Elsevier

Ecological Modelling

Volume 368, 24 January 2018, Pages 41-51
Ecological Modelling

Research Paper
Long-term structural and functional changes driven by climate variability and fishery regimes in a sandy beach ecosystem

https://doi.org/10.1016/j.ecolmodel.2017.11.007Get rights and content

Highlights

  • Long-term structural and functional changes were assessed in a sandy beach ecosystem.

  • Trophic models showed a combined effect of climate variability and fishing intensity.

  • Mass mortalities of a harvested clam were reflected at population and ecosystem levels.

  • Clam mortalities and stock recovery occurred with low and high system productivity respectively.

  • Temporal simulation showed that climate variability shaped ecosystem function and structure.

Abstract

Structural and functional changes in a sandy beach ecosystem in the southwestern Atlantic (Barra del Chuy, Uruguay) were assessed by contrasting four Ecopath trophic models and performing temporal dynamic simulations using Ecosim. Each model (1982, 1989, 1996 and 2012) represents a historical period of a clam fishery in which regulatory structure, management tools and resource status varied substantially. The results showed that this land-ocean interface experienced significant changes reflected at the population and ecosystem levels, owing to a combined effect of fishing and climate variability. Most system biomass (excluding phytoplankton and detritus) consisted of benthic invertebrates. Phytoplankton increased significantly over time, whereas the biomass of benthic macrofaunal components varied among the periods due to bottom-up processes, mass mortalities of the harvested clams and fishing intensity. Major fishing impacts on the targeted clam and mass mortalities occurred concurrently with low phytoplankton biomass, and clam recovery occurred in the absence of harvesting and increasing primary production. Ecosystem-level attributes (e.g., Total System Throughput, Ascendency) showed considerable temporal fluctuations, which were primarily related to changes in system productivity associated with a climatic shift from a cold phase to a warm phase and increasing onshore winds. An analysis of robustness and order showed an ecosystem state lacking the flexibility to adapt to new perturbations. Dynamic simulations showed the prominent bottom-up role of environmental variability on ecosystem function and structure. Temporal dynamics is conducted by changes in primary production forced mainly by temperature patterns. The concurrent role of climate variations and fishing explained the long-term dynamics of this ecosystem, suggesting that sandy beaches are fragile social-ecological systems whose services are increasingly threatened by long-lasting stressors.

Introduction

The proper function of marine ecosystems is essential to sustain the services that they provide (Balvanera et al., 2014). However, diverse human activities impose a complex blend of effects on ecosystems (Costanza, 1998). Management of human activities in marine environments has evolved to better account for anthropogenic impacts and natural variability toward sustainable ecosystem services. In this setting, the Ecosystem Approach (SCBD, 2004) has been developed as a planning procedure that integrates the management of human activities, considering the structure and function of the ecosystems. Usually, this approach requires practitioners to “identify and take action on influences that are critical to the health of ecosystems, thereby achieving sustainable use of ecosystem goods and services and maintenance of ecosystem integrity” (Borja et al., 2016). The ecosystem approach to fisheries (EAF) has been adopted to integrate the conservation of the structure, diversity and function of ecosystems and the fisheries management actions taken to satisfy societal demands for food and economic benefits (Garcia et al., 2003).

Fishery collapses may result from a combination of bottom-up (environmental) and top-down (fishing) effects, e.g., overfishing and recruitment failures caused by adverse environmental conditions (Larkin, 1996, Boudreau et al., 2015). Therefore, it is necessary to understand the species interactions along with the abiotic variables while recognizing the responses of fishers to changes in stock abundance. In particular, EAF requires an integrated system analysis that can differentiate between the human and natural factors underlying resource variability and ecosystem health. In this vein, climate variability strongly influences ocean productivity and these changes dramatically affect coastal marine ecosystems (Hoegh-Guldberg and Bruno, 2010). This is particularly noticeable in intertidal habitats that harbor valuable benthic small-scale fisheries (Defeo et al., 2016), where harvesting and environmental drivers acting together may alter demographic and life history traits of harvested species, and may propagate to higher-order ecological effects, such as disruptions of food-web linkages (Defeo et al., 2013).

Food web-based metrics are fundamental measures of ecosystem structure and function (Cury and Christensen, 2005, Libralato et al., 2014), which convey information about the dynamics, patterns and processes of fisheries management (ICES, 2014). Fisheries regulation, pollution reduction, pest control and other management activities benefit from information about food web components, which are also necessary for defining the environmental sustainability of marine ecosystems (Fath, 2015, EU Directive, 2008). Some food web indicators are potentially useful as proxies for decision criteria in EAF (Link, 2002, Shannon et al., 2014), including the mean trophic levels of the catches and the primary production required to sustain the fisheries (Pauly et al., 1998, Branch et al., 2010). Moreover, comparative modeling studies in which trophic representations of the same system are developed for different time periods (Shannon et al., 2014, Coll et al., 2009) allow comparisons of the changes in ecosystem structure and trophic relationships due to fishing, environmental perturbations, or combinations thereof (Corrales et al., 2015). In this way, modeling can provide scientifically based information on ecosystem health to regulatory and management systems, and constitute an essential input in data-poor situations, such as in the benthic small-scale fisheries referred above.

In Latin America, few studies have focused on analyzing the changes in food web structure in relation to resource management and environmental variations (Ortiz and Wolff, 2002, Neira et al., 2014). Barra del Chuy beach (BCB) is an exposed intertidal ecosystem on the Atlantic coast of Uruguay with a rich and abundant benthic community (Defeo et al., 1992). In this highly productive ecosystem, seabirds, fishes and gastropods are top predators (Lercari et al., 2010). The trophic function of this system, elucidated through stable isotopes, shows the combined importance of autochthonous phytoplankton and terrestrial organic matter infueling the food web (Bergamino et al., 2013). The yellow clam (Mesodesma mactroides) constitutes a major portion of the total community biomass at BCB; it has been harvested by indigenous people since prehistoric times (Villamarzo, 2010). During the past 50 years, this species has been subject to a small-scale fishery (Ortega et al., 2012), which has undergone contrasting phases of management, regulatory and resource status (Gianelli et al., 2015). Several studies have focused on understanding population fluctuations of the target species (the only one harvested in the study site), as linked to environmental variability and fishing effort (e.g., Defeo et al., 2016). However, comprehensive studies to elucidate changes occurring in ecosystem structure and function, and the interacting drivers of changes in these environments are still lacking.

We assessed temporal responses of the yellow clam population and ecosystem functioning and dynamics to concurrent changes in fishery management scenarios and primary production. The research strategy included the implementation of static trophic models representing four different historical periods to obtain ecological indicators employed to analyze structural and functional changes in the ecosystem. This description was complemented with dynamic simulations considering temporal changes in primary production, fishing effort and trophic effects. Thus, the main questions addressed were: 1) how did the ecosystem structure and function changed over 30 years? and 2) what were the main factors driving these changes?

Section snippets

Study area

BCB is a dissipative sandy beach (mean grain size = 0.20 mm, sorting = 0.70 mm, slope = 3.53 cm m−1, tide range = 0.5 m) (Lercari et al., 2010) 23 km long and 300 m wide (total area 7 km2), located on the eastern coast of Uruguay in the southwestern Atlantic Ocean (SAO) (33°40′ S, 53°29′ W) (Fig. 1). Intertidal sandy beaches are peculiar ecosystems because of their small dimensions and ecological simplicity. The high productivity of this microtidal system sustains the highest diversity of macrobenthic

Static food web modeling

Basic estimated parameters (i.e., model outputs) produced for each functional group allowed us to compare long-term variations in the ecosystem structure (Table 3). The four models fulfilled the thermodynamic and physiological constraints and showed normal trends for biomass and vital rates across trophic levels e.g., a decline in biomass of larger-sized organisms at upper trophic levels (Supplementary materials C). Species composition (presence/absence) showed minor long-term changes, and most

Main trends

Our study shows the following: a) BCB experienced important changes that were reflected at the species and ecosystem levels; b) clam population recovery happened in the absence of harvesting during an increase in primary production of the system; and c) ecosystem-level attributes showed considerable temporal fluctuations primarily related to changes in system productivity. Theses changes were associated with a climatic shift from a cold phase to a warm phase that ocurred in the region.

The first

Acknowledgments

Financial support from CONICYT (Projects 1018 and 4034), CSIC-Grupos (N° 32), PEDECIBA, PDT SC OP0749, National Institute of Fisheries (DINARA, Uruguay) and Inter-American Institute for Global Change Research (grant CRN3070), which is supported by the US National Science Foundation (Grant GEO-1128040) are acknowledged. Special thanks to CSIC-VUSP program. We thank the Benthic Ecology Group from UNDECIMAR for field and laboratory assistance. We would like to thank the reviewers for their

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