Will rising carbon dioxide levels really boost plant growth?

New research finds more CO₂ can actually make most plants smaller in the long term— but the story for crops isn't so simple

Although experiments with CO₂ enhanced crop yields look promising, it might not be the answer to the future of farming (Alamy)

Plants have become an unlikely subject of political debate. Many projections suggest that burning fossil fuels and the resulting climate change will make it harder to grow enough food for everyone in the coming decades. But some groups opposed to limiting our emissions claim that higher levels of carbon dioxide (CO₂) will boost plants’ photosynthesis and so increase food production.

New research published in Science suggests that predicting the effects of increasing CO₂ levels on plant growth may actually be more complicated than anyone had expected.

To understand what the researchers have found out requires a bit of background information about photosynthesis. This is the process that uses light energy to power the conversion of CO₂ into the sugars that fuel plant growth and ultimately provide the food we depend on. Unfortunately, photosynthesis is flawed.

Molecules of CO₂ and oxygen are similar shapes and the key mechanism that harvests CO₂, an enzyme with the catchy name of RuBisCO, sometimes mistakes an oxygen molecule for one of CO₂. This wasn’t a problem when RuBisCO first evolved. But about 30 million years ago CO₂ levels in the atmosphere dropped to less than a third of what they had been.

With less CO₂ around, plants began mistakenly trying to harvest oxygen molecules more often. Today this is often a substantial drain upon a plant’s energy and resources.

As it gets hotter, RuBisCO becomes even more prone to errors. Water also evaporates faster, forcing plants to take measures to avoid drying out. Unfortunately, stopping water getting out of their leaves also stops CO₂ getting in and, as RuBisCO becomes starved of CO₂, it wastes more and more of the plant’s resources by using oxygen instead.

At 25C, this can consume a quarter of what the plant produces – and the problem becomes more extreme as temperatures rise further.

However, some plants developed a way to avoid the problem by pumping CO₂ to the cells where the RuBisCO is located to turbocharge photosynthesis. These are known as C4 plants, as opposed to normal C3 plants which can’t do this.

C4 plants can be much more productive, especially under hot and dry conditions. They came to dominate Earth’s tropical grasslands from 5 million to 10 million years ago, probably because the world became drier at this time and their water use is more efficient.

Maize (corn) and sugar cane are C4 plants but most crops are not, although a project initially funded by the Bill and Melinda Gates Foundation has been seeking to improve yields in rice by adding C4 machinery to it.

Corn is more productive in hot, dry conditions (Alamy)

Most models of how plant growth and crop yields will be affected by the CO₂ released by burning fossil fuels have assumed that regular C3 plants may perform better. Meanwhile, the RuBisCO in C4 plants already gets enough CO₂ and so increases should have little effect on them. This has been supported by previous short-term studies.

The new Science paper reports data from a project that has been comparing C3 and C4 plants for the past 20 years. Their findings are surprising. As was expected, for the first ten years, C3 grasses grown under extra CO₂ did better – but their C4 equivalents did not.

However, in the second decade of the experiment the situation reversed, with the C3 plants producing less biomass under higher levels of CO₂ and the C4 plants producing more.

It seems that this perplexing result may be because as time went by, less nitrogen was available to fertilise growth of plants in the C3 plots and more in the C4 plots. So the effect was not just due to the plants themselves but also to their interactions with the chemistry of the soil and its microbes.

These results suggest that the way that changes in CO₂ affect established ecosystems are likely to be complex and hard to predict. They may hint that, as CO₂ in the atmosphere increases, C4 tropical grasslands could perhaps absorb more carbon than expected, and forests, which are predominantly C3, might absorb less. But the exact picture is likely to depend on local conditions.

What this means for food production may be more straightforward and less comforting than at first glance. These results are from grasses that survive and continue to grow year on year. But current cereal crops are “annual plants” that die after one season and have to be replanted.

As a result, they don’t have the opportunity to build up the soil interactions that seem to have boosted growth of the C4 plants in the experiment. We can’t expect that our food security problems will be solved by C4 crop yields increasing in response to CO₂ as they did in the experiment. Similarly, the eventual fall in biomass seen in the C3 plots shouldn’t happen in C3 annual crops.

Stuart Thompson is a senior lecturer in plant biochemistry at the University of Westminster. This article was originally published on TheConversation.com