Map Oxbridge Applications, 58 Buckingham Gate, London, SW1E 6AJ

It’s December, and for many of you reading this, you will be shortly doing your formal application interviews at Oxbridge and Cambridge – good luck! You have been preparing for this moment and in the days running up to your interviews, please take the time to get some rest and prepare mentally. Hopefully no last minute panicked revision is required but rather just a calm review of your notes and recent studies.

While I am sure you have all had plenty of interview preparation advice, I thought I would use this blog to touch upon climate change, which has been a hot topic for years, but of course has been in the news a lot recently given the climate change talks occurring in Paris. Interviews often have a set list of questions prepared for the interview, but it is common for key issues in the media (that are science related!) to also be discussed in the interviews.

While climate change and the increase in global average temperatures gets a lot of media attention, this blog will focus on the flip side of climate change —the massive absorption of CO2 by the ocean—which has received far less attention. The planet’s seas quickly absorb 25 to 30 percent of humankind’s CO2 emissions and about 85 percent in the long run, as water and air mix at the ocean’s surface. We have “disposed” of 530 billion tons of the gas in this way, and the rate worldwide is now one million tons per hour, faster than experienced on earth for tens of millions of years. We are acidifying the ocean and fundamentally changing its remarkably delicate geochemical balance. Scientists are only beginning to investigate the consequences, but comparable natural changes in our geologic history have caused several mass extinctions throughout the earth’s waters.

That careful balance has survived over time because of a near equilibrium among the acids emitted by volcanoes and the bases liberated by the weathering of rock. The pH of seawater has remained steady for millions of years. Before the industrial era began, the average pH at the ocean surface was about 8.2 (slightly basic; 7.0 is neutral). Today it is about 8.1.

Although the change may seem small, similar natural shifts have taken 5,000 to 10,000 years. We have done it in 50 to 80 years. Ocean life survived the long, gradual change, but the current speed of acidification is very worrisome. Emissions could reduce surface pH by another 0.4 unit in this century alone and by as much as 0.7 unit beyond 2100. We are hurtling toward an ocean different than the earth has known for more than 25 million years.

About 89 percent of the carbon dioxide dissolved in seawater takes the form of bicarbonate ion, about 10 percent as carbonate ion, and 1 percent as dissolved gas. Modern marine life has evolved to live in this chemistry. A wide variety of organisms use carbonate ion to manufacture their skeletons: snails, urchins, clams, crabs and lobsters. And notably, it forms the calcified plates of microscopic phytoplankton that are so abundant and crucial to the entire marine food chain. Meanwhile carbon dioxide levels influence the physiology of water-breathing organisms of all kinds, which for most creatures has been optimized to operate in a narrow range of dissolved CO2 and ocean pH.

We are now carrying out an extraordinary chemical experiment on a global scale. Our fossil-fuel emissions raise the dissolved CO2 levels in the ocean, which reduces carbonate ion concentrations and lowers pH. The ocean’s sunlit surface layer (the top 100 yards or so) could easily lose 50 percent of its carbonate ion by the end of this century unless we reduce emissions dramatically. Marine animals will find it harder to build skeletons, construct reefs, or simply to grow and breathe. Compared with past geologic events, the speed and scale of this conversion is astonishing.

If a topic such as this does arise in an interview setting, it is key to remember that as a whole, humanity does not know what the implications of acidification will be. However, based off of our knowledge of biology and chemistry, we can make some hypotheses. Indeed, you could be asked what the impact of acidification could be, and you should try to come up with as broad an answer as possible – ranging from the chemistry spectrum (impact on pH and carbonate ion concentration) through to the ecological (food web impact). Any answer is applicable, as long as you can back it up with a sound scientific argument, so see what ideas you can come up with!

Oxbridge Applications Logo

Our Oxbridge-graduate consultants are available between 9.00 am – 5.00 pm from Monday to Friday, with additional evening availability when requested.

Oxbridge Applications, 58 Buckingham Gate, London, SW1E 6AJ

Added to cart

View Cart