I shall first put
The concept of ocean acidification is a recent phenomenon For the Ocean Acidification Database see
This set the scene for future
Proponents of this hypothesis demonize carbon dioxide further by claiming that increasing carbon dioxide causes the ocean to become more
This despite the fact that the oceans are alkaline, with a pH about 8.2, and have been alkaline throughout their existence on Earth. We are implored to reduce the production of anthropogenic carbon dioxide to
In this article, I show that such claims are baseless, and indeed that carbon dioxide is beneficial to the ocean.
The carbonic acid then allegedly
In words, carbon dioxide reacts with calcium oxide to make calcium carbonate, which
pH is a measurement of the amount of hydrogen ion concentration in a solution, the log of the hydrogen ion concentration with the sign changed. Because it is a log scale, it is very hard to move a pH of 8.2 to 7.0, which is neutral. The pH needs to be less than 7 to be
One of the factors affecting ocean pH is photosynthesis by plants. Experimental results show that plants grow better if CO2 is increased, and greenhouse managers commonly increase the CO2 artificially to increase crops, often by 30% or more. There is every reason to suppose that marine plants also thrive if CO2 is increased. There is also experimental evidence that carbonate secreting animals thrive in higher CO2. Herfort et al. (2008) concluded that the likely result of human emissions of CO2 would be an increase in oceanic CO2 that could stimulate photosynthesis and calcification in a wide variety of corals.
The pH scale is shown in Figure 1, which shows the generally accepted average seawater pH of 8.2 and the pH of a few other substances for comparison. The pH of seawater can be very variable. Ocean pH varies regionally by 0.3, and also seasonally in a particular location by 0.3. Rhodes Fairbridge told me that he found the day-night variation in a coral pool was 9.4 to 7.5 (personal comm.).
Fig. 1
Position of oceanic waters on the pH scale.

Marine life, including that part that fixes CO2 as the carbonate in limestones such as coral reefs, evolved on an Earth with CO2 levels many times higher than those of today, as reported by Berner and Kothavala (2001). It may be true to say that today’s marine life is getting by in a CO2-deprived environment.
As just one example of the alarmist approach the Great Barrier Reef Marine Park Authority predicts that oceanic pH may decrease by as much as 0.4 of a pH unit by 2100 and that
this will be disastrous for coral calcification. However, that oceanic pH would then be about 7.8, which is still alkaline and corals can flourish at this pH. A sample from next to a
The current use by alarmists of
Chemical equilibrium is a bit too complex to describe here, but some of the Alarmists make use of it to create scares. Gasutto and Hansson (2011) edited a book called
Calcite is fixed by oysters, foramanifera and coccolithophores amongst others, and aragonite by corals, mussels and clams and others, so what is the problem? One problem, perhaps, is that despite the waters being supersaturated, bubbling carbon dioxide causes further increase biological activity, described later. Maybe carbon dioxide is not involved and the emissions contain other nutrients.
There is another factor called Henry’s Law, which states that the amount of dissolved gas in a liquid is proportional to its partial pressure above the liquid (Henry 1803). One effect is that cold water can hold more CO2 than warm, so if you warm saturated water it gives off CO2. You can see the effect if you warm a glass of fizzy drink: it goes flat. The ocean-air interface is usually rough so interchange is rapid. Actually if the aim of the Anthropogenic Global Warming activists is to keep the world cooler by reducing atmospheric CO2 they are going in the direction of decreasing alkalinity, or in their terms increasing
It is important to note the dissolution of CO2 in water is governed by Henry’s Law, evidenced by the fact there is approximately 50 times more CO2 dissolved in the ocean than in the atmosphere at present. It is this vast mass of dissolved CO2 in the ocean that holds the regulating power—not the relatively small amount of CO2 contained in the air.
Furthermore, the chemical reaction speeds involved in the dissolution of CO2 are high, as is the ocean circulation speed in the upper parts of the ocean. The ocean acidification hypothesis also ignores the presence of vast amounts of dissolved calcium in the ocean: the upper 200 m of ocean water contains enough dissolved calcium to bind all anthropogenic CO2 as precipitated calcium carbonate (in the ocean) without affecting the ocean’s pH (Segalstad 2014).
The story of pH measurement is not as clear as one might hope. Scientists have had pH meters and measurements of the oceans for over one hundred years. Doogue and Nova (2015) present the data, and note that overall the trend is messy but more up than down, and
At the centre of the scandal is the National Oceanic and Atmospheric Administration (NOAA), the United States federal scientific agency which measures and researches changes in the oceans and atmosphere. One of NOAA’s departments – the Pacific Marine Environmental Laboratory (PMEL ) – also happens to be one of the mainstays of the alarmist story of
Feely and Sabine (2004), two of PMEL’s senior oceanographers, wrote a paper often cited in support of
But further investigation by Wallace (2015) shed doubt on these conclusions. While studying a chart produced by Feely and Sabine, Wallace noticed that some key information had been omitted. The chart only began in 1988, but Wallace knew that there were oceanic pH measurements dating back to at least 100 years earlier. He wondered why this solid data had been ignored, in favour of computer-modelled projections. Wallace (2015) asked Feely and Sabine why. Sabine replied that it was inappropriate for Wallace to impugn the
Many marine organisms need CO2 to make their coral skeletons, carbonate shells and so on. Corals also have symbiotic plants within their flesh that use CO2 in photosynthesis. Marine life flourishes where CO2 is abundant. Starck (2010) described the relationship between organisms and pH at two carbon dioxide
A study of seawater pH near active volcanic CO2 vents in the Mediterranean (Kerrison et al. 2011) found that the pH immediately adjacent to the vent was still alkaline, despite being subjected to the equivalent of nearly 5,600 ppm CO2. Other such sites are known around the world, such as the Champagne Reef, a premier diving site in Dominica, which is reported to be
As the modern investigation into the potential impacts of increasing carbon dioxide in seawater on marine life continues, one narrative is beginning to emerge across the scientific literature, which is that rising atmospheric CO2 concentrations will likely
In a comprehensive analysis of experimental studies that explored the effects of rising atmospheric CO2 concentrations on marine biota, Hendriks et al. (2010) assembled a database of 372 experimentally evaluated responses of 44 different marine species to ocean acidification that was induced by equilibrating seawater with CO2-enriched air. This they did
A significant contribution was made by McCulloch et al. (2017) who studied
There is a completely fake argument used by alarmists including NASA implying that coral bleaching is caused by carbon dioxide. Bleached coral is perfectly normal, and occurs when wave driven mixing ceases during periods of extended calm associated with unusual warming of the surface 1–2 m of seawater. The reef recovers in a few years by recolonization.
Minor amount of carbonate are found in many areas, such as small shelly beaches, but some areas with massive accumulation are much more important in global limestone production. Coral reefs are a major one, and data on this is presented below with the Great Barrier Reef as a prime example. Elsewhere there are exceptionally large accumulations of carbonate sands. Bourman et al. (2016) provide a good recent example of a study of such deposits from South Australia. The coasts are dominated by carbonate sands in the form of beaches and dunes. The authors frequently refer to the
In Gulf St Vincent seagrasses thrive with extremely productive calcareous algae, foraminifers and molluscs manufacturing vast amounts of calcareous sediment. The dominant processes of coastal development in Spencer Gulf are related to the massive production and accumulation of biogenic skeletal carbonate fragments derived from coralline algae, foraminifers, molluscs and bryozoans; the site is a major carbonate factory sequestering much CO2.
The iconic Great Barrier Reef is one of the best-known features of Australia, and we are constantly told it is in danger. The Australian Government’s Great Barrier Reef Marine Park Authority (2019) claimed:
Another example is provided by Albright et al. (2016) who claim their research shows, the reduction in seawater pH – caused by carbon dioxide from human activities such as burning fossil fuels – is making it more difficult for corals to build and maintain their skeletons. Possibly the greatest danger to the Great Barrier Reef is the huge amount of money, tens of millions of dollars, made available for research on the reef. This has led to a feeding-frenzy of people wanting to use the money, who maintain that the reef is in danger, to keep the money flowing.
David Barnes has spent many hours measuring the pH in all parts of the reef. He tells me ...
The Great Barrier Reef has been able to re-establish itself repeatedly during high sea level episodes associated with major environmental fluctuations in sea level, temperature and CO2 over the past several hundred thousand years. The Great Barrier Reef complex goes back about two million years, but the reef, as we know it is only about 10,000 years old. Before that, there were huge changes in climate and sea level. Where the Great Barrier Reef complex is from tens to over a hundred Km in width today, it was reduced to a narrow fringing reef along the edge of a vast coastal plain during the last glacial period. It was not great and was not a barrier reef. It also experienced earlier glacial periods, with sea level falls. The Great Barrier Reef has survived many wide changes in environmental conditions, yet still ocean acidification is singled out by alarmists as the great threat to the reef.
Marine life depends on CO2, and some plants and animals fix it as limestone, which is not generally re-dissolved. Marine life, including that part that fixes CO2 as the carbonate in limestones such as coral reefs, evolved on an Earth with CO2 levels many times higher than those of today, as reported by Berner and Kothavala (2001). It may be true to say that today’s marine life is surviving in a CO2-deprived environment. Over geological time enormous amount of CO2 have been sequestered by living things, so that today there is far more CO2 in limestones than in the atmosphere or ocean waters. This sequestration of CO2 by living things is far more important than trivial additions to the atmosphere caused by human activity. Carbon dioxide in seawater does not dissolve coral reefs or other marine limestones, but is essential to their survival.
In the grand geochemical cycle, carbon dioxide originates from volcanic eruptions and is fixed by limestone formation in the sea. Whether the Earth started as a hot or cold body, any primordial gas would have escaped. Volcanic eruptions produced the gases, including water, which formed the oceans, and carbon dioxide which formed 98% of the original atmosphere. The evolution of life changed that. When photosynthesis started, more and more oxygen was introduced into the atmosphere (which changed the course of rock weathering), and when carbonate secretion arrived in the late Precambrian, limestone deposition started to sequester CO2. The production of limestone became significant in the late Precambrian, and has increased through geological time.
Most modern reef coral genera have fossil histories going back from 5–10 million years to over 100 million years. They have survived both ice ages and very warm periods, and times when CO2 was at 5–10 times current levels.
Contrary to popular belief, at 400 parts per million (0.04%), CO2 is lower now in the atmosphere than it has been during most of the 550 million years since modern life forms emerged during the Cambrian period. CO2 was about 10 times higher than it is today. Corals and shellfish evolved early and have obviously managed to survive through eras of much higher CO2 than present levels. Finally, it is a fact that people who have saltwater aquariums sometimes add CO2 to the water in order to increase coral growth and to increase plant growth.
The truth is CO2 is the most important food for all life on Earth, including marine life. It is the main food for photosynthetic plankton (algae), which in turn is the start for the entire food chain in the sea. On top of this, some marine organisms use CO2 to produce their skeletons of calcium carbonate.
Marine life depends on CO2, and some plants and animals fix it as limestone, which is not generally re-dissolved. Over geological time enormous amount of CO2 have been sequestered by living things, so that today there is far more CO2 in limestones than in the atmosphere or ocean. This sequestration of CO2 by living things is far more important than trivial additions to the atmosphere caused by human activity.
The
Fig. 1

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