Introduction
As global warming morphs into climate change and anthropogenic CO2 emissions give way to the Sun, the stars and our oceans as the primary drivers of climate change, environmental extremists like Al Gore are raising a new CO2-driven ecological disaster scenario to hysterical levels: Ocean acidification. Claims have been made that oceanic pH levels have declined from ~8.2 to ~8.1 since the mid-1700’s. This pH decline (acidification) has been attributed to anthropogenic CO2 emissions – This should come as no surprise because the pH estimates are largely derived from atmospheric CO2 concentrations (Orr et al., 2005). It has also been postulated that anthropogenic CO2 emissions will force an additional 0.7 unit decline in oceanic pH by the year 2100 (Caldeira et al., 2003).
Alarmist organizations like the National Resources Defense Council are hard at work extrapolating these oceanic pH model predictions into ecological nightmares…
Scientists predict the Arctic will become corrosive to some shelled organisms within a few decades, and the Antarctic by mid-century. This is pure chemistry; the vagaries of climate do not apply to this forecast.
OA is expected to impact commercial fisheries worldwide, threatening a food source for hundreds of millions of people as well as a multi-billion dollar industry. In the United States alone, ocean-related tourism, recreation and fishing are responsible for more than 2 million jobs.
Shellfish will be affected directly, thus impacting finfish who feed on them. For example, pteropods—tiny marine snails that are particularly sensitive to rises in acidity— comprise 60 percent of the diet for Alaska’s juvenile pink salmon. And this affects diets farther up the food chain, as a diminished salmon population would lead to less fish on our tables.
Coral reefs will be especially hard hit by ocean acidification. As ocean acidity rises, corals will begin to erode faster than they can grow, and reef structures will be lost worldwide. Scientists predict that by the time atmospheric CO2 reaches 560 parts per million (a level which could happen which could happen by mid-century; we are currently nearing 400 ppm), coral reefs will cease to grow and even begin to dissolve. Areas that depend on healthy coral reefs for food, shoreline protection, and lucrative tourism industries will be profoundly impacted by their loss.
This sounds like a serious threat… As have all of the other alarmist clarion calls to halt capitalism in the name of the most recent environmental causes célèbres. Since all of the previous environmental extremist causes célèbres have proven to be totally without merit, it’s a fair assumption that Ocean Acidification might also be lacking in merit. Just to be fair, before pitching Ocean Acidification into the dustbin of junk science along with Anthropogenic Global Warming, Ozone Holes, DDT, etc., let’s look at the science.
The answers to the following questions will tell us whether or not CO2-driven ocean acidification is a genuine scientific concern:
- Is atmospheric CO2 acidifying the oceans?
- Is there any evidence that reefs have been damaged by CO2-driven ocean acidification and/or global warming?
- Does the geological record support the oceanic acidification hypothesis?
Is atmospheric CO2 acidifying the oceans?
Before we can answer this question, we have to understand a bit about how the oceans make limestone and other carbonate rocks. The Carbonate Compensation Depth (CCD or Lysocline) is the depth at which carbonate shells dissolve faster than they accumulate. That depth is primarily determined by several factors…
-Water temperature
-Depth (pressure)
-CO2 concentration
-pH (high pH values aid in carbonate preservation)
-Amount of carbonate sediment supply
-Amount of terrigenous sediment supply
Calcium carbonate solubility increases with increasing carbon dioxide content, lower temperatures, and increasing pressure.
SOURCE
What evidence do we have that the lysocline or CCD has been becoming shallower or that the oceans have been acidifying over the last 250 years? The answer is: Almost none.
From Pelejero et al., 2005…
The actual trend and range of natural variability in oceanic pH remains largely unknown, yet it is crucial to understand the possible consequences of acidification on marine ecosystems. A reliable proxy record is needed to assess long-term trends and variability in seawater pH. Instrumental records of the seawater CO2 system, such as those collected at the Hawaii Ocean Time Series Station, which only commenced in 1989 (12), are short. In this Report, we present a reconstruction of seawater pH spanning the last three centuries, based on the boron isotopic composition ( 11B) (13) of a long-lived massive coral (Porites) from Flinders Reef in the western Coral Sea…
[...]

Pelejero et al., 2005, Fig. 2. Record of Flinders Reef coral 11B, reconstructed oceanic pH, aragonite saturation state, PDO and IPO indices, and coral calcification parameters. (A) Flinders Reef coral 11B as a proxy for surface-ocean pH (24); 11B measurements for all 5-year intervals are available in table S1. (B) Indices of the PDO (28, 39) and the IPO (27) averaged over the same 5-year intervals as the coral pH data. Gray curves in panels (A) and (B) are the outputs of Gaussian filtering of coral pH and IPO values, respectively, at a frequency of 0.02 ± 0.01 year–1, which represent the 1/50-year component of the pH variation (fig. S2). (C) Comparison of high-resolution coral Sr/Ca (plotted to identify the seasonal cycle of SST) (32), 11B-derived pH, and wind speed recorded at the Willis Island meteorological station (data from the Australian Bureau of Meteorology) (40). Note the covariation of wind speed and seawater pH; strong winds generally occur at times of high pH, and weak winds generally occur at times of low pH. All high-resolution 11B measurements are available in table S2. (D) Aragonite saturation state, , where is the stoichiometric solubility product of aragonite, calculated from our reconstructed pH assuming constant alkalinity (24). (E) Coral extension and calcification rates obtained from coral density measured by gamma ray densitometry (38).
[...]
Although the lowest 11B value for the entire record corresponds to the 5-year average around 1988 [23.0 per mil ( ), 7.91 pH units; Fig. 2A and table S1], there is no notable trend toward lower 11B values. The dominant feature of the coral 11B record is a clear interdecadal oscillation of pH, with 11B values ranging between 23 and 25 (7.9 and 8.2 pH units; Fig. 2A). Spectral analysis of the coral pH record demonstrates a substantial cyclicity of about 50 years (Fig. 2A and fig. S2). Moreover, the variation in pH is synchronous with the Interdecadal Pacific Oscillation (IPO) (27), the Pacific-wide equivalent of the Pacific Decadal Oscillation (PDO) (28), which is also well represented by a 50- to 70-year cyclicity (29) (Fig. 2B and fig. S2). The IPO is well represented by a spatial pattern of sea surface temperature (SST) anomalies over the Pacific Ocean, such that the index is positive when the equatorial Pacific is warm and the southwest Pacific and central North Pacific are cold. This pattern of interdecadal climate variability shares similarities with the El Niño-Southern Oscillation (ENSO), with periods of positive and negative IPO values displaying climatic patterns similar to El Niño and La Niña, respectively (30, 31).
Rather than finding a secular trend of declining pH (ocean acidification), Pelejero et al. found that oceanic pH changes cyclically along with the Pacific Decadal Oscillation and El Niño/La Niña cycle. So there really is no solid evidence that the oceans have been acidifying since mankind started to burn fossil fuels.
Is there any evidence that reefs have been damaged by CO2-driven ocean acidification and/or global warming?
Using the data from Pelejero et al., 2005, I found no correlation between pH and reef calcification rates…

Flinders Reef: Calcification Rate vs. pH (Pelejero et al., 2005)
On top of that… There is solid evidence that elevated atmospheric CO2 levels have actually caused carbonate deposition to increase over the last 220 years (
Iglesias-Rodriguez et al., 2008)…

Iglesias-Rodriguez et al., 2008, Fig. 4. Average mass of CaCO3 per coccolith in core RAPID 21-12-B and atmospheric CO2. The average mass of CaCO3 per coccolith in core RAPID 21-12-B (open circles) increased from 1.08 x 10–11 to 1.55 x 10–11 g between 1780 and the modern day, with an accelerated increase over recent decades. The increase in average pre="average ">coccolith mass correlates with rising atmospheric PCO2, as recorded in the Siple ice core (gray circles) (26) and instrumentally at Mauna Loa (black circles) (38), every 10th and 5th data point shown, respectively. Error bars represent 1 SD as calculated from replicate analyses. Samples with a standard deviation greater than 0.05 were discarded. The smoothed curve for the average coccolith mass was calculated using a 20% locally weighted least-squares error method.
And when sudden increases of atmospheric CO2 have been tested under laboratory conditions, “otoliths (aragonite ear bones) of young fish grown under high CO2 (low pH) conditions are larger than normal, contrary to expectation” (Checkley et al., 2009).
There is no evidence to support the notion that rising atmospheric CO2 levels have ever caused ocean acidification… And the hypothesis has been falsified under empirical conditions.
Does the geological record support the oceanic acidification hypothesis?
The Paleocene-Eocene Thermal Maximum (PETM) was a period of significant global warming approximately 55 million years ago and has often been cited as a geological analogy for the modern threat of ocean acidification. There is solid evidence that the Lysocline “shoaled” or became shallower for a brief period of time during the PETM. Several cores obtained from the Walvis Ridge area in the South Atlantic during Ocean Drilling Program (ODP) Leg 208 contained a layer of red clay at the P-E boundary in the middle of an extensive carbonate ooze section (Zachos et al., 2005). This certainly indicates a disruption of the lysocline during the PETM; but it doesn’t prove that it was ocean acidification.
The PETM was a period of extensive submarine and subaerial volcanic activity (Storey et al., 2007) and pedogenic carbonate reconstructions do support the possibility that seafloor methane hydrates released by that volcanic activity may have sharply increased oceanic CO2 saturation.
But… The terrigenous paleobotanical evidence does not support elevated atmospheric CO2 levels during the PETM (Royer et al., 2001). The SI data indicate CO2 levels in North America to have been between 300 and 400 ppmv during the PETM.
So, the PETM may have been an example of ocean acdification… But there is NO evidence that it was caused by a sharp increase in atmospheric CO2 levels.
Some have asserted that there is no geological precedent; claiming atmospheric CO2 concentrations have risen faster in the last 150 years than at any time in recent geological history. Ice core-derived CO2 data certainly do indicate that CO2 has not risen above ~310 ppmv at any point in the last 600,000 years and that it varies little at the decade or century scale. However, there are other methods for estimating past atmospheric CO2 concentrations.
Plants “breath” CO2 through microscopic epidermal pores called stomata. The density of plant stomata varies inversely with the atmospheric partial pressure of CO2. Several recent studies of plant stomata from living, herbarium and fossil samples of plant tissue have shown that atmospheric CO2 fluctuations comparable to that seen in the industrial era have been fairly common throughout the Holocene and Recent times.
Plant stomata measurements reveal large variations in atmospheric CO2 concentrations over the tast 2,000 years that are not apparent in ice core data (Kouwenberg, 2004)…

Kouwenberg (2004) Figure 5.4: Reconstruction of paleo-atmospheric CO2 levels when stomatal frequency of fossil needles is converted to CO2 mixing ratios using the relation between CO2 and TSDL as quantified in the training set. Black line represents a 3 point running average based on 3–5 needles per depth. Grey area indicates the RMSE in the calibration. White diamonds are data measured in the Taylor Dome ice core (Indermühle et al., 1999); white squares CO2 measurements from the Law Dome ice-core (Etheridge et al., 1996). Inset: Training set of TSDL response of Tsuga heterophylla needles from the Pacific Northwest region to CO2 changes over the past century (Chapter 4).
Century-scale fluctuations in atmospheric CO2 concentrations have also been demonstrated in the early Holocene (Wagner et al., 1999)…

(Wagner et al., 1999)Fig. 1. (A) Mean SI values (±1 ) for B. pendula and B. pubescens from the early Holocene part of the Borchert section (Netherlands; 52.23°N, 7.00°E) and reconstructed CO2 concentrations. The scale of the section is in centimeters. Three lithological (Lith.) units can be recognized (18): a basal gyttja (=), succeeded by Drepanocladus peat (//), which is subsequently overlain by Sphagnum peat ( ). Six conventional 14C dates (in years before the present) are available (indicated by circled numbers): 1, 10,070 ± 90; 2, 9930 ± 45; 3, 9685 ± 90; 4, 9770 ± 90; 5, 9730 ± 50; and 6, 9380 ± 80. Summary pollen diagram includes arboreal pollen (white area) with Pinus ( ) and with Betula ( ) and nonarboreal pollen with Gramineae ( ) and with Cyperaceae, upland herbs, and Ericales ( ). Regional climatic phases after (18): YD, Younger Dryas; Fr., Friesland phase; Ra., Rammelbeek phase; and LP, Late Preboreal. For analytical method, see (13). Quantification of CO2 concentrations according to the rate of historical CO2 responsiveness of European tree birches (Fig. 2). P indicates the reconstructed position of the Preboreal Oscillation.
If the plant stomata data are correct, the increase in atmospheric CO2 that has occurred over the last 150 years is not anomalous. Past CO2 increases of similar magnitude and rate have not caused ocean acidification.
Conclusion
Once again, we have an environmental catastrophe that is entirely supported by predictive computer models and totally unsupported by correlative and empirical scientific data. We can safely pitch ocean acidification into the dustbin of junk science.