Science
 
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Overview

Potential Response
Increasing acidification may speed the breakdown of organic matter by bacteria, reducing oxygen levels, affecting marine life and potentially releasing other greenhouse gases.

Researcher
Steven Hallam
Institute
University of British Columbia


Background
Ocean acidification is thought to be contributing to low-oxygen zones in the oceans, which offer fertile breeding grounds for organisms that capture CO2 but do not photosynthesise and so do not release oxygen into the waters. When these organisms die, they are broken down by bacteria, a process which consumes more of the low levels of oxygen in the area and releases carbon dioxide. This eventually leaves the seawater unable to support advanced aquatic life.

If oxygen concentrations in the water fall to an extremely low level, the carbon compounds in these plants are converted into nitrous oxide, not carbon dioxide, which could escape into the atmosphere.

Nitrous oxide is a greenhouse gas 300 times more powerful than carbon dioxide. It also attacks the ozone layer and causes acid rain.
 
Planned Research
Research is needed to determine whether these effects can be observed in the Arctic Ocean, and if there are any correlations between increasing CO2 levels with increasing biological breakdown of organic matter.

To do so oxygen levels will be analysed at different depths using an oxygen sensor. Microbes and bacteria that may increase deoxygenation of the water will also be analysed.



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