Main contributors: Juan Carlos Rocha, Christine Hammond
Other contributors: Reinette (Oonsie) Biggs, Garry Peterson
Last update: 2011-02-28
Bivalves form reefs that filter water removing sediments and nutrients maintaining clear water. Bivalve reefs also produce spatial structure that provides habitat to other aquatic species. A low abundance regime can be induced by harvesting. Low abundances of bivalves do not provide water filtering, leading to murkier water, which can impede bivalve population growth.
Ecosystem type:’
Key ecosystem processes:
Biodiversity:
Provisioning services:
Regulating services:
Cultural services:
Human well-being:
Links to other regime shifts:
Key drivers:
Land use:
Spatial scale:
Time scale:
Reversibility:
Evidence:
Confidence: existence of the regime shift
Confidence: mechanisms underlying the regime shift
Bivalve mollusks play an important role in aquatic ecosystems by filtering and sequestering nutrients. When bivalve abundance changes, it can have substantial ecosystem impacts, creating two different, self-reinforcing regimes.
Bivalve mollusk reef regime
When aquatic ecosystems have high bivalve mollusk density, they form reefs that include many bivalves and are shallow, nearing the water’s surface. The filtering activity of the bivalves results in clear water with high levels of dissolved oxygen. Plankton populations are limited in these conditions. The bivalves themselves operate as reinforcing feedbacks in that their abundance ensures sufficient filtration to maintain this clear water regime. The clear water in turn reinforces bivalve abundance by maintaining hydrodynamics that are conducive to bivalve health (Scheffer 2009). Large, shallow bivalve mollusk reefs encourage biodiversity by providing habitat and filtering nutrients.
Isolated, low density bivalve mollusk regime
When aquatic ecosystems have low bivalve mollusk density, the reefs are small and deep. Water is turbid, with low levels of dissolved oxygen. Plankton and filamentous algae flourish under these conditions. Poor reef size and water filtration limit biodiversity. The low bivalve abundance state is reinforced as bivalve health and fecundity is weakened by turbid water conditions. The turbid water conditions are in turn reinforced by low bivalve abundance(Weijerman et al. 2005, Powell et al. 2008).
The regime of low bivalve abundance is expected to reduce fish populations, water cleansing and the ability of the ecosystem to maintain biodiversity. Such effects would have an impact on fisheries, human health, and recreation.
Mechanized anthropogenic over-harvesting of bivalve mollusks is the main driver of the shift from high to low abundance (Thrush and Dayton 2002). High inputs of nutrients from agricultural or urban sources can act as a slow driver that weakens bivalve health by creating plankton blooms that the bivalves are unable to filter. Plankton blooms can further weaken the health of bivalves by producing organic matter, whose decay, reduces oxygen availability. A disturbance that can trigger a regime shift is bivalve disease (Powell et al. 2008). When populations are weakened by eutrophication and anoxia, they become physiologically susceptible to diseases that can rapidly devastate remaining populations (Leniham 1999).
Shift from high to low bivalve mollusk abundance regime
The loss of abundant bivalve mollusk reefs threatens diverse ecosystem services. The most direct impact is the loss of valuable shellfisheries. A secondary, but potentially substantial impact is the loss of the filtering service provided by bivalves. In urbanized estuaries, it can necessitate the installation of costly synthetic water filtration technology (Gren et al. 2009). In other areas it can lead to declines in water quality that shift populations and reduce recreation opportunities, and potentially the value of waterfront property.
The loss of bivalve habitat structure leads to lower species abundances, and to declines in species richness (Airoldi et al. 2008). Both structural and functional biodiversity is threatened by loss of bivalve abundance, with far reaching effects on marine ecosystems and human ability to exploit such systems (Worm et al. 2006). The regime of low bivalve abundance is expected to reduce fisheries, water cleansing and the ability of the ecosystem to maintain biodiversity. Such effects would have an impact on fishing productivity and human health.
The loss of bivalve nutrient filtration can lead to other regime shifts, such as eutrophication and hypoxia, which can produce unproductive and undesirable ecosystems (see Hypoxia and Eutrophication regime shifts).
Options for enhancing resilience
Estuaries are the world’s most degraded marine ecosystems, receiving land-based pollution from crop cultivation and urbanization, and suffering from anthropogenic over-harvesting (Lotze et al. 2006). The resulting problems are complex, impacting bivalve health and fecundity as well as many other species, with far reaching implications in both biological and social domains.
Experience has shown that management focused on one species or problem tends to be ineffective. Newer research stresses the need to address natural resources as part of complex social-ecological systems, often with long histories of human exploitation (Jackson et al. 2001). Rather than addressing problems on a species-by-species basis, multi -species management has shown to have synergistic effects. For example, in Chesapeake bay, fisheries management looks at oyster, blue crab, striped bass and shad together (Boesch 2004).
Taking this approach further, Ecosystem-based fishery management efforts focus on recognizing interactions between multiple species and environmental stressors, such as low dissolved oxygen levels. Success is measured by the degree to which management efforts include ecosystem-based approaches, rather than by an assessment of fishing stocks (Lotze et al. 2006).
Options for reducing resilience to encourage restoration or transformation
The main option exercised for preventing or reversing a regime shift regarding bivalve abundance is to import bivalve mollusks from another region for aquaculture (Van de Koppel 2008) . Another practice commonly used is to hang bivalves from the surface or build artificial reefs to elevate bivalves in order to avoid the hypoxic conditions in deeper water (Carlsson et al. 2009).
Feedback mechanisms
The bivalve mollusk reef regime
Filtration feedback (local, well established): The filtration feedback consist of the function bivalves perform for the aquatic ecosystem. They increase local movement of water and remove nutrients and small particle from water resulting turbidity. Clearer water favors the growth of bivalves populations as well as other species, bivalve reefs by creating habitat structural complexity and increasing dissolved oxygen in the water.
Competition feedback (local, well established): This feedback capture the competition between bivalves and plankton and filamentous algae for resources, in this case nutrients. Both group of species depend on nutrients for survival, however, by dominating the ecosystem both reinforce the conditions favouring their growth.
Herbivourous fish feedback (local, proposed): Reefs provide habitat for fish that can graze on algal populations, decreasing the growth of algae and enabling the continued maintenance of bivalves.
The low bivalve mollusk density regime
Plankton feedback (local, well established): Plankton and filamentous algae grow well in turbid water with low levels of dissolved oxygen. Hence, when bivalves fail to deliver their filtration function, plankton and filamentous algae prosper by taking advantage of the nutrients surplus that bivalves leave, reducing in turn dissolved oxygen and reinforcing their growing conditions. This feedback is the same mechanism as the filtration feedback.
Fishing feedback (regional, proposed): As bivalves abundance decrease and biodiversity is less supported by habitat complexity built by bivalves reefs, fishing productivity is reduced, hence food supply, resulting on an increase of food demand. A local increase on food demand sends a signal through the market to import food from somewhere else, or increase food production locally. Although it’s very hard to track how the signal dissipates on the market and where the replacing goods come from, one can certainly expect that at least some of them will work as incentive to increase agriculture, nutrients use and hence nutrients input. The latest is one of the drivers that initially trigger bivalves collapse.
Drivers
Important shocks
Eutrophication or hypoxia events (local, proposed) produced to weather or marine currents can lead to a temporary growth in alage that can overwhelm herbivore grazing.
The main external direct drivers that contribute to the shift include:
Nutrients input (local, well established): Nutrients usually come from agricultural activities or urban settlements. The increase of nutrients in water can increase plankton and algae abundance, as well as turbidity, reducing the habitat preferences of bivalves through the plankton and competition feedbacks described above.
Fishing (local, well established): Fishing directly reduces bivalves abundance and mid-predator fish which consume plankton and algae. Hence, favoring the abundance of the later.
The main external indirect drivers that contribute to the shift?
Technology (regional, well established): Technology increase the efficiency of fishing effort, both for fish and oyster fisheries.
Food demand increase fishing pressure locally, as well as incentives to increase agricultural productivity. The later may include the use of fertilizers or the expansion of the agricultural frontier, both leading to increase leaking of nutrients into water bodies.
Urbanization (regional, well established): urban development in coastal areas increase the production of sewage and the leakage of nutrients and sediments into water bodies.
Human population (regional, well established): Human population growth both in numbers and density has been strongly correlated with the increase of nutrients in coast lines (Diaz and Rosemberg 2008). Human growth increase urbanization and food demand.
Slow internal system changes that contribute to the regime shift include:
Nutrients in water (local, well established): the build up of nutrients in water is a slow process that is balanced by bivalves filtration and other organism consumption. Only when surplus levels are reached, plankton and algae take advantage and tend to dominate.
Reef structure (local, well established): reefs are slowly produced and slowly destroyed. By producing habitat complexity bivalves can increase the resilience of bivalve populations.
Acknowledge this review as:
Juan Carlos Rocha, Christine Hammond, Reinette (Oonsie) Biggs, Garry Peterson. Bivalves collapse. In: Regime Shift Database, www.regimeshifts.org. Last revised: 2011-02-28
This work is licensed under CC BY-NC-SA 4.0. It is an initiative lead by the Stockholm Resilience Centre. The website was developed by Juan Rocha and build with Rmarkdown.