Carbon dioxide (CO2) is a greenhouse gas, that humans are releasing into the atmosphere at rates exceeding historical values. In 2011, CO2 accounted for 84% of all greenhouse gas emissions, and between 1990 and 2011 emissions had increased by 10%. We know that the release of greenhouse gases are increasing air temperatures. However, this increase is not only affecting the atmosphere, it is also having an impact on the ocean as well. CO2 in the atmosphere mixes with the ocean via gas exchange. This causes a chemical reaction to occur in the ocean that is causing changes in both biological and physical properties of the ocean. These changes can have a serious impact on life as we know it.
Human activities, such as the burning of fossil fuels for energy, are increasing the amount of carbon dioxide (CO2). This is having an impact on the ocean, most notably to the types of organisms pictured to the right.
Take a moment and answer the following questions about this image.
In this activity you will investigate the following research challenge...
What relationship is there, if any, between increased levels of carbon dioxide in the atmosphere and the physiological changes that are occurring in calcifying organisms.
Analyze the datasets below to learn more about Ocean Acidification. Investigate each piece of evidence and answer the investigation questions for each dataset. After viewing all of the data, continue to the Explanation page for instructions on how to answer the Challenge question. You will need to justify your answers based on the evidence you review here.
When you're done investigating each dataset, continue to the last section.
The graph above shows different scenarios based upon population, economic growth, etc. as predicted by the IPCC (Intergovernmental Panel on Climate Change) The top chart shows projected CO2 levels from 2000 to 2100, the bottom global pH levels for the same timeframe. The different lines represent different emission scenarios. (credit IPCC).
This graph combines historical data with predictions made using models to show pH and oceanic dissolved carbon dioxide over time.
This graph is known as a Bjerrum plot. It shows the proportion of dissolved carbon dioxide (CO2), bicarbonate (HCO3-), and carbonate (CO32-) at different pH levels in a solution at equilibrium.
Credit/Source: TBD
The graph above shows Atmospheric carbon dioxide levels from the 1800's to predicted levels in 2300. Two different IPCC models are used in this graph. IS92a with carbon concentrations increasing at 1% per year after 1990 and is what would be predicted if we continue emitting CO2 at the same rate we do today. S650 is a stabilization scenario, where we begin to decrease CO2 emissions and eventually Atmospheric CO2 levels stabilize.
A number of different species from each of the different major group were subjected to increased CO2 levels. The species response was then recorded as either: a. negative, b. positive, c. static, or d. parabolic (responded in a non-linear fashion, the species had a negative response both above and below present day CO2 levels). (table edited from: Doney et. al., 2009.) Note: The numbers for each species response do not add always add up because this information was taken from a review of data collected from multiple experiments, and in some cases a species could have shown multiple responses in different studies, depending on technique and experiment parameters.
Above are scanning electron microscopy (SEM) images of coccolithophores. The coccolithophores were subjected to different levels of CO2 (described in the table on the right).
The images above are scanning electron microscopy (SEM) of M. mercenaria (a type of saltwater clam) for 36 days. They were grown under different CO2 levels ranging from 250 ppm to 1500 ppm.
The graphs above show the relationship between net calcification and Partial Pressure of CO2, Concentration of carbonate ions, and pH for two different species, mytilus edulis (blue mussel) and crassostrea gigas (pacific oyster). Net calcification is given in µmol CaCO3 g FW-1h-1 or how much calcium carbonate will be lost per hour.
Recall that the research challenge you are trying to address is:
What relationship is there, if any, between increased levels of carbon dioxide in the atmosphere and the physiological changes that are occurring in calcifying organisms.
As you consider the data you just investigated, consider the following questions:
Assessment
Additional Instructions
As you take into account the data you just viewed, consider questions #1-3 as you try to summarize what you have learned. Then consider questions #4-7 and try to extrapolate your knowledge based on what you have learned.