To the untrained eye, salt marshes don't seem like the coolest ecosystem. They smell like a hard-boiled egg that’s been in the fridge for three months, they're flat, and if you don't watch where you're walking, you could end up knee-deep in a muddy hole. Despite being somewhat unappealing to the senses, salt marshes have some incredible qualities that make them important to the climate, animals, and local communities. Since they are often unrecognized for their better qualities, between 25% and 67% of salt marshes have been altered globally. With the impending doom of sea-level rise and climate change, people are starting to realize the importance of salt marshes in fighting these risks. Fortunately, many researchers have begun to reclaim salt marshes. Aulac may be a small community in New Brunswick, but it’s making big waves in salt marsh restoration. Spencer Virgin, his research team, and other partners conducted the first managed realignments in Maritime Canada, which is reversing historical ecosystem alterations.
The origin story of salt marshes is an amazing one. Salt marshes are an ecosystem that are on the border between marine and terrestrial ecosystems and are heavily influenced by tides. A few thousand years ago, when sea levels began to rise, much of the terrestrial ecosystems on the coast were flooded with seawater, destroying all the plants that lived there. When tides flooded these coastal areas, they deposited large amounts of sediment, which created a blank slate for new species to colonize. However, the salty and waterlogged soil isn't an ideal habitat for most plants. Fortunately, Spartina alterniflora, a salt marsh grass, finds these conditions perfect for survival and stays in the marsh zone that’s flooded daily (Fig. 1). S. alterniflora is known as an ecosystem engineer because it can slow the flow of water and increase sediment deposition, which is critical for other species to establish. Think of S. alterniflora like people in a pool and the tides like a whirlpool. When the people in the pool stop moving, the water circulating in the whirlpool slows. Slow-moving water doesn't have enough strength to carry sediment, so it drops it onto the marsh. Accumulation of soil causes the salt marsh to elevate until it escapes the daily flooding in the high marsh zones (Fig.1). Other grasses, such as Spartina patens, who are less tolerant to flooding and salt, can live in the less frequently floored area that S. alterniflora creates (Fig. 1). As the sediments accumulate and increase the elevation of the marsh, it creates areas even less exposed to tides so salt and flood intolerant species can colonize (Fig. 1).
Figure 1. Salt marsh structure and tidal influence.
Hypothetically, this process of sediment deposition can go on forever. That is part of the reason why salt marshes are so important in the fight against sea-level rise. If salt marshes have space to move horizontally along the landscape, they can continue to elevate and prevent the ocean from flooding neighboring communities. Salt marshes are also one of the most productive ecosystems in the world. They produce new grass annually that can extract CO2 from the atmosphere and store it in their leaves. Finally, salt marshes host many ecologically and economically important marine species, such as striped bass, shrimp, eels, and mussels.
Unfortunately, a huge proportion of salt marshes in eastern North America have been dramatically altered to suit the needs of settlers. How do you alter a salt marsh, and what do you change it to? The sediment the tides bring in from the ocean is chalked full of nutrients and makes a perfect fertilizer. Flat ground and abundant fertilizer create the perfect conditions for growing crops. The only problem is that most agricultural species can’t tolerate salt and flooding. However, farmers found a way around this: in a Trump mentality, they built a wall to keep the ocean out and the nutrients in. These walls are called dikes. But diking causes a problem for salt marshes since tides are one of the driving forces that shape salt marshes. Eventually, salt marshes lose all their carbon sequestration and flood reduction properties.
In New Brunswick (NB), Canada, 30500 hectares (approximately the size of 57000 football fields) of salt marshes have been diked to create farmlands. The Bay of Fundy in NB is known for its nutrient-rich waters, which makes it ideal for salt marsh conversion. The Aulac salt marsh is one of many salt marshes in NB that has been diked. In 2010, sea-level rise and coastal erosion began to wear so heavily at the dike that it broke open. Researchers, local organizations, and the community saw this as an opportunity for restoration. First, they built another dike behind the old one to keep the tides away from the neighboring farms, then removed the old dikes. This process is called a managed realignment and was the first in Maritime Canada. Since the dike was removed, the tides of the Bay of Fundy could reclaim the agricultural fields and turn them back into salt marshes. Virgin et al. saw this as an opportunity to learn about the stages of salt marsh restoration.
After the dike was breached, they did not intervene with any other aspects of the marsh and let the restoration process occur naturally. However, Virgin et al. did conduct an extensive monitoring program to see what steps occurred as the marsh restored itself. Aulac has four salt marshes that are divided from one another, but only two were diked. The remaining two healthy salt marshes are adjacent to the restored ones and were used as a reference for what the final product of the salt marsh restoration should be. Over eight consecutive years, the team monitored changes in plant species, fish and invertebrate communities, and sediment deposition in all four salt marshes. From 2010 to 2018, they noticed a change in the restoration sites from the freshwater grass Spartina pectinata to the salt marsh engineer Spartina alterniflora as sediment increased on the marsh platform. In general, the plant and animal communities became more and more analogous to the reference marshes over time. Although the salt marsh has not yet seen the establishment of Spartina patens and other salt/flood intolerant species, it is firmly in the third stage of salt marsh restoration, where S. alterniflora is abundant and can create the conditions for those species to establish and thrive.
Managed realignment is the perfect compromise to maintain active farmlands while restoring salt marshes that will help combat climate change. For communities like NB, which are at risk for sea-level rise and have lost salt marshes, this research will be an important guideline for future restoration projects.
Cheers,
The Novel Ecologist
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