Ocean acidification has severe effects on marine life, particularly coral reefs, which are vulnerable to acidification and may collapse due to rising ocean acidity and intense storms, with a predicted 90% destruction of the world's coral reefs.

Ocean acidification is caused by the absorption of excess carbon dioxide by the oceans, which forms carbonic acid and increases the acidity of the water.

Ocean acidification has a significant impact on marine ecosystems, particularly coral reefs, making it harder for them to repair their structures and potentially leading to their collapse.

Increased ocean heat can lead to wide-scale coral bleaching, death of marine life, and elevation of sea level, with coral reefs being particularly vulnerable to acidification.

"Biological removal of CO2 through primary production is a key factor in addressing ocean acidification, and international cooperation is also necessary to mitigate its effects."

Ocean acidification has a significant impact on marine ecosystems, particularly coral reefs, which are vulnerable to acidification and may collapse due to rising ocean acidity.

The study on ocean acidification was published in Scientific Reports.

Ocean acidification has a significant impact on the early life stages of marine life, particularly those with calcium carbonate shells, such as clams. The addition of shell hash to their environment can help mitigate the effects of acidification.

Climate change affects marine life by decreasing oxygen levels in the water as temperatures rise, forcing species to move.

Ocean acidification causes marine organisms to have thinner and smaller shells due to the decrease in water pH levels.

Ocean acidification threatens marine calcifiers such as clams, mussels, and oysters by inhibiting the flourishing of species with calcium carbonate shells, which can lead to a decline in their harvest.

Ocean acidification has severe effects on marine life, particularly coral reefs, which are vulnerable to acidification and may collapse due to rising ocean acidity and intense storms, with a predicted 90% destruction of the world's coral reefs.

Title:

Content: If we continue to live the way we are, I am worried for the people who will see the next 90 years.
The latest scientific explanation suggests that the biological world is on the verge of destruction.
The collapse has indeed begun, and it is bound to accelerate, leading to an increase in the scale of the collapse and its impact.
Everything that we depend on for our survival — what our environment has always given us — may begin to falter or disappear altogether.
The predicted disaster will be more devastating than Chernobyl or any event to date, not only causing floods, powerful hurricanes and summer wildfires, but also reducing the quality of life for each victim and their descendants, with irreparable consequences.
When the global ecological collapse is finally resolved and a balance is reached, humanity will live forever on a barren planet if it still exists on Earth.
2030s
Decades of large-scale deforestation and illegal burning in the Amazon basin by people who want to develop more land for agricultural purposes will reduce the area of the Amazon rainforest to 75% of the original forest by the 2030s.
Although still massive, this could be a tipping point in the Amazon rainforest, triggering a phenomenon known as forest dieback.
Forests suddenly become unable to generate enough water from the shrinking canopy to nourish rain clouds, and the most vulnerable areas of the Amazon rainforest degenerate first into seasonal drylands and later into savannahs.
The phenomenon of this decline is self-propelled — the more cases of blight occur, the more trees will die; as a result, drought will quickly sweep across the Amazon basin, causing severe damage.
The loss of biodiversity is devastating, with one in 10 known species in the world inhabiting the Amazon basin, representing innumerable local extinctions that create a domino effect across the ecosystem.
All wild populations will be severely damaged, and it will become increasingly difficult for each individual to feed and find a mate.
Perhaps some of the species used in medicine, new food, and industry disappeared before we even knew it existed, and the human cost was even more profound and heavy.
As the forests wither, the Amazon basin floods frequently, flushing the soil from tree roots into rivers; 30 million people may have to leave the watershed, including nearly 3 million native inhabitants; changes in moisture in the air could show signs of reduced rainfall across much of South America, leading to water shortages in many large cities, ironically because, As a result, the farmland developed in the forest is also dry.
Food production in Brazil, Peru, Bolivia and Paraguay will be significantly affected.
For the Holocene, the Amazon rainforest ’ s best environmental service is absorbing more than 100 billion tons of carbon.
Forest wildfires that occur in each new dry season release large amounts of carbon into the atmosphere, while the reduced capacity of forest photosynthesis means less carbon is absorbed by the region each year.
The extra carbon dioxide in the atmosphere will undoubtedly accelerate the rate of global warming.
On the other side of the globe, the Arctic Sea is expected to experience its first completely ice-free summer in the 2030s, making the Arctic open water.
Even if the sea ice that has been in the safe haven for many years, the thick ice layer freezes over and over again, it cannot avoid warming and may start to disappear.
The seaweed forests that lie beneath the ice fall to the ocean floor, affecting the entire Arctic food chain.
As the Earth's ice layer decreases, the white area will gradually shrink each year, which means that the solar energy reflected back into space will also decrease, and the pace of global warming will accelerate again.
The Arctic began to lose its ability to cool the Earth.
The 1950s
Forest wildfires and melting ice over the next three decades will dramatically increase carbon emissions in the atmosphere.
As always, the surface of the sea absorbs too much carbon, and carbon dioxide will form carbonic acid after it is dissolved in the water, first at the shallow beach, then into the ocean circulation, and finally throughout the water body.
By the 2050s, the entire ocean could reach enough acid levels to cause a catastrophic decline.
Coral reefs are the most abundant of all marine ecosystems and are particularly vulnerable to acidification.
Due to years of coral bleaching, rising ocean acidity makes it harder for coral reefs to repair their calcium carbonate structure.
In this era of warmer air and intense storms, coral reefs may collapse as a result.
It is predicted that 90% of the world ’ s coral reefs will be destroyed within a few years.
The oceans are also vulnerable to acidification.
Various plankton species at the bottom of the food chain also have calcium carbonate shells. An increasingly acidified ocean will inhibit its flourishing, and fish populations throughout the food chain will suffer from it, and the harvest of oysters and mussels will begin to decline.
The rest of commercial fishing and fish farming may begin to come to an end in the 1950s, with the lives of more than half a billion people directly affected, and some source of protein that humans have been consuming will disappear from our diets.
The 1980s
By the 1980s, global food production on land may be in crisis.
In the cool and affluent regions of the world, intensive agriculture has used too much fertilizer for a century, resulting in depletion of land forces, no vitality and no harvest; while in warm and poor regions, global warming will cause temperature rise, monsoon, storm and dry season changes, making farming doomed to failure.
Millions of tons of topsoil lost around the world could enter rivers, bringing flooding to downstream towns.
If current levels of pesticide use remain high, habitat loss continues, and pollinator diseases such as bees continue to spread, the disappearance of insect species will affect three-quarters of our food crops by the 1980s.
Harvests of nuts, fruits, vegetables, and oilseeds will be greatly affected if you can ’ t rely on the diligent pollination of insects.
At some stage, the condition may worsen while another disease is endemic.
We just learned that there is a link between the emergence of new viruses and the survival of the planet, with an estimated 1.7 million potentially human viruses hiding in mammalian and bird populations.
The more we cut down forests, expand farmland, and illegally trade wildlife to destroy nature, the more likely we are to cause another outbreak of infectious diseases.
2100s
The 20th century could set off a massive global humanitarian crisis, which would be the largest forced migration in history.
In the 21st century, coastal cities around the world are expected to face a sea level rise of 0.9 meters due to the slow melting of the ice sheets in Greenland and Antarctica and the increasing warming of the oceans.
Over five decades, more than a billion of the 500 coastal cities may have been affected by storm surges, but by the 20th century, sea levels will rise enough to inundate ports and flood hinterlands.
Ports in Rotterdam, Ho Chi Minh City, Miami and other countries will not be able to withstand flooding, so they cannot take risks and become uninhabitable.
Those who were displaced had to move inland.
But there is a more serious problem.
If all of the above had happened, the Earth would be 4 degrees warmer by 2010 than it is today.
More than a quarter of the population may live in places where the average temperature exceeds 29 degrees Celsius, and today only the Sahara Desert can reach this daily high temperature.
It is impossible to farm in these areas, and a billion rural people may be forced to find a better way out.
Areas where the global climate is still milder will be under enormous pressure from population migration, where borders between countries will inevitably disappear, and conflicts may erupt around the world.
In this context, the arrival of the sixth great extinction will become overwhelming.
(Excerpt from Living on Our Planet)
【 Introduction 】
Netflix documentary of the same name
Forest fires, Arctic ice melting, torrential rain, floods, high temperatures to jump electric connection...
Is the Sixth Great Extinction Coming?
The human mind!
A 100-year-old man who wants to save young people ’ s lives tomorrow.
This is the planet we live on, and we can only protect our future on our own.
★ British National Treasure Nature Science Moderator, Historian, Witness of Earth History
★ Awarded the Order of the Lord by the Queen of England
★ IMDb top ten films, four of which are his works
Breaking the Guinness World Record with 4 Hours of IG Tracking Millions
★ Twice winner of the Emmy Award for Best Narrator
He traveled to 39 countries and photographed 650 species.
There are dozens of animals and plants all over the world named after him.
“I ’ m 95 years old, I ’ ve been making nature documentaries for over 60 years, and I ’ ve been witnessing the change of the planet all my life.
Having witnessed the decline of the earth from its beauty to its present day, and watching the oceans, wastelands, rainforests, and glaciers disappear and destroy their habitats, I will surely feel guilty if I choose to ignore them. "
After 2020, we will experience the following:
By 2030, the Amazon rainforest will be 75% less able to produce water and absorb carbon dioxide, and the Arctic Sea will have its first ice-free summer.
In 2040, the permafrost of the North melts, releasing 1,400 trillion tons of carbon dioxide and accelerating climate change.
By 2050, the oceans will absorb too much carbon leading to acidification, serious ecological damage, and reduced fish populations.
In 2080, the world is plunged into a food crisis due to overuse, exhaustion of land and failure of farming.
By 2100, the Earth's temperature had risen by 4 degrees, most areas were uninhabitable, national borders had disappeared, and wars had broken out.
The sixth great extinction is coming.
This book is the life story of David Attenborough and tells how we committed this terrible disaster, our present predicament, and our vision for the future.
But we ’ re lucky if we act now, make changes, and fix everything.
Live on our planet and make it better.
There is still time and a last chance to restore this beautiful world.
The book will teach you to take action, and what the earth needs is your will.
【 About the Author 】
by David Attenborough
In 1985, he was awarded a knighthood by the Queen of England for his contribution to the filming of natural and historical documentaries. In 2020, he was selected as one of the “Top 100 People in the UK ”.
Born in 1926, he is a natural science broadcaster and historian.
In collaboration with the BBC Natural History Unit, he has written nine comprehensive documentary films on animals and plants on Earth, four of which are ranked in the top 10 of IMBD. He won the Emmy Award for Best Interpreter in 2018 and 2019, and produced Living on Our Planet in 2020, documenting his life ’ s testimony to the Earth and his future. Attention.
> Johnny.
by Jonnie Hughes
A science writer and documentary director, he produces science and natural history films for the BBC, Discovery, National Geographic and Netflix, and has been involved in the BAFTA award-winning BBC series The Hunt and Emmy Award-winning Our Planet.
【 Translator 's Profile 】
＞ CHEN Si-wah
Graduated from the Department of Applied English at Ming Chuan University, he is interested in reading and writing, and is now a freelance translator.
# Earth # 22nd Century # Sea Level Rise # Rainforest # Extinction

What factors lead to damage of coral reefs?

Ocean acidification is caused by the absorption of excess carbon dioxide by the oceans, which forms carbonic acid and increases the acidity of the water.

What is the main cause of ocean acidification?

water absorbs carbon dioxide from the atmosphere

Ocean acidification has a significant impact on marine ecosystems, particularly coral reefs, making it harder for them to repair their structures and potentially leading to their collapse.

What factors lead to damage of coral reefs?

Increased ocean heat can lead to wide-scale coral bleaching, death of marine life, and elevation of sea level, with coral reefs being particularly vulnerable to acidification.

What factors lead to damage of coral reefs?

ocean acidification
sea surface temperature

"Biological removal of CO2 through primary production is a key factor in addressing ocean acidification, and international cooperation is also necessary to mitigate its effects."

Title:

Content: There were 974 press releases posted in the last 24 hours and 451,057 in the last 365 days.

Editorial: the changing carbonate systems in coastal, estuarine, shelf areas and marginal seas

Editorial on the Research Topic
The changing carbonate systems in coastal, estuarine, shelf areas and marginal seas

Global atmospheric CO2 concentrations have increased from 320 ppm in the 1960s to the present-day value of 420 ppm, primarily due to anthropogenic activities. This increase influences the seawater carbonate system, impacting the marine ecosystem. There are still gaps that need to be resolved for predicting how these marine systems respond to current and future CO2 levels. Any actions to mitigate the change in pH will require adaptive management of multiple stressors across several spatial scales. Combined, these perspectives yield a more comprehensive picture of events during ocean acidification (OA).

This Research Topic brings together articles from different regions, including coastal, estuarine, and shelf areas and marginal seas, all susceptible to changing atmospheric conditions, riverine inputs, air-sea CO2 exchanges, and multiple acid-base reactions that can alter carbonate chemistry. Articles on the long-term trends of CO2 system descriptors and the interactions with calcifying organisms were also sought. The present Research Topic is primarily based on original articles devoted to carbonate systems in the marginal seas, but it is a pity that some interesting papers dealing with freshwater inflows, estuaries, and related coastal areas were not accepted.

Fransson et al. examined the effects of glacial and sea-ice meltwater on ocean acidification in the waters near the 79 North Glacier (79 NG) and the northeast Greenland shelf. The researchers investigated various ocean acidification factors and the influence of freshening, primary production, and air-sea CO2 exchange. One of the key findings was that the biological removal of CO2 through primary production played a crucial role in offsetting the negative impact of freshwater dilution on the aragonite saturation state (ΩAr), which is a measure of ocean acidification. This compensation effect was most pronounced in 2012, especially in the vicinity of the 79 NG front, where there was a significant presence of glacial meltwater and surface stratification. In 2016, a different scenario was observed, with a more homogenized water column due to sea-ice meltwater. In this case, the compensation effect of biological CO2 removal on ΩAr was weaker compared to 2012. The study also suggests that in the future, with ongoing climate and ocean chemistry changes, the increasing influence of meltwater may surpass the mitigating effects of biological CO2 removal. This could lead to unfavorable conditions for organisms that rely on calcium carbonate for their shells and skeletons. Thus, all the proposed factors need to be closely monitored as they could have significant implications for marine ecosystems and calcifying organisms in the face of ongoing environmental changes.

In a study by You et al., the researchers assessed ocean acidification in the Western Pacific using boron isotopic analysis in a large tropical coral core from Lanyu Islet in Southeast Taiwan. They used a well-preserved coral skeleton (Porites lobata) for detailed major and trace element analysis, including boron (B) and its isotopes (δ11B), as well as stable isotopes of oxygen (O) and carbon (C). Their primary objective was to investigate environmental changes during the period from 1991 to 1997. The coral records revealed a distinct temporal trend in sea surface temperatures (SSTs) based on elemental/calcium ratios on both annual and monthly scales. Notably, the most temperature-sensitive proxy, Mg/Ca-SSTs, indicated a significant warming trend during the study period. The researchers also observed subtle changes in the annual δ11B record, corresponding to a pH decrease of approximately 0.2 units. This change was consistent with other coral records in the Pacific, in-situ measurements of pH and pCO2, and model predictions, highlighting the impact of human-induced ocean acidification. When combined with Mg/Ca-SST data, the intra-annual coral data exhibited a clear seasonal cycle, with higher pH levels during the winter, aligning with surface ocean pCO2 patterns. These chemical and isotopic findings in corals underscore the value of marine biogenic carbonates as informative tools for reconstructing oceanic pH changes.

Rivaro et al. investigated freshwater inflow into the Ross Sea in Antarctica, particularly through the eastern gate and along the Ross Ice Shelf. They conducted a survey during the austral summer of 2019-20 to assess the contribution of Amundsen Sea Water (ASW) to salinity variations. The researchers used data on total alkalinity (AT), pH, temperature, and salinity to analyze the properties of the carbonate system, including total inorganic carbon, pCO2, and the calcium carbonate saturation state of aragonite and calcite (Ω), along with the Revelle factor. They also estimated anthropogenic carbon (Cant) using the TrOCA method to gain insights into the carbon cycle and its impact on ocean acidification due to atmospheric CO2 uptake. The study found that changes in the carbonate chemistry of surface waters were primarily influenced by physical properties. AT and pH were effective indicators of the entry of ASW, demonstrating limited mixing between different water masses in the shelf area. Additionally, shelf waters were enriched in Cant, leading to levels lower than what was estimated for shelf waters generated in the western Ross Sea.

Ingrosso et al. investigated the factors influencing the absorption of anthropogenic carbon dioxide (Cant) in the Ross Sea, an area known for its capacity to absorb carbon due to its cold waters, high primary productivity, and unique circulation on the Antarctic continental shelf. The researchers focused on the carbonate system to assess the current levels of anthropogenic carbon and understand how physical and biological processes regulate Cant sequestration along the shelf-slope continuum. They found that the Winter Water mass, formed during convective events, contained high levels of Cant due to the mixing of layers during the cold season. In contrast, the older and less-ventilated Circumpolar Deep Water entering the Ross Sea had minimal anthropogenic carbon contributions. The study also revealed variations in Cant content between different areas, such as polynyas and the shelf break, influenced by their distinct hydrographic and biological characteristics. The intense microbial activity in these regions consumed a significant portion of particulate organic carbon, leading to the release of CO2 into the intermediate and deep layers of the continental shelf zone. The findings underscored the importance of summer biological activity over the Ross Sea shelf in facilitating the transfer of anthropogenic CO2 between organic and inorganic carbon pools. This process contributed to ocean acidification in the upper mesopelagic zone and the long-term sequestration of Cant in the deep ocean.

Hassoun et al. conducted a comprehensive review of ocean acidification (OA) research in the Mediterranean region using data from the United Nations’ International Atomic Energy Agency’s Ocean Acidification International Coordination Center (OA-ICC) database and an extensive survey. Their analysis revealed several important knowledge gaps in understanding OA trends and biological impacts in the semi-enclosed and densely populated Mediterranean Sea. These gaps are attributed to disparities in OA research capabilities among Mediterranean countries and the intricate, long-term interactions among biological, chemical, and physical factors. The study highlighted an uneven distribution of OA research efforts across the region, with the Algero-Provencal and Ionian sub-basins being the least studied areas. Furthermore, the carbonate system in coastal zones remains inadequately quantified, and there is a scarcity of long-term time series data in the Mediterranean, making it challenging to assess OA trends along the coast. While certain groups of organisms, such as autotrophs (algae, phanerogams, phytoplankton), mollusks, and corals, have received considerable attention in research, others, including microbes, small mollusks (particularly pteropods), and sponges, have been relatively understudied. Despite available resources and agreements for enhanced and coordinated OA governance, there is a lack of consistent OA policies in the Mediterranean Sea. To address these challenges, the article offers recommendations based on their literature review and insights from the Mediterranean OA scientific community.

Curbelo-Hernández et al. conducted an analysis of the carbon dioxide (CO2) system, anthropogenic carbon (Cant) inventory, and air-sea CO2 fluxes (FCO2) in the waters surrounding the Macaronesian archipelago. They found that variations in CO2 levels were primarily influenced by temperature changes, biological activity, and advection processes driven by differences in the Canary Upwelling System, mixed layer depth, mesoscale activity, and circulation patterns. Surface CO2 levels (fCO2,sw) were found to be influenced by biological production and the injection of CO2-rich water in tropical waters, while temperature fluctuations played a significant role in subtropical waters. The study also examined the factors that control changes in the total inorganic carbon normalized to a constant salinity (NCT) in the upper ocean. The research revealed an increase in the uptake and storage of anthropogenic carbon compared to preexisting levels, as calculated using the TrOCA 2007 approach, which served as an upper limit for NCT. The importance of the organic carbon pump diminished in subtropical waters, while the carbonate pump had minimal contribution. Regarding FCO2, the area behaved as a CO2 sink during the winter, but strong outgassing was observed over the Cape Blanc filament. To enhance understanding in this region, the authors compared their data with existing datasets (SOCAT and GLODAP) and provided a new set of equations for calculating fCO2,sw, Cant, and FCO2 in the Macaronesian area.

All these studies emphasize the urgency of addressing ocean acidification and its multifaceted impacts on marine ecosystems. They call for continued monitoring, research, and international cooperation to better understand and mitigate the effects of rising CO2 levels on our oceans and the life they support.

Ogrinc N., Giani M. & Faganeli J., 2023. Editorial: the changing carbonate systems in coastal, estuarine, shelf areas and marginal seas. Frontiers Marine Science 10: 1325363. doi: 10.3389/fmars.2023.1325363. Article.

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Ocean acidification has a significant impact on marine ecosystems, particularly coral reefs, which are vulnerable to acidification and may collapse due to rising ocean acidity.

What factors lead to damage of coral reefs?

The study on ocean acidification was published in Scientific Reports.

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Content: There were 1,516 press releases posted in the last 24 hours and 395,342 in the last 365 days.

Effects of water flow and ocean acidification on oxygen and pH gradients in coral boundary layer

Effects of water flow and ocean acidification on oxygen and pH gradients in coral boundary layer

Published 10 June 2024 Science Leave a Comment
Tags: biological response, chemistry, corals, morphology

Reef-building corals live in highly hydrodynamic environments, where water flow largely controls the complex chemical microenvironments surrounding them—the concentration boundary layer (CBL). The CBL may be key to alleviate ocean acidification (OA) effects on coral colonies by partially isolating them. However, OA effects on coral CBL remain poorly understood, particularly under different flow velocities. Here, we investigated these effects on the reef-building corals Acropora cythereaPocillopora verrucosa, and Porites cylindrica. We preconditioned corals to a control (pH 8.0) and OA (pH 7.8) treatment for four months and tested how low flow (2 cm s−1) and moderate flow (6 cm s−1) affected O2 and H+ CBL traits (thickness, surface concentrations, and flux) inside a unidirectional-flow chamber. We found that CBL traits differed between species and flow velocities. Under OA, traits remained generally stable across flows, except surface pH. In all species, the H+ CBL was thin and led to lower surface pH. Still, low flow thickened H+ CBLs and increased light elevation of surface pH. In general, our findings reveal a weak to null OA modulation of the CBL. Moreover, the OA-buffering capacity by the H+ CBL may be limited in coral species, though low flow could enhance CBL sheltering.

Martins C. P. P., Ziegler M., Schubert P., Wilke T. & Wall M., 2024. Effects of water flow and ocean acidification on oxygen and pH gradients in coral boundary layer. Scientific Reports 14: 12757. doi: 10.1038/s41598-024-63210-9. Article.

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Ocean acidification has a significant impact on the early life stages of marine life, particularly those with calcium carbonate shells, such as clams. The addition of shell hash to their environment can help mitigate the effects of acidification.

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Content: There were 1,862 press releases posted in the last 24 hours and 393,697 in the last 365 days.

Utilizing biogeochemical and genetic tools to understand and support clam populations in a changing ocean

Marine bivalves are at risk due to anthropogenic climate change. This poses a threat to commercial aquaculture, and the communities that depend on bivalves for food security. Ocean acidification, the lowering of seawater pH, is of particular concern for marine calcifiers, including bivalves. Ocean acidification occurs as carbon dioxide enters the atmosphere at a rate faster than natural geologic processes can buffer. It is energetically costly for marine calcifiers like clams, mussels, and oysters, to mineralize under acidic conditions, and low pH leads to the dissolution of calcium carbonate shells and skeletons. This problem warrants research on acidification adaptation strategies that will keep coastal populations healthy. Adding calcium carbonate shell hash to coastal sediments may mitigate negative effects of acidification on infaunal shellfish by altering the chemistry of pore fluids, thus providing a potential mitigation strategy for local populations, including species like the Pacific littleneck clam (Leukoma staminea).

Here, I present the first in-depth description of the shell mineralogy, microstructure, body size variability, and geochemical properties of modern L. staminea, a common eastern Pacific, shallow, infaunal bivalve. Additionally, I document the impact of ocean acidification on the shell growth and gene expression of L. staminea, and test whether adding shell hash to its infaunal environement can promote growth under acidified conditions. Juvenile clams were raised in four experimental conditions for 90 days: control seawater, acidified seawater, control seawater with shell hash, and acidified seawater with shell hash. Clam shell weight, soft tissue weight, and new shell growth were measured. The presence of shell hash increased the pH, alkalinity and aragonite saturation state of pore fluids across all treatments, and increased shell growth on average, although growth metrics were variable across and within treatments. Lastly, RNA-sequencing revealed the impacts of experimental acidification on juvenile clam gene expression. Clams grown in the presence of shell hash had gene expression profiles more similar to those grown in control (non-acidified) conditions. In all, this research suggests that adding shell hash to coastal sediments alters the chemistry of pore fluids and buffers against acidic conditions that deleteriously affects clam mineralization.

Kempf H., 2024. Utilizing biogeochemical and genetic tools to understand and support clam populations in a changing ocean. PhD Thesis, University of California, Davis. 33 p. Thesis (restricted access).

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At what stage of life are calcium carbonate-based organisms most vulnerable to changes in water pH?

How does coastal ocean acidification affect shellfish?

What do shellfish use to build their shells?

Climate change affects marine life by decreasing oxygen levels in the water as temperatures rise, forcing species to move.

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Content: How climate change and warming waters are affecting the health of the oceans

(NEW YORK) — Oceans do so much to sustain life on Earth, including bearing the brunt of global temperatures that have been steadily warming for decades.

An IPCC special report published in 2019 found that oceans — which make up more than 70% of the world’s surface — have absorbed between 20% and 30% of human-made carbon dioxide emissions since the 1980s. They’re also responsible for absorbing more than 93% of the “combined heat stored by warmed air, sea, and land, and melted ice” since the 1970s, according to the Fifth Assessment report published in 2013 by the United Nations Intergovernmental Panel on Climate Change.

The tipping point is near, experts told ABC News. But there are collective actions to take that could revitalize oceans to a healthier state — the theme of the United Nations World Oceans Day 2022.

“We really see oceans as the biggest ally in the climate change crisis,” Lea d’Auriol, founder of nonprofit Oceanic Global, told ABC News.

This is how climate change is affecting the health of the world’s oceans:

Species are faced with adapting or becoming extinct

Currently, the oceans “are in a state of complete imbalance” that has nearly doubled since the 1990s, d’Auriol said. Look no further than the fishermen, who supply sustenance to more than three billion people who rely on seafood as their main source of protein, as witnesses that climate change is already here, d’Auriol, said.

“If you wanted to ask someone if climate change is really happening, probably the most surest answer you’d get from anyone aside from a scientist is a fisherman,” Arlo Hemphill, senior oceans campaigner for Greenpeace USA, told ABC News. “Because fishermen are seeing these things happen in real time.”

One of the changes long-time fisherman are witnessing is the presence of new species venturing north as the area with their preferred water temperature expands.

Marine organisms maintain the same temperature as the surrounding water, so that when temperature increases, so does the temperature of the organism, Martin Grosell, professor of ichthyology and chair of the University of Miami’s Department of Marine Biology and Ecology, told ABC News. As the temperature rises, the organisms require more energy to move and survive. But, conversely, the levels of oxygen in the water decrease as the temperature warms, forcing the species to move, Grosell said.

The migrations may seem innocuous, but they are disrupting ecosystems all over the world, such as the phenology, or timing, of when grey seals give birth, Hemphill said.

Conversely, species are continuing to die off due to repeated events of marine heatwaves, Anne Christianson, director of international climate policy for the Center for American Progress, a public policy research organization, told ABC News.

Coral reefs are among the most threatened marine ecosystems in the world, scientists say. Coral bleaching, a process that occurs when water is too warm and the corals expel algae from their tissues, causing them to turn completely white, is happening at “alarming” rates — increasing by a rate of 4% per year — along with an uptick in mortality events along entire regions, d’Auriol said.

A study published in the National Academy of Sciences found that coral reefs could stop growing in 10 years unless greenhouse gases are significantly reduced and that, under a worst-case scenario, 94% of all reefs could erode by 2050.

Reefs are often the indicator of the health of an ecosystem, Brenda Ekwurzel, director of climate science for the Union of Concerned Scientists, told ABC News.

Mammals that rely on Arctic ice, such as polar bears and ringed seals, one of the polar bears’ main food sources that live their lives almost entirely on the ice, are also at risk, Ekwurzel said.

Vegetation such as mangroves, seagrass plants and marshes, some of the largest carbon sinks on the planet, which absorb and store carbon dioxide from the atmosphere, are also at risk of extinction, d’Auriol said.

The number of dead zones are increasing

A dead zone, or the process of hypoxia, occurs when an algal bloom sucks up all the oxygen in an area, making it impossible for marine life to survive — essentially a biological desert, according to the National Oceanic and Atmospheric Administration.

A study published in 2008 in Science found that there were 400 dead zones around the world. By 2019, the number of dead zones had increased to about 900, d’Auriol said.

The dead zones often occur in regions with rampant nutrient runoff, such as at the base of the Mississippi River, where it empties into the Gulf of Mexico, Hemphill said.

Sea level rise will change coastal communities

The biggest contributor to sea level rise is the melting ice in the Arctic, which is heating up twice as fast as the rest of the world, according to the 2021 Arctic Report Card by NOAA. Increases in sea level rise of 6 inches to a foot since the Industrial Revolution may seem like small increments, but crucial infrastructure near oceans was not built to withstand the added inches of water, experts say.

Millions of people living in coastlines around the world, including those in mega cities such as New York, Los Angeles and San Francisco, will be displaced by the rise in sea levels, d’Auriol said.

Carbon dioxide emissions sparks ocean acidification

Ocean acidification, which occurs when water’s pH levels are lowered as a result of carbon dioxide in the atmosphere, is not directly caused by warming temperatures but rather by excess carbon dioxide emissions, Hemphill said.

“The alarming thing about it is that shellfish everything from from microscopic plankton, to clams and crabs and coral reefs themselves use calcium carbonate to build their shells,” he said. “And as the ocean acidifies, it becomes more difficult to create the shells.”

Ocean acidification, rather than coral bleaching, will likely be the culprit behind the demise of coral reefs, Ekwurzel said.

Collective actions are necessary to protect the oceans

In line with the 2022 theme for World Oceans Day, “Revitalization: Collective Action for the Ocean,” scientists and conservationists are highlighting the need for individuals, communities, nonprofits, the private sector and governments to come together to create solutions, d’Auriol said.

This includes ensuring the health of marine protected areas by eliminating housing, fishing zones and shipping traffic in the vicinity, d’Auriol said.

Governments will need to create policies to protect both human life and the health of the ocean, Christianson said.

“There isn’t one silver bullet for solving this crisis in the ocean and on land,” Christianson said.

However, the ticking time bomb is the race to drastically reduce global greenhouse gas emissions within the next decade, the experts said.

“We can’t afford to delay those solutions any longer,” Ekwurzel said.

Along the path to properly protecting and preserving oceans is ridding the narrative that oceans are a separate environmental issue from climate change and the conservation of biodiversity, d’Auriol said.

“Because we do live on a water planet, and it’s responsible for sustaining all life on Earth,” she said.

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Ocean acidification causes marine organisms to have thinner and smaller shells due to the decrease in water pH levels.

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The Logical Indian Crew

Rise In CO2 Levels In Air Is Wounding Sundarbans' Marine Life: Scientists

This has been analysed by a team of marine scientists working in the Sunderbans, who said ocean acidification is a part of global warming and climate change. The experts found the pH level of water dropping from around 8.3 in the early 1980s to approximately 7.9 in 2019.

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A continuous increase in the carbon dioxide (CO2) levels in the air is harming the marine life of the Sunderbans estuary in West Bengal by turning it acidic. Animals, especially with shells such as oysters, clams, crabs, and lobsters, are prone to danger.

This has been analysed by a team of marine scientists working in the Sunderbans, who said ocean acidification is a part of global warming and climate change, Hindustan Times reported. The experts found the pH level of water dropping from around 8.3 in the early 1980s to approximately 7.9 in 2019.

Speaking to the media, Abhijit Mitra, former head of the marine science department (Calcutta University), informed that the western part of Sunderban, close to the urban area, had observed a massive drop in its pH level, while the central part is declining slowly.

Mitra said the decline affects the population of shelled organisms and their shell size as well, which has become thinner and smaller. Fishermen said that several fish and other animals have gotten smaller, and they hardly get big ones.

Their population has also fallen by 35-40 per cent in the western area.

"The size of Saccostrea cucullata, a species of edible oyster around Kakdwip and Namkhana fishing harbour, has dropped by over 40 per cent. In the central Sunderbans, the size of the species has dropped by around 20 percent," the media quoted him as saying.

Asst. Professor of Indian Institute of Science Education and Research, Punyasloke Bhadury, explained that water contains calcium and carbonate ions, which the shelled animals need to develop and corals to build the reef. But the acidity reduces these components in the water, affecting the shell size and slowing down the growth of reefs.

Experts said the decline in the pH level is alarming. Just as the slightest drop in the pH level of a human body (pH 7.35 to 7.45) can make them sick, the same takes a heavy toll on marine animals.

The scientists said the decline is not just in Sunderbans but other estuaries as well.

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