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Global Carbon Cycle

Every year around 10 Gigatons of carbon (that’s 10 x 109 tons of carbon per year, written as GtC/yr) is emitted by combustion of fossil fuels. Where does all this carbon come from? Where does it all go? How does it get there? And, is it possible to get it there faster? These questions and more are the main focus of Biocycle, also known as the Denning Research Group. With all the recent talk about climate change, going green, and reducing carbon footprints, these questions are more important than ever. Our research, and the research of groups like ours, will help to answer these questions, provide knowledge, and lead to change.

Anthropogenic carbon emissions are strictly regulated and documented, so the 10 GtC/yr is a well defined approximation. Where does all this carbon go? From taking measurements, either physically or remotely, we know that about half is added to the carbon in the atmosphere. Another 2 GtC/yr is dissolved into the oceans. This carbon is documented by tracing the concentrations of radioactive carbon dissolved into the oceans. Then 2 GtC/yr remain that land surfaces need to account for.

Plants photosynthesize, taking in CO2 and H2O to make sugars to grow and emitting O2. Plants also respire, which emits CO2back into the atmosphere. There is a slight discrepancy in the calculated numbers for what plants are able to photosynthesize and what is respired. This discrepancy and the fact that photosynthesis as currently modeled does not account for the entire 2GtC/yr that must be absorbed into terrestrial biospheres means that more research must be done. There must lie a larger sink of carbon – a larger area that absorbs carbon- than was previously believed to exist. The goal of Biocycle and global carbon cycle science is to determine the location of this significant sink, why and how it is able to absorb more carbon than was previously believed. Do the conditions in this area allow it to absorb more carbon? Can we recreate these conditions in other areas to absorb even more carbon? Is there a cap on how much carbon this sink can absorb? The answers to these questions will undoubtedly be instrumental in future climate change policy.

The most important thing we know at the moment is that we don’t know enough. Continued research and public outreach are vital to this branch of science. With every experiment, every project, we are learning. Every success and even every failure gets us that little bit closer to the answers that will shape the future of life on the planet.

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  1. […] human activity (i.e. anthropogenic) are accumulated in the atmosphere. We know from intensive study of the carbon cycle and good record-keeping that CO2 has increased from human activity. The confusion, controversy, […]