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Fixes to the ocean climate could make the oxygen crisis worse.

A geochemical alternative with fewer hazards

By Francis DamiPublished 7 months ago 6 min read

Scientists are looking to the ocean to slow down global warming. About 25% of CO2 emissions caused by humans are absorbed by the sea, which is the greatest carbon sink on Earth. Potential ways to lower atmospheric carbon and perhaps restore diminishing oxygen levels are provided by this enormous system.

However, recent studies indicate that not all remedies benefit the ocean itself. Deoxygenation is one of the ocean's most pressing issues, and some of the most talked-about marine carbon dioxide removal (mCDR) methods may make it worse.

The rate at which oceans are losing oxygen is shocking. About 2% of the oxygen in the world's oceans has been lost since the 1960s. There is more to this trend than just statistics. It manifests itself in declining marine ecosystems, increased fish mortality, and biodiversity loss.

The ocean's ability to move oxygen to deeper layers is diminished by global warming, which results in warmer water and more robust layering. However, what if this loss is exacerbated by the very strategies intended to halt warming?

Unexpected consequences of carbon removal

This subject is addressed in a recent study that was published in the journal Environmental Research Letters. The research team examined several mCDR techniques under the direction of Dr. Andreas Oschlies of the GEOMAR Helmholtz Centre for Ocean Research.

Among these were artificial upwelling, ocean fertilisation, macroalgae farming, and improving the alkalinity of the ocean. They investigated the direct and indirect impacts of these methods on ocean oxygen using fictitious worldwide models.

"What benefits the climate does not necessarily benefit the ocean," Oschlies stated. In order to compare how each approach strikes a compromise between the objective of carbon removal and its unintentional oxygen implications, his team worked with the UNESCO Global Ocean Oxygen Network (GO2NE).

The work demonstrates that significant oxygen losses can result from a variety of biotic mCDR techniques, particularly those that include sinking and biomass production.

The severe disadvantages of ocean fertilisation

Ocean fertilisation is one of the earliest mCDR techniques that has been suggested. It entails supplementing the ocean surface with nutrients, mostly iron, to promote the growth of phytoplankton.

After absorbing CO₂, these small plants sink, transferring carbon to deeper seas. However, they also use up oxygen when the phytoplankton decompose.

According to model projections, a century of constant fertilisation of the Southern Ocean would result in a worldwide oxygen depletion of roughly 3%. That is over twice as much oxygen loss as warming alone.

Oxygen levels may decrease by more than 50 micromoles in some places beneath the fertilised zones. The deoxygenation observed in high-emission climatic scenarios is mirrored or surpassed by these changes.

Simulations show that all oxygen increases due to reduced global warming are placed in the shade thanks to this carbon removal due to biomass losses.

"Our model simulations show that such an approach can lead to a reduction in dissolved oxygen. This is times higher than oxygen gain, which is expected from a reduction in global warming," Oschlies said.

Setang Solutions and Its Boundary

Macroalgae have gained popularity as a promising MCDR strategy. Algae grow rapidly, do not require fresh water, and absorb large amounts of carbon. However, what happens after growth determines its environmental impact.

When macroalgae submerge into the deep sea, they will eventually decompose as fertilized plankton. Complete remineralization of submerged macroalgae can reduce the world's marine oxygen cloud by more than 10% within a century.

The oxygen impact is strong, even if only a part of it decomposes. Projects that suggest large-scale open-ocean kelp sinking as a climate remedy should be wary of these findings.

One variation of this technique, however, does not degrade oxygen levels. Oxygen is preserved when seaweed is harvested and removed, either for use in goods or for safe storage. The removal of nutrients even lowers oxygen use elsewhere, and there is no breakdown in the water.

According to model calculations, harvesting might increase ocean oxygen levels by more than 2% worldwide. The benefit of less heat alone is 10 times smaller than this gain.

Cooler surfaces, lower damage

artificial rise is another MCDR idea. It involves pumping deep, cold, nutrient-rich water onto the surface to stimulate photosynthesis.

This helps to absorb CO2, but also increases the production of organic matter. This biomass consumes oxygen as soon as it sinks and collapses.

The simulation shows that artificial rise can reduce oxygen by about 1.5 pmol. This effect is particularly focused on tropical and subtropical zones, and is already susceptible to waste of depletion.

Some areas may be reduced by 10%. Worse, when used next to macroalgae breeding, oxygen drainage can be further increased.

The cooling effect from the upward direction provides a small benefit of oxygen solubility. However, these benefits are compensated for by biomass loss. As mentioned in this study, if upward trends are not managed carefully, they can lead to higher warming in the long run.

Daily oxygen cycles in the ocean

include the falling of land biomass, such as marine wood and plant waste. In this case, the ocean acts not as a carbon producer, but as a storage space. Depending on the biomass composition, oxygen consumption can be slower than that of marine materials.

However, when nutrients reach the surface from this disintegration, they can fertilize surface water and cause the same oxygen consumption cycle as seen during marine fertilization.

mCDR techniques also focus on Blue Carbon Ecosystems, like seagrass beds, salt marshes, and mangroves. They store CO₂ in sediments after absorbing it. The effects of oxygen in these areas are complicated. While respiration lowers oxygen at night, photosynthesis increases it during the day.

Both oxygen-rich and oxygen-poor stages of marine life may be stressed by these systems' capacity to produce strong daily oxygen cycles. Despite their limited global size, their local oxygen dynamics are worth closely observing.

A geochemical alternative with fewer hazards

Not every mCDR technique exacerbates oxygen loss. One notable feature of ocean alkalinity enhancement (OAE) is its low oxygen impact. Using this technique, seawater is treated with alkaline materials such as pulverised limestone. Without promoting the creation of biomass, it alters the chemistry of the ocean to absorb more CO₂.

Large-scale OAE may marginally raise ocean oxygen levels worldwide, according to model studies. The increase is steady but modest, roughly 0.5 Pmol.

OAE does not introduce nutrients that could promote oxygen-consuming degradation, in contrast to biotic approaches. From an oxygen perspective, this makes it one of the safer marine carbon methods for the time being.

Monitoring oxygen and removing carbon from the ocean

The study ends with a compelling suggestion. Oxygen must be measured throughout the whole mCDR project, regardless of its size, from a small-scale trial to a full deployment.

"The ocean is a complex system that is already under pressure," Oschlies said. "If we intervene in large-scale measures, no matter how good our intentions are, we need to ensure that marine environmental conditions are no longer threatened.

Oxygen is one of six important climate variables already followed for marine health. It directly connects to biological diversity, ecosystem services, and carbon storage. However, when it comes to carbon removal, it is often overlooked.

Oxygen monitors aren't just for it. In some cases, oxygen, such as macroalgae harvesting, can signal the cosystem. Otherwise, it could reveal unintended risks in endangered areas. In both cases, oxygen provides important feedback on whether our climate options will help or harm the ocean.

Carbon removal must protect marine oxygen.

Carbon Dioxide Removal is no longer an option. Even the most ambitious emissions rule out unavoidable emissions. To achieve the net-zero goal, carbon must be drawn out of the air. The ocean, with its scale and its buffering power, seems to be an obvious partner. However,

should assess the solution more than its climate impact. It needs to protect the ocean's lifespan, support biological diversity, and prevent further damage.

This study reveals that biotype MCDR strategies must be treated with caution. Without oxygen, it is an ocean-collapsing ecosystem. And climate protection solutions that empty the ocean of life are not the solution at all.

ClimateHumanityNatureScienceSustainability

About the Creator

Francis Dami

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  • Carmen Torres7 months ago

    The ocean's role in absorbing CO2 is crucial, but some mCDR methods might worsen deoxygenation. It's a complex issue, and we need to find solutions that balance carbon removal and ocean health. We've seen how warming affects oxygen movement. These new findings show we gotta be careful with mCDR techniques to avoid making the ocean's oxygen problem even worse.

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