediterranean. Journal of Biogeography, 26: 297-313.
Zupanovic, S. and Jardas, I. (1989) Fauna i flora Jadrana: Jabucka Kotlina. Logos,
Split. Institut za Oceanografiju i Ribarstvo.Vol IV.
Following is to be placed in a ‘box’ separate from the text:
Quick look at Ecopath with Ecosim (EwE)! • ECOPATH
Mass balance Ecopath models provide a quantitative representation, or snapshots, of marine ecosystems in terms of trophic flows and biomasses for a defined time period, usually a year. Model parameters are expressed in terms of nutrient or energy related currency per unit of surface (frequently expressed as t·km-2·yr-1 for fisheries applications) (Pauly et al. 2000, Christensen and Walters 2004).
The ecosystem is represented by functional groups, which can be composed of species, groups of species with ecological similarities or ontogenetic fractions of a species. The model is based on two linear equations that represent the energy balance among groups (production equation) and the energy balance within a group (consumption equation). For each group, the model describes a mass balance situation, where the energy removed from the ecosystem due to, for example, predation or fishing, is balanced by consumption.
(1) The production (P) of each functional group (i) is divided into predation mortality (M2ij) caused by the biomass of the other predators (Bj), exports from the system via fishing activity (Yi) and other exports (Ei), biomass accumulation in the ecosystem (BAi) and a baseline mortality or other mortality (1-EEi), where EE is the ecotrophic efficiency, or the proportion of the production of group (i) that is exported out of the ecosystem (e.g. by fishing) or consumed by predators:
∑ −++++=j
iiiiiijji EE1PBAEY2MBP )·(·
(1)
(2) The energy balance within each group is then ensured when consumption by group (i) equals the sum of production by (i), respiration by (i) and food that is unassimilated by (i).
Ecological analyses integrated in Ecopath can be used to examine many ecosystem features based on trophic flows and network analyses, thermodynamic concepts and information theory (Christensen and Walters, 2004; Cury et al., 2005).
• ECOSIM
The trophodynamic simulation module Ecosim (Walters et al., 1997) re-expresses the linear equations of the Ecopath model as difference and differential equations that dynamically respond to changes in fishing mortality and biomass. This enables the performance of dynamic simulations at the ecosystem level from the initial parameters of a baseline Ecopath model as follow:
( ) iiiiijii
i BeFMIQijQQP
dtdB
⋅++−+−⋅⎟⎟⎠
⎞⎜⎜⎝
⎛= ∑∑
(2)
where dBi/dt is the growth rate of (i) during the time interval dt in terms of Bi, (P/Q)i is the gross efficiency, Mi is the non-predation natural mortality rate, Fi is the fishing mortality rate, ei is the emigration rate, Ii is the immigration rate, and ei · Bi –Ii is the net migration rate. Consumption rates (Q) are calculated based upon the “foraging arena” theory where the biomass of (i) is divided into a vulnerable and a non-vulnerable fraction and the transfer rate υ between the two fractions is what determines the flow control (Walters et al. 1997, Christensen and Walters 2004). Default values of υ represent mixed flow control, whilst these values can be modified to represent bottom-up flow control and top-down flow control.
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