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CCL Monthly Conference Call – Saturday, February 2, 2013, 12:45 pm Guest speaker: Dr. Martin Tresguerres, Scripps Institution of Oceanography Dr. Tresguerres will shed some light on global warming’s evil twin – ocean acidification, which could lead to a collapse of the marine food chain if left unchecked. He is currently working with a four-year grant from the National Science Foundation to study the effect of ocean acidification on coral. He’ll share some preliminary findings from that study. February Conference Call Ocean acidification is the name given to the ongoing decrease in the pH of the Earth’s oceans, caused by the uptake of anthropogenic carbon dioxide (CO2) from the atmosphere (measured since the 1950’s). About 30–40% of the carbon dioxide released by humans into the atmosphere dissolves into the oceans, rivers and lakes. To maintain chemical equilibrium, some of it reacts with the water to form carbonic acid. Some of these extra carbonic acid molecules react with a water molecule to give a bicarbonate ion and a hydronium ion, thus increasing the ocean's "acidity" (H+ ion concentration). Between 1751 and 1994 surface ocean pH is estimated to have decreased from approximately 8.25 to 8.14, representing an increase of almost 30% in H+ ion concentration in the world's oceans. pH measures the concentration of H+ on a non-linear scale (logarithmic), consequently slight pH changes (8.1 to 7.8 – his recent data) represent huge changes in acidity. The lower the pH, the higher the acidity . The pH of the ocean is increasing at a very rapid rate which is unprecedented in the history of the earth. He suggests it may be too fast for organisms to adapt – some will be able to cope better than others. This increasing acidity is thought to have a range of direct undesirable consequences such as depressing metabolic rates and affecting metabolic processes in some organisms. Dr. Tresguerres studies cell biology and processes in corals sharks, crustaceans and others to look at how these organisms adapt (or not) to ocean acidification. Other chemical reactions are also triggered which result in an actual net decrease in the amount of carbonate ions available. In the oceans, this makes it more difficult for marine calcifying organisms, such as coral and some plankton, to form biogenic calcium carbonate, and existing structures become vulnerable to dissolution. Thus, ongoing acidification of the oceans also poses a threat to the food chains connected with the oceans. Ocean acidification, which like global climate change is driven by increased levels of carbon dioxide, has been regarded by climate scientists as the "equally evil twin" of global climate change. Largely from Wikipedia http://en.wikipedia.org/wiki/Ocean_acidification Ocean Acidification Illustration Ocean Acidification: The Other Carbon Dioxide Problem Fundamental changes in seawater chemistry are occurring throughout the world's oceans. Since the beginning of the industrial revolution, the release of carbon dioxide (CO2) from humankind's industrial and agricultural activities has increased the amount of CO2 in the atmosphere. The ocean absorbs about a quarter of the CO2 we release into the atmosphere every year, so as atmospheric CO2 levels increase, so do the levels in the ocean. Initially, many scientists focused on the benefits of the ocean removing this greenhouse gas from the atmosphere. However, decades of ocean observations now show that there is also a downside — the CO2 absorbed by the ocean is changing the chemistry of the seawater, a process called ocean acidification. http://www.pmel.noaa.gov/co2/story/Ocean+Acidification Questions 1. Any possibility of carbon sinks in the ocean? Variability exists in the ocean but he has no knowledge of potential side effects of interference. 2. Can the process be mitigated? CO2 in the atmosphere will continue to rise for seeral decades after emissions have halted. Urgent to dramatically reduce rate of carbon dioxide emissions. 3. How does ocean acidification vary with depth and latitude? Complex – upwellings, and topography will influence values. CO2 has higher solubility in colder temperatures In general, pH data refers to ocean surface where most organisms live Other stresses on ocean organisms include pollution and increased water temperature. Organisms are very resilient, but require more energy to cope with a single stress. Multiple stresses leaves even less energy for metabolic processes such as reproduction, digestion, etc. He is doing some research in this… how stresses affect the cellular functions of various organisms . .