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Ecosystem effects of fishing & El Niño at the Galápagos Marine Reserve

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Ecosystem effects of fishing & El Niño at the #Galapagos Marine Reserve
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RT @nereusprogram: @nereusprogram fellow Tyler Eddy @tyzissou is a co-author on the article 'Ecosystem effects of fishing and El Niño at th…
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RT @nereusprogram: @nereusprogram fellow Tyler Eddy @tyzissou is a co-author on the article 'Ecosystem effects of fishing and El Niño at th…
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New paper out in @thePeerJ with Alan Friedlander and @PelayoSalinas @NG_PristineSeas: Ecosystem effects of fishing & El Niño at the Galápagos Marine Reserve @coru_ubc @DalScience @DarwinFound @nereusprogram https://t.co/lUxY4KQTis
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New paper out in @thePeerJ with Alan Friedlander and @PelayoSalinas @NG_PristineSeas: Ecosystem effects of fishing & El Niño at the Galápagos Marine Reserve @coru_ubc @DalScience https://t.co/omnQ83v65H
Aquatic Biology

Introduction

Understanding how environmental factors interact with exploitation of resources is a common concern among natural resource managers, biological conservationists, and scientists (Bender, Case & Gilpin, 1984). In the marine environment, it has been suggested that fishing magnifies fluctuations in natural populations due to removing older individuals of the population which changes demographic parameters such as intrinsic growth rates (Anderson et al., 2008). Removing top predators and keystone species from ecosystems can also cause trophic cascades and reshuffling of ecosystems (Worm et al., 2009; Smith et al., 2011; Collie et al., 2016). We are now in the Anthropocene and changes in environmental conditions are the greatest that they have ever been (Bopp et al., 2013), therefore, it is important to understand how populations are affected by the interaction between resource use and a changing world (Cheung, Reygondeau & Frölicher, 2016).

The Galapágos Archipelago hosts ecologically important, diverse, and fragile ecosystems with high levels of endemism (Edgar et al., 2010). The strong upweling of the eastward-flowing Cromwell Current on the western portion of the archipelago produces some of the world’s most productive tropical waters (Wolff, Ruiz & Taylor, 2012). This region is strongly affected by El Niño events when upweling slows causing water temperatures to increase and substantially reducing primary production flow through ecosystems resulting in dramatic declines in abundance of many species (Edgar et al., 2010; Wolff, Ruiz & Taylor, 2012).

For local people living in the Galapágos, fisheries are an important source of income. Landed fish are sold within the Archipelago to supply the rapidly growing tourism industry, as well as exported. The handline fishery for the regionally-endemic sailfin grouper (Mycteroperca olfax; locally referred to as bacalao) has operated since the 1920s and was once the most valuable fishery in the Galápagos, comprising over 40% of the mixed whitefish catch (Reck, 1983). More recently, bacalao has accounted for <10% of the finfish catch, with fishers indicating that catch rates and average individual size have declined significantly over time (Bustamante, 1998; Burbano et al., 2014; Schiller et al., 2015). Recent data indicate that 96% of bacalao caught are below reproductive size, with few large spawning individuals, and an extremely skewed sex ratio, suggesting eminent reproductive failure (Usseglio et al., 2016). Historical photographs from 1925 to 1938 indicate that average size of caught bacalao has declined from 77 to 47 cm in 2012 (Usseglio et al., 2016). The economic value of the fishery for bacalao has decreased tremendously over time and is not as economically important today as the fisheries for lobster (locally referred to as langosta; Panulirus penicillatus and P. gracilis), sea cucumber (locally referred to as pepino; Isostichopus fuscus) or pelagic fishes—mainly wahoo, yellowfin tuna, and swordfish (Acanthocybium solandri, Thunnus albacares, and Xiphias gladius, respectively).

In 1998, the Special Law of Galápagos established the Galápagos Marine Reserve, which excluded industrial fishing fleets within 40 nautical miles of the islands. The coastal zoning scheme for the Galápagos Marine Reserve implemented in 2000, closed some areas to fishing (approximately 20% of the coastline, however <1% of the entire Galápagos Marine Reserve), however compliance among fishers is poor—with many fishers claiming to not know the locations of protected areas—and there is little to no enforcement of closed areas (Castrejón & Charles, 2013; Usseglio, Schuhbauer & Friedlander, 2014). Socio-economic inputs dominated the selection process of no-take zones in the Galápagos Marine Reserve, with ecological considerations having a lower priority (Edgar et al., 2004; González et al., 2008; Castrejón & Charles, 2013). Other than no-take zones, there are no specific regulations for managing bacalao or any other finfish species within the Galápagos Marine Reserve.

The IUCN Red List currently categorizes bacalao as vulnerable due to its limited range and declining fishery catches (Erisman & Craig, 2018). The distribution of bacalao is limited to the offshore islands of Cocos, Costa Rica; Malpelo, Colombia; and Galápagos, Ecuador in the Tropical Eastern Pacific, however, it is rare at both Cocos and Malpelo (Marconi, Beck & Majluf, 2001). Bacalao is a top predator in the coastal ecosystems of the Galápagos and is a sequential hermaphrodite, as all individuals are born as females, and transition to males at approximately 12 years of age and 80 cm total length (Usseglio et al., 2015). The life history characteristics that make bacalao susceptible to overfishing, its ecological role within the Galápagos ecosystem, and its current threatened conservation status have prompted recent efforts to inform sustainable management of bacalao (Salinas-de-León, Rastoin & Acuña-Marrero, 2015; Usseglio et al., 2015, 2016).

Understanding the impacts of fisheries and environment on marine ecosystems is a central tenant of ecosystem-based fisheries management (Pikitch et al., 2004; Browman et al., 2004; Link, 2010). Ecosystem models are one tool that have been used extensively to understand ecosystem effects of fishing (Christensen & Walters, 2004; Worm et al., 2009; Smith et al., 2011; Collie et al., 2016), as well as to understand climate change impacts on marine ecosystems (Brown et al., 2010; Cornwall & Eddy, 2015; Payne et al., 2016, Cheung, Reygondeau & Frölicher, 2016). It is also important to understand how fisheries and environmental effects on ecosystems have changed through time, as exploited populations can have reduced roles within ecosystems—especially for keystone groups (Coll, Palomera & Tudela, 2009; Eddy et al., 2014). In the absence of detailed historical fisheries data, historical ecology, catch reconstructions, and fishers’ ecological knowledge are tools that can be used to estimate the biomass of unfished populations (Jackson et al., 2001; Johannes, Freeman & Hamilton, 2000; Rosenberg et al., 2005; Lotze et al., 2006; Pauly & Zeller, 2016).

Here, we use estimates of unfished bacalao, langosta, and pepino biomass to understand the magnitude of depletion throughout history. We employ existing ecosystem models for the Bolivar Channel (Ruiz & Wolff, 2011; Wolff, Ruiz & Taylor, 2012), in the cold western bioregion, and Floreana Island, in the warmer central bioregion (Okey et al., 2004), to run simulations of varying levels of bacalao fishing for unfished and modern periods. We then examine the impacts of bacalao fishing on its biomass and ecosystem role, as well as its impacts on other groups in the ecosystem and how these impacts change during El Niño years at the Bolivar Channel.

Methods

Ecosystem models

We used published Ecopath with Ecosim (EwE; Christensen & Walters, 2004; Christensen et al., 2008) models for Floreana Island (Okey et al., 2004) located in the warm, central bioregion and two models for Bolivar Channel, located in the cold, west bioregion, representing normal, and El Niño years (Ruiz & Wolff, 2011; Wolff, Ruiz & Taylor, 2012; Fig. 1). All three of these models include fisheries for bacalao. The Floreana Island model is available online from Ecobase (http://sirs.agrocampus-ouest.fr/EcoBase/), while the Bolivar Channel models are available by contacting the model developers.

Map of the Galápagos Marine Reserve (GMR) indicating ecosystem model locations at the Bolivar Channel and Floreana Island.

Figure 1: Map of the Galápagos Marine Reserve (GMR) indicating ecosystem model locations at the Bolivar Channel and Floreana Island.

Floreana Island

Floreana Island is located in the warm, central bioregion, characterized by a high regional mix of cold and warm-water biota (Fig. 1; Okey et al., 2004). The Floreana Island ecosystem model was parameterized for the rocky reefs surrounding the island between 0 and 20 m depth (partial depth range inhabited by bacalao), covering 6.44 km2 or 36% of the rocky reef habitat of the island. The model was parameterized for the time period 2000–2001, and is characterized by 42 functional groups including bacalao—estimated to have a trophic level of 4.2 (Table 1)—with prey groups that consisted of planktivorous reef fishes accounting for 60% of diet, small benthic invertebrate eating fishes accounting for 20% of diet, and 20% of diet represented by imports and informed by the literature (Okey et al., 2004).

Table 1:
Floreana Island ecosystem model characteristics and fishing simulation results.
Functional group TL Prey groups Unfished Modern
1 Sharks 4.4 3–12, 14, 17–19, 21, 22, 27, 29, 32–36 +
2 Toothed cetaceans 4.4 1, 3, 5–11, 21, 27, 32
3 Bacalao 4.2 12, 14 ‐‐‐ ‐‐‐
4 Birds 4.1 3, 6, 7, 9–12, 14, 15, 18, 21, 27, 32
5 Sea lions 4.0 3, 6, 8–10, 12, 14, 21, 27 + +
6 Pelagic predators 3.9 7, 11, 18, 21, 32 + +
7 Non-commercial reef predators 3.8 12, 14, 15, 18, 19, 21, 37, 39, 43 ++ +
8 Octopods 3.5 7, 10–12, 14, 16–19, 21, 38 +
9 Pelagic planktivores 3.4 15, 19, 37, 39, 40
10 Other commercial reef predators 3.3 11, 12, 15, 18, 19, 22, 24, 37, 39
11 Large benthic invertebrate eaters 3.3 13, 16–19, 21, 24, 28, 31, 35, 36, 38
12 Planktivorous reef fishes 3.3 15, 39, 40 + +
13 Hexaplex gastropod 3.0 38, 43
14 Small benthic invertebrate eaters 3.0 15, 19, 22, 24, 25, 28, 31, 37–39, 41–43 + +
15 Carnivorous zooplankton 2.8 39, 40
16 Spiny lobsters 2.8 19, 20, 22–24, 26, 28, 35, 36, 38, 41–43
17 Slipper lobster 2.7 12, 14, 18, 19, 21, 22, 24, 28, 35, 36, 38, 42, 43
18 Omnivorous reef fishes 2.7 15, 19, 23–25, 28, 37–39, 41–43
19 Shrimps and small crabs 2.6 12, 14, 15, 21, 23–25, 28, 37–43
20 Asteroids 2.5 19, 23–25, 28, 30, 38, 41–43
21 Other herbivorous fishes 2.4 15, 28, 37, 39, 42, 43
22 Eucidaris urchin 2.2 25, 42, 43 + +
23 Anemones 2.2 13, 15, 19, 20, 22, 24–26, 28, 30–31, 34–43 + +
24 Worms and ophioroids 2.2 15, 25, 28, 37–43
25 Stony corals 2.2 15, 39–43
26 Chitons 2.2 15, 41–43 +
27 Detritivorous fishes 2.1 39–43
28 Small gastropods 2.1 24, 25, 37, 38, 41–43 + +
29 Sea turtles 2.1 15, 42 + +
30 Sea cucumbers 2.1 23, 24, 41, 43 + +
31 Other urchins 2.0 25, 41–43
32 Parrotfishes 2.0 25, 41–43 + +
33 Marine iguana 2.0 42 + +
34 Other sea cucumbers 2.0 40, 42, 43
35 Tripneustes urchin 2.0 42, 43 + +
36 Lytechinus urchin 2.0 42, 43 + +
37 Small crustaceans 2.0 40–43
38 Filter + suspension feeders 2.0 40, 43
39 Herbivorous zooplankton 2.0 40, 43
40 Phytoplankton 1.0
41 Microphytobenthos 1.0 + +
42 Benthic algae 1.0 + +
43 Detritus 1.0
DOI: 10.7717/peerj.6878/table-1

Note:

Floreana Island ecosystem model characteristics and results indicating direction and magnitude of change in biomass of functional groups at modern levels of bacalao depletion (85%) compared to unfished bacalao biomass (1 − (Bi/B0)) for unfished and modern versions of the model (TL = trophic level; ‐ = ‐ <20% change, ‐‐ = ‐ >20% and ‐ <40% change, ‐‐‐ = >40% change; + = <20% change, ++ = >20% and <40% change, +++ = >40% change).

Floreana Island production, consumption, and diet data were mostly derived from the literature; biomass estimates of benthic, demersal, and pelagic fish groups, large invertebrates, birds, turtles, sharks, and marine mammals were based on site-specific observations; and primary production was estimated from ocean color satellite data (Okey et al., 2004).

Bolivar channel

The Bolivar Channel is located in the cold west bioregion, characterized by cool, nutrient rich, upwelled waters, and associated biota including dense macroalgae beds, the world’s only tropical penguin, and the flightless cormorant (Fig. 1; Ruiz & Wolff, 2011). The Bolivar Channel ecosystem model was parameterized for rocky habitat between 0 and 30 m depth surrounding Isabela and Fernandina islands, covering 44 km2 or 14% of the total Bolivar Channel area (Ruiz & Wolff, 2011; Fig. 1). This model represents the average ecosystem state for the years 2004–2008, and includes 30 different functional groups, including bacalao, with a predicted trophic level of 3.39 (Table 2), and a diet of 26% sea stars and sea urchins, 20% benthic omnivorous fishes, 9% small planktivorous reef fishes, 8% surgeonfish, chubs, and giant damselfishes, 7% mullets, 6% benthic predatory fish, 5% gorgonians, and six other groups each accounting for <5% of total diet (Ruiz & Wolff, 2011). There was also a Bolivar Channel model that was forced using a 16-year time series of satellite-derived phytoplankton biomass from 1994 to 2009, which included the strong El Niño of 1997–1998 (Wolff, Ruiz & Taylor, 2012; Table 2). The El Niño version of the model has a primary productivity reduction of 76% relative to the non El Niño model (Wolff, Ruiz & Taylor, 2012).

Table 2:
Bolivar Channel ecosystem model characteristics and fishing simulation results.
Functional group TL Prey groups Direction and magnitude of biomass change
Unfished non El Niño Modern non El Niño Unfished El Niño Modern El Niño
1 Phytoplankton 1.00 + - - -
2 Macroalgae + others 1.00 + + - -
3 Surgeonfishes, chubs and giant damiselfishes 2.00 2, 30 + + ++ +
4 Sea cucumbers and other 2.00 30 + + + +
5 Herbivorous zooplankton 2.00 1, 2, 30 - - - -
6 Sea turtles and marine iguanas 2.01 2, 5, 30 - - - -
7 Small herbivorous gastropods 2.01 2, 5, 30 - - - - -
8 Sponges and polychaetes 2.01 1, 5, 18, 30 - + - -
9 Gorgonians 2.07 1, 5, 18, 30 + - ++ +
10 Parrotfishes 2.11 2, 9, 30 - - + - -
11 Mullets 2.11 1, 5, 30 ++ + +++ +
12 Benthic omnivorous fishes 2.14 1, 2, 5, 30 ++ + ++ +
13 Anemones and zooanthids 2.14 1, 5, 18, 30 - + - - -
14 Sea stars and sea urchins 2.28 2, 8, 9, 13, 19, 30 - - + -
15 Planktivorous reef fishes 2.34 1, 5, 18, 30 + + +++ +
16 Small planktivorous reef fishes 2.47 1, 5, 18, 30 - - ++ +
17 Lobsters 2.64 2, 14, 30 - - + +
18 Predatory zooplankton 2.80 1, 5, 30 - - - - -
19 Large gastropods and other sea stars 2.92 2, 7, 9, 13, 14, 20, 30 + + + +
20 Small predatory gastropods 2.96 5, 7–9, 13, 18, 30 + + ++ +
21 Small benthic predatory fishes 3.19 5, 11, 12, 14, 16, 18 +++ ++ +++ ++
22 Benthic predatory fishes 3.36 3, 7, 11, 12, 14, 16, 17, 20, 21, 23, 24 +++ + ++ +
23 Barracudas 3.37 3, 11, 12, 15, 16, 21, 22 +++ + +++ +
24 Groupers 3.39 3, 7, 11, 12, 14, 15–17, 20–23 - - - - - - - - - - - -
25 Jacks and mackerels 3.40 3, 11, 16 - - - +++ +
26 Rays 3.43 4, 14, 17, 19 - - - -
27 Predatory marine mammals 3.49 10, 11, 12, 15–17, 19, 21–25, 29 +++ + +++ -
28 Seabirds 3.50 3, 11, 16, 23 - - +++ +
29 Sharks 3.89 6, 11, 12, 16, 21–23, 25–27 +++ + +++ +
30 Detritus 1.00 - + - -
DOI: 10.7717/peerj.6878/table-2

Note:

Bolivar Channel ecosystem model characteristics and results indicating direction and magnitude of change in biomass of functional groups at modern bacalao level of depletion (85%) compared to unfished bacalao biomass (1 − (Bi/B0)) for unfished and modern versions of the El Niño and non El Nino models (TL = trophic level; (TL = trophic level; - = - <20% change, - - = - >20% and - <40% change, - - - = >40% change; + = <20% change, ++ = >20% and <40% change, +++ = >40% change).

Bolivar Channel production, consumption, and diet parameters were estimated from the literature, while biomass estimates of fish, invertebrate, sea bird, marine mammal, and reptile were based on observations from within the model area (Ruiz & Wolff, 2011; Wolff, Ruiz & Taylor, 2012). Primary production estimates were derived from satellite observations of ocean color, while zooplankton biomass was estimated from observational data (Ruiz & Wolff, 2011; Wolff, Ruiz & Taylor, 2012).

Unfished biomass estimates

To understand the ecosystem impact of bacalao fishing through time in the absence of stock assessments, we estimated unfished biomass of the most heavily exploited species (bacalao, langosta, and pepino), using a variety of sources. Burbano et al. (2014) interviewed fishers of different ages, asking them to recall their best catches of bacalao. Older fishers indicated a 6.82-fold decline in their best catches from the 1940–1950s compared to 2010. Ruttenberg (2001) surveyed reef fishes using underwater visual surveys in the Galápagos Marine Reserve at both lightly and heavily fished areas in 1998, and found 22-fold less biomass in heavily fished areas. Schiller et al. (2015) performed catch reconstructions at the Galápagos Islands, however did not provide specific values of catches or biomass of bacalao. Pepino were estimated at six- to eightfold greater biomass when unfished (Okey et al., 2004) and there has been a 10-fold decrease in catch per unit effort (CPUE; Defeo, Castilla & Castrejón, 2009). Langosta are reported to be 10-fold greater in the more remote northern Darwin and Wolf Islands (Edgar et al., 2010). We applied the bacalao multiplier of 6.82 from Burbano et al. (2014) to the modern biomass values to estimate unfished biomasses in each of the three ecosystem models. We applied unfished biomass multipliers of seven for pepino (mean value from Okey et al., 2004) and 10 for langosta (Edgar et al., 2010).

Modeling strategy

We simulated a range of bacalao fisheries mortality rates (F)—from no exploitation (F = 0) to local extinction—using the Floreana Island and Bolivar Channel models to understand the ecosystem effects of fishing (sensu Eddy et al., 2015). For the modern models, we held fishing mortality (F) of all other exploited groups constant at their most recent levels. For the unfished models, we removed all fishing morality aside from that for bacalao. Simulations were run until the end of their historical time series when available, and then run for 100 years to allow models to reach equilibrium following the change in bacalao fishing mortality. Additionally, in order to understand the ecosystem effects of bacalao exploitation during El Niño years, we ran a similar range of exploitation rates of bacalao using the Bolivar Channel El Niño model. Only the Bolivar Channel El Niño model was fit to time series data to tune vulnerability values. In the absence of model fits to time series for the other two models, we used the default vulnerabilities.

In order to standardize exploitation levels across all models, we calculated the level of bacalao depletion as the proportion of biomass compared to unfished biomass (1(Bi/B0)). We report ecosystem effects for 60% depletion as this is a common target used in fisheries management (Worm et al., 2009; Smith et al., 2011). We calculated maximum sustainable yield (MSY) as the maximum bacalao catch produced by any simulation.

Ecosystem impacts

We calculated the ecosystem impacts of varying levels of bacalao exploitation on the biomasses of all other functional groups in the ecosystem. We represent the biomasses of the other functional groups as the proportion of their biomass when bacalao was fished at the level of depletion i (Bi) compared to the biomass when bacalao was unfished (B0). This impact is analgous to the interaction strength index developed by Okey (2004) presented in the original Floreana Island EwE model description (Okey et al., 2004).

Keystone species are those that display disproportionately large impacts on the biomasses of other groups in an ecosystem compared to their biomass (Power et al., 1996). Keystone values of bacalao in each of three models for each time period were calculated by EwE using the mixed trophic analysis which quantifies how much other functional groups are impacted in their biomass (Christensen & Walters, 2004) and the keystone index developed by Libralato, Christensen & Pauly (2006) which quantifies how the ecosystem impacts relate to the biomass of the impacting group. The Okey (2004) dynamic keystoneness index more explicitly accounts for the relative biomass of the impacting group, whereas the Libralato, Christensen & Pauly (2006) keystone index tends to emphasize interaction strength. We compare the results from both approaches in the discussion.

Sensitivity analysis

To assess how sensitive model results were to parameter estimates, we performed a sensitivity analysis on bacalao unfished biomass estimates and bacalao diet. For the three unfished models, instead of using the 6.82 bacalao biomass multiplier, we used a conservative estimate of half of the biomass multiplier of 3.41. Using this conservative estimate, we ran the same fishing simulations as above. We compared the results of these simulations to the results from the original unfished models and calculated sensitivity as the difference in ecosystem impacts that resulted from 100% bacalao depletion (local extinction), as these simulations produced the greatest ecosystem impacts—measured as biomass changes in other functional groups. As indicated above, using the multiplier of 22 times more bacalao biomass in unfished versions of the model did not produce simulations that reached equilibrium. We also examined the effect of switching bacalao diets from the Floreana model to the Bolivar Channel models and vice versa. The only stomach content analysis of bacalao indicates that it is piscivorous (Rodriguez, 1984). The Floreana bacalao diet is piscivorous, therefore the Bolivar Channel model was run with the Floreana diet to represent a piscivorous bacalao diet. We examined model sensitivity in the same way as for biomass, and also by comparing the estimated trophic levels of bacalao with each diet. The Bolivar Channel El Niño model parameterized with the Floreana diet did not reach equilibrium during simulations and therefore results are not presented.

Results

Ecosystem role of bacalao

Unfished biomass versions of the Bolivar Channel El Niño and non El Niño ecosystem models indicated much greater ecosystem impacts of bacalao exploitation compared to the modern day models (Fig. 2). In the unfished non El Niño model, at the modern level of bacalao depletion (85%), 38% of functional groups were impacted by at least a 20% change in biomass, while 21% of functional groups were impacted by at least a 40% change in biomass (Table 1; Fig. 2A). In the modern day model, at the current level of bacalao depletion (85%), 21% and 7% of functional groups were impacted by at least 20% and 40% biomass, respectively (Table 1; Fig. 2B). There was an even greater impact of bacalao exploitation in the unfished El Niño version of the Bolivar Channel model, where at 85% bacalao depletion, 62% and 34% of functional groups were impacted by at least 20% and 40% of their biomass, respectively, compared to when bacalao was unfished (Table 1; Figs. 2C and 2D). The modern day version of the model also showed much smaller ecosystem impacts, similar to the modern day non El Niño model at modern level of depletion (85%), with 7% and 3% of functional groups impacted by 20% and 40% of biomass compared to when bacalao was unexploited (Table 1; Figs. 2B and 2D).

Trade-offs between ecosystem impacts and catches of bacalao as a function of fishing exploitation for different EwE models during historical and modern times.

Figure 2: Trade-offs between ecosystem impacts and catches of bacalao as a function of fishing exploitation for different EwE models during historical and modern times.

Ecosystem impact is represented as the proportion of trophic groups other than bacalao with a biomass change of by at least 20% (blue line) or 40% (red line) of their unfished biomass. Modern level of bacalao depletion (LOD) is represented by the yellow line. Catch is plotted on the secondary axis as a proportion of maximum sustainable yield (MSY). (A) Unfished Bolivar Channel; (B) Bolivar Channel; (C) Unfished Bolivar Channel El Niño; (D) Bolivar Channel El Niño; (E) Unfished Floreana Island; (F) Floreana Island.

The functional groups that differed in biomass the most at modern bacalao level of depletion (85%) in the unfished non El Niño Bolivar Channel model compared to the modern day version with increased biomasses were: phytoplankton, gorgonians, mullets, benthic omnivorous fishes, small benthic predatory fishes, benthic predatory fishes, predatory marine mammals, and sharks (Table 1). Groups that showed decreased biomasses in their unfished non El Niño model compared to the modern day version were: small herbivorous gastropods, sponges and polychaetes, parrotfishes, anemones and zooanthids, jacks and mackerels, and detritus (Table 1). Comparing the two El Niño Bolivar Channel models at modern bacalao levels of depletion, functional groups that were at greater biomass in the unfished model compared to the modern day version were: surgeonfishes, chubs and giant damiselfishes, gorgonians, mullets, benthic omnivorous fishes, sea stars and sea urchins, planktivorous reef fishes, small planktivorous reef fishes, small predatory gastropods, small benthic predatory fishes, barracudas, jacks and mackerels, predatory marine mammals, seabirds, and sharks (Table 1). Functional groups that showed the greatest biomass decreases were: anemones and zooanthids and predatory zooplankton (Table 1).

The unfished bacalao biomass version of the Floreana Island model showed greater influence of bacalao compared to the modern version (Table 2; Figs. 2E and 2F). In the unfished biomass model, at 85% bacalao depletion, 5% of functional groups were impacted by at least 20% biomass, while 2% were impacted by 40% of their biomass (Table 1; Fig. 2E). Only 3% and 2% of groups were impacted by both 20% and 40% of their biomass, respectively in the modern day model when bacalao was depleted by 85% (Table 2; Fig. 2F). The functional groups most impacted by 85% bacalao depletion in the unfished biomass model were sharks, non-commercial reef predators, and chitons which were all at greater biomasses compared to modern day, while octopods had lower biomass in the unfished model (Table 2).

Tradeoffs between bacalao catch and ecosystem impacts

The modern level of bacalao exploitation of 85% depletion is higher than that predicted to yield MSY in all six ecosystem models (Fig. 2). Unfished biomass MSY was predicted to occur at lower levels of exploitation in the El Niño Bolivar Channel and Floreana models (44% and 38% depletion, respectively) compared to the modern day versions (45% and 58% depletion, respectively; Figs. 2C2F). The non El Niño Bolivar Channel models predicted MSY to occur at 45% depletion at unfished biomass and 43% in the modern day (Figs. 2A and 2B). In all of the unfished models, fishing at levels producing MSY compared to the modern day exploitation rate (vertical yellow lines) reduces ecosystem impacts, and increases fisheries catches (Fig. 2). The reduction of ecosystem impacts by reducing fishing depletion to MSY levels is greatest for the unfished Bolivar Channel models (Figs. 2A and 2C). In the unfished Floreana model, reducing fishing depletion to MSY levels results in decrease in functional groups impacted by both 40% and 20% of their biomass (Fig. 2F). In the modern versions of all models, the ecosystem role of bacalao has been diminished due to greater levels of depletion (Figs. 2B, 2D and 2F). In the Bolivar Channel models, reducing fishing pressure to MSY levels decreases ecosystem impacts (Figs. 2A2D).

It is clear that the reduction of bacalao biomass due to fishing represented in the modern models has resulted in a diminished ecosystem role (Fig. 2). By comparing the Bolivar Chanel models during El Niño and non El Niño years and during unfished and modern states, it is possible to weigh the relative effects of fishing through top-down trophic control and environmental conditions that affect bottom-up primary production (Fig. 2). Comparatively, the El Niño models do show opposite responses in the unfished and modern models, whereby ecosystem effects of bacalao exploitation get amplified during El Niño unfished, while in the modern Bolivar Channel models, ecosystem impacts of bacalao exploitation are diminished during El Niño (Figs. 2A2D).

Keystone role of bacalao

In the unfished versions of all three models, the keystone role (Libralato, Christensen & Pauly, 2006) of bacalao was greater than in modern versions of the models (Fig. 3). Of the unfished models, bacalao showed the greatest keystone value in the Bolivar Channel, followed by the El Niño version of the Bolivar Channel, and Floreana Island (Fig. 3). For the modern day models, this ranking remained the same, however, all of the values were lower, indicating a diminished keystone role (Fig. 3).

Keystone values (Libralato, Christensen & Pauly, 2006) for bacalao during unfished and modern time periods for the Galápagos EwE models.

Figure 3: Keystone values (Libralato, Christensen & Pauly, 2006) for bacalao during unfished and modern time periods for the Galápagos EwE models.

RTI, relative total impact.

Sensitivity analysis

Reducing unfished bacalao biomass reduced the ecosystem effects of bacalao exploitation (Table 3). The greatest reduction in ecosystem impacts was observed for the Bolivar Channel El Niño model, which also showed the greatest ecosystem impacts during simulations with the greater estimate of unfished bacalao biomass (Fig. 2). Similarly, for the unfished Bolivar Channel and Floreana models, reduced bacalao biomass also reduced ecosystem impacts (Table 3; Fig. 2). Swapping the Floreana and Bolivar Channel bacalao diets led to increased ecosystem impacts in both cases. Swapping diets reduced bacalao trophic level at Floreana decreased from 4.2 to 4.0, while it increased bacalao trophic level at Bolivar Channel from 3.4 to 3.5.

Table 3:
Sensitivity analysis results from reducing unfished bacalao biomass and from switching bacalao diets from the Floreana model to the Bolivar Channel models and vice versa.
Sensitivity scenario Per cent change in number of functional groups impacted by >±40% of their biomass Per cent change in number of functional groups impacted by >±20% of their biomass
Bolivar Channel unfished with reduced bacalao biomass −10% −24%
Bolivar Channel El Niño unfished with reduced bacalao biomass −24% −24%
Floreana unfished with reduced bacalao biomass −2% −12%
Bolivar Channel with Floreana diet +7% +7%
Floreana with Bolivar diet 0 +4%
DOI: 10.7717/peerj.6878/table-3

Note:

Results are from simulations that produced the maximum ecosystem impacts (100% bacalao depletion).

Discussion

Impact of bacalao fishing

We have shown how the ecosystem role of bacalao has been greatly diminished with overexploitation—which has depleted the stock by 85% compared to unfished levels. This reduced biomass has led to decreases in the ecosystem role played by bacalao in all models examined, through direct and indirect feeding interactions with other groups. We did not observe any local extinctions of other species when bacalao was fished to local extinction, however, there were large changes in biomass of many functional groups, indicating large ecosystem reshuffling. Our results also suggest that bacalao catches could be much greater if their populations were allowed to recover to approximately half of their unfished biomass. This recovery would also reduce ecosystem impacts, creating a win-win situation. The cost associated with such a management action would be a short-term reduction in fisheries catches, which would allow stocks to recover to levels that produce MSY. Such trade-offs among ecological, economical, and societal factors are a central tenant of fisheries policy and management, and have been examined in detail in many marine ecosystems (Worm et al., 2009; Smith et al., 2011; Eddy et al., 2017).

Ecosystem role of groupers

Our results indicate that when unfished, bacalao has a much greater keystone role in all three models, also reflected by greater ecosystem effects when unfished with dynamic simulations of bacalao exploitation. A low bacalao keystone value was also reported for the modern Floreana Island model using a different keystone index, adding confidence to our findings (Okey, 2004; Okey et al., 2004). Recent work indicates that bacalao are extremely size over-fished, suggesting that their modern diet could be different than historically (Usseglio et al., 2016). These observations are consistent with other studies that have quantified the change in keystone role of species resulting from intensive exploitation, such as dolphins in the northwest Mediterranean (Coll, Palomera & Tudela, 2009), and lobster (Jasus edwardsii) in New Zealand (Eddy et al., 2014). For lobster in New Zealand, the increase in keystone role resulted from a density-dependent change in their diet in unfished areas where greater lobster biomass was observed, where they were more generalist and herbivorous, resulting in decreased trophic level (Freeman, 2007; Jack, Wing & McLeod, 2009). Currently, it is unclear how the diet of bacalao at the Galápagos may have changed since historical times when they were found in much higher abundance, but previous work has shown bacalao to be highly piscivorous (Rodriguez, 1984). Our sensitivity analysis indicates that a change in bacalao diet is a source of variation in ecosystem impacts, however not as great as impacts due to reduced biomass due to fishing.

The aim of using non-traditional, quantitative sources such as fishers’ ecological knowledge is to extend time series to avoid the “shifting baseline syndrome” (Pauly, 1995) in order to provide appropriate targets for fisheries management and conservation (Rosenberg et al., 2005; Eddy, Gardner & Pérez-Matus, 2010; Burbano et al., 2014; Eddy, Cheung & Bruno, 2018). It has been found that a greater sample size of interviewed fishers leads to less biased estimates of past fishing activities (Shepperson et al., 2014). The study that informed our unfished bacalao biomass estimate interviewed 124 fishers, accounting for 24% of the fishing population (Burbano et al., 2014).

Groupers are particularly vulnerable to overexploitation due to their life history characteristics (Sadovy de Mitcheson et al., 2013; Usseglio et al., 2015). A massive decline in the IUCN designated “endangered” goliath grouper (Epinephelus itajara) was documented in south Florida USA, using old photographs of winning catches from fishing competitions that indicated a 86% decline in grouper populations from 1956 to 1979, and newspaper accounts dating back to 1923 suggested that the population was already impacted by fishing prior to 1950 (McClenachan, 2009). The prey of goliath grouper likely benefited directly by this large reduction in predation by grouper, and we would also expect indirect negative effects on prey of grouper prey through meso-predator release, as well as increased competition among grouper prey with other species (McClenachan, 2009). In our simulations, the groups that benefitted most from bacalao exploitation in the Bolivar Channel were anenomes and zooanthids for both El Niño and non El Niño models; parrotfishes and sponges and polychaetes for the non El Niño model, and predatory zooplankton in the El Niño model. Following the strong 1997–1998 El Niño, anemone barrens were observed, providing new benthic habitat for colonization (Okey, Shepherd & Martínez, 2003). For Floreana Island, octopods benefitted from bacalao exploitation. All of these increases were due to indirect feeding interactions, highlighting ecosystem cascades that result from removing a key species.

Unfished biomass estimates

Working with data poor study systems and trying to reconstruct historical ecosystem states often requires using qualitative information sources that have a high amount of uncertainty in parameter estimates (McClenachan, 2009; Schiller et al., 2015). We only presented results for the lower estimate of unfished bacalao biomass, because the higher estimate of 22-fold more bacalao from surveys (Ruttenberg, 2001) caused the model to become highly unbalanced, without an equilibrium being reaching during simulations. Therefore, our simulations should be considered a conservative estimate of unfished bacalao biomass. We acknowledge that this is one of many hypotheses of how the unfished ecosystem may have looked. Species other than those that were primarily targeted by the artisanal fishery have also been exploited, through bycatch, bait or subsistence fisheries.

Bacalao diet estimates

The results from the food-web modeling approach that we have employed here are dependent on diet preferences specified in the models. As above, bacalao diet composition varies substantially between the two models. Therefore, we can think of these two different ecosystem models as alternate hypotheses of ecosystem structure and function at the Galápagos Islands, which can be further tested and refined as future data become available. It should also be noted that these two model areas are located in different bioregions with different community compositions, which likely contribute to differences in diet. Surveys do not indicate higher abundances of bacalao in no-take areas, likely due to lack of compliance and enforcement (Edgar et al., 2004), which has also been observed for lobster (Buglass et al., 2018). In the future, if these areas do provide bacalao populations protection from fishing, they will be an invaluable resource to understand not only how bacalao diet composition changes as biomass increases, but also how the biomasses of all other species in the ecosystem change as a result of direct and indirect interactions.

Fisheries management in a changing world

Understanding the impact that regular, although not always predictable, environmental events, such as El Niño have on ecosystems is extremely important for ecosystem-based fisheries management, as exploitation of marine resources does not occur in isolation—these events impact species of conservation interest and species of importance for the tourism sector (Lynham et al., 2015; Salinas-de-León et al., 2016). The cold-west upwelling region of the Galápagos is particularly sensitive to El Niño events, which result in increased water temperatures and large declines in primary production (Wolff, Ruiz & Taylor, 2012) with catastrophic effects on many marine species (Okey, Shepherd & Martínez, 2003; Okey, 2004; Edgar et al., 2010). Climate change projections for the Galápagos Islands from an ensemble of Earth system models indicate an increase in primary production under the strong mitigation of emissions scenario (RCP 2.6; Bopp et al., 2013). However, the business as usual emissions scenario (RCP 8.5) indicates a decrease in primary production (Bopp et al., 2013), which could lead to an ecosystem state observed in Bolivar Channel El Niño model. Considering the relative contributions of bacalao fishing and environmental factors to changes in simulated ecosystem effects, our results indicate that reduced bacalao biomass through overexploitation has produced greater ecosystem effects than El Niño. This finding is similar to another study which concluded that the ecosystem effects of fishing greatly outweighed projected impacts of ocean acidification (Cornwall & Eddy, 2015).

Bacalao is not the only species that has been heavily exploited at the Galápagos, as there have been collapses of pepino (sea cucumber) and langosta (lobster) fisheries in recent history (Bustamante, Okey & Banks, 2008). Additionally, the Galápagos Archipelago is home to a number of species of conservation interest, and understanding the trophic relationships that mediate direct and indirect interactions among these species is imperative to understand how the decline or recovery of one species will affect others. This approach is the basis of ecosystem-based fisheries management, which sets the management unit at the scale of ecosystem rather than individual populations. This study, along with other recent studies describing life history (Usseglio et al., 2015), reproductive behavior (Salinas-de-León, Rastoin & Acuña-Marrero, 2015), fishery bycatch and discards rates (Zimmerhackel et al., 2015), and fisheries characteristics (Usseglio et al., 2016) of bacalao will allow for an evidence-based management plan for this species, to be developed in partnership with the fisheries managing authority, the Galápagos National Park Directorate, and stakeholders such as fishers, the tourism industry, and environmental NGOs.

Conclusions

Using multiple lines of evidence about how exploited populations have changed through time, we have created hypotheses about how unfished ecosystems at the Galápagos may have been structured. The large reduction in bacalao biomass due to fishing has reduced its ecosystem role through direct and indirect feeding interactions. Allowing bacalao populations to recover to approximately half of their unfished biomass will partially restore their ecosystem roles as well as provide greater fisheries productivity.

Supplemental Information

Output simulation data.

Output simulation data used for Fig. 2

DOI: 10.7717/peerj.6878/supp-1

Keystone simulation data.

Keystone simulation data used to create Fig. 3.

DOI: 10.7717/peerj.6878/supp-2