Ocean acidification is a process whereby excess atmospheric carbon dioxide (CO2) dissolves into the ocean, lowering seawater pH and fundamentally altering its chemistry.

Since pre-industrial times, ocean acidity has increased by 26%, with projections suggesting a rise of up to 150% by 2100 if current emissions persist, posing profound risks for marine organisms and ecosystems .

While coral bleaching is a visible consequence, ocean acidification’s impacts extend far beyond corals.

Many marine organisms, including shell-building animals like clams, oysters, mussels, shrimp, and some plankton, face direct threats due to their reliance on calcium carbonate for shells and skeletons.

Acidification weakens or dissolves these structures, especially in early life stages, resulting in reduced survival and growth, and endangering both wild stocks and aquaculture operations .

Fish are also vulnerable; behavioral changes, impaired predator avoidance, and increased mortality have been documented in acidified waters, particularly among young fish.

These changes threaten fish populations and the many human communities that depend on them .

Cephalopods, such as cuttlefish and octopuses, are somewhat less reliant on calcium carbonate but are not immune.

Their early developmental stages and physiological processes remain susceptible to the rapid changes in ocean chemistry and oxygen content brought on by acidification and warming, threatening their populations and the larger food webs they support .

Zooplankton, especially key Arctic species, show similar vulnerabilities, which may have cascading effects on marine mammals and higher predators .

Overall, ocean acidification jeopardizes not only individual species but also the balance and productivity of marine ecosystems, with direct consequences for biodiversity, food security, and global livelihoods .

Ocean acidification is a process whereby excess atmospheric carbon dioxide (CO2) dissolves into the ocean, lowering seawater pH and fundamentally altering its chemistry.

Title:

Content: The Arctic region is currently undergoing rapid and significant changes, with acidification and warming occurring at alarming rates.
These shifts raise concerns about the resilience of marine communities in the face of such environmental shifts.
Marine zooplankton, especially copepods, play a crucial role in the Arctic food web.
However, differences in environmental conditions can disrupt zooplankton populations, leading to adverse consequences for the entire ecosystem.
Recent research has focused on understanding the extent to which copepods in early life are exposed to environmental stressors, as they represent a critical bottleneck in the copepods life cycle.
A study by Espinel Velasco et al.
(2023) Explore the responses of 4-day-old Kalanos Hyperborius Lenobli to acidification (pH 7.5 and 8.1) and warming (0 and 3 ° C), both individually and collectively.
The study revealed that the larvae 'breathing rates increased significantly when exposed to a combination of acidification and warming.
Surprisingly, exposure to these stressors individually did not produce the same effect.
Surprisingly, the researchers did not find any noticeable differences in fat content and fatty acid composition in the larvae across various experimental treatments.
Wax esters, which make up about 75% of the fat reserve, and high amounts of long-chain fatty acids 20: 1 and 22: 1, necessary for copepods to reproduce, have been detected in all treatments.
By highlighting the sensitivity of larvae to the combined effects of acidification and warming, this study aligns with a growing body of evidence from relevant research.
It highlights the potential impacts of global change on Arctic copepod populations and stresses the importance of understanding early life stage responses to environmental stressors.
Questions and Answers:
Q: What are zooplankton?
A: Zooplankton refers to small, often microscopic, organisms that drift into the ocean or other bodies of water and serve as one of the main sources of food for many marine species.
Q: What is the role of copepods in the Arctic food web?
A: Copepods, especially calanotic copepods such as Calanus Hyperboreus, are a critical component of the Arctic food web.
They serve as a vital link between primary producers (such as phytoplankton) and higher trophic levels, serving as a food source for various marine species.
Q: What is acidification?
A: Acidification refers to the process of increasing acidity (lowering pH) in seawater due to the absorption of carbon dioxide from the atmosphere.
This occurs as a result of human activities, such as the burning of fossil fuels.
Q: How does global warming affect marine ecosystems?
A: Ocean warming can have various impacts on marine ecosystems, including changes in species distribution, changing reproductive cycles, and potential disruptions to the delicate balance of food webs.
Source: Frontiers in Marine Science, DOI: 10.3389 / fmars.2023.1240673

What factors lead to damage of coral reefs?

What is the main cause of ocean acidification?

water absorbs carbon dioxide from the atmosphere

Since pre-industrial times, ocean acidity has increased by 26%, with projections suggesting a rise of up to 150% by 2100 if current emissions persist, posing profound risks for marine organisms and ecosystems .

Title:

Content: Sun. Nov 20th, 2022

This is a small proportion in view of conservatively projected $step one

Because the within , more than twenty four mil km2, or 17 %, off seas around national legislation (to two hundred nautical kilometers of shore) have been included in safe areas, over doubling in the the quantity since 2010

On average, one.dos percent regarding federal search finances are spent on water research between 2013 and you can 2017, having amounts anywhere between 0.02 per cent so you’re able to nine.5 %. 5 trillion contribution of the ocean towards the all over the world economy inside 2010.

Of a lot Says enjoys ratified or acceded into United nations Meeting on feeld review Rules of your Ocean (168 events) as well as using plans (150 people toward Agreement regarding the utilization of Area XI of your Us Seminar on the Rules of one’s Water and 91 functions towards United nations Fish Stocks Arrangement). Numerous Claims features followed these products thanks to court, policy and you may institutional buildings, but further advances becomes necessary in a number of developing places, particularly the least set up regions.

Waters and you can fisheries went on to help with the global population’s monetary, public and you can environment means whenever you are distress unsustainable exhaustion, environment destruction and you may carbon dioxide saturation and you may acidification. Current jobs to guard trick marine surroundings and you can quick-measure fishers and you may buy sea technology commonly yet , fulfilling the new immediate need to include that it huge, sensitive capital.

The ocean assimilates up to 23 % of your own yearly pollutants from anthropogenic carbon dioxide toward surroundings, helping to alleviate the impacts regarding weather change on the planet, although not, ultimately causing a bringing down pH and you can acidification of one’s water. A separate water acidification analysis portal suggests an increase in variability into the pH plus the acidity of one’s waters of the 10 to 31 per cent in the period 2015–2019.

The brand new sustainability off globally fishery info continues to decline, regardless if at the a diminished rates, with the ratio regarding fish stocks within biologically alternative account from the 65.8 % when you look at the 2017, down out of 90 per cent when you look at the 1974 and you may 0.8 fee area less than 2015 profile.

The new expansion away from protected elements having marine biodiversity and you can established rules and you may treaties that prompt in control entry to ocean resources are still insufficient to fight new undesireable effects regarding overfishing, increasing ocean acidification due to weather changes and you may worsening seaside eutrophication

Because the within , how many parties to the Arrangement towards Port State Procedures to get rid of, Deter and you can Eliminate Unlawful, Unreported and Unregulated Fishing – the original joining in the world agreement you to particularly needs illegal, unreported and unregulated fishing – risen to 66 (like the Eu) away from 58 in the earlier year, and you will nearly 70 % out of nations stated rating at the top of the fresh implementation thereof.

The share of alternative marine grab fisheries remained steady at around the globe height, with regional adaptation, representing the biggest contribution with the GDP within the Pacific brief isle development States and you will the very least build countries, averaging 1.55 and 1.15 percent, correspondingly, in 2011 to help you 2017.

Once the vast amounts of somebody count on oceans due to their livelihood and you may dinner source as well as on the fresh new transboundary characteristics regarding waters, improved jobs and you can interventions are needed to cut and you can sustainably have fun with water information at all profile.

  • Water acidification is caused by new consumption off atmospheric Carbon-dioxide of the the sea, and this change this new chemical substances constitution of one’s seawater. Long-label observations from ocean acidification for the past thirty years has found the typical increase from acidity regarding 26 per cent given that pre-commercial times, and also at which rates, a rise off a hundred to help you 150 % try predicted from the the termination of the newest century, having really serious effects to possess marine life.
https://atlanticfinancialmanagement.co.uk/

By tushar

How do scientists expect ocean acidification to impact specific fish species?

What factors lead to damage of coral reefs?

While coral bleaching is a visible consequence, ocean acidification’s impacts extend far beyond corals.

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?

Many marine organisms, including shell-building animals like clams, oysters, mussels, shrimp, and some plankton, face direct threats due to their reliance on calcium carbonate for shells and skeletons.

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.

Like this:

Like Loading...

Related

What do shellfish use to build their shells?

Which marine organism is vulnerable to increased levels of ocean acidification?

Acidification weakens or dissolves these structures, especially in early life stages, resulting in reduced survival and growth, and endangering both wild stocks and aquaculture operations .

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

How do scientists expect ocean acidification to impact specific fish species?

it will affect their physiology and growth

How does coastal ocean acidification affect shellfish?

it slows their growth
it can kill shellfish

How does elevated water acidity affect fish ability to survive?

What factors lead to damage of coral reefs?

Fish are also vulnerable; behavioral changes, impaired predator avoidance, and increased mortality have been documented in acidified waters, particularly among young fish.

Title:

Content: There were 734 press releases posted in the last 24 hours and 394,615 in the last 365 days.

Study explores combined impacts of ocean warming and acidification on pacific cod

Newly hatched Pacific cod larva. (Image credit: NOAA Fisheries/Emily Slesinger)

As the climate changes, the ocean is simultaneously warming and acidifying. Both have been shown to adversely affect the vulnerable early life stages of Pacific cod. But until now, the interplay of these two environmental stressors was unknown.

new NOAA Fisheries study takes a look into the future by replicating predicted Alaska ocean conditions in the laboratory. The study is the first to look at the interactive effects of ocean warming and acidification on Pacific cod. Researchers evaluated the growth and survival of eggs and larvae at combinations of temperature and acidity representing current and future ocean environments. The findings can help improve predictions to ensure climate-ready Alaska fisheries and communities in the future.

Alaska Fish Face Multiple Climate-Driven Stressors

Ocean warming and acidification are escalating faster in Alaska and other high latitude regions than anywhere else on the planet. Alaska produces more than half of the nation’s wild-caught seafood. Local communities depend on the ecosystem for their livelihoods. Understanding how climate-driven stressors will affect these valuable resources is critical to ensuring resilient Alaska communities and a strong blue economy in the future.

Because fish are cold-blooded, temperature profoundly affects their growth and behavior. The effects of acidification are more nuanced. Fish can buffer acidity in the bloodstream but at an energetic cost.

Very young fish—eggs and larvae—tend to be the most sensitive stages of the fish life cycle to both warming and acidification. Unlike adult fish that can move to cooler waters, these tiny creatures are incapable of migrating to more favorable conditions. Subtle differences in their growth and condition can make a big difference to the number of young fish that make it to the adult population.

Laboratory set up for ocean acidification and ocean warming experiments with early stages of Pacific cod. Large tanks in the background provide chilled and ambient seawater that are mixed to temperature. Small round tanks house eggs and larvae at different temperatures and acidification levels. Acidification is controlled by bubbling carbon dioxide into the seawater: more carbon dioxide causes higher acidity (lower pH). (Image credit: NOAA Fisheries/Emily Slesinger)

Pacific cod is an important subsistence food, a key species in the food web, and the second-largest commercial groundfish catch in Alaska. Understanding how warming and acidification together may affect this ecologically, culturally, and commercially valuable species is key to predicting future climate impacts.

“Knowing how individual species will respond to multiple climate stressors helps us put together this puzzle to figure out what species are more vulnerable than others,” Emily Slesinger said. “And that will help guide ecosystem-based fisheries management to ensure their sustainability.”

Partnerships and Unique Laboratory Capabilities Expand Possibilities for Studying Alaska Species

Finding answers posed some hurdles. “It’s really challenging to study these fish that are found in remote and cold environments,” Slesinger said.

They met those challenges through partnerships and a specially equipped laboratory facility.

Fishermen played a key role. To obtain eggs and larvae for experiments, they first needed live adults, ready to spawn. Commercial fishermen used baited fishing pots to catch adults off Kodiak Island during the spawning season.

Fertilized eggs were shipped to the NOAA Fisheries Alaska Fisheries Science Center Laboratory in Newport, Oregon. The eggs and larvae were reared at six combinations of temperature (3°C, 6°C, 10°C) and acidification (ambient and high acidity). Scientists measured their hatch success, growth, nutritional condition, and mortality throughout the nine-week experiment.

“The Newport lab is very special,” Slesinger said. “What is most unique is our seawater system that can chill water to Arctic temperatures. The lab has the capacity to house many fish at all life stages and the expertise to keep them thriving. And it has the facilities to run these complicated experiments on the younger life stages.”

Experiments Reveal a Dominant Stressor

The study found that overall, Pacific cod’s early life stages were more sensitive to warming than to acidification:

  • Temperature affected all measured traits: growth, condition, and mortality
  • Mortality of both eggs and larvae was highest at the warmest temperature
  • 6°C was the optimal temperature for hatching, condition, and survival
  • At the warmest temperature (10°C), Pacific cod grew the fastest but were in poor condition with high mortality rates
  • At the coldest temperature (3°C), mortality rates were lower, but both growth and condition were also low
  • Acidification effects were more modest and inconsistent
  • The single instance of a negative effect of acidification was at the optimal 6°C temperature

“We’re seeing that either temperature or acidification drove the response—they were not additive. At optimal temperatures, Pacific cod may be impaired by acidification. At the warm temperature, they were overwhelmingly negatively impacted, but there was pretty much no effect of acidification,” Slesinger said. “Our findings suggest that temperature is the dominant stressor and ocean warming is likely the greater threat.”

The research highlights the complexity of species- and stage-specific responses to multiple climatic stressors and the importance of understanding them.

“This work is exciting because we are able to provide information about these fish that can be useful for future management. It is really important to me that my research can be directly helpful to societies, economies, and communities,” Slesinger said. “This research contributes to our common goal of ensuring productive, sustainable fishing into the future.”

Ecomagazine, 30 April 2024. Press release.

Like this:

Like Loading...

Related

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

How do scientists expect ocean acidification to impact specific fish species?

it will affect their physiology and growth

How does elevated water acidity affect fish ability to survive?

fish becomes easy prey for other predators

These changes threaten fish populations and the many human communities that depend on them .

Title:

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).

Like this:

Like Loading...

Related

How do scientists expect ocean acidification to impact specific fish species?

How does elevated water acidity affect fish ability to survive?

Cephalopods, such as cuttlefish and octopuses, are somewhat less reliant on calcium carbonate but are not immune.

Which marine organism is vulnerable to increased levels of ocean acidification?

Their early developmental stages and physiological processes remain susceptible to the rapid changes in ocean chemistry and oxygen content brought on by acidification and warming, threatening their populations and the larger food webs they support .

Title:

Content: Carbon Dioxide Makes Ocean Acidification Study Suggests Rapid Evolution Could Make Fish Easier to Deal With
March 03, 2022 17: 00
Eastern Network Television
More News Clips
Some fish can evolve rapidly to cope with ocean acidification.
(courtesy of Shutterstock)
In addition to causing climate warming, global emissions of large amounts of carbon dioxide will also cause sea water to become acidic, and marine life may be affected.
The study found that volcanic infiltration of high CO2 partial pressure, that is, high concentrations of CO2 dissolved in water, changes in the genetic transcription of fish, predict the response of wild fish to the continuous acidification of the marine environment.
The results show that some fish with faster rates of evolution may be more flexible in coping with ocean acidification, maintaining population size and diversity. One species of fish may be able to acidify the marine environment with its rapid evolution of gene molecular transcription regulation, but the population size and diversity of fish with slower rates of evolution are difficult to maintain in acidified environments.
As carbon dioxide emissions from human activities increase year by year, and the CO2 absorbed by the ocean continues to rise, causing the pH of seawater to decline and become acidic, scientists expect “ocean acidification ” on the surface of the world ’ s oceans, which may affect the physiology, growth and survival of some fish, and change some key behaviors that affect survival chances.
A team led by Celia SCHUNTER from the Faculty of Biosciences of the University of Hong Kong and the Swire Institute of Marine Science, along with foreign researchers, travelled to Papua New Guinea, the Pacific island nation, to extract the brains of six species of coral fish, including five species of finch and one species of celestial bream, from a carbon dioxide spill at the bottom of a volcano and about 500 m nearby coral reef. The organization conducts gene transcription group sequencing to understand the changes in fish gene transcription in the ocean acidification environment.
The results show that high CO2 partial pressure can cause transcription changes in genes related to circadian clock and immune function in several species, demonstrating that fish function is important in coping with acidifying environments, and that the core genes of circadian rhythms determine the 24-hour cycle of most species.
Immune-related regulation has been found in many species of fish in acidified environments, so regulation of the immune response may also be an important response to acidification, especially in nocturnal fish, which exhibit a greater proportion of immune regulation and are modulated in the opposite direction to diurnal fish.
In contrast to the fish body ’ s ability to regulate the pH value of the cells, the researchers found that the brain of the spinosus is used to maintain a large number of changes in potassium, sodium, chlorine and calcium ions that transmit signals in the carbon dioxide ooze. Corresponding changes are needed to cope with the acidification environment, but differences in the expression of related genes disappear when stress is reduced, and genes return to normal levels of expression.
Further research by the team found that this finch has evolved significantly faster than other fish over the past 15 million years, potentially giving it greater potential to adapt to environmental changes.
It is speculated that this species may have evolved molecular mechanisms to cope with future ocean acidification.

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

How do scientists expect ocean acidification to impact specific fish species?

it will affect their physiology and growth

How does coastal ocean acidification affect shellfish?

How does elevated water acidity affect fish ability to survive?

What factors lead to damage of coral reefs?

Zooplankton, especially key Arctic species, show similar vulnerabilities, which may have cascading effects on marine mammals and higher predators .

Title:

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.

Copyright (C) 2022, ABC Audio. All rights reserved.

Which marine organism is vulnerable to increased levels of ocean acidification?

Which regions are most affected by ocean acidification?

Overall, ocean acidification jeopardizes not only individual species but also the balance and productivity of marine ecosystems, with direct consequences for biodiversity, food security, and global livelihoods .

How do scientists expect ocean acidification to impact specific fish species?