Blue Finance & Investment

Voluntary Carbon Markets vs Compliance Carbon Markets in Ocean Context

Voluntary Carbon Markets vs Compliance Carbon Markets in Ocean Context

Two systems price carbon, and they are routinely discussed as if they were two versions of the same thing. They are not. One is a market that exists because governments made emitting expensive by law. The other is a market that exists because organisations chose to pay for something no law required. That difference in origin runs through everything: who participates, what a credit is worth, what counts as rigorous, and which projects can get funded at all. In an ocean context the distinction becomes sharper still, and in a direction most summaries miss. The ocean appears in these two markets in almost opposite roles. In voluntary markets it appears mainly as supply, as mangroves and seagrass and tidal marsh generating credits for sale. In compliance markets it appears mainly as demand, as a shipping industry now legally obliged to buy allowances for the carbon it emits. Money flows into the ocean through one system and out of it through the other, and the two flows are not connected. Here is how the comparison works, row by row.   Meaning   A voluntary carbon market is one in which organisations buy carbon credits without being legally required to, in order to support climate action or make a claim about their own emissions. A compliance carbon market is one in which covered entities are legally required to hold and surrender allowances or eligible credits against their emissions. The word voluntary does a lot of work and can mislead. Participation is voluntary, but the buying is increasingly driven by disclosure regimes, investor pressure, supply chain requirements and net zero commitments that are themselves becoming semi-enforceable. Compliance markets, meanwhile, are not uniformly strict. They vary enormously in coverage, price and whether they permit offsets at all. The clean binary of choice versus obligation describes the legal architecture accurately and the commercial reality only roughly.   Ocean Relevance   Voluntary markets fund blue carbon projects directly. Mangrove restoration, seagrass conservation and coastal wetland protection all generate credits sold almost exclusively into the voluntary market, because that is where buyers who want a conservation story will pay for one. The compliance side is where the infographic's framing needs qualifying, because compliance revenue rarely reaches ocean projects and in the largest ocean-relevant system it cannot reach them at all. The European Union Emissions Trading System, which now covers shipping, is a cap and trade scheme built on allowances rather than offsets, and it does not accept project credits. A mangrove project cannot sell into the EU ETS under any circumstances. The compliance markets that do admit blue carbon are narrower and national. Australia is the clearest case: its Clean Energy Regulator established a Tidal Restoration of Blue Carbon Ecosystems method under the Australian Carbon Credit Unit scheme in 2022, crediting projects that reintroduce tidal flow to coastal wetlands by removing tidal restriction structures, over a 25-year crediting period, with abatement modelled through the Blue Carbon Accounting Model rather than physical soil sampling. Credits issued under that method are ACCUs, and ACCUs can be surrendered by facilities regulated under Australia's Safeguard Mechanism. That is a genuine bridge from coastal restoration into compliance demand, and it remains close to unique.   Main Driver   Voluntary demand is driven by corporate climate commitments, sustainability strategy, brand positioning and the perceived need to address emissions a company cannot yet eliminate. Compliance demand is driven by regulation and the price of non-compliance. The consequence is that the two markets respond to entirely different signals. Voluntary demand is sentiment-sensitive and reputation-sensitive, which is why it contracted sharply after the integrity controversies of 2023 and why recovery has been uneven. A wave of critical journalism can collapse demand for a credit type in months. Compliance demand does not behave that way. A regulated shipping company facing a surrender obligation in April buys allowances regardless of what was published about carbon markets that year, because the alternative is a penalty. Compliance markets are therefore far more stable, far deeper in liquidity, and far less interested in the qualitative merits of any particular project.   Participation   Voluntary participation is open. Any organisation can buy, any developer can seek certification under a private standard, and no jurisdiction has to approve the transaction. Compliance participation is mandatory for covered entities and closed to everyone else. Scope definitions therefore carry enormous weight in compliance systems. The EU ETS maritime extension applies to ships above 5,000 gross tonnage calling at EU ports, covering all emissions on voyages within the European Economic Area and half of emissions on voyages into or out of it. That threshold and that geographic split determine which operators face a cost and which do not, and both are the product of negotiation rather than atmospheric physics. Voluntary markets have no equivalent gatekeeping, which is simultaneously their great advantage in flexibility and their great weakness in rigour.   Credits and Units   Voluntary markets trade project-generated credits verified under private standards such as Verra, Gold Standard and Plan Vivo. Compliance markets trade government-issued allowances, and in some systems a limited quantity of approved compliance credits alongside them. The distinction between an allowance and a credit is the most important technical point in the whole comparison and the most commonly blurred. An allowance is a permit to emit, created by a regulator, and its total quantity is capped. A credit is a claim that an emission was avoided or a tonne of carbon removed somewhere else, relative to a counterfactual of what would otherwise have happened. Allowances require no counterfactual, so they raise no additionality question. Credits depend entirely on one, which is why almost every integrity dispute in carbon markets concerns credits rather than allowances. Blue carbon sits squarely in the credit category, and inherits every difficulty that comes with it.   Ocean Examples   The voluntary example is straightforward: a company buys credits from a mangrove restoration project and claims the associated removals against its own footprint. The compliance example in an ocean context is shipping, and it has moved fast. From 1 January 2026 the EU ETS maritime phase-in reached 100 percent, after 40 percent in 2024 and 70 percent in 2025, meaning shipping companies now surrender allowances for the full extent of their covered emissions. The same date expanded the system's scope beyond carbon dioxide to include methane and nitrous oxide, with the overall allowance cap raised to reflect the addition and the extra allowances auctioned or directed to the Innovation Fund. The methane inclusion matters commercially, because it narrows the advantage of liquefied natural gas as a transitional marine fuel by capturing the methane slip that engines release unburned. The global counterpart remains unfinished. The IMO Net-Zero Framework, designed to combine a global marine fuel greenhouse gas intensity standard with a pricing mechanism, as binding amendments to MARPOL Annex VI, failed to secure adoption at an extraordinary session in October 2025. Negotiations were adjourned for a year, with talks scheduled to resume in late 2026. Its delay does not suspend anything in Europe. EU ETS and FuelEU Maritime obligations continued unaffected, which is why shipping is currently governed by a regional compliance price rather than a global one.   Key Challenge in Ocean Projects   For voluntary blue carbon, the challenges are additionality, permanence, leakage and measurement. For compliance participation, the challenge is meeting regulatory eligibility, accounting and verification standards that were largely not written with coastal ecosystems in mind. The blue carbon difficulties are worth stating concretely rather than abstractly, because the numbers are sobering. Calyx Global found that as of October 2025 only 10 of 81 blue carbon projects worldwide were actively issuing credits, and that a single project, Delta Blue Carbon-1 in Pakistan's Indus Delta, accounted for roughly 73 percent of all blue carbon credits ever issued. The active projects cover around two million hectares and target roughly 20.4 million tonnes of CO2 in removals annually. A market with one dominant supplier and a long tail of projects that have never issued anything is not yet a market in any meaningful sense. The reasons are structural. Measuring carbon stored metres deep in waterlogged, anoxic coastal soil is technically difficult and expensive, and the monitoring cost often consumes a large share of what the credits are worth. Permanence is genuinely fragile, because coastal ecosystems sit directly in the path of the sea level rise, storm intensification and marine heatwaves the credits are meant to help mitigate. Additionality is contested wherever a mangrove was already under legal protection, and tenure disputes are common because coastal communities usually hold customary rather than documented rights to the land being credited. Compliance eligibility, by contrast, fails for a simpler reason: most compliance systems either exclude offsets entirely or have never written a methodology that a coastal wetland could satisfy.   Primary Goal   The voluntary market exists to finance climate action beyond an organisation's own operations. The compliance market exists to reduce regulated emissions in line with law. These goals are less compatible than they sound. Compliance systems are designed to lower emissions inside a defined boundary, and every tonne that leaves that boundary through an offset weakens the cap. This is precisely why the EU excluded international credits from its ETS. Voluntary markets exist to move money outside the boundary, to places where emissions are unregulated and mitigation is cheap. One system is built to contain, the other to redistribute. Blue carbon is a redistribution instrument, and attempts to fit it into containment systems tend to fail for reasons of design rather than quality.   The Asymmetry at the Heart of the Comparison   Setting the two columns side by side in an ocean context reveals something the row labels do not. The ocean's largest and fastest-growing involvement in carbon pricing is not as a source of credits. It is as a regulated emitter. Shipping moves roughly 80 percent of world trade by volume and produces close to 3 percent of global greenhouse gas emissions, and it is now paying a compliance carbon price in Europe on the full scope of its covered emissions. That is, by orders of magnitude, the largest sum of money the ocean economy has ever moved through a carbon market. Blue carbon, by contrast, has produced a credit supply dominated by a single Pakistani project. The money also flows in opposite directions, and almost none of it circulates. EU ETS maritime revenue accrues to member states and the Innovation Fund. It is not earmarked for mangroves, seagrass or coastal communities. A shipping company paying a European carbon bill is not funding ocean restoration, and a mangrove project in Indonesia is not receiving shipping money. The two ocean carbon stories, one about emission and one about sequestration, are financially disconnected despite occupying the same conceptual frame. The proposed IMO pricing mechanism is the most credible route to changing that, because a global levy on marine fuel emissions would generate a revenue pool and a live argument about where it should go, including claims from climate-vulnerable coastal states. That argument is one of the reasons adoption stalled. Revenue distribution, not emissions targets, is where the hardest disagreement sits.   What the Comparison Really Shows   The practical conclusion is that anyone planning an ocean carbon project should design for the voluntary market and treat compliance eligibility as a distant option, while anyone operating ships should plan for compliance costs that are now real, rising and no longer regional in ambition. Blue carbon's defensible case has also shifted, and honestly so. Coastal restoration delivers storm protection, fisheries nursery habitat, water quality improvement and local livelihoods, and those benefits are more reliable and easier to verify than the carbon accounting attached to them. The more sophisticated end of the market has begun pricing blue carbon on that bundle rather than on tonnes alone, which is a better fit for what these ecosystems actually do. Selling a mangrove primarily as a carbon asset means competing on a metric where it is expensive, difficult to measure and vulnerable to the very climate it is meant to address. Selling it as coastal infrastructure that also stores carbon is both more accurate and, on current evidence, more bankable.   Note: This article reflects the state of both markets as of September 2026, drawing on sources including the European Commission's EU ETS maritime provisions, International Maritime Organization proceedings on the Net-Zero Framework, Calyx Global research on blue carbon issuance, Verra and Plan Vivo methodology documentation, and the Australian Clean Energy Regulator's ACCU scheme methods. Carbon market conditions change quickly and figures should be checked against primary sources before use in transactions.

Policy & Governance

Bird-Johnson Propeller Facility Breaks Ground in Pascagoula With AUKUS Funding

Bird-Johnson Propeller Facility Breaks Ground in Pascagoula With AUKUS Funding

US Navy leaders have joined industry and international partners to break ground on a new facility in Pascagoula, Mississippi, that will manufacture critical components for submarines. The 60 million dollar project will deliver a modern facility capable of producing propulsors, propellers and other components for several shipbuilding programmes. The US Navy is contributing funding via a partnership, with a further sum sourced from Australia’s contribution to the US submarine industrial base under AUKUS.   Details of the Groundbreaking   Leaders broke ground on a facility. It is in Mississippi. It will make components. These serve submarines. It supports several programmes. The project is substantial. It is valued at 60 million dollars. It delivers a modern facility. It spans 38,000 square feet. It expands capacity.   The Funding Structure   The project has mixed funding. The US Navy contributes. A partnership channels it. Australia provides part. This comes under AUKUS. The funding reflects a commitment. Australia is contributing broadly. It supports the industrial base. It increases capacity. It enables submarine sales.   The Australian Contribution   Australia’s contribution is significant. It totals billions. The first portion arrived last year. It is invested purposefully. It aligns the industrial base. The contribution serves AUKUS goals. It uplifts the industrial base. It increases maintenance. It boosts production. It supports submarine delivery.   Read More: https://oceaneconomist.com/articles/general-dynamics-slcm-n-contract   The Strategic Purpose   The investment strengthens foundations. It underpins the submarine force. It augments congressional funds. It enables programmes. It delivers capability. The investment is coordinated. Teams worked together. They developed a spend plan. It targets high-impact areas. It maximises benefit.   The Stakeholder Perspectives   US officials welcomed the project. They cited industrial strength. It supports the fleet. It readies submarines. It delivers capability. Australian officials echoed this. They welcomed the investment. It supports industrial capacity. It demonstrates momentum. It reflects shared commitment.   Significance of the Facility   The facility produces critical components. These serve submarines. They cover several programmes. They support new construction. They aid in-service vessels. The facility advances AUKUS. It activates the industrial base. It readies more submarines. It supports delivery. It reflects trilateral cooperation.

Shipping & Ports

Sinarmas Adds First Two ASD Tugboats to Its Indonesian Fleet

Sinarmas Adds First Two ASD Tugboats to Its Indonesian Fleet

Sinarmas LDA Maritime has taken delivery of its first Chinese-built azimuth stern drive tugboats as it expands its fleet supporting ships in ports. The Indonesian owner received two vessels from Jiangsu Zhenjiang Shipyard after ordering them in 2025. When its new tugs enter service, they will form one of the first fleets of azimuth stern drive tugboats to operate in Indonesia.   Details of the Delivery   The owner took delivery of two tugs. These are azimuth stern drive vessels. A Chinese yard built them. They were ordered in 2025. They expand the fleet. The tugs serve port operations. They support ships. They assist in harbours. They are the owner’s first of this type. They mark a milestone.   The Vessel Specifications   The tugs have strong specifications. They measure 32.5 metres. They offer good installed power. Twin engines drive them. These combust diesel and biofuels. The tugs are capable. They deliver 51 tonnes ahead. They offer 45 tonnes astern. They reach 12 knots. Two thrusters feature.   The Fleet Expansion   The owner is expanding further. Seven more tugs are on order. The same yard builds them. At least three are due in 2027. These continue the series. The expansion is significant. It brings a new fleet type. Most Indonesian vessels differ. They use conventional propulsion. These are among the first ASD tugs.   Read More: https://oceaneconomist.com/articles/kongsberg-port-hedland-vts   The Shipyard Activity   The yard has been busy. It delivered another tug. This was twin-screw. It launched two ASD tugs. These serve Chinese owners. The yard has more work. It laid keels for anchor handlers. It cut steel on a tug. These serve various owners. Activity is strong.   The Wider Chinese Orders   Another yard won a contract. It covers two escort tugs. An overseas owner ordered them. They use a specific design. They offer strong bollard pull. The yard has further work. It builds anchor handlers. Support vessels feature. These serve several owners. Many are overseas.   Significance of the Delivery   The delivery advances the owner’s growth. It adds modern tugs. It introduces a new type. It expands capability. It supports ports. The delivery reflects a shift. Indonesia is modernising. ASD tugs are emerging. The owner leads this. It sets a precedent.

Fisheries & Aquaculture

How Fish Aggregating Devices Reshape Tuna Fishing

How Fish Aggregating Devices Reshape Tuna Fishing

There is an old observation among fishers that tuna gather beneath anything floating. A drifting log, a mat of seaweed, a piece of wreckage: whatever the object, small fish shelter under it, larger fish come to feed on them, and tuna arrive in turn. Nobody fully understands why the behaviour exists, but people have exploited it for centuries. What has changed in the past three decades is scale and technology. Fishing fleets no longer wait to find a floating log. They manufacture logs by the tens of thousands, fit them with satellite buoys and sonar, and scatter them across the open ocean, then return when the instruments say enough fish have gathered. Fish Aggregating Devices have transformed tuna fishing from a search problem into a monitoring problem, and in doing so they have become one of the most consequential and most contested technologies in commercial fishing. Here is how they work and what they have changed, step by step.   1. FADs Create Artificial Gathering Points   A Fish Aggregating Device is a floating object built to exploit the natural tendency of tuna and other pelagic species to associate with things drifting at the surface. In its simplest form it is a raft of bamboo, cork, or plastic floats with a submerged appendage hanging beneath it, historically old netting and increasingly rope or biodegradable material. Two types exist and the distinction matters. Anchored FADs are moored to the seabed, usually in coastal waters, and are widely used by small-scale and artisanal fishers, particularly in Pacific island states where they can bring fish within reach of small boats and reduce fuel costs. Drifting FADs, which are the subject of most controversy, float freely on the open ocean and are used almost entirely by industrial purse-seine fleets. It typically takes a month or two for a new drifting FAD to accumulate a substantial aggregation of skipjack, so the device is planted and left to work.   2. Fishers Can Find Tuna More Efficiency   The economic logic is straightforward. Searching an ocean for free-swimming tuna schools is slow, fuel-hungry, and uncertain. Deploying hundreds of FADs and monitoring them remotely converts that search into a scheduling exercise, where a vessel sails to the device the data says is most productive. The productivity gains are large and well documented. Research indicates FAD fishing is roughly 1.35 to 3 times more productive than free-school fishing for yellowfin and bigeye, and 2 to 7 times more productive for skipjack. The difference in reliability is starker still: for the European purse-seine fleet over one period, around 96 percent of FAD sets in the Atlantic and 94 percent in the Indian Ocean caught at least a tonne of tuna, against 80 percent and just 58 percent respectively for sets on free-swimming schools. A null set, where the net is deployed and comes up empty, is enormously expensive, and FADs nearly eliminate them. This efficiency is also why FAD-caught skipjack is cheap enough to fill the world's canned tuna market.   3. Satellite Buoys Add Technology   Modern drifting FADs carry solar-powered satellite buoys with GPS, and most now include an echosounder. The buoy reports the device's position continuously, and the sonar estimates how much fish biomass is beneath it, in some systems distinguishing between species and depths. This is the change that transformed the technology from a passive attractor into an active remote sensing network. A fleet operating a thousand instrumented FADs effectively runs a distributed array of ocean sensors reporting back by satellite, allowing a vessel to rank every device by expected catch and steam only to the best. It also created an unusual property rights situation, since the buoys are privately owned and their data proprietary, which means the most detailed information about tuna aggregation across large parts of the ocean sits with fishing companies rather than with the bodies that manage the stocks.   4. Catches Can Become Larger   The instrumentation measurably increases catch. Research in the Indian Ocean found that echosounder-equipped FADs raised the average catch per set by roughly two to two and a half tonnes, about ten percent, compared with FADs carrying only position buoys. That figure is worth dwelling on, because it illustrates something important about fisheries management. Catch limits are typically set in tonnes, but fishing capacity is not fixed, and a technological improvement of this kind increases the effective fishing power of a fleet without adding a single vessel. Managers refer to this as technological creep, the steady erosion of the relationship between nominal fishing effort and actual fishing mortality. If a quota assumes a certain catch rate per vessel-day and the technology quietly makes each vessel-day more productive, the stock experiences more pressure than the paperwork suggests.   5. Juvenile Tuna Can Be a Concern   FAD aggregations are not made up only of the target species. Skipjack dominates, accounting for around seventy percent of the catch by weight from drifting FAD sets, but juvenile bigeye and yellowfin tuna associate with floating objects too and are caught alongside it. This is the most consequential biological concern, because bigeye and yellowfin are far more valuable and far more vulnerable than skipjack. Skipjack is fast-growing and highly productive, and can sustain heavy fishing. Bigeye grows slowly, matures late, and cannot. Catching immature bigeye before they have spawned removes them from the population entirely, altering the age structure of the stock and reducing its future reproductive output. The WCPFC assessed that juvenile bigeye taken on FADs in the Western Pacific rose from essentially nothing in the 1960s to close to 80,000 tonnes a year by 2010. It is a textbook growth overfishing problem: a fishery targeting an abundant species inflicts its heaviest damage on a different, scarcer one.   6. Bycatch Risks Increase   Sharks, rays, turtles, and other non-target species also aggregate around FADs and are caught when the purse seine closes. Studies consistently find higher bycatch rates on FAD sets than on free-school sets, and the effect on pelagic sharks in particular has been linked to rising extinction risk for several species. An honest comparison requires a caveat that is often omitted. FAD sets have more bycatch per set than free-school sets, but they also catch more tuna per set, and in the Eastern Pacific the main alternative historically involved setting nets on dolphins, which carried its own severe consequences. The question is therefore not simply whether FADs cause bycatch, which they plainly do, but how the total ecological cost of a given tonnage of tuna compares across methods. That framing matters because it explains why the policy debate has generally landed on regulating FADs rather than banning them outright.   7. Lost FADs Can Keep Fishing   FADs are frequently lost, abandoned, or simply allowed to drift away once they leave a fleet's area of interest, and the scale of this is only now becoming clear. A 2025 study in Science Advances estimated that 1.41 million drifting FAD buoys were released between 2007 and 2021, drifting across at least 134 million square kilometres, equivalent to 37 percent of the ocean surface, and that lost devices have stranded in 104 maritime jurisdictions. The consequences are twofold. Devices built with netting continue to entangle sharks, turtles, and other animals long after anyone is watching, which is ghost fishing in miniature and repeated on an enormous scale. Beached devices damage coral reefs and litter coastlines, and the burden falls disproportionately on small island states that did not deploy them. More than 1,300 beaching events were recorded in the Western and Central Pacific over 2016 and 2017 alone, concentrated in Papua New Guinea, the Solomon Islands, and Tuvalu, driven simply by where prevailing currents carry the devices. There is also a subtler worry that deploying tens of thousands of artificial floating objects may alter tuna behaviour itself, potentially acting as an ecological trap that changes feeding and migration patterns in ways not yet understood.   8. RFMOs Are Tightening Management   The four tropical tuna Regional Fisheries Management Organisations, covering the Pacific, Eastern Pacific, Indian, and Atlantic oceans, have progressively brought FADs under regulation. Measures now include limits on how many active FADs a vessel may deploy, seasonal closures on FAD fishing, mandatory reporting of deployments and buoy data, requirements for non-entangling designs that replace netting with rope, encouragement or requirement of biodegradable materials, and emerging recovery and retrieval obligations. Progress has been real but uneven, and the same institutional constraints described in any account of RFMO decision-making apply here. Consensus requirements slow the adoption of stricter limits, member states disagree over whether FAD caps disadvantage particular fleets, and reporting obligations depend on data that fishing companies own. Independent assessments of thirty years of FAD regulation have concluded that although meaningful progress has been made on data quality, entanglement, and pollution, concerns persist over unregulated deployments, bycatch levels, and industry accountability. The transition to biodegradable designs, in particular, has proved slower in practice than in commitment.   The Real Question   It is tempting to treat FADs as straightforwardly harmful, and much campaigning has taken that line, but the trade-off is genuinely difficult. Banning drifting FADs would not eliminate tuna fishing; it would push fleets back toward free-school sets, which means more searching, more fuel burned, more sets made per tonne landed, and in some regions a return to methods with their own serious problems. It would also raise the price of canned tuna, which is among the cheapest animal protein available globally. Against that, FADs demonstrably increase juvenile bigeye mortality, elevate shark and turtle bycatch, and scatter plastic across a third of the ocean surface. The productive framing, and the one the management bodies have largely adopted, is that FADs are a tool whose harms are mostly design and volume problems rather than intrinsic ones. Non-entangling construction removes most of the entanglement risk. Biodegradable materials remove most of the pollution risk. Caps on deployment numbers address the volume. Recovery obligations address abandonment. Better data addresses everything else. None of that reduces juvenile bigeye catch, which remains the hardest problem and probably requires seasonal closures or direct limits on FAD sets rather than better FADs. What is clear is that a technology which now underpins a majority of the world's tuna supply cannot simply be legislated away, and that the interesting work lies in making it less damaging rather than in arguing about whether it should exist.   Did You Know?   More than sixty percent of the world's tuna is caught by purse-seine vessels, and around 37 percent of tropical tuna purse-seine sets are made on floating objects, which is why the way these fleets use FADs is such a central issue in global tuna management. The numbers behind that are striking: somewhere between 81,000 and 121,000 FADs are deployed worldwide each year, over 100,000 are drifting or anchored in the ocean at any given moment, and roughly 40 percent of the world's skipjack catch, the fish in most cans of tuna, comes from fishing on them. A technology that began as fishers noticing that tuna like to gather under logs has become an instrumented, satellite-tracked infrastructure spanning more than a third of the ocean surface.   Note: This article reflects the state of FAD use and regulation as of mid-2026, drawing on sources including studies published in Science Advances, Fish and Fisheries, and the ICES Journal of Marine Science, together with the International Seafood Sustainability Foundation, the Marine Stewardship Council, and the tropical tuna RFMOs. Deployment estimates vary considerably between sources and ocean basins.

Ocean Pollution & Waste

How Chemical Pollution Reaches the Deep Sea

How Chemical Pollution Reaches the Deep Sea

For most of the twentieth century, the deep ocean was assumed to be beyond human reach. It was too far down, too dark, too vast, too remote from factories and farms to be touched by anything people did on land. That assumption collapsed in 2017, when researchers hauled up small scavenging crustaceans from nearly eleven kilometres beneath the Pacific and found their tissues loaded with industrial chemicals banned decades earlier. In the Mariana Trench, the deepest place on the planet, concentrations of some pollutants were higher than in the estuaries of the most polluted rivers in China. There is no longer any part of the ocean that human chemistry has not reached. The more interesting question is how it got there, because the journey from a factory outfall or a farm field to the bottom of a trench turns out to involve a remarkable and rather elegant chain of physical and biological processes. Here is how that chain works, step by step.   1. Pollutants Are Released   The journey begins on land, in the ordinary business of an industrial civilisation. Chemicals enter rivers, estuaries, and coastal waters from factories and industrial discharge, from pesticides and fertilisers washing off farmland, from mining operations, from treated and untreated wastewater, and from the diffuse runoff of streets and rooftops in every city. The cast of characters matters, because different pollutants behave very differently once they reach the water. Persistent organic pollutants, or POPs, are the most consequential for the deep sea. This family includes polychlorinated biphenyls, or PCBs, once used in electrical equipment and in ship antifouling coatings, and polybrominated diphenyl ethers, or PBDEs, used as flame retardants in furniture and electronics. These compounds share three dangerous properties: they resist breaking down, they are fat-soluble so they accumulate in animal tissue, and they travel. Alongside them come heavy metals such as mercury, pharmaceutical residues, and the microplastics that act as rafts for other chemicals to ride on. A sobering detail is that PCBs were banned in most countries in the late 1970s, yet they remain among the dominant contaminants found at the bottom of the ocean today. Once released, these substances effectively never leave the system.   2. Rivers Carry Them to the Ocean   Rivers are the great conveyor belts of pollution, gathering the runoff of entire continents and delivering it to the coast. Pesticides, heavy metals, pharmaceuticals, and industrial chemicals all move downstream, some dissolved in the water and many more bound to suspended sediment. This is why coastal seas near industrialised and densely farmed regions carry the heaviest contaminant loads, and why the deep-sea pollution story is not evenly distributed across the globe. It also introduces a theme that runs through the entire process: most of these pollutants do not simply float freely in seawater. They prefer to stick to particles, and it is that stickiness, more than anything else, that determines where they ultimately end up.   3. Ocean Currents Spread Pollution   Once contaminants reach the sea, currents and tides take over, carrying dissolved chemicals and contaminated particles far from where they were released. Surface circulation can move pollution across entire ocean basins, which is how contaminants originating on one continent turn up in waters thousands of kilometres from any industry. There is a striking piece of evidence for this. Researchers examining the Mariana Trench have suggested that its unusually high pollutant burden may draw on the North Pacific Subtropical Gyre, better known as the Great Pacific Garbage Patch, which sits in the same broad circulation system and concentrates floating debris and its associated chemicals before that material eventually sinks. Currents do not only disperse pollution; in places they concentrate it, gathering contaminants into particular regions of the ocean that then feed the depths below them.   4. Pollutants Attach to Marine Particles   Here is the key chemical fact that makes the whole journey possible. Most persistent organic pollutants are hydrophobic, meaning they do not dissolve readily in water and instead bind tightly to anything organic or fatty they encounter. In the ocean that means they attach to tiny fragments of organic matter, to sediment grains, to plankton, and to microplastics suspended in the water column. This binding transforms the problem entirely. A dissolved chemical would remain diffuse, drifting in the immensity of the ocean and diluting toward insignificance. A chemical stuck to a particle, by contrast, acquires the ability to sink, and it becomes part of the ocean's own vertical transport system. In effect, pollutants hitch a ride on the biological machinery that has been carrying carbon from the surface to the seafloor for hundreds of millions of years. Microplastics have added a new and efficient vehicle to that system, since they both carry pollutants adsorbed onto their surfaces and are themselves ingested throughout the food web.   5. Marine Snow Sinks   Marine snow is one of the most beautiful phenomena in the ocean and, it turns out, one of the most consequential for pollution. It is the continuous downward drift of organic debris, dead plankton, faecal pellets, mucus, and fragments of decaying material, that falls perpetually through the water column like a slow blizzard. It is the primary food supply for the deep sea, which has no sunlight of its own, and it is the engine of the biological carbon pump. Once contaminated particles are incorporated into marine snow, that same shower becomes a delivery system for toxins. Sinking carcasses of fish and marine mammals, which carry accumulated pollutants in their fat, add to the flux, and other mechanisms accelerate it further: turbidity currents, the underwater avalanches that sweep down submarine canyons, can transport and bury pollutants and microplastics in deep-sea sediments, and research on the Japan Trench has shown that earthquake-driven sediment flows deliver contaminants directly into hadal basins. The result is that pollutants reach the deep faster than anyone once expected. A study of mercury in trench sediments concluded that the turnover time for anthropogenic pollutants moving from the surface to the deep sea is likely far shorter than the previous estimate of more than a thousand years.   6. The Deep Sea Becomes a Sink   Everything that sinks eventually stops, and where it stops is the seafloor, above all in the deep trenches. As marine snow and heavier flows settle, pollutants accumulate in deep-sea sediments and remain there for decades or centuries. Trenches are especially effective traps because they are the lowest points on Earth's surface, funnel-shaped and enclosed, collecting material from the slopes around them. The findings are stark. Microplastics in Mariana Trench sediments have been measured at concentrations far higher than in most other deep-sea sediments. Hadal trenches, despite occupying less than half a percent of the ocean's area, have been identified as a disproportionately important and previously overlooked sink for mercury. Researchers have described these trenches, with some justification, as the ocean's ultimate trashcan. The deep-sea researcher Alan Jamieson, who led the landmark trench study, put the underlying logic plainly: once material sinks deep enough, there is no mechanism to bring it back to the surface again. The deep sea is not a place pollution passes through. It is where pollution stops.   7. Deep-Sea Wildlife Is Exposed   Deep-sea animals live directly in and on this contaminated sediment, and they eat the marine snow as it arrives. Bottom-dwelling organisms absorb pollutants from the sediment or from their food, and once inside the food web the contaminants biomagnify, concentrating at higher levels in each successive predator. The specifics are remarkable and unsettling. In the 2017 study led by Jamieson's team, amphipods collected from between seven and ten kilometres deep in the Mariana and Kermadec trenches contained PCBs and PBDEs in every sample, across all species and all depths. In the most contaminated Mariana specimens, PCB levels were reported as up to fifty times higher than in crabs from paddy fields fed by the Liaohe River, one of the most polluted waterways in China. Separate work has found man-made fibres and microplastics ingested by amphipods in six of the deepest ecosystems on Earth, including the Challenger Deep. There is a particular cruelty in the biology here: these scavengers store energy as fat to survive long famines between food falls, and fat is exactly where fat-soluble pollutants accumulate. The very adaptation that allows them to endure the deep sea makes them efficient collectors of its toxins.   8. Pollution Persists   Finally, the contamination stays. Deep-sea environments are cold, dark, and slow, with little sunlight or microbial activity to break down complex chemicals, and the organisms living there are typically long-lived and slow-growing. Recovery, where it happens at all, happens on timescales of decades to centuries. Two conclusions follow, and they are worth stating clearly. The first is that this is a genuinely irreversible form of pollution in any human timeframe. There is no plausible technology for cleaning contaminants out of sediments eleven kilometres beneath the sea, which means prevention at the source is not merely the best option but effectively the only one. The second is that the deep sea has been quietly recording our chemical history all along. PCBs banned nearly half a century ago are still being found in the bodies of animals in the deepest place on the planet, which is both an indictment of how long these substances endure and a vindication of why they were banned. The Mariana Trench, the most remote habitat on Earth, has turned out to be one of the most polluted, and that fact alone dissolved the last comfortable illusion that any part of the ocean lies beyond our reach.   Did You Know?   Studies have detected persistent organic pollutants, mercury, and microplastics in some of the deepest parts of the ocean, including the Mariana Trench. The scale of the contamination surprised even the researchers who found it: crustaceans from nearly eleven kilometres down were reported to carry PCB concentrations up to fifty times those measured in crabs from one of China's most polluted rivers, and around ten times the industrial pollution burden of an average earthworm in farmland soil. These are animals that have never encountered sunlight, let alone a factory. Their contamination is the clearest possible demonstration that the ocean has no away, only down.   Note: This article reflects the state of deep-sea contamination research as of mid-2026, drawing on sources including studies published in Nature Ecology and Evolution, PNAS, Royal Society Open Science, Water Research, and Communications Earth and Environment. Contaminant concentrations vary considerably between trenches, species, and sampling methods.

Offshore Energy

IMCA Launches IMCA 2030 Strategy to Help Offshore Construction Industry Navigate Changing World

IMCA Launches IMCA 2030 Strategy to Help Offshore Construction Industry Navigate Changing World

The International Marine Contractors Association has launched IMCA 2030, a four-year strategy to keep the association relevant and valuable as the offshore construction industry navigates significant change. Launched at the IMCA Global Summit in Antwerp, the strategy responds to major industry trends including AI, automation, the energy transition and evolving regulation. The association represents more than 850 members across 66 countries.   Details of the Launch   The association launched a strategy. It is called IMCA 2030. It spans four years. It was launched at a summit. This was in Antwerp. The strategy responds to change. It addresses major trends. These include AI. Automation features. The energy transition is included.   The Strategic Pillars   The strategy has three pillars. One covers technical excellence. Another covers the workforce. A third covers sustainability—these guide activity. The pillars shape investment. They direct services. They guide activities. They span coming years. They reflect priorities.   The Technical Focus   The association maintains authority. It leads in diving. Dynamic positioning features. Safety is included. ROV operations are covered. The association will strengthen its marine work. Autonomy features. Remote operations are included. Decarbonization is covered. Offshore wind is addressed.   Read More: https://oceaneconomist.com/articles/chouest-horizon-arctic-partnership   The People Focus   The strategy supports people. It covers skills and careers and features a campaign. Early-career support is included. A network helps. The strategy builds a system. It supports competence. New initiatives are featured. Digital logbooks are included. A skills platform is planned.   The Advocacy Focus   The association will enhance advocacy. It builds on existing work. It engages regulators. The EU features. Governments are included. The advocacy targets practical regulation. It improves safety. It aids efficiency. It supports decarbonization. It avoids unnecessary cost.   Significance of the Strategy   Leadership cited profound change. New technologies reshape the sector. Markets are shifting. Regulation is growing. Competition for talent rises. The strategy builds on a legacy. It spans 50 years. It ensures relevance. It delivers member value. It keeps the industry fit for the future.

Ocean Technology

WHOI Research Vessel Neil Armstrong to Make First-Ever Voyage Through the Great Lakes

WHOI Research Vessel Neil Armstrong to Make First-Ever Voyage Through the Great Lakes

The research vessel Neil Armstrong, operated by the Woods Hole Oceanographic Institution, is embarking on a first-of-its-kind journey through the Great Lakes to help scientists investigate elusive subatomic particles. The 238-foot vessel departed its home port bound for Duluth, Minnesota, where it will support a neutrino research project in Lake Superior. The journey spans more than 2,500 nautical miles through rivers, locks, and inland waterways.   Details of the Voyage   A research vessel began a voyage. It is the Neil Armstrong. A US institution operates it. It heads for the Great Lakes. It is a first. The voyage is substantial. It covers over 2,500 nautical miles. It takes 11 days. It ends in Minnesota. It reaches Lake Superior.   The Research Project   The voyage supports a project. It studies neutrinos. These are subatomic particles. They rarely interact. They are hard to detect. The project has several partners. A university leads it. An agency sponsors it. Other bodies cooperate. It investigates fundamental physics.   The Deployment Task   The vessel will deploy detectors. These are arrays. A specialist group designed them. They support sensors. These are central to the research. The task is demanding. Frames will be lowered. These are large and heavy. They need precise positioning. Cables will connect them.   Read More: https://oceaneconomist.com/articles/oceanalpha-environmental-usv-expo   The Engineering Challenge   The equipment is substantial. Each frame is tall. Each is heavy. They carry mounted equipment. They must be positioned carefully. The deployment is complex. Frames go to the lakebed. Cables follow—these are fiber-optic. The process repeats for each.   The Navigational Challenge   The journey is unusual. It moves from ocean to lake. It requires route planning. Coordination is essential. The team prepares carefully. The journey has unique challenges. Buoyancy differs in fresh water. Rivers are narrow—locks are a feature. Weather must be considered.   Significance of the Voyage   Leadership cited versatility. Ocean capabilities enable discovery. This is in a new setting. The vessel adapts. The crew is skilled. The voyage highlights the fleet’s role. Vessels are floating laboratories. They deploy instruments. They collect data. They sustain research.   Source: WHOI

Nature & Climate

The World's Largest Animal Migration Happens Every Night

The World's Largest Animal Migration Happens Every Night

During the Second World War, sonar operators kept finding the seabed in the wrong place. Their instruments returned a solid echo at two or three hundred metres in waters charted as kilometres deep, and the false bottom moved: rising toward the surface after sunset, sinking again before dawn. It took years to establish that the echo was not geology but biology, a layer of living animals so dense it reflected sound like rock. They named it the deep scattering layer, and in doing so accidentally discovered the largest animal migration on Earth. Every night, across every ocean, an immense quantity of marine life swims upward from the twilight zone to feed in surface waters, and every morning it descends again. The animals involved are mostly small, mostly unfamiliar, and almost entirely unseen. Collectively they may outweigh every other fish in the sea, they help regulate the composition of the atmosphere, and until very recently almost nobody was arguing about who owns them. That has now changed, which is why this hidden migration has become a policy question as well as a biological one.   An Entire Ecosystem Moves After Dark   The mesopelagic zone, the ocean between roughly 200 and 1,000 metres, makes up about a fifth of the ocean's volume. It is too deep for photosynthesis and too shallow to be fully dark, lit by a faint blue residue of surface light that fades to nothing at the bottom. This is the twilight zone, and it is where the migrants spend their days. The cast is enormous and mostly anonymous. Copepods and other zooplankton at the base. Krill and shrimp. Squid. And above all lanternfish, the family Myctophidae, which are probably the most abundant vertebrates on the planet and which most people have never heard of. A lanternfish is typically a few centimetres long, silvery, with rows of light-producing photophores along its body. The distances involved deserve a moment of attention. An animal five centimetres long that climbs four hundred metres and returns the same night has travelled roughly sixteen thousand times its own body length in a day. Scaled to a human, that is something close to a thousand kilometres. These animals do it every twenty-four hours, for their entire lives, without rest and without navigation aids beyond the fading of the light. How much biomass is moving is a genuinely open question, and the spread of estimates is the most honest indicator of how little is known. Figures cited in the current policy debate range from around 600 million tonnes of mesopelagic fish at the conservative end to as much as 10 billion tonnes at the upper end, with the higher figures implying that roughly 90 percent of all fish in the sea by weight live in this layer. That is a span of more than an order of magnitude for one of the largest animal populations on the planet. Part of the reason is that these fish actively avoid trawls, so net surveys systematically undercount them, and acoustic estimates depend on assumptions about swim bladders and body composition that are themselves uncertain.   Why They Wait Until Night   The explanation is a trade-off, and it is one of the cleanest illustrations of predation risk shaping behaviour anywhere in nature. Food is at the surface. Photosynthesis happens only where there is light, so the phytoplankton that feed the zooplankton, which feed everything else, are concentrated in the upper layers. An animal that stayed in the twilight zone permanently would be safe and hungry. Predators are also at the surface, and most of them hunt by sight. Tuna, billfish, seabirds and marine mammals rely heavily on vision, and a small silvery fish in sunlit water is extremely visible. An animal that fed at the surface during the day would be well fed and eaten. Vertical migration resolves the conflict by separating the two in time rather than space. The animals ascend when darkness neutralises visual predators, feed through the night, and retreat below the photic zone before dawn. Light is both the cue and the constraint: the migration tracks changing light intensity so precisely that it shifts with moon phase, with cloud cover, and even during solar eclipses. There is a real cost to it, in energy spent swimming and in metabolic rate, and the fact that so many unrelated lineages independently pay that cost is strong evidence of how severe the predation pressure must be.   This Migration Helps Move Carbon   The biological carbon pump is the process by which carbon fixed at the surface ends up in the deep ocean, where it is isolated from the atmosphere for centuries. Most descriptions of it focus on gravity: dead plankton, faecal pellets and aggregates sinking slowly through the water column. That passive flux is estimated to export somewhere in the range of four to nine petagrams of carbon a year globally. Vertical migration adds a second, active mechanism, and it works differently in a way that matters. A migrating animal feeds at the surface and then physically swims the carbon downward inside its own body. At depth it respires, defecates and sometimes dies, releasing that carbon several hundred metres below where it was consumed. The crucial point is that this bypasses the water column in between. A sinking particle is intercepted, eaten and remineralised repeatedly on its way down, which is why only a small fraction of surface production ever reaches depth. A migrating lanternfish carries its cargo through that gauntlet in a few hours and delivers it intact. This is sometimes called the migrant pump, and estimates of its contribution range from roughly 0.9 to 3.6 petagrams of carbon a year, against the four to nine petagrams moved by gravitational sinking. Studies attributing export specifically to mesopelagic fishes put their share of total organic carbon export at anywhere from above 10 percent to more than 40 percent, with strong regional variation: under 10 percent in the California Current, above 40 percent in the North Pacific Subtropical Gyre. A caution is warranted on one widely repeated claim. It is sometimes stated that without mesopelagic fish, atmospheric carbon dioxide would be 50 percent higher and global temperatures several degrees warmer. That figure rests on a single estimate and should be treated as illustrative rather than established. The defensible version of the claim is less dramatic and still significant: a substantial share of the ocean's ability to move carbon into long-term storage depends on animals swimming it there, and the ocean's carbon uptake is not simply a matter of physics and chemistry. Recent modelling work underlines how much remains unresolved. A 2025 study in Biogeosciences built a trait-based model of micronekton migration, covering fishes, crustaceans and cephalopods between roughly 10 and 80 millimetres, using environmental data from a long-term station in the northeast Atlantic. It found active carbon transport reaching almost 40 milligrams of carbon per square metre per year in temperate conditions, peaking in summer, with respiration rates and prey capture efficiency explaining most of the variability. The authors' conclusion is the one worth carrying forward: micronekton are an important but under-represented component of the biological pump, and their behaviour under a warming ocean is uncertain.   Why This Suddenly Became a Policy Question   For most of the twentieth century the twilight zone was interesting and commercially irrelevant. The fish are small, bony, oily and widely dispersed, and catching them costs more than they are worth as food. That calculation is shifting. Aquaculture needs fishmeal and fish oil, demand for both is rising, and the forage fisheries that currently supply them are fully exploited. A biomass measured in hundreds of millions or billions of tonnes, sitting outside anyone's quota system, is an obvious place to look. Norway and Iceland have run trial fisheries. The European Union has invested on the order of 17 million dollars in feasibility research. The United States moved early in the other direction, prohibiting directed commercial mesopelagic fishing off its West Coast in 2016 and its East Coast in 2017. Trial results have been inconsistent in a pattern that should be familiar to anyone who has watched a new fishery open: large initial hauls followed by rapid decline, which is the classic signature of fishing down aggregations rather than harvesting a stock. The blue whiting fishery's boom and bust is cited as the cautionary precedent. Modelling also suggests that depleting mesopelagic fish would propagate upward, reducing populations of tuna, sharks, marine mammals and deep-sea species that depend on them, which means a twilight zone fishery would compete directly with existing surface fisheries for the same production. The governance position is close to a blank page. The high seas account for 61 percent of the ocean, no regulations specifically protect twilight zone fish there, and mesopelagic species were largely absent from the negotiations that produced the high seas biodiversity treaty. There is no stock assessment, no quota framework, no bycatch reporting and, for most of the zone, no competent management authority.   What Happened at the IUCN Congress   On 15 October 2025, delegates at the IUCN World Conservation Congress in Abu Dhabi adopted a motion on protecting the mesopelagic zone, by 713 votes to 46. The motion is non-binding, and it is deliberately narrower than it might have been. It calls for activities that could harm the zone, including fishing, geoengineering and deep-sea mining, to proceed cautiously and be guided by the best available science, for catch and bycatch to be reported, for marine protected areas, monitoring and strategic environmental assessment to be used, and for policymakers to recognise the zone's role in climate regulation. What it does not do is call for a pause, unlike the IUCN's 2021 motion on deep-sea mining. Its logic is preventive rather than restorative: get the rules written before the fishery exists rather than after. The disagreement it papers over is real and worth stating fairly. Chris Dorsett of Ocean Conservancy framed the vote as a step toward awareness and summarised the position as looking before leaping. Esben Sverdrup-Jensen of the European Association of Fish Producers Organisations took the other view, arguing that if mesopelagic biomass is sustainably managed, the potential of the resource is limitless. Blue Marine Foundation has gone further than the motion, calling for a global moratorium on new mesopelagic fisheries while research continues and for marine protected areas spanning the full water column rather than just the seabed. What makes this argument unusual is that both sides are reasoning from the same gap in knowledge. Nobody can currently say with confidence whether the twilight zone holds 600 million tonnes of fish or ten billion, how quickly they reproduce, how much carbon they move, or what a fishery would do to any of it. One side reads that uncertainty as a reason to wait. The other reads it as a reason not to foreclose an opportunity.   A Hidden Migration Shapes Ocean Life   Diel vertical migration is the mechanism that connects two ocean worlds that would otherwise barely interact. Surface production feeds the deep, deep-dwelling animals subsidise surface predators, and carbon moves downward faster and further than physics alone would carry it. It happens every night, everywhere, and has done so for far longer than there have been humans to miss it. The practical point for anyone thinking about ocean policy is that the twilight zone is now simultaneously the least understood major ecosystem on the planet and one of the few remaining unclaimed biological resources of global scale. Those two facts are arriving at the same moment, which is precisely the combination that has gone badly before. The IUCN vote suggests a reasonable number of people have noticed.   Note: This article reflects the state of research and policy as of October 2026, drawing on sources including the IUCN World Conservation Congress motion on the mesopelagic zone adopted in October 2025, Blue Marine Foundation's 2025 report on the twilight zone, Thibault et al. in Biogeosciences (2025) on micronekton contributions to carbon export, and published estimates of mesopelagic biomass and carbon flux. Biomass and carbon figures for this zone carry exceptionally wide uncertainty and are presented as ranges for that reason.

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