Coastal Wetlands
Mangroves, salt marshes and seagrass bury carbon in waterlogged mud where it cannot rot. Per acre, they beat every forest on land.
The effect is immediate. This stops an emission that is happening right now.
Project Drawdown classifies this as Emergency Brake.
Origins
For most of the twentieth century, a mangrove was a problem to be solved.
They were mosquito swamps. They stood between a city and its waterfront, between a farmer and his field, between a developer and a beach. Florida drained them. Southeast Asia bulldozed them for shrimp ponds, an industry that boomed in the 1980s on the reasoning that a hectare of mangrove produced nothing and a hectare of shrimp produced money. By some estimates, more than a third of the world’s mangroves were destroyed in the space of a few decades.
Then, in December 2004, the Indian Ocean tsunami killed roughly a quarter of a million people, and researchers began comparing the villages that were destroyed with those that were not. Coastlines that had kept their mangroves fared measurably better. The evidence was contested and imperfect, as evidence in a catastrophe usually is, but the intuition had landed and it did not leave: the swamp had been doing something.
The carbon story arrived later and from a different direction. In 2011, Daniel Donato and colleagues published a study in Nature Geoscience finding that mangroves were among the most carbon-rich forests in the tropics, holding three to five times the carbon of a comparable area of terrestrial forest, most of it not in the trees at all but in metres of black mud beneath them. The term blue carbon entered the language. An ecosystem the world had spent a century filling in turned out to be the most concentrated carbon store on the coastline.
What it actually is
The trick is the same one the peat bogs use, and it works for the same reason: things do not rot properly underwater.
In a normal forest, a fallen leaf decomposes and most of its carbon returns to the air within a year or two. In the waterlogged, oxygen-starved sediment beneath a mangrove or a salt marsh, decomposition stalls. Organic matter accumulates instead of returning, and the mud gets deeper, and it keeps getting deeper for centuries. This is why roughly three-quarters of the carbon in a mangrove is underground, and why the store keeps growing rather than saturating the way a forest eventually does.
Seagrass does the same job entirely underwater. It covers a fraction of a percent of the ocean floor and accounts for something close to a tenth of all the carbon buried in ocean sediment each year, which is a remarkable ratio for a plant most people have never knowingly seen.
These systems also do work we would otherwise have to pay for. Mangroves and marshes absorb storm surge and break waves before they reach a shoreline. They are the nursery for a large share of the fish we eat. They filter sediment and nutrient out of runoff before it reaches reefs and open water. A community that clears them usually discovers the value of this precisely once, during the next storm.
And here is the part that makes coastal wetlands urgent rather than merely valuable: destroying them does not stop the accumulation, it reverses it. Drain a mangrove and centuries of buried carbon begins oxidising. The sink becomes a source.
The numbers
The density. Mangroves store on the order of 900–1,000 tonnes of carbon per hectare, three to five times a comparable area of tropical forest, and they sequester it two to four times faster (Donato et al., 2011). Roughly 75% of it sits below ground, in sediment that can be several metres deep.
The disproportion. Mangroves, tidal marshes and seagrass together cover the equivalent of only about 2–6% of the area of tropical forest, yet their degradation accounts for an estimated 3–19% of emissions from global deforestation (The Blue Carbon Initiative). Pound for pound, nothing on the coast is doing more.
The bleeding. Ongoing loss of blue carbon ecosystems releases roughly 0.45 billion tonnes of CO₂ a year — comparable to the total annual fossil fuel emissions of the United Kingdom. Somewhere between 340,000 and 980,000 hectares are destroyed annually.
What has already gone. Estimates suggest up to 67% of mangroves, at least 35% of tidal marshes and 29% of seagrass meadows have been lost. We removed most of it before we understood what it was.
Restoration works, and quickly. A global synthesis of over 370 restoration sites found that re-foresting mangroves where they previously grew stores substantially more carbon per hectare than planting them on bare tidal flats — and that restoring the feasible deforested area could take up 671–689 million tonnes of CO₂-eq over 40 years (Nature Communications, 2023). Put them back where they were, not where it is convenient.
Why it matters
A mangrove is where the land teaches itself to swim, and it is one of the very few places on Earth where protecting nature and protecting people are not even distinguishable as separate activities.
The same trees that bury the carbon are the ones standing between a village and the next storm surge. The same roots that trap the sediment are the nursery for the fish that the village eats and sells. There is no trade-off to negotiate here, no jobs-versus-owls argument to have. You are either defending the coastline and its people, or you are not.
And the mud beneath is the same kind of inheritance the peat is: laid down slowly, over centuries, by plants that grew and fell and refused to rot. When a shrimp pond is dug, that is what is being spent, and it is being spent for perhaps five to ten years of production before the pond turns acid and is abandoned. It is one of the worst trades our species routinely makes: an ecosystem that took a thousand years to build, exchanged for a decade of shrimp.
Coastal communities have known the first half of this for generations. The science has now caught up to them and added a second reason. It is unusual and rather cheering for the ancestral knowledge and the satellite data to agree this completely.
What it actually takes
Get the water right, then plant. This is the single most common failure in mangrove restoration, and it is the reason so many replanting projects photograph beautifully and are dead within three years. Mangroves are exquisitely sensitive to tidal position, salinity and inundation. Planting seedlings into the wrong hydrology is gardening, not restoration. Fix the water flow and mangroves will frequently return on their own, for free.
Restore where they were, not where it is easy. The evidence is now clear that reforesting former mangrove areas substantially outperforms planting on marginal tidal flats. The convenient site is usually the wrong site.
Confront the shrimp economics honestly. Mangroves were not cleared by vandals. They were cleared by people making a rational short-term calculation, often under a government incentive. Restoration that does not offer those communities something better simply loses the argument again in five years.
Measurement is genuinely hard. Most of the carbon is in deep, wet mud, which makes verification expensive and technically demanding. This is a real barrier to blue carbon finance and it is honest to say so.
Where it matters most
Southeast Asia holds the greatest concentration of mangrove carbon and has lost the most of it, principally to shrimp aquaculture and oil palm. Sundaland and the Coral Triangle are the epicentre: this is where a hectare protected avoids the most emissions in the world.
The Gulf and Atlantic coasts of the Americas are where restoration has the most momentum. Louisiana’s vanishing marshes, the Gulf Coast and the Florida mangroves are the front line where sea-level rise, subsidence and hurricane recovery all converge on the same question.
The Chesapeake and the North Atlantic marshes are the temperate version of the same story, and the place where the argument about “managed retreat” — letting the marsh migrate inland as the sea rises, rather than walling it out — is being had first.
The Mesoamerican Reef is the clearest illustration of ridge-to-reef logic: the mangroves filter what the land sends down, and the reef survives or does not depending on how well they do it.
How to tell it’s being done well
Did they fix the hydrology before they planted anything? If the answer is no, the project will fail, and the only question is how many years it takes to admit it. Ask about tidal flow before you ask about seedling counts.
Are they restoring former mangrove, or planting bare mudflat? The former works far better. The latter is often chosen because it is easier and unowned, which is exactly why it should raise your eyebrows.
Do they count survival, not planting? Seedlings planted is a vanity metric. Trees alive at year five is the measurement. Many programmes report the first and quietly never publish the second.
Have they dealt with the people? A restored mangrove adjacent to a community with no alternative livelihood is a mangrove with a countdown on it.
What you can do
Anyone
- Know where your shrimp comes from. Farmed tropical shrimp is the single largest driver of mangrove loss on Earth, and most people eating it have no idea.
- If you live on a coast, find out whether your marsh is being allowed to migrate inland as the sea rises, or being walled in until it drowns.
- Support the groups doing hydrological restoration. It is unphotogenic and it is the part that works.
Coastal communities
- Mangroves are storm protection that maintains itself and gets stronger over time. No sea wall does that.
- Restoration frequently costs less than the engineering it replaces, and it produces fish.
Policymakers
- Protect intact wetland first. The carbon in the mud is irrecoverable on any timescale that matters.
- Stop subsidising the conversion. Much of the world's mangrove loss was publicly funded.
- Plan for landward migration. A marsh that cannot retreat as the sea rises is a marsh that drowns.
Business and investors
- Blue carbon credits are real but hard to verify, because the carbon is in deep wet sediment. Demand rigorous measurement or do not buy them.
- Fund the hydrology, not the photo. The restoration that works is the boring kind.
Where this matters most
Who is working on this
We are researching which organizations in our directory of 8,493 actively work on this solution, and we only list an organization once we have verified it. That research is ongoing. In the meantime, search the directory yourself:
Questions
Why do mangroves store more carbon than rainforest?
Because their soil is waterlogged and oxygen-poor, so dead plant material does not fully decompose. It accumulates and is buried instead of rotting back into the air. Mangroves hold roughly 900 to 1,000 tonnes of carbon per hectare, three to five times a comparable area of tropical forest, and about 75% of it is underground rather than in the trees.
What is blue carbon?
Carbon captured and stored by coastal and marine ecosystems, principally mangroves, tidal salt marshes and seagrass meadows. The term entered wide use after research in 2011 showed these systems to be among the most carbon-dense on Earth. The defining feature is that most of the carbon is buried in sediment rather than held in living plants.
What happens to the carbon when a mangrove is cleared?
Draining the sediment exposes it to oxygen and centuries of buried organic matter begins to oxidise and release. Destruction does not merely stop the storage, it reverses it, turning a carbon sink into a carbon source. Ongoing loss of blue carbon ecosystems is estimated to release around 0.45 billion tonnes of CO2 a year, comparable to the entire fossil fuel emissions of the United Kingdom.
Why do so many mangrove planting projects fail?
Because they plant before fixing the water. Mangroves are extremely sensitive to tidal position, salinity and inundation, and seedlings put into the wrong hydrology die. Restoring the water flow often brings mangroves back naturally without planting anything. Ask about hydrology before you ask about seedling counts.
Does restoration actually work?
Yes, and relatively fast. Restored mangroves begin accumulating carbon again within years rather than decades. A global synthesis of over 370 restoration sites found that replanting where mangroves previously grew substantially outperforms planting on bare tidal flats, and that restoring feasible deforested areas could take up 671 to 689 million tonnes of CO2-equivalent over 40 years.
Do mangroves really protect against storms and tsunamis?
The evidence indicates they meaningfully reduce wave energy and storm surge, and coastlines that retained mangroves fared better in the 2004 Indian Ocean tsunami. They are not an absolute shield and the evidence from any single catastrophe is messy. But as coastal defence that maintains itself, gets stronger over time, and produces fish, they have no engineered equivalent.
Sources
- Project Drawdown - Protect Coastal Wetlands (Drawdown Explorer) Framework and classification. Cited, not reproduced.
- Donato et al. (2011), Nature Geoscience - Mangroves among the most carbon-rich forests in the tropics
- Su et al. (2023), Nature Communications - Mangrove reforestation provides greater blue carbon benefit than afforestation
- The Blue Carbon Initiative
- Sasmito et al. (2025), Nature Communications - Half of land use carbon emissions in Southeast Asia can be mitigated through peat swamp forest and mangrove conservation
- NOAA - Blue Carbon
The solution taxonomy follows the framework popularised by Project Drawdown. The analysis above is our own; for their carbon modeling and rankings, visit them directly.