Anthropogenic, Direct Pressures on Coastal Wetlands

Coastal wetlands, such as saltmarshes and mangroves that fringe transitional waters, deliver important ecosystem services that support human development. Coastal wetlands are complex social-ecological systems that occur at all latitudes, from polar regions to the tropics. This overview covers wetlands in five continents. The wetlands are of varying size, catchment size, human population and stages of economic development. Economic sectors and activities in and around the coastal wetlands and their catchments exert multiple, direct pressures. These pressures affect the state of the wetland environment, ecology and valuable ecosystem services. All the coastal wetlands were found to be affected in some ways, irrespective of the conservation status. The main economic sectors were agriculture, animal rearing including aquaculture, fisheries, tourism, urbanization, shipping, industrial development and mining. Specific human activities include land reclamation, damming, draining and water extraction, construction of ponds for aquaculture and salt extraction, construction of ports and marinas, dredging, discharge of effluents from urban and industrial areas and logging, in the case of mangroves, subsistence hunting and oil and gas extraction. The main pressures were loss of wetland habitat, changes in connectivity affecting hydrology and sedimentology, as well as contamination and pollution. These pressures lead to changes in environmental state, such as erosion, subsidence and hypoxia that threaten the sustainability of the wetlands. There are also changes in the state of the ecology, such as loss of saltmarsh plants and seagrasses, and mangrove trees, in tropical wetlands. Changes in the structure and function of the wetland ecosystems affect ecosystem services that are often underestimated. The loss of ecosystem services impacts human welfare as well as the regulation of climate change by coastal wetlands. These cumulative impacts and multi-stressors are further aggravated by indirect pressures, such as sea-level rise.

Introduction

Transitional waters are naturally fringed by many types of coastal wetlands, such as tidal flats, seagrass meadows, saltmarshes and mangroves, that are an integral part of the transitional ecosystems (Perillo et al., 2019). The coastal wetlands covered in this article fringe river mouth systems, estuaries, deltas and other transitional waters, such as coastal lagoons and shallow, semi-enclosed, coastal systems, such as bays (Newton et al., 2013). They include a variety of habitats: mudflats, seagrass meadows, saltmarshes, and mangrove swamps. The article covers wetlands from the tropics, temperate zones and polar regions as examples to illustrate the main direct pressures (Figure 1 and Table 1). The wetlands have been chosen to give a broad range and variety, including very large wetlands (e.g., the Mekong Delta) and much smaller ones (e.g., Malanza).

TABLE 1

Table 1. List of coastal wetlands used as examples in this article, with some of the descriptors.

FIGURE 1

Figure 1. Map showing location of the coastal wetlands in the text. (Credit: Dylan Taille).

The range of population and human pressures also varies from sparsely populated, (e.g., Mackenzie-Beaufort), to very large populations, (e.g., Yangtze-Changjiang). Nevertheless, the resident population numbers are not always the best indicator of human pressure, for example, the Venice municipality has a low resident population (about 85,000), but a very large number of visitors (20 million y^–1).

The examples chosen include some very well-known systems, such as the Chesapeake Bay, but an effort has been made to also include some less well-known systems, such as the mangroves of Gulf of Papua and Malanza. Many other systems could have been chosen, but there were limitations to the length of the article, so information on some additional examples is included only in Supplementary Tables S1–S5. There is also a recent review of coastal wetlands in North Africa by El Mahrad et al. (2020).

The human pressures on wetlands are both direct and indirect. An example of a direct pressure is the loss of connectivity and interruptions to sediment supply as a result of constructing a dam. Indirect, human pressures are mostly related to climate change and these include rising temperature, acidification, changes in precipitation/runoff, as well as sea level rise. The aim of this article is to give an overview of the multiple, anthropogenic, direct pressures on coastal wetlands resulting from human activities, the effect that these pressures have on the state of the wetland and ecosystem services, as well as the eventual impacts on human welfare.

There are many possible frameworks for analyzing Social-Ecological Systems such as coastal wetlands (Binder et al., 2013). The present analysis follows a ‘Activity-Pressure-State-Impact on Human Welfare’ approach, modified from the ‘Driver Pressure State Impact Response’ framework (DPSIR), (Gari et al., 2015; Patrício et al., 2016; Elliott et al., 2017). This approach has been selected because it is widely used in international studies by international organizations, (e.g., the Organization for Economic Cooperation and Development, the European Environment Agency, the United Nations Environment Programme, and the United Nations World Ocean Assessment). It was also recently applied to eleven coastal wetlands in North Africa, El Mahrad et al. (2020). The focus is on direct pressures that result from human activities (Elliott and Whitfield, 2011) and follows the typology proposed by Elliott et al. (2014).

The article focuses on Activities-Pressures-State-Impact and these are bolded in the text rather than sub-dividing the sections. The article also considers the effect of the change in state of the environment and the wetland ecosystem on the delivery of ecosystem services (ES). Ecosystem services provide an important link between the state of the natural system and human welfare. The are the answer to the questions ‘so what’? ‘why is this important’? In this review, we used the Millennium Ecosystem Assessment [MEA] (2005) classification of ecosystem services. There are more recent classifications of ecosystem services but the Millennium Ecosystem Assessment [MEA] (2005) is still widely used by international organizations, and there remain challenges to the valuation of ecosystem services in coastal wetlands (Newton et al., 2018).

At the end of each section, we have also included some brief comments about indirect pressures. Indirect pressures, such as climate induced sea-level rise, are uncontestably important to coastal wetlands. However, they are not the focus of the current article and thus not discussed at length. They are especially important in the wetlands where local population and the direct pressures are low, such as the Mackenzie-Beaufort polar wetland and the Gulf of Papua.

Human Activities and Anthropogenic Pressures on Coastal Wetlands

Polar Coastal Wetlands

Arctic and Antarctic coasts have low human population densities. The development, structure, and land use of northern Polar coastal wetlands has been reviewed by Martini et al. (2019). The inhabitants still carry out some traditional activities but there is an increase in economic activities. A large proportion of small settlements on the polar coasts of Alaska, northern Canada, Greenland and parts of Russia have mixed cash and subsistence economies, in contrast to northern Norway, Iceland, or large urban centers such as Murmansk (Jungsberg et al., 2019). Regions where economic activities are more developed have more extensive industrial infrastructure, such as the Prudhoe Bay oilfield on the Alaskan North Slope (Walker and Peirce, 2015). Past activities, such as dumping of mine tailings or encasement of drilling muds in permafrost, may still exert pressures on coastal wetlands, decades after the activity has stopped (Thienpont et al., 2013).

The low populations result in relatively low or localized anthropogenic, direct pressures on coastal wetlands. The loss of sea ice and resulting rapid increase in navigation along Arctic coasts will increase pressures from shipping, tourism, commercial fishing, hydrocarbon exploration and extraction, and mining activities. Economic investment from globalization has stimulated human activities and pressures that are increasing environmental state changes, with progressive reduction of sea ice, degradation of permafrost (Forbes, 2011). Many polar coastal wetlands exhibit relatively rapid state changes attributed to global and regional climate warming (Forbes and Hansom, 2011).

Where traditional activities remain important, e.g., subsistence harvesting, loss of ecosystem services may translate to impacts on welfare, food insecurity and affect cultural integrity, health, and wellbeing.

The negative effects may be magnified in the future because of indirect pressures that cause changes in key environmental variables, e.g., temperature, pH, and redox potential (Kokelj et al., 2010; Barkay et al., 2011; Grosse et al., 2016).

Mackenzie-Beaufort Coastal Wetland, Canada

The Mackenzie Delta covers an area of 13,000 km² (∼60 km × ∼200 km) in the southeastern Beaufort Sea, on the western Arctic coast of Canada (Forbes, 2019). The Arctic tree-line bisects the delta, the southern part of which is forested. Slightly over 50% of the delta plain is occupied by sedge wetlands, channels, and over 49,000 lakes (Emmerton et al., 2007). Permafrost extends to about 60 m depth in Holocene delta sediments, with many thaw taliks beneath lakes or channels that do not freeze completely in winter (Todd and Dallimore, 1998). There is higher ground to the east and west of the outer delta, with permafrost extending to a depth of 500–700 m. Erosional breaching of thaw lake basins has created a highly indented coast with eroding bluff headlands, local dunes, low spits and barrier islands, and shallow estuaries with supratidal Puccinellia phryganodes flats and accumulations of driftwood from the Mackenzie River (Ruz et al., 1992; Forbes and Hansom, 2011; Forbes et al., 2014). The delta is micro-tidal (range <0.5 m), but storm surges of up to 2.5 m cause extensive flooding (Manson and Solomon, 2007; Lamoureux et al., 2015).

The human population in the region is small (Kokelj et al., 2012), consisting of the regional administrative, industrial, and transportation hub of Inuvik (2015 pop. 3265, 68% indigenous), the smaller delta settlement of Aklavik (2015 pop. 668, 94% indigenous), and the outer-coast community of Tuktoyaktuk (2015 pop. 965, 89% indigenous).

Some human activities are seasonal and intermittent, such as the extensive occupation of hunting and fishing camps throughout the delta and at seasonal traditional settlements along the outer coast (Lamoureux et al., 2015). Human activities of the Inuvialuit (western Arctic Inuit) and Gwich’in people include subsistence hunting and fishing as well as administration and public services. Land and resource uses are co-managed with federal and territorial government agencies under the Inuvialuit Final Agreement 1984, the Gwich’in Land Claim Settlement Act 1992, and fisheries and game co-management bodies. Subsistence food harvesting and hunting activities in the Inuvialuit Settlement Region includes berries, medicinal plants, fish including cisco (Coregonus spp.) and char (Salvelinus spp.), birds (especially geese and ducks), and mammals such as polar bear, caribou, moose, muskrat, beluga whale, bearded and ringed seal (Stephenson, 2004).

Human activities related to economic development in the wetland region include infrastructure development, such as construction of Distant Early Warning (DEW) line sites in the 1950s; establishment of the planned community of Inuvik in 1953–1960 to replace flood-prone Aklavik; roads, airports, and port facilities; fuel storage, electric generation and distribution infrastructure; freshwater and waste management systems; hydrocarbon exploration and production installations (well sites, mud sumps, other waste dumps, and camps); seismic cut-lines and degraded artificial islands on the inner shelf (Lamoureux et al., 2015). Road access to Aklavik (and until 2017 to Tuktoyaktuk) has been by winter ice road on delta channels, but the ice season is shortened by climate warming (Lesack et al., 2014; Lamoureux et al., 2015). Tuktoyaktuk is a regional shipping hub for remote community sea-lift operations and offshore hydrocarbon exploration activities. Artificial shore protection at Tuktoyaktuk has been partially successful at limiting erosion. There has been dredging in harbour approaches and to build artificial islands for drilling. Future activities such as infrastructure development, new travel routes, and growing tourism opportunities may impact cultural sites (Irrgang et al., 2019).

Direct pressures related to activities such as oil and gas exploration have ended with increased supply of low-cost natural gas. Oil exploration on the shelf and offshore supply activities in Tuktoyaktuk have also been suspended (Byers, 2016). These past activities still exert pressures on the environment. Contaminated hydrocarbon exploration waste, such as drilling fluids, was placed in sumps to be contained in permafrost. However, about 50% of legacy drilling mud and camp sumps in the delta have collapsed due to warmer temperatures (Kokelj and GeoNorth Limited, 2002).

These pressures affect the state of the environment. Dredging for artificial island construction in the past disturbed the state of the benthic habitat, but ubiquitous and perennial seabed scouring by ice causes more disturbance (Blasco et al., 2013). The changes in the state of the environment result in a loss of ecosystem services. The Mackenzie Delta and Kendall Island Bird Sanctuary are of international importance for the large numbers of migratory birds – particularly shorebirds, cranes, swans, geese, and ducks – that depend on the extensive staging and breeding habitat. The wetlands also provide critical habitat for fish and other wildlife. Regional (glacial-isostatic) and local (compaction) subsidence combined with climate-driven rising sea level causes the gradual inundation of outer-delta avian breeding habitat and low-lying tundra along the coast (Lamoureux et al., 2015; Forbes, 2019), and accelerating erosional retreat of the delta front and adjacent coast, increasing carbon inputs to the Arctic Ocean (Fritz et al., 2017; Couture et al., 2018; Tanski et al., 2019). The Tarium Niryutait Marine Protected Area was established in 2010 in three areas totaling 1,800 km² of the outer Mackenzie Delta and estuary. One of the objectives was the conservation of one of the largest summering stocks of beluga whale (Delphinapterus leucas), anadromous fish, waterfowl, and their habitat. This preserves provisioning and cultural services as well as indigenous harvesting traditions¹.

Loss of ecosystem services and localized contamination have negatively impacted the welfare of subsistence-dependent residents, with implications for community and household health and food security (Wesche and Chan, 2010). The leaching of contaminants, especially hydrocarbons, into the surrounding soil and groundwater has caused localized contamination of the wetlands, raising health concerns due to extensive fish consumption and impacts on human welfare.

Indirect pressures resulting from global emissions and climate change have much greater consequences in the Mackenzie-Beaufort region than direct pressures. These indirect pressures include: accelerated sea-level rise; reduced sea ice, increased open water in the Beaufort Sea; increased wave energy with expanded open-water fetch; increased frequency and reach of storm surges; and accelerated coastal erosion; reduced snowfall; earlier and more rapid ice breakup in the Mackenzie delta; lower peak water levels and reduced off-channel flooding in the delta; rising temperatures contributing to thaw subsidence; accelerated coastal erosion, and ecological change (Manson and Solomon, 2007; Barber et al., 2008; Burn and Kokelj, 2009; Lesack et al., 2013; Vermaire et al., 2013; Obu et al., 2016; Forbes, 2019).

Coastal Wetlands in North America (Excluding Arctic)

Chesapeake Bay Wetlands, United States

The Chesapeake Bay is a 320 km long, shallow, north-south estuary surrounded by the states of Maryland and Virginia on the east coast of the United States. Major tributaries supply freshwater to the bay, including the Susquehanna that supplies more than 50% of the freshwater, the Patuxent, Potomac, York, and James rivers. There were approximately 114,100 ha of tidal wetlands, consisting of saltmarsh and tidal fresh and saltwater wetlands in 2010, almost 37,200 ha of Submerged Aquatic Vegetation (SAV) in 2012, primarily eelgrass (Zostera marina) and widgeon grass (Ruppia maritima) (Chesapeake Bay Program [CBP], 2012).

The watershed is large, approximately 165,760 km², including both heavily urbanized areas in and around the major cities, as well as large portions of distinctly rural, agricultural lands. It includes almost all the state of Maryland, and parts of Virginia, West Virginia, Delaware, Pennsylvania, and New York. Major cities include Washington DC, Baltimore, Richmond, Norfolk, and Harrisburg. The total watershed population is approximately 17.7 million people, (2012 census), expected to grow to 20 million by 2030. The increased spread of urban areas is expected to continue with population growth.

Human activities in the watershed that exert pressures on the Chesapeake wetlands include agriculture, land-use changes, shoreline modification and introduction of non-indigenous species. The watershed includes many thriving economic sectors such as sales, services, construction, manufacturing, government, agriculture and use of natural resources (McKendry, 2009). Activities such as hardening of shorelines are now strictly regulated. Nevertheless, existing shoreline modification and intense development along the shoreline can lead to wetland loss or prevent new wetlands from forming, blocking the migration of wetlands to upland areas as sea levels rise (Torio and Chmura, 2013; Raposa et al., 2016), a synergy of direct and indirect pressures.

A complex mixture of direct pressures result from intensive land-use and the introduction of invasive species. Nutria (Myocastor coypus, a South American rodent) was introduced in the late 1960s and displaced native species such as beaver, muskrat and otter. Nutria thrived on native marsh grasses, damaging thousands of hectares of wetland through destructive feeding (National Fish and Wildlife Service, 2016). In addition, the invasive common reed, Phragmites australis, grows rapidly to outcompete other wetland vegetation, such as native grasses (Chesapeake Bay Program [CBP], 2012). However, the main direct pressures to the overall condition of Chesapeake wetlands are now nutrient and sediments from intensive land-use, urban wastewater and atmospheric deposition of nitrogen (Zhang et al., 2015).

Pressures from intense land use activities directly and indirectly affects the state of Chesapeake wetlands. Excess nutrients result in areas of low dissolved oxygen and reduced water clarity (Kemp et al., 2005). This has affected the state of the submerged aquatic vegetation (SAV), and habitat for commercial species, including oysters (Crassostrea virginica), crabs (Callinectes sapidus), and bass (Morone saxatilis). Fishing pressure has also contributed to the decline in the state of these important species and may mask the signal from eutrophication effect (Kemp et al., 2005). Sediment inputs affect the benthic state, cover hard-bottom habitat, smother oyster reefs, increase turbidity, reducing light available for SAV (Lefcheck et al., 2017). Lefcheck et al. (2017) document a change of state, a 29% decline in eelgrass area from 1991 to 2016, primarily from decreasing water clarity increases and water temperature. Despite this degradation of the state, management measures to reduce nutrient pressures can increase SAV growth and area (Lefcheck et al., 2018). This is a positive sign that the state of ecosystems may recover after humans alleviate pressures put on sensitive habitats like SAV (Lefcheck et al., 2018).

Loss of ecosystem services include a decrease of Chesapeake wetland habitat for economically valuable species of fish and crabs, both of which are cultural keystones in the Chesapeake region (Paolisso, 2008). There is also a loss of storm surge mitigation, filtration of sediments and nutrients from urban and agricultural stormwater runoff, sequestration of organic carbon and opportunities for recreation (Costanza et al., 1989; Millennium Ecosystem Assessment [MEA], 2005). Tidal marshes are carbon, nutrient and sediment sinks, so the degradation of their state increases pressures from nutrient and sediment fluxes to Chesapeake Bay (Kemp et al., 2005).

The main indirect pressure on the Chesapeake wetland is from sea-level rise. Wetlands and marshes can increase elevation in response to indirect pressures, such as sea level rise, under favorable conditions of sediment supply, root growth, and litterfall (Becket et al., 2016). Mean sea level rise in Chesapeake Bay ranged from 2.7–4.5 mm y⁻¹ from 1950 to 2000, faster than the global mean of 1.8 mm y⁻¹, probably due to land subsidence. Predicted future rates of sea-level rise (about 6 mm y⁻¹) will increase marsh loss rates and area (Cahoon, 2007), as sea levels are expected to rise by 0.4–1.6 m by 2100 (Rybicki and Landwehr, 2007; Najjar et al., 2010). In a conservative scenario of 60 cm sea-level rise by 2100, 65,000 ha of coastal marsh would be converted to brackish marsh and 11,735 ha of tidal swamp to saltmarsh or open water, which is less diverse. Chesapeake wetlands at risk from sea-level rise include Blackwater Wildlife Refuge, Tangier Sound, and Virginia’s Eastern Shore. Shifts in salinity will make the current marshes more favorable for certain species and less for others (Najjar et al., 2010).

Mississippi River Delta Coastal Wetlands, United States

The Mississippi River, the largest in North America, meanders across the coastline every 700–1,200 years, seeking the hydrologic path of least resistance to the sea. These cycles of delta growth and decay (Frazier, 1967) created 17,417 km² of fresh to salt marshes in a micro-tidal regime, which represent 41% of the United States coastal wetlands. The soils alongside the main channel wetlands are mostly comprised of inorganic matter, and hurricanes deposit a considerable return flow of inorganics to the fringing coast (Tweel and Turner, 2014). In contrast, the wetland soils between the distributary levees are organic-rich. The rates of land loss rose in the 1930s, peaked in the between 1965 and 1986 (126 km² y⁻¹; 0.07% y⁻¹) and the current rates are near zero (Couvillion et al., 2017). The cumulative losses in the last 100 years are about 25% of the original amount, but are expected to increase with the rate of sea-level rise (Strauss, 2013; Church et al., 2014). These losses are well-publicized through media campaigns to acquire restoration funding.

New Orleans is the main urban area and population center, (population 393,000 in 2017). New Orleans is vulnerable to natural disasters because it is built on land of low elevation, in an area of relatively frequent hurricanes as well as storm surges, and it has a weak evacuation strategy (Turner, 2007). There are multiple human activities by the approximately 2 million people who live in the twelve coastal parishes of the Mississippi River delta, such as: fishing, shellfish (e.g., oysters) and aquaculture (e.g., catfish); poultry rearing; agriculture (cotton, sugar, rice, corn, and soybean); oil and gas; shipping and ports; recreation (hunting, fishing, and tourism).

Anthropogenic pressures are well-documented. Sediment fluxes to the coastal zone have varied in the last 200 years. River-mouth wetlands expanded in the 1800s, when trees in the watershed were cut and soils were plowed, enhancing sediment delivery to the coastal zone (Turner and Rabalais, 2003; Tweel and Turner, 2012). Implementation of soil conservation measures trapped sediments behind dams, which decreased sediment loads after the 1930s. River-mouth wetland areas receded dramatically and are now close to the 1700s area (Turner, 2017). The dredging of canals for navigation and drilling for oil-gas exploration have left spoil banks of dredged material as a continuous, 20,000 km long levee that reaches 1–2 m in wetlands where the tidal range is only 20–30 cm. This presents a barrier to tidal water flowing in and out of wetlands, so canal density is directly related to land loss rates from 1900s to present throughout the deltaic plain (Turner and McClenachan, 2018). The Deepwater Horizon oil spill in 2010 released 5 million barrels of oil in 2010 with a surface slick covering 149,000 km² of the Gulf of Mexico and oiling coastal marshes for decades (Turner et al., 2019). The nutrient pressure from the Mississippi River watershed has increased nitrogen and phosphorous loads in the last 100 years (Turner and Rabalais, 2003). This is a much greater nutrient pressure than the sewage and local runoff.

These pressures affect the state of the Mississippi wetlands. The contaminated sediments from the Deepwater Horizon oil spill (Rabalais and Turner, 2016) degraded the salt marsh vegetation, decreasing the cover of living marsh vegetation, covering and killing marsh fauna. Marsh shoreline erosion was 2.5 times higher after oiling and the marsh will not recover (Turner et al., 2016). Diversions of the Mississippi water to deltaic wetlands for restoration (a point-source) or cultural eutrophication (non-point source) increase the availability of nitrogen and phosphorous to the wetlands, contributing to general eutrophication of the delta, which also affects the state of the soils and causes carbon losses (Darby and Turner, 2008; Kearney et al., 2011; Deegan et al., 2012; Bulseco et al., 2019).

The delivery of ecosystem services is affected by the degradation of the wetland. This includes regulating services, such as protection from hurricanes, by increasing resistance and lowering storm surge height. The reduction in storm-surge height is ∼0.3 m per 1–2 km of wetland and the presence of vegetation is especially important (Barbier et al., 2008; Costanza et al., 2008; Gedan et al., 2011; Shepard et al., 2011). This contributes to the protection and restoration of coastal areas, which costs $50 billion in Louisiana (Coastal Protection Restoration Authority [CPRA], 2017). Furthermore, the wetland provides an important fish and shrimp habitat for juveniles (Turner, 1977) that become 25–35% of the United States commercial fish landings value and tonnage.

The loss of these ecosystem services can impact human welfare, including loss of life, public infrastructure and private property. A third (36%) of the land in the United States that is less than 3.5 m elevation is in coastal Louisiana and the height of a Category 3 storm-surge is at least 3 m. The slope (elevation gradient) is gradual and sediment supply has been reduced by flood protection levees. New Orleans is a ‘city below sea level’ in this vulnerable zone, seaward of the edge of the upland. Water does not drain out naturally when it rains but must be pumped out uphill. Urban expansion and construction consolidate and compact the fine-grained and highly organic sediments, squeezing out the water and resulting in soil subsidence. The structural integrity of foundations, levees, gas lines and roads are affected by the slow changes in soil oxidation, drainage, volume, settling and subsidence.

Future indirect pressures from sea level rise (SLR) rates will affect the vulnerability and sustainability of river deltas. The Mississippi delta formation began when SLR slowed about 8,000 years ago to around 5 mm y⁻¹ or less (Turner and Rabalais, 2018; Turner et al., 2018). The rates were 5.6 mm y⁻¹ from 1996 to 2016, which is at the limit of vertical accretion (Morris et al., 2016). Future estimates of SLR vary from an intermediate low rate of 5.6 mm y⁻¹ to a high rate of 16 mm y⁻¹ (National Research Council [NRC], 2010), reaching 8–16 mm y⁻¹ by 2080–2100 (Church et al., 2014). The Mississippi River delta has been sustained and protected by substantial, compensating infrastructure and by multiple, short-term and energy-intensive strategies. This has lowered its vulnerability to risks and raised its sustainability relative to other deltas (Tessler et al., 2015). However, such energy-intensive interventions will become more expensive and less sustainable in a more energy-constrained future scenario. Sustaining the delta in the future will require long-term policies to develop, sustainability solutions (Tessler et al., 2015).

Coastal Wetlands in South America

Bahia Blanca Wetlands, Argentina

The Bahia Blanca is a temperate and mesotidal coastal wetland located in southwest of Buenos Aires Province, Argentina. Despite its size, most of the estuary is marine dominated (Perillo, 1995), with very little river input (Piccolo and Perillo, 1990; Perillo and Piccolo, 2020). The extensive coastal wetland is roughly triangular, about 90 km in length and 53 km wide at the mouth, about 3,000 km², cut by NW-SE tidal channels and islands (Perillo and Piccolo, 1999, 2020). Large areas of tidal flats, as well as Spartina and Salicornia marshes, have developed, providing conditions for a rich benthic infauna that supports significant artisanal fisheries. This wetland includes both a provincial natural reserve that includes the whole estuary south of the Canal Principal and a municipal reserve of only 3 km², SW of the city of Bahia Blanca (Perillo and Iribarne, 2003a, b). The wetland is part of the Western Hemisphere Shorebird Reserve Network since March 2016. To the north of Canal Principal, there are two major cities, Bahía Blanca, population 350,000, and Punta Alta, population 70,000, as well as several small towns, such as Villa del Mar, Ingeniero White and General Cerri. The total population around the wetland was estimated at 440,000 in 2016. There is no direct access or settlements on other parts of the wetland.

There are many important human activities in and around the wetland. The main economic sector is maritime transport and shipping, with construction and maintenance of port facilities providing one of the major activities. The largest and deepest harbor system in Argentina is on the coast of the Canal Principal, that exports industrial products and grain. There are oil transfer buoys in the harbors, a trading dock at the port of Rosales and a navy base at Puerto Belgrano. There are two ports further in the estuary, Ingeniero White that has an area devoted to grain and another for general merchandise (i.e., oil, containers, and petrochemical products), and Puerto Galván for oil and petrochemical products (Zilio et al., 2013).

Dredging is a significant human activity that keeps the port facilities accessible to large ships. The navigation channel was dredged to deepen it from 10 to 13.5 m during 1989–1991, which facilitated the development of one of the most important petrochemical complexes in Argentina (Zilio et al., 2013). The navigation channel was further deepened to 15 m depth at low tide during 2012–2014. Additionally, there is dredging of the piers for maintenance purposes. The port authorities are planning to further develop harbor facilities and the installation of new industries planned for 2020. Furthermore, the wetland is used for sewage disposal (Speake et al., 2020).

These activities exert anthropogenic pressures on the wetland along the northern coast of the Canal Principal. Pressures include pollution, harbor, and industrial development. The major Urban Waste-Water Treatment is not working properly and there are four untreated discharges of sewage into the wetland, two from Bahía Blanca City, one for Punta Alta City, and one for the navy base. Pollution is mainly due to sewage discharges, with minor industrial pollution from the industrial flares and deposition of airborne contaminants. These include Salmonella and Escherichia from sewage discharge and metals from industrial discharges (Simonetti et al., 2017; Severini et al., 2018). The material from the dredging has covered many tidal flats and marshes along the Canal Principal, in some cases forming new islands where the port authorities are planning to develop future harbor facilities.

These pressures have affected the state of the wetland environment and ecosystem. The estuary is eutrophic from the pressures of nutrients from untreated discharges (Freije et al., 2008) that may result in widespread eutrophication, if the flushing capacity of the estuary is exceeded. Nevertheless, pollution is low at present because of the strong currents and rapid mixing of the water in the Canal Principal (Botté et al., 2007). The disposal of dredged materials has affected the most important nesting area of the Olrog’s Gull (Larus atlanticus), which is an endangered species native of Argentina, Uruguay, and Brazil, of which 2/3 of the total population lives in the Bahia Blanca wetland.

This degradation of the state of the wetland environment and ecosystem leads to a loss of ecosystem services. The long-term effects of sewage pollution could be damaging to the regulating services of the wetland such as denitrification. Meanwhile, there is a decrease in the provisioning services of the wetland, i.e., the catch of prawns, shrimp and local fish. Nevertheless, there is little evidence at present that this reduction can be directly associated to pollution rather than large scale effects, such as Southern Oscillation events, especially during dry La Niña periods. However, artisanal fishers complain of the deformations of fish caught in the vicinity of effluent discharges and there maybe impacts on human welfare (Speake et al., 2020).

There are also indirect pressures from climate change. The islands in the wetland ecosystem are only 50 cm above spring high water levels. Mean sea level rise for Argentina is on the order of 1.6 mm y^–1 (Lanfredi et al., 1988). However, the estimated global increase of about 83 cm by year 2,100 (Oppenheimer et al., 2019) would completely flood the estuary (Perillo and Piccolo, 2020), and overwhelm the wetland and islands. There is no practical way to mitigate this situation. There also appears to be changes in the typical wind regime. These are strong winds from the N-NW blowing about 40% of the time with average speeds of the order of 20 km h^–1. These winds blow parallel to major channels affecting tidal prediction, navigation programming and the generation of large wind-tide interaction waves (Perillo and Sequeira, 1989; Perillo and Piccolo, 1991). However, in the last 5 years the number of calm days has increased significantly, which reduced the number of storm surge phenomena on the town of Ingeniero White from once a year to once every 2 or 2.5 years. That also changed the conditions in beaches just outside the estuary where there is a reduction of the appearance of jelly fishes (always associated to upwelling forced by N winds) during the summer months (Brendel et al., 2017).

Coastal Wetlands in Europe

Only two European case studies are presented in the text in order to reduce the length of the article. This is to provide examples of less well-known wetland systems, outside Europe. Nevertheless, some details of 12 further coastal wetlands in Europe are included in the supporting Supplementary Tables S1–S5. These European wetlands that are not represented in the text are shown in italics where they appear in a supporting table.

Ria Formosa Wetland, Portugal

The Ria Formosa wetland is part of a temperate, mesotidal, 80 km² coastal lagoon, on the south coast of Portugal (Aníbal et al., 2019). The Gilão is the only permanent river flowing into the wetland that is connected to the Atlantic by several inlets. The wetland includes extensive areas of salt marsh (Arnaud-Fassetta et al., 2006) and seagrass meadows (Cabaço et al., 2009). There are three main towns in the catchment: Faro, the district capital (∼64,500); Olhão (∼45,000); and Tavira (∼26,000), as well as several smaller urban areas (population data from 2011 Census, Instituto Nacional de Estatistica²). The influx of visitors in the summer increases the population, in some cases several-fold, overwhelming infrastructure designed for the resident population, such as Urban Waste-Water Treatment facilities (Newton et al., 2013; Cravo et al., 2015; Veríssimo et al., 2019).

Multiple human activities cause pressures on the Ria Formosa wetlands. These include change of land-use, such as conversion of saltmarsh into salt-extraction pans (salinas), a historical activity. Some of these ponds have now been converted for aquaculture of fish (Cunha et al., 2013), and others have been converted into Urban Waste-Water Treatment ponds, e.g., near the airport (Veríssimo et al., 2019). Construction in the three towns (Faro, Olhão, and Tavira) has encroached on the surrounding wetlands as well as on the sand dunes of the barrier islands that separate it from the Atlantic. Construction includes groin to retain sand along beaches to the west of the lagoon, the creation of consolidated inlets, such as Barra do Farol (Carrasco and Matias, 2019). An airport, a port (Faro) and several marinas (Faro, Olhão, and Tavira) have been constructed from the wetland. The wetland channels are regularly dredged for sediment extraction and to keep the access to the ports and marinas navigable, since the mean depth is only 1.5 m. Several small, torrential streams (e.g., the Ribeira de São Lourenço and Gondra) were dammed with dykes to retain freshwater in the 19th Century, and some land was reclaimed from the wetland marshes for agriculture (e.g., Ludo). An artificial inlet, Nova Barra do Ancão, was opened in the western part of the lagoon in June 1997. Artisanal fishing and shellfish harvesting are important activities in the Ria Formosa and shellfish concessions are also in the wetland. Olhão is a large fishing port, but most of the catch comes from the adjacent coastal waters rather than the lagoon. The Campina de Faro in the watershed is the richest agricultural region of the Algarve. Intensive farming includes water cress and salads (Vitacress), fruit and vegetables in greenhouses, as well as orange groves. Some agricultural land has been converted to golf (e.g., Quinta do Lago). There are also intensive poultry farms (Ludo) and pig-farms in the catchment of the wetland. The area around the Ria Formosa is not industrial, although there are some food industries, such as fish processing in Olhão.

The various human activities in the catchment of the Ria Formosa exert multiple anthropogenic pressures on the wetlands. Foremost of these is the loss of habitat and associated biodiversity, especially the loss of seagrass meadows and saltmarsh, as well as dunes. The groin, impoundments, ponds, obstructed channels and dykes, represent a loss of connectivity of the wetlands that disrupt both the hydrology and the sedimentology. This has resulted in a saline intrusion and salinization of the western part of the wetland, ever since the 19th century. Overfishing, shellfish harvesting, illegal harvesting of sea-cucumbers (Holothuria arguinensis) and the attempted introduction of non-indigenous species (Manila clam, Ruditapes philippinarum; Japanese prawn, Penaeus japonicus; Pacific oyster, Crassostrea gigas) are further pressures on the ecosystem. The use of fertilizers in the agricultural zone and golf-courses around the Ria Formosa, manure from animal-rearing, and inadequate sewage treatment are all pressures that can lead to eutrophication (Newton et al., 2003) and microbial contamination (Cravo et al., 2015). Several studies have documented contamination and pollution of the Ria Formosa by metals and organic chemicals (Bebianno, 1997; Mudge and Duce, 2005; Bebianno et al., 2019; Moreira da Silva et al., 2019), despite the low industrial development around the wetland.

The deteriorating state of the environment and ecosystem has consequences on the ecosystem services provided by the Ria Formosa wetland (Newton et al., 2018). This has been most notable in the declining clam harvest (provisioning service). Decline in the coastal fisheries has also been attributed to the decline in seagrass (García-Marín et al., 2013) and nursery supporting services (Abecasis et al., 2009). The Ria Formosa is a popular destination for ‘beach and sand’ tourism (Zacarias et al., 2011; Semeoshenkova and Newton, 2015) as well as eco-tourism, thus contributing revenues to the local economy through cultural services. Perturbation of sediment fluxes and supply by construction on the dunes of the barrier islands, as well as the retention of sediment by dams in the catchment and groin to the west, make the wetland vulnerable to erosion (loss of regulating services) (Ceia et al., 2010) and storm surges. This threatens including important infrastructure, such as the international airport, thus potentially affecting tourism (cultural services).

The decline of ecosystem services has impacts on human welfare (Bebianno et al., 2019). Continued microbial contamination from sewage (Cravo et al., 2015) as well as algal toxins from HAB (Lage et al., 2014) and other public health issues (Bebianno et al., 2019) are related to the degradation of the wetland. The declining incomes of shellfish harvesters and artisanal fishers eventually make these culturally unique lifestyles unsustainable and fishers seek other sources of income and ultimately employment.

Like all coastal wetlands, the Ria Formosa is also threatened by indirect pressures such as sea-level rise and increased temperature (Brito et al., 2012), and storm surges. Violent Atlantic storms in recent years have frequently washed over the barrier islands (Almeida et al., 2012). So far, there has not been any loss of life, although infrastructure (airport) and housing has been affected by a tornado on 2011. These indirect pressures ultimately threaten the whole Ria Formosa wetland, which is constrained by urban development at its landward boundary.

Venice Lagoon Wetlands, Italy

The lagoon of Venice (Italy) is in the NW part of the Adriatic Sea and includes one of the largest Mediterranean wetlands. The lagoon is shallow (mean depth 1.5 m) and covers about 550 km², of which 432 km² are tidal. The mean tidal amplitude is about 0.6 m, with about 60% of water being renewed through three inlets every 12 h (Facca et al., 2014). Freshwater inputs are about 30 m³ s⁻¹, delivered by small rivers and a network of artificial channels. The main rivers, Brenta and Sile, where diverted long ago in order to avoid the siltation of the lagoon (Solidoro et al., 2010).

Due to its complex morphology, the wetland includes subtidal flats, intertidal mudflats, saltmarshes, ‘valli da pesca’ (marginal areas close to tidal exchanges) and a network of relatively deep channels (Rova et al., 2015). Macroalgae and seagrasses account for most of the primary production. Besides the city of Venice, there are several small islands, such as Murano, Burano, Lido, S. Erasmo, which collectively host about 85,000 residents, according to Venice Municipality data. Venice and its lagoon are a highly attractive touristic venue and the numbers of visitors exceed the resident population.

Shipping and navigation, from small boat to large cruise ships, have always been important human activities for the islands of Venice lagoon, and tourism also increases the internal navigation. Shipping has entailed several modifications including rivers diversions and the construction of jetties at the inlets in the 19th and early 20th centuries. More recently, from 1927 to 1970, the navigation channels were dredged and enlarged for access to the main port facilities at Porto Marghera, which stimulated industrial development and activities around Mestre, affecting the wetlands. Clam dredging activities are now mostly illegal because of contamination. The catchment of the lagoon (Veneto) includes areas of market gardening, fruit-growing and vine-growing reclaimed from the wetland. Groundwater extraction in the 1960’s and 1970’s was excessive and contributed to the subsidence of the wetland.

Resulting direct pressures include disruption of hydrology, re-suspension of large amounts of sediment that exacerbate the erosion of the wetland, increased nutrient and organic matter supply, as well as inputs of industrial effluents and contaminants to the wetland. Nutrient run-off from agriculture represents the main source of Nitrogen and nutrient pressure to the wetland. Poorly controlled shellfish harvesting, Manila clam (Ruditapes philippinarum), has increased sediment disturbance and resuspension in the wetland. Resuspension is exacerbated by increased internal navigation, mainly linked to tourism. Sediment resuspension can release contaminants that were trapped in the sediment as a legacy of industrial pollution in the 20th century, especially in the central part of the wetland (O’Higgins et al., 2014; Giubilato et al., 2016).

The state of the water and wetland sediment quality have been degraded by industrial activities that heavily contributed to the pollution of the lagoon in the past. Both sediment budget and sediment transport processes have been heavily affected by anthropogenic interventions. The disruption of hydrology and sediment supply has resulted in subsidence. Eutrophication can cause macrophyte blooms (Ulva), localized anoxia in confined areas of the lagoon wetlands and loss of seagrass, as in 2013. However, concentrations of inorganic nitrogen and phosphorus is decreasing in the water and at the sediment surface (Facca et al., 2014). The loss of wetland habitat, especially the reduction of seagrass meadows, saltmarshes and associated biodiversity, as well as the introduction of exotic, invasive algal species are severe. The area of saltmarshes has halved from 68 to 32 km² between 1927 and 2002, while the area of subtidal flats has increased from 88 to 206 km². Overall, the average depth of the lagoon has increased from 0.62 m in 1927 to 0.88 m in 2002 (Sarretta et al., 2009).

Ecosystem services provided by the Lagoon of Venice are still being assessed (Rova et al., 2015; Newton et al., 2018). Overfishing has led to sharp decrease in clam yield, from about 40,000 tons in the 1990s to 2,000–5000 tons in 2016. Seagrass meadows have recently recolonized large areas of southern sub-basin, contributing to sediment bio-stabilization. Recolonization in the northern part is being stimulated by an EU funded LIFE project³.

Indirect pressures such as sea level rise are expected to worsen due to climate change. Thus, the conservation of the wetland islands and protection from acqua alta flooding is one of the main current issues, with disastrous floods in November 2019. This has led to the major infrastructural changes to the inlets, e.g., the MOSES flood barrier.

Coastal Wetlands in Africa

A DPSIR analysis of coastal wetlands in North Africa includes 11 systems from south west Morocco to Egypt (El Mahrad et al., 2020). Thus, only one North African example is included in the present review, because of its unique characteristics as a ‘double’ system, the Bizerte–Ichkeul wetlands.

Bizerte Lagoon and Ichkeul Lake Wetlands, Tunisia

Bizerte lagoon and Ichkeul lake are linked, coastal wetlands in Tunisia, where the climate is Mediterranean, semi-arid, with a hot, dry summer and mild, wet winter (MAERH, 2003). Bizerte lagoon, also known as ‘Lac de Bizerte’ or ‘Mezaouka’, has an area of 128 km² and a mean depth of 7 m. A 6 km long inlet connects to the Mediterranean Sea and a 5 km long Tinja channel connects to Ichkeul lake (Béjaoui et al., 2008). Ichkeul is a brackish-freshwater lake with an annual depth variation of 1–3 m, low winter salinity (S = 3) and high summer salinity (S = 30–50), (Savoure, 1977; Hollis, 1986; Ben Rejeb-Jenhani et al., 1991; Tamisier et al., 2000). Rainfall during autumn and winter flows in through 6 wadis, seasonal rivers, some overflowing through the Tinja channel into Bizerte lagoon. The reverse happens in summer, when high evaporation lowers the water level in Ichkeul lake and water flows in from Bizerte lagoon through the Tinja channel (Casagranda et al., 2006). The exceptional salinity gradient (3–45) is a unique feature that gives Ichkeul lake and wetlands a rich biodiversity. The area comprises three units: the 89 km² brackish water lake, 27 km² marshes, and a 13 km² isolated and wooded massif; Djebel Ichkeul (Trabelsi et al., 2012).

Few people (about 350 in 1999) work in the quarries and live in the Ichkeul reserve. Activities in the Ichkeul wetland include quarrying fishing, grazing of cattle, sheep and goats. Over-grazing is causing serious degradation and causing erosion, as well as affecting the water buffalo (Bousquet, 1988). Poaching, illegal hunting and overfishing are further activities in the Ichkeul wetland ecosystem. However, there is intensive agriculture, plowed land, orchards and pasture in both densely populated Ichkeul and Bizerte catchments, so the wadis have been dammed for freshwater (Koundouri et al., 2006).

The area around Bizerte lagoon is much more developed and densely populated. Economic sectors and activities include industry (petrochemical, metallurgical, textile, agro-alimentary, and cement), farming, animal rearing, aquaculture, fisheries, shipping and port, tourism.

These activities exert various direct, anthropogenic pressures on the lagoon and lake wetlands. Bizerte wetlands are affected by pressures from domestic sewage, industrial waste, atmospheric pollution, farmland runoff, effluents from fisheries and bivalve aquaculture (Béjaoui et al., 2010). The urban and industrial effluents are mainly discharged in the southeast, southwest and the north sectors of the lagoon wetlands. The southeastern sector is affected by the domestic and industrial effluent through the Guenniche River, the southwestern sector by the steel factory discharge, and the northern sector by urban wastes and sewage effluent. The mismanagement of the fisheries sector has resulted in an increase in the numbers of illegal fishing boats. The fishing pressure has decreased the stock to such a low level that the reproductive capacity is in peril (DGPA, 2012).

The main, direct, anthropogenic pressure on the Ichkeul wetland comes from the dams that have changed the hydrology and sediment supply to the lake. The dams have modified the connectivity and hydrology of both the Ichkeul and Bizerte wetlands. The changes in hydrology and freshwater supply in the lake and lagoon have altered the water equilibrium between the wetlands, rivers, lake, lagoon, and the sea (Smart, 2004; Saied and Elloumi, 2007). A lock on the Tinja channel was constructed in 1996 to control salinization and the decline of the high biodiversity (IUCN, 1994). Drainage canals have lowered water in the Ichkeul wetland, so livestock now graze formerly inaccessible reedbeds. Open cast quarrying threatens the wetland ecosystem and pollutes the lake water (Bousquet, 1988).

Direct, anthropogenic pressures affect the state of the environment and ecology of both wetlands. The dominant flora of Ichkeul wetlands was extensive meadows of Potamogeton pectinatus L., the major food source for wintering waterfowl (Bousquet, 1988), and Ruppia cirrhosa (Petagna Grande), (Hollis, 1986; Bureau Central d’Etudes pour les Equipements d’Outre-Mer [BCEOM], FresinusConsult, CESalzgitter, and STUDI, 1995; Tamisier et al., 2000) until the early 1990s. The area occupied by P. pectinatus varied both annually and seasonally, with a summer-autumn maximum and a late winter minimum (Hollis et al., 1977; Hollis, 1986). The annual yield of P. pectinatus was cropped largely by wintering birds. However, rising salinity now restricts the growth of this species (Zairi, 1997). The wetland marshes were famous for their variety of hydrophilic vegetation, especially Scirpus maritimus, important for geese (Anser anser), (Hollis et al., 1977; Hollis, 1986). Poaching, illegal hunting and overfishing have caused a decrease in biodiversity. The damming of the water supply to Ichkeul lake has led to evaporation of the Scirpus maritimus marshes, which have been replaced by invasive, annual weeds. Salt-loving plants have replaced fresh-water species in the wetland marshes. Industrial development in the catchment has contributed to the contamination and pollution of Ichkeul lake by organo-metals and organic chemicals (Zairi, 1997).

The pressures have also affected the state of Bizerte lagoon. Run-off of fertilizers led to eutrophication and increases in water temperature have stimulated microbial activity, hypoxia and eutrophication of Bizerte lagoon (Essid et al., 2008; Ben Omrane et al., 2010; Fertouna-Bellakhal et al., 2014). The relatively high levels of organic matter recorded in the wetland sediment caused a decrease in dissolved oxygen causing repeated fish kills (Béjaoui et al., 2008). Industrial contamination is the source of metal (Pb and Zn) in the sediments of Bizerte (Zaaboub et al., 2014), and accumulation of Zn may contribute to sediment toxicity. Increase of marine navigation contaminates the lagoon and wetlands with Polycyclic Aromatic hydrocarbons and Polychlorinated biphenyls. There are occurrences of harmful algal blooms (HAB) of species belonging to the genus Alexandrium in Bizerte lagoon (Turki et al., 2007, 2014; Sahraoui et al., 2009), possibly related to the increase in internal marine navigation and introduction of non-indigenous dinoflagellates from ballast water.

The degradation of the state of the environment has led to a loss of ecosystem services. The provisioning services of fishing and aquaculture of Bizerte lagoon and wetland are threatened by changes in salinity, pollution, harmful algal blooms and overfishing. The Tunisian government created Ichkeul National Park in 1977 as an internationally important wintering ground for waterfowl (Scott, 1980; Hollis, 1986). The lake and wetlands of Ichkeul are the most important stopping-over point in the Western Mediterranean basin for migrating birds (150,000–250,000), as recognized by the Ramsar Convention List, the MAB Biosphere Reserve, and the UNESCO World Heritage List (Hollis et al., 1977; Tamisier and Boudouresque, 1994; Casagranda et al., 2006). The deteriorating state of the environment and ecosystem has consequences on the supporting and regulating ecosystem services provided by the Ichkeul wetland, especially a decrease population of migratory birds such as ducks, geese, storks, and pink flamingoes. Important species are Anse ranser, Anas penelope, Aythya farina, and Fulica atra (Tamisier and Boudouresque, 1994; Tamisier et al., 2000). The degradation meant that Ichkeul National Park was placed on the list of World Heritage in Danger in 1996, while in 1998 data from IUCN showed that the increase in salinity threatened the value of the World Heritage site.

There are also impacts on human welfare such as food safety, public health, decreased fisheries and aquaculture revenues. Mussel production in Bizerte lagoon has decreased in recent decades due to harmful microalgae and mortality (Sahraoui et al., 2009; Turki et al., 2014) with considerable economic losses (Sahraoui et al., 2009; Turki et al., 2014) and this is an obstacle to the development of shellfish aquaculture industry. This has also been associated with increased bacterial activity (Sakka Hlaili et al., 2006, 2007; Essid et al., 2008; Ben Omrane et al., 2010; Fertouna-Bellakhal et al., 2014). The decrease of fish stock and diversity has also caused a decline in jobs of fishers and aquaculture farmers. Ichkeul Park is a popular destination for eco-tourism and cultural heritage, thus contributing revenues to the local economy through cultural services, although eco-tourism has decreased. Numbers of visitors were 23,000 in 1987 and 2,500 in a 6-week period of 1988 (IUCN, 1994). However, visitor numbers decreased by 2016, partly because of security issues in the tourism sector.

Indirect pressures on both wetlands are expected to increase with climate change. In particular, the hydrological imbalance between Lake Ichkeul and Bizerte lagoon (Tamisier and Boudouresque, 1994; Tamisier et al., 2000), initiated by the reduction in freshwater supply to the lake, will be aggravated by sea-level rise in the lagoon, (Casagranda et al., 2006; Koundouri et al., 2006; Béjaoui et al., 2008; Béjaoui et al., 2010).

Watamu, Mangrove Wetland of Mida Creek, Kenya

Mida Creek covers an area of 31.6 km² at Watamu, on the Indian Ocean coast of Kenya (Dahdouh-Guebas et al., 2000). The climate is tropical with temperatures of 26–32°C. The monsoons bring two, distinct rainy seasons, in April/May and in October/November (Gang and Agatsiva, 1992). Mida Creek has habitats that include mangrove forest, rock outcrops, sandflats, seagrass beds, and coral reefs adjacent to deeper waters. The mangroves dominate the wetland occupying 1,746 ha, (Dahdouh-Guebas et al., 2000; Kairo et al., 2002). Seven of the nine mangrove species found in Kenya occur in Mida Creek with abundant Rhizophora mucronata, Avicennia marina, and Ceriops tagal and more sparsely distributed Sonneratia alba, Xylocarpus granatum, Bruguiera gymnorhiza, and Lumnitzera racemosa, (Kairo et al., 2002).

Mida Creek is part of the Watamu-Malindi marine protected area established in 1968 and was designated in 1979 as a Biosphere Reserve by UNESCO (Dahdouh-Guebas et al., 2000). Nevertheless, human activities continue in the national marine reserve, because traditional harvesting of resources, as well as research and tourism, are allowed. The traditional communities use the mangrove forest as a source of food (honey, crab, and fish), construction material, firewood, and medicinal purposes (Gang and Agatsiva, 1992; Dahdouh-Guebas et al., 2000). The population live in traditional villages around the administrative sub-locations Gede (∼29,600 people) and Matsangoni (∼16,000 people) and tourist developments around Watamu of ∼26,000 people (2009 census in KNBS, 2010). Associated activities include nature watching, recreational fishing and boating, scientific research and education (Frank et al., 2017; Owuor et al., 2017, 2019a). Farming activities include cultivation of coconuts, cashew nuts and mangoes. Artisanal fishing using traditional methods is also important activity (Gang and Agatsiva, 1992). Cultural shrines associated with the forest are important to the traditional communities in Mida Creek (McClanahanan et al., 2005).

The human activities exert direct pressures by the selective removal of specific species and the increasing encroachment of settlements, within the reserve. Other pressures are land derived pollutants from agricultural runoff, untreated sewage, litter and oil spills due the substantial increase in maritime activity (Lang’at and Kairo, 2008).

These pressures result in a degradation of state of the mangrove. This includes a decline in the mangrove cover and a change to the mangrove community structure (Owuor et al., 2017), contributing to the overall rate of decline in mangrove cover for Kenya of between 0.76% per year between 1985 and 2015 (Kirui et al., 2013). High sediment loads, due to poor agricultural practices in the hinterland, have been particularly destructive for mangroves, causing siltation of aerial roots during periods of flooding, such as during the El Nino years of 1997 and 1998 (Lang’at and Kairo, 2008). Oil spills have also contributed to damage of mangrove aerial roots.

Mida Creek provides important ecosystem services (ES) for provisioning timber and firewood, medicinal uses, and food products; whilst its cultural services are spiritual shrines, educational, recreational, and tourism (Owuor et al., 2017; Frank et al., 2017; Newton et al., 2018). The supporting and regulation services of the creeks are critical for providing shore protection, water filtration, pollution regulation, and habitat to many organisms (Frank et al., 2017; Owuor et al., 2017, 2019a,b). The mangroves provide an important habitat for fauna, including commercially important crabs and fish, as well as providing a breeding ground and nursery (Nagelkerken et al., 2000; Granek et al., 2009). Mangroves have a high capacity to sequester and store carbon (Alongi, 2014), which is an important ecosystem service contributing to mitigation measures such as Reduced Emissions from Deforestation and Degradation (REDD), (Webber et al., 2016).

Indirect pressures related to climate change and sea level rise (SLR) are not well studied for Africa (Ward et al., 2016). However, two studies in Kenya provide some idea what could happen to the mangroves of Mida Creek in the future, with Kebede et al. (2010) predicting an SLR of 1 mm.y^–1, although Lang’at et al. (2014) observed an increase of 4.2 mm.y^–1 in surface elevation in mangrove stands from Gazi Bay, approximately 150 km south of the Creek.

Malanza Wetlands, São Tomé and Príncipe

São Tomé is an equatorial island, west of Gabon with two main seasons, rainy September–May and dry June–September. The Malanza mangrove is only 0.7 km², however, it is the largest in São Tomé and located in Obô Natural Park (PNOST), created in 2006. The wetland is constituted by a complex network of shallow, narrow, channels flowing to a central basin that is connected to the Atlantic through a constricted opening. The fringing vegetation is dominated by the black mangrove Avicennia germinans and the red mangrove Rhizophora racemosa.

There are two village communities, Malanza and Porto Alegre. Each village has a population of approximately 500 inhabitants who rely on coastal fisheries and agricultural activities. Fisheries inside Malanza lagoon include a high percentage of juveniles (Félix et al., 2017). The communities of Malanza and Porto Alegre organize boat tours that complement the income of local families.

The human activities exert several anthropogenic pressures on the wetland. A challenging pressure is the introduction of non-indigenous species, such as the tilapia Oreochromis mossambicus, which tends to be an aggressive invader (Canonico et al., 2005) in the wetland. The construction of a road-bridge that crosses the lagoon to give access to the village of Porto Alegre, severely restricts the flow of water and sediments (Félix et al., 2017). Agricultural intensification and oil palm monoculture threaten the natural wetland habitats and biodiversity.

The current state of the environment includes water column stratification and hypoxia/anoxia at the bottom and wetland sediments. Oxygen depletion can reduce vegetation and biodiversity, as well as affect fish and shellfish stocks. Inputs of nutrients from fertilizer run-off may also promote future eutrophication.

The state changes affect the provision of wetland ecosystem services. The local population is poor and very dependent on the natural resources available in the wetland. Provision of food (e.g., fish and shellfish protein) is affected by the current oxygen depletion at the bottom, with reports of declining fish populations and impacts on human welfare. The wetland also provides an opportunistic feeding ground for marine species and a nursery for the juveniles (Félix et al., 2017). Moreover, palm tree plantations have also reduced the land area available for local agriculture. On the other hand, recreational and cultural activities related to tourism have been increasing, providing a valuable contribution to local subsistence.

Indirect pressures from climate change and sea level rise will affect the future of this mangrove, since the whole system is only just above present sea level. In recent years, the ocean has been claiming a sand bar to the west of the system, near Praia Jalé. If this sand bar disappears, it may affect the entire dynamic of the region, effectively turning the southern tip of the island of São Tomé into an islet, with consequences for the ecology of the mangroves.

Coastal Wetlands in Asia

Vembanad Wetlands, India

Vembanad Lake is a RAMSAR site that spans three districts Alappuzha (Alleppey), Kottayam and Ernakulam, and comprises 4% of the state of Kerala, SW India. It is narrow (0.8–6.9 km), but the longest (96 km) and largest (area 1521.5 km²) wetland in India, running parallel to the coast and broadening in the south. Barrier spits separate the wetland from the Arabian Sea, to which it is connected by two tidal inlets, at Kochi (400 m) and further north at Azhikode (250 m). The wetland includes marshes, mangrove forests, a network of canals and backwaters, small islands and reclaimed land. The wetland has a freshwater southern zone and a saltwater northern zone. The total drainage area is 40% of the area of the State, and there are 10 main rivers draining into the wetland. The annual surface runoff is 2.19 × 10¹⁰ m³, nearly 30% of the surface water resource of Kerala (Anon, 2016).

The Vembanad wetland supports a diverse flora and fauna, including small, isolated patches of mangrove (e.g., at Kumarakom, Vypeen, Kannamali, and Chettuva), (Anon, 2016). The Vembanad wetland and the Kumarakom Bird Sanctuary on the east coast support waterfowl migrating along the Central Asian Flyway and a large wintering population (Narayanan et al., 2011). Fauna also includes a large variety of reptiles and commercial fish (mainly oligohaline), valuable crustaceans, (e.g., prawns), and molluscs, (e.g., clams).

The population density (1,103 km^–2) in the 2011 census was almost three times the mean for India, (382 km^–2). There are many human activities in settlements along the wetland, including shipping, agriculture, fisheries, aquaculture, shell mining for lime and houseboat tourism on the famous backwaters. The town of Alappuzha is sandwiched between the wetland, the lagoon and the Arabian Sea and famed for its large network of canals that meander through the town. The major shipping port of Kochi (Cochin) is located at one of the inlets to the Arabian Sea and recently, the new container terminal at Vallarpadam has been added⁴. The 1,252 m long Thanneermukkom salt-water barrier, the largest mud-regulator in India, is located where the lagoon is narrowest and has changed the hydrology of the wetland. Thanneermukkom barrage was built in 1976 to prevent saline ingression during the dry season in the low lying Kuttanad region, known as the ‘Rice bowl of Kerala.’ Shallow parts have been bounded for punja cultivation, Padasekharam/low lying rice fields. Rice cultivation is the main crop, with extensive plantations of coconut, banana, tapioca, cereals such as millet, pigeon peas, peanut, and pawpaw grown as intercrops (Planning Commission Government of India, 2008). Constructed infrastructure includes roads across drainage canals, as well as a network of roads and bridges in the Kuttanad region, and commercial developments. Fermentation of coconut husk for coir manufacture is carried out extensively on the surface waters of the lagoon (Kumar, 2018). The black clam Villorita cyprinoides is harvested by hand picking or using a canoe for its shell rather than as shellfish (Laxmilatha and Appukuttan, 2002).

Changes in land-use from reclamation is a major and growing direct, anthropogenic pressure. There are extensive encroachments changing the land-use of the wetland for agriculture, especially rice cultivation (Planning Commission Government of India, 2008). Excess fertilizers and pesticides used in agriculture drain into the wetland system. Another major pressure results from changes in hydrology for irrigation and hydroelectric schemes affecting the connectivity of wetlands and surface waters, tidal and inundation regimes, circulation and mixing patterns (Haldar et al., 2019). Untreated sewage is discharged directly into the lake from houses in the wetland, as well as from houseboats used by the tourism industry. Also, many rivers in the catchment area flow through industrial areas carrying polluted effluents to the wetland (Varkey et al., 2016). Indiscriminate exploitation of small-sized clams, closure of the Thaneermukkom Barrage, frequent dredging, pollution due to retting, effluents from shrimp processing plants/factories and extensive weed growth are major pressures on the wetland (Laxmilatha and Appukuttan, 2002).

The state of the environment and ecosystem of the wetland is affected by these pressures, especially south of the barrage at Thaneermukkom, which affects the distribution and ecology of the wetland. The area of Vembanad wetland has decreased by 465 ha from 2002 to 2014 (Varkey et al., 2016). Reduced connectivity and flushing has resulted in eutrophication (Varkey et al., 2016). It has also led to the proliferation of non-indigenous, invader species (Eichhornia crassipes and Salvinia molesta) from Latin America that are widely distributed and a threat to the wetland (Kumar and Rajan, 2012). The 2008–2011 fish count by the Ashoka Trust for Research in Ecology and the Environment (ATREE), recorded 67 species of fin fishes and 14 species of shellfish. Earlier studies indicated that the fish fauna of Vembanad was dominated by marine migratory species (56%), but the 2011 fish-count indicated that salinity-tolerant, freshwater species dominated (69%) and the marine migrants were reduced to 31% (Kumar and Rajan, 2012). Plastic bags, bottles and other wastes dumped in the wetland and lake settle to the bottom and adversely affect bottom feeders, e.g., gobids, and the fishes that attach their eggs to the benthic substratum, (Kumar and Rajan, 2012). A decline in carnivores and a dominance of omnivores (58%) followed by 6% herbivores, 6% larvivores, and 2% detritivores also indicates organic pollution (Kumar and Rajan, 2012). The discharges of industrial effluents contaminate and pollute the wetland. The pollution load index indicates that the sediment is heavily polluted in the north and moderately polluted in the extreme south port region (Selvam et al., 2012). For example, there is severe and moderately severe enrichment of Cd and Zn with minor enrichment of Pb and Cr in the north. Mercury contamination is also higher in the north (Mohan et al., 2014). The presence of high mercury concentration in the subsurface sediment indicates historic, industrial mercury deposition.

The degradation results in the loss of ecosystem services in the wetland. The Thaneermukkom barrage has affected the production of fish and shrimp from the lagoon but has been successful in keeping the Kuttanad water fresh for agriculture (Varkey et al., 2016). The estimated annual mean fishery catch (provisioning ecosystem service) is 4774.46 t, only 10.1% in the south and 89.9% in the north (Asha et al., 2015). The main commercial species are marine penaeid prawns, clams such as Villorita cyprinoides that represents 70% of the production, cyprinoid fish and Meretrix meretrix (Kumar and Rajan, 2012).

Furthermore, indirect pressures from climate change and rising sea levels are of concern as the entire wetland is low lying. Estimates indicate that a 1m rise in sea level will inundate about 169 km² of the coastal region around Kochi, especially areas adjacent to the tidal creeks, backwaters and lakes reaching inland areas far from the coast (INCCA, 2010).

Sundarbans Wetlands, Bangladesh and India

The Sundarbans coastal wetland on the south coast of Bangladesh and northeastern India is fed by the river Ganges and hundreds of tributaries. It includes the largest, single tract, mangrove forest in the world with a total area of 10,000 km², 62% in Bangladesh and 38% in India (Islam and Gnauck, 2009). This mangrove forest constitutes about 51% of the forest area of Bangladesh and about 50% of the revenue for the forestry sector (Islam and Gnauck, 2009). The Sundarbans wetland is famous for its diverse biodiversity, which includes about 334 species of plants, 282 bird species, 49 mammal species, 210 fish species, 63 reptile species, and 10 each of amphibians and molluscs (Rashid et al., 1994; Biswas et al., 2007). Several rare species such as the tiger (Panthera tigris), the dolphins (Platanista gangetica), and the crocodile (Gavialis gangeticus) are found in Sundarbans wetland (Gopal and Chauhan, 2006). Endangered species such as the tiger and dolphin epitomize the conflict between the loss of habitat (quantity and quality) and human activities in the Sundarbans wetland. In 1992, about 601,700 ha of forest reserve of the Sundarbans in Bangladesh, and in 2019, 423,000 hectares of the Indian Sundarbans were declared Ramsar sites⁵. In 1999, 32,400 hectares of the Sundarbans in Bangladesh part were declared a UNESCO World Heritage Site (Islam and Gnauck, 2009).

Human activities in the Sundarbans mangrove forest ecosystem exert multiple pressures on this coastal wetland and the over-exploitation of natural resources. Sundarbans has a population of over 3.5 million inhabitants, mostly living below the poverty level and heavily dependent on forest natural resources (e.g., fire wood, livestock fodder, timber, honey, and fishes) for their food and livelihood (Hoq, 2007; Ahmad et al., 2009). Households that are dependent on Sundarbans obtain important monetary benefits annually from capture fishery (U$ 976 ha⁻¹), fuel energy (U$ 80 ha⁻¹), honey (U$ 53 ha⁻¹), and fodder (U$ 26 ha⁻¹), (Rahman et al., 2018). Unplanned developments threaten this World Natural Heritage (Islam et al., 2018). Land-reclamation and polders in the 1960’s increased agricultural land. Aquaculture farms cleared large areas of mangrove for shrimp ponds, without considering the externalities such as the chemicals from the effluents. Poor people, especially women and children, use illegal, fine-meshed push nets to catch of wild post larvae (PL) of Penaeus monodon shrimp. Barrages in the catchment (e.g., the Farakka barrage in the river Ganges) have decreased the freshwater flux to the wetland, especially in dry season February–June (Hoque and Alam, 1995; Wahid et al., 2007; Islam and Gnauck, 2009; Bahar and Reza, 2010). Dykes to protect from coastal flooding have also been constructed in the SW of Bangladesh, further disrupting the natural hydrology. The construction of the Rampal power station (Bangladesh), a 1,300 MW, coal-fired power plant close to Sundarbans territory (Tamim et al., 2013; Islam and Al-Amin, 2019), has resulted in protest from environmentalist groups anxious about pollution of the Sundarbans wetlands. Consequences include atmospheric emissions and land storage of fly ash from the power plant (Tamim et al., 2013).

Human activities in the Sundarbans exert multiple pressures on this coastal wetland and the over-exploitation of natural resources. Pressures include modifications of hydrology, changes in land-use and encroachment into the forest, for example to construct aquaculture ponds, unsustainable harvesting of shrimp post-larvae, over-fishing and illegal logging. The balance of freshwater and seawater, to the mangrove wetlands (Islam, 2006) has been modified.

These pressures have affected the state of the environment and ecology of the Sundarbans wetlands (Islam and Gnauck, 2009; Rahman et al., 2010). Pressures such as oil pollution, metals and industrial waste, untreated sewage effluents degrade the environmental state (Iftekhar, 2004; Rahman et al., 2009; Islam et al., 2017; Ranjan et al., 2018). The water and soil salinity in Sundarbans area has increased due to low freshwater influx from upstream, which is the main cause of top-dying and die-back diseases of trees, especially the Sundari (Heritiera fomes) and Goran (Ceriops decandra), (Khan et al., 1994; Islam and Gnauck, 2009). The destruction of 9,500 ha of mangrove forest for shrimp cultivation has caused a dramatic decline in dominant mangrove species such as Excoecaria agallocha and Xylocarpus mekongensis (Iftekhar and Saenger, 2007) and widespread loss of biodiversity.

There is a loss of ecosystem services because of the degradation of the state of the wetland. The provisioning services that supply natural resources (mainly forest products) from the Sundarbans have declined since 1996 (Hossain et al., 2016). The reduction of fresh water flow from the river Ganges, the over-capture of wild shrimp post-larvae, the simultaneous bycatch of juvenile fish and crustaceans, salinity intrusion, uncontrolled tourism, inadequate planning and lack of ecosystem based management are effecting the biodiversity of Sundarbans ecosystems, hence affecting livelihood and food security of coastal community of Sundarbans region (Ahmed and Troell, 2010; Islam and Bhuiyan, 2018; Rahman et al., 2018; Islam, 2019). The collection of Penaeus monodon post-larvae destroys the larvae and juveniles of other shrimps, finfish, and other macro- zooplankton (Hoq et al., 2001). Therefore, the collection of shrimp PL from natural sources for aquaculture operations is directly influencing in reduction of wild fisheries (Primavera, 2006). The wild aquatic biodiversity (specially the benthic community) might be also in risk due to the toxicological effect of various chemicals used in shrimp ponds (Flaherty et al., 2000). The Sundarbans provide a regulating ecosystem service as a protective, natural boundary during cyclones, and in the last couple of decades it has protected over 10 million human lives from cyclonic storms (CEGIS, 2007). Clearing the mangrove for agriculture or aquaculture has a deleterious effect on this regulating ecosystem service.

With respect to indirect pressures, the population density and the susbsidence low-lying lands of the Sundarbans make them especially vulnerable to flood risk, whether from sea-level rise or cyclone storm surges (Brown et al., 2018). Like all coastal wetlands, the Sundarbans regions is at greatest risk due to global climate change, which will influence the distribution and productivity of Sundarbans resources and aquatic biodiversity (Loucks et al., 2010). An additional problem is the increased salinity of the wetlands that affects the distribution and survival of the mangroves (Dasgupta et al., 2017). The loss of the coastal protection ecosystem service of mangroves would only increase the vulnerability of the whole system (Barbier, 2016).

Huang He (Yellow River) Delta Wetland, People’s Republic of China

The coastal wetland of the delta of the Huang He (Yellow River) is near the city of Dongying, in the Shandong Province, China. The area of the wetland is 18,000 km² with a population of 5.2 million. The continental monsoon climate is warm and temperate (Li et al., 2014) with a mean annual temperature range from 11.7 to 12.6°C and ∼200 frost-free days. The mean annual precipitation is 530–630 mm, with 70% of the rainfall during the wet, early summer from May to July (Li et al., 2014). The wetlands include various aquatic habitats such as rivers and channels, estuarine waters, coastal and salt lakes, ponds and reservoirs, shrimp and crab cultivation ponds (Cui et al., 2009). Migrating birds from northeast Asia and from the western Pacific rim use the wetland as an overwintering and breeding site.

The delta wetland is affected by huge pressures from several human activities especially agriculture, aquaculture of fish and petro-chemical industries (Li et al., 2014). Land-use changes have converted grassland and wilderness to cultivate salt-tolerant crops and grasses, clover, maize, cotton, and Chinese date. Shrimp ponds and saltpans have been constructed in large areas of the wetland (Zhang et al., 2011). There are also thousands of oil wells of the Shengli oilfield in the wetland.

These human activities exert direct pressures on the wetland. Intensive agriculture and the growth of urban areas have almost halved the area of natural wetlands from 1976 to 2008 (Chen et al., 2011). The construction of roads between the river and wetland has decreased the water supply to the wetland. The implementation of flow-sediment regulation has reduced connectivity and modified the hydrological conditions, hence the wetland landscape (Bai et al., 2012). River diversions for irrigation have altered the hydrology and decreased the river fluxes to the wetland (Ottinger et al., 2013). Over-extraction of deep groundwater causes land subsidence, which could accelerate local relative sea level rise, increasing the vulnerability to storm surge, flooding, saltwater intrusion and coastline erosion (Liu and Huang, 2013). Saline aquaculture may cause secondary salinization in the future. The oil exploration and flow-sediment regulation could cause contamination by petroleum hydrocarbon, polycyclic aromatic hydrocarbons, arsenic, and cadmium (Wang et al., 2009; Bai et al., 2012).

The state of the ecosystems in the wetland was seriously affected by the depleting water resources, degradation of soil quality, pollution, agricultural, and industrial activities (Zhang et al., 2016). Economic development has resulted in a decrease of the habitat for the red-crowned crane habitat by 5,935 ha from 1992 to 2008 (Wang et al., 2017). The coastal blue carbon storage in the delta has decreased by 10.2% during 1970–2010 due to land use change (Ma et al., 2019). Since 2000s, the implementation of a wetland restoration project and a water regulation scheme (WSRS) has significantly improved the structure and functions of the wetland ecosystem. However, the altered flux and grain-size composition of sediments due to the implementation of the WSRS may in turn aggravate elemental imbalance, impacting estuarine and coastal geochemical processes and the wider ecosystem (Li et al., 2019).

There are impacts on human welfare from the loss of wetland ecosystem services. The lost wetland area and the decreased water supply has degraded bird habitats. Construction of dams in the catchment perturbs sediment supply, making the wetland vulnerable to erosion. Houses and oil fields on the coast have been partly destroyed by storm surges and coastal erosion (Liu and Huang, 2013). The increased salinity level in groundwater and soils caused by seawater intrusion has decreased agricultural production. Potential heavy metals and oil contamination from agro-activities and oil exploration taint seafood and are public health issues.

Indirect pressures from sea-level rise also affect the Yellow River Delta wetlands. The topography is such that the river delta has changed position many times in the past but it is now constrained by engineering projects. The combined effects of these changes, subsidence and sea-level rise threaten the wetland habitat, highlighting the need for a social-ecological adaptive management plan (Zhang et al., 2016). Nevertheless, the Yellow River Delta is one of the few large deltas in the world that can offset Sea Level Rise by 2100 due to the huge sediment input from the Yellow River (Giosan et al., 2014).

Changjiang (Yangtze) Coastal Wetlands, People’s Republic of China

The Changjiang (Yangtze) River, the longest river in China, discharges into the East China Sea in a temperate climate zone near Shanghai. The Changjiang coastal wetlands are estuarine and meso-tidal. The wetland, including the intertidal land and the areas shallower than 6 m water depth, occupies an area of some 3,050 km² at the beginning of the 21st century. There are saltmarshes, mudflats, and estuarine shoals (Li et al., 2009). The deltaic areas are extensive, with a total area of around 25,000 km², and they are densely populated, with more than 1,000 million inhabitants. Shanghai had a population of 22.3 million (Statutory City = SC) to 34 million (Functional Urban Area = FUA) in 2010 (OECD, 2015). In addition, there are other large cities in the Changjiang River delta, such as Nanjing (7.2 million SC to 11.7 million FUA) as well as Suzhou, Wuxi, Nantong, Changzhou, Yangzhou, Taizhou, Jiaxing, and Huzhou. The area is experiencing rapid changes in response to both natural processes (e.g., shoreline hydrodynamics and sediment dynamics) and human activities (e.g., land reclamation). The shoreline is often hit by typhoon induced storm surges, which has a trend of enhancing intensity in response to sea level rise and the warming climate (Gao et al., 2019).

Intensive human activities exert direct pressures on the Changjiang coastal wetlands. The most important ones include: dam construction that causes modifications to hydrology and sediment dynamics; rapid urbanization in the catchment and increased pollutant discharges; land reclamation along the estuarine shoreline; artificial introduction of the Spartina alterniflora species into the region; and projects for water resource utilization. More than 50,000 dams have been built in the Changjiang catchment, of which the Three Gorges Dam is the largest. As a result, the sediment discharge has been reduced by up to 70% since the 1980s (Yang et al., 2005) and the suspended sediment concentration of the river water in the downstream section is significantly reduced (Yang et al., 2018). Land-reclamation for the urban development of Shanghai and Pudong has been an important activity up to the 1990s.

These activities have resulted in pressures on the wetland. Foremost are pressures on the hydrological system and delivery of sediments. Although the total water discharge remains almost the same, the timing of the delivery has changed with an increase in the dry seasons but a decrease in flood seasons. The Changjiang River delta reached the limits to its expansion after the construction of the Three Gorges Dam (Gao, 2007), and shoreline recession is now occurring in some places. Water supply to Shanghai is a critical issue. The treatment of the water from local small rivers is costly, and the main body of the estuary is affected by saline water intrusion. To solve this problem, reservoirs to store Changjiang freshwater have been built on deltaic islands such as Chongming (the largest) and Jiuduansha (newly formed). The largest reservoir, Qingcaosha, is on Changxing Island. It was completed in 2010 and provides some 7.2 million m³ of water per day, which is sufficient for 11 million people. Land reclamation has declined because the shoreline progradation has slowed down in response to the reduction of river sediment input. The rapid industrial, agricultural, and urban development has also resulted in increased pollutant discharges, including nutrients, heavy metals, pesticides and micro- plastic particles (Zhao et al., 2014). A non-indigenous species from North America, Spartina alterniflora, was artificially introduced into the wetland in the 1980s. It has expanded rapidly (Gao et al., 2014) since the 1990s and is now a dominant species in the Changjiang wetland (Li et al., 2009). The local nematodes and macrobenthic invertebrates have adapted to the S. alterniflora marsh, but the native marsh plants such Scirpus mariqueter and P. australis are affected (Chen et al., 2004, 2007; Zhao et al., 2009). S. alterniflora occupies a lower position in the tidal flat compared with the native species, so land reclamation is primarily of Scirpus mariqueter and P. australis marshes and these species have very limited space to expand outside the sea dykes. Ecological restoration has become a recent focus for regional development. Five Nature Reserves were established by the State Council in 2005 to protect the coastal wetlands, including the Chongming Dongtan National Nature Reserve. The Ramsar Convention listed it as a ‘wetland of international importance’ in 2002. New techniques and measures have been adopted to create wetland along the shorelines that are artificially modified. For example, underwater dykes are built parallel with the sea dykes to enhance the accretion rate and the area of intertidal zone, so that new marshes can be formed in front of the sea dykes.

The anthropogenic pressures from human activities have changed the state of the environment and ecosystem. Land reclamation, the reduction of riverine sediment input and decreasing deltaic shoreline growth have led to a large-scale decrease of coastal wetland area and loss of biodiversity. The wetland area in 2016 was less than half that of 15–20 years prior. The native saltmarshes are disappearing because of lack of space for expansion. Although some are conserved in the nature reserves, future morphological changes due to sediment accretion may eventually destroy these last refuges. The S. alterniflora marsh initially expanded, but now its area is also decreasing because of reclamation. If the wetland loss from reclamation is not compensated by the various ecological restoration schemes, future land use requirements for urban development will further reduce the area. Contamination and pollution of the estuary affect the ecosystem health. Water quality becomes a critical problem due to the enhanced input of heavy metals and organic chemicals (Cao et al., 2012). The contaminant concentrations are high in the wetland sediment of the estuary. The pressure from excessive loading of nitrogen from fertilizer, manure, sewage and aquaculture stimulate eutrophication, hence Harmful Algal Blooms and hypoxia events occur with an increased frequency of occurrence and spatial extent (Bianchi and Allison, 2009).

The present changes taking place in the wetlands have consequences on the ecosystem services. The loss of area decreases all the ecosystem services of the wetland such as coastal protection, denitrification and carbon sequestration. The wetland provided fish spawning grounds and a nursery feeding place for young fish. Thus, the life cycle of fish species in the 3 traditional fishing grounds near the Changjiang River mouth is affected. The loss of 71% loss of wetlands from 1990 to 2000 has caused an estimated loss of 62% of the total value of ecosystem services in the Chongming Dongtan Nature Reserve (Zhao et al., 2004). Although S. alterniflora marshes increased the primary productivity, some sea birds (e.g., Charadriidae and Scolopacidae) that need mudflats are affected, and the natives have insufficient space to grow (Ma et al., 2007, 2009; Li et al., 2009). How the ecosystem functioning is influenced by S. alterniflora needs further investigation.

Efforts have been made by the Shanghai government to reduce the negative effects of wetland changes on human welfare. One of the responses has been the establishment of nature reserves and areas for ecological restoration. The fishery catch is decreasing, partly because of the insufficient wetland space (Jin et al., 2007). The management response would be to maintain the stability of the native saltmarshes and simultaneously to use the S. alterniflora marsh as an ecological restoration tool. Soft engineering could be adopted to increase the space for wetland development, and pollutant input should be controlled to improve the water quality of the estuary. For these purposes, efficient management is required, in the context of the long-term climate and sea level factors and the short- term anthropogenic influences (Cheng and Chen, 2016; Ding, 2016).

Indirect pressures also affect the Changjiang (Yangtze), where a megacity is built on a low-lying, sinking deltaic wetland, in a zone prone to supertyphoons that is also very vulnerable to flooding and storm surges (Cui et al., 2015).

Mekong Delta Wetlands, Vietnam

The Mekong delta in the south of Vietnam includes 13 provinces occupying 40,600 km² and is home to about 18 million inhabitants. Here, the Mekong drains via nine branches into the South China Sea. The subtropical delta undergoes distinct dry and rainy seasons. The delta includes temporarily inundated sandbars and mudflats, as well as several types of wetlands. These are: salt marshes; coastal mangrove ecosystems, such as Ca Mau National Park, Soc Trang, and Bac Lieu; reed wetlands, such as Ha Thien Plain and Tram Chim National Park (Plain of Reeds); and peat swamp wetlands, such as U Minh Thuong National Park. Several National Parks and nature reserves have been established in the Mekong Delta wetland. The area of mangrove in Mekong delta coast is 100,000 Ha. These mangrove forests are especially biodiverse with 98 species of trees, 36 species of mammal, 182 species of birds, 34 species of reptile, 6 species of amphibians, and 260 species of fishes. The main cities in the delta are Can Tho, Ho Chi Minh, Ca Mau, Bac Lieu, My Tho, Tra Vinh, Soc Trang cities and these are growing rapidly in population and area.

The main human activity is rice crop cultivation in rice paddy fields that are human controlled wetlands. Some are protected by complex diking systems and are intensively farmed, yielding 2, 3, and recently up to 4 harvests per year. Some paddies are under less intensive use and used as fishing grounds during the flooding season (Duy et al., 2015). Illegal clear cutting of mangroves continues in strictly managed and protected regions, such as the famous Can Gio Mangrove Biosphere reserve (Kuenzer and Vo, 2013). These illegal activities are hard to monitor and law enforcement is still weak. The overall socio-economic transformation, urbanization (e.g., the Delta Cities of Ca Mau, Soc Trang, Ben Tre, and especially Can Tho, just to name a few), and industrial expansion (petrochemical and coal/fuel) ongoing in the delta (e.g., sea-food processing and agro-industry especially around Can Tho and Long Anh) lead to a general overexploitation of resources, including overfishing (Pangasius, sting ray, catfish, and elephant fish to name only a few), unsustainable sand dredging, and the sale of topsoil. Economic activities are rice cultivation, animal husbandry (chicken, ducks, pigs, and cows) and aquaculture (especially shrimp and Pangasius). Extensive mangrove areas have been destroyed by the rapid expansion of coastal aquaculture (Kuenzer and Vo, 2013; Vo et al., 2015).

Many human activities exert direct pressures on these fragile wetlands. The construction of dykes, dams, urban, and industrial areas affect the hydrology and connectivity of the wetland. Coastal engineering activities are often driven by the hope for economic benefits and are executed for ministerial line agencies and related companies. These result in the ongoing closure of Mekong River main stem and tributary channels, decreasing connectivity. Wetland connectivity is decreased as the network of river branches and canals in the delta are increasingly obstructed by dykes, levees and sluice gates. The same applies to terrestrial ecosystem connectivity, which is decreasing due to fractionation by highways and roads. These are aggravated by the decrease in sediment loads from the upstream areas (Kuenzer et al., 2013).

These pressures affect the state of the wetlands, so that flora and fauna biodiversity is declining. The state of the water quality affected by fertilizer, pesticides and endocrine disruptors from rice farming, vegetable cultivation and animal husbandry. Furthermore, chemicals and antibiotics used in aquaculture ponds contaminate groundwater, soils, and the food chain (Ottinger et al., 2016). Elevated levels of pesticide have resulted in water pollution with traces detectable in ground, surface and even locally filled bottled drinking water (Toan et al., 2013). The area of area of mangrove in Mekong delta coast is decreasing with rate of 5% per year induced by human activities.

The deteriorating state of the wetland affects the delivery of ecosystem services. Healthy mangroves provide: provisioning services, e.g., fire wood, construction wood, medicinal products, honey, and fish; supporting, e.g., breeding grounds; protecting services, e.g., erosion and storm control; regulating services, e.g., water filtration and buffering capacities; cultural and recreational services, e.g., resting, eco-tourism, and spiritual activities (Vo et al., 2012, 2015; Kuenzer et al., 2013). The conversion of natural reed wetlands decreases their delivery of ecosystem services. These include a loss of provisioning ecosystem services, e.g., roofing and weaving material, fish supply; ecosystem services, e.g., water filtration and cleansing; and cultural- recreational ecosystem services (Vo et al., 2012, 2015; Kuenzer et al., 2013). Natural mangrove belts acted as barriers against high tides, storm surges and general sea level rise. The loss of these mangroves results in increased salt-water intrusion into the aquifers and soils of the delta.

The activities and related pressures exerted on the Mekong wetland have led to partially irreversible impacts on human welfare, especially affecting the rural poor who depend on natural resources for their livelihood. Artisanal fishers report a loss of fish species and decreased catch landings. Salt-water intrusion affects small-scale rice farmers. The rural population often drink untreated ground and surface water and suffer from intestinal problems and other health issues. Boat-dependent mobility is impaired by an increased regulation of water ways. Many typical, traditional lifestyles are likely to disappear in the next years, including floating markets, artisanal clam collection and fisheries, small-scale water transportation and complex, sustainable farming approaches, such as the multispecies duck-rice-vegetable agriculture. This will entail a loss of cultural values and an overall decrease of the unique character of the Mekong delta wetland.

Climate change and related sea level rise are the main causes of indirect pressures in the wetland, including coastal erosion and salt-water intrusion. Managing flood risks in the Mekong Delta is a serious challenge in the context of climate change and socioeconomic developments (Hoang et al., 2018).

Coastal Wetlands of Oceania

Mangrove Forests of the Gulf of Papua, Papua New Guinea

The Central Highlands of Papua New Guinea are drained by the rivers Purari, Kikori, and Fly that pass through regions of extremely high rainfall and into a complex of tide- and river-dominated estuaries, delivering (384 Mt a⁻¹ of sediment and 470–690 km³ water into the Gulf of Papua) (Aller et al., 2008). The wetlands are dynamic, with accretion and erosion occurring simultaneously indifferent parts of the deltas, with delta-front erosion of up to 43 m per year over the period 1973–2002 (Shearman, 2010). There are 3,780 km² of wetland mangrove on the Gulf of Papua (Bryan et al., 2015), the largest, virtually pristine mangrove forests in the Asia-Pacific Region (Cragg, 1983), and particularly diverse (Duke et al., 1998). Pioneering species, e.g., Sonneratia lanceolata dominate accreting shorelines. Mature forests with canopies of up to 30 m are dominated by Rhizophora and Bruguiera. Transitional forests occur at the boundary with freshwater habitats (Cragg, 1983). There are large areas of pure Nypa palm stands in low salinity parts of the deltas. The mangrove wetlands are nursery grounds for fish, crabs, and prawns, (Frusher, 1983). Offshore of the mangroves, there are feeding and breeding grounds for commercially harvested prawns (Gwyther, 1983), and rock lobster (Dennis et al., 2001).

Human activities in the immediate vicinity of this huge mangrove are remarkably small. Four to five hundred years ago, traditional trading Hiri voyages traversed the Gulf (Barker et al., 2015; David et al., 2015). There are no urban areas but some villages on sand bars at the seaward edge or just inland of the mangrove rather than within the mangrove (Cragg, 1983). The population is low, approximately 107,000, and relies on subsistence utilization of a range of mangrove resources: mangrove wood for poles for house construction, fuel and tools; edible mangrove fruits and palm hearts; medicinal uses and dyes (Liebezeit and Rau, 2006); thatching and basket weaving using Nypa fruticans fronds. Offshore there is one of the most commercially important fisheries in Papua New Guinea – the demersal prawn trawl fishery that gains an income of (US$3M per year through a local fishing fleet) (Kompas and Kuk, 2008; White et al., 2019).

The low population and subsistence utilization of mangrove resources represent only a low, local direct pressure at present. The estimated use of fuel wood is only 6.4 kg person⁻¹ d⁻¹ and construction wood at 0.6 m⁻³ household⁻¹ a⁻¹ (Page et al., 2016). The main pressures are from human activities elsewhere: the large, commercial logging concessions inland of the wetland (Bryan et al., 2015); the oil pipelines from the highlands at Kutubu through the mangrove forests to the Kumul Marine Terminal offshore; and the huge Ok Tedi open-pit gold and copper mine is in the watershed of the river Fly. Mine tailings have increased the sediment load at peak rainfall (Shearman et al., 2013), transporting copper in dissolved and particulate form (Bolton, 2009).

Direct pressures may increase as the area is further developed in the future. Logging inland of the mangroves is likely to increase sediment input to the wetland and may require construction of coastal log-loading facilities. The potential commercial exploitation of ethanol production from tapping Nypa syrup has been explored but not exploited. There have been evaluations of potential for pulp wood and wood chips, but the soft sediments make harvesting problematic. Bark from Rhizophora trees was used to produce tannin extract (cutch) in a factory that operated between 1954 and 1957, but this activity ceased due to competition from alternatives to cutch (Percival and Womersley, 1975). The construction of a hydroelectric dam on the Purari River (Wabo) has not yet taken place. A multidisciplinary environmental impact study of plans predicted a reduction in sediment load and increased predation on prawn larvae, but no significant effects on delta fertility (Cragg, 1983). A project to exploit natural gas envisages an additional pipeline from the highlands into the Gulf.

The effect of these pressures may affect the state of the wetland and will entail a loss of ecosystem services such as supporting services, e.g., the high primary production and the nursery function for fish and crustaceans. Unusually high bacterial decomposition rates of sediment organic carbon leads to close benthic-pelagic coupling supporting the Gulf of Papua prawn fishery (Alongi, 1995). The regulating services of the mangrove forests help to stabilize the sedimentation and erosion of the delta. Furthermore, the sequestration of carbon by the Papua New Guinea mangroves is a globally significant ecosystem service: 2.9% of global carbon stocks in mangroves is estimated to be in Papua New Guinea mangrove forests (Hamilton and Friess, 2018). This is the 5th most important mangrove ecosystem in the world, in terms of carbon stocks once the additional offshore sequestration is combined. Dead plant matter is rich in the lignocellulose complex, which is more resistant to break down than marine-generated particulate organic matter, particularly under anoxic conditions in sediments (Cragg et al., 2020). Part of the forest detritus and almost all subterranean roots are retained, accounting for the exceptionally high carbon sequestration capacity of mangrove wetlands, particularly in New Guinea (Sasmito et al., 2020). An estimated 1.7 × 109 kg a⁻¹ of the organic carbon, derived from the vascular plants and plankton of the mangroves, is exported through the Fly delta to the Gulf of Papua and the Coral Sea Robertson and (Alongi, 1995). The residence-time of soil organic matter is longer in marine sediments (Goni et al., 2006), so 13–27% of the organic matter accumulates long-term offshore (Aller et al., 2008).

Indirect pressures from climate change may alter rainfall patterns, hydrology, intensity and frequency of storms affecting the delta region. Sea level rise is interacting with subsidence of the delta sediments in affecting mangrove distribution (Shearman, 2010).

Summary of the Main Direct Pressures on Coastal Wetlands and Consequences

The Millennium Ecosystem Assessment [MEA] (2005) identified that human population growth and economic development lead to the degradation and loss of coastal wetlands. Anthropogenic degradation and loss of wetland was mainly due to land-use changes, construction of infrastructure, water extraction, eutrophication and pollution, overharvesting of commercial species and overexploitation of natural resources, as well as the introduction of non-indigenous species (Millennium Ecosystem Assessment [MEA], 2005).

We identified that the most important human activities exerting anthropogenic pressures on coastal wetlands can be placed in 2 groups: (i) land reclamation and conversion to agriculture, aquaculture, ports, and urban areas; and, (ii) construction of dams, dykes, polders, drainage channels, dredging that modify the natural hydrology, connectivity, and sedimentology. Thus, the main anthropogenic pressures are land-use change and changes in hydrology, as well as connectivity. The main anthropogenic pressures on the coastal wetlands included in this overview are summarized in Supplementary Table S1. The relationship between these human activities in or around coastal wetlands and resulting anthropogenic pressures on the environment and ecosystem are summarized in Supplementary Table S2.

The anthropogenic pressures (direct and indirect) alter the dynamics of ecosystem function of the coastal wetlands. This affects the natural resilience of the systems and increases their vulnerability. This overview is summarized in Figure 2. Damming in the catchment disrupts the sediment fluxes to coastal wetlands. This leads to erosion and subsidence, (Syvitski and Saito, 2007; Syvitski et al., 2009). Wetlands are dynamic systems, illustrated by the ‘wandering mouths,’ of deltas, such as the Huang He (Yellow River) and Mississippi. In the case of dynamic, coastal lagoons such as the Ria Formosa, inlets open and close. Humans try to stabilize the position of river mouths and inlets for shipping, and channels are dredged to accommodate ships of increasing size. These modifications in the catchment and at the mouth cause changes to the sedimentology and hydrology. Over-extraction of water for agriculture is another common feature that changes the freshwater-saline water balance, so that wetlands that naturally vary from freshwater to saline become increasingly saline. The linked coastal wetlands of Bizerte lagoon and Ichkeul lake illustrate the dramatic effects of loss in connectivity. Changes in hydrology, flow rates and timing of freshwater inputs to estuarine wetlands affects the flora of the wetlands, whether it is seagrass, saltmarsh or mangrove. The vegetation is fundamental to the ecosystem services of the coastal wetlands and have dramatic impacts on human welfare, for example, provisioning services such as fish catch (Kennedy and Barbier, 2016). A holistic understanding of the interlinked hydrology, sedimentology and biology is fundamental for the management of estuarine systems such as coastal wetlands (Alber, 2002). This is particularly important for the assessment of diffuse sources, for example nutrient pressures from farming activities such as fertilizer application.

FIGURE 2

Figure 2. Conceptual diagram summarising the findings, showing an estuarine wetland ecosystem in an unimpacted and impacted state. Symbols are courtesy of the Integration and Application Network, University of Maryland Center for Environmental Science (https://www.umces.edu/ian/search). (Credit: Sonia Cristina).

Another important and widespread anthropogenic pressure is the point source discharge of effluents by industry, farms and domestic sewage shown in Supplementary Table S3. Effluents, especially from industries, can contaminate and pollute wetlands, while eutrophication may result from the discharge of effluents that are rich in organic matter and nutrients shown in Supplementary Table S4.

Most of the anthropogenic pressures identified in this overview correspond to the types I to N of “anthropogenic hazards” from the typology of Elliott et al. (2014) and are summarized in Supplementary Table S5. The value of ecosystem services of a wetland, e.g., the mangroves of Papua Guinea can be globally significant, but the lack of understanding about the value of coastal wetland ecosystem services (Newton et al., 2018) continues to contribute to their degradation. Externalities and the long-term value of ecosystem services are often ignored, for short term, economic gain and/or development. Even when the knowledge exists, it may be disregarded, as in the case of the dredge spoil dumping onto the Abbot Point and Caley Valley wetlands in Australia, which is a habitat of more than 40,000 water-birds (Australian Marine Conservation Society, 2014), despite lessons learned in the Mississippi and other coastal wetlands.

Cumulative pressures change both the state of the environment (e.g., anoxia) and the state of the ecosystem (e.g., loss of saltmarsh, mangrove, and seagrasses). Coastal wetlands provide ecosystem services, such as regulatory services for water quality, coastal protection, carbon sequestration and denitrification, as well as supporting services such as habitat for a wide variety of fauna. The loss of vegetation of the coastal wetlands, represents a loss of a wide range of ecosystem services. There is a decrease in provisioning ecosystem services, e.g., timber from mangroves, seafood yield from the wetland, and also from the adjacent sea; supporting ecosystem services, e.g., oxygenation from seagrasses, nursery services, denitrification, carbon sequestration, and habitat for migrating wildfowl; regulating ecosystem services, e.g., water purification and natural hazard protection, e.g., floods, storm surge, and tsunamis cultural ecosystem services, such as loss of traditional lifestyles and artisanal fisheries.

However, there are some ‘bright-spots.’ Awareness and recognition of the value and importance of coastal wetlands is improving, and some nations are now developing ambitious management plans. In particular, the protecting ecosystem service of coastal wetlands gained recognition after the 2004 Banda Aceh tsunami (Spalding et al., 2014). Some of these efforts are transdisciplinary and bring together scientists, policy makers and environmental managers, as in the case of the Huang He (Yellow River) delta and coastal wetlands management plan (Wohlfart et al., 2016).

This is also the case for mangrove wetlands. Papua New Guinea is implementing the UN-REDD+ mechanism (the United Nations Reducing Emissions from Deforestation and forest Degradation plus Sustainable Forest Management, Conservation of Forests, Enhancement of carbon sinks), (Grussu et al., 2014). This aims to decrease emissions (e.g., from slash and burn deforestation) and enhance forest carbon-sequestration. The remote-sensing methodology detailed by Hamilton and Friess (2018), could be used for monitoring to support payment for ecosystem services such as REDD+.

The emphasis of this article has been direct pressures rather indirect, but both will affect the future of wetlands. Coastal wetlands, mangrove forests, saltmarshes and seagrasses are particularly effective at sequestering carbon, as illustrated by the Papua New Guinea mangroves. It is important to consider both historical and contemporary environmental factors to better understand this regulating ecosystem service of coastal wetlands (Witman, 2017). Marshes, seagrass meadows, and mangroves are some of the ecosystems that sequester carbon most efficiently and store large amounts of carbon dioxide as “blue” carbon (Lovelock and Duarte, 2019; Cragg et al., 2020). Conservation of coastal wetlands can therefore contribute to the mitigation and adaptation to climate change (Neubauer and Verhoeven, 2019; Serrano et al., 2019). However, the Blue Carbon potential of coastal wetland restoration varies with inundation and rainfall (Negandhi et al., 2019) as well as management approaches (O’Connor et al., 2020). Degraded coastal wetlands could potentially be re-naturalized to promote an increase in carbon sequestration, as well as additional and valuable ecosystem services, such as denitrification and halophyte cultivation, for example Salicornia.

We conclude this overview by highlighting the importance of coastal wetlands both ecologically and economically. They provide an important buffer between land and sea in the context of sea-level rise and climate change. They are important cogs in the biogeochemical cycles, providing exceptional services such as denitrification and carbon sequestration. The ecosystem services that they provide are consistently underestimated leading to irreversible land-use changes that ultimately destroy the wetlands and impact human welfare. The conservation and ecosystem-based management of coastal wetlands will contribute to several of the United Nations Sustainable Development Goals, SDG, in particular, 2, 3, 6, 12, 13, 14, 15 but also 1, 4, 8, 11.

Author Contributions

AN wrote several sections and edited the entire manuscript. JI wrote Mida Creek, mangroves and edited the entire manuscript for submission. SoC wrote Ria Formosa lagoon and produced the conceptual diagram. GP wrote the Bahia Blanca estuary. RT wrote the Mississippi River. DA wrote the Sunderbans mangroves. SiC wrote the Gulf of Papua mangroves. YLi, CT, YLu, and HZ wrote the Yellow River delta wetland. RR wrote Vembanad Lake. DF wrote Polar coastal wetlands and Mackenzie-Beaufort coastal wetland. CS and BB wrote Bizerte lagoon and Ichkeul Lake. SG wrote Yangtze coastal wetlands. RP wrote Venice lagoon. HK and DT wrote Chesapeake Bay. NN and CK wrote Mekong delta wetlands. AB and RL wrote Malanza coastal lagoon.

Funding

JI was funded by the European Union’s Horizon 2020 Research and Innovation Programme under grant agreement no. 678193 (CERES, Climate Change and European Aquatic Resources) ; CERES project funded this article. AN was funded by a Chinese Academy of Sciences (CAS-YIC) scholarship and an SKLEC-ECNU project 111 scholarship. SoC was funded by Fundação para a Ciência e a Tecnologia (FCT) Scientific Employment Stimulus Programme (CEECIND/01635/2017). This work received additional support through FCT’s strategic projects (UID/MAR/00350/2019CIMA). DF was funded by Natural Resources Canada contribution no. 20200070. AB was funded by Fundação para a Ciência e a Tecnologia (FCT) Scientific Employment Stimulus Programme (CEECIND/00095/2017). This work received additional support through FCT’s strategic projects (UID/MAR/04292/2019).

Conflict of Interest

JI is senior researcher with the research centre CIMA at the University of Algarve, Portugal and is also the co-owner of the Portuguese company Sagremarisco-Viveiros de Marisco Lda.

The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.

Acknowledgments

The authors acknowledge the support and contribution of Future Earth Coasts (FEC), Integrated Marine Biosphere Research (IMBeR), Future Earth Oceans Knowledge-Action Network, and Scientific Committee on Oceanic Research (SCOR).

Supplementary Material

The Supplementary Material for this article can be found online at: https://www.frontiersin.org/articles/10.3389/fevo.2020.00144/full#supplementary-material

Footnotes

1. ^ https://laws-lois.justice.gc.ca/PDF/SOR-2010-190.pdf
2. ^ https://www.ine.pt
3. ^ http://www.lifeseresto.eu/
4. ^ https://ernakulam.nic.in/vallarpadam-terminal/
5. ^ https://rsis.ramsar.org/ris/2370

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