Ocean acidification harms marine life, including cephalopods like cuttlefish, by decreasing water pH levels, making it harder for them to build and maintain their shells and skeletons.

The decrease in pH levels is caused by excess carbon dioxide reacting with water to form carbonic acid, reducing calcium carbonate availability.

Cephalopods, including cuttlefish, are vulnerable to ocean acidification due to their calcium carbonate shells and skeletons.

Pteropods are showing signs of stress due to ocean acidification, with reduced shell growth and increased mortality.

Ocean acidification can have cascading effects on the food web, as pteropods are a key food source for many marine species.

Some fish can rapidly evolve to cope with ocean acidification, but it's unclear if cuttlefish can adapt similarly.

Seagrass meadows and kelp cultivation may help mitigate ocean acidification's effects on some marine species, including possibly cuttlefish.

Ocean warming can significantly impact marine life, affecting distribution, behavior, and physiology.

Cuttlefish, as sentient cephalopods, are likely affected by ocean acidification, though the effects are not well-documented.

More research is needed to understand ocean acidification's impact on cuttlefish and develop effective monitoring strategies.

Ocean acidification can have long-term consequences for marine ecosystems, affecting cuttlefish populations, food webs, and biodiversity.

Reducing greenhouse gas emissions is crucial for preserving marine biodiversity and protecting cuttlefish populations.

International cooperation and research are necessary to address ocean acidification's impacts on marine life, including cuttlefish.

Place-based and integrated SDG actions can help protect cuttlefish and mitigate ocean acidification.

Ocean acidification is a complex issue affecting marine life, including cuttlefish.

Ocean acidification harms marine life, including cephalopods like cuttlefish, by decreasing water pH levels, making it harder for them to build and maintain their shells and skeletons.

Title:

Content: Newswise — When carbon dioxide (CO2) enters the oceans, it can make the water more acidic, which is called ocean acidification. This can make it harder for some ocean creatures, like pteropods, to build and keep their shells. Pteropods are important for the ocean environment.

Pteropods are small sea creatures, including shelled sea butterflies. Not much is known about them because of their size, and they don't survive well in captivity. A team of marine scientists studied the life cycles, abundance, and seasonal changes of shelled sea butterflies in the north-east Scotia Sea, where climate change is happening quickly.

Dr Clara Manno, a researcher at the British Antarctic Survey and the corresponding author of the study published in Frontiers in Marine Science, said that the decrease in pteropod populations in the Antarctic Ocean could have significant consequences for the food web and carbon cycle. She also said that understanding the life cycle of this important organism could help to predict the impact of ocean acidification on the Antarctic ecosystem.

Population stability essential for species survival

To study the life cycle, abundance, and seasonal variability of shelled sea butterflies in the north-east Scotia Sea, a team of marine scientists collected sea butterflies in a sediment trap, a sampling device that was anchored at a depth of 400 meters. Since observing the entire life cycle of sea butterflies in a laboratory setting is impossible, the researchers had to gather information about their spawning, growth rate, and population structure. They were able to reconstruct the sea butterflies' life cycle for a year using the samples from the sediment trap.

The scientists found that the two most commonly collected species, Limacina rangii and Limacina retroversa, have different life cycles and therefore have different levels of vulnerability to changes in the ocean. During the winter months, L. rangii, which is a polar species, can be found as both adults and juveniles, while L. retroversa, a subpolar species, is only found as adults during the winter.

Sea butterflies that exist during the coldest season are more vulnerable to increased levels of ocean acidification. This is because ocean water is more acidic during this season than during other times of the year due to cooler temperatures that increase CO2 dissolution in the ocean. The researchers explained that the life stages of sea butterflies during this time are more exposed and vulnerable to the effects of ocean acidification.

L. rangii has a survival advantage over L. retroversa because both adults and juveniles coexist during winter, which reduces the risk of population instability if one cohort is vulnerable. In contrast, if one cohort is removed from L. retroversa, the entire population could be at risk.

Prolonged exposure is a survival challenge

The researchers pointed out that although the two species are affected differently, both are likely to suffer harm if they are exposed to unfavorable conditions for prolonged periods.

The scientists cautioned that the intensifying and prolonged events of ocean acidification overlap with the spring spawning period, posing a threat to the most vulnerable life stage, the larvae. This could endanger the future populations of sea butterflies.

The research team plans to further study the sea butterflies in the Scotia Sea to see how they would be affected by the increase in the intensity and duration of ocean acidification events. They will study multiyear sediment trap samples to identify potential changes in the life cycle that may occur due to environmental changes. Dr Jessie Gardner of the British Antarctic Survey, lead author of the study, said this will be the next step in their research.

Journal Link: Frontiers in Marine Science

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?

What factors lead to damage of coral reefs?

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

The decrease in pH levels is caused by excess carbon dioxide reacting with water to form carbonic acid, reducing calcium carbonate availability.

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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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What factors lead to damage of coral reefs?

What is the main cause of ocean acidification?

water absorbs carbon dioxide from the atmosphere

Cephalopods, including cuttlefish, are vulnerable to ocean acidification due to their calcium carbonate shells and skeletons.

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

How does coastal ocean acidification affect shellfish?

What do shellfish use to build their shells?

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

Pteropods are showing signs of stress due to ocean acidification, with reduced shell growth and increased mortality.

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

Which ocean creatures have trouble forming shells due to ocean acidification?

Ocean acidification can have cascading effects on the food web, as pteropods are a key food source for many marine species.

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

Which ocean creatures have trouble forming shells due to ocean acidification?

Some fish can rapidly evolve to cope with ocean acidification, but it's unclear if cuttlefish can adapt similarly.

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
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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.

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

Seagrass meadows and kelp cultivation may help mitigate ocean acidification's effects on some marine species, including possibly cuttlefish.

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Content: There were 1,566 press releases posted in the last 24 hours and 464,440 in the last 365 days.

Seagrass meadows as ocean acidification refugia for sea urchin larvae

Higlights

  • Sea urchin larvae were grown at ambient or low pH in tanks with or without plants.
  • Plant photosynthesis increased pH and altered seawater chemistry at both pH levels.
  • Positive effects of plant metabolism on larval development and growth at low pH
  • Seagrass meadows as a tool against climate-driven loss of calcifying species

Abstract

Foundation species have been widely documented to provide suitable habitats for other species by ameliorating stressful environmental conditions. Nonetheless, their role in rescuing stress-sensitive species from adverse conditions due to climate change remains often unexplored. Here, we performed a mesocosm experiment to assess whether the seagrassPosidonia oceanica, through its photosynthetic activity, could mitigate the negative effects of ocean acidification on larval development and growth of the calcifying sea urchinParacentrotus lividus. Sea urchin larvae at early and late developmental stages that are generally associated to benthic habitats, were grown in aquaria with or without P. oceanica plants, under ambient or low pH conditions predicted by the end of the century under the worst climate scenario (RCP8.5). The percentage of abnormal larvae and their total body length under different experimental conditions were assessed on early- (i.e., pluteus; 72 h post-fertilization) and final-developmental stages (i.e., echinopluteus; 30 days post-fertilization), respectively. The presence of P. oceanica increased mean daily pH values of ∼0.1 and ∼0.15 units at ambient and low pH conditions, respectively, compared with tanks without plants. When grown at low pH in association with P. oceanica, plutei showed a ∼23 % reduction of malformations and echinoplutei a ∼34 % increase in total body length, respectively, compared with larvae developing in tanks without plants. Our results suggest that P. oceanica, by increasing pH and altering seawater carbonate chemistry through its metabolic activity, could buffer the negative effects of ocean acidification on calcifying organisms and could, thus, represent a tool against climate-driven loss of biodiversity.

Ravaglioli C., De Marchi L., Giannessi J., Pretti C. & Bulleri F., 2024. Seagrass meadows as ocean acidification refugia for sea urchin larvae. Science of the Total Environment 906: 167465. doi: 10.1016/j.scitotenv.2023.167465. Article.

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Content: Newswise — STONY BROOK, NY, May 25, 2022 – While kelp is known as a nutritious food item for sea creatures and humans alike, harvesting kelp may be a new way to help keep bivalves such as clams and oysters – a more common food source and marine industry staple – healthy and more abundant. A new study led by Christopher Gobler, PhD, and a team of scientists at the Stony Brook University School of Marine and Atmospheric Sciences (SoMAS) shows that the presence of kelp significantly reduces ocean acidification, a result of climate change.

Published in Frontiers in Marine Science, the study also demonstrated that the deployment of kelp on an oyster farm nullifies ocean acidification and therefore protects bivalves against acidification. The process may also have additional ecosystem and aquaculture benefits, including the sequestration and extraction of carbon and nitrogen, and protection against harmful algae blooms.

For shellfish, one of the most serious climate change-related threats is ocean acidification. Carbon dioxide or CO2 levels in Earth’s atmosphere continue to rise, infiltrating oceans where it causes chemical reactions that lower pH and cause ocean acidification. For the past two decades, one of the most robust conclusions of ocean climate change research has been that increasing levels of CO2 in surface waters threaten shellfish that rely on higher pH waters to grow and survive. This threat is particularly acute in coastal zones where additional sources of acidity can further reduce pH and slow shell formation in shellfish, especially bivalves. And while many wild populations of bivalves have collapsed, a burgeoning wave of aquaculture in the U.S. and around the World has caused the global production of seafood via aquaculture to grow and now exceed wild capture.

“Despite this wave of aquaculture, the intensification of ocean acidification now threatens bivalve aquaculture and has necessitated a solution,” explains Professor Gobler, the Endowed Chair of Coastal Ecology and Conservation at SoMAS.  “We believe our work is foundational to a solution.”

In the study, titled “Kelp (Saccharina latissima) Mitigates Coastal Ocean Acidification and Increases the Growth of North Atlantic Bivalves in Lab Experiments and on an Oyster Farm,” Professor Gobler and colleagues conducted six experiments to assess the effects of elevated CO2 and presence of kelp (S. latissima) on the growth rates of three different species of bivalves: (Eastern oysters (Crassostrea virginica), blue mussels (Mytilus edulis), and hard clams / Northern quahogs (Mercenaria mercenaria).

In each of the experiments, acidification was significantly reduced with the cultivation of kelp. They furthered the research with the ultimate test – a field experiment at the Great Gun oyster farm in Moriches Bay, New York.

They found that during a one-month deployment, oysters that were surrounded by kelp enjoyed higher pH water and grew significantly faster than individual shellfish located further away where the pH of the water was significantly lower.

Professor Gobler and colleagues emphasize that these findings have powerful implications for oyster farming in coastal zones.

“We have been witnessing coastal ocean acidification for years and have documented its ability to slow the growth, and even kill off, shellfish. We began growing kelp on oyster farms to simply expand aquaculture, regionally. After seeing its ability to rapidly take up CO2 and improve low pH conditions, we knew it had the potential to benefit shellfish experiencing acidification. And while showing that in the lab was exciting, being able to improve the growth of oysters on an oyster farm experiencing coastal acidification proves this approach can have very broad applications,” explains Professor Gobler.

Overall, the research clearly shows, according to the authors, that “the cultivation of kelp constitutes an environmentally friendly means of protecting shellfisheries against present and future ocean acidification and other coastal stressors.”

Building on the work, helping the oyster farms

“We’ve helped grow kelp on 10 oyster farms across New York since 2018 and more and more aquaculturists have been hoping to incorporate kelp into their farms,” says Mike Doall, Associate Director of Shellfish Restoration and Aquaculture at Stony Brook University. “In addition to providing crop diversification and additive revenue streams, the ability of kelp to fight ocean acidification gives these oyster farmers one more reason to add kelp as a second crop.”

The recent study builds on other research by the same SoMAS group, which published a study in Harmful Algae in 2021. That study demonstrated that kelp has the ability to deter the intensity of harmful algal blooms, another environmental threat to shellfish aquaculture.

Such scenarios with kelp appear to create a win-win scenario for oyster farmers like Paul McCormick, owner of the Great Gun oyster farm where the current study was performed.

“Kelp looks to be the perfect complement to oysters on my farm,” says McCormick. “It grows during winter and spring, when the oysters need less attention, and there is lots of interest in kelp from restaurants. If it is offering protection to my oysters against poor water quality, well that’s another good reason to add it to my farm.”

Citations:

Young, C. S., Sylvers, L. H., Tomasetti, S. J., Lundstrom, A., Schenone, C., Doall, M. H., & Gobler, C. J. (2022) Kelp (Saccharina latissima) mitigates ocean acidification and increases the growth of North Atlantic bivalves in lab experiments and on an oyster farm. Frontiers in Marine Science, Volume 9 | Article 881254

Sylvers, P. H., & Gobler, C. J. (2021). Mitigation of harmful algal blooms caused by Alexandrium catenella and reduction in saxitoxin accumulation in bivalves using cultivable seaweeds. Harmful Algae, 105, 102056.

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

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

Ocean warming can significantly impact marine life, affecting distribution, behavior, and physiology.

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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.

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What factors lead to damage of coral reefs?

Cuttlefish, as sentient cephalopods, are likely affected by ocean acidification, though the effects are not well-documented.

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Cooked crabs, octopuses and lobsters will be illegal, UK report says they are so afraid of pain
The study found that octopuses have a "very strong" ability to sense.
(AFP file photo)
2021 / 11 / 23 15: 09
When eating seafood, such as lobster, crab, shrimp, etc., people like to throw live them into hot water to cook, I want to say that this is the only way to eat fresh, octopus is even more delicious in South Korea.
But a new report from the UK shows that octopuses, crabs and lobsters can feel pain or distress.
Under new animal welfare laws, the UK government has added octopus, crabs and lobsters to its list of protected “sentient beings ”.
The report, conducted by experts at the London School of Economics through an evaluation of 300 scientific studies, concluded that cephalopods (such as octopus, squid and cuttlefish) and complete animals (such as crabs, lobsters and small lobsters) should be considered sentient beings.
In the Animal Welfare Sentience Bill being discussed in the UK, vertebrates are already classified as sentient animals.
The bill would require any restaurant or chef to ban "live cooking" of such animals in order to startle them or freeze them quickly, in a more humane manner and to reduce their suffering.
The bill, which has not yet become law, requires the UK to set up an animal awareness committee to issue a number of situational reports on the welfare of sentient animals.
The previous report used eight different methods to measure perception, including the ability to learn, the presence of pain receptors, the connection between pain receptors and specific brain regions, the response to anesthesia or analgesics, and behavior, including balancing the return of threats and opportunities, and protection from harm or threat.
Octopuses have a "very strong" perception, and most crabs also have a "strong" perception, the study found.
Netflix ’ s recent documentary, My Octopus Teacher, also showcases the unique abilities of octopuses.
The brain structure of an octopus is very different from that of a human, but it has some of the same functions as the mammalian brain, such as the ability to learn, including the ability to solve problems, and possibly the ability to dream.
As early as 2018, the Swiss government took an earlier step to amend the new law to prohibit live cooking of seafood with shells, and also to require restaurant operators to cook lobster only by electric shock or removal of the lobster head before cooking.
The United Kingdom will legislate to ban the cooking of "live cooked" lobster on humanitarian grounds.
Illustration. (Associated Press)
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How do scientists expect ocean acidification to impact specific fish species?

it will affect their physiology and growth

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

More research is needed to understand ocean acidification's impact on cuttlefish and develop effective monitoring strategies.

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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 can have long-term consequences for marine ecosystems, affecting cuttlefish populations, food webs, and biodiversity.

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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

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

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

Reducing greenhouse gas emissions is crucial for preserving marine biodiversity and protecting cuttlefish populations.

Title:

Content: Scientists warn of what could lead to a “mass extinction ” of marine life that“ rivals ” the severity of the Great Death!
The Libyan Observatory Newspaper
A new study has revealed that greenhouse gas emissions could lead to mass extinctions of marine life to levels not seen since before the dinosaurs.
Researchers in New Jersey modeled the future extinction risk of marine life in all of the world's oceans under different projected climate scenarios.
If emissions are not curbed, the loss of marine species due to global warming and oxygen depletion could reverse the “Great Death, ” the most serious extinction event on Earth, by about 2100, they say.
The Great Death, known as the deadliest extinction on Earth, saw the loss of 95% of all marine species when it occurred about 250 million years ago.
It can also match other major extinction events in Earth's history, including the mass extinction at the end of the Cretaceous that killed the dinosaurs 66 million years ago.
According to the researchers, tropical waters will face the greatest loss of biodiversity, while polar species are more at risk of extinction.
On a more positive note, experts say reversing greenhouse gas emissions could reduce the risk of extinction by more than 70 percent.
Lead author Justin Penn, at Princeton University ’ s Department of Earth Sciences, said: “The bright side is that the future is not written in stone.
The scale of the extinction we have discovered depends heavily on the amount of carbon dioxide [CO2] we release going forward.
“There is still enough time to reverse the trajectory of CO2 emissions and prevent the magnitude of warming that could cause this mass extinction. ”
The Great Death marks a period when life on Earth has never been so close to extinction without recovery, either before or after.
When carbon dioxide dissolves in the oceans, it becomes extremely acidic and the level of oxygen in the water drops, killing marine life.
Scientists have long debated theories of the cause of extinction ranging from meteorite impact to volcanoes, which could have caused climatic and environmental changes that make the Earth uninhabitable.
But in the event of the next mass extinction, history will directly blame anthropogenic greenhouse gas emissions.
For the study, Ben and co-author Curtis Deutsch, also based at Princeton, combined existing data on marine species with climate change models to predict how changes in habitat conditions will affect their survival.
The experts compared their model to the size of the “Big Five, ” five historical mass extinctions recorded in the fossil record, among them the“ Great Death. ”
The researchers say that with global temperatures rising “as usual, ” marine life is likely to be subjected to a mass extinction that could potentially rival the size and severity of the Great Death.
Since the Great Death is the deadliest extinction event on Earth, the next marine extinction is likely to surpass the other four species.
Among the events, they found a common pattern – as the ocean warms and oxygen availability decreases, there is a clear decline in the abundance of marine life.
Water temperature and oxygen availability are key factors that will change as the climate warms due to human activity.
Warm water is not only a risk factor for species adapted to cold climates; it also contains less oxygen than cold water, slowing ocean circulation further and reducing the supply of oxygen at depth.
Paradoxically, the metabolic rates of the species increase as the water warms, and therefore the demand for oxygen rises as the supply decreases.
“Once the oxygen supply is less than what a species needs, we expect to see significant species losses, ” he said.
Experts say marine animals have physiological mechanisms that allow them to adapt to environmental changes, but only to a certain extent.
The researchers found that polar species are more likely to become extinct globally if climate warming occurs because they will not have suitable habitats to move to.
Tropical marine species are likely to be better off because they have traits that allow them to cope with warm, low-oxygen waters in the tropics.
To determine the relative importance of climate in the occurrence of extinctions, the team also compared future extinction risks from climate warming with data from the International Union for Conservation of Nature (IUCN) on current threats to various marine animals.
They found that climate change currently affects 45% of marine species at risk of extinction, but is only the fifth most important stressor after overfishing, transport, urban development and pollution.
However, Ben said climate change could soon overcome all these stressors in importance.
"Extreme warming will lead to climate-induced extinctions, which, towards the end of the century, will compete with all current human pressures combined," he said.
The study, “Avoiding mass extinction of oceans due to climate warming, ” was published in the journal Science.
Source: Daily Mail

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

International cooperation and research are necessary to address ocean acidification's impacts on marine life, including cuttlefish.

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

it will affect their physiology and growth

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

Place-based and integrated SDG actions can help protect cuttlefish and mitigate ocean acidification.

Title:

Content: There were 1,357 press releases posted in the last 24 hours and 396,480 in the last 365 days.

Integrated actions across multiple sustainable development goals (SDGs) can help address coastal ocean acidification

Integrated actions across multiple sustainable development goals (SDGs) can help address coastal ocean acidification

Published 17 June 2024 Science Leave a Comment
Tags: policy, review

The Sustainable Development Goals (SDGs) adopted by the United Nations in 2015 constitute a set of 17 global goals established as a blueprint for achieving a more sustainable and equitable world for humanity. As part of the SDGs, target 14.3 is focuses on minimizing and addressing the impacts of Ocean Acidification (OA). We argue that moving forward in meeting the targets related to pH levels in the coastal ocean can be facilitated through accounting for various drivers of pH change, which are associated with advancing a suite of SDG goals. Addressing ‘coastal acidification’ via a suite of linked SDGs may help avoid inaction through connecting global phenomena with local impacts and drivers. This in turn can provide opportunities for designing novel place-based actions or partnerships that can aid and provide synergies for the joint implementation of programs and policies that tackle a suite of SDGs and the specific targets related to coastal ocean pH.

Vargas C. A. & Gelcich S., 2024. Integrated actions across multiple sustainable development goals (SDGs) can help address coastal ocean acidification. Communications Earth & Environment 5: 319. doi:10.1038/s43247-024-01485-6. Article.

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Ocean acidification is a complex issue affecting marine life, including cuttlefish.

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Content: A submarine is tracking CO2 in the ocean.
01 / 06 / 2022 | 05: 45 - Source: The Morning
(This Day's News Encyclopedia | Iraq News) - Mark Thyssen
Translated by: Bahaa Salman
In the cold, choppy waters of Easter Bay in Alaska, all eyes were staring at the gray waters, looking for just one thing.
It wasn ’ t a fountain flowing from humpback whales active in this magnificent fjord, or a beaver lazily relaxing on the water ’ s surface.
Instead, everyone on board the Nanoc, the research ship of the University of Alaska Fairbanks, was looking at where the tiny 1.52 meter submarine used under the sea (Sea Glider) for research appeared.
The submarine, believed to be the first to be equipped with a large sensor to measure carbon dioxide levels within the ocean, had just completed its first night mission.
Designed to dive up to 1,000 meters, roaming parts of the ocean far away, the autonomous vehicle was placed in the Gulf of Alaska this spring to provide a deeper understanding of the chemistry of the sea in the era of climate change.
The research may be a major step toward monitoring ocean greenhouse gases, because until now, carbon dioxide concentrations to determine ocean acidity have been measured mostly by ships, buoys and moorings tied to the ocean floor.
“Ocean acidification is a process by which humans release carbon dioxide into the atmosphere because of burning fossil fuels and changing land uses, ” says Andrew McDonnell, an oceanographer at the University of Alaska Fairbanks ’ School of Oceanography.
The oceans provide a valuable service by containing some of the carbon dioxide.
Otherwise, there would be too much of it in the atmosphere, absorbing the sun ’ s heat and raising the planet ’ s warmth.
“But the problem now is that the ocean is changing its chemistry because of this absorption, ” says Claudine Hawrie, an oceanographer at the University ’ s International Center for Arctic Research.
The vast amount of data collected to study ocean acidification that can harm and kill specific species of marine life is currently under review.
For several weeks this spring, the couple, Claudine and Andrew, worked with engineers from Kepers Subsea Services, which equipped the research submarine, and with a German company, 4H-Jena, which supplied the sensor attached to the submarine.
On most days, researchers have gone too far into Easter Bay from the coast of Seward to conduct tests.
After the first mission, the research submarine was towed to the ship.
The sensor is then pulled out of the submarine and quickly sent to the ship ’ s cabin to upload its data, and the sensor analyzes carbon dioxide, records the data and stores it within a temperature-controlled system.
Many sensor components use battery power to perform their work.
As far as industrial standards are concerned, this sensor is the same as any other vessel or laboratory measuring CO2.
Claudine says the use of this new technology was “a huge step towards accommodating such an avid enthusiast, and that ’ s what characterizes the current project. ”
Associated Press
Note: The content entitled "A submarine tracking CO2 in the ocean" was first published on the Al-Sabah website and this day's news encyclopedia does not bear its content in any way.
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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?

What factors lead to damage of coral reefs?

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